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Anomalies in global carbon cycling and extinction at the Triassic/Jurassic boundary: evidence from a marine C-isotope record

Author(s): Maria Teresa Galli , Flavio Jadoul , Stefano M. Bernasconi , Helmut Weissert

Publication date Created: February 2005

Publication date (Print): February 2005

Journal: Palaeogeography, Palaeoclimatology, Palaeoecology

Publisher: Elsevier BV

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Most cited references 29

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Geochemical consequences of increased atmospheric carbon dioxide on coral reefs

Kleypas, Buddemeier, Archer … (1999)

A coral reef represents the net accumulation of calcium carbonate (CaCO3) produced by corals and other calcifying organisms. If calcification declines, then reef-building capacity also declines. Coral reef calcification depends on the saturation state of the carbonate mineral aragonite of surface waters. By the middle of the next century, an increased concentration of carbon dioxide will decrease the aragonite saturation state in the tropics by 30 percent and biogenic aragonite precipitation by 14 to 30 percent. Coral reefs are particularly threatened, because reef-building organisms secrete metastable forms of CaCO3, but the biogeochemical consequences on other calcifying marine ecosystems may be equally severe.

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Large igneous provinces and mass extinctions

P.B. Wignall (2001)

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Interpreting carbon-isotope excursions: carbonates and organic matter

Michael Arthur, Lee Kump (1999)

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Author and article information

Journal

Title: Palaeogeography, Palaeoclimatology, Palaeoecology

Abbreviated Title: Palaeogeography, Palaeoclimatology, Palaeoecology

Publisher: Elsevier BV

ISSN (Print): 00310182

Publication date Created: February 2005

Publication date (Print): February 2005

Volume: 216

Issue: 3-4

Pages: 203-214

Article

DOI: 10.1016/j.palaeo.2004.11.009

SO-VID: 6ee946cc-35d0-4304-8f2e-8d0e9926e800

Copyright © © 2005

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http://www.elsevier.com/tdm/userlicense/1.0/

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