Evidence for local carbon-cycle perturbations superimposed on the Toarcian carbon isotope excursion
| Autor: | Ronny Schoenberg, Mario‐Erich Saussele, Annette Schmid‐Röhl, Frantz Ossa Ossa, Martin Wille, Simon Lukas Schurr, Yunfeng Wang |
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| Přispěvatelé: | Ossa Ossa, Frantz, 1Department of Geosciences University of Tuebingen Tuebingen Germany, Wille, Martin, 3Institute of Geological Sciences University of Bern Bern Switzerland, Schurr, Simon, 4Institute of Geology and Paleontology University of Muenster Muenster Germany, Saussele, Mario‐Erich, Schmid‐Röhl, Annette, 5Fossil Museum and Werkforum Holcim (Süddeutschland) GmbH Dotternhausen Germany, Schoenberg, Ronny |
| Rok vydání: | 2019 |
| Předmět: |
Geologic Sediments
551.9 010504 meteorology & atmospheric sciences Oceans and Seas Perturbation (astronomy) Toarcian 010502 geochemistry & geophysics 01 natural sciences green sulfur bacteria Isotopes of oxygen Carbon cycle Carbon Cycle Paleontology Germany 550 Earth sciences & geology δ13Ccarb‐δ13Corg decoupling Ecology Evolution Behavior and Systematics 0105 earth and related environmental sciences General Environmental Science Carbon Isotopes carbon isotope excursion local carbon cycling Anoxic waters Carbon Diagenesis Carbon isotope excursion General Earth and Planetary Sciences Bloom Lipid biomarkers Geology |
| Zdroj: | Wang, Yunfeng; Ossa Ossa, Franz; Wille, Martin; Schurr, Simon; Saussele, Mario-Erich; Schmid-Röhl, Annette; Schoenberg, Ronny (2020). Evidence for local carbon-cycle perturbations superimposed on the Toarcian carbon isotope excursion. Geobiology, 18(6), pp. 682-709. Wiley 10.1111/gbi.12410 |
| ISSN: | 1472-4669 |
| DOI: | 10.1111/gbi.12410 |
| Popis: | A Jurassic negative carbon isotope excursion (CIE), co‐evolved with Toarcian Oceanic Anoxic Event (OAE) at ~183 Ma, is suggested to be linked to a global carbon‐cycle perturbation and is well documented for Toarcian terrestrial fossil woods and marine sediments around the globe. A theoretically coupled δ13Ccarb‐δ13Corg pattern due to such dubbed global carbon‐cycle event from the negative CIE in Dotternhausen Toarcian stratigraphic profile (southwest Germany) is unexpectedly disturbed by two‐step δ13Ccarb‐δ13Corg decoupling in which the last step, upper in the stratigraphic order, is of higher magnitude. However, the trigger(s) for these sudden decoupling disturbances are still poorly constrained. Here, connecting new carbon and oxygen isotope data with documentary lipid biomarkers shows that the global carbon cycle during the Toarcian OAE was disturbed by enhanced green sulfur bacteria (GSB) metabolisms and early diagenesis at local scales. The first step δ13Ccarb‐δ13Corg decoupling was induced in the initial stage of the GSB bloom. The second step of much larger δ13Ccarb‐δ13Corg decoupling arising from a GSB prosperity was, however, exaggerated by early diagenesis through the respiration of sulfate‐reducing bacteria (SRB). Paleo‐geographically distinct localities of the Tethys region show contrasting decoupled δ13Ccarb‐δ13Corg patterns, which implies that the second‐order carbon‐cycle perturbations have pervasively and independently impacted the global carbon event during the Toarcian OAE. China Scholarship Council http://dx.doi.org/10.13039/501100004543 |
| Databáze: | OpenAIRE |
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