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Title: Phanerozoic trends in shell accumulations: A comparison of Ordovician-Silurian and Tertiary records

Conference · · Geological Society of America, Abstracts with Programs; (United States)
OSTI ID:5096089
 [1];  [2]
  1. Univ. of Chicago, IL (United States). Dept. of Geophysical Sciences
  2. Univ. of Liverpool (United Kingdom). Dept. of Earth Sciences

Evolutionary changes in the diversity and bathymetric deployment of major benthic invertebrate groups, both those that produce and those that modify bioclasts, suggest that the nature of shell accumulations is likely to have also changed through the Phanerozoic. Specifically, it has been suggested that, excepting crinoidal deposits, the Paleozoic-Triassic record is dominated by thin shell concentrations (< few 10s cm) whereas the Cretaceous-Cenozoic record includes much thicker accumulations (> 1 m). To test this, the authors focused on siliciclastic records in two end-point periods. Using the literature on North America and Europe combined with extensive field-checking, they found that brachiopod-, trilobite-, and bryozoan-dominated accumulations in the Ord-Sil are typically thin but that there are important exceptions. In the Tertiary, thick concentrations are composed of a much larger variety of groups, occur in a wider range of environments, and exhibit a greater diversity of biostratinomic features and inferred accumulation histories. Information on the paleobathymetry, paleolatitude and tectonic setting was evaluated for all data points, and so the contrasting patterns of shell accumulation can clearly be related to differences in geologic age rather than to environmental biases in data collection. Even the analysis of only a few shell-bed features, therefore, provides strong evidence for long-term changes in the nature of the bioclastic fossil record. Work still in progress suggests that there are also long-term changes in the distribution and nature of bioclastic deposits through stratigraphic (3rd-order) sequences, particularly in the character of skeletal material associated with key surfaces.

OSTI ID:
5096089
Report Number(s):
CONF-9305259-; CODEN: GAAPBC
Journal Information:
Geological Society of America, Abstracts with Programs; (United States), Vol. 25:5; Conference: 89. annual meeting of the Cordilleran Section and the 46th annual meeting of the Rocky Mountain Section of the Geological Society of America (GSA), Reno, NV (United States), 19-21 May 1993; ISSN 0016-7592
Country of Publication:
United States
Language:
English

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