Sedimentary organic matter and δ13CKerogen variation on the southern Iberian palaeomargin (Betic Cordillera, SE Spain) during the latest Pliensbachian

Sedimentary organic matter and δ13CKerogen variation on the southern Iberian palaeomargin (Betic Cordillera, SE Spain) during the latest Pliensbachian–Early Toarcian

Published:2019-11 Issue: Volume:534 Page:109342
ISSN:0031-0182
Container-title:Palaeogeography, Palaeoclimatology, Palaeoecology
language:en
Short-container-title:Palaeogeography, Palaeoclimatology, Palaeoecology

Author:

Rodrigues Bruno,Silva Ricardo L.,Reolid Matías,Mendonça Filho João Graciano,Duarte Luís V.

Funder

Fundação para a Ciência e Tecnologia

Irish Centre for Research in Applied Geosciences

Publisher

Elsevier BV

Subject

Paleontology,Earth-Surface Processes,Ecology, Evolution, Behavior and Systematics,Oceanography

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3. Charcoal evidence that rising atmospheric oxygen terminated Early Jurassic ocean anoxia;Baker;Nat. Commun.,2017

4. Ocean circulation in the Toarcian (Early Jurassic): a key control on deoxygenation and carbon burial on the European Shelf;Baroni;Paleoceanogr. Paleoclimatol.,2018

5. Mapping and geochemical characterization of the Toarcian organic matter in the Mediterranean Tethys and Middle East;Baudin;Org. Geochem.,1990

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