Post-Cambrian closure of the deep-water slope-basin taphonomic window
Abstract
Exceptional faunas (Konservat-Lagerstatten that preserve traces of volatile nonmineralized tissues) are statistically overabundant in the Cambrian Period; almost all examples preserved in continental-slope and shelf-basin environments are of this age. The hypothesis that an increase in the amount and complexity of bioturbation was an important agent in the elimination of this deep-water slope-basin taphonomic window is supported. Post-Cambrian ichnofaunal assemblages contain a higher proportion of pascichnia and agrichnia, ethologies produced by a mobile infauna. They also illustrate the lateral partitioning of organisms into different environmental niches; both opportunistic and equilibrium infaunas occur in low-oxygen environments in which the preservation of nonbiomineralized tissues was favored. Direct consumption of carcasses by bioturbating organisms was less important than changes to sediment properties as a result of bioturbation, notably enhanced microbial degradation of reactive organic matter, increased permeability, and the disruption of geochemical gradients necessary for mineral authigenesis.
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During the Precambrian, from the late Archean until the Ediacaran-Cambrian boundary interval, near-surface diagenetic processes including phosphatization and pyritization likely occurred closer to the sediment surface than at later times, leading to earlier and more rapid permineralization of unprocessed carbonaceous materials.
“The key feature of this model is that during the Precambrian, from the late Archean until the Ediacaran-Cambrian boundary interval, near-surface diagenetic processes including phosphatization and pyritization likely occurred closer to the sediment surface than at later times (McIlroy & Logan, 1999; Orr et al., 2003; Bailey et al., 2006), leading to the earlier and more rapid permineralization of”
From Remarkable preservation of microbial mats in Neoproterozoic siliciclastic settings: Implications for Ediacaran taphonomic models (2009) · cites this paper as Orr et al., 2003
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- Authors
- Orr, P. J., Benton, M. J., & Briggs, D. E. G.
- Affiliations
- University College Dublin (IE)
- University of Bristol (GB)
- Yale University (US)
- Venue
- Geology
- Publisher
- Geological Society of America
- Published
- 2003
- Volume
- 31
- Issue
- 9
- Pages
- 769
- ISSN
- 0091-7613 (ISSN-L)
- OpenAlex
- W2087292482
- Semantic Scholar
- 0b8ad8fd0ac5c372b4a58bb72e22fa84181bde92
- Cited by
- 73
- References
- 33
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- FWCI
- 1.29
- Type
- journal article
- Language
- en
- Open access
- closed
- Locations
- Geology (publishedVersion)
- Explore Bristol Research (submittedVersion)
- Bristol Research (University of Bristol) (submittedVersion)
- Funders
- University of Chicago
- Topics
- Physical Sciences › Earth and Planetary Sciences › Paleontology › Paleontology and Stratigraphy of Fossils
- Physical Sciences › Earth and Planetary Sciences › Paleontology › Paleontology and Evolutionary Biology
- Physical Sciences › Earth and Planetary Sciences › Earth-Surface Processes › Geological formations and processes
- Keywords
- taphonomy, Lagerstätte, bioturbation, continental slope, infauna, low oxygen environment, authigenesis, microbial degradation, sediment permeability, geochemical gradients, Cambrian
About these checks
Registry, retraction, Cites and statistics results are computed, not judged, with one exception: a printed reference that no index lists is read once by a model before it counts as a citation error. Claims are extracted by a model and kept only when their quote appears verbatim in the text; each cited source is then checked, with a model’s help, for whether it says what the claim relies on. Those verdicts can be wrong — read the claim’s quote and the cited source before relying on one.
Statistics and arithmetic are recomputed, not judged.
Confidence bands are shown only for fields calibrated on our annotated test set. None is calibrated yet, so no band is shown.
What counts as a claim ›How we measure confidence ›How we check this ›
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