Long-term changes in dissolved oxygen concentrations in the ocean caused by protracted global warming

In the Earth's geological record massive marine ecological change has been attributed to the occurrence of widespread anoxia in the ocean [Jahren, 2002; White, 2002; Wignall and Twitchett, 1996]. Climate change projection till the end of this century predict a 4 to 7% decline in the dissolve ox...

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Veröffentlicht in:	Global biogeochemical cycles 2003-12, Vol.17 (4), p.35.1-n/a
Hauptverfasser:	Matear, R. J., Hirst, A. C.
Format:	Artikel
Sprache:	eng
Schlagworte:	Animal and plant ecology Animal, plant and microbial ecology Biological and medical sciences climate system model Earth sciences Earth, ocean, space Exact sciences and technology External geophysics Fundamental and applied biological sciences. Psychology Geochemistry Marine Mineralogy oceanic biogeochemical model oxygen Physical and chemical properties of sea water Physics of the oceans protracted global warming Sea water ecosystems Silicates Synecology thermocline Water geochemistry
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