Geochemistry of oceanic anoxic events

Geochemistry of oceanic anoxic events

Oceanic anoxic events (OAEs) record profound changes in the climatic and paleoceanographic state of the planet and represent major disturbances in the global carbon cycle. OAEs that manifestly caused major chemical change in the Mesozoic Ocean include those of the early Toarcian (Posidonienschiefer...

Podrobná bibliografie
Hlavní autor:	Jenkyns, H
Médium:	Journal article
Jazyk:	English
Vydáno:	2010

Podobné jednotky

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A global event with a regional character: the Early Toarcian Oceanic Anoxic Event in the Pindos Ocean (northern Peloponnese, Greece)
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Transient cooling episodes during Cretaceous Oceanic Anoxic Events with special reference to OAE 1a (Early Aptian)
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Further evidence for the development of photic-zone euxinic conditions during Mesozoic oceanic anoxic events
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Significant increases in global weathering during Oceanic Anoxic Events 1a and 2 indicated by calcium isotopes
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Significant increases in global weathering during Oceanic Anoxic Events 1a and 2 indicated by calcium isotopes
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Uranium isotope evidence for two episodes of deoxygenation during Oceanic Anoxic Event 2
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