Thermogenic carbon release from the Central Atlantic magmatic province caused major end-Triassic carbon cycle perturbations.

Autor:	Heimdal TH; Centre for Earth Evolution and Dynamics, University of Oslo, Blindern, NO-0315 Oslo, Norway t.h.heimdal@geo.uio.no., Jones MT; Centre for Earth Evolution and Dynamics, University of Oslo, Blindern, NO-0315 Oslo, Norway., Svensen HH; Centre for Earth Evolution and Dynamics, University of Oslo, Blindern, NO-0315 Oslo, Norway.
Jazyk:	angličtina
Zdroj:	Proceedings of the National Academy of Sciences of the United States of America [Proc Natl Acad Sci U S A] 2020 Jun 02; Vol. 117 (22), pp. 11968-11974. Date of Electronic Publication: 2020 May 18.
DOI:	10.1073/pnas.2000095117
Abstrakt:	The Central Atlantic magmatic province (CAMP), the end-Triassic mass extinction (ETE), and associated major carbon cycle perturbations occurred synchronously around the Triassic-Jurassic (T-J) boundary (201 Ma). Negative carbon isotope excursions (CIEs) recorded in marine and terrestrial sediments attest to the input of isotopically light carbon, although the carbon sources remain debated. Here, we explore the effects of mantle-derived and thermogenic carbon released from the emplacement of CAMP using the long-term ocean-atmosphere-sediment carbon cycle reservoir (LOSCAR) model. We have tested a detailed emission scenario grounded by numerous complementary boundary conditions, aiming to model the full extent of the carbon cycle perturbations around the T-J boundary. These include three negative CIEs (i.e., Marshi/Precursor, Spelae/Initial, Tilmanni/Main) with sharp positive CIEs in between. We show that a total of ∼24,000 Gt C (including ∼12,000 Gt thermogenic C) replicates the proxy data. These results indicate that thermogenic carbon generated from the contact aureoles around CAMP sills represents a credible source for the negative CIEs. An extremely isotopically depleted carbon source, such as marine methane clathrates, is therefore not required. Furthermore, we also find that significant organic carbon burial, in addition to silicate weathering, is necessary to account for the positive δ 13 C intervals following the negative CIEs. Competing Interests: The authors declare no competing interest.
Databáze:	MEDLINE
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