High-precision U/Pb dating of the Cenomanian-Turonian boundary Kaiparowits Plateau, Utah
Thesis: S.B., Massachusetts Institute of Technology, Department of Earth, Atmospheric, and Planetary Sciences, 2012.
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Format: | Thesis |
Language: | eng |
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Massachusetts Institute of Technology
2018
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Online Access: | http://hdl.handle.net/1721.1/114340 |
_version_ | 1811098293239808000 |
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author | Stangroom, Amber M |
author2 | Samuel Bowring. |
author_facet | Samuel Bowring. Stangroom, Amber M |
author_sort | Stangroom, Amber M |
collection | MIT |
description | Thesis: S.B., Massachusetts Institute of Technology, Department of Earth, Atmospheric, and Planetary Sciences, 2012. |
first_indexed | 2024-09-23T17:12:45Z |
format | Thesis |
id | mit-1721.1/114340 |
institution | Massachusetts Institute of Technology |
language | eng |
last_indexed | 2024-09-23T17:12:45Z |
publishDate | 2018 |
publisher | Massachusetts Institute of Technology |
record_format | dspace |
spelling | mit-1721.1/1143402019-04-11T13:16:02Z High-precision U/Pb dating of the Cenomanian-Turonian boundary Kaiparowits Plateau, Utah High-precision Uranium-Lead dating of the Cenomanian-Turonian boundary Kaiparowits Plateau, Utah Stangroom, Amber M Samuel Bowring. Massachusetts Institute of Technology. Department of Earth, Atmospheric, and Planetary Sciences. Massachusetts Institute of Technology. Department of Earth, Atmospheric, and Planetary Sciences. Earth, Atmospheric, and Planetary Sciences. Thesis: S.B., Massachusetts Institute of Technology, Department of Earth, Atmospheric, and Planetary Sciences, 2012. Cataloged from PDF version of thesis. Includes bibliographical references (pages 33-40). The massive marine species turnover at the Cenomanian-Turonian boundary is associated with Oceanic Anoxic Event 11 (OAE II) and is often identified by an increase of a13C in the carbon isotopic record. A high-precision chronology of the Cenomanian- Turonian boundary is needed to better constrain the cause, timing, and extent of OAE II. To create such a timeline, four bentonite samples from the Kaiparowits Plateau, Utah were dated using U/Pb geochronology. The Cenomanian-Turonian boundary is constrained to be 94.040 ± 0.029/0.098/0.14 Ma, in agreement with recent astrochronologic studies of the same time period. This research will help improve the calibration of the astronomical time scale, as well as provide a greater understanding of the Cretaceous environment.. by Amber M. Stangroom. S.B. 2018-03-27T14:18:14Z 2018-03-27T14:18:14Z 2012 2012 Thesis http://hdl.handle.net/1721.1/114340 1028749591 eng MIT theses are protected by copyright. They may be viewed, downloaded, or printed from this source but further reproduction or distribution in any format is prohibited without written permission. http://dspace.mit.edu/handle/1721.1/7582 40 pages application/pdf n-us-ut Massachusetts Institute of Technology |
spellingShingle | Earth, Atmospheric, and Planetary Sciences. Stangroom, Amber M High-precision U/Pb dating of the Cenomanian-Turonian boundary Kaiparowits Plateau, Utah |
title | High-precision U/Pb dating of the Cenomanian-Turonian boundary Kaiparowits Plateau, Utah |
title_full | High-precision U/Pb dating of the Cenomanian-Turonian boundary Kaiparowits Plateau, Utah |
title_fullStr | High-precision U/Pb dating of the Cenomanian-Turonian boundary Kaiparowits Plateau, Utah |
title_full_unstemmed | High-precision U/Pb dating of the Cenomanian-Turonian boundary Kaiparowits Plateau, Utah |
title_short | High-precision U/Pb dating of the Cenomanian-Turonian boundary Kaiparowits Plateau, Utah |
title_sort | high precision u pb dating of the cenomanian turonian boundary kaiparowits plateau utah |
topic | Earth, Atmospheric, and Planetary Sciences. |
url | http://hdl.handle.net/1721.1/114340 |
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