Plants—the great survivors!

[en] The marine fossil record shows five mass extinctions at the Ordovician–Silurian, Frasnian–Famennian (Late Devonian), Permian–Triassic, Triassic–Jurassic and Cretaceous–Palaeogene transitions. However, only one of these significantly disrupted plant evolution. We clearly need to look again at what we really mean by mass extinctions events, especially in the context of the so-called sixth mass extinction occurring today. © 2018 John Wiley & Sons Ltd, The Geologists' Association & The Geological Society of London

Disciplines :

Earth sciences & physical geography

Author, co-author :

Cascales-Miñana, B.; CNRS, University of Lille, UMR 8198 – Evo-Eco-Paleo, Lille, F-59000, France

Servais, T.; CNRS, University of Lille, UMR 8198 – Evo-Eco-Paleo, Lille, F-59000, France

Cleal, C. J.; Department of Natural Sciences, National Museum Wales, Cardiff, CF10 3NP, United Kingdom

Gerrienne, Philippe ; Université de Liège - ULiège > Département de géologie > Evolution and diversity dynamics lab

Anderson, J.; Evolutionary Studies Institute, Witwatersrand University, Johannesburg, South Africa

Language :

English

Title :

Plants—the great survivors!

Publication date :

2018

Journal title :

Geology Today

ISSN :

0266-6979

eISSN :

1365-2451

Publisher :

Wiley-Blackwell

Volume :

Issue :

Pages :

224-229

Peer reviewed :

Peer Reviewed verified by ORBi

Available on ORBi :

since 02 July 2019

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Bibliography

Anderson, J.M., Anderson, H.M. & Cleal, C.J. 2007. Brief History of the Gymnosperms: Classification, Biodiversity, Phytogeography and Ecology. South Africa National Biodiversity Institute, Pretoria
Bonis, N.R. & Kürschner, W.M. 2012. Vegetation history, diversity patterns, and climate change across the Triassic/Jurassic boundary. Paleobiology, v.38, pp.240–264
Cascales-Miñana, B. & Cleal, C.J. 2014. The plant fossil record reflects just two great extinction events. Terra Nova, v.26, pp.195–200
Cascales-Miñana, B., Cleal, C.J. & Diez, J.B. 2013. What is the best way to measure extinction? Reflection from the palaeobotanical record. Earth-Science Reviews, v.124, pp.126–147
Cascales-Miñana, B., Diez, J.B., Gerrienne, P. & Cleal, C.J. 2016. A palaeobotanical perspective on the great end-Permian biotic crisis. Historical Biology, v.28, pp.1066–1074
Cleal, C.J. & Cascales-Miñana, B. 2014. Composition and dynamics of the great Phanerozoic Evolutionary Floras. Lethaia, v.47, pp.469–484
Hochuli, P.A., Sanson-Barrera, A., Schneebeli-Hermann, E. & Bucher, H. 2016. Severest crisis overlooked—worst disruption of terrestrial environments postdates the Permian–Triassic mass extinction. Nature Scientific Reports, v.6, srep28372
Mander, L., Kürschner, W.M. & McElwain, J.C., 2013. Palynostratigraphy and vegetation history of the Triassic–Jurassic transition in East Greenland. Journal of the Geological Society, v.170, pp.37–46
McElwain, J.C. & Punyasena, S.W. 2007. Mass extinction events and the plant fossil record. Trends in Ecology & Evolution, v.22, pp.548–557
Jianxin Y., Broutin, J., Zhong-Qiang, C., Xiao, S., Hui, L., Darling C. & Qisheng, H. 2015. Vegetation changeover across the Permian–Triassic Boundary in Southwest China: Extinction, survival, recovery and palaeoclimate: A critical review. Earth-Science Reviews, v.149, pp.203–224

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