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Biomarker records associated with mass extinction events

Biomarker records associated with mass extinction events
Biomarker records associated with mass extinction events
The history of life on Earth is punctuated by a series of mass extinction episodes that vary widely in their magnitude, duration, and cause. Biomarkers are a powerful tool for the reconstruction of historical environmental conditions and can therefore provide insights into the cause and responses to ancient extinction events. In examining the five largest mass extinctions in the geological record, investigators have used biomarkers to elucidate key processes such as eutrophy, euxinia, ocean acidification, changes in hydrological balance, and changes in atmospheric CO2. By using these molecular fossils to understand how Earth and its ecosystems have responded to unusual environmental activity during these extinctions, models can be made to predict how Earth will respond to future changes in its climate.
evolution, carbon cycling, atmospheric CO2
0084-6597
581-612
Whiteside, Jessica H.
5d9ad7aa-eba3-4ad9-9f6f-81be71b6829b
Grice, Kliti
81653f25-68b0-4da0-b8e2-34211dbc5239
Whiteside, Jessica H.
5d9ad7aa-eba3-4ad9-9f6f-81be71b6829b
Grice, Kliti
81653f25-68b0-4da0-b8e2-34211dbc5239

Whiteside, Jessica H. and Grice, Kliti (2016) Biomarker records associated with mass extinction events. Annual Review of Earth and Planetary Sciences, 44 (1), 581-612. (doi:10.1146/annurev-earth-060115-012501).

Record type: Article

Abstract

The history of life on Earth is punctuated by a series of mass extinction episodes that vary widely in their magnitude, duration, and cause. Biomarkers are a powerful tool for the reconstruction of historical environmental conditions and can therefore provide insights into the cause and responses to ancient extinction events. In examining the five largest mass extinctions in the geological record, investigators have used biomarkers to elucidate key processes such as eutrophy, euxinia, ocean acidification, changes in hydrological balance, and changes in atmospheric CO2. By using these molecular fossils to understand how Earth and its ecosystems have responded to unusual environmental activity during these extinctions, models can be made to predict how Earth will respond to future changes in its climate.

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More information

Published date: June 2016
Keywords: evolution, carbon cycling, atmospheric CO2
Organisations: Paleooceanography & Palaeoclimate

Identifiers

Local EPrints ID: 399727
URI: http://eprints.soton.ac.uk/id/eprint/399727
ISSN: 0084-6597
PURE UUID: 9a87ff95-a93c-4988-bad4-3eb90969ce42

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Date deposited: 24 Aug 2016 12:39
Last modified: 15 Mar 2024 01:59

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Contributors

Author: Kliti Grice

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