What is it about?
A coupled change in ocean circulation and atmospheric CO2 during oceanic anoxic event 2 (OAE 2), and also pulses of volcanism, probably from the High Arctic large igneous provinces (LIPs), were detected during OAE 2.
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Why is it important?
A direct reconstruction of ocean circulation during OAE 2, and its link to climatic changes during the event.
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This page is a summary of: Changing ocean circulation and hydrothermal inputs during Ocean Anoxic Event 2 (Cenomanian–Turonian): Evidence from Nd-isotopes in the European shelf sea, Earth and Planetary Science Letters, August 2013, Elsevier,
DOI: 10.1016/j.epsl.2013.05.053.
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