Unraveling short- and long-term carbon cycle variations during the Oceanic Anoxic Event 2 from the Paris Basin Chalk

The Oceanic Anoxic Event 2 (OAE2, ca. 94.6 Ma) is one of the major perturbations in the global carbon cycle during the Phanerozoic. Stable carbon isotopes (δ13C) from marine and continental sedimentary environments document this carbon cycle perturbation with a pronounced (> 2‰) positive carbon i...

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Veröffentlicht in:	Global and planetary change 2020-03, Vol.186, p.103126, Article 103126
Hauptverfasser:	Boulila, Slah, Charbonnier, Guillaume, Spangenberg, Jorge E., Gardin, Silvia, Galbrun, Bruno, Briard, Justine, Le Callonnec, Laurence
Format:	Artikel
Sprache:	eng
Schlagworte:	Carbon cycle CTB Diachroneity Earth Sciences Eccentricity amplification Geochemistry OAE2 Paleontology Paris Basin Sciences of the Universe Stratigraphy Volcanism
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