Was the Late Ordovician mass extinction truly exceptional?

Research output: Contribution to journalJournal articleResearchpeer-review

Standard

Was the Late Ordovician mass extinction truly exceptional? / Rasmussen, Christian M. Ø.; Vandenbroucke, Thijs R. A.; Nogues-Bravo, David; Finnegan, Seth.

In: Trends in Ecology and Evolution, Vol. 38, No. 9, 2023, p. 812-821.

Research output: Contribution to journalJournal articleResearchpeer-review

Harvard

Rasmussen, CMØ, Vandenbroucke, TRA, Nogues-Bravo, D & Finnegan, S 2023, 'Was the Late Ordovician mass extinction truly exceptional?', Trends in Ecology and Evolution, vol. 38, no. 9, pp. 812-821. https://doi.org/10.1016/j.tree.2023.04.009

APA

Rasmussen, C. M. Ø., Vandenbroucke, T. R. A., Nogues-Bravo, D., & Finnegan, S. (2023). Was the Late Ordovician mass extinction truly exceptional? Trends in Ecology and Evolution, 38(9), 812-821. https://doi.org/10.1016/j.tree.2023.04.009

Vancouver

Rasmussen CMØ, Vandenbroucke TRA, Nogues-Bravo D, Finnegan S. Was the Late Ordovician mass extinction truly exceptional? Trends in Ecology and Evolution. 2023;38(9):812-821. https://doi.org/10.1016/j.tree.2023.04.009

Author

Rasmussen, Christian M. Ø. ; Vandenbroucke, Thijs R. A. ; Nogues-Bravo, David ; Finnegan, Seth. / Was the Late Ordovician mass extinction truly exceptional?. In: Trends in Ecology and Evolution. 2023 ; Vol. 38, No. 9. pp. 812-821.

Bibtex

@article{b8cca0f0dd524138b82f34c22730a60b,
title = "Was the Late Ordovician mass extinction truly exceptional?",
abstract = "The Late Ordovician mass extinction event is the oldest of the five great extinction events in the fossil record. It has long been regarded as an outlier among mass extinctions, primarily due to its association with a cooling climate. However, recent temporally better resolved fossil biodiversity estimates complicate this view, providing growing evidence for a prolonged but punctuated biodiversity decline modulated by changes in atmospheric composition, ocean chemistry, and viable habitat area. This evolving view invokes extinction drivers similar to those that occurred during other major extinctions; some are even factors in the current human-induced biodiversity crisis. Even this very ancient and, at first glance, exceptional event conveys important lessons about the intensifying {\textquoteleft}sixth mass extinction{\textquoteright}.",
keywords = "anthropogenic extinction analogues, ecosystem tipping points, large igneous provinces, Ordovician biodiversity loss, Phanerozoic extinction determinants",
author = "Rasmussen, {Christian M. {\O}.} and Vandenbroucke, {Thijs R. A.} and David Nogues-Bravo and Seth Finnegan",
note = "Publisher Copyright: {\textcopyright} 2023 Elsevier Ltd",
year = "2023",
doi = "10.1016/j.tree.2023.04.009",
language = "English",
volume = "38",
pages = "812--821",
journal = "Trends in Ecology & Evolution",
issn = "0169-5347",
publisher = "Elsevier Ltd. * Trends Journals",
number = "9",

}

RIS

TY - JOUR

T1 - Was the Late Ordovician mass extinction truly exceptional?

AU - Rasmussen, Christian M. Ø.

AU - Vandenbroucke, Thijs R. A.

AU - Nogues-Bravo, David

AU - Finnegan, Seth

N1 - Publisher Copyright: © 2023 Elsevier Ltd

PY - 2023

Y1 - 2023

N2 - The Late Ordovician mass extinction event is the oldest of the five great extinction events in the fossil record. It has long been regarded as an outlier among mass extinctions, primarily due to its association with a cooling climate. However, recent temporally better resolved fossil biodiversity estimates complicate this view, providing growing evidence for a prolonged but punctuated biodiversity decline modulated by changes in atmospheric composition, ocean chemistry, and viable habitat area. This evolving view invokes extinction drivers similar to those that occurred during other major extinctions; some are even factors in the current human-induced biodiversity crisis. Even this very ancient and, at first glance, exceptional event conveys important lessons about the intensifying ‘sixth mass extinction’.

AB - The Late Ordovician mass extinction event is the oldest of the five great extinction events in the fossil record. It has long been regarded as an outlier among mass extinctions, primarily due to its association with a cooling climate. However, recent temporally better resolved fossil biodiversity estimates complicate this view, providing growing evidence for a prolonged but punctuated biodiversity decline modulated by changes in atmospheric composition, ocean chemistry, and viable habitat area. This evolving view invokes extinction drivers similar to those that occurred during other major extinctions; some are even factors in the current human-induced biodiversity crisis. Even this very ancient and, at first glance, exceptional event conveys important lessons about the intensifying ‘sixth mass extinction’.

KW - anthropogenic extinction analogues

KW - ecosystem tipping points

KW - large igneous provinces

KW - Ordovician biodiversity loss

KW - Phanerozoic extinction determinants

U2 - 10.1016/j.tree.2023.04.009

DO - 10.1016/j.tree.2023.04.009

M3 - Journal article

C2 - 37183151

AN - SCOPUS:85159069493

VL - 38

SP - 812

EP - 821

JO - Trends in Ecology & Evolution

JF - Trends in Ecology & Evolution

SN - 0169-5347

IS - 9

ER -

ID: 347298418