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...

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Bibliografische gegevens
Hoofdauteur:	Jenkyns, H
Formaat:	Journal article
Taal:	English
Gepubliceerd in:	2010

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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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A global event with a regional character: the Early Toarcian Oceanic Anoxic Event in the Pindos Ocean (northern Peloponnese, Greece)
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The Cenomanian- Turonian Oceanic Anoxic Event, II. Palaeoceanographic controls on organic-matter production and preservation.
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Transient cooling episodes during Cretaceous Oceanic Anoxic Events with special reference to OAE 1a (Early Aptian)
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Nitrogen isotope evidence for water mass denitrification during the early Toarcian (Jurassic) oceanic anoxic event
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A global perturbation to the sulfur cycle during the Toarcian Oceanic Anoxic Event (vol 312, pg 484, 2011)
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Nitrate reduction, sulfate reduction, and sedimentary iron isotope evolution during the Cenomanian-Turonian oceanic anoxic event
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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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Isotopic evidence for changes in the zinc cycle during Oceanic Anoxic Event 2 (Late Cretaceous)
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Evidence for the Toarcian oceanic anoxic event in the Southern hemisphere (Los Molles Formation, Neuquen Basin, Argentina)
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TOARCIAN ANOXIC EVENT IN EUROPE - AN ORGANIC GEOCHEMICAL STUDY
door: Farrimond, P, et al.
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STRATIGRAPHIC AND PALEO-OCEANOGRAPHIC SETTING OF ORGANIC CARBON-RICH STRATA DEPOSITED DURING CENOMANIAN-TURONIAN OCEANIC ANOXIC EVENT
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Black shale deposition, atmospheric CO2 drawdown, and cooling during the Cenomanian-Turonian Oceanic Anoxic Event
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Sulfur isotopes track the global extent and dynamics of euxinia during Cretaceous Oceanic Anoxic Event 2.
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