The Toarcian oceanic anoxic event (T-OAE) is recorded by the presence of globally distributed marine organic carbon– rich black shales and a negative carbon isotope shift, with δ13Corg values as low as -33‰, interrupting an overarching positive excursion. Here we present new biostratigraphic data and high-resolution δ13Corg data from two Southern Hemisphere localities: Arroyo Serrucho in the north and Arroyo Lapa in the south of the Neuquén Basin, Argentina. Previous studies at these localities aimed to provide an accurate numerical age for the T-OAE and characterization of its carbon isotope stratigraphy. The new carbon isotope data and ammonite biostratigraphy presented here from Arroyo Serrucho show the T-OAE to be recorded lower in the ...
The early Aptian Oceanic Anoxic Event (OAE) 1a represents a major perturbation in the global carbon ...
An important episode of carbon sequestration, Oceanic Anoxic Event 1a (OAE-1a), characterizes the Lo...
The marked 3-8[per mille sign] negative carbon isotope excursion associated with the Early Toarcian ...
The Toarcian, Early Jurassic, Oceanic Anoxic Event (T-OAE: ~183 Ma) was characterized by globally sy...
The Pliensbachian–Toarcian boundary interval is characterized by a ~ 3‰ negative carbon-isotope excu...
This is the final version. Available on open access from Nature Research via the DOI in this recordT...
The first record of the Early Toarcian Oceanic Anoxic Event (c. 183 Ma) from the Southern Hemisphere...
New data from a Lower Jurassic shale section in the Neuquén Basin, Argentina, are presented in order...
<p>The first record of the Early Toarcian Oceanic Anoxic Event (<em>c</em>. 183 Ma) from the Souther...
Oceanic anoxic events were time intervals in the Mesozoic characterized by widespread distribution o...
The late Albian–early Cenomanian oceanic anoxic event 1d (OAE-1d; ~103 to 99.5 Ma) represents a glob...
The present paper reports on the sedimentological and geochemical record of Albian–Turonian neritic ...
The lack of a continuous high-resolution carbon-isotope (δ13C) record based on a single material, an...
The first carbon and oxygen isotope curves for the Valanginian to Early Barremian (Early Cretaceous)...
The lack of a continuous high-resolution carbon-isotope (δ13C) record based on a single material, a...
The early Aptian Oceanic Anoxic Event (OAE) 1a represents a major perturbation in the global carbon ...
An important episode of carbon sequestration, Oceanic Anoxic Event 1a (OAE-1a), characterizes the Lo...
The marked 3-8[per mille sign] negative carbon isotope excursion associated with the Early Toarcian ...
The Toarcian, Early Jurassic, Oceanic Anoxic Event (T-OAE: ~183 Ma) was characterized by globally sy...
The Pliensbachian–Toarcian boundary interval is characterized by a ~ 3‰ negative carbon-isotope excu...
This is the final version. Available on open access from Nature Research via the DOI in this recordT...
The first record of the Early Toarcian Oceanic Anoxic Event (c. 183 Ma) from the Southern Hemisphere...
New data from a Lower Jurassic shale section in the Neuquén Basin, Argentina, are presented in order...
<p>The first record of the Early Toarcian Oceanic Anoxic Event (<em>c</em>. 183 Ma) from the Souther...
Oceanic anoxic events were time intervals in the Mesozoic characterized by widespread distribution o...
The late Albian–early Cenomanian oceanic anoxic event 1d (OAE-1d; ~103 to 99.5 Ma) represents a glob...
The present paper reports on the sedimentological and geochemical record of Albian–Turonian neritic ...
The lack of a continuous high-resolution carbon-isotope (δ13C) record based on a single material, an...
The first carbon and oxygen isotope curves for the Valanginian to Early Barremian (Early Cretaceous)...
The lack of a continuous high-resolution carbon-isotope (δ13C) record based on a single material, a...
The early Aptian Oceanic Anoxic Event (OAE) 1a represents a major perturbation in the global carbon ...
An important episode of carbon sequestration, Oceanic Anoxic Event 1a (OAE-1a), characterizes the Lo...
The marked 3-8[per mille sign] negative carbon isotope excursion associated with the Early Toarcian ...