"86% of strata in this 430-m succession are unbioturbated" — Lidya Tarhan and eleven co-authors, on a Lower Devonian section in Algeria, Science Advances, 20251
"Only a small fraction of the total thickness has an ichnofabric index of 1, while the majority of the total thickness has an ichnofabric index of 3 or greater." — John Woodmorappe, creationist geologist, on 1,151 metres of Cambrian strata, Journal of Creation, 20062
"However, neither perspective is consistent with the actual rock record" — Carl Froede Jr., creationist geologist, on the diluvial prediction that Flood strata should be little burrowed, Journal of Creation, 20093
Summary
A burrow is a record of an animal living in sediment after that sediment stopped arriving. Count the burrowed surfaces in a formation, multiply by the time each one needed, and the result is a minimum duration for the formation that owes nothing to radiometric dating. That is why bioturbation is a problem for any model that deposits hundreds of metres of rock in days.
Andrew Snelling, whose Earth's Catastrophic Past carries the fullest young-earth treatment of the subject, states the problem himself: "Because bioturbation requires the passage of time, the degree of bioturbation found preserved in sedimentary strata at numerous levels in the rock record would likewise presumably testify to the passage of perhaps significant amounts of time."44 His answer is that the time needed is short, and that most Flood strata are not burrowed anyway.
The verdict. Bioturbation is unevenly distributed through the column, and the young-earth generalisation is about half right. Long stretches of lower Palaeozoic rock really are barely burrowed, and mainstream ichnologists say so in print with numbers. Cretaceous shelf sediments are the opposite: homogenised through their whole thickness, with reworking outpacing deposition, and they sit inside the Flood year on the young-earth models that put the boundary in the late Mesozoic or the Cenozoic, which is most of them. The rate literature the creationist side cites does not rescue them. Its one community-scale measurement is the fast end of a range running to 24 weeks, and no young-earth author has counted the colonisation surfaces in a named formation and shown they fit in a year. Four young-earth authors have published in their own movement's journals that its answers here do not work.
Nine points, stated first.
- Mainstream ichnology reports the pattern the Flood side predicts, in parts of the Palaeozoic, and this article leads with it. A 2025 compilation in Science Advances by Lidya Tarhan and eleven co-authors reports that in a 430 metre Lower Devonian succession in Algeria, "86% of strata in this 430-m succession are unbioturbated."11 Frasnian carbonates of the Great Basin and Rockies have "a mean ii of 2.0."1 Lower Cambrian strata "only rarely exceed ii 3 and are most commonly characterized by ii 1 or 2."1 None of that came from a creationist source.
- An unbioturbated bed is not proof of rapid burial, and the standard textbook says so. Richard Bromley lists other causes: "In particular, fluctuation in salinity may severely reduce the biological diversity of a fauna … Another important limiting factor is the availability of oxygen."55 Any argument that runs from bare laminae straight to a Flood has skipped a step.
- Where the creationist literature's own cited survey looked, the rocks are heavily burrowed, and the creationist author reports it accurately. Woodmorappe, writing in Journal of Creation, points his readers at "48 Cambrian stratigraphic sections and 1,151 total metres of sedimentary strata in the western USA" and states: "Only a small fraction of the total thickness has an ichnofabric index of 1, while the majority of the total thickness has an ichnofabric index of 3 or greater."22 His figure checks out against the primary, where Mary Droser and David Bottjer logged 810 metres of inner shelf plus 341 metres of middle shelf.666
- Two young-earth authorities describe the same rocks incompatibly. Snelling writes that "there is so little bioturbation of sedimentary strata in the geologic record" that the record is evidence for rapid deposition.4 Woodmorappe puts the majority of 1,151 Cambrian metres at index 3 or above, meaning at least 10% of bedding destroyed and often all of it.
- The one fast community-scale rate in the creationist literature is the low end of a range, and the range is never printed. Snelling gives "a 12-cm-thick layer of sediment can be 67 percent bioturbated in as little as 5.5 hours."4 His source, Woodmorappe, prints 15.5 hours for the same sentence and citation.2 The primary, Kurt Grimm and Karl Föllmi in Palaios, gives "Estimated durations range from 15.5 to 4020 hours (~1 day to 24 weeks)" and calls 15.5 hours "the shortest estimated duration."777 Neither creationist source reports the upper bound.
- Measured reworking rates span five orders of magnitude, and the fast figure is a maximum-density model. Murray Gingras and colleagues X-rayed estuarine animals in aquaria and scaled the result to one square metre. Ten filter feeders: 115 years. Ten irregular echinoderms: 42 days. Maximum modelled densities: 61 minutes.88 Their verdict on the ichnofacies that dominates the Grand Canyon's Cambrian sandstones is not the 61-minute case: "highly burrowed examples of the Skolithos Ichnofacies reflect high population densities and at least seasonal time spans."8
- The layer animals mix is thin and nearly the same everywhere, so a homogenised column is a stack of thin reworked slices. Bernard Boudreau compiled tracer profiles worldwide and found the mixed layer "is essentially independent of burial velocity with a worldwide mean of 9.8 ± 4.5 cm."99 Cambrian mixing was shallower still, 2 to 6 centimetres.6 In the lower Cambrian Zhushadong Formation of North China, burrow shafts reach 3.1 centimetres but repeated post-storm colonisation amalgamates into intervals "up to 170 cm thick," roughly 55 successive colonisations of one patch of seafloor.1010
- Woodmorappe's own time budget fails on his own numbers. He allows "one year (8,766 hours) of overall deposition with active sedimentation occurring half of this time," leaving 4,383 quiet hours.2 At the 15.5 hours per surface he himself cites, that buys about 283 surfaces, roughly 34 metres of heavily reworked rock for the entire Flood, worldwide. The arithmetic is this article's, run on his figures. The one Cambrian survey he points at covers 1,151 metres.
- Four young-earth authors have published that the movement's answers fail, and nobody has answered them. Carl Froede Jr., 2009: of the diluvial prediction of little bioturbation and its uniformitarian rival, "neither perspective is consistent with the actual rock record," and one Skolithos horizon took "months, not years or decades."333 Chad Arment, 2023: the time needed for Palaeocastor burrows "clearly disconfirms" formation during the Flood.1111 Froede, Jerry Akridge and John Reed, 2022: tracks of living animals run "well past the megasequence-defined Day 150 termination of all terrestrial life."1212
What decides the case, and what does not
Speed of digging is the wrong variable. Bromley's textbook says a Flood-like event can produce fast pioneer burrowing: after a storm deposit, opportunists "speedily colonize a habitat," making low-diversity vertical dwelling burrows.5 Nobody needs to deny that. What rapid deposition cannot produce is his other category, the climax community: high trace-fossil diversity, deep tiers occupied, later burrowers cutting across earlier ones. The question to ask of a disputed formation is not whether an animal could dig that fast, but whether the rock records pioneers or a mature community, and how many times over.
Part 1: How bioturbation is measured
The ichnofabric index
Before 1986 there was no agreed way to write down how burrowed a rock is. Mary Droser and David Bottjer supplied one in a two-page note in the Journal of Sedimentary Petrology. They photographed vertical rock faces 50 centimetres by 35 centimetres in lower Palaeozoic carbonates of the Great Basin, measured the disrupted area on each photograph with a planimeter, and cut the results into six bands.1313 The bands are the ichnofabric index, written ii 1 to ii 6:
| Index | Definition, verbatim |
|---|---|
| ii 1 | "No bioturbation recorded; all original sedimentary structures preserved." |
| ii 2 | "Discrete, isolated trace fossils; up to 10% of original bedding disturbed." |
| ii 3 | "Approximately 10 to 40% of original bedding disturbed. Burrows are generally isolated, but locally overlap." |
| ii 4 | "Last vestiges of bedding discernable; approximately 40 to 60% disturbed. Burrows overlap and are not always well defined." |
| ii 5 | "Bedding is completely disturbed, but burrows are still discrete in places and the fabric is not mixed." |
| ii 6 | "Bedding is nearly or totally homogenized." |
The scale is applied with printed cards: "Enlargements of the schematic diagrams of ichnofabric indexes 1 through 5 (Fig. 1) can be used in the field as 'flash cards' to rank bioturbation."13 A section is logged continuously, index against thickness, "analogous to the continuous logging of thicknesses of strata in a section for properties such as rock color or lithology."6
Two cautions come from the authors themselves and both help the young-earth side. The cards were drawn for one kind of rock, so "different schematic 'flash cards' will be necessary to study different types of strata," built on the same definitions "so that the data are comparable."13 Comparing Cambrian carbonate with Cretaceous shale is not straightforward. And the index measures percentage of bedding destroyed: not depth, not time. Turning an index into a duration takes a second step, a rate, and that step is where every disagreement in this article lives.
The bioturbation index
A second scale, the bioturbation index or BI, runs 0 to 6 and attaches explicit percentages. It comes from Andrew Taylor and Roland Goldring in 1993. That paper could not be obtained for this article. Its definitions are reproduced verbatim in the methods of an open-access 2017 paper by Li-Jun Zhang and colleagues, and are quoted here from that reproduction:10
| Index | Percent reworked | Definition, as reproduced by Zhang et al. |
|---|---|---|
| BI 0 | 0% | "no bioturbation" |
| BI 1 | 1–4% | "sparse bioturbation with few discrete biogenic structures locally overprinting the well-preserved sedimentary fabric" |
| BI 2 | 5–30% | "low bioturbation in sediment with well-preserved sedimentary structures" |
| BI 3 | 31–60% | "discrete trace fossils, moderate bioturbation and still distinguishable bedding contacts" |
| BI 4 | 61–90% | "intense bioturbation, high trace-fossil density, common overlap trace fossils, and primary sedimentary structures mostly erased" |
| BI 5 | 91–99% | "intense bioturbation and a completely disturbed bedding" |
| BI 6 | 100% | "completely bioturbated and reworked sediment, revealed by repeated overprinting of trace fossils" |
The two scales are close but not identical, and the literature uses whichever the underlying study used. Nothing below silently converts one into the other.
Tiers, and the layer that actually gets mixed
Burrowers do not work at one depth. The standard division, as Zhang and colleagues state it, is that "The shallow tier is represented by structures emplaced in the upper 6 cm of the substrate, the mid tier comprises those produced within 6–12 cm of the substrate, the deep tier consists of those formed below 12–100 cm, and the ultra-deep tier is represented by those traces emplaced below 100 cm."10
Bromley's textbook explains why this matters for reading a rock. "Deepest structures are the most complete. Only their upper parts are cross-cut by shallower structures. Activity within each tier cross-cuts structures produced in shallower tiers and tends to obliterate them."5 A preserved ichnofabric is therefore biased towards the deep end of what was there.
Tarhan and colleagues split the same idea into two measurable things: a mixed layer, the homogenised top, which "extends downward from the sediment-water interface to, on average, nearly 10 cm depth in the seafloor," and beneath it a transition layer of "discrete and actively occupied deep burrows that may, in certain settings, extend to >1 m deep."1
The mixed layer's thickness is the number the whole argument turns on. Boudreau assembled published tracer profiles from lead-210, thorium-234, caesium-137, plutonium-239, silicon-32, beryllium-7, tektites and volcanic ash across coastal, shelf, slope and deep-sea settings, and found the depth barely varies: "the tracer-identified surface mixed-depth … is essentially independent of burial velocity with a worldwide mean of 9.8 ± 4.5 cm."9 He credits physics rather than ecology: "the depth of mixing L is limited primarily by the physical difficulty and increasing energy costs of reworking and excavating deeper than 10-15 cm in a sediment medium."9
Boudreau's caveat helps the young-earth reading and belongs here. The tracer-defined depth is not a ceiling: "Specific organisms are known to burrow to depths of over 1 m … Most of the values in Table 1 are less than 20 cm. Therefore, these quoted mixing depths represent the thickness of some zone that is most frequently mixed."9 Ten centimetres is the most-worked slice, not the deepest hole.
Part 2: What the strata actually show
Start with the cases that favour a Flood
The strongest evidence for the young-earth position here is in the mainstream literature, and it is recent.
Tarhan and her co-authors compiled Phanerozoic mixed-layer and transition-layer data in 2025. Four of them are Droser, Bottjer, Boudreau and A. A. Ekdale, so the people who built the ichnofabric index, the mixing-depth compilation and the standard ichnology short course all signed the paper. For the lower Palaeozoic they report bioturbation that is sparse and shallow. Lower Cambrian heterolithic and carbonate strata "only rarely exceed ii 3 and are most commonly characterized by ii 1 or 2."1 Across the early Palaeozoic the mixed layer deepened only "from approximately 0.2 to 1.5 cm in heterolithic siliciclastic settings," which is thin enough that storm beds averaging 1.3 centimetres survived intact because burrowers could not blend across their junctions.1
The Devonian case is sharper. In a 430 metre Lochkovian to Emsian succession in the Reggane Basin of Algeria, "86% of strata in this 430-m succession are unbioturbated; 7% are characterized by BI 2, 7% by BI 4, and <1% by BI 5."1 In Frasnian carbonates of the Great Basin and the Rockies the mean ichnofabric index is 2.0, intensely bioturbated intervals "account for less than 30% of measured strata," and "beds that are vertically mixed rarely exceed 10 cm in thickness."1
Leonard Brand and Arthur Chadwick, two young-earth geologists, did the field work the movement's rate arguments should have been built on. They logged bioturbation bed by bed in "a number of rock formations in Utah and western Colorado, quantifying in detail the amount of bioturbation in rocks from Cambrian to Eocene," on their own scale of levels 1 to 4, and found "the vast majority of vertical intervals in all deposits surveyed had no bioturbation or a small amount (level 1), not enough to noticeably disturb the bedding."1414 That is the best empirical card the young-earth side holds.
Three qualifications belong beside it. Their scale is their own, levels 1 to 4, and does not map cleanly onto ii 1 to 6. Their sample is Utah and western Colorado, heavily Mesozoic and marginal-marine, while the contradictory Cambro-Ordovician data come from Great Basin shelf carbonate. And the circulated summary of their survey, that 37 formations were measured and 97% of the thickness showed no bioturbation or isolated burrows, appears in no publication this project could find. Their book gives no percentage at all. That figure is not used here; the reasons are in quarantine.
Finally, the textbook caution. Bromley's chapter on ichnofabric lists the causes of incomplete bioturbation and speed is only one: "This implies a stress factor that has prevented the completion of the work of the endobenthic community … Clearly, however, other stress factors may inhibit the complete bioturbation of the substrate. In particular, fluctuation in salinity may severely reduce the biological diversity of a fauna … Another important limiting factor is the availability of oxygen."5 He adds the reverse warning too: where erosion has cut below the burrowed top of a bed, "no bioturbation is preserved, but it would be unwise to assume that the depositional environment was devoid of life."5 An unburrowed bed is weak evidence on its own.
Then the Cambrian and Ordovician shelf
Droser and Bottjer logged the Great Basin continuously. In Cambrian rocks, "A total of 810 m of ichnofabric index data were collected from 34 Cambrian stratigraphic sections (Fig. 2) interpreted to have been deposited in an inner-shelf environment. The most commonly recorded ichnofabric indices were 3, 4, and 5."6 Further offshore the picture is quieter: "A total of 341 m of ichnofabric index data were collected from 14 Cambrian sections (Fig. 2) interpreted to have been deposited in a middle-shelf environment. The most common ichnofabric indices recorded were 2 and 3."6
The Ordovician is worse for a Flood year. The average index on the carbonate inner shelf climbs in two steps: "an increase in average ichnofabric index from 1.02, recorded from the pre-trilobite strata, to 3.1, recorded from the trilobite-bearing Lower Cambrian strata … The second major increase in extent of bioturbation occurred approximately 110 m.y. later between the Middle and Late Ordovician, when the average ichnofabric index increased from 3.1 to 4.5."1515 An average of 4.5 means the average metre of Upper Ordovician inner-shelf carbonate has lost 40% to 100% of its bedding to animals. And "From the Middle to the Late Ordovician, in carbonate inner shelf strata, the percentage of totally reworked beds increased by nearly an order of magnitude."15
Two details in these papers help the young-earth reading and are printed here for that reason. The burrowing is shallow: "Throughout the remaining 65 m.y. of Cambrian time bioturbation increased, although depth of bioturbation remained relatively constant at less than 6 cm."6 Middle Cambrian burrows "averaged 2-3 cm; the maximum depth was 5 cm."6 Depth stays "consistently less than 6 cm through the Middle Ordovician," reaching "as much as 30 cm" only in the Late Ordovician.15 A Flood model only has to rework a thin skin at each colonisation. And the authors consider a rival reading of their own trend: "This increase in occurrence of more extensively bioturbated beds through the Cambrian could simply be the result of a constant rate of bioturbation coupled with a systematic decrease in sediment accumulation rate."6 They reject it on lithofacies grounds, but they raise it, and it is the right kind of objection.
The Mesozoic reverses the picture
Tarhan and colleagues describe the Cretaceous shelf in terms that no Flood-year model can absorb: "throughout the Cretaceous, the majority of offshore and shelf sediments were completely homogenized by biogenic mixing … even in comparatively high-energy shallow marine settings, rates of bioturbation commonly outpaced rates of sediment accumulation."1 Also: "Cretaceous chalks deposited in epicontinental settings are commonly completely bioturbated," and "Primary sedimentary structures are relatively rare in Cretaceous and Cenozoic shallow marine deposits."11 In 48 deep-sea cores of Cenozoic age, "rates of bioturbation appear to have, under most circumstances, outpaced sediment accumulation rates."1
Depth rises with extent. Deep-tier transition layers make up 34.1% of the Palaeozoic sample, 37.1% of the Triassic, 57.1% of the Jurassic and 65.9% of the Cretaceous, and median maximum burrow depth climbs from 8.0 centimetres in the Triassic to 17.6 in the Jurassic, with a Cretaceous 75th percentile of 40 centimetres.1
This is where the young-earth position takes its real damage, and the reason is stratigraphic. Most young-earth models put the Flood boundary in the late Mesozoic or the Cenozoic, so the Cretaceous chalks and shelf carbonates fall inside the Flood year. The Chalk itself is treated in Chalk, Limestone, and the Flood.
The Grand Canyon, where a Flood model has to move fastest
The Tonto Group is the first thick pile most young-earth models deposit. The published ichnology, compiled by Anne Miller and colleagues for the National Park Service, records burrowing in all three formations. In the Tapeats Sandstone, Hagadorn and others "reported the abundance of Arenicolites in the Tapeats Sandstone creating highly bioturbated beds at outcrops within eastern and western GRCA."1616 Diplocraterion is common there too and carries spreiten, which "indicates adjusting behavior to maintain a connection with the changing sediment-water interface."16 A spreite records an animal re-cutting its burrow to keep pace with sediment arriving in small increments, with living time between them.
In the Bright Angel Shale "21 ichnogenera have been reported and classified into 15 architectural designs," a deposit-feeder assemblage assigned to the Cruziana Ichnofacies, "typical of shallow-marine settings with moderate to low energy," where "Low rates of sedimentation and erosion favor the preservation of locomotion traces."1616 The primary behind that count describes the formation the same way. Christopher Baldwin and colleagues: "The Middle Cambrian Bright Angel Shale in the eastern Grand Canyon contains a depauperate normal marine fauna, but trace fossils and palynomorphs are abundant throughout the formation."1717 Their reading of those traces is a steady estuarine setting, not one burial event: "Initial correspondence between organic matter content in mudstones and feeding type and intensity (as indicated by traces) is consistent with an estuarine setting for this deposit."17 Only their abstract could be obtained. In the Muav Limestone, "bioturbation is extremely common within calcareous-dominated sediment and is responsible for the mottled appearance."16 The rock's texture is burrowing.
One honest gap: no continuous ichnofabric log of the Tapeats, Bright Angel or Muav was found for this article. The descriptions above are qualitative, and no percentage should be attached to Tonto Group bioturbation until somebody logs it.
The cleanest single test in the literature
Zhang and colleagues logged 34, 53 and 28 metres of the lower Cambrian Zhushadong Formation at three sections in North China. The beds are storm beds, laid down fast, which is the depositional style a Flood model wants. What sits on top of them is the problem: "Maximum penetration of individual burrow shafts is 3.1 cm, but bioturbated zones are amalgamated forming up to 170 cm thick bioturbated intervals. Also, some of the shafts connect burrow systems formed at different depths, indicating that these are multi-layer colonizers able to penetrate more than one event bed. In these cases, maximum burrow depth is 32.4 cm. Beds were most likely deposited by discrete storm events. Thalassinoides records post-storm colonization and intense bioturbation has locally obliterated bedding boundaries, resulting in the amalgamation of bioturbated zones."10
A 170 centimetre interval assembled from 3.1 centimetre increments is about 55 separate colonisations of the same patch of seafloor, each following a separate storm bed. That is the pattern a Flood year has to compress, and it is not one bed worked once.
The mainstream disagrees with itself here, and the disagreement is worth stating. Zhang and colleagues find deep-tier burrowing in the lower Cambrian of North China; Tarhan and colleagues find lower Cambrian fabrics mostly at ii 1 to 2. Neither position is anywhere near a Flood year. The dispute is whether early Cambrian seafloors were churned to 3 centimetres or to 30, over intervals both sides measure in millions of years.
Part 3: How fast burrowers really rework sediment
A single animal digging is not a bed being reworked
Snelling's rate case runs to eleven numbered notes, and only two of them measure a community rather than an animal. The rest are single-animal burial times: he lists "annelid worms, numerous kinds of bivalves, certain razor clams, a pelecypod, several different kinds of gastropods, many crustaceans, and various crabs," each with its own citation.4 Woodmorappe's list is the same kind. A clam burying itself in seconds says nothing about how long a square metre of seafloor takes to lose its bedding. That depends on how many animals there are, how much each moves per hour, and how deep they work.
Snelling's fifth citation is a population-scale study, and it does not report what he takes from it. He writes that "certain urchins are known to rework the upper 5 cm of sediment in three days," citing Lohrer and colleagues 2005.4 That paper is a probabilistic computer model of the heart urchin Echinocardium australe at six shallow subtidal sites in northern New Zealand. Its third parameter, urchin movement rate, was obtained "from one time and place only (Site OB5)," and OB5 "had the highest sediment reworking rate of all sites," so the authors offer the output as "a good upper bound estimate."1818 The three-day figure is that upper bound: "The volume of sediment displaced by Echinocardium populations reached 20,000 cm³ m⁻² d⁻¹ at OB5, suggesting that surface sediment is reworked about every 3 days at sites where Echinocardium is abundant."18 The same abstract carries a result the creationist versions drop: "Experimental work with a fluorescent tracer at OB5 suggested limited downward particle movement as a result of Echinocardium bioturbation."18 A dense urchin herd furrowing the sediment surface is not the same thing as destroying bedding at depth. No "5 cm" figure appears anywhere in the abstract or in the published section snippets; the full text is paywalled and was not obtained, so where Snelling's depth came from is unknown.
Gingras and colleagues did that scaling in 2008, collecting bivalves, arthropods and echinoderms from the Ogeechee estuary in Georgia and X-raying them through the walls of thin aquaria. Froede, summarising their methods for a creationist audience, records that the tanks were "filled with alternating layers of sand and heavy minerals with each layer being approximately 5 to 10 mm thick" and imaged "at 1, 6, 24, 72 and 144 hour intervals."3 The abstract reports the result: "Burrowing rates ranged between 0.01 and 0.15 cm³/h for suspension-feeding animals. Deposit-feeding animals moved between 1 and 10 cm³ of sand per hour, approximately 10 to 100 times more sediment than the suspension feeders moved over similar times. Neoichnological experiments show that ten filter-feeding individuals could take as long as 115 yr to churn a 1 m² plot of sediment, by indexing the measured burrowing rates to realistic animal population densities. Ten such mobile deposit feeders as irregular echinoderms could bioturbate the same sediment in just 42 days. Under the maximum population densities modeled, the animals could bioturbate the sediment plot in 61 min."8
Three answers for one plot: 115 years, 42 days, 61 minutes. The difference is not the biology of digging but how many animals are assumed and what they eat. The full text could not be obtained; everything here is from the abstract, verified by two routes that agree word for word.
The authors' own translation to the rock record is the part the creationist literature leaves alone: "highly burrowed examples of the Skolithos Ichnofacies reflect high population densities and at least seasonal time spans. Highly burrowed examples of the Cruziana Ichnofacies may represent moderate population densities and short time spans."8 Skolithos piperock is exactly what the Tapeats Sandstone carries. A Flood year cannot supply a season of high population density at every horizon that shows one.
The one community-scale measurement, read in full
Grimm and Föllmi published the only community-scale reworking calculation the creationist literature uses. Their subject is the Oligo-Miocene San Gregorio Formation of Baja California Sur: laminated, organic-rich, anaerobic basin mud containing 41 isolated horizons of Thalassinoides and Gyrolithes burrows, each tied to a phosphatic turbidite.7 Their thesis is in the title, "Doomed pioneers": the burrowers were carried in by the turbidity currents, dug in an anoxic basin that could not support breeding, and died.
For one 12 centimetre bed they measured burrow volume on serial slabs, 67 plus or minus 2% over 250 counts, and divided the resulting 80,400 cubic centimetres by several published density and rate combinations. The result is a range: "Estimated durations range from 15.5 to 4020 hours (~1 day to 24 weeks). Of course, these values provide only the loosest constraints upon the duration of the burrowing interval for this bed. However, it is clear that extensively bioturbated horizons do not necessarily require protracted intervals of time for their development."7
The fast end is flagged by its own authors: "calculated duration = 80,400 cm³/(58 cm³/hour/hole x 89 holes/m²) = 15.5 hours (this method yielded the shortest estimated duration)."7 A second published estimate for the same bed, using a measured population reworking rate rather than a per-hole rate, comes out at 1,073 hours, about 45 days.7 And their conclusion is about density, not speed: "it seems reasonable to conjecture that some extensively bioturbated horizons may record an unusually high density of redeposited tracemakers which inhabited the substrate, rather than an extended interval of bioturbation."7
The two rates the creationist literature uses disagree with each other
Gingras measured deposit feeders at 1 to 10 cubic centimetres per hour. The callianassid figure behind Grimm and Föllmi's 15.5-hour minimum is 58 cubic centimetres per hour per entry hole, six times faster than any animal Gingras measured. Both cannot be typical, and any argument that prints one point value misrepresents the state of measurement.
Part 4: The number the young-earth case rests on, and where it came from
A chain of three documents
Snelling's chapter on bioturbation gives one community-scale rate, and it is the only one in the young-earth literature: "Indeed, depending primarily upon the density of fast-burrowing organisms such as callianassid shrimp, a 12-cm-thick layer of sediment can be 67 percent bioturbated in as little as 5.5 hours."4
His source is Woodmorappe's 2006 paper, which prints the same sentence with a different number: "Moreover, depending primarily upon the density of fast-burrowing organisms such as callianassid shrimp, a 12-cm thick layer of sediment can be 67% bioturbated (ichnofabric index of ~5, figure 1) in as little as 15.5 hours".2
Woodmorappe's source is Grimm and Föllmi, who print 15.5 hours as the shortest of an ensemble running to 4,020 hours. So Snelling's figure is nearly three times too fast against his own chain of custody. That is a transcription slip, not dishonesty, and it should be read as one. Both men reproduce the authors' sentence about extensively bioturbated horizons not necessarily requiring protracted intervals. Neither reproduces the sentence immediately before it, which gives the range.
The omission is the substantive defect, not the digit. A Flood-year timetable can absorb a day. It cannot absorb 24 weeks at even a few horizons. The two worked examples the paper prints in full come out at 15.5 hours and 1,073 hours, and 15.5 is the one the creationist literature carries.
The setting is the opposite of the one the argument needs
The San Gregorio beds are isolated burrowed horizons in otherwise laminated anoxic mud, made by animals transported in that could not reproduce. That is the pattern a Flood model predicts: rare, thin, event-driven burrowing between undisturbed layers. Using this paper to explain a formation burrowed continuously through hundreds of metres inverts what it shows. A turbidite dumping an unusual density of animals cannot be invoked for a whole shelf logged at ii 3 to 5 for a kilometre of section.
The arithmetic nobody on the young-earth side has run
Woodmorappe supplies the time budget himself, in note 103: "As an upper limit of episodicity, assume one year (8,766 hours) of overall deposition with active sedimentation occurring half of this time. Theoretically speaking, there was time available for the construction of 4,383 superimposed 1-hour bioturbating events or 52,596 superimposed 5-minute bioturbating events. Of course, the foregoing example is extreme; intentionally so for the purpose of illustration."2
Take the extreme case at face value and put his own rate into it. A one-hour event does not produce an ichnofabric index of 5; by the figure Woodmorappe himself cites, that takes 15.5 hours. So 4,383 quiet hours divided by 15.5 hours per surface gives 283 surfaces, and at 12 centimetres each that is about 34 metres of heavily reworked rock for the whole Flood, on the whole planet. The calculation is this article's, run on Woodmorappe's stated inputs; he does not perform it. At the other published estimates for the same bed the budget buys 4 surfaces, roughly half a metre, or at the slowest, one.
Against that, set the thicknesses in the literature. The Cambrian survey Woodmorappe points his readers to logged 1,151 metres, most of it at ii 3 or above.2 One lower Cambrian formation in North China has a single amalgamated interval 170 centimetres thick built from 3.1 centimetre increments.10 The Cretaceous shelf is homogenised over most of its area.1
A second route gives the same order of answer. The mixed layer is about 10 centimetres worldwide and Cambrian mixing depth was 2 to 6 centimetres, so a thoroughly reworked column is a stack of thin slices, each of which had to be the seafloor separately.96 Divide a thick homogenised formation by its own measured burrow depth and the required seafloors run into the thousands. Spread over 371 days, that leaves a few hours each, at or below the fastest rate anyone has measured.
No young-earth publication does this arithmetic for a named formation. That is the largest single hole in the position, and it is a hole that could be filled with a spreadsheet and a published ichnofabric log.
Part 5: Where creationist authors have conceded the point
Concessions inside the argument
Woodmorappe's paper is the most careful young-earth treatment of the subject, and it concedes more than any critic has extracted from the outside. He states the difficulty: "Very thick sedimentary lithologies that have been extensively bioturbated present more of a challenge to a Flood model, even if they occur at or near the top of the local lithostratigraphic column. Thick sequences of sedimentary rock, characterized by high ichnofabric indices, and occurring in undoubted superposition, may have had insufficient time during the Flood for them to be explained by one-horizon-at-a-time bioturbation."2
His escape is the PPLC hypothesis, short for promptly-precipitated lithified crust. Thin cemented crusts form above buried animals, shield them from the overburden, and let several horizons be worked at once, giving "a thick but cryptically composite, highly bioturbed interval."2 He also suggests thick bioturbated sequences "may be at least partly illusory" because such horizons are often discontinuous.2 And he ends honestly: "The efficacy of the PPLC hypothesis requires experimental validation."2 Twenty years on, no such experiment was found for this article, in the creationist journals or outside them.
John Whitmore and Paul Garner, setting out criteria for recognising Flood strata, rank bioturbation as their weakest indicator, a 3 on a scale where 1 is diagnostic: "we would expect extensively bioturbated horizons, with the resultant disruption of internal stratification and sedimentary structures, to be less common in Flood-deposited sediments. Before and after the Flood, as more time became available between depositional events, we would expect bioturbation to become much more abundant."1919 Half of that prediction succeeds. Bioturbation really does increase up the column, from a mean index of 1.02 in the pre-trilobite Cambrian to 4.5 in the Upper Ordovician, with deep tiers rising from a third of Palaeozoic samples to two thirds of Cretaceous ones. It fails on where the increase happens: the most homogenised rocks are Cretaceous and Cenozoic, and those lie inside the Flood on the models that make the prediction.
Kurt Wise uses bioturbation as a mainstream sedimentologist would. Testing whether a fossil forest grew where it is found, he writes that "the sediment substrates of modern communities are heavily bioturbated, usually completely obliterating original bedding. In contrast, the Flood usually involved a sediment production rate that was too high to permit extensive infaunal bioturbation," so an in-place assemblage "should display much more substrate bioturbation than will be displayed in allochthonous assemblages."2020 He rules Fossil Grove transported because its laminae survive.20 The method is sound. Applied consistently, a thoroughly bioturbated Cretaceous chalk or Ordovician inner shelf is an in-place community by Wise's own criterion, and those rocks are Flood deposits on his own stratigraphy.
Three published statements that the answers fail
Carl Froede Jr. reviewed the Gingras aquarium results for a creationist audience in 2009 and reported the awkward part first. Some diluvialists expect little bioturbation because deposition was fast, others expect the record to alternate between intensely burrowed and unburrowed intervals: "However, neither perspective is consistent with the actual rock record."3 Of a Skolithos horizon in the Meridian Sand at Campbell Mountain, Alabama, he wrote: "Conditions were optimum for trace maker activity and the amount of time necessary to create these traces could be measured in months, not years or decades."3 Months, inside a year that also has to deposit the Phanerozoic.
Chad Arment, in Answers Research Journal in 2023, argued that Palaeocastor helical burrows in the Miocene Arikaree Group mark post-Flood strata, and rejected the standard young-earth alternative by name. Michael Oard had written that such structures "represent animal activity during the Flood," made on "briefly exposed diluvial sediments."2121 Arment answers: "Could Palaeocastor burrows have been formed during the Flood? The amount of time necessary for burrow formation, then plant growth and burrow infiltration, then fossilization, at multiple vertical levels, clearly disconfirms this as a possibility."11 And directly: "Clearly, extensive plant growth, episodic and vertically staggered burrow formation, and a large terrestrial beaver population demonstrate that this phenomenon didn't 'briefly' occur during the Flood."11 The root infiltration in that argument is the same evidence treated in Buried Soils.
Froede, Jerry Akridge and John Reed attacked Tim Clarey's megasequence model in 2022 using the same logic. Genesis has land life dead by Day 150, so tracks made by living animals should stop there. They do not: "They are found well past the megasequence-defined Day 150 termination of all terrestrial life, as conveyed by Scripture."12 Their premise is that traces cannot be moved: footprints "must be formed in situ."12 The megasequence framework they are attacking is described in Megasequences; the vertebrate trackways themselves belong to The Coconino Sandstone.
An unresolved contradiction inside the movement
Woodmorappe's mechanism requires that burrowers were transported to where their traces are found. Three other young-earth authors deny that traces can be transported at all. Riley Isaacs writes that "ichnofossils are primarily autochthonous and only rarely transported."2222 Arment writes that burrows "by definition are non-transportable" and "Fossilization had to have occurred in place."11 Froede, Akridge and Reed say tracks "must be formed in situ."12 Nothing found for this article adjudicates the disagreement, and the three in-place positions remove the mechanism the fourth depends on.
Snelling's other answer, that hardgrounds were cut, cemented, encrusted by oysters and re-eroded "within a few hours" by tidal surges, has the same shape: a rate is asserted for the cementation and none for the encrusting animals' growth.4 Hardground borings are covered in Flat Gaps.
Objections and responses
"Most of the column is unbioturbated, so the Flood is fine." Partly true, and the best version comes from mainstream work: 86% of a 430 metre Devonian section in Algeria, a Frasnian mean index of 2.0, lower Cambrian fabrics mostly at ii 1 or 2. It fails as a generalisation. The same compilation describes Cretaceous offshore and shelf sediments as completely homogenised, with reworking outpacing deposition, and on the young-earth models that put the Flood boundary in the late Mesozoic or the Cenozoic, which is most of them, those rocks are Flood deposits. A model does not survive by fitting the quiet stretches.
"Burrows form in hours, so bioturbation is no clock." Individual burrows do, and Bromley's textbook says pioneers colonise a fresh storm bed quickly. The clock is not one burrow. It is the number of times a surface has to be colonised, worked and buried to build a thick reworked interval, times the length of each cycle. The one community-scale measurement in the creationist literature gives 15.5 to 4,020 hours for one 12 centimetre bed.
"Animals fleeing the Flood burrowed into briefly exposed sediment." This is Oard's BEDS proposal, and it predicts shallow, single-episode, low-diversity escape structures on bedding planes. It predicts against deep tiers, against burrows re-cut to follow a rising sediment surface, and against high trace-fossil diversity. The Bright Angel Shale has 21 ichnogenera in 15 architectural designs, and the Tapeats has Diplocraterion with spreiten. Arment, a young-earth author, rejects BEDS in print for the case Oard applied it to.
"Ichnofabric depends on oxygen, salinity and food supply, not on time." It depends on all of them, and Bromley says so. That is why a bare laminated bed is weak evidence for speed, and why this article does not argue from unburrowed rock. The argument runs the other way. A thoroughly homogenised bed needs animals, oxygen, food and time, and removing any of the first three explains an absence of bioturbation, not a presence of it.
"Woodmorappe's cemented crusts let several tiers be worked at once, so the surfaces need not be counted one at a time." It is the best idea the movement has produced here, and it is untested. Its author wrote that it "requires experimental validation," and twenty years later none was found for this article. The pass condition is clear: show that an early carbonate crust of achievable thickness deflects enough overburden for an animal beneath it to keep working, and that the resulting fabric can be told apart from stacked colonisation.
"This was settled by Droser and Bottjer in the 1980s, so why revisit it." Because the mainstream position has moved, and it has moved towards the young-earth observation. The 2025 compilation by Tarhan and co-authors, which includes Droser and Bottjer, reports large parts of the Palaeozoic as lightly mixed and shallowly burrowed, and states plainly where its own data are thin: "with limited exception (e.g., the lower Paleozoic, the Permian–Triassic transition, and recent intervals of the Cenozoic), the data necessary to robustly quantify mixed layer depths are sparse to nonexistent."1 Anyone citing the 1980s alone is citing an argument the field has since qualified.
"Ichnofabric index counts are subjective field estimates, not measurements." Fair as far as it goes. The scale was calibrated by planimeter but is applied by eye against printed cards, and its authors warn that cards drawn for one lithology do not transfer to another. The disagreement here is not about a band or two. It is between "the majority of the total thickness has an ichnofabric index of 3 or greater" and "there is so little bioturbation of sedimentary strata in the geologic record."
Issues and unanswered questions
- Five sources were not obtained in full. Taylor and Goldring 1993, the origin of the bioturbation index, is closed everywhere tried, so its scale is quoted only as reproduced by Zhang and colleagues. The Ekdale, Bromley and Pemberton 1984 short course is not online. Gingras and colleagues 2008 is closed, so only its abstract is used. Lohrer and colleagues 2005 is closed too; its abstract and Elsevier's published section snippets were obtained, and they are enough to show that Snelling's version of it overstates a modelled upper bound, but the full text and the origin of his "5 cm" are still out of reach; see quarantine. Baldwin and colleagues 2004 on Bright Angel ichnoguilds and Hagadorn and colleagues 2011 on Tapeats Arenicolites yielded abstracts only, and neither abstract carries an ichnofabric or bioturbation index; Raisanen and Hasiotis 2018 on Morrison Formation burrows was not chased.
- No continuous ichnofabric log of the Tonto Group appears to exist. The Grand Canyon evidence here is qualitative. Somebody should log the Tapeats, Bright Angel and Muav the way Droser and Bottjer logged the Great Basin.
- Brand and Chadwick's survey has never been published with numbers. The book describes it and gives no percentages. If a CRSQ, Origins, ICC or GSA version exists, it would materially change what this article can say.
- The colonisation-surface count has not been done by anyone, on either side. The inputs exist: published ichnofabric logs, measured burrow depths, and a measured range of reworking times. Producing the full grid rather than a point estimate would settle more than another round of quotations.
- The disagreement between Zhang and colleagues and Tarhan and colleagues about early Cambrian burrow depth is live and unresolved.
Verdict
Bioturbation is a real clock, and the young-earth literature agrees that it is. Snelling says burrowed layers record "at least a few hours." The dispute is only over how many hours, at how many levels.
The young-earth answer works for the rocks it was built on. Large parts of the lower Palaeozoic are lightly and shallowly burrowed, and the best evidence for that is mainstream and recent. The answer fails for the Mesozoic, where shelf sediments are homogenised through their thickness and mixing outpaced deposition, and those rocks fall inside the Flood year on the young-earth side's own stratigraphy.
The rate literature does not close the gap. The single community-scale measurement in circulation is the fast end of a range reaching 24 weeks, taken from isolated burrowed horizons in laminated mud, which is the opposite of the setting needing explanation. Run it through the movement's own time budget and it yields about 34 metres of heavily reworked rock for the entire Flood.
And the sharpest objections are already in print, in creationist journals, from Froede, Arment, and Froede with Akridge and Reed. Nobody has answered them.
Sources
- 1.
Tarhan, Lidya G. et al. “Tracking bioturbation through time: The evolution of the marine sedimentary mixed and transition layers.” Science Advances 11(31):eadu7719. Jul 30, 2025. A 2025 compilation of published measurements of how deep animals mix seafloor sediment (the mixed layer) and how far their burrows reach below it (the transition layer), across the Phanerozoic. It grades burrowing with the ichnofabric index (ii), where ii 1 means undisrupted layering and higher numbers mean more burrowing; it finds that lower Cambrian strata rarely exceed ii 3 and that Cretaceous shelf sediments were completely homogenised. The article leads with it because the mainstream literature reports, in parts of the Palaeozoic, the sparse burrowing that the Flood side predicts. ↩
- 1a.
On a Lochkovian to Emsian succession in the Reggane Basin, Algeria: “86% of strata in this 430-m succession are unbioturbated; 7% are characterized by BI 2, 7% by BI 4, and <1% by BI 5.” ↩ ↩ ↩
- 1b.
On Frasnian carbonates of the Great Basin and Rocky Mountains: “a mean ii of 2.0”. intensely bioturbated intervals. “account for less than 30% of measured strata”. and. “beds that are vertically mixed rarely exceed 10 cm in thickness.” ↩ ↩
- 1c.
“lower Cambrian heterolithic siliciclastic and carbonate strata only rarely exceed ii 3 and are most commonly characterized by ii 1 or 2.” ↩ ↩
- 1d.
Mixed-layer depth increased across the early Palaeozoic. “from approximately 0.2 to 1.5 cm in heterolithic siliciclastic settings.” Mean lower Cambrian sandstone tempestite thickness (a bed laid down by a storm) is 1.3 cm, preserved because burrowers could not blend across bed junctions. ↩
- 1e.
The modern reference state: the mixed layer. “extends downward from the sediment-water interface to, on average, nearly 10 cm depth in the seafloor, and an underlying transition layer composed of discrete and actively occupied deep burrows that may, in certain settings, extend to >1 m deep.” ↩
- 1f.
“throughout the Cretaceous, the majority of offshore and shelf sediments were completely homogenized by biogenic mixing … even in comparatively high-energy shallow marine settings, rates of bioturbation commonly outpaced rates of sediment accumulation.” ↩ ↩
- 1g.
“Cretaceous chalks deposited in epicontinental settings are commonly completely bioturbated.” ↩
- 1h.
“Primary sedimentary structures are relatively rare in Cretaceous and Cenozoic shallow marine deposits.” ↩
- 1i.
From 48 deep-sea cores: “rates of bioturbation appear to have, under most circumstances, outpaced sediment accumulation rates.” ↩
- 1j.
Proportion of transition layers reaching deep infaunal tiering levels: 34.1% Palaeozoic, 37.1% Triassic, 57.1% Jurassic, 65.9% Cretaceous. Median maximum uncorrected burrow depth: 8.0 cm Triassic, 17.6 cm Jurassic, 15.0 cm Cretaceous, with a Cretaceous 75th percentile of 40.0 cm. For the lower Palaeozoic, “41.0% of Cambrian and Ordovician transition layers reach deep infaunal tiering levels,”. and the median maximum burrow depth is 7.6 cm. ↩
- 1k.
The authors' own statement of their data's limits: “with limited exception (e.g., the lower Paleozoic, the Permian–Triassic transition, and recent intervals of the Cenozoic), the data necessary to robustly quantify mixed layer depths are sparse to nonexistent.” They also state that the dataset is geographically skewed to Asia, Europe and North America. ↩
- 1a.
- 2.
Woodmorappe, John. “Are soft-sediment trace fossils (ichnofossils) a time problem for the Flood?” Journal of Creation 20(2):113–122. 2006. A young-earth paper by John Woodmorappe, who supports the Flood as the source of most sedimentary rock, asking whether burrows made in soft sediment (trace fossils, or ichnofossils) could form during it. He proposes a hypothetical mechanism in which layers harden soon after they are laid down, protecting burrowing animals below from being immobilized by the weight of the sediment above, so that several layers can be churned at once. The article uses it for the author's own admission that most of 1,151 metres of mostly Cambrian strata in the western USA are heavily burrowed, and for his time budget for the Flood. ↩
- 2a.
Page 116: “Moreover, depending primarily upon the density of fast-burrowing organisms such as callianassid shrimp, a 12-cm thick layer of sediment can be 67% bioturbated (ichnofabric index of ~5, figure 1) in as little as 15.5 hours”. ↩ ↩
- 2b.
Page 119: “Attention is directed to the ichnofabric indices comprising 48 Cambrian stratigraphic sections and 1,151 total metres of sedimentary strata in the western USA, which also includes some Ordovician strata. Only a small fraction of the total thickness has an ichnofabric index of 1, while the majority of the total thickness has an ichnofabric index of 3 or greater.” ↩ ↩ ↩
- 2c.
Page 119: “Very thick sedimentary lithologies that have been extensively bioturbated present more of a challenge to a Flood model, even if they occur at or near the top of the local lithostratigraphic column. Thick sequences of sedimentary rock, characterized by high ichnofabric indices, and occurring in undoubted superposition, may have had insufficient time during the Flood for them to be explained by one-horizon-at-a-time bioturbation.” ↩
- 2d.
Page 119: On the promptly-precipitated lithified crust proposal. “The end result is a thick but cryptically composite, highly bioturbed interval of sediment.” ↩
- 2e.
Page 119: “To the extent that highly-bioturbed horizons are generally discontinuous, the abundance of considerable thicknesses of highly-bioturbed sedimentary rock may be at least partly illusory.” ↩
- 2f.
Page 120: “The efficacy of the PPLC hypothesis requires experimental validation.” ↩
- 2g.
Page 122: Woodmorappe's note 103. “As an upper limit of episodicity, assume one year (8,766 hours) of overall deposition with active sedimentation occurring half of this time. Theoretically speaking, there was time available for the construction of 4,383 superimposed 1-hour bioturbating events or 52,596 superimposed 5-minute bioturbating events. Of course, the foregoing example is extreme; intentionally so for the purpose of illustration.” The 283-surface and 34-metre figures in the body are this article's arithmetic on these inputs and his own cited 15.5 hours per surface. Woodmorappe does not run the calculation. ↩ ↩
- 2a.
- 3.
Froede Jr., Carl R. “Sediment bioturbation experiments and the actual rock record.” Journal of Creation 23(3):3–5. Dec 2009. A short 2009 article in the young-earth Journal of Creation in which Carl Froede reviews a laboratory study by Gingras and colleagues. That study put clams, shrimp and crabs, and sea urchins and brittle stars from an estuary in Georgia into aquaria of layered sand, and measured how fast they churned it. The article uses it because Froede admits that neither the uniformitarian nor the diluvial (Flood-based) prediction matches the rock record. ↩
- 3a.
“some diluvialists have predicted that we should expect little sediment bioturbation due to the high-energy conditions associated with the Genesis Flood. Within this diluvial interpretation it could be postulated that the rapid deposition of sediments, one atop another, would leave little time for trace makers to move in and stir them. However, neither perspective is consistent with the actual rock record.” The other perspective he rejects: “the vertical rock record should exhibit layers of intense bioturbation interrupted by nonbioturbated sedimentary events followed by intense bioturbation. However, this is not typically found in the actual rock record.” ↩ ↩ ↩
- 3b.
Section 1: On the Gingras experiment, citing Gingras et al., ref. 2. “They were placed into glass aquaria filled with alternating layers of sand and heavy minerals with each layer being approximately 5 to 10 mm thick. Examination of the rate of bioturbation occurred at 1, 6, 24, 72 and 144 hour intervals by collecting X-ray images of the aquaria sidewalls.” ↩
- 3c.
Figure 3: The caption, on Skolithos (vertical burrows) in the Meridian Sand at Campbell Mountain, Alabama. “Conditions were optimum for trace maker activity and the amount of time necessary to create these traces could be measured in months, not years or decades. Sediment deposition during this portion of the Flood was low enough to allow the bioturbation of the sediments and the destruction of any preexisting sedimentary fabric.” ↩ ↩
- 3a.
- 4.
Snelling, Andrew A. Earth's Catastrophic Past: Geology, Creation & the Flood. Institute for Creation Research, Dallas. 2009. A young-earth book on geology, creation and the Flood, in 2 vols. The article cites its chapter 92, pages 739–740, and chapter 114, pages 917–923. The article calls it the fullest young-earth treatment of the subject. ↩
- 4a.
Page 917: “Because bioturbation requires the passage of time, the degree of bioturbation found preserved in sedimentary strata at numerous levels in the rock record would likewise presumably testify to the passage of perhaps significant amounts of time between the successive deposition of those strata.” 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.” ↩
- 4b.
Page 740: “the fact that there is so little bioturbation of sedimentary strata in the geologic record, and that it is only some strata surfaces that have burrows, tracks, and marks on and in them, is evidence for rapid deposition of the strata within a timeframe consistent with the global Flood catastrophe.” ↩
- 4c.
Page 919: “Indeed, depending primarily upon the density of fast-burrowing organisms such as callianassid shrimp, a 12-cm-thick layer of sediment can be 67 percent bioturbated in as little as 5.5 hours.” The figure his own cited source gives is 15.5 hours. Read as a transcription slip; the substantive defect is the omitted upper bound of the range, which both he and Woodmorappe leave out. ↩ ↩
- 4d.
Page 918: “Extensive bioturbation of individual sedimentary layers can happen rapidly. For example, certain urchins are known to rework the upper 5 cm of sediment in three days.” His note 5 is. “A. N. Lohrer and others, 2005, Rapid reworking of subtidal sediments by burrowing spatangoid urchins, Journal of Experimental Marine Biology and Ecology, 321: 155-169.” The first initial is a slip; the author is A. M. Lohrer. ↩
- 4e.
Pages 918–920: notes 5 to 15. Note 5 is Lohrer and others 2005 and note 7 is Grimm & Föllmi 1994; those two are the only community-scale sources in the list. Note 6 is Howard & Elders 1970, Kranz 1974 and Stanley 1970. Notes 9 to 15 support the sentence. “Among the many such organisms, for which such burrowing rates have been measured, are annelid worms, numerous kinds of bivalves, certain razor clams, a pelecypod, several different kinds of gastropods, many crustaceans, and various crabs,”. and every one of them reports how fast an individual animal buries itself. ↩
- 4f.
Page 921: “As soon as the carbonate sediments were deposited, organisms began to scurry across, and burrow into, their surfaces. However, hardening of the carbonate cement in the sediments would have been rapid at the same time, thus fossilizing the burrows and trails, while oysters attached themselves to these hardened surfaces. Nevertheless, within a few hours, these now hardened sediment surfaces, or hardgrounds, would have been eroded by the next tidal surges of sediment-laden waters.” ↩
- 4a.
- 5.
Bromley, Richard G. Trace Fossils: Biology and Taphonomy. London: Unwin Hyman. 1st edition. 1990. A 280-page book on trace fossils, the burrows and tracks that animals leave in rock, and on how they came to be preserved. The article uses it for the standard account of why a bed may lack burrows, why rapid burial may stop communities from maturing, and why the deepest burrows are the ones usually preserved. ↩
- 5a.
Page 202, section Incomplete bioturbation: “This implies a stress factor that has prevented the completion of the work of the endobenthic community … Clearly, however, other stress factors may inhibit the complete bioturbation of the substrate. In particular, fluctuation in salinity may severely reduce the biological diversity of a fauna … Another important limiting factor is the availability of oxygen.” ↩ ↩
- 5b.
Page 190: “Deepest structures are the most complete. Only their upper parts are cross-cut by shallower structures. Activity within each tier cross-cuts structures produced in shallower tiers and tends to obliterate them.” ↩
- 5c.
Pages 204–205: Opportunists. “are the pioneers that speedily colonize a habitat after a major and abrupt environmental change (e.g. storm deposition)”. producing ichnocoenoses of. “a low ichnodiversity and high density”. in which. “the pioneer species are small worms that produce vertical domichnia equivalent to Skolithos”. Equilibrium species. “are slow to enter new environments … typically members of high diversity, persistent, climax communities”. Page 218: On rapid deposition: “Rapid rate of sedimentation may also prevent the maturing of communities, deep tiers may not be occupied, and the Zoophycos–Chondrites ichnoguild is generally not represented.” ↩
- 5d.
Page 204, figure 11.14 series: Where erosion cuts below the bioturbated top of a bed, “no bioturbation is preserved, but it would be unwise to assume that the depositional environment was devoid of life.” ↩
- 5a.
- 6.
Droser, Mary L., and David J. Bottjer. “Trends in depth and extent of bioturbation in Cambrian carbonate marine environments, western United States.” Geology 16(3):233–236. Mar 1988. A 1988 paper in which the authors logged Cambrian carbonate rock sections in the western United States, rated each one on the ichnofabric index and measured how deep the burrows went. Burrowing grew more extensive through the Cambrian while the burrows stayed less than about 6 centimetres deep. The article uses it as the field record behind a creationist author's own cited figures and as the source of the shallow Cambrian burrow depths. ↩
- 6a.
Page 233, section Abstract: “Throughout the remaining 65 m.y. of Cambrian time bioturbation increased, although depth of bioturbation remained relatively constant at less than 6 cm.” ↩
- 6b.
Page 234: “A total of 810 m of ichnofabric index data were collected from 34 Cambrian stratigraphic sections (Fig. 2) interpreted to have been deposited in an inner-shelf environment. The most commonly recorded ichnofabric indices were 3, 4, and 5 (Fig. 1).” ↩ ↩
- 6c.
Page 235: “A total of 341 m of ichnofabric index data were collected from 14 Cambrian sections (Fig. 2) interpreted to have been deposited in a middle-shelf environment. The most common ichnofabric indices recorded were 2 and 3.” 810 plus 341 metres, across 34 plus 14 sections, is the "1,151 total metres" and "48 Cambrian stratigraphic sections" that Woodmorappe 2006 p. 119 cites. ↩ ↩
- 6d.
Page 234: “Stratigraphic sections were logged for depositional environments and ichnofabric indices (Fig. 3). This method is analogous to the continuous logging of thicknesses of strata in a section for properties such as rock color or lithology.” ↩
- 6e.
Page 234: “In Middle Cambrian strata the record of sediment disruption is more extensive (Fig. 4), and includes common Thalassinoides maze burrow networks. Depth of bioturbation measured from 22 horizons averaged 2-3 cm; the maximum depth was 5 cm.” Upper Cambrian depths from 35 horizons averaged 2 to 4 cm, maximum about 6 cm. ↩ ↩ ↩
- 6f.
Page 235: “This increase in occurrence of more extensively bioturbated beds through the Cambrian could simply be the result of a constant rate of bioturbation coupled with a systematic decrease in sediment accumulation rate.” The authors raise this alternative and reject it on lithofacies control. ↩
- 6a.
- 7.
Grimm, Kurt A., and Karl B. Föllmi. “Doomed pioneers: Allochthonous crustacean tracemakers in anaerobic basinal strata, Oligo-Miocene San Gregorio Formation, Baja California Sur, Mexico.” Palaios 9(4):313–334. Aug 1994. A 1994 field study of 41 burrowed layers in the San Gregorio Formation of Baja California Sur, Mexico, which is organic-rich mud laid down without oxygen. Each burrowed layer is tied to a deposit left by an underwater sediment flow. The authors found the burrows only in those flow deposits and not in the surrounding mud. The article uses it because the creationist literature takes its burrowing-time calculation from this paper. ↩
- 7a.
Page 313, section Abstract: “Laminated, organic-rich hemipelagic sediments from the Oligo-Miocene San Gregorio Formation, Baja California Sur, Mexico, contain isolated horizons (n = 41) of Thalassinoides and Gyrolithes burrows which are exclusively associated with gravity-flow event deposits (phosphatic turbidites).” ↩
- 7b.
Page 328: “Estimated durations range from 15.5 to 4020 hours (~1 day to 24 weeks). Of course, these values provide only the loosest constraints upon the duration of the burrowing interval for this bed. However, it is clear that extensively bioturbated horizons do not necessarily require protracted intervals of time for their development.” The second and third sentences are the ones Woodmorappe 2006 and Snelling 2009 reproduce. The first is not reproduced in either. ↩ ↩
- 7c.
Page 328, section calculation box: “We measured 89 entry holes/m² in bed; Suchanek and Colin (1986) report reworking rate of 58 cm³/hour per entry hole; calculated duration = 80,400 cm³/(58 cm³/hour/hole x 89 holes/m²) = 15.5 hours (this method yielded the shortest estimated duration).” The 80,400 cm³ comes from. “Total sediment volume = (area) x (thickness); = 100 cm x 100 cm x 12 cm = 120,000 cm³”. multiplied by a burrowed fraction measured. “on serial slabs cut through the bed parallel to bedding (67 ± 2%; n = 250 counts).” ↩ ↩
- 7d.
Page 328: “Suchanek and Colin (1985) report subtidal callianassid populations which rework 3.4 kg/day of wet sediment, wet sediment density = 1.89 g/cm³ (Branch and Pringle, 1987); volumetric burrowing rate = 74.9 cm³/hour; duration = 80,400 cm³/74.9 cm³/hour = 1073 hours.” ↩
- 7e.
Page 328: “it seems reasonable to conjecture that some extensively bioturbated horizons may record an unusually high density of redeposited tracemakers which inhabited the substrate, rather than an extended interval of bioturbation.” ↩
- 7a.
- 8.
Gingras, Murray K. et al. “How fast do marine invertebrates burrow?” Palaeogeography, Palaeoclimatology, Palaeoecology 270(3–4):280–286. 2008. A 2008 laboratory study that X-rayed burrowing animals from the Ogeechee estuary in Georgia through thin-walled aquaria and timed how fast each one moved sediment. Ten filter feeders could take as long as 115 years to churn one square metre at realistic population densities, ten irregular echinoderms 42 days, and the maximum modelled density 61 minutes. The article uses it to show that the fastest figure, 61 minutes, is a maximum-density model rather than a typical rate. ↩
- 8a.
Page 280, section Abstract: “The burrowing of bivalves, arthropods, and echinoderms collected from tidal flats and shallow subtidal sediments of the Ogeechee estuary, Georgia, U.S.A was analyzed using time-elapse, X-ray analysis of thin-walled aquaria. The rate of sediment intrusion was determined for each animal. Burrowing rates ranged between 0.01 and 0.15 cm³/h for suspension-feeding animals. Deposit-feeding animals moved between 1 and 10 cm³ of sand per hour, approximately 10 to 100 times more sediment than the suspension feeders moved over similar times. Neoichnological experiments show that ten filter-feeding individuals could take as long as 115 yr to churn a 1 m² plot of sediment, by indexing the measured burrowing rates to realistic animal population densities. Ten such mobile deposit feeders as irregular echinoderms could bioturbate the same sediment in just 42 days. Under the maximum population densities modeled, the animals could bioturbate the sediment plot in 61 min. Given the reported results, qualitative interpretation of the rock record is possible: highly burrowed examples of the Skolithos Ichnofacies reflect high population densities and at least seasonal time spans. Highly burrowed examples of the Cruziana Ichnofacies may represent moderate population densities and short time spans.” ↩ ↩ ↩ ↩
- 8a.
- 9.
Boudreau, Bernard P. “Is burial velocity a master parameter for bioturbation?” Geochimica et Cosmochimica Acta 58(4):1243–1249. Feb 1994. A paper from February 1994 that asks whether the speed at which sediment is buried controls how deep animals mix it. The mixed layer, measured with marker substances, averages 9.8 centimetres whatever the burial speed, and the depth is limited by the energy cost of digging below 10 to 15 centimetres. The article uses it for the thickness of the mixed layer, the number its argument turns on, and the 9.8-centimetre figure comes from this paper, not the 1998 Limnology and Oceanography note. ↩
- 9a.
Page 1243, section Abstract: “A similar analysis of the tracer-identified surface mixed-depth shows that it is essentially independent of burial velocity with a worldwide mean of 9.8 ± 4.5 cm. Depth of mixing is probably more closely related to the energetic costs of deep burrowing.” Page 1247: “Further statistics on this sample population indicate a mean and median of 9.8 cm with a standard deviation of ±4.5 cm.” ↩ ↩ ↩
- 9b.
Page 1247: “Very likely, the depth of mixing L is limited primarily by the physical difficulty and increasing energy costs of reworking and excavating deeper than 10-15 cm in a sediment medium (JUMARS and WHEATCROFT, 1989).” ↩
- 9c.
Page 1246: “The L values quoted in all the studies in Table 1 cannot represent the maximum depths to which infaunal organisms disturb sediments. Specific organisms are known to burrow to depths of over 1 m … Most of the values in Table 1 are less than 20 cm. Therefore, these quoted mixing depths represent the thickness of some zone that is most frequently mixed.” ↩
- 9a.
- 10.
Zhang, Li-Jun et al. “The impact of deep-tier burrow systems in sediment mixing and ecosystem engineering in early Cambrian carbonate settings.” Scientific Reports 7:45773. Apr 4, 2017. A field study of deep burrows in early Cambrian carbonate rocks in North China, measured in three sections of 34, 53 and 28 metres. The authors suggest that sediment mixing in early Cambrian carbonate seas may have been greater than earlier models assumed. The article uses it for the thickness of the mixed intervals: single burrow shafts reach 3.1 cm, but repeated colonisation builds bioturbated zones up to 170 cm thick. ↩
- 10a.
Section Methods: The index definitions are reproduced by Zhang and colleagues, who attribute them to their reference 19, Taylor & Goldring 1993. BI 0, 0%: “no bioturbation … a pristinely preserved primary fabric.” BI 1, 1–4%: “sparse bioturbation with few discrete biogenic structures locally overprinting the well-preserved sedimentary fabric.” BI 2, 5–30%: “low bioturbation in sediment with well-preserved sedimentary structures.” BI 3, 31–60%: “discrete trace fossils, moderate bioturbation and still distinguishable bedding contacts.” BI 4, 61–90%: “intense bioturbation, high trace-fossil density, common overlap trace fossils, and primary sedimentary structures mostly erased.” BI 5, 91–99%: “intense bioturbation and a completely disturbed bedding.” BI 6, 100%: “completely bioturbated and reworked sediment, revealed by repeated overprinting of trace fossils.” ↩
- 10b.
Section Methods: “The shallow tier is represented by structures emplaced in the upper 6 cm of the substrate, the mid tier comprises those produced within 6–12 cm of the substrate, the deep tier consists of those formed below 12–100 cm, and the ultra-deep tier is represented by those traces emplaced below 100 cm.” ↩
- 10c.
Section Abstract and results: On 34 m at Guankou, 53 m at Lushan and 28 m at Mianchi in the lower Cambrian Zhushadong Formation, North China: “Maximum penetration of individual burrow shafts is 3.1 cm, but bioturbated zones are amalgamated forming up to 170 cm thick bioturbated intervals. Also, some of the shafts connect burrow systems formed at different depths, indicating that these are multi-layer colonizers able to penetrate more than one event bed. In these cases, maximum burrow depth is 32.4 cm. Beds were most likely deposited by discrete storm events. Thalassinoides records post-storm colonization and intense bioturbation has locally obliterated bedding boundaries, resulting in the amalgamation of bioturbated zones.” The figure of about 55 colonisations is this article's arithmetic: 170 cm divided by 3.1 cm. The authors give no colonisation count and no duration for a colonisation window. ↩ ↩ ↩
- 10a.
- 11.
Arment, Chad. “Palaeocastor Burrows as Post-Flood Biostratigraphic Markers.” Answers Research Journal 16:183–187. 2023. A 2023 paper in the young-earth Answers Research Journal by Chad Arment, arguing that the helical burrows of Palaeocastor, a burrowing beaver of the early Miocene Harrison Formation in Nebraska and Wyoming, can mark rocks laid down after the Flood. The burrows survive because grass roots grew into their walls and silicified them, and Arment argues that this took too long to happen during the Flood. The article uses it as the most recent young-earth answer to Oard's claim that such burrows were made during the Flood, and for its claim that they must have been formed in place. ↩
- 11a.
“Could Palaeocastor burrows have been formed during the Flood? The amount of time necessary for burrow formation, then plant growth and burrow infiltration, then fossilization, at multiple vertical levels, clearly disconfirms this as a possibility.” ↩ ↩
- 11b.
“Oard (2010, 91) noted that it had been argued that these burrows couldn't have been formed during the Flood, so must be post-Flood. Oard disagreed, arguing instead that these represent 'animal activity during the Flood,' on 'briefly exposed diluvial sediments.' Clearly, extensive plant growth, episodic and vertically staggered burrow formation, and a large terrestrial beaver population demonstrate that this phenomenon didn't 'briefly' occur during the Flood.” ↩
- 11c.
“Burrows are lebensspuren (biogenic sedimentary structures) which by definition are non-transportable (Frey 1975). Fossilization had to have occurred in place.” Arment also lists burrows, in the Blackleaf, Entrada, Morrison, Fremouw, Lashly, Naobaogou and Teekloof formations, that fall inside every Flood model, and answers them by saying the animals. “were just trying to escape the Flood waters by burrowing into mud or sand.” ↩
- 11a.
- 12.
Froede Jr., Carl R. et al. “Fossilized animal and bird footprints in megasequences.” Journal of Creation 36(3):6–9. 2022. A 2022 article in the Journal of Creation by three young-earth authors, Carl Froede, Jerry Akridge and John Reed, who test whether fossil footprints of living animals and birds fit creationist megasequences. Megasequences are a young-earth scheme that groups the rock record into large units, adapted from a naturalistic scheme called Sloss sequences, and the authors argue that the footprints continue well past the point in the Flood when all land life is supposed to have died. The article uses it for the authors' argument that footprints of living animals run past Day 150 of the Flood, and for their claim that such tracks must have formed in place. ↩
- 12a.
Section Fossilized animal/bird footprints in the Tejas megasequence: “The fossil record of animal/bird footprints/tracks/trackways created by formerly living creatures does not fit the Sloss-derived creationist megasequence model. They extend from the Kaskaskia megasequence to the present (top of the Tejas megasequence). These living creatures somehow left footprints in Flood deposits as evidence of their survival. They are found well past the megasequence-defined Day 150 termination of all terrestrial life, as conveyed by Scripture.” Their one allowance: “We recognize that footprints are possible following the 150th day of the Flood, based on dead and bobbing animals drifting prone along a soft sediment substrate leaving isolated impressions. However, we would expect these traces to be few in number, random in orientation, and isolated in occurrence.” ↩ ↩
- 12b.
“While floodwater can mix the remains of animals and marine fossils, rendering them allochthonous deposits of limited use, the fossilized footprints/tracks/trackways of formerly living creatures must be formed in situ.” ↩ ↩
- 12a.
- 13.
Droser, Mary L., and David J. Bottjer. “A semiquantitative field classification of ichnofabric.” Journal of Sedimentary Petrology 56(4):558–559. Jul 1986. A 1986 paper that sets out a six-grade field scale for rating how much of a rock's layering animals have churned. The authors photographed vertical cross-sections of rock 50 by 35 centimetres in lower Palaeozoic carbonates of the Great Basin and measured the disturbed share of each photograph with a planimeter, a tool for measuring areas on a picture. The article uses this scale, the ichnofabric index, as its common measure of how burrowed a rock is. ↩
- 13a.
Page 558: “In order to document variations in the extent of bioturbation recorded in the stratigraphic record, we have designed a semiquantitative field classification of ichnofabric … based on pattern recognition of the percentage of original sedimentary fabric which has been disrupted by biogenic reworking. Six ichnofabric indexes have been established.” The calibration: “ichnofabric was examined in numerous stratigraphic sections from lower Paleozoic carbonates in the Great Basin region of California, Nevada, and Utah. Field photographs were taken of 50-cm by 35-cm vertical cross-sectional areas. Using a planimeter, the amount of disruption represented in each photograph was determined.” The six definitions quoted in the table are on p. 558 for indexes 1 to 4 and p. 559 for indexes 5 and 6. ↩
- 13b.
Page 559: “Enlargements of the schematic diagrams of ichnofabric indexes 1 through 5 (Fig. 1) can be used in the field as 'flash cards' to rank bioturbation.” ↩
- 13c.
Page 559: “Because the primary physical structures and bed thicknesses of strata will vary from those presented here for Great Basin lower Paleozoic carbonates (Fig. 1), different schematic 'flash cards' will be necessary to study different types of strata. However, they should be constructed using the same definitions for ichnofabric indexes utilized herein, so that the data are comparable.” ↩
- 13a.
- 14.
Brand, Leonard, and Arthur Chadwick. Faith, Reason, & Earth History: A Paradigm of Earth and Biological Origins by Intelligent Design. Andrews University Press, Berrien Springs. 3rd edition. 2016. A young-earth book by Leonard Brand and Arthur Chadwick, presenting their account of Earth and biological origins by intelligent design. The cited chapter, 'Evidence for Short-Age Geology' (chapter 18), reports the authors' own survey of the bioturbation in rock formations from Utah and western Colorado. The article calls it the best empirical evidence the young-earth side holds on bioturbation. ↩
- 14a.
Section Persistent Bedding in Rocks: “We have been surveying a number of rock formations in Utah and western Colorado, quantifying in detail the amount of bioturbation in rocks from Cambrian to Eocene. Although a simple diagram showing bioturbation in the geological column (fig. 18.13A) could be interpreted to indicate an abundance of bioturbation all through the column, detailed quantification reveals a different picture. There are some small vertical sections of sediment with abundant burrows (level 4) or a lesser amount (levels 2 or 3), but the vast majority of vertical intervals in all deposits surveyed had no bioturbation or a small amount (level 1), not enough to noticeably disturb the bedding.” Earlier in the chapter the authors give a homogenisation time. Chapter 18: “Modern studies indicate that homogenization of sediments requires from one hour (experimental) to one year (field observations) to a depth of about ten centimeters.” ↩
- 14a.
- 15.
Droser, Mary L., and David J. Bottjer. “Ordovician increase in extent and depth of bioturbation: Implications for understanding early Paleozoic ecospace utilization.” Geology 17(9):850–852. Sep 1989. A short 1989 paper by the same two authors as the 1988 Cambrian study, extending their survey to the Ordovician, the period after the Cambrian. It compares the average burrowing index and the burrow depths of Cambrian and Ordovician rock and finds that burrowing became more extensive and deeper by the Late Ordovician. The article uses it for the Ordovician jump in burrowing and for the shallow depths the authors report before it. ↩
- 15a.
Page 851: “In Great Basin carbonate inner shelf settings, the first major increase in bioturbation occurred in the Early Cambrian and is reflected by an increase in average ichnofabric index from 1.02, recorded from the pre-trilobite strata, to 3.1, recorded from the trilobite-bearing Lower Cambrian strata (Droser and Bottjer, 1988) (Fig. 3A). The second major increase in extent of bioturbation occurred approximately 110 m.y. later between the Middle and Late Ordovician, when the average ichnofabric index increased from 3.1 to 4.5 (Fig. 3A).” ↩
- 15b.
Page 852: “From the Middle to the Late Ordovician, in carbonate inner shelf strata, the percentage of totally reworked beds increased by nearly an order of magnitude (Fig. 2).” ↩
- 15c.
Page 851: “Depth of bioturbation is consistently less than 6 cm through the Middle Ordovician (Droser, 1987). Measurements for depth of bioturbation observed in strata of Late Ordovician age are as much as 30 cm (Droser, 1987).” ↩
- 15a.
- 16.
Miller, Anne E. et al. “Chapter 8. Paleozoic Invertebrate Ichnology of Grand Canyon National Park.” Grand Canyon National Park Centennial Paleontological Resource Inventory, Utah Geological Association Special Publication 1, 131–170. 2021. A chapter in the park's centennial inventory of its fossils, written by one park staff member with three outside researchers. It classifies the Paleozoic trace fossils (burrows, trails and tracks in rock) by the behaviour that made them, and it records burrowing in the Tapeats Sandstone, Bright Angel Shale and Muav Limestone. The article uses it for that published record of burrowing in the three formations of the Tonto Group. ↩
- 16a.
Page 138: Hagadorn and others (2011) said: “reported the abundance of Arenicolites in the Tapeats Sandstone creating highly bioturbated beds at outcrops within eastern and western GRCA.” ↩
- 16b.
Page 138: Diplocraterion is. “common in the Tapeats Sandstone”. and, unlike Arenicolites, “contains spreiten, which indicates adjusting behavior to maintain a connection with the changing sediment-water interface.” ↩
- 16c.
Page 131: “the Bright Angel Shale, where 21 ichnogenera have been reported and classified into 15 architectural designs.” ↩
- 16d.
Page 149: “The predominance of ichnotaxa related to deposit-feeding behaviors (e.g., Cruziana, Palaeophycus, Phycodes, Planolites, Scolicia, and Teichichnus) characterizes the Cruziana Ichnofacies. This ichnofacies is typical of shallow-marine settings with moderate to low energy, ranging from the offshore to most distal shoreface. Low rates of sedimentation and erosion favor the preservation of locomotion traces.” ↩
- 16e.
Page 152: “Although body fossils are sparse in the Muav Limestone, bioturbation is extremely common within calcareous-dominated sediment and is responsible for the mottled appearance.” ↩
- 16a.
- 17.
Baldwin, Christopher T. et al. “Palaeoecology of the Bright Angel Shale in the eastern Grand Canyon, Arizona, USA, incorporating sedimentological, ichnological and palynological data.” Geological Society, London, Special Publications 228:213–236. Edited by Duncan McIlroy. 2004. A study of the Bright Angel Shale, a Middle Cambrian shale in the eastern Grand Canyon, that combines the rock texture, the trace fossils and the palynomorphs (organic microfossils) found in it. It finds a freshwater source for the mud, and its burrowing data are consistent with an estuary, a place where river water meets the sea. The chapter appears in The Application of Ichnology to Palaeoenvironmental and Stratigraphic Analysis, edited by Duncan McIlroy. The article uses it as the primary source for the Bright Angel ichnoguild scheme that Miller and colleagues 2020 summarise at their p. 149. ↩
- 17a.
Section Abstract: “The Middle Cambrian Bright Angel Shale in the eastern Grand Canyon contains a depauperate normal marine fauna, but trace fossils and palynomorphs are abundant throughout the formation. … Initial correspondence between organic matter content in mudstones and feeding type and intensity (as indicated by traces) is consistent with an estuarine setting for this deposit.” ↩ ↩
- 17a.
- 18.
Lohrer, Andrew M. et al. “Rapid reworking of subtidal sediments by burrowing spatangoid urchins.” Journal of Experimental Marine Biology and Ecology 321(2):155–169. Jul 13, 2005. A computer model of how much sediment heart urchins (Echinocardium australe) churn up, a process called bioturbation, built from field counts at six shallow sites in northern New Zealand. Its movement rate came from one site only, OB5, where the urchins reworked sediment fastest, so the authors call the output "a good upper bound estimate." The article cites it because Snelling relies on it for the three-day figure, and the paper's own figure is that surface sediment is reworked about every 3 days where the urchins are abundant. ↩
- 18a.
Section Abstract, page 155: “To better understand the bioturbation potential and functional role of Echinocardium, we developed a mathematical model and parameterized it with field data from six locations in northern New Zealand in order to estimate bioturbation rates in these places. Although urchin sizes and densities were measured in consecutive years at all six locations, we obtained a third model parameter, urchin movement rate, from one time and place only (Site OB5). Because confidence in model output was greatest at OB5, and since OB5 had the highest sediment reworking rate of all sites, our model yielded a good upper bound estimate for the bioturbation potential of Echinocardium in the areas examined. The volume of sediment displaced by Echinocardium populations reached 20,000 cm³ m⁻² d⁻¹ at OB5, suggesting that surface sediment is reworked about every 3 days at sites where Echinocardium is abundant. Experimental work with a fluorescent tracer at OB5 suggested limited downward particle movement as a result of Echinocardium bioturbation, though vertical profiles of chlorophyll a and organic matter content indicated well mixed sediment.” ↩ ↩ ↩
- 18a.
- 19.
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. Creation Science Fellowship, Pittsburgh. 2008. A 2008 conference paper by John Whitmore and Paul Garner, two authors who take a literal reading of Genesis that dates the Earth to about 6,000 years. It proposes ranking a set of geological criteria from 1 (most diagnostic) to 3 (least) to decide whether a rock unit formed before, during or after the Flood, without relying on radiometric dates or zone fossils, and applies the method to the rocks of Wyoming. The article uses it for the authors' ranking of bioturbation (animal burrowing) as one of their weakest indicators, scored 3. ↩
- 19a.
Page 430, section Bioturbation (rank = 3): “Since the Flood involved the rapid accumulation of sediments without the passage of long periods between the deposition of individual layers, we would expect extensively bioturbated horizons, with the resultant disruption of internal stratification and sedimentary structures, to be less common in Flood-deposited sediments. Before and after the Flood, as more time became available between depositional events, we would expect bioturbation to become much more abundant. We recognize that bioturbation could have occurred during the Flood on select horizons (and vertically within beds), but we expect the more slowly deposited post-Flood sediments to contain much more evidence of biological disruption. We rank bioturbation as '3' because it may have occurred at any time during earth history, although we think its preservation potential is highest in post-Flood times.” ↩
- 19a.
- 20.
Wise, Kurt P. “Fossil Grove and other Paleozoic Forests as Allochthonous Flood Deposits.” Answers Research Journal 11:237–256. 2018. A 2018 paper in the young-earth Answers Research Journal by Kurt Wise, arguing that the lycopod stumps at Fossil Grove in Glasgow, Scotland, were carried in by floodwater rather than growing where they are found. It sets out twelve criteria for telling a fossil forest that grew in place from one that was transported, and applies them to the Fossil Grove stumps. The article uses it because Wise applies the bioturbation test as a mainstream sedimentologist would: a forest that grew in place should show heavy burrowing, and this one shows none. ↩
- 20a.
Page 251: Criterion 5. “Infaunal organisms are so abundant and active in modern communities that the sediment substrates of modern communities are heavily bioturbated, usually completely obliterating original bedding. In contrast, the Flood usually involved a sediment production rate that was too high to permit extensive infaunal bioturbation (e.g. Brand and Chadwick 2016, 1086–1097). Autochthonous assemblages, then, should display much more substrate bioturbation than will be displayed in allochthonous assemblages.” Page 252: Criterion 7 of his summary list: an autochthonous (in-place) assemblage should. “include a thoroughly bioturbated substrate [vs. minor bioturbation]”. ↩
- 20b.
Page 252: Criterion 7, applied. “the preservation of original depositional laminae in Unit B and the corresponding lack of bioturbation is most consistent with allochthony.” ↩
- 20a.
- 21.
Oard, Michael J. “Is the K/T the Post-Flood Boundary?—Part 2: Paleoclimates and Fossils.” Journal of Creation 24(3):87–93. Dec 2010. The second part of a series in the young-earth Journal of Creation by Michael Oard, who places the end of the Flood in the late Cenozoic rather than at the Cretaceous-Tertiary (K/T) boundary. This part tests three further evidences for the K/T view: the Tertiary cooling trend, Tertiary mammals of the western United States, and Tertiary bird and mammal tracks with the Devil's corkscrews, and finds that they raise more questions than they answer. The article uses it for Oard's account of the tracks and corkscrews, which he assigns to the Flood. ↩
- 21a.
Page 91: “Like dinosaur tracks, bird and mammal tracks, as well as the Devil's corkscrews, represent animal activity during the Flood, before Day 150. Such tracks were made on 'briefly exposed diluvial sediments' (BEDS) during fluctuations in relative sea level during the Flooding Stage.” Page 90: On his time limit. “Debate over whether all animals were killed during the first 40 or 150 days of the Flood continues, but I accept the latter as the maximum allowable time for terrestrial life to exist outside the Ark, at the end of the Flooding Stage.” ↩
- 21a.
- 22.
Isaacs, Edward A. “Ichnofossils Refute Hydroplate Theory's Liquefaction Submodel.” Answers Research Journal 15:97–108. 2022. A 2022 paper in the young-earth Answers Research Journal by Edward A. Isaacs, which tests Walt Brown's Hydroplate Theory, a minority position within young-earth geology, against trace fossils (burrows, tracks and trails). It argues that the liquefaction (sediment turning temporarily into a fluid-like state) that Brown's model needs would erase the burrows, and that the model cannot explain the order of terrestrial vertebrate tracks. The article uses it for the statement that trace fossils are primarily formed in place and only rarely transported. ↩
- 22a.
Section Ichnofossils: A Vibrant Dataset for Diluvial Geologists: The sentence quoted here is a general statement about ichnofossils, although Isaacs is answering Walt Brown's Hydroplate Theory. “Because they are preserved strictly as a feature of the host fabric (most often sand), ichnofossils are primarily autochthonous and only rarely transported (Buatois and Mángano 2011, 15; Seilacher 1967).” ↩
- 22a.