Mercury anomalies and the timing of biotic recovery following the end-Triassic mass extinction

The association between Central Atlantic Magmatic Province (CAMP) eruption volatiles and the end-Triassic mass extinction remains ambiguous. Here, the authors present mercury and palaeontological evidence from the same archive and show that significant biotic recovery did not begin until CAMP erupti...

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Main Authors:	Alyson M. Thibodeau, Kathleen Ritterbush, Joyce A. Yager, A. Joshua West, Yadira Ibarra, David J. Bottjer, William M. Berelson, Bridget A. Bergquist, Frank A. Corsetti
Format:	Article
Language:	English
Published:	Nature Publishing Group 2016-04-01
Series:	Nature Communications
Online Access:	https://doi.org/10.1038/ncomms11147

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spelling	doaj-a7a9f7be67d84e6f87abf16b5b7adbca2021-05-11T10:49:33ZengNature Publishing GroupNature Communications2041-17232016-04-01711810.1038/ncomms11147Mercury anomalies and the timing of biotic recovery following the end-Triassic mass extinctionAlyson M. Thibodeau0Kathleen Ritterbush1Joyce A. Yager2A. Joshua West3Yadira Ibarra4David J. Bottjer5William M. Berelson6Bridget A. Bergquist7Frank A. Corsetti8Department of Earth Sciences, University of TorontoDepartment of Geology and Geophysics, University of Utah, Salt Lake City, Utah 84103, USADepartment of Earth Sciences, University of Southern CaliforniaDepartment of Earth Sciences, University of Southern CaliforniaDepartment of Earth System Science, Stanford UniversityDepartment of Earth Sciences, University of Southern CaliforniaDepartment of Earth Sciences, University of Southern CaliforniaDepartment of Earth Sciences, University of TorontoDepartment of Earth Sciences, University of Southern CaliforniaThe association between Central Atlantic Magmatic Province (CAMP) eruption volatiles and the end-Triassic mass extinction remains ambiguous. Here, the authors present mercury and palaeontological evidence from the same archive and show that significant biotic recovery did not begin until CAMP eruptions ceased.https://doi.org/10.1038/ncomms11147
collection	DOAJ
language	English
format	Article
sources	DOAJ
author	Alyson M. Thibodeau Kathleen Ritterbush Joyce A. Yager A. Joshua West Yadira Ibarra David J. Bottjer William M. Berelson Bridget A. Bergquist Frank A. Corsetti
spellingShingle	Alyson M. Thibodeau Kathleen Ritterbush Joyce A. Yager A. Joshua West Yadira Ibarra David J. Bottjer William M. Berelson Bridget A. Bergquist Frank A. Corsetti Mercury anomalies and the timing of biotic recovery following the end-Triassic mass extinction Nature Communications
author_facet	Alyson M. Thibodeau Kathleen Ritterbush Joyce A. Yager A. Joshua West Yadira Ibarra David J. Bottjer William M. Berelson Bridget A. Bergquist Frank A. Corsetti
author_sort	Alyson M. Thibodeau
title	Mercury anomalies and the timing of biotic recovery following the end-Triassic mass extinction
title_short	Mercury anomalies and the timing of biotic recovery following the end-Triassic mass extinction
title_full	Mercury anomalies and the timing of biotic recovery following the end-Triassic mass extinction
title_fullStr	Mercury anomalies and the timing of biotic recovery following the end-Triassic mass extinction
title_full_unstemmed	Mercury anomalies and the timing of biotic recovery following the end-Triassic mass extinction
title_sort	mercury anomalies and the timing of biotic recovery following the end-triassic mass extinction
publisher	Nature Publishing Group
series	Nature Communications
issn	2041-1723
publishDate	2016-04-01
description	The association between Central Atlantic Magmatic Province (CAMP) eruption volatiles and the end-Triassic mass extinction remains ambiguous. Here, the authors present mercury and palaeontological evidence from the same archive and show that significant biotic recovery did not begin until CAMP eruptions ceased.
url	https://doi.org/10.1038/ncomms11147
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Mercury anomalies and the timing of biotic recovery following the end-Triassic mass extinction

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