First record of the Early Toarcian Oceanic Anoxic Event from the Southern Hemisphere, Neuquen Basin, Argentina

The first record of the Early Toarcian Oceanic Anoxic Event (c. 183 Ma) from the Southern Hemisphere is described from the Neuquén Basin, Argentina, identified chemostratigraphically on the basis of a relative increase in marine organic carbon and a characteristic negative carbon-isotope excursion (...

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Main Authors: Al-Suwaidi, A, Angelozzi, G, Baudin, F, Damborenea, SE, Hesselbo, S, Jenkyns, H, Mancenido, M, Riccardi, A
Format: Journal article
Language:English
Published: 2010
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author Al-Suwaidi, A
Angelozzi, G
Baudin, F
Damborenea, SE
Hesselbo, S
Jenkyns, H
Mancenido, M
Riccardi, A
author_facet Al-Suwaidi, A
Angelozzi, G
Baudin, F
Damborenea, SE
Hesselbo, S
Jenkyns, H
Mancenido, M
Riccardi, A
author_sort Al-Suwaidi, A
collection OXFORD
description The first record of the Early Toarcian Oceanic Anoxic Event (c. 183 Ma) from the Southern Hemisphere is described from the Neuquén Basin, Argentina, identified chemostratigraphically on the basis of a relative increase in marine organic carbon and a characteristic negative carbon-isotope excursion (δ13Corg) in bulk rock and fossil wood. The negative excursion of -6‰ in bulk organic carbon (falling to -31.3‰) crosses the boundary of the tenuicostatum-hoelderi Andean ammonite Zones, equivalent to the tenuicostatum-falciferum/serpentinum zones of Europe. These data indicate that the Early Toarcian Oceanic Anoxic Event was a global phenomenon. © 2010 Geological Society of London.
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spelling oxford-uuid:ff646c8e-21d5-490b-9c22-3e98f6d8eb7e2022-03-27T13:44:35ZFirst record of the Early Toarcian Oceanic Anoxic Event from the Southern Hemisphere, Neuquen Basin, ArgentinaJournal articlehttp://purl.org/coar/resource_type/c_dcae04bcuuid:ff646c8e-21d5-490b-9c22-3e98f6d8eb7eEnglishSymplectic Elements at Oxford2010Al-Suwaidi, AAngelozzi, GBaudin, FDamborenea, SEHesselbo, SJenkyns, HMancenido, MRiccardi, AThe first record of the Early Toarcian Oceanic Anoxic Event (c. 183 Ma) from the Southern Hemisphere is described from the Neuquén Basin, Argentina, identified chemostratigraphically on the basis of a relative increase in marine organic carbon and a characteristic negative carbon-isotope excursion (δ13Corg) in bulk rock and fossil wood. The negative excursion of -6‰ in bulk organic carbon (falling to -31.3‰) crosses the boundary of the tenuicostatum-hoelderi Andean ammonite Zones, equivalent to the tenuicostatum-falciferum/serpentinum zones of Europe. These data indicate that the Early Toarcian Oceanic Anoxic Event was a global phenomenon. © 2010 Geological Society of London.
spellingShingle Al-Suwaidi, A
Angelozzi, G
Baudin, F
Damborenea, SE
Hesselbo, S
Jenkyns, H
Mancenido, M
Riccardi, A
First record of the Early Toarcian Oceanic Anoxic Event from the Southern Hemisphere, Neuquen Basin, Argentina
title First record of the Early Toarcian Oceanic Anoxic Event from the Southern Hemisphere, Neuquen Basin, Argentina
title_full First record of the Early Toarcian Oceanic Anoxic Event from the Southern Hemisphere, Neuquen Basin, Argentina
title_fullStr First record of the Early Toarcian Oceanic Anoxic Event from the Southern Hemisphere, Neuquen Basin, Argentina
title_full_unstemmed First record of the Early Toarcian Oceanic Anoxic Event from the Southern Hemisphere, Neuquen Basin, Argentina
title_short First record of the Early Toarcian Oceanic Anoxic Event from the Southern Hemisphere, Neuquen Basin, Argentina
title_sort first record of the early toarcian oceanic anoxic event from the southern hemisphere neuquen basin argentina
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