The Calcium Isotope (δ<sup>44/40</sup>Ca) Record Through Environmental Changes: Insights From the Late Triassic
نویسندگان
چکیده
Abstract Calcium isotopes (δ 44/40 Ca) are particularly useful in palaeo‐environmental studies due to the key role of carbonate minerals continental weathering and their formation seawater. The calcium isotope ratio can provide hints on past changes fluxes, environmental shifts, ecological factors alternatively diagenesis rocks. investigation Late Triassic record offers a great opportunity evaluate such time interval that witnessed important turnovers, as first appearance calcareous nannoplankton, ocean acidification periods elevated extinction rates. In this study, we present δ Ca data set from upper Norian (Upper Triassic) through lower Hettangian (Lower Jurassic) interval. records reveal two globally significant signals: ∼ 0.20‰ decrease early Rhaetian small, negative (∼0.14‰) excursion corresponding emplacement Central Atlantic Magmatic Province, at end Triassic. possible explanations for these signals isotopic influx high chemical rate carbonates possibly acidification, respectively. considerable (∼0.15–0.30‰) offset between study areas is likely combined result local differences lithology marine diagenesis. major evolutionary step represented by occurrence nannoplankton did not have determining signature carbonates.
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ژورنال
عنوان ژورنال: Geochemistry Geophysics Geosystems
سال: 2022
ISSN: ['1525-2027']
DOI: https://doi.org/10.1029/2022gc010405