Sediment bioturbation experiments and the actual rock record
The bioturbation of sediments by trace makers is often perceived by naturalists as a process requiring extensive periods of time. Little experimental work has been conducted to either support or refute such a concept. However, recent laboratory analysis indicates that the bioturbation of marine sediments can occur within short periods of time.
Marine worms, bivalves (clams), arthropods (shrimp and crabs), and echinoderms (sea urchins and brittle stars) are just some of the many animals that live on or in marine sediments (figures 1 and 2). The study of traces created in sediment is identified as ichnology (Gk ichnos = trace).1
Recently, an investigation was conducted to determine the rate that select bivalves, arthropods, and echinoderms could bioturbate marine sediments. The animals were collected from tidal flats and shallow subtidal sediments from the Ogeechee estuary, Georgia (U.S.A).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.2 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.2
The results of the study indicate 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 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.”3
It should be noted that the filter-feeding animals are interpreted to occur in the Skolithos Ichnofacies (figure 3) while the mobile deposit feeders would be found in the Cruziana Ichnofacies (figure 4). The benthic environment for each of these ichnofacies is defined as:
“Skolithos Ichnofacies (shifting substrates)—Lower littoral to infralittoral, moderate to relatively high-energy conditions most typical. Associated with slightly muddy to clean, well-sorted, shifting sediments subject to abrupt erosion or deposition. Higher energy increases physical reworking and obliterates biogenic sedimentary structures, leaving a preserved record of physical stratification. Generally corresponds to the beach foreshore and shoreface; but numerous other settings of comparable energy levels also may be represented, such as some estuarine point bars, tidal deltas, and deep-sea fans.
“Cruziana Ichnofacies (shifting to stable substrates)—In shallow marine settings, typically includes infralittoral to shallow circalittoral substrates below minimum but not maximum wave base, to somewhat quieter conditions offshore; moderate to relatively low energy; well-sorted silts and sands, to interbedded muddy and clean sands, moderately to intensely bioturbated; negligible to appreciable (though not necessarily rapid) sedimentation. A very common type of depositional environment, including not only shelves and epeiric embayments but also littoral to sub-littoral parts of certain estuaries, bays, lagoons, and tidal flats.”4
Implications for the rock record
If we are consistent in applying the uniformitarian philosophy to the rock record then we should expect a high level of bioturbation for almost all of the sediments deposited in a former marine setting, especially if that environment existed with little to no change for thousands to millions of years. Counter to that conceptualization, some diluvialists have predicted that we should expect little sediment bioturbation due to the high-energy conditions associated with the Genesis Flood.5 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 (figure 5).
The presence or absence of trace fossils and bioturbated sediments is dependent on many different factors including trace maker population density, sediment firmness, salinity, pH, food and oxygen. Also, the behavior of trace makers facing abnormal environmental stress should be considered. For example, Woodmorappe6 proposed a unique idea suggesting that rapid bioturbation could occur concurrently in several vertical tiers if the stressed ichnofauna were protected from sediment compaction and provided an aerobic environment. Many different factors would go into determining if this occurred or if the traces were rapidly produced as individual layers. There are many reasons why sediments may or may not have been bioturbated within a proposed diluvial setting and the site-specific paleoenvironmental factors should be identified.
Recent laboratory experiments document that the bioturbation of marine sediments can occur over a short period of time depending on the type and population density of trace makers. For uniformitarians, the lack of any stirred sediment requires that they appeal to punctuated catastrophic events. Such events do not eliminate their reliance on deep time assumptions—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.
As diluvialists, we can use trace fossils to help define the probable geologic conditions in which the traces were created relative to the Flood setting. Knowing the differences in the rate of bioturbation between the Skolithos and Cruziana ichnofacies allows diluvialists to possibly estimate the time period in which these traces were formed. Where no bioturbation has occurred, we need to determine the factors that prevented trace makers from stirring those sediments.
The importance of this new experimental work cannot be overemphasized as the challenge to explaining highly bioturbated sediments no longer requires deep time—it depends on the availability and types of trace makers. A large population of filter-feeding or mobile sediment-feeding animals could easily bioturbate marine sediments within the short time frames of the global Flood of Genesis. The lack of any bioturbation should direct us to other important considerations why sediment stirring did not occur.
- Cowart, J.H. and Froede, C.R., Jr., The use of trace fossils in refining depositional environments and their application to the creationist model, Creation Research Society Quarterly 31:117–124, 1994. This is an overview of the field of ichnology as it relates to the global Flood of Genesis. Return to text.
- Gingras, M.K., Pemberton, S.G., Dashtgard, S. and Dafoe, L., How fast do marine invertebrates burrow? Palaeogeography, Palaeoclimatology, Palaeoecology 270:280–286, 2008. Return to text.
- Gingras et al., ref. 2, p. 280. Return to text.
- MacEachern, J.A., Pemberton, S.G., Gingras, M.K. and Bann, K.L., The ichnofacies paradigm: A fifty-year retrospective; in: Miller, W., III. (Ed.), Trace Fossils: Concepts, Problems, Prospects, Elsevier, New York, pp. 52–77, 2007; p. 59. Return to text.
- Anonymous, Burrowing rates, Geoscience Newsletter 17:2, 2009. Return to text.
- Woodmorappe, J., Are soft-sediment trace fossils (ichnofossils) a time problem for the Flood? Journal of Creation 20(2):113–122, 2006. Return to text.
- Froede, C.R., Jr. and Cowart, J.H., Dougherty Gap: evidence for a turbidity current paleoenvironment, Creation Research Society Quarterly 32:202–214, 1996. Return to text.
- Donovan, A.A., Sedimentology of the Providence Formation; in: Reinhardt, J. (Ed.), Stratigraphy and Sedimentology of Continental Nearshore and Marine Cretaceous Sediments of the Eastern Gulf Coastal Plain, Georgia Geological Society, Atlanta, GA, pp. 29–44, 1986. Return to text.