Literature DB >> 19541995

Fossil plant relative abundances indicate sudden loss of Late Triassic biodiversity in East Greenland.

Jennifer C McElwain1, Peter J Wagner, Stephen P Hesselbo.   

Abstract

The pace of Late Triassic (LT) biodiversity loss is uncertain, yet it could help to decipher causal mechanisms of mass extinction. We investigated relative abundance distributions (RADs) of six LT plant assemblages from the Kap Stewart Group, East Greenland, to determine the pace of collapse of LT primary productivity. RADs displayed not simply decreases in the number of taxa, but decreases in the number of common taxa. Likelihood tests rejected a hypothesis of continuously declining diversity. Instead, the RAD shift occurred over the upper two-to-four fossil plant assemblages and most likely over the last three (final 13 meters), coinciding with increased atmospheric carbon dioxide concentration and global warming. Thus, although the LT event did not induce mass extinction of plant families, it accompanied major and abrupt change in their ecology and diversity.

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Year:  2009        PMID: 19541995     DOI: 10.1126/science.1171706

Source DB:  PubMed          Journal:  Science        ISSN: 0036-8075            Impact factor:   47.728


  12 in total

1.  An explanation for conflicting records of Triassic-Jurassic plant diversity.

Authors:  Luke Mander; Wolfram M Kürschner; Jennifer C McElwain
Journal:  Proc Natl Acad Sci U S A       Date:  2010-08-16       Impact factor: 11.205

2.  Mercury evidence for pulsed volcanism during the end-Triassic mass extinction.

Authors:  Lawrence M E Percival; Micha Ruhl; Stephen P Hesselbo; Hugh C Jenkyns; Tamsin A Mather; Jessica H Whiteside
Journal:  Proc Natl Acad Sci U S A       Date:  2017-06-19       Impact factor: 11.205

3.  Graptolite community responses to global climate change and the Late Ordovician mass extinction.

Authors:  H David Sheets; Charles E Mitchell; Michael J Melchin; Jason Loxton; Petr Štorch; Kristi L Carlucci; Andrew D Hawkins
Journal:  Proc Natl Acad Sci U S A       Date:  2016-07-18       Impact factor: 11.205

4.  An exceptional role for flowering plant physiology in the expansion of tropical rainforests and biodiversity.

Authors:  C Kevin Boyce; Jung-Eun Lee
Journal:  Proc Biol Sci       Date:  2010-06-16       Impact factor: 5.349

5.  Compound-specific carbon isotopes from Earth's largest flood basalt eruptions directly linked to the end-Triassic mass extinction.

Authors:  Jessica H Whiteside; Paul E Olsen; Timothy Eglinton; Michael E Brookfield; Raymond N Sambrotto
Journal:  Proc Natl Acad Sci U S A       Date:  2010-03-22       Impact factor: 11.205

6.  Tracking taphonomic regimes using chemical and mechanical damage of pollen and spores: an example from the Triassic-Jurassic mass extinction.

Authors:  Luke Mander; Cassandra J Wesseln; Jennifer C McElwain; Surangi W Punyasena
Journal:  PLoS One       Date:  2012-11-07       Impact factor: 3.240

7.  Increased atmospheric SO₂ detected from changes in leaf physiognomy across the Triassic-Jurassic boundary interval of East Greenland.

Authors:  Karen L Bacon; Claire M Belcher; Matthew Haworth; Jennifer C McElwain
Journal:  PLoS One       Date:  2013-04-10       Impact factor: 3.240

8.  A microbial carbonate response in synchrony with the end-Triassic mass extinction across the SW UK.

Authors:  Yadira Ibarra; Frank A Corsetti; Sarah E Greene; David J Bottjer
Journal:  Sci Rep       Date:  2016-01-27       Impact factor: 4.379

9.  Thermal erosion of cratonic lithosphere as a potential trigger for mass-extinction.

Authors:  Jean Guex; Sebastien Pilet; Othmar Müntener; Annachiara Bartolini; Jorge Spangenberg; Blair Schoene; Bryan Sell; Urs Schaltegger
Journal:  Sci Rep       Date:  2016-03-24       Impact factor: 4.379

10.  End-Triassic mass extinction started by intrusive CAMP activity.

Authors:  J H F L Davies; A Marzoli; H Bertrand; N Youbi; M Ernesto; U Schaltegger
Journal:  Nat Commun       Date:  2017-05-31       Impact factor: 14.919

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