Evolution of the Toarcian (Early Jurassic) carbon-cycle and global climatic controls on local sedimentary processes (Cardigan Bay Basin, UK)

The late Early Jurassic Toarcian Stage represents the warmest interval of the Jurassic Period, with an abrupt rise in global temperatures of up to ∼7 °C in mid-latitudes at the onset of the early Toarcian Oceanic Anoxic Event (T-OAE; ∼183 Ma). The T-OAE, which has been extensively studied in marine...

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Bibliographic Details
Main Authors:	Xu, Weimu, Ruhl, Micha, Jenkyns, Hugh C., Leng, Melanie J., Huggett, Jennifer M., Minisini, Daniel, Ullmann, Clemens V., Riding, James B., Weijers, Johan W.H., Storm, Marisa S., Percival, Lawrence M.E., Tosca, Nicholas J., Idiz, Erdem F., Tegelaar, Erik W., Hesselbo, Stephen P.
Format:	Article
Published:	Elsevier 2018
Subjects:	carbon-isotope stratigraphy; global weathering rates; gravity-flow deposits; oceanic anoxic event (OAE); siderite; Toarcian (Early Jurassic)
Online Access:	https://eprints.nottingham.ac.uk/48997/

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https://eprints.nottingham.ac.uk/48997/

Evolution of the Toarcian (Early Jurassic) carbon-cycle and global climatic controls on local sedimentary processes (Cardigan Bay Basin, UK)

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