Sedimentary mercury enrichments as a marker for submarine Large Igneous Province volcanism? Evidence from the Mid-Cenomanian Event and Oceanic Anoxic Event 2 (Late Cretaceous)

Sedimentary mercury enrichments as a marker for submarine Large Igneous Province volcanism? Evidence from the Mid-Cenomanian Event and Oceanic Anoxic Event 2 (Late Cretaceous)

Oceanic Anoxic Event 2 (OAE 2), during the Cenomanian‐Turonian transition (∼94 Ma), was the largest perturbation of the global carbon cycle in the mid‐Cretaceous and can be recognized by a positive carbon‐isotope excursion in sedimentary strata. Although OAE 2 has been linked to large‐scale volcanis...

Podrobná bibliografie
Hlavní autoři:	Scaife, J, Ruhl, M, Dickson, A, Mather, T, Jenkyns, H, Percival, L, Hesselbo, P, Cartwright, J, Eldrett, J, Bergman, S, Minisini, D
Médium:	Journal article
Vydáno:	American Geophysical Union 2017

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