Constraints on the preservation of proxy data in carbonate archives – lessons from a marine limestone to marble transect, Latemar, Italy-Reference-Cited by-同舟云学术

Constraints on the preservation of proxy data in carbonate archives – lessons from a marine limestone to marble transect, Latemar, Italy

Published:2021-10-08 Issue:2 Volume:69 Page:423-460
ISSN:0037-0746
Container-title:Sedimentology
language:en
Short-container-title:Sedimentology

Author:

Mueller Mathias¹^ORCID,Jacquemyn Carl²^ORCID,Walter Benjamin F.³,Pederson Chelsea L.¹^ORCID,Schurr Simon L.⁴,Igbokwe Onyedika A.¹⁵,Jöns Niels¹,Riechelmann Sylvia¹,Dietzel Martin⁶,Strauss Harald⁴,Immenhauser Adrian¹⁷

Affiliation:

1. Institute of Geology, Mineralogy and Geophysics Ruhr‐University Bochum Universitätsstraße 150 Bochum 44801 Germany

2. Department of Earth Science and Engineering Imperial College London Exhibition Road London SW7 2AZ UK

3. AGW Institute for Applied Geoscience Karlsruhe Institute for Technology Campus South, Adenauering 20b Karlsruhe 76131 Germany

4. Institut für Geologie und Paläontologie Westfälische Wilhelms‐Universität Münster Corrensstr. 24 Münster 48149 Germany

5. Department of Geology Alex Ekwueme Federal University Ndufu‐Alike, Ikwo P.M.B. 1010 Abakaliki Ebonyi State Nigeria

6. Institute of Applied Geosciences Graz University of Technology Rechbauerstraße 12 Graz 8010 Austria

7. Fraunhofer IEG (Institution for Energy Infrastructures and Geothermal Systems) Am Hochschulcampus 1 Bochum 44801 Germany

Funder

Deutsche Forschungsgemeinschaft

Publisher

Wiley

Subject

Stratigraphy,Geology

Link

https://onlinelibrary.wiley.com/doi/pdf/10.1111/sed.12939

Reference140 articles.

1. Pb, O, and C isotopes in silicified Mooidraai dolomite (Transvaal Supergroup, South Africa): implications for the composition of Paleoproterozoic seawater and ‘dating’ the increase of oxygen in the Precambrian atmosphere

2. A model for coupled fluid-flow and mixed-volatile mineral reactions with applications to regional metamorphism

3. Stable Isotope Transport and Contact Metamorphic Fluid Flow

4. Burial-induced oxygen-isotope re-equilibration of fossil foraminifera explains ocean paleotemperature paradoxes

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