2004 Denver Annual Meeting (November 7–10, 2004)
Paper No. 71-5
Presentation Time: 9:15 AM-9:30 AM

LOWER TRIASSIC MICROBIALITES AND THEIR RELATIONSHIP TO LONG-TERM ENVIRONMENTAL STRESS FOLLOWING THE END-PERMIAN MASS EXTINCTION

PRUSS, Sara Brady, Organismic and Evolutionary Biology, Harvard Univ, 26 Oxford Street, Cambridge, MA 02138, spruss@usc.edu and BOTTJER, David J., Earth Sciences, Univ of Southern California, Los Angeles, CA 90089-0740

In studies of Lower Triassic strata exposed in the southwestern United States and southern Turkey, the Early Triassic has been found to represent an anachronistic time period dominated by depositional systems reminiscent of the Neoproterozoic—Early Paleozoic. In particular, planar microbialites, small stromatolites, thrombolites, and microbial reefs developed extensively in normal marine carbonate environments of the Early Triassic. These microbialites have been found in strata deposited immediately after the end-Permian mass extinction (southern Turkey), as well as in sections deposited in the latest Early Triassic (southwestern United States). In the 4-7 million years that followed the end-Permian mass extinction, there existed a metazoan reef gap, a reduction in trace fossil infaunalization, and an abundance of opportunists, which point to an overall long-term ecologic relaxation that set the stage for the proliferation of disaster taxa. Lower Triassic strata also provide evidence for increased oceanic alkalinity in the form of carbonate precipitates and flat-pebble conglomerates, indicating that unusual environmental conditions existed and likely played a role in microbialite formation. The presence of Lower Triassic wrinkle structures, indicators of microbial mats in siliciclastic environments, represents a reduction in infaunal bioturbation, suggesting that ecological changes fostered the resurgence of disaster form microbial structures. It is therefore hypothesized that the environmentally widespread and global development of microbial structures represents an ecological response to a decimation of organisms during the end-Permian mass extinction followed by a prolonged interval of environmental stress that suppressed the recovery of metazoans and fostered the formation of microbial structures in their absence.

2004 Denver Annual Meeting (November 7–10, 2004)
General Information for this Meeting
Session No. 71
Adversity, Advantages, Opportunities: Phanerozoic Stromatolites as "Survivor" vs. "Disaster" Taxa
Colorado Convention Center: Ballroom 2&3
8:00 AM-12:00 PM, Monday, 8 November 2004

Geological Society of America Abstracts with Programs, Vol. 36, No. 5, p. 182

© Copyright 2004 The Geological Society of America (GSA), all rights reserved. Permission is hereby granted to the author(s) of this abstract to reproduce and distribute it freely, for noncommercial purposes. Permission is hereby granted to any individual scientist to download a single copy of this electronic file and reproduce up to 20 paper copies for noncommercial purposes advancing science and education, including classroom use, providing all reproductions include the complete content shown here, including the author information. All other forms of reproduction and/or transmittal are prohibited without written permission from GSA Copyright Permissions.