T245 Scientific Ocean Drilling’s Impact on Geoscience: Past, Present, and Future
Wednesday, 25 September 2019
8:00 AM - 12:00 PM
Room 228AB, North Building
HABITAT OF THE NASCENT CHICXULUB CRATER
Paper number: T245-6
Program: Technical Sessions
Time: 9:15 AM – 9:30 AM
Authors
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Christopher LoweryUniversity of Texas at Austin, Austin, TX
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Shelby LyonsPennsylvania State University, State College, PA
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Joanna V. MorganImperial College London, London
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Benjamin PasseyUniversity of Michigan, Ann Arbor, MI
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Vivi VajdaDept of Palaeobotany, Stockholm
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Michael T. WhalenUniversity of Alaska Fairbanks, Fairbanks, AK
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Axel WittmannArizona State University, Tempe, AZ
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Natalia ArtemievaPlanetary Science Institute, Tucson, AZ
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Charles CockellUniversity of Edinburgh, Edinburgh
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Kenneth A. FarleyCalifornia Institute of Technology, Pasadena, CA
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Julie CosmidisPenn State University, University Park, PA
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Joshua M. GarberUniversity of Texas at Austin, Austin, TX
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Joshua M. GarberPennsylvania State University, State College, PA
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Matthew GonzalezPenn State University, University Park, PA
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Kliti GriceCurtin University of Technology, Bentley
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David KringLunar and Planetary Institute, Houston, TX
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Bettina SchaeferCurtin University of Technology, Bentley
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Sonia M. TikooStanford University, Stanford, CA
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James C. ZachosUniv California - Santa Cruz, Santa Cruz, CA
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Matthew S. FantleThe Pennsylvania State University, University Park, PA
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Katherine FreemanPennsylvania State University, University Park, PA
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Sean P.S. GulickJackson School of Geosciences, University of Texas at Austin, Austin, TX
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Elizabeth HajekPenn State University, State College, PA
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Peter HeaneyPennsylvania State University, University Park, PA
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Heather JonesCalgary, AB
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Lee KumpPenn State Univ - Univ ParkDept Geosciences, University Park, PA
Abstract
The crater became a habitat for life soon after impact with an earliest Danian nannoplankton and dinocyst assemblage appearing at the top of the tsunami bed. Diversity dropped at the top of the seiche deposits where a monogeneric calcareous dinoflagellate resting cyst assemblage is found without other nannoplankton or dinocysts, suggesting deteriorating environmental conditions. Microbial fossils made of apatite and calcite at the top of the seiche deposits suggest a thriving bacterial community in the surface ocean and at the seafloor, which we postulate was supported by energy and nutrients supplied by hydrothermal activity.
Geological Society of America Abstracts with Programs. Vol. 51, No. 5
doi: 10.1130/abs/2019AM-336889
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