What Does Graptolite Origination and Extinction Reveal about the Cause of the Late Ordovician Mass Extinction?

Language: English

Published by Cambridge University Press, GB, 2026

1009684051 / 9781009684057

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Assesses the macroevolutionary turnover of paleotropical planktic graptolites during the Late Ordovician Mass Extinction (LOME) via automated sequencing and capture-mark-recapture modeling. Graptolites exhibited a succession of turnover pulses (sensu Elizabeth Vrba) that were coincident with the main phases of the Hirnantian glaciation and during which the Diplograptina experienced declining metapopulation size, elevated extinction, zero species originations, and ultimately, complete extermination. Concurrently, the Neograptina (latest Katian temperate zone immigrants) exhibit pulses of both extinction and adaptive radiation. Thus, the LOME involved intense species selection and the wholesale alteration of the clade diversity structure of a major element of the zooplankton. The LOME is unlikely to have been a direct effect of ocean anoxia or sampling bias but rather resulted from Hirnantian climate change, which altered nutrient supplies and plankton community compositions along with ecological displacement and loss of habitat that together drove the succession of turnover pulses. This title is also available as open access on Cambridge Core.…

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Title
What Does Graptolite Origination and Extinction Reveal about the Cause of the Late Ordovician Mass Extinction?
Author
Charles E. Mitchell, H. David Sheets, Michael J. Melchin, Chris Holmden
Publisher
Cambridge University Press, GB
Publication year
2026
Condition
New
Binding
Paperback
Language
English
ISBN 10
1009684051
ISBN 13
9781009684057
Item weight
157 grams

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