|2008 Joint Meeting of The Geological Society of America, Soil Science Society of America, American Society of Agronomy, Crop Science Society of America, Gulf Coast Association of Geological Societies with the Gulf Coast Section of SEPM|
|Paper No. 303-4|
|Presentation Time: 8:00 AM-6:00 PM|
Preliminary Reassessment of Upper Ordovician (Sandbian-Katian) Conodont Biostratigraphy at Dolly Ridge, West Virginia and Its Integration with Tephrochronology and Graptolite Biostratigraphy
HAWKINS, A.D.1, DEROSE, L.M.1, LESLIE, S.A.1, YOUNG, S.A.2, SELL, B.K.3, SAMSON, S.D.3, MITCHELL, C.E.4, and SADLER, P.M.5, (1) Geology and Environmental Sciences, James Madison University, MSC 6903, Harrisonburg, VA 22807, email@example.com, (2) Department of Geological Sciences, Indiana University, 1001 East 10th Street, Bloomington, IN 47405, (3) Earth Sciences, Syracuse University, Heroy Geology Laboratory, Syracuse, NY 13244, (4) Geology, The University at Buffalo, Box 603050, Buffalo, 14260-3050, (5) Department of Earth Sciences, University of California, Riverside, Riverside, CA 92521|
The temporal framework of the Nealmont Formation to Dolly Ridge Formation succession exposed at Dolly Ridge, West Virginia is of interest because it contains multiple K-bentonites and evidence of the Guttenburg carbon isotope excursion (GICE). Previously published work suggested that the top of the Dolly Ridge Formation is the base of the Belodina confluens Zone. The GICE is reported at other locations to begin in the lower part of the P. tenuis Zone and end at the start of the B. confluens Zone. We collected 14 samples throughout the upper Nealmont and Dolly Ridge formations for conodonts in an effort to improve the conodont biostratigraphic resolution and to place the GICE and K-bentonite beds into a more complete biostratigraphic framework. Three samples were collected in the upper Nealmont. They contain a fauna of Curtognathus sp., Drepanoistodus suberectus, Erismodus sp., and Plectodina sp. This sparse fauna consists of long-ranging taxa that does not better constrain the age of the top of the Nealmont. The Dolly Ridge Formation is approximately 91 meters thick. Samples were taken approximately 10 meters apart throughout the formation. With one exception, conodont recovery was low. The lower part of the Dolly Ridge Formation has a conodont fauna that includes Amorphognathus tvaernensis, Dapsilodus? sp., Drepanoistodus suberectus, Panderodus gracilis, Phragmodus undatus, and Yaoxianognathus abruptus. The upper part of the Dolly Ridge Formation has a conodont fauna consisting of Belodina sp., Curtognathus sp., Drepanoistodus suberectus, Erismodus sp., Panderodus gracilis and Phragmodus undatus. Three Belodina elements recovered are fragmentary and key elements in identifying the species of Plectodina are absent. The fauna recovered so far does not help to better resolve a biostratigraphic framework for the K-bentonites or for the GICE. Further collecting to enable a higher resolution conodont biostratigraphy integrated with tephrochronology and graptolite biostratigraphy is underway.
2008 Joint Meeting of The Geological Society of America, Soil Science Society of America, American Society of Agronomy, Crop Science Society of America, Gulf Coast Association of Geological Societies with the Gulf Coast Section of SEPM
General Information for this Meeting
|Session No. 303--Booth# 92|
Paleontology (Posters) IV - Stratigraphy and Morphology
George R. Brown Convention Center: Exhibit Hall E
8:00 AM-6:00 PM, Wednesday, 8 October 2008
Geological Society of America Abstracts with Programs, Vol. 40, No. 6, p. 475
© Copyright 2008 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.