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dc.contributor.authorWhiteside, J.
dc.contributor.authorGrice, Kliti
dc.date.accessioned2017-01-30T15:13:11Z
dc.date.available2017-01-30T15:13:11Z
dc.date.created2016-07-21T19:30:15Z
dc.date.issued2016
dc.identifier.citationWhiteside, J. and Grice, K. 2016. Biomarker Records Associated with Mass Extinction Events. Annual Review of Earth and Plantary Sciences. 44: pp. 581-612.
dc.identifier.urihttp://hdl.handle.net/20.500.11937/44281
dc.identifier.doi10.1146/annurev-earth-060115-012501
dc.description.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.

dc.publisherANNUAL REVIEWS
dc.titleBiomarker Records Associated with Mass Extinction Events
dc.typeJournal Article
dcterms.source.volume44
dcterms.source.startPage581
dcterms.source.endPage612
dcterms.source.issn0084-6597
dcterms.source.titleAnnual Review of Earth and Plantary Sciences
curtin.departmentDepartment of Chemistry
curtin.accessStatusFulltext not available


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