"Creation scientists do not consider these as true “extinction” events. Instead, these horizons are interpreted as major shifts in the burial pattern of fossils during the Flood." — Jeffrey Tomkins and Tim Clarey, Institute for Creation Research, 20231
"A creation/Flood framework would have much more difficulty dealing with a global pattern of uniform sharp 'cut-off' at the K-T boundary, rather than a blurry picture, which appears to be the reality." — Carl Wieland, Creation Ministries International, 19982
Summary
A mass extinction is a level in the rock where many kinds of fossils stop at once. Five such levels stand out in the marine record: the end of the Ordovician, the Late Devonian, the end of the Permian, the end of the Triassic and the end of the Cretaceous. These are the "Big Five." Smaller ones sit between them.
This article asks four questions of each. What died? How abruptly, measured in the rock of a single section? What came back above it, and in what order? And where do young-earth creationist models place it: inside Noah's Flood, at its end, or after it?
The article works from the order of the layers alone. Ages in years appear only when quoting what mainstream geologists claim; nothing here depends on them.
Eight conclusions, stated first.
- The extinctions are real patterns in the rock, not artefacts of how the timescale is divided. Each shows up in single sections, where the order of the beds is not in dispute. At Meishan in China, the classic end-Permian section, most species stop in one bed. In the Hell Creek badlands of Montana, the youngest dinosaur bone found in place sits 13 cm below the layer where Cretaceous pollen disappears and fern spores take over.3 A database check run for this article agrees with the published curves: of 602 marine genera that enter the last Permian stage and can be placed in single stages, 387 have no record above it, by far the largest such loss in the record.4
- The order above each boundary is the order of a recovery, and it repeats. Above the end-Permian come a few holdovers that soon vanish, a handful of hardy survivors, dwarfed shells and mats of microbes. Swimmers such as ammonoids and conodonts rebound within the Lower Triassic; animals fixed to the sea floor stay scarce until the base of the Middle Triassic, and reefs and coal are missing throughout. About two-thirds of the genera found both below and above the Lower Triassic are missing from the Lower Triassic itself, and so is every one of the 53 demosponge genera among them, most of them reef builders.5 Above the end-Cretaceous come a fern spike on land and, in the sea, one surviving plankton species followed by the first new ones, then burrowing animals.
- Every active young-earth model puts four of the five inside the Flood year. The Institute for Creation Research (ICR) assigns the Cambrian to Mississippian rocks to the first 40 days and the end-Permian and end-Triassic to Days 40 to 90.6 No active camp puts the end of the Flood below the Cretaceous; the 1996 group that did withdrew its model in 2000.7
- The end-Cretaceous splits the young-earth camps. One camp, founded by Steven Austin and colleagues in 1994 and carried by John Whitmore, Paul Garner and Kurt Wise, ends the Flood at or just above it. ICR's Tim Clarey and Davis Werner put it at the Flood's high-water mark, Day 150, with months of Flood still to come; Andrew Snelling and Michael Oard also place the end of the Flood well above it.
- The camps also split on whether the extinctions happened at all. ICR says there are "no real extinction events in the rock record," only the last level at which each group was buried.8 Most other young-earth writers, including the founders of the end-Cretaceous camp, treat the losses as real deaths caused by the Flood.9
- The "only burial order" reading fails a test it sets itself. If trilobites, rugose and tabulate corals, fusulinid forams and productid brachiopods were still alive in the sea after the end-Permian level, the Flood went on burying sea creatures in great numbers: 404,784 later Mesozoic marine occurrences against 124,185 from the whole Permian. At even a hundredth of their last-Permian share, those five groups should have left about 9, 53, 6, 91 and 584 fossils in that later rock. It holds 0, 3, 0, 1 and 8 outside the first Triassic substage.10 A companion prediction, that extinctions fall at the Flood's megasequence boundaries, fails for three of the five on ICR's own figure.1
- The "real deaths" reading survives that test but leaves the recoveries unexplained. On every model the whole Early Triassic recovery, with its dwarfs, its missing reefs, its missing coal and its stepwise rebuilding of food webs, was laid down in days. On the end-Cretaceous boundary, the whole Cenozoic recovery has to fit into the few centuries before the Ice Age, which the founders of that camp put at about five centuries after the Flood.11 No young-earth source found for this article addresses the dwarfing, the reef gap or the stepwise rebuilding at all.
- The critics of the mainstream picture have real points. A sampling effect named after Signor and Lipps makes sudden extinctions look gradual, and it can also blur the reverse. Two of the Big Five are as much failures of new forms to appear as surges of loss. The timing of the land turnover in South Africa is in open dispute, and land plants may not have suffered a mass extinction at the end of the Permian at all.
Verdict. Against the reading of mass extinctions as artefacts of burial order: that reading predicts fossils that are not there. For the young-earth view that the Flood itself was the killer, the position is unfinished: the deaths fit a catastrophe, but the ordered recoveries above them have no published young-earth account.
Part 1: What counts as a mass extinction, and which ones stand out
How the five were found
The "Big Five" come from a 1982 paper by David Raup and Jack Sepkoski of the University of Chicago. They compiled the first and last appearances of thousands of marine animal families and asked which intervals lost far more families than the long-run trend predicts. Their answer was four, not five: "four mass extinctions in the marine realm are statistically distinct from background extinction levels. These four occurred late in the Ordovician, Permian, Triassic, and Cretaceous periods. A fifth extinction event in the Devonian stands out from the background but is not statistically significant in these data."12 The Late Devonian joined the list by convention.
Later work with genera instead of families sharpened the picture and also blurred it. Richard Bambach, Andrew Knoll and Steve Wang ranked the extinction intensity of every Phanerozoic substage and found "a continuous distribution, with the five traditionally recognized mass extinctions located in the upper tail." Compared with their neighbours in time, "only the end-Ordovician, end-Permian, and end-Cretaceous extinction intensities appear as outliers."13 The other two lost diversity mainly because few new genera appeared: "about two-thirds of the diversity loss in the late Frasnian and almost 60% in the end-Triassic can be ascribed to origination failure, not elevated extinction."13 Bambach's 2006 review found 18 intervals that fit Sepkoski's definition of a mass extinction and concluded that "mass extinctions are not a homogeneous group of events."14 John Alroy, working with occurrence data rather than published ranges, found "no sharp distinction between background and mass extinctions" across the whole record, while confirming that the end-Permian and "several" others "were particularly severe."15
So the young-earth complaint that mass extinctions are "arbitrarily defined," made by Kurt Wise and Matthew Richardson, is half right.16 The threshold for calling an interval a mass extinction is a convention. The end-Permian is not, and young-earth writers have said so: Oard called it "the most singular extinction event in the supposed history of life."17 It is the largest loss on every measure, and Wise and Richardson's own data show it most clearly of all: of 2,556 species they found in the last Permian stage, only 4 occur on both sides of the boundary within 2 degrees of each other, 0.2 %, where ordinary stage boundaries run at about 3 to 17 %.16
How big they were
The size of each loss depends on whether species, genera or families are counted, and on how the counts are corrected. The most careful recent estimates are smaller than the figures usually quoted. Steven Stanley of the University of Hawaii, correcting for the way rare fossils make extinctions look earlier than they were, put the end-Permian at "only ∼81% of marine species," not the "90–96%" often quoted, and wrote that "Life did not nearly disappear at the end of the Permian, as has often been claimed."18 For genera he estimated 42 to 43 % for the end-Ordovician, 16 to 20 % for the Frasnian event of the Late Devonian, and 38 to 40 % for the end-Cretaceous.18 He left out the end-Triassic because "its timing and list of marine victims remain controversial."18
Creationist writers quote the larger figures. Emil Silvestru repeats National Geographic's "some 90 percent of the planet’s species" for the end-Permian;19 Clarey's table gives 96 % of species.20 Neither number is wrong as a citation, but both are older estimates that later work has revised downward.
A check against the whole database
The published curves rest on compilations that a reader cannot easily rerun. So this article ran its own check on the Paleobiology Database, the largest open compilation of fossil occurrences. For every animal genus with fossils of known age, it took PBDB's first and last appearance, placed each in one of the 101 named stages, and asked, stage by stage, what share of the genera that entered a stage from below have no record above it.4 Only the order of the stages matters here. The stage ages serve as labels.
| Stage at the top of the event | Marine genera entering from below | Last seen in that stage | Share | New genera, share of those leaving upward |
|---|---|---|---|---|
| Katian, end-Ordovician first pulse | 334 | 157 | 47.0 % | 30.9 % |
| Hirnantian, end-Ordovician second pulse | 256 | 62 | 24.2 % | 9.3 % |
| Frasnian, Late Devonian | 411 | 100 | 24.3 % | 15.9 % |
| Famennian, Late Devonian | 370 | 103 | 27.8 % | 29.9 % |
| Changhsingian, end-Permian | 602 | 387 | 64.3 % | 10.5 % |
| Rhaetian, end-Triassic | 346 | 146 | 42.2 % | 10.0 % |
| Maastrichtian, end-Cretaceous | 544 | 233 | 42.8 % | 17.5 % |
| Typical stage, for comparison: Toarcian | 310 | 65 | 21.0 % | 20.7 % |
Three things stand out, and all three match the published work. The end-Permian is far ahead of every other well-sampled stage. The Late Devonian does not show as one great loss, and its Frasnian stage made few new genera, which is Bambach's "origination failure." And above each event the share of new genera climbs back: after the end-Permian it runs 10.5 % in the last Permian stage, about 26 % in each of the two Lower Triassic stages, and 45.9 % in the first Middle Triassic stage, the Anisian. Cambrian stages score as high as the end-Permian on these measures, but on samples of a few dozen genera. The numbers are raw. They are not corrected for how much each stage has been collected, so they check the published curves rather than replace them.
The sampling effect that cuts both ways
A fossil's last appearance is almost never the moment its species died. A rare animal is found less often, so its last fossil usually sits some way below the true extinction level. When many species die at once, their last fossils therefore scatter below the kill horizon, and a sudden event looks gradual. This is the Signor-Lipps effect, named for Philip Signor and Jere Lipps, who described it in 1982: "the incorrect assignment of extinctions that occurred during a crisis to an interval preceding the crisis because of the incompleteness of the fossil record," in Stanley's definition.18
Charles Marshall showed it in a single section. On Seymour Island, Antarctica, ammonites "disappeared gradually over a stratigraphic interval 10–50 m below the boundary" if the record is read literally, yet the pattern "is consistent with a sudden mass extinction" at the end-Cretaceous, and the iridium layer falls where his method predicts the extinction should be. He was careful to add that gradual scenarios spread over as much as 20 m also fit, so that "without saturation collecting near the K-T boundary it will be impossible to distinguish between gradual and sudden extinction scenarios" from the ammonites alone.21
The effect also runs the other way. Steven Holland and Mark Patzkowsky simulated how fossils accumulate in real sedimentary sequences and found that last appearances "tend to cluster at subaerial unconformities, surfaces of forced regression, flooding surfaces and intervals of stratigraphical condensation." A long period of raised extinction can therefore look like a sudden pulse. "With the possible exception of the end‐Cretaceous," they wrote, the mass extinctions show exactly such clusters, which "may represent brief pulses of elevated extinction" but "are equally likely to form by stratigraphical processes."22 This is the mainstream version of a point Clarey makes from a young-earth survey: that many sudden-looking extinctions sit at sudden changes of rock type.20 Both are right that the shape of an extinction in one section can be an artefact. Neither shows that the extinction itself is one.
Part 2: The end-Permian, bed by bed
The kill in one section
The reference section for the end of the Permian is a quarry at Meishan in Zhejiang, China. Its beds are numbered from the bottom up. The boundary is defined by the first appearance of a small conodont, Hindeodus parvus, at the base of Bed 27c. The extinction lies a little lower. Ian Metcalfe and colleagues place "the main mass extinction level in Bed 25," with another conodont restricted "to the narrow boundary interval immediately above," in Beds 26 to 29. Bed 28 lies "just 8 cm above the GSSP boundary."23 A study of 162 genera and 333 species through the section "confirms a sudden extinction event."24
Meishan is thin at this level, and its students say so. At Shangsi, another Chinese section, the boundary conodont first appears "about 5 m above the highest level from which a typical Permian fauna is recovered," which, Metcalfe's team wrote, "may suggest that that some section may be missing at Meishan."23 Where the sequence is condensed, a loss spread over some thickness of rock elsewhere is squeezed into a few beds. That is Holland and Patzkowsky's warning from Part 1, made by the people who measured the section.
Looking across seven Chinese sections and 537 species, Haijun Song and colleagues found two steps, not one. The first, in the latest Permian, removed "57% of species, namely all plankton and some benthic groups, including algae, rugose corals, and fusulinids." The second, in the earliest Triassic, removed "71% of the remaining species."25 Between them lie the first Triassic beds, where a few Permian holdovers persist. In the Paleobiology Database, 107 of the 115 productid brachiopod records above the Permian come from the Griesbachian, the first Triassic substage, among them Paryphella, Fusichonetes and Spinomarginifera. Above it there are essentially none.10
On land
The best land record is the Karoo Basin of South Africa, where the Permian Daptocephalus fauna gives way to the Triassic Lystrosaurus fauna. The mass-death beds of the Karoo are treated in Fossil Graveyards; what matters here is the order. Roger Smith and Jennifer Botha found "a 69% mass extinction of Late Permian terrestrial vertebrates" followed by "a lesser extinction event (31%)" involving four taxa that crossed the boundary, and a "main extinction zone" about 40 m thick at two separate sections.26 Pia Viglietti and colleagues, with a larger database, found extinction spread "through a protracted interval," "initially co-occurring with low origination rates," with the peak "near the Daptocephalus–Lystrosaurus declivis Assemblage Zone boundary."27
Two disputes run through this record, and both favour caution. Robert Gastaldo's team accepts "an abrupt turnover" between the two faunas but argues that it happened before the marine extinction.28 That argument rests on radiometric dates, which this series sets aside, so it is noted and not weighed here. And Hendrik Nowak and colleagues found that "evidence for a mass extinction among plants in the latest Permian is not robust," because the plant record is so unevenly sampled.29 Tomkins and Clarey make a related observation from the young-earth side: land plants show "a more tiered extinction, with many of their fossils extending well into the Triassic."1 On this they are right. The end-Permian was a marine catastrophe first.
What came back, and in what order
Above the kill, the same sequence turns up section after section. It is the core of this article's question, so it is set out in order.
- Hardy survivors take over. The aftermath is dominated by what Song and colleagues call "opportunistic organisms," naming "cyanobacteria, small foraminifers, Claraia bivalves, and linguloid brachiopods."30 On land the earliest Triassic is dominated by Lystrosaurus. Sean Modesto has argued that the textbook label "disaster taxon" does not fit it, and that at most its species "could be described as opportunistic species."31
- Everything is small. Jonathan Payne's global database of snail shells found that "no specimens of unambiguous Early Triassic age larger than 2.6 cm have been reported, in contrast to common 5–10-cm specimens of both Permian and Middle Triassic age." The shrinking was sudden and the return slow: "The loss of large gastropods is abrupt even at a fine scale of stratigraphic resolution, whereas the return of larger individuals in the Middle Triassic appears gradual when finely resolved."32 Palaeontologists call this the Lilliput effect.
- Much is missing. Of the 570 animal genera that the Paleobiology Database records both in the Permian or earlier and in the Middle Triassic or later, 387, or 68 %, have no record in the Lower Triassic between. All 53 demosponge genera among them are missing, most of them reef builders such as Amblysiphonella and Girtycoelia.5 Such "Lazarus taxa" could be an artefact of poor collecting. Paul Wignall and Michael Benton tested that and found "no link with the abundance of fossiliferous sites and the proportion of Lazarus taxa," concluding that the gaps reflect "the extreme rarity of organisms at this time."33 The PBDB numbers agree on the sampling point: the whole Lower Triassic holds 20,730 marine occurrences, about the same as the last Permian stage alone. But preservation matters too. An exceptionally preserved Lower Triassic fauna from Idaho includes leptomitid sponges known otherwise from the Cambrian and Ordovician, "a 200–million year Lazarus taxon."34
- The sea floor stays quiet, then stirs in steps. In the Werfen Formation of the Italian Dolomites, 250 to 700 m of Lower Triassic shelf sediment,35 Richard Hofmann reports that in the lowest Triassic member "bioturbation virtually vanished," that "a first significant rebound in ichnodiversity" comes in the lower Siusi Member, that the next two members "again record a drop," and that the highest member "signifies the most advanced recovery stages."36 William Foster and colleagues, sampling 328 fossil beds in six Werfen sections, found two further bursts of extinction within the recovery, "not only in the Dienerian, as previously recognised, but also around the Smithian/Spathian boundary."35 In Utah and Nevada, the last Lower Triassic stage still shows "persistent small size, low average ichnofabric index, low bedding-plane coverage, and reduced tiering" of burrows.37
- Swimmers return first; animals fixed to the sea floor return last. Song, Wignall and Alexander Dunhill found that non-motile animals, those fixed to or lying on the sea floor, fell "from more than 500 genera in the Late Permian to fewer than 100 genera in the Early Triassic" and reached pre-extinction levels only "after a rapid rebound in the initial Middle Triassic."30 By contrast, recovery "was rapid for some nektonic-pelagic groups, such as ammonoids and conodonts."34 Marine genus diversity as a whole "attained pre-extinction levels in the early Anisian," the first Middle Triassic stage.30 That is where the PBDB check finds the peak of new genera.
- No reefs. Reefs built by animals and algae vanish at the boundary. Brian Kelley and colleagues summarise earlier work that "metazoan-algal reefs were absent for 8−10 m.y. following extinction," and show that when they returned, at the top of the Lower Triassic, "calcareous sponges, calcareous algae, and early scleractinian corals occurred progressively."38 The corals of the returning reefs were a new group, the scleractinians, not the rugose and tabulate corals of the Paleozoic.
- No coal. Gregory Retallack and colleagues: "Early Triassic coals are unknown, and Middle Triassic coals are rare and thin." They found the sedimentary settings that hold coal elsewhere, with "fluctuating sea levels and sedimentary facies and paleosols," present in Lower Triassic rocks without the coal.39 Their explanation, the extinction of peat-forming plants, is weakened by Nowak's finding; the gap itself is not.
How the food web was rebuilt is disputed among mainstream workers, and the disagreement should be reported. Zhong-Qiang Chen and Benton read the record as rebuilt "stepwise from low to high trophic levels," with "a stable, complex ecosystem" not back "until the beginning of the Middle Triassic."40 Song and colleagues found the opposite direction: "animals at high trophic levels recovered faster than those at lower levels."30 Arnaud Brayard's team described an Idaho fauna from the upper Lower Triassic that is already "trophically multileveled ... from primary producers up to top predators."34 And the Middle Triassic Luoping fauna of China added "new trophic levels ... most notably among top predators in the form of the diverse marine reptiles."41 What all four agree on is the frame: a crash at one level, a long interval of impoverished, small-bodied, opportunist-dominated communities, and a return of full complexity some distance up the section.
Part 3: The end-Cretaceous, centimetre by centimetre
The crater left by the Chicxulub impact, and the worldwide layer of ejecta at the boundary, are covered in Impact Craters and the Flood. The chalk below the boundary and the bryozoan limestone above it at Stevns Klint in Denmark are covered in Chalk, Limestone, and the Flood. This part asks only what died, how abruptly, and what came back.
On land: the last dinosaurs and the fern spike
In the Western Interior of North America the boundary is drawn where Cretaceous pollen types disappear. Robert Tschudy and colleagues found that it "occurs at the top of an iridium-rich clay layer" and is marked "by the abrupt disappearance of certain pollen species, immediately followed by a pronounced, geologically brief change in the ratio of fern spores to angiosperm pollen."42 That jump in fern spores, the "fern spike," is the expected first stage of plant succession on devastated ground. Vivi Vajda and colleagues found the same thing, with an iridium layer, in New Zealand: "a diverse flora being abruptly replaced by one dominated by a few species of fern."43
Whether the dinosaurs died out suddenly or dwindled was argued for decades, and the argument turned on statistics. Peter Sheehan's team surveyed the Hell Creek Formation for three years and found "no evidence (probability P < 0.05) of a gradual decline of dinosaurs."44 Stuart Hurlbert and David Archibald replied that the methods "provide no basis for choosing between scenarios of abrupt extinction and gradual decline."45 Their reply cut both ways, and its title says so: "No statistical support for sudden (or gradual) extinction of dinosaurs."
Field work since then has narrowed the gap. The Hell Creek "3-m gap," a barren interval below the boundary once read as a decline, proved partly a problem of where the boundary was drawn: it "actually lies anywhere from –5 to +3 m relative to the contact" between the formations. At Camel Butte, Montana, Tyler Lyson and colleagues fixed the boundary by pollen samples taken centimetres apart and found a horned dinosaur's brow horn "in a poorly rooted, silty, mudstone floodplain deposit located no more than 13 cm below the palynologically defined boundary." Just above it the fern spike begins, with "as much as 80% ferns," and Cretaceous pollen types drop "from 14% in sample 190-1 to 1–3% in the overlying samples."3
Other land animals tell the same story. Nicholas Longrich and colleagues counted 30 lizard and snake species in the last Cretaceous beds of North America and found "only five" in the Paleocene: "Species-level extinction was 83%," and "Survival was associated with small body size."46 Of birds, "at least four separate lineages of archaic birds persisted up to the K–Pg boundary," and none has been found above it.47 The bird record is covered in Archaeopteryx and Bird Origins.
The recovery on land has its own order. At Corral Bluffs near Colorado Springs, Lyson's team found that above the boundary, mammal diversity doubled first; then the largest mammal body size tripled, together with a rise in the number of plant species; and then more large mammals arrived together with "the first appearance of Leguminosae (the bean family)."48 The same team's pollen work at Corral Bluffs found the fern spike followed by "low diversity assemblages often dominated by palm pollen."49 The order is ferns, then palms and a few flowering plants, then a richer forest, then legumes, with the mammals growing in size and number alongside.
In the sea: plankton, ammonites and the first burrows
The open-ocean plankton give the cleanest record, because they lived everywhere and sank everywhere. The standard zones for the first Paleocene stage were set out in 1999 by Richard Olsson and colleagues. The lowest, P0, is the range of a single Cretaceous survivor, Guembelitria cretacea, between the last appearance of the Cretaceous species "at the K/P boundary as delineated by the essentially global iridium spike" and the first appearance of the first new species, Parvularugoglobigerina eugubina.50 Then come, in fixed order, the first appearances of Subbotina triloculinoides, of Globanomalina compressa or Praemurica inconstans, and of Praemurica uncinata.50 The new microperforate species "evolved from the survivor-species Guembelitria cretacea."50
At El Kef in Tunisia, the reference section for the base of the Paleocene, the iridium shows "a millimetre thick pulse-like feature occurring in perfect coincidence with the beginning of the biological crisis." Ammonites there end below it: "A rich assemblage, consisting of at least 17 taxa, occurs in the interval from meters 7 to 2 below the K/Pg boundary."51 That two-metre gap in the very section that defines the boundary is the Signor-Lipps effect at work.
Inside the Chicxulub crater itself, Christopher Lowery and colleagues read the first Paleocene sediment from a drill core. Its numbers are depths in the core, so they decrease upward. Burrows of Planolites and Chondrites "characterize the upper 20 cm of the transitional unit (above 54 cm)," evidence "for benthic life in the crater within years of the impact," on the authors' reading.52 Above that, the lowest sample of the overlying limestone, at 34 cm, holds the first new plankton species, P. eugubina, together with the survivor G. cretacea, and "many other species that originate within Zone Pα first appear a few cm higher in the section (31–32 cm)."52
A few ammonites outlived the boundary for a short time. At Stevns Klint, Marcin Machalski and colleagues found ammonites in the Cerithium Limestone 10 and 37 cm above the base of the 5 to 10 cm boundary clay, the Fiskeler, and concluded that "our results confirm ammonite survival into the Danian for the bulk of the Cerithium Limestone fauna."53 In the whole Paleobiology Database there are 9 ammonite records from the first Paleocene stage against 2,622 from the last Cretaceous stage, and essentially none above.10
Not every group fell at the line. Charles Marshall and Peter Ward's statistics on the molluscs of the European Tethys found "a major extinction at or near the Cretaceous-Tertiary (K-T) boundary," but also "gradual extinction of most inoceramid bivalves well before the K-T boundary."54 Mass extinctions are often a sharp kill laid over losses that were already under way.
Part 4: The other three, and the smaller events
End-Ordovician: two pulses
The first of the five came in two steps. David Harper and colleagues summarise it as "two discrete pulses, both linked in different ways to an intense but short-lived glaciation at the South Pole." The first, "at, or just below, the Normalograptus extraordinarius graptolite Biozone, mainly affected nektonic and planktonic species together with those living on the shallow shelf and in deeper water." The second, "within the N. persculptus graptolite Biozone, was less focused." In all, "about 85% of marine species were removed."55 Seth Finnegan and colleagues put the loss at "an estimated 61% of marine genera globally" and found that falling sea level and tropical cooling "played important roles in the first pulse" in North America.56 The PBDB check shows the same two steps: 47 % of boundary-crossing marine genera last seen in the Katian stage, then 24 % in the Hirnantian.
The order is fixed by graptolite zones that follow one another in the same sequence wherever they are found. On ICR's timetable both pulses fall inside the Tippecanoe megasequence, within the Flood's first 40 days.6 That places the glaciation Harper describes, and a two-step extinction tied to it, inside the opening weeks of the Flood. No young-earth source found for this article discusses the end-Ordovician extinction in particular.
Late Devonian: a crisis of missing newcomers
The Late Devonian is the event that Raup and Sepkoski found "not statistically significant." It was real, but it worked differently. Alycia Stigall's study of the brachiopods and other shallow-sea animals of the time concluded that "the primary cause of biodiversity decline was reduced speciation during the crisis interval, not elevated extinction rates," so that "The Frasnian-Famennian event is, therefore, better termed a “biodiversity crisis” than a “mass extinction.”"57 Bambach's team put about two-thirds of the late Frasnian diversity loss down to origination failure.13 The PBDB check agrees: no single Late Devonian stage shows an outsized loss, but the Frasnian made unusually few new genera. What did collapse was the reef. Stigall notes that the Middle Devonian held "the most geographically widespread metazoan reef ecosystem in Earth’s history, but its extent was reduced by a factor of 5000 following the crisis interval."57 The stromatoporoid-and-coral reefs did not return in that form.
End-Triassic: dinosaurs above, crocodile relatives below
On land, the end-Triassic is best known from the rift basins of eastern North America. Paul Olsen and colleagues analysed "tetrapod footprints and skeletal material from more than 70 localities" and found that "large theropod dinosaurs appeared" just above the boundary, "synchronous with a terrestrial mass extinction," which was "associated with an iridium anomaly ... and a fern spore spike."58 The pattern is the end-Cretaceous pattern in miniature: iridium, ferns, then a new set of dominant animals. In the sea the picture is less clear. Stanley left the end-Triassic out of his estimates because "its timing and list of marine victims remain controversial,"18 and Bambach's team attribute almost 60 % of its diversity loss to origination failure.13 On ICR's timetable the end-Triassic falls late in the Absaroka, close to Day 90; Tomkins and Clarey note that "crocodylomorphs, pterosaurs, and dinosaurs somehow selectively avoided extinction" at this level.1
The smaller events
Bambach counted 18 intervals that meet Sepkoski's definition of a mass extinction.14 The best known of the smaller ones are the end of the Middle Permian, the early Jurassic, the middle Cretaceous and the end of the Eocene. The PBDB check gives their last stages, the Capitanian, Toarcian, Cenomanian and Priabonian, marine extinction shares of 20, 21, 22 and 15 %. The Capitanian also made only 4.5 % new genera, the lowest origination of any well-sampled stage. Stanley points out that the frequently quoted 90 to 96 % for the end-Permian "were incorrectly based on combined data for the Middle and Late Permian mass extinctions," that is, by merging the Capitanian event with the end-Permian one.18
One more extinction belongs in any list but not in this argument. The large mammals of the last Ice Age, mammoths, ground sloths, sabre-toothed cats and many others, died out in rocks that every young-earth model places after the Flood. Austin and colleagues already allowed that the Ice Age "contributed to the megafaunal extinctions of the Pleistocene."11 That event is treated with the post-Flood world in The Ice Age.
Part 5: Where young-earth models put each extinction
Every young-earth model reads most of the fossil-bearing rock as the record of Noah's Flood. So every model must say where each extinction level falls in the Flood year, and whether it records a real death or only the order of burial. The answers below come from the models' own primary papers.
Four of the five are inside the Flood on every live model
The Institute for Creation Research (ICR) gives the most detailed timetable. Tim Clarey and Davis Werner tie each of Sloss's six megasequences, the continent-wide packages of sediment that frame their model, to days of the Flood. The Sauk, Tippecanoe and Kaskaskia, which hold the Cambrian to Mississippian rocks and the end-Ordovician and Late Devonian extinction levels, "may represent the first 40 days of the Flood." "We interpret Days 40 to about 90 of the Flood as corresponding to the Absaroka megasequence," which holds the end-Permian and end-Triassic levels. The Zuni runs "from about Day 90 of the Flood to Day 150," and its top, at the end-Cretaceous, is "the highest point of the Flood."6 The rocks above, the Tejas megasequence, are "the receding phase of the Flood."1
Andrew Snelling of Answers in Genesis puts the end of the Flood "certainly" above the end-Cretaceous, so all five extinctions are Flood events on his model too.59 Kurt Wise and Matthew Richardson place the start of the Flood in the Precambrian-Cambrian rocks and its end "just below the Danian/Selandian boundary," the first stage boundary above the end-Cretaceous.16 On their reading the end-Cretaceous extinction and most of the first Paleocene stage, with its first recovery faunas, were laid down in the closing days of the Flood.
The only published young-earth model that made the end-Permian post-Flood was the 1996 "recolonisation" proposal of four British creationists. In 2000 they wrote: "None of us is satisfied with the model that we proposed in 1996."7 The Flood/Post-Flood Boundary article records that no active camp now puts the end of the Flood below the Cretaceous. So the end-Permian extinction and the whole Early Triassic recovery above it are Flood rock on every model now defended.
The end-Cretaceous divides the camps
The end-Cretaceous is where the boundary fight sits, and the two camps read it in opposite ways.
- The end of the Flood. Steven Austin and five colleagues founded catastrophic plate tectonics in 1994 and wrote: "we tentatively place the Flood/post-Flood boundary at approximately the Cretaceous/Tertiary (K/T) boundary."11 John Whitmore and Paul Garner's criteria put it "somewhere in the Lance or Fort Union Formation" in Wyoming, the two formations that straddle the end-Cretaceous.9 On this reading the extinction is the Flood's last kill, and everything above it, including the whole Paleocene recovery, is post-Flood.
- The high-water mark. ICR puts the end-Cretaceous at Day 150, "when all land animals finally succumbed and drowned," in the words Clarey uses for this view.20 Michael Oard, who places the end of the Flood late in the Cenozoic, wrote that the dinosaurs "simply died in the Genesis Flood (except those dinosaurs likely taken on the Ark, which probably died soon after the Flood)."17 On this reading the Paleocene rocks above the extinction are not a recovery at all. They were laid down by the receding Flood, and their fossils are the next communities it reached.
The full boundary debate, including its arithmetic for the mammals, is in The Flood/Post-Flood Boundary. This article takes only what each camp's placement implies for the extinction and recovery pattern.
Real deaths, or only the order of burial?
Here the young-earth literature splits in a way it rarely acknowledges.
ICR says the extinctions are not extinctions. Jeffrey Tomkins and Clarey: "There are no real extinction events in the rock record, only the last appearance of organisms as they were encapsulated by the tsunami-like floodwaters."8 In their 2023 conference paper: "Creation scientists do not consider these as true “extinction” events. … So-called extinctions are merely the level at which certain fossils were no longer being actively buried."1 Clarey and Werner explain how: "rapid changes in water level that buried completely new types of organisms from new biozones," "the simultaneous inundation of a complete ecological environment at the same approximate elevation globally."6 Clarey called the end-Cretaceous extinction "probably just the last appearance of many organisms in Flood-deposited strata,"20 and he applies the idea to ammonites, which "never really went extinct—they just didn’t get fossilized after a certain level," and "might have survived the Flood."60 Carl Wieland of Creation Ministries International (CMI) put the same view in 1998: in Flood rock, "'extinctions' simply mean points above which there are no more such fossils found buried."2
ICR does not deny that groups died out. Tomkins and Clarey grant that the Flood destroyed pre-Flood environments, so that "a lot of marine animals" went extinct "during or shortly after the Flood," trilobites and many Paleozoic brachiopods and corals among them. "The exact reason for this is unclear."1 The claim is about the rock: the level where a group stops is set by burial, not by the death of its last member.
Most other young-earth writers treat the losses as real deaths in the Flood. Whitmore and Garner, founders of the end-Cretaceous camp, use extinctions as one of their criteria for Flood rock: "most marine extinctions are likely to have occurred directly as a result of the global Flood, due to the non-representation of these organisms on the Ark."9 Snelling calls the extinction levels places where a great variety of organisms "were buried on a global scale," by processes that "transcended specific ecological, morphological, and taxonomic groupings," and he accepts impacts and volcanic outpourings as part of the Flood.59 59 Emil Silvestru, then a geologist with CMI, put it most compactly: "The Flood can wrap the whole nine extinctions in one 400-day event."19 Leonard Brand and Arthur Chadwick propose that each crisis came "when the geological catastrophe reached some critical point and the remaining members of certain groups of organisms were all killed and buried. A life zone may have been destroyed." They add, frankly: "Those who accept a short-age theory also do not know exactly what happened."61 Wise explains the end of the Paleozoic land flora and fauna as the destruction of a floating forest that "residual catastrophism" kept from re-forming after the Flood.62 CMI's 2006 answer to a PBS documentary splits the losses by habitat: marine extinctions in the Flood, land extinctions "in subsequent centuries," since every land kind was on the Ark.63
The table sets the placements side by side.
| Event | ICR (Clarey, Tomkins) | Snelling | Wise and Richardson | Austin et al.; Whitmore and Garner |
|---|---|---|---|---|
| End-Ordovician | Flood, Days 1-40 | Flood | Flood | Flood |
| Late Devonian | Flood, Days 1-40 | Flood | Flood | Flood |
| End-Permian | Flood, early Absaroka, after Day 40 | Flood | Flood | Flood |
| End-Triassic | Flood, late Absaroka, near Day 90 | Flood | Flood | Flood |
| End-Cretaceous | Flood, Day 150, high water | Flood | Flood, near its end | End of the Flood |
| Paleocene recovery | Flood, receding phase | Flood | Earliest part Flood, rest post-Flood | Post-Flood |
| Real deaths or burial order? | Burial order, though groups did die out | Real global burials | Real; "arbitrarily defined" thresholds | Real deaths in the Flood |
Two of these positions make predictions about the rock that can be checked with numbers. Snelling's is that the extinctions "would be expected to coincide with" the megasequence unconformities.59 ICR's is that the groups which stop at an extinction level were still alive while the next levels were buried. Part 6 tests both, and then prices what every model has to fit above the boundaries.
Part 6: Testing and pricing the young-earth readings
Test 1: did the "extinct" groups go on living, unburied?
ICR's reading makes a prediction that can be counted. If a group "just didn’t get fossilized after a certain level," it was still alive in the sea while the Flood went on burying sea creatures above that level. Then the question is how much burying went on, and whether a living group could have escaped all of it.
The Paleobiology Database answers the first part. It holds 124,185 marine fossil occurrences from the whole Permian, 19,697 from its last stage, the Changhsingian, and 404,784 from the Mesozoic rocks above the Permian. So on ICR's own timetable, the Flood buried more than three times as many sea creatures after the end-Permian level as in all the Permian rocks below it. These were the same kinds of shelf, reef and open-sea settings: brachiopods, bivalves, snails, corals, sponges, ammonoids.
Five large Paleozoic marine groups stop at or near the end-Permian level. The table asks how many fossils each should have left in that later Mesozoic rock if it had lived on at only one hundredth of its share of the last Permian stage.10
| Group | Share of the last Permian stage's marine fossils | Expected later, at 1 % of that share | Found after the Permian | Chance of finding so few |
|---|---|---|---|---|
| Trilobites | 0.234 % | 9 | 0 | about 1 in 13,000 |
| Rugose corals | 1.300 % | 53 | 3 | about 1 in 3 billion billion |
| Tabulate corals | 0.147 % | 6 | 0 | about 1 in 390 |
| Fusulinid forams | 2.259 % | 91 | 1 | less than 1 in 10^37 |
| Productid brachiopods | 14.43 % | 584 | 115, of which 107 in the first Triassic substage | less than 1 in 10^120 |
The few survivors that do appear sit where a real extinction puts them. Of the 115 productid records above the Permian, 107 are in the Griesbachian, the first substage of the Triassic: the "mixed fauna" of South China, in which Permian-type brachiopods such as Paryphella and Fusichonetes persist into the first Triassic beds and then vanish. The pattern at the end-Cretaceous is the same. Ammonites make up 6.5 % of the marine fossils of the last Cretaceous stage. At that share they should appear about 849 times in the first Paleogene stage, and 41,202 times in all the marine rock after it. They appear 9 and 11 times, the nine being the Danian survivors discussed in Part 3. Mosasaurs, plesiosaurs, inoceramid clams and rudist clams, 2,262 occurrences in the last Cretaceous stage between them, have none in the first Paleogene stage.
ICR's own paper supplies the fact that closes the obvious escape. If these groups lived on in some other sea, mixing from that sea should have carried a few of their shells into later Flood deposits. Clarey and Werner report the opposite: "we do not observe significant numbers of reworked early Paleozoic fossils and mixed fossil debris in younger, Absaroka, Zuni and Tejas strata."6 Tomkins and Clarey raise the escape themselves for the end-Permian: "Did larger tsunami-like waves bring in distinctly different marine fossils at the same level? Or were waves coming from different directions with different marine fossils?"1 For that to work, every wave after the early Absaroka, some time after Day 40 on ICR's timetable, had to come from seas that held none of these five groups, on every continent, for the rest of the year.
The land-elevation mechanism does not reach this problem at all. ICR explains extinction levels as water reaching "the next ecological zone" at "higher elevations."60 Trilobites, rugose corals and ammonites did not live at elevations. They lived in the sea, and the sea went on being buried.
Verdict on Test 1. The reading of the end-Permian and end-Cretaceous as burial order alone predicts thousands of fossils that are not there. The groups stop because they died. This does not touch the young-earth writers who say the Flood killed them; it refutes only the claim that they were never extinct at those levels.
Test 2: do extinctions fall at the Flood's big unconformities?
Snelling's prediction was that "the so-called mass extinctions would be expected to coincide with these major unconformities," the erosion surfaces that bound the megasequences, because each new wave of sediment carried new creatures.59
ICR checked this against its own megasequence chart and found that it holds for two of the five. The end-Cretaceous sits at the top of the Zuni and the end-Triassic near the Absaroka-Zuni boundary; "the other three major extinction horizons fall within the middle or toward the top of the megasequence boundaries."1 The largest of all sits in the middle of the Absaroka, and Tomkins and Clarey ask the question themselves: "why did this event occur in the middle of a global megasequence (Absaroka) and not at one of its boundaries?"1
Wise and Richardson, testing the same idea against the Paleobiology Database, go further. They see "no connection" between the megasequences and the biostratigraphic divisions, and the end-Permian "has no special relation to the Absaroka megasequence in which it is found." Their conclusion: "It would seem that the sequence of burial of organisms was not at all affected by the changing energy levels of Flood waters."16 That sentence is a creationist's, and it removes the mechanism by which Snelling expected the waves to sort the dead.
Verdict on Test 2. The prediction fails on the young-earth side's own reckoning. The order of the fossils does not follow the rhythm of the Flood model's sediment.
Test 3: can the Early Triassic recovery fit inside the Flood year?
This test applies to every live young-earth model, because all of them put the end-Permian and the whole Triassic inside the Flood. On ICR's timetable the Absaroka, which runs from the Upper Carboniferous to the Lower Jurassic, took Days 40 to about 90. The Lower and Middle Triassic recovery therefore had, at the very most, those 50 days, and in fact a fraction of them.
Three features of that recovery are hard to place inside 50 days, in rising order of difficulty.
The rebuilding is recorded by animals living where they are found. Burrows cannot be carried in by a current; they are dug in place, in sediment that was the sea floor at the time. Snelling allows that each burrowed layer represents "the passing of at least a few hours."59 The Werfen Formation records not one burrowed surface but a sequence of them: burrowing nearly absent through the lowest member, a rebound, a fall, and a final recovery with larger burrows, across 250 to 700 m of rock. At 50 days for the whole Absaroka, that sequence was laid down while the same Flood was depositing the Permian and Jurassic rocks above and below it on other continents. The hours are not the problem. The order is: why should the burrowers of the lowest Triassic all be small and few, everywhere, and the burrowers a few days later be larger and more varied, everywhere?
The same genera vanish and return. Two-thirds of the genera found below and above the Lower Triassic are missing from it. On a burial-order model, every wave that reached the sea floor during the Lower Triassic days carried none of them, in every basin, and then the waves of the Middle Triassic carried them again. Tomkins and Clarey's suggestion, "waves coming from different directions with different marine fossils," would have to switch the source of every wave on Earth at once, twice.
A reef grew in place, and its builders arrived in order. At the Great Bank of Guizhou in southern China, a platform-margin reef began in the uppermost Lower Triassic and "persisted in situ" into the Middle Triassic, "reaching a stratigraphic thickness of ∼900 m." Its framework is a boundstone, rock bound together as it grew, with early marine cement. Its builders enter in sequence up the section: microbial Tubiphytes at the base, the first reef-building calcareous sponges 365 m above it, the first framework-building calcareous algae at 665 m, and the first scleractinian corals at 895 m.38 The young-earth answer to fossil reefs in general, that they are broken debris or reefs that grew before the Flood, is weighed in Fossil Preservation; neither answer fits here. This reef sits on top of Lower Triassic rock that every young-earth model calls Flood sediment, so it could not have grown before the Flood, and its authors describe it as a reef that grew in place. Modern reef margins in sheltered settings build upward at "1 to 25 mm year⁻¹, with a mode of 9 mm year⁻¹."64 Building 900 m inside the 50 days that ICR allows for the entire Absaroka requires 18 m a day, about 6,600 m a year, which is roughly 260,000 times the fastest of those averages.65
Verdict on Test 3. No young-earth publication found for this article addresses the Early Triassic recovery: not the dwarfing, the missing genera, the reef gap, the coal gap or the stepwise return of burrowers and reef builders. The deaths at the end-Permian can be fitted to a catastrophe. The ordered recovery above it cannot yet be fitted to anything inside a single year, and nobody on the young-earth side has tried. This is an unsolved problem for every live model.
Test 4: the end-Cretaceous recovery, read by each camp
The two camps face different bills here.
The end-of-the-Flood camp predicts the right kind of pattern. If the Flood ended at or near the end-Cretaceous, the beds just above should record life coming back onto bare ground and into emptied seas. That is what they show: a fern spike over an iridium clay, then palms, then a richer forest and the first legumes, with mammals multiplying and growing larger; and in the sea one surviving plankton species followed by new ones in fixed order. On this point the camp of Austin, Whitmore and Garner reads the boundary more naturally than the late-boundary camp does. Their bill is time. Austin and colleagues fit the whole Cenozoic, with its cooling oceans and its turnover from woodland to grassland faunas, into the centuries before an Ice Age that began "about five centuries after the Flood."11 The cost of that, a doubling of mammal genera roughly every two decades, is priced in The Flood/Post-Flood Boundary.
The camp also faces a consistency problem it has not addressed. The end-Triassic of eastern North America shows the same signature as the end-Cretaceous: an iridium anomaly, a fern spike, and a new set of dominant animals just above.58 The end-Permian shows the same aftermath of survivors, dwarfs and slow return. On the end-Cretaceous camp's own model those two events happened in the middle of the Flood, near Days 90 and 40 on ICR's timetable or their equivalents. If an iridium layer topped by a fern spike and a recovery fauna means "the Flood is over" at the end-Cretaceous, the camp needs a reason why the same sequence means something else twice lower down.
The high-water camp has to read a recovery as a burial order. On ICR's model the Paleocene beds were laid down by the receding Flood after Day 150, and their fossils are the next communities it reached. The land plants might be read that way. The sea cannot. Planktic foraminifera floated in the open ocean, which has no "higher elevations" for a rising flood to reach. Yet the same sequence, a single surviving species first and then Parvularugoglobigerina eugubina and the later species in a fixed order, is found from Tunisia to the Chicxulub crater. Inside the crater, burrowing animals lived on the sea floor before the first new plankton species arrived in the sediment above them.52 A receding flood would have had to sort the world's plankton by species into the same order in every ocean, and to pause for burrowers in between. Tomkins and Clarey acknowledge that their model "still has a bit of difficulty explaining the trackways and footprints found in some layers of the Cenozoic."1 The ordered return of the plankton is a larger version of the same difficulty.
Verdict on Test 4. The end-Cretaceous recovery fits the end-of-the-Flood camp in kind and fails it on time. It fits the high-water camp in neither.
Objections and responses
"The stage boundaries were drawn where the fossils change, so of course extinctions fall at stage boundaries. The Big Five are an artefact of the timescale." Half true. Many boundaries were indeed drawn at faunal changes, and Wise and Richardson are right that the threshold for a "mass" extinction is a convention. But every boundary was drawn the same way, and they are not all alike. On Wise and Richardson's own count, the end-Permian keeps 0.2 % of its species across the boundary where ordinary boundaries keep 3 to 17 %.16 And the strongest evidence does not use the timescale at all: a dinosaur horn 13 cm below a pollen change in one Montana hillside, a single extinction bed at Meishan, a 900-m reef whose builders appear in order.
"A last appearance is not an extinction. The coelacanth vanished from the record and is alive today." True, and the young-earth writers who make this point are right that the record misses things. Brand and Chadwick use exactly this example.61 Lazarus taxa are common: two-thirds of the genera that range through the Lower Triassic are missing from it. But the argument proves too little. A rare fish can hide in the deep sea for a long time. Productid brachiopods, fusulinid forams and rugose corals were among the commonest fossils of the last Permian stage, with 2,842, 445 and 256 database occurrences there, and outside the first Triassic substage they are all but absent from a later marine record three times the size of the whole Permian.10 Trilobites, with only 46 occurrences in that last stage, carry less weight on their own, since the coelacanth survived a longer stretch of missing record. The coelacanth is the subject of the article on Living Fossils.
"The suddenness is an effect of changing rock type, not of a sudden kill." Clarey reports a survey in which 72 % of sudden extinctions in 110 papers coincided with a "rapid shift in rock type."20 The mainstream literature agrees that rock architecture shapes the pattern: Holland and Patzkowsky find last appearances clustering at unconformities and flooding surfaces in every mass extinction "with the possible exception of the end‐Cretaceous."22 So the shape of a loss in one section, sharp or smeared, can mislead. Two things survive the objection. Studies built to control for it still find the loss: Sheehan's team compared "results only from similar facies" and still found no gradual decline of dinosaurs.44 And the size of the loss is not a matter of shape. Clarey's survey has not been published in a form that could be checked: his reference list gives it as a two-page abstract in the Journal of Creation Theology and Science, Series C, volume 2, which this article could not obtain.
"Mainstream scientists cannot agree what caused any of these extinctions." True. Bambach's review says flatly that "No consensus has been reached on the kill mechanism for any marine mass extinction."14 Impact, volcanism, cooling, warming and anoxia are all argued. But the dispute is about cause, and this article is about pattern. No side of the cause dispute questions that the losses happened, in the order the rocks show, or that recovery took far longer than a year. The disagreement among mainstream workers lies entirely inside a range that is millions of times longer than a Flood year.
"The famous 90 to 96 % figure for the end-Permian is exaggerated." It is. Stanley's corrected figure is about 81 % of marine species, and he notes that "About 90 orders and more than 220 families of marine animals survived."18 This cuts against popular writing on both sides. It does not change the order of events or the size of the recovery problem.
"Recovery was fast: burrowers were back in the Chicxulub crater within years, and a complex fauna lived in Idaho early in the Triassic." These findings are real and the article reports them. Mainstream authors call them fast in mainstream terms: years to hundreds of thousands of years. None of the tests above depends on how many years passed. They depend on order, on animals living where they are found, and on a reef that grew in place.
"Hydrodynamic sorting puts small shells on top. The Lilliput effect is sorting." Sorting by settling makes each event bed fine at the top and coarse at the base. It does not make every snail in 250 to 700 m of Lower Triassic rock smaller than 2.6 cm, worldwide, and then let 5 to 10 cm snails return gradually in the beds above.32 And Wise and Richardson found that the order of burial "was not at all affected by the changing energy levels of Flood waters,"16 which removes sorting by flow strength as an explanation of the large-scale pattern.
"The Flood killed these animals. Of course they are not found higher up: they were dead." That is the real-death reading of Whitmore and Garner, Snelling, Wise and Brand. It passes Test 1. Its difficulty is Test 3: whatever lived through the end-Permian level had to rebuild ordered communities, with dwarfs, absences, a stepwise return of burrowers and a reef 900 m thick, within the days the model allows before the Middle Triassic.
From the skeptic's side: "Calling the real-death reading 'unfinished' is too kind. It is simply wrong." A model can be shown wrong only once it says something specific. No young-earth publication found for this article says anything about the Early Triassic recovery. The reef arithmetic shows how large the gap is, and a skeptic may judge that no model will close it. But the series' rule is to call a position unfinished when the pattern is real, the standard answers fail, and no answer has yet been offered.
From the defender's side: "Microbial reefs cemented on the sea floor may grow much faster than modern coral reefs, so the 260,000-fold figure is unfair." This is a fair point, and Issue 3 below records it. The Guizhou reef's lower part is microbial boundstone with marine cement, not coral. No published growth rate for such a reef was found. To close the gap, it would have to build about 260,000 times faster than the fastest modern coral reef margins, while its builders entered in sequence.
Issues and unanswered questions
- Several key papers were read only as abstracts. Jin and colleagues' bed-by-bed counts at Meishan, Song's two-pulse data, Chen and Benton's review, Lyson's metre-by-metre recovery at Corral Bluffs, Twitchett's Lilliput study and Signor and Lipps's original paper were not obtained in full. The claims made from them here are the claims in their abstracts.
- The database check is raw. It is not corrected for sampling intensity, PBDB's environment tags are incomplete, and some "Lazarus" genera may be later look-alikes given an old name. The published sampling-corrected studies agree with its ranking, which is why it is offered as a check and not as a finding of its own.
- The reef rate compares unlike reefs. Modern reef-growth figures come from coral reefs; the lower Guizhou reef is microbial and cement boundstone. A measured growth rate for a modern or ancient microbial-cement reef would sharpen or weaken Test 3.
- Nobody has counted the burrowed surfaces. No paper read here counts the burrowed horizons in the Werfen Formation or any other Lower Triassic section. With that count, Snelling's "few hours" per surface could be turned into a minimum time.
- The South African land record is disputed. Whether the Karoo turnover is the same event as the marine extinction rests on radiometric dates, which this series does not use. The order of the Karoo faunas is not in dispute; their correlation with Meishan is.
- The end-Ordovician glaciation sits in the Flood's first 40 days on ICR's timetable. No young-earth source found for this article discusses it.
- A young-earth model of the Early Triassic would need to say where the small-bodied, low-diversity Lower Triassic communities lived before the Flood, why the same genera reappear above them, and how a reef grew 900 m in place during the Flood. A pre-Flood "stressed habitat" zone might answer the first question; it would not answer the other two.
- A citation defect in the young-earth literature. Oard's 1997 list of objections to the impact theory includes "no statistical support for a sudden extinction of dinosaurs," citing Hurlbert and Archibald 1995, whose title reads "No statistical support for sudden (or gradual) extinction of dinosaurs."17 The paper found the data unable to decide either way.
- The Flood/post-Flood boundary is not settled by this article. Test 4 shows that the end-Cretaceous recovery suits the end-of-the-Flood camp in kind; the rate problem that camp faces is in The Flood/Post-Flood Boundary.
Verdict
The Big Five, and the smaller events between them, are not artefacts of how geologists divide the column. In single sections they appear as losses within centimetres or a few metres, followed by a recognisable aftermath: short-lived holdovers, opportunists, dwarfs, missing groups, and a stepwise rebuilding of communities and reefs. The end-Permian is by far the largest on every measure, including a young-earth one. The Late Devonian and end-Triassic were as much failures of new forms to appear as surges of loss, and the size of the end-Permian has been overstated in popular writing.
Every live young-earth model places the four oldest events inside Noah's Flood and splits over whether the end-Cretaceous is its end or its high-water mark. The ICR reading, that extinctions are only the levels where each group stopped being buried, fails on its own terms: even at a hundredth of their last-Permian share it predicts about 740 trilobites, Paleozoic corals, fusulinids and productids in the later marine record, and outside the first Triassic substage there are 12. Its companion prediction, that extinctions fall at the megasequence boundaries, fails for three of five on ICR's own chart. The reading in which the Flood itself did the killing survives those tests. But it has no account of the recoveries: the Early Triassic, with its dwarfs, its absences and a reef 900 m thick built in place by builders arriving in sequence, has to fit inside a few weeks, and no young-earth author has attempted it. That position is unfinished, and the size of the gap is now measured.
Sources
- 1.
Tomkins, Jeffrey P., and Timothy L. Clarey. “Developing a Comprehensive Model of Global Flood Paleontology: Integrating the Biostratigraphic Record with Global Megasequence Deposition.” Proceedings of the Ninth International Conference on Creationism 9:561–587. Cedarville University. 2023. The Institute for Creation Research's own account of how its megasequence Flood model explains the fossil record, written by its geneticist and its director of research. It maps Paleobiology Database occurrences onto Clarey's six megasequences and states ICR's position on every major extinction: none is a real extinction, each is a level where one ecological zone stopped being buried. It concedes that the marine end-Permian losses are "more difficult to explain."
- 1a.
Page 563: “Creation scientists do not consider these as true “extinction” events. Instead, these horizons are interpreted as major shifts in the burial pattern of fossils during the Flood. So-called extinctions are merely the level at which certain fossils were no longer being actively buried, so they disappear upward in the geological column.” ↩ ↩
- 1b.
Page 563: “Figure 2 shows that several of the major extinction events do closely coincide with the six megasequences, one coinciding with the Cretaceous-Paleogene (K-Pg) and one with the Triassic-Jurassic (Tr-J) (Clarey 2020). The other three major extinction horizons fall within the middle or toward the top of the megasequence boundaries.” Page 586: “Two of the megasequences line up approximately with two of the so-called major extinction events. The other three major extinctions may be a consequence of high-water stands and/or smaller sequence boundaries within the six megasequences.” ↩ ↩
- 1c.
Page 564: “However, that is not to say the Flood did not cause extinctions. Many of the presumably unique pre-Flood environments were likely destroyed by the Flood’s tectonic activity during the destruction of “the world that then was.” This caused a lot of marine animals to go extinct during or shortly after the Flood. For example, animals like trilobites and many of the Paleozoic brachiopods and corals seem to be extinct today. The exact reason for this is unclear.” ↩
- 1d.
Page 573: “Permian strata leading up to the alleged mass extinction of marine life at the P-Tr actually represented the increasing accumulation and systematic burial of the many offshore ocean ecosystems.” “It is possible the so-called P-Tr extinction is another example of a dramatic shift in environment as the water reached different ecological zones on land. However, marine extinctions at this level are more difficult to explain. Did larger tsunami-like waves bring in distinctly different marine fossils at the same level? Or were waves coming from different directions with different marine fossils?” ↩
- 1e.
Page 573: “Furthermore, why did this event occur in the middle of a global megasequence (Absaroka) and not at one of its boundaries?” Asked by the authors of their own model. ↩
- 1f.
Page 577: “The plethora of geological data gathered by studying the stratigraphic columns around the globe strongly indicate that the K-Pg is the high water point of the Flood, and represents Day 150 of the Flood year (Johnson and Clarey 2021; Clarey and Werner 2023). That would make the Tertiary (Tejas Megasequence) the receding phase of the Flood (Clarey and Werner 2023).” ↩
- 1g.
Page 573: “Many Permian marine organisms were abundant right up to the P-Tr boundary, but land life showed several smaller extinction events leading up the P-Tr boundary. This is especially true with land plant fossils that allegedly exhibited a more tiered extinction, with many of their fossils extending well into the Triassic.” ↩
- 1h.
Page 575: “This extinction event is also contained within the sediments of the upper-Absaroka (Figures 1 and 2). … On land, a large variety of Archosauria dropped from the fossil record, but crocodylomorphs, pterosaurs, and dinosaurs somehow selectively avoided extinction.” ↩
- 1i.
Page 577: “Our interpretation still has a bit of difficulty explaining the trackways and footprints found in some layers of the Cenozoic. It is possible some of these layers have been misidentified and should be Pleistocene (post-Flood), but more research is needed on each site.” ↩
- 1a.
- 2.
Wieland, Carl. “The Great Dinosaur Extinction Controversy (book review).” CEN Technical Journal 12(2):154–158. 1998. A review by the founder of Creation Ministries International of Officer and Page's 1996 book against the impact theory. It gives his own view that extinctions in Flood rock are only the tops of burial, and concedes what kind of K-T boundary would trouble a Flood model.
- 2a.
Page 156: “However, it is interesting to note in passing that a creation/Flood framework would have much more difficulty dealing with a global pattern of uniform sharp 'cut-off' at the K-T boundary, rather than a blurry picture, which appears to be the reality.” ↩
- 2b.
Page 156: “since creationists regard most of the fossil record as being the record of the Flood, 'extinctions' simply mean points above which there are no more such fossils found buried.” ↩
- 2a.
- 3.
Lyson, Tyler R. et al. “Dinosaur extinction: closing the '3 m gap'.” Biology Letters 7(6):925–928. 2011. The report of the stratigraphically youngest non-avian dinosaur fossil found in place, a ceratopsian brow horn in Montana, with the boundary fixed by closely spaced pollen samples. Mirror: PMC
- 3a.
Page 925: “a ceratopsian brow horn found in a poorly rooted, silty, mudstone floodplain deposit located no more than 13 cm below the palynologically defined boundary”. “the K–T boundary actually lies anywhere from –5 to +3 m relative to the contact”. Page 927: “Dinosaur extinction (K-taxa) drops significantly from 14% in sample 190-1 to 1–3% in the overlying samples. A ‘fern spike’ is also identified starting at sample 190-2, where the assemblage consists of as much as 80% ferns”. The PDF's text layer renders the plus sign in "+3 m" as "þ". ↩ ↩
- 3a.
- 4.
This article's own count from the Paleobiology Database, retrieved 17 October 2026. Query:
taxa/list.csv?base_name=Animalia&rank=genus&taxon_status=valid&show=app,class,ecospace&pres=regular&limit=all, which returned 88,505 valid animal genera;pres=regularremoves trace and form taxa. Each genus's first-appearance and last-appearance age brackets were placed in PBDB's 101 named stages, keeping only genera whose brackets each fall inside a single stage (39,363 genera; 13,233 tagged marine in PBDB's environment field). For each stage, extinction is the share of genera entering it from below whose last record is in it; origination is the share of genera leaving it upward whose first record is in it. Genera known from one stage only are left out of both. Putting a bracket that spans two stages into the stage holding its midpoint, instead of dropping it, gives the same ranking: Changhsingian 57.5 %, Katian 48.1 %, Maastrichtian 31.8 %. The figures are raw and are not corrected for collecting effort. Code:research/pbdb-turnover.ts; full results inresearch/pbdb-turnover.md. ↩ ↩ - 5.
This article's own count from the Paleobiology Database, retrieved 17 October 2026. Lower Triassic occurrences:
occs/list.csv?max_ma=251.902&min_ma=247&timerule=contain&pres=regular&show=coords,class&limit=all, 22,811 occurrences naming 1,761 genera. A genus "ranges through" the Lower Triassic if PBDB's whole first-appearance bracket is older than its base and its whole last-appearance bracket younger than its top; 570 animal genera do. 387 of them (67.9 %) carry no Lower Triassic occurrence; allowing any collection that merely overlaps the Lower Triassic still leaves 373 (65.4 %). Of the 285 tagged marine, 183 (64.2 %) are missing. By class: Demospongiae 53 of 53, Gastropoda 76 of 101, Bivalvia 49 of 97, Rhynchonellata 16 of 23, Conodonta 5 of 24, Lingulata 1 of 7. Marine occurrences: Lower Triassic 20,730; Changhsingian 19,697. Code:research/pbdb-lazarus.ts. ↩ ↩ - 6.
Clarey, Timothy L., and Davis J. Werner. “A Progressive Global Flood Model Confirmed by Rock Data Across Five Continents.” Proceedings of the Ninth International Conference on Creationism 9:412–445. Cedarville University. 2023. ICR's flagship statement of its Flood model, built on its own database of about 3,000 stratigraphic columns from five continents. It assigns each of Sloss's six megasequences to a span of Flood days and explains extinctions as levels where rising water reached new "biozones." The database behind it has not been released.
- 6a.
Page 430: “We interpret Days 40 to about 90 of the Flood as corresponding to the Absaroka megasequence.” Page 431: “We suspect the Zuni was deposited from about Day 90 of the Flood to Day 150 of the Flood.” The same page assigns the Sauk, Tippecanoe and Kaskaskia, which hold the end-Ordovician and Late Devonian levels, to "the first 40 days of the Flood" (p. 430), and calls the end of the Zuni, at the end-Cretaceous, "the highest point of the Flood, which we believe was at or near Day 150" (p. 431). ↩ ↩ ↩
- 6b.
Page 430: “Finally, the so-called Permian extinction occurs in the early portion of the Absaroka. This has been hailed by secular scientists as the largest ‘extinction’ of all geologic time, or at least exhibiting the most abrupt changes in fossil species. Many of the fossils found above and below this horizon are, in fact, vastly different. However, most creation geologists explain ‘extinction events’ as the last occurrence of organisms in the Flood record. Specifically, we explain them as a result of rapid changes in water level that buried completely new”. Page 431: “types of organisms from new biozones. In this view, the so-called ‘extinctions’ are merely a record of abrupt disappearances of many organisms at the same location in the fossil record. This was likely caused by the simultaneous inundation of a complete ecological environment at the same approximate elevation globally.” ↩
- 6c.
Page 423: “Secondly, we do not observe significant numbers of reworked early Paleozoic fossils and mixed fossil debris in younger, Absaroka, Zuni and Tejas strata. … The pattern of sudden appearance, stasis, and sudden disappearance of fossils is prevalent throughout the entire Phanerozoic sedimentological record, Sauk through Tejas (Wise 2017). Reworking significant amounts of fossils would likely have blurred this pattern.” ↩
- 6a.
- 7.
Garner, Paul et al. “Flood models.” TJ 14(3):79–80. 2000. A letter in which the four British creationists who in 1996 had put the end of the Flood in the Paleozoic, making the end-Permian and everything above it post-Flood, say they no longer hold that model.
- 8.
Tomkins, Jeffrey P., and Tim Clarey. “Cretaceous-Paleogene Boundary Shenanigans.” Acts & Facts. Institute for Creation Research. Dec 29, 2017. A short ICR magazine piece answering a 2017 study that found placental mammals diversifying straight through the end-Cretaceous. It restates ICR's position in its strongest form.
- 9.
Whitmore, John H., and Paul Garner. “Using Suites of Criteria to Recognize Pre-Flood, Flood, and Post-Flood Strata in the Rock Record with Application to Wyoming (USA).” Proceedings of the Sixth International Conference on Creationism, 425–448. 2008. Sets out 27 ranked criteria for telling Flood rock from post-Flood rock and applies them in Wyoming, where they place the end of the Flood near the end-Cretaceous. Both authors are working creationist geologists; the paper is the founding method of the end-Cretaceous boundary camp.
- 9a.
Page 429: “Since most marine extinctions are likely to have occurred directly as a result of the global Flood, due to the non-representation of these organisms on the Ark, the last appearances of extinct marine species would be expected to occur predominantly in Flood-deposited sediments. … However we believe most marine extinctions probably occurred during the Flood.” ↩ ↩
- 9b.
Page 433, caption of the Wyoming criteria table: “From our preliminary data, we would place the Flood/post-Flood boundary somewhere in the Lance or Fort Union Formation.” ↩
- 9a.
- 10.
This article's own count from the Paleobiology Database, retrieved 17 October 2026, with every query
occs/list.json?…&timerule=contain&pres=regular&show=coords&limit=0&rowcount, so that a collection counts only if its whole age bracket lies in the interval. Marine occurrences (envtype=marine): Permian 124,185; Changhsingian 19,697; Lower Triassic 20,730; post-Permian Mesozoic (251.902 to 66 Ma) 404,784; everything after the Permian 1,043,856; Maastrichtian 40,609; Danian 13,142; everything after the Cretaceous 638,121. Group counts, Changhsingian then everything after the Permian: Trilobita 46 and 0; Rugosa 256 and 3; Tabulata 29 and 0; Fusulinoidea 445 and 1; Productida 2,842 and 115, of which 107 are labelled Griesbachian. Maastrichtian, Danian, everything after: Ammonoidea 2,622, 9, 11; Mosasauridae 325, 0, 0; Plesiosauria 170, 0, 0; Inoceramidae 435, 0, 0; Hippuritida 1,332, 0, 4. "Expected" is a group's share of the last-stage marine occurrences, times one hundredth, times the later marine count; the chances are Poisson probabilities of finding that few or fewer. Shares of database occurrences reflect collecting and naming as well as abundance, which is why only one hundredth of the share is assumed. ↩ ↩ ↩ ↩ ↩ - 11.
Austin, Steven A. et al. “Catastrophic Plate Tectonics: A Global Flood Model of Earth History.” Proceedings of the Third International Conference on Creationism, 609–621. Creation Science Fellowship. 1994. The founding paper of catastrophic plate tectonics, by six young-earth scientists. It places the end of the Flood near the end-Cretaceous and assigns the whole Cenozoic record of ocean cooling and biotic change to the first post-Flood centuries.
- 11a.
Page 614: “Therefore, we tentatively place the Flood/post-Flood boundary at approximately the Cretaceous/Tertiary (K/T) boundary.” ↩
- 11b.
Page 615: “We would expect floral and faunal communities to have tracked the cooling of the oceans and the corresponding cooling and drying of the continents. … According to Oard's [67,68] model, by about five centuries after the Flood, the cooling oceans had led to the advance of continental glaciers and the formation of polar ice caps.” ↩ ↩
- 11c.
Page 615: “Oard [68] suggests that rapid melting of the continental ice sheets (in less than a century) … contributed to the megafaunal extinctions of the Pleistocene”. ↩
- 11a.
- 12.
Raup, David M., and J. John Jr. Sepkoski. “Mass extinctions in the marine fossil record.” Science 215(4539):1501–1503. 1982. The paper that named the "Big Five." The two University of Chicago palaeontologists compiled the ranges of marine animal families and tested which intervals lost more than the background trend predicts. Four passed the statistical test; the Late Devonian did not.
- 12a.
Section Abstract: “four mass extinctions in the marine realm are statistically distinct from background extinction levels. These four occurred late in the Ordovician, Permian, Triassic, and Cretaceous periods. A fifth extinction event in the Devonian stands out from the background but is not statistically significant in these data.” ↩
- 12a.
- 13.
Bambach, Richard K. et al. “Origination, extinction, and mass depletions of marine diversity.” Paleobiology 30(4):522–542. 2004. A re-analysis of Sepkoski's genus compendium that measures extinction and origination for every substage and compares each event with its neighbours in time. It finds that only three of the Big Five are true outliers of extinction, and that the Late Devonian and end-Triassic losses came largely from a failure of new genera to appear.
- 13a.
Page 522: “Plotted by magnitude, extinction intensities for all Phanerozoic substages show a continuous distribution, with the five traditionally recognized mass extinctions located in the upper tail. … Compared with other stages and substages in the same neighborhood, only the end-Ordovician, end-Permian, and end-Cretaceous extinction intensities appear as outliers.” ↩
- 13b.
Page 535: “about two-thirds of the diversity loss in the late Frasnian and almost 60% in the end-Triassic can be ascribed to origination failure, not elevated extinction”. ↩ ↩ ↩
- 13a.
- 14.
Bambach, Richard K. “Phanerozoic biodiversity mass extinctions.” Annual Review of Earth and Planetary Sciences 34:127–155. 2006. A review by one of the leading analysts of the marine diversity record, comparing the different ways of tabulating Sepkoski's database. It counts 18 intervals that qualify as mass extinctions and stresses how different they are from one another.
- 14a.
Section Abstract: “A review of different methods of tabulating data from the Sepkoski database reveals 18 intervals during the Phanerozoic have peaks of both magnitude and rate of extinction that appear in each tabulating scheme. These intervals all fit Sepkoski's definition of mass extinction. However, they vary widely in timing and effect of extinction, demonstrating that mass extinctions are not a homogeneous group of events. No consensus has been reached on the kill mechanism for any marine mass extinction.” ↩ ↩ ↩
- 14a.
- 15.
Alroy, John. “Dynamics of origination and extinction in the marine fossil record.” Proceedings of the National Academy of Sciences 105(supplement 1):11536–11542. 2008. An analysis of extinction and origination rates from the occurrence-level Paleobiology Database by one of its founders. It finds that very high extinction is followed by very high origination, and that extinction rates form a continuum rather than two classes.
- 15a.
Section Abstract: “very high extinction rates are followed by equally high origination rates. … The data also confirm that extinction and origination rates both declined through the Phanerozoic and that several extinctions in addition to the Permo-Triassic event were particularly severe. However, the trend may be driven by taxonomic biases and the rates vary in accord with a simple log normal distribution, so there is no sharp distinction between background and mass extinctions.” ↩
- 15a.
- 16.
Wise, Kurt P., and Matthew Richardson. “What Biostratigraphic Continuity Suggests About Earth History.” Proceedings of the Ninth International Conference on Creationism 9:611–625. Cedarville University. 2023. A Paleobiology Database study by the creationist palaeontologist Kurt Wise and a colleague. For each of 114 stage boundaries it counts the species found on both sides within 2 degrees of each other, uses the pattern to place the start and end of the Flood, and compares the result with published mass-extinction rankings and with the megasequences. It concludes that "the global biostratigraphic column seems to be real."
- 16a.
Table 1: Row 63, Changhsingian/Induan: 2,556 species in the stage below; 4 found on both sides within 2 degrees, 0.2 %; ranked first among mass extinctions. Ordinary boundaries run from about 3 to 17 %. Maastrichtian/Danian: 3,247 species, 207 straddling, 6 %. ↩ ↩
- 16b.
Page 622: “Since ‘mass extinctions’ are nothing more than higher than ‘normal’ ‘extinction rate,’ they are arbitrarily defined. There is no consensus on what is a ‘higher than normal’ extinction rate.” ↩
- 16c.
Page 623: “Although the Cretaceous/Paleogene ‘extinction’ event is close to the end of the Zuni megasequence, the largest ‘extinction’ event (that of the Permo-Triassic) has no special relation to the Absaroka megasequence in which it is found. … It would seem that the sequence of burial of organisms was not at all affected by the changing energy levels of Flood waters.” ↩ ↩
- 16d.
Page 620: “This strongly argues that the Flood/post-Flood boundary is located just below boundary 94—i.e., just below the Danian/Selandian boundary (the first biostratigraphic boundary above the Cretaceous/Paleogene boundary).” ↩
- 16a.
- 17.
Oard, Michael J. “The extinction of the dinosaurs.” CEN Technical Journal 11(2):137–154. 1997. A review of the dinosaur-extinction debate by a retired meteorologist who is the most prolific author on Flood geology at Creation Ministries International. It sides with the volcanist critics of the impact theory and concludes that the dinosaurs died in the Flood.
- 17a.
Page 142: “For most creationists, the extinction of the dinosaurs, as well as other extinctions, is not a mystery. In fact, the extinction of the dinosaurs and many other creatures has an easy answer — they simply died in the Genesis Flood (except those dinosaurs likely taken on the Ark, which probably died soon after the Flood).” ↩
- 17b.
Page 138: “The most singular extinction event in the supposed history of life was not the End Cretaceous disappearance of the dinosaurs, but the End Permian demise of most groups of marine and terrestrial animals.” ↩
- 17c.
Page 141: “(10) no statistical support for a sudden extinction of dinosaurs;113”. Oard's footnote 113 is Hurlbert and Archibald 1995, whose title is "No statistical support for sudden (or gradual) extinction of dinosaurs." The paper found the data too sparse to decide either way; the list drops "(or gradual)." ↩
- 17a.
- 18.
Stanley, Steven M. “Estimates of the magnitudes of major marine mass extinctions in earth history.” Proceedings of the National Academy of Sciences 113(42):E6325–E6334. 2016. A re-estimate of the size of the major marine extinctions by a University of Hawaii palaeontologist. It corrects for background extinction and for the backward smearing of last appearances, and finds most events smaller than usually quoted, the end-Permian at about 81 % of species. Mirror: PMC
- 18a.
Section Abstract: “They indicate that only ∼81% of marine species died out in the great terminal Permian crisis, whereas levels of 90–96% have frequently been quoted in the literature. Calculations of the latter numbers were incorrectly based on combined data for the Middle and Late Permian mass extinctions. About 90 orders and more than 220 families of marine animals survived the terminal Permian crisis … Life did not nearly disappear at the end of the Permian, as has often been claimed.” ↩ ↩ ↩
- 18b.
Section Results: “a best estimate of 42–43% for the total Ashgillian event”. “My best estimates for generic losses in the Frasnian crisis are relatively small (16–20%)”. “a preferred estimate of 38–40% for the magnitude of the Maastrichtian mass extinction”. ↩
- 18c.
Section Introduction: “All five events recognized by Raup and Sepkoski except that of the Late Triassic are evaluated here; the latter is excluded because its timing and list of marine victims remain controversial”. ↩ ↩
- 18d.
Section Abstract: “the Signor–Lipps effect, which is the incorrect assignment of extinctions that occurred during a crisis to an interval preceding the crisis because of the incompleteness of the fossil record.” ↩
- 18a.
- 19.
Silvestru, Emil. “The Permian extinction: National Geographic comes close to the truth.” TJ 15(1):6–8. 2001. A short perspective piece by a Romanian-born karst geologist then on the staff of Creation Ministries International, responding to a National Geographic feature. It accepts the end-Permian as a real catastrophe and says the Flood "can wrap the whole nine extinctions in one 400-day event."
- 19a.
Page 6: “About 250 million years ago, at the end of the Permian period, something killed some 90 percent of the planet’s species.” Silvestru quoting National Geographic. ↩
- 19b.
Page 8: “Unlike evolutionary geologists, creationists do not need sophisticated scenarios to explain P/T or K/T, or any other extinction. The Flood can wrap the whole nine extinctions in one 400-day event.” ↩
- 19a.
- 20.
Clarey, Timothy L. “The Hell Creek Formation: The Last Gasp of the Pre-Flood Dinosaurs.” Creation Research Society Quarterly 51(4):286–298. 2015. A review of the Montana and Dakota rocks that hold the last dinosaurs, by the ICR geologist whose megasequence model puts the end-Cretaceous at the Flood's high-water mark. It cites an unpublished survey with Heim of 110 papers to argue that the abruptness of the end-Cretaceous extinction is partly a change in rock type.
- 20a.
Page 286: “The so-called Cretaceous-Paleogene (K-Pg) extinction is more complicated than many are led to believe, and is probably just the last appearance of many organisms in Flood-deposited strata.” ↩
- 20b.
Page 288: “A review of 110 secular research papers on the K-Pg extinction, examining all organisms, showed that a sudden extinction was noted in only 50% of the papers, and that 72% of those sudden extinctions were associated with a corresponding rapid shift in rock type (Clarey and Heim, 2012).” ↩ ↩
- 20c.
Page 289: “Some creation scientists think the “K-Pg” was about the high point of the Floodwaters, when all land animals finally succumbed and drowned. That may be why at this point so many organisms seemed to simultaneously go “extinct.”” ↩
- 20d.
Page 287, table 1: Table 1, "The so-called five great extinctions," gives species extinction of 70 % for the Cretaceous-Paleogene, 76 % for the Upper Triassic, 96 % for the Permian-Triassic, 82 % for the Upper Devonian and 85 % for the Upper Ordovician, without naming the compilation they come from. ↩
- 20a.
- 21.
Marshall, Charles R. “Distinguishing between sudden and gradual extinctions in the fossil record: predicting the position of the Cretaceous-Tertiary iridium anomaly using the ammonite fossil record on Seymour Island, Antarctica.” Geology 23(8):731–734. 1995. A statistical method, using confidence intervals on stratigraphic ranges, for telling a sudden extinction from a gradual one, applied to the ammonites of one Antarctic section. It shows a literal reading can look gradual over tens of metres when the data fit a sudden loss, and says plainly that the data also fit some gradual scenarios.
- 21a.
Section Abstract: “their pattern of disappearances is consistent with a sudden mass extinction at the Cretaceous-Tertiary (K-T) boundary, even though a literal reading of the fossil record shows they disappeared gradually over a stratigraphic interval 10–50 m below the boundary. … without saturation collecting near the K-T boundary it will be impossible to distinguish between gradual and sudden extinction scenarios for the Seymour Island ammonites based on the ammonite fossil record alone.” ↩
- 21a.
- 22.
Holland, Steven M., and Mark E. Patzkowsky. “The stratigraphy of mass extinction.” Palaeontology 58(5):903–924. 2015. Numerical simulations, by two specialists in sequence stratigraphy and the fossil record, of how last appearances are distributed in real sedimentary sequences. They find last appearances cluster at erosion and flooding surfaces, so a protracted extinction can look like a sudden pulse.
- 22a.
Section Abstract: “last occurrences are not randomly distributed, but tend to cluster at subaerial unconformities, surfaces of forced regression, flooding surfaces and intervals of stratigraphical condensation … With the possible exception of the end‐Cretaceous, mass extinctions in the fossil record are characterized by clusters of last occurrences at these sequence stratigraphical horizons. Although these clusters of last occurrences may represent brief pulses of elevated extinction, they are equally likely to form by stratigraphical processes during a protracted period”. ↩ ↩
- 22a.
- 23.
Metcalfe, Ian et al. “The Permian-Triassic boundary & mass extinction in China.” Episodes 24(4):239–244. 2001. A report by an Australian, American and Chinese team on the conodonts, beds and ash layers of the Meishan and other South China boundary sections. It fixes the bed numbers used for the extinction and the boundary, and notes that Meishan may be missing some section.
- 23a.
Page 239: “The first appearance of Hindeodus parvus (Kozur & Pjatakova) at the Permian-Triassic (P-T) GSSP level (base of Bed 27c) at Meishan is here confirmed. Hindeodus changxingensis Wang occurs from Beds 26 to 29 at Meishan and appears to be restricted to the narrow boundary interval immediately above the main mass extinction level in Bed 25.” “Bed 28, just 8 cm above the GSSP boundary”. ↩
- 23b.
Page 239: “Our collections from the Shangsi section confirm that the first occurrence of Hindeodus parvus in that section is about 5 m above the highest level from which a typical Permian fauna is recovered. This may suggest that that some section may be missing at Meishan.” "that that" is in the original. ↩
- 23a.
- 24.
Jin, Y. G. et al. “Pattern of marine mass extinction near the Permian-Triassic boundary in South China.” Science 289(5478):432–436. 2000. A statistical analysis of the ranges of 162 genera and 333 species through the Meishan section, by a Chinese team with the Smithsonian palaeontologist Douglas Erwin. It found the losses consistent with a single sudden event.
- 24a.
Section Abstract: “A statistical analysis of the occurrences of 162 genera and 333 species confirms a sudden extinction event”. ↩
- 24a.
- 25.
Song, Haijun et al. “Two pulses of extinction during the Permian–Triassic crisis.” Nature Geoscience 6:52–56. 2013. A range study of 537 species in 17 marine groups across seven South China sections. It splits the end-Permian marine extinction into two pulses with different victims, the first taking all the plankton.
- 25a.
Section Abstract: “We evaluated the range of 537 species representing 17 marine groups in seven Chinese sections … The first stage of extinction occurred during the latest Permian, and was marked by the extinction of 57% of species, namely all plankton and some benthic groups, including algae, rugose corals, and fusulinids. The second phase occurred in the earliest Triassic, and resulted in the extinction of 71% of the remaining species.” ↩
- 25a.
- 26.
Smith, Roger, and Jennifer Botha. “The recovery of terrestrial vertebrate diversity in the South African Karoo Basin after the end-Permian extinction.” Comptes Rendus Palevol 4:623–636. 2005. Field logs of 225 vertebrate fossils found in place across the Permian-Triassic boundary at two Karoo localities, by two South African museum palaeontologists who did much of the collecting. It describes a two-step loss and the Triassic recovery fauna.
- 26a.
Page 623: “Field data demonstrates a 69% mass extinction of Late Permian terrestrial vertebrates lasting some 300 kyr terminating at the PTB, followed by a lesser extinction event (31%) approximately 160 kyr later involving four survivor taxa that crossed the PTB.” Page 624: “The main extinction zone is approximately 40 m thick at both the Bethulie and the Graaff-Reinet sections”. ↩
- 26a.
- 27.
Viglietti, Pia A. et al. “Evidence from South Africa for a protracted end-Permian extinction on land.” Proceedings of the National Academy of Sciences 118(17):e2017045118. 2021. A sampling-standardised analysis of 588 Karoo tetrapod specimens in thirteen stratigraphic bins. It finds high extinction spread through the upper Permian beds with an acme near the boundary between the two faunal zones. Mirror: PMC
- 27a.
Section Abstract: “High regional extinction rates occurred through a protracted interval of ∼1 Ma, initially co-occurring with low origination rates. This resulted in declining diversity up to the acme of extinction near the Daptocephalus–Lystrosaurus declivis Assemblage Zone boundary.” The duration is the authors' figure from radiometric ages; the article uses only the order. ↩
- 27a.
- 28.
Gastaldo, Robert A. et al. “The base of the Lystrosaurus Assemblage Zone, Karoo Basin, predates the end-Permian marine extinction.” Nature Communications 11:1428. 2020. A field and dating study by the team that has long argued the Karoo turnover is not the same event as the marine extinction. Its argument rests on uranium-lead ash dates.
- 28a.
Section Abstract: “The current model for the end-Permian terrestrial ecosystem crisis holds that systematic loss exhibited by an abrupt turnover from the Daptocephalus to the Lystrosaurus Assemblage Zone (AZ; Karoo Basin, South Africa) is time equivalent with the marine Permian–Triassic boundary (PTB).” ↩
- 28a.
- 29.
Nowak, Hendrik et al. “No mass extinction for land plants at the Permian–Triassic transition.” Nature Communications 10:384. 2019. A comparison of global occurrence data for plant macrofossils and for spores and pollen across the boundary. It finds the two records disagree and that the case for a plant mass extinction does not survive the sampling problems. Mirror: PMC
- 29a.
Section Abstract: “We show that the plant fossil record is strongly biased and that evidence for a mass extinction among plants in the latest Permian is not robust.” ↩
- 29a.
- 30.
Song, Haijun et al. “Decoupled taxonomic and ecological recoveries from the Permo-Triassic extinction.” Science Advances 4(10):eaat5091. 2018. A database of 51,055 occurrences of marine genera from the latest Permian to the end of the Triassic, sorted into non-motile, motile and swimming groups. It finds genus counts back to pre-extinction levels early in the Middle Triassic, but ecosystems rebuilt from the top of the food chain down over a much longer span. Mirror: PMC
- 30a.
Section Results and Discussion: “The apparent vulnerable nature of the ecosystem at this time is also supported by the dominance of opportunistic organisms in the aftermath of the P-Tr extinction (e.g., cyanobacteria, small foraminifers, Claraia bivalves, and linguloid brachiopods)”. ↩
- 30b.
Section Ecological recovery: “Non-motile animals suffered the most severe extinction, and their diversity declined markedly from more than 500 genera in the Late Permian to fewer than 100 genera in the Early Triassic. Non-motile animals achieved pre-extinction levels after a rapid rebound in the initial Middle Triassic.” ↩
- 30c.
Section Taxonomic recovery: “Following the P-Tr mass extinction, marine generic diversity finally attained pre-extinction levels in the early Anisian”. ↩
- 30d.
Section Abstract: “In Triassic oceans, animals at high trophic levels recovered faster than those at lower levels.” ↩
- 30a.
- 31.
Modesto, Sean P. “The disaster taxon Lystrosaurus: a paleontological myth.” Frontiers in Earth Science 8:610463. 2020. A review of the definitions of "disaster taxon" and of the stratigraphy and family tree of Lystrosaurus species, by a Canadian vertebrate palaeontologist. It concludes the label does not fit.
- 31a.
Section Abstract: “leads to the conclusion that the genus is not a “disaster taxon”. … At most, species of Lystrosaurus that form the informal “Lystrosaurus abundant zone” in the lower Katberg Formation, Lower Triassic of South Africa, could be described as opportunistic species.” ↩
- 31a.
- 32.
Payne, Jonathan L. “Evolutionary dynamics of gastropod size across the end-Permian extinction and through the Triassic recovery interval.” Paleobiology 31(2):269–290. 2005. A global database of fossil snail sizes from the Permian to the Middle Triassic by a Stanford palaeobiologist. It tests whether the small size of Lower Triassic snails is real or an artefact of preservation, and finds it real.
- 32a.
Section Abstract: “no specimens of unambiguous Early Triassic age larger than 2.6 cm have been reported, in contrast to common 5– 10-cm specimens of both Permian and Middle Triassic age. The loss of large gastropods is abrupt even at a fine scale of stratigraphic resolution, whereas the return of larger individuals in the Middle Triassic appears gradual when finely resolved.” ↩ ↩
- 32a.
- 33.
Wignall, Paul B., and Michael J. Benton. “Lazarus taxa and fossil abundance at times of biotic crisis.” Journal of the Geological Society 156(3):453–456. 1999. A test of why so many groups vanish from the record after the end-Permian and end-Triassic and return later. It compares the share of missing groups with the number of fossil sites and with likely refuges.
- 33a.
Section Abstract: “there is no link with the abundance of fossiliferous sites and the proportion of Lazarus taxa nor are missing taxa encountered in potential refuges. Therefore, the abundance of Lazarus taxa in the aftermath of these extinctions is probably a reflection of the extreme rarity of organisms at this time.” ↩
- 33a.
- 34.
Brayard, Arnaud et al. “Unexpected Early Triassic marine ecosystem and the rise of the Modern evolutionary fauna.” Science Advances 3(2):e1602159. 2017. The description of the Paris Biota, an exceptionally preserved fauna from the upper Lower Triassic of Idaho with at least seven phyla. It shows that complex communities existed earlier, at least locally, than the stepwise model allows, and that soft-bodied groups can vanish from the ordinary record for very long spans. Mirror: PMC
- 34a.
Section Abstract: “it illustrates a phylogenetically diverse, functionally complex, and trophically multileveled marine ecosystem, from primary producers up to top predators and potential scavengers.” ↩
- 34b.
Section Abstract: “primitive Cambrian-Ordovician leptomitid sponges (a 200–million year Lazarus taxon)”. ↩
- 34c.
Section Introduction: “The postcrisis biotic recovery was rapid for some nektonic-pelagic groups, such as ammonoids and conodonts”. ↩
- 34a.
- 35.
Foster, William J. et al. “Subsequent biotic crises delayed marine recovery following the late Permian mass extinction event in northern Italy.” PLOS ONE 12(3):e0172321. 2017. A bed-by-bed study of six sections of the Werfen Formation in the Dolomites, sampling 328 fossil beds. It finds the recovery interrupted by later extinction bursts within the Lower Triassic.
- 35a.
Page 2: “The Lower Triassic succession of the Dolomites, Italy, is represented by the Werfen Formation which is approximately 250m thick in the Adige Valley and up to 600-700m thick in the eastern Dolomites”. ↩
- 35b.
Page 1: “Here, we show that elevated extinction rates were recorded not only in the Dienerian, as previously recognised, but also around the Smithian/Spathian boundary.” Page 5: “In total, 328 fossiliferous beds were sampled for invertebrate macrofossils.” ↩
- 35a.
- 36.
Hofmann, Richard. “Trace fossils of the Werfen Formation.” Geo.Alp 14:93–105. 2017. A field guide to the burrows and trails of the Lower Triassic Werfen Formation in the Dolomites by a trace-fossil specialist, member by member.
- 36a.
Page 93: “Observations from the Griesbachian Mazzin Member suggest that bioturbation virtually vanished during the early post-extinction aftermath with only shallow deposit feeding structures occurring in some levels. A first significant rebound in ichnodiversity and both epi- and infaunal ecosystem complexity is recorded in the lower Seis/Siusi Member … The succeeding Gastropod Oolite and Campil Members again record a drop in general bioturbation intensity and trace fossil diversity. Finally, with the presence of comparably larger Thalassinoides and Palaeophycus-type burrows, the fully marine Val Badia Member signifies the most advanced recovery stages observed in the Werfen Formation.” ↩
- 36a.
- 37.
Pruss, Sara B., and David J. Bottjer. “Early Triassic trace fossils of the western United States and their implications for prolonged environmental stress from the end-Permian mass extinction.” Palaios 19(6):551–564. 2004. A study of the burrows and trails in the Virgin Limestone, the last Lower Triassic stage in Utah and Nevada.
- 37a.
Section Abstract: “Whereas diversity of trace-fossil assemblages increased from earliest to late Early Triassic time, persistent small size, low average ichnofabric index, low bedding-plane coverage, and reduced tiering point to prolonged stressful environmental conditions”. ↩
- 37a.
- 38.
Kelley, Brian M. et al. “Prolonged and gradual recovery of metazoan-algal reefs following the end-Permian mass extinction.” Geology 51(11):1011–1016. 2023. Field mapping, satellite imagery and 164 thin sections through the oldest and thickest Lower to Middle Triassic platform-margin reef known, at the Great Bank of Guizhou in southern China. It records the order in which the reef builders appear.
- 38a.
Page 1011: “Previous work suggests that metazoan-algal reefs were absent for 8−10 m.y. following extinction … In contrast, our analyses indicate that calcareous sponges, calcareous algae, and early scleractinian corals occurred progressively in the GBG reef and that biotic recovery metrics increased gradually.” ↩
- 38b.
Page 1012: “The reef initiated in the upper Spathian (Payne et al., 2006) and persisted in situ to upper Pelsonian or lower Illyrian strata (Kelley et al., 2020), reaching a stratigraphic thickness of ∼900 m (Lehrmann et al., 1998). The reef facies is characterized by the occurrence of Tubiphytes boundstone.” Page 1014: “The lowest stratigraphic occurrence of identifiable reefbuilding metazoans (calcareous sponges) coincides with the base of zone 2, 365 m above the reef base … the first framework-contributing calcareous algae (Fig. 4L; 665 m above the reef base), and the first scleractinian corals (Figs. 4M and 4N; 895 m above the reef base).” ↩
- 38a.
- 39.
Retallack, Gregory J. et al. “Global coal gap between Permian–Triassic extinction and Middle Triassic recovery of peat-forming plants.” GSA Bulletin 108(2):195–207. 1996. A worldwide survey of coal through the Permian and Triassic by a palaeosol specialist and two Australian colleagues, testing tectonic, climatic and biological explanations for the Lower Triassic's lack of coal.
- 39a.
Section Abstract: “Early Triassic coals are unknown, and Middle Triassic coals are rare and thin. … Tectonic and climatic explanations for the coal gap fail because deposits of fluctuating sea levels and sedimentary facies and paleosols commonly found in coal-bearing sequences are present also in Early Triassic rocks.” ↩
- 39a.
- 40.
Chen, Zhong-Qiang, and Michael J. Benton. “The timing and pattern of biotic recovery following the end-Permian mass extinction.” Nature Geoscience 5:375–383. 2012. A widely cited review of the Triassic recovery by a Chinese palaeontologist and the Bristol vertebrate palaeontologist Michael Benton. It reads the record as a stepwise rebuilding from the bottom of the food chain up.
- 40a.
Section Abstract: “Triassic ecosystems were rebuilt stepwise from low to high trophic levels through the Early to Middle Triassic, and a stable, complex ecosystem did not re-emerge until the beginning of the Middle Triassic”. ↩
- 40a.
- 41.
Hu, Shi-xue et al. “The Luoping biota: exceptional preservation, and new evidence on the Triassic recovery from end-Permian mass extinction.” Proceedings of the Royal Society B 278(1716):2274–2282. 2011. The description of an exceptionally preserved Middle Triassic marine fauna from Yunnan, China, with fishes, marine reptiles and arthropods. It is used as the marker of a fully rebuilt marine ecosystem. Mirror: PMC
- 41a.
Page 2274: “New trophic levels were introduced, most notably among top predators in the form of the diverse marine reptiles that had no evident analogues in the Late Permian.” ↩
- 41a.
- 42.
Tschudy, Robert H. et al. “Disruption of the terrestrial plant ecosystem at the Cretaceous-Tertiary boundary, Western Interior.” Science 225(4666):1030–1032. 1984. Pollen and spore counts across the boundary at two widely separated Western Interior sites by a U.S. Geological Survey team, the paper that first described the fern spike over the iridium clay.
- 42a.
Section Abstract: “The palynologically defined Cretaceous-Tertiary boundary in the western interior of North America occurs at the top of an iridium-rich clay layer. The boundary is characterized by the abrupt disappearance of certain pollen species, immediately followed by a pronounced, geologically brief change in the ratio of fern spores to angiosperm pollen.” ↩
- 42a.
- 43.
Vajda, Vivi et al. “Indication of global deforestation at the Cretaceous-Tertiary boundary by New Zealand fern spike.” Science 294(5547):1700–1702. 2001. Pollen and spore counts across the boundary in New Zealand, the first Southern Hemisphere record of the fern spike, found together with an iridium anomaly.
- 43a.
Section Abstract: “The devastating effect on terrestrial plant communities of a bolide impact at the Cretaceous-Tertiary boundary is shown in fossil pollen and spore assemblages by a diverse flora being abruptly replaced by one dominated by a few species of fern.” ↩
- 43a.
- 44.
Sheehan, Peter M. et al. “Sudden extinction of the dinosaurs: latest Cretaceous, upper Great Plains, U.S.A.” Science 254(5033):835–839. 1991. A three-year field survey of dinosaur families through three levels of the Hell Creek Formation in Montana and North Dakota, comparing like rock types to control for preservation.
- 44a.
Section Abstract: “Results of a three-year field study of family-level patterns of ecological diversity of dinosaurs in the Hell Creek Formation of Montana and North Dakota show no evidence (probability P < 0.05) of a gradual decline of dinosaurs at the end of the Cretaceous. … preservational biases were corrected for by comparison of results only from similar fades”. "fades" is "facies" as printed in the abstract. ↩ ↩
- 44a.
- 45.
Hurlbert, Stuart H., and J. David Archibald. “No statistical support for sudden (or gradual) extinction of dinosaurs.” Geology 23(10):881–884. 1995. A statistical critique of Sheehan's survey by an ecologist known for his work on experimental design and a vertebrate palaeontologist. It argues the data cannot decide between sudden and gradual.
- 45a.
Section Abstract: “Examination of the quantitative methodologies used shows that these provide no basis for choosing between scenarios of abrupt extinction and gradual decline.” ↩
- 45a.
- 46.
Longrich, Nicholas R. et al. “Mass extinction of lizards and snakes at the Cretaceous–Paleogene boundary.” Proceedings of the National Academy of Sciences 109(52):21396–21401. 2012. A revision of the latest Cretaceous and earliest Paleocene lizards and snakes of western North America from museum collections, by three Yale palaeontologists. Mirror: PMC
- 46a.
Page 21396: “Species-level extinction was 83%, and the K-Pg event resulted in the elimination of many lizard groups and a dramatic decrease in morphological disparity. Survival was associated with small body size and perhaps large geographic range.” Page 21398: “Of the 30 species found in the late Maastrichtian, only five … occur in the Paleocene.” ↩
- 46a.
- 47.
Longrich, Nicholas R. et al. “Mass extinction of birds at the Cretaceous–Paleogene (K–Pg) boundary.” Proceedings of the National Academy of Sciences 108(37):15253–15257. 2011. A description of 17 bird species from the last Cretaceous beds of western North America, most known from shoulder bones, testing whether archaic birds dwindled before the boundary. Mirror: PMC
- 47a.
Section Discussion: “rather than disappearing gradually over the course of the Cretaceous, at least four separate lineages of archaic birds persisted up to the K–Pg boundary … Definitive fossils of archaic birds have never been reported from the Paleogene”. ↩
- 47a.
- 48.
Lyson, Tyler R. et al. “Exceptional continental record of biotic recovery after the Cretaceous-Paleogene mass extinction.” Science 366(6468):977–983. 2019. A study by a Denver Museum of Nature & Science team of unusually complete mammal, reptile and plant fossils in a time-calibrated section at Corral Bluffs, Colorado, covering the first part of the Paleocene. It gives the order in which mammal diversity, mammal size and plant diversity recovered.
- 48a.
Section Abstract: “Within ~100 thousand years (ka) post-KPgE, mammalian taxonomic richness doubled, and maximum mammalian body mass increased to near pre-KPgE levels. A threefold increase in maximum mammalian body mass and dietary niche specialization occurred at ~300 ka post-KPgE, concomitant with increased megafloral standing species richness. The appearance of additional large mammals occurred by ~700 ka post-KPgE, coincident with the first appearance of Leguminosae (the bean family).” The ages are the authors' figures from radiometric and magnetic dating; the article uses only the order. ↩
- 48a.
- 49.
Fuentes, Anthony J. et al. “Constructing a timescale of biotic recovery across the Cretaceous-Paleogene boundary, Corral Bluffs, Denver Basin, Colorado.” bioRxiv. 2019. The preprint of the stratigraphic framework for the Corral Bluffs fossils, with the pollen record used to place the boundary in ten sections.
- 49a.
Section Results: “Samples from above show the appearance of typical Paleocene Momipites, and low diversity assemblages often dominated by palm pollen (Arecipites spp.).” ↩
- 49a.
- 50.
Olsson, Richard K. et al. “Atlas of Paleocene Planktonic Foraminifera.” Smithsonian Contributions to Paleobiology 85. Smithsonian Institution Press. 1999. The standard taxonomic atlas and zonal scheme for Paleocene planktic foraminifera, by the working group of the specialists who defined the zones.
- 50a.
Page 9: “Biostratigraphic interval characterized by the partial range of the nominate taxon between the Last Appearance Datum (LAD) of Cretaceous taxa (Globotruncana, Rugoglobigerina, Globigerinelloides, among others) at the K/P boundary as delineated by the essentially global iridium spike and the First Appearance Datum (FAD) of Parvularugoglobigerina eugubina.” Definition of Zone P0, the Guembelitria cretacea Partial Range Zone. ↩
- 50b.
Page 9: Subzone P1a ends with the first appearance of Subbotina triloculinoides; P1b with the first appearance of Globanomalina compressa and/or Praemurica inconstans; P1c with the first appearance of Praemurica uncinata. ↩
- 50c.
Page 10: “The microperforate species, which evolved from the survivor-species Guembelitria cretacea”. ↩
- 50a.
- 51.
Molina, Eustoquio et al. “The Global Boundary Stratotype Section and Point for the base of the Danian Stage (Paleocene, Paleogene, "Tertiary", Cenozoic) at El Kef, Tunisia.” Episodes 29(4):263–273. 2006. The formal description of the section chosen as the world reference for the base of the Paleocene, with its fossil, iridium and isotope records.
- 51a.
Page 266: “The Ir distribution shows a millimetre thick pulse-like feature occurring in perfect coincidence with the beginning of the biological crisis.” Page 268: “A rich assemblage, consisting of at least 17 taxa, occurs in the interval from meters 7 to 2 below the K/Pg boundary.” The second quotation is about the ammonites. ↩
- 51a.
- 52.
Lowery, Christopher M. et al. “Rapid recovery of life at ground zero of the end-Cretaceous mass extinction.” Nature 558:288–291. 2018. Fossils, trace fossils and chemistry from the first Paleocene sediment in a drill core through the Chicxulub crater's peak ring, by the International Ocean Discovery Program's Expedition 364 team.
- 52a.
Section Main text: “Clear, discrete trace fossils, including Planolites and Chondrites, characterize the upper 20 cm of the transitional unit (above 54 cm) (Fig. 1, Extended Data Fig. 2), providing unequivocal evidence for benthic life in the crater within years of the impact.” ↩
- 52b.
Section Main text: “The lowermost sample taken in this limestone (34 cm) contains the planktic foraminifer Parvularugolobigerina eugubina, which marks the base of Zone Pα, as well as P. extensa, P. alabamensis, and Guembelitria cretacea. Because many other species that originate within Zone Pα first appear a few cm higher in the section (31–32 cm)”. The depths are measured down the core, so smaller numbers are higher in the section. ↩ ↩
- 52a.
- 53.
Machalski, Marcin et al. “Ammonite survival across the Cretaceous–Paleogene boundary confirmed by new data from Denmark.” Scientific Reports 15:45802. 2025. A study of ammonites in the earliest Paleocene limestone at Stevns Klint, Denmark, testing whether they lived there or were washed in from older beds. It concludes most are true survivors.
- 53a.
Page 1: “In summary, our results confirm ammonite survival into the Danian for the bulk of the Cerithium Limestone fauna”. Page 3: “The Fiskeler is typically 5–10 cm thick”. Page 5: “Main Cerithium Limestone, 10 cm above the Fiskeler base … Main Cerithium Limestone, 37 cm above the Fiskeler base”. ↩
- 53a.
- 54.
Marshall, Charles R., and Peter D. Ward. “Sudden and gradual molluscan extinctions in the latest Cretaceous of western European Tethys.” Science 274(5291):1360–1363. 1996. A statistical analysis of ammonite and clam ranges in latest Cretaceous sections of Spain and France, separating the sudden boundary loss from earlier losses.
- 54a.
Section Abstract: “(i) a major extinction at or near the Cretaceous-Tertiary (K-T) boundary, probably caused by the impact, (ii) either a faunal abundance change or an extinction of up to nine ammonite species associated with a regression event shortly before the boundary, (iii) gradual extinction of most inoceramid bivalves well before the K-T boundary”. ↩
- 54a.
- 55.
Harper, David A. T. et al. “End Ordovician extinctions: a coincidence of causes.” Gondwana Research 25(4):1294–1307. 2014. A review of the end-Ordovician extinction, its two pulses and their proposed causes, by Durham and Copenhagen palaeontologists.
- 55a.
Section Abstract: “It comprised two discrete pulses, both linked in different ways to an intense but short-lived glaciation at the South Pole. The first, occurring at, or just below, the Normalograptus extraordinarius graptolite Biozone, mainly affected nektonic and planktonic species together with those living on the shallow shelf and in deeper water whereas the second, within the N. persculptus graptolite Biozone, was less focused, eradicating faunas across a range of water depths. In all about 85% of marine species were removed.” ↩
- 55a.
- 56.
Finnegan, Seth et al. “Climate change and the selective signature of the Late Ordovician mass extinction.” Proceedings of the National Academy of Sciences 109(18):6829–6834. 2012. A statistical model of which North American marine genera died in the first end-Ordovician pulse, using sixteen ecological and geological variables. Mirror: PMC
- 56a.
Page 6829: “it eliminated an estimated 61% of marine genera globally”. “glacioeustatic sea-level fall and tropical ocean cooling played important roles in the first pulse of the Late Ordovician mass extinction in Laurentia”. ↩
- 56a.
- 57.
Stigall, Alycia L. “Speciation collapse and invasive species dynamics during the Late Devonian "Mass Extinction".” GSA Today 22(1):4–9. 2012. A synthesis of species-level studies of Late Devonian marine animals by an Ohio University palaeontologist, arguing that the crisis came from a collapse in the formation of new species as invasive species spread between basins.
- 57a.
Page 4: “Statistical evaluation of diversity change reveals that the primary cause of biodiversity decline was reduced speciation during the crisis interval, not elevated extinction rates.” “The Frasnian-Famennian event is, therefore, better termed a “biodiversity crisis” than a “mass extinction.”” ↩
- 57b.
Page 4: “The Middle Devonian included the most geographically widespread metazoan reef ecosystem in Earth’s history, but its extent was reduced by a factor of 5000 following the crisis interval (Copper, 1994).” Stigall is citing Paul Copper's 1994 study of Devonian reefs. ↩
- 57a.
- 58.
Olsen, Paul E. et al. “Ascent of dinosaurs linked to an iridium anomaly at the Triassic-Jurassic boundary.” Science 296(5571):1305–1307. 2002. A study of footprints and bones from more than 70 localities in the rift basins of eastern North America, with iridium and spore counts across the boundary, by a Columbia University team.
- 58a.
Section Abstract: “Analysis of tetrapod footprints and skeletal material from more than 70 localities in eastern North America shows that large theropod dinosaurs appeared less than 10,000 years after the Triassic-Jurassic boundary … synchronous with a terrestrial mass extinction. This extraordinary turnover is associated with an iridium anomaly … and a fern spore spike”. ↩ ↩
- 58a.
- 59.
Snelling, Andrew A. Earth's Catastrophic Past: Geology, Creation & the Flood. Institute for Creation Research. 2009. A two-volume, 1,100-page textbook of Flood geology by Answers in Genesis's director of research, an Australian geologist with a Sydney PhD. It treats mass extinctions as global burials inside the Flood and places the end of the Flood above the end-Cretaceous.
- 59a.
Page 575: “At these levels in the geologic record a great variety of organisms, those that would have been living in both marine and terrestrial environments, both stationery and swimming forms, carnivores and herbivores, protozoans and metazoans, were buried on a global scale, so the catastrophic processes involved transcended specific ecological, morphological, and taxonomic groupings of organisms simultaneously on the land and in the sea.” "stationery" is in the original. ↩
- 59b.
Page 576: “Asteroid or comet impacts, and/or catastrophic volcanic outpourings, as explanations for this global catastrophism have evidence to support them, and both are consistent with the global catastrophic Flood within the biblical framework for earth history.” ↩
- 59c.
Page 741: “Of course, the so-called mass extinctions would be expected to coincide with these major unconformities, because the abrupt change in sedimentation, and/or lowered water levels, would likely have resulted in the mass burial of the creatures carried in each major wave of sedimentation, prior to different creatures being carried by the subsequent sedimentation.” ↩ ↩
- 59d.
Page 740: “Those rock layers that have some bioturbation in their rock portions, however, would represent the passing of at least a few hours for the animals to have walked around and left their footprints and trails, or to have burrowed in the sediment surfaces before the next layers were deposited.” ↩
- 59e.
Page 761: “available evidence suggests that the Flood/post-Flood boundary certainly must be above the Cretaceous/Tertiary boundary in the strata record.” ↩
- 59a.
- 60.
Clarey, Tim. Ammonites on Both Sides of the K-Pg Best Explained by the Global Flood, Not an Asteroid. Institute for Creation Research. Apr 23, 2026. An ICR news article on Machalski and colleagues' 2025 finding of ammonites living into the earliest Paleogene in Denmark. It applies ICR's view that extinctions are only last burials to ammonites and to living fossils.
- 60a.
Section paragraphs 3–5: “Most extinction events described by conventional scientists are not really extinctions at all. They are merely the last occurrence of a species, or many species at about the same level, in the rock record. … Then, as the water rose even higher to the next ecological zone, it buried new types of animals and plants that lived at higher elevations in the pre-Flood world. … They never really went extinct—they just didn’t get fossilized after a certain level. The ammonites may be like the coelacanths in that they might have survived the Flood and lived in the seas much more recently than thought.” ↩ ↩
- 60a.
- 61.
Brand, Leonard, and Arthur Chadwick. Faith, Reason, & Earth History: A Paradigm of Earth and Biological Origins by Intelligent Design. Andrews University Press. 3rd edition. 2016. A college textbook by two Adventist scientists, a biologist and a geologist, who did much of the published creationist field work on fossil whales and on the Coconino sandstone. Its "short-age" model treats each mass extinction as the final destruction of a life zone during the catastrophe.
- 61a.
Chapter 18, section Extinctions: “Short-age geology proposes, on the other hand, that these crises occurred when the geological catastrophe reached some critical point and the remaining members of certain groups of organisms were all killed and buried. A life zone may have been destroyed. … In some cases, a group of organisms went almost extinct, and those individuals that survived the extinction avoided getting buried and fossilized. … Those who accept a short-age theory also do not know exactly what happened”. ↩ ↩
- 61a.
- 62.
Wise, Kurt P. “The Pre-Flood Floating Forest: A Study in Paleontological Pattern Recognition.” Proceedings of the Fifth International Conference on Creationism, 371–381. 2003. Proposes that the Paleozoic land plants and their animals lived on a continent-sized floating mat that the Flood broke up from the edge inward, giving the order of Paleozoic plants and the Carboniferous coals. It is the main young-earth account of why the Paleozoic land flora and fauna are gone. ICR's geologists later rejected the floating forest.
- 62a.
Page 371: “It is further suggested that the residual catastrophism of the post-Flood period prevented the restoration of the antediluvian floating forest biome and resulted in the extinction of most of the Paleozoic plants and ‘land’ animals.” Page 376: “The permanent destruction of the floating forest biome would explain why virtually all Paleozoic 'land' animals are extinct.” ↩
- 62a.
- 63.
Creation Ministries International. Response to PBS NOVA Evolution series, Episode 3: Extinction! Feb 14, 2006. CMI's rebuttal of a television documentary on mass extinctions. It is the one source found that separates the losses by habitat: marine extinctions in the Flood, land extinctions in the centuries after it.
- 63a.
Section Creationist explanation: “Biblical creationists would explain much of the fossil record by the global Flood of Noah’s day. However, this didn’t directly cause any land vertebrates to become extinct, because each kind was represented on the Ark … But many became extinct in subsequent centuries, because of factors already well known to conservationists. … But the Flood probably did cause many marine species to become extinct.” ↩
- 63a.
- 64.
Montaggioni, Lucien F. “History of Indo-Pacific coral reef systems since the last glaciation: development patterns and controlling factors.” Earth-Science Reviews 71:1–75. 2005. A review of the drilled and dated Holocene reefs of the Indo-Pacific, tabulating how fast reef margins built upward and outward in different settings.
- 64a.
Page 43: “In exposed settings, the mean aggradation rates range between 1.5 and 12 mm year⁻¹, with a mode of 5 mm year⁻¹ (Table 5). In semi-exposed to sheltered reef margins, vertical accretion rates average 1 to 25 mm year⁻¹, with a mode of 9 mm year⁻¹ (Table 6).” ↩
- 64a.
- 65.
This article's arithmetic. 900 m of reef in at most the 50 days ICR assigns to the whole Absaroka (Days 40 to about 90) is 18 m a day, or 6,570 m a year. Divided by 25 mm a year, the top of the range Montaggioni gives for average vertical accretion of modern sheltered reef margins, the ratio is about 263,000. The Guizhou reef spans only part of the Absaroka, so the true requirement on ICR's timetable is higher. ↩