The Calcium Isotope (δ <sup>44/40</sup> Ca) Record Through Environmental Changes: Insights From the Late Triassic-Reference-Cited by-同舟云学术

The Calcium Isotope (δ ^44/40 Ca) Record Through Environmental Changes: Insights From the Late Triassic

Published:2022-12 Issue:12 Volume:23 Page:
ISSN:1525-2027
Container-title:Geochemistry, Geophysics, Geosystems
language:en
Short-container-title:Geochem Geophys Geosyst

Author:

Kovács Zsófia¹²^ORCID,Demangel Isaline¹²^ORCID,Baldermann Andre³^ORCID,Hippler Dorothee³^ORCID,Schmitt Anne‐Désirée⁴,Gangloff Sophie⁴^ORCID,Krystyn Leopold⁵,Richoz Sylvain¹²

Affiliation:

1. NAWI Graz Geocenter Institute of Earth Sciences University of Graz Graz Austria

2. Department of Geology University of Lund Lund Sweden

3. NAWI Graz Geocenter Institute of Applied Geosciences Graz University of Technology Graz Austria

4. CNRS University of Strasbourg ENGEES Strasbourg France

5. Department of Palaeontology University of Vienna Vienna Austria

Funder

Austrian Science Fund

Publisher

American Geophysical Union (AGU)

Subject

Geochemistry and Petrology,Geophysics

Link

https://onlinelibrary.wiley.com/doi/pdf/10.1029/2022GC010405

Reference72 articles.

1. Explaining the Phanerozoic Ca isotope history of seawater

2. Significant increases in global weathering during Oceanic Anoxic Events 1a and 2 indicated by calcium isotopes

3. Calcium isotope evidence for dramatic increase of continental weathering during the Toarcian oceanic anoxic event (Early Jurassic)

4. Co-variation of silicate, carbonate and sulfide weathering drives CO2 release with erosion

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