|2011 GSA Annual Meeting in Minneapolis (9–12 October 2011)|
|Paper No. 79-5|
|Presentation Time: 9:00 AM-9:15 AM|
CONODONT BIOSTRATIGRAPHY OF THE VIRGIN LIMESTONE AT LOST CABIN SPRING: IMPLICATIONS FOR THE STUDY OF EARLY TRIASSIC BIOTIC EVENTS
MARENCO, Pedro J.1, LEPES, Erin M.1, CLAPHAM, Matthew E.2, FRAISER, Margaret L.3, and ORCHARD, Michael J.4, (1) Department of Geology, Bryn Mawr College, Bryn Mawr, PA 19010, firstname.lastname@example.org, (2) Department of Earth and Planetary Sciences, University of California, Santa Cruz, 1156 High Street, Santa Cruz, CA 95064, (3) Department of Geosciences, University of Wisconsin-Milwaukee, 3209 N. Maryland Ave, Milwaukee, WI 53201, (4) Geological Survey of Canada, 605 Robson Street, Vancouver, BC V6B 5J3, Canada|
The aftermath of the End Permian mass extinction is not yet well-understood, but low-diversity faunas, geochemistry, unusual lithologic features and evidence for anoxia suggest that environmental conditions were not conducive to biotic recovery during the Early Triassic (e.g., Hallam and Wignall, 1997; Payne et al., 2004; Pruss et al., 2006). The Lower Triassic of the western United States has been an invaluable natural laboratory for studying the aftermath because of its well-exposed mixed carbonate and siliciclastic strata. The Virgin Limestone Member of the Lower Triassic Moenkopi Formation at Lost Cabin Spring has received particular attention because of its well-exposed microbialite build-ups and because its upper Lower Triassic strata contain the transition to the biotic recovery (Fraiser and Bottjer, 2007) which began in earnest during the Anisian.
The Virgin Limestone Member section at Lost Cabin Spring has been assumed to be Spathian in age based on the occurrence of the ammonoid Tirolites in the Virgin Limestone Member near St. George, Utah about, 220 km to the northeast (Poborsky, 1954). Recent radiometric dating suggests that the Spathian represents 3 of the 5 million years of the Early Triassic (Ovtcharova et al., 2006). Given the attention that the Lost Cabin Spring section has received and its importance for understanding the mass extinction aftermath, it is vital to better constrain the timing of this section. Here we present preliminary results from an ongoing investigation of the conodont biostratigraphy of Lost Cabin Springs.
The top of the section is probably Anisian in age based on previously-reported strontium isotope results (Marenco, 2007). The Spathian-Anisian boundary is still uncertain, but the strontium isotope data suggests that the boundary is well above the sponge-microbe patch reefs that occur approximately 155 m from the base of the section. Our tentative identification of Triassospathodus homeri group P1 elements at 195 m supports our interpretation of the strontium isotope results and a Spathian age for the sponge-microbe patch reefs. Conodont elements from the base of the section are either Smithian or Spathian in age pending further analysis.
2011 GSA Annual Meeting in Minneapolis (9–12 October 2011)
General Information for this Meeting
|Session No. 79|
The Triassic: Turning Point for Phanerozoic Life
Minneapolis Convention Center: Room 205AB
8:00 AM-12:00 PM, Monday, 10 October 2011
Geological Society of America Abstracts with Programs, Vol. 43, No. 5, p. 209
© Copyright 2011 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.