Biotic e¡ects of impacts and volcanism
The biotic effects of late Maastrichtian mantle plume volcanism on Ninetyeast Ridge and Deccan volcanism mirror those of the Cretaceous^Tertiary (KT) mass extinction and impact event. Planktonic foraminifera responded to high stress conditions with the same impoverished and small-sized species assem...
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ftciteseerx:oai:CiteSeerX.psu:10.1.1.506.6483 2023-05-15T18:00:32+02:00 Biotic e¡ects of impacts and volcanism Gerta Keller The Pennsylvania State University CiteSeerX Archives 2003 application/pdf http://citeseerx.ist.psu.edu/viewdoc/summary?doi=10.1.1.506.6483 http://geoweb.princeton.edu/research/Paleontology/Keller_2003_EPSL.pdf en eng http://citeseerx.ist.psu.edu/viewdoc/summary?doi=10.1.1.506.6483 http://geoweb.princeton.edu/research/Paleontology/Keller_2003_EPSL.pdf Metadata may be used without restrictions as long as the oai identifier remains attached to it. http://geoweb.princeton.edu/research/Paleontology/Keller_2003_EPSL.pdf volcanism impacts biotic e¡ects Maastrichtian Cretaceous^Tertiary DSDP Site 216 text 2003 ftciteseerx 2016-01-08T09:24:22Z The biotic effects of late Maastrichtian mantle plume volcanism on Ninetyeast Ridge and Deccan volcanism mirror those of the Cretaceous^Tertiary (KT) mass extinction and impact event. Planktonic foraminifera responded to high stress conditions with the same impoverished and small-sized species assemblages dominated by the disaster/ opportunists Guembelitria cretacea, which characterize the KT mass extinction worldwide. Similar high stress late Text Planktonic foraminifera Unknown |
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ftciteseerx |
language |
English |
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volcanism impacts biotic e¡ects Maastrichtian Cretaceous^Tertiary DSDP Site 216 |
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volcanism impacts biotic e¡ects Maastrichtian Cretaceous^Tertiary DSDP Site 216 Gerta Keller Biotic e¡ects of impacts and volcanism |
topic_facet |
volcanism impacts biotic e¡ects Maastrichtian Cretaceous^Tertiary DSDP Site 216 |
description |
The biotic effects of late Maastrichtian mantle plume volcanism on Ninetyeast Ridge and Deccan volcanism mirror those of the Cretaceous^Tertiary (KT) mass extinction and impact event. Planktonic foraminifera responded to high stress conditions with the same impoverished and small-sized species assemblages dominated by the disaster/ opportunists Guembelitria cretacea, which characterize the KT mass extinction worldwide. Similar high stress late |
author2 |
The Pennsylvania State University CiteSeerX Archives |
format |
Text |
author |
Gerta Keller |
author_facet |
Gerta Keller |
author_sort |
Gerta Keller |
title |
Biotic e¡ects of impacts and volcanism |
title_short |
Biotic e¡ects of impacts and volcanism |
title_full |
Biotic e¡ects of impacts and volcanism |
title_fullStr |
Biotic e¡ects of impacts and volcanism |
title_full_unstemmed |
Biotic e¡ects of impacts and volcanism |
title_sort |
biotic e¡ects of impacts and volcanism |
publishDate |
2003 |
url |
http://citeseerx.ist.psu.edu/viewdoc/summary?doi=10.1.1.506.6483 http://geoweb.princeton.edu/research/Paleontology/Keller_2003_EPSL.pdf |
genre |
Planktonic foraminifera |
genre_facet |
Planktonic foraminifera |
op_source |
http://geoweb.princeton.edu/research/Paleontology/Keller_2003_EPSL.pdf |
op_relation |
http://citeseerx.ist.psu.edu/viewdoc/summary?doi=10.1.1.506.6483 http://geoweb.princeton.edu/research/Paleontology/Keller_2003_EPSL.pdf |
op_rights |
Metadata may be used without restrictions as long as the oai identifier remains attached to it. |
_version_ |
1766169653771501568 |