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P-ISSN 0002-9599
E-ISSN 1945-452X
Science Paper
Vol. 318, Issue 8, 2018October 01, 2018 EDT

Does Large Igneous Province Volcanism Always Perturb the Mercury Cycle? Comparing the Records of Oceanic Anoxic Event 2 and the end-Cretaceous to Other Mesozoic Events

Lawrence M.E. Percival, Hugh C. Jenkyns, Tamsin A. Mather, Alexander J. Dickson, Sietske J. Batenburg, Micha Ruhl, Stephen P. Hesselbo, Richard Barclay, Ian Jarvis, Stuart A. Robinson, Lineke Woelders,
mercuryCenomanian–Turonian OAEend-CretaceousLarge Igneous Provincevolcanic styledepositional environment
https://doi.org/10.2475/08.2018.01
American Journal of Science
Percival, L. M. E., Jenkyns, H. C., Mather, T. A., Dickson, A. J., Batenburg, S. J., Ruhl, M., Hesselbo, S. P., Barclay, R., Jarvis, I., Robinson, S. A., & Woelders, L. (2018). Does large igneous province volcanism always perturb the mercury cycle? Comparing the records of Oceanic Anoxic Event 2 and the end-Cretaceous to other Mesozoic events. American Journal of Science, 318(8), 799–860. https:/​/​doi.org/​10.2475/​08.2018.01

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