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Steep oceanic DIC δ13C depth gradient during the Hirnantian Glaciation

Yang, Shengchao; Fan, Junxuan; Algeo, Thomas J; Shields, Graham A; Zhou, Ying; Li, Chao; Chen, Jitao; ... Shen, Shuzhong; + view all (2024) Steep oceanic DIC δ13C depth gradient during the Hirnantian Glaciation. Earth-Science Reviews , 255 , Article 104840. 10.1016/j.earscirev.2024.104840.

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Abstract

The Hirnantian carbon isotopic excursion (HICE) was characterized by a positive δ13C excursion (up to ∼ + 7‰) of oceanic dissolved inorganic carbon (DIC). However its mechanism remains controversial, impeding our understanding of this global event and its environmental significance. Here, we conducted a comprehensive analysis of global carbon-isotope records, based on 65 paleogeographically-widely distributed sections (4612 carbon-isotope data), documenting a steep oceanic DIC δ13C water-depth gradient (e.g., a 4.6‰ offset in the HICE excursion magnitude within Laurentia) during the Hirnantian Stage. We propose a hybrid hypothesis that the HICE records a shift toward more positive values owing to a large glacio-eustatic fall (>100 m) under the herein-identified steep δ13C water-depth gradient, with potential contributions from global-ocean δ13CDIC changes and authigenic carbonates. This study provides the first large-data evidence for a widely density-stratified ocean during the Hirnantian Glaciation, with implications for reconstructions of ocean circulation and the carbon cycle during the Early Paleozoic.

Type: Article
Title: Steep oceanic DIC δ13C depth gradient during the Hirnantian Glaciation
DOI: 10.1016/j.earscirev.2024.104840
Publisher version: https://doi.org/10.1016/j.earscirev.2024.104840
Language: English
Additional information: This version is the author accepted manuscript. For information on re-use, please refer to the publisher’s terms and conditions.
Keywords: Ordovician; HICE; carbon cycle; ice age; dissolved inorganic carbon
UCL classification: UCL
UCL > Provost and Vice Provost Offices > UCL BEAMS
UCL > Provost and Vice Provost Offices > UCL BEAMS > Faculty of Maths and Physical Sciences
UCL > Provost and Vice Provost Offices > UCL BEAMS > Faculty of Maths and Physical Sciences > Dept of Earth Sciences
URI: https://discovery.ucl.ac.uk/id/eprint/10193643
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