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dc.contributor.author
Remirez, Mariano Nicolas
dc.contributor.author
Algeo, Thomas
dc.date.available
2020-12-10T18:41:22Z
dc.date.issued
2020-10
dc.identifier.citation
Remirez, Mariano Nicolas; Algeo, Thomas; Carbon-cycle changes during the Toarcian (Early Jurassic) and implications for regional versus global drivers of the Toarcian oceanic anoxic event; Elsevier Science; Earth-science Reviews; 209; 10-2020; 1-25
dc.identifier.issn
0012-8252
dc.identifier.uri
http://hdl.handle.net/11336/120145
dc.description.abstract
The Early Jurassic Toarcian oceanic anoxic event (T-OAE) is characterized by an extinction event, a major sea-level rise, enhanced marine primary productivity, elevated seawater temperatures, widespread deposition of organic-rich sediments, and a negative carbon-isotope excursion (CIE). However, the T-OAE exhibits significant interregional variation in its expression, with strong spatial variation in lithology, total organic carbon (TOC) content, and the magnitude of the negative CIE in both carbonate and organic carbon profiles. It is better developed as a distinct geological event on the Northwest European Shelf (NWES), exhibiting both a large organic CIE (to –5 to –7 ‰) and high TOC content (to ~10 %), than in other regions globally. The reason for the regionally variable expression of the T-OAE has been a matter of debate, with models based on both regional and global factors proposed. We review these models in the context of the global sedimentary record of the T-OAE. The T-OAE records a global carbon-cycle perturbation that has been linked to Karoo-Ferrar Large Igneous Province magmatism, suggesting that volcanic emissions of greenhouse gases were the main cause of contemporaneous paleoenvironmental changes. Increases in seawater temperature have been documented only on the NWES to date, although lithologic and geochemical evidence of enhanced chemical weathering intensities is transregional. Mercury (Hg) enrichments are found mainly in shallow-marine settings, and their provenance in volcanic emissions remains uncertain. The exceptional expression of the T-OAE on the NWES points to regional oceanographic factors in the development of watermass stratification, deepwater anoxia, and enhanced organic matter accumulation. At a global scale, shifts toward more reducing oceanic redox conditions were spatially variable, and the T-OAE may therefore be more widely recognizable by its negative CIE than by paleo-environmental redox changes.
dc.format
application/pdf
dc.language.iso
eng
dc.publisher
Elsevier Science
dc.rights
info:eu-repo/semantics/restrictedAccess
dc.rights
Atribución-NoComercial-CompartirIgual 2.5 Argentina (CC BY-NC-SA 2.5 AR)
dc.rights.uri
https://creativecommons.org/licenses/by-nc-sa/2.5/ar/
dc.subject
ANOXIA
dc.subject
BLACK SHALES
dc.subject
CARBON ISOTOPES
dc.subject
KAROO-FERRAR
dc.subject
LOWER JURASSIC
dc.subject
T-OAE
dc.subject.classification
Geociencias multidisciplinaria
dc.subject.classification
Ciencias de la Tierra y relacionadas con el Medio Ambiente
dc.subject.classification
CIENCIAS NATURALES Y EXACTAS
dc.title
Carbon-cycle changes during the Toarcian (Early Jurassic) and implications for regional versus global drivers of the Toarcian oceanic anoxic event
dc.type
info:eu-repo/semantics/article
dc.type
info:ar-repo/semantics/artículo
dc.type
info:eu-repo/semantics/publishedVersion
dc.date.updated
2020-12-04T18:36:07Z
dc.journal.volume
209
dc.journal.pagination
1-25
dc.journal.pais
Países Bajos
dc.journal.ciudad
Amsterdam
dc.description.fil
Fil: Remirez, Mariano Nicolas. Consejo Nacional de Investigaciones Científicas y Técnicas. Centro Científico Tecnológico Conicet - La Plata. Centro de Investigaciones Geológicas. Universidad Nacional de La Plata. Facultad de Ciencias Naturales y Museo. Centro de Investigaciones Geológicas; Argentina. University of Cincinnati; Estados Unidos
dc.description.fil
Fil: Algeo, Thomas. China University Of Geosciences; China. University of Cincinnati; Estados Unidos
dc.journal.title
Earth-science Reviews
dc.relation.alternativeid
info:eu-repo/semantics/altIdentifier/doi/http://dx.doi.org/10.1016/j.earscirev.2020.103283
dc.relation.alternativeid
info:eu-repo/semantics/altIdentifier/url/https://www.sciencedirect.com/science/article/abs/pii/S0012825220303299?via%3Dihub
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