Geochemical Records Reveal Protracted and Differential Marine Redox Change Associated With Late Ordovician Climate and Mass Extinctions-Reference-Cited by-同舟云学术

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Geochemical Records Reveal Protracted and Differential Marine Redox Change Associated With Late Ordovician Climate and Mass Extinctions

Published:2022-01-10 Issue:1 Volume:3 Page:
ISSN:2576-604X
Container-title:AGU Advances
language:en
Short-container-title:AGU Advances

Author:

Kozik Nevin P.¹^ORCID,Gill Benjamin C.²^ORCID,Owens Jeremy D.¹^ORCID,Lyons Timothy W.³^ORCID,Young Seth A.¹^ORCID

Affiliation:

1. Department of Earth, Ocean, and Atmospheric Science and National High Magnetic Field Laboratory Florida State University Tallahassee FL USA

2. Department of Geosciences Virginia Polytechnic Institute and State University Blacksburg VA USA

3. Department of Earth and Planetary Sciences University of California Riverside CA USA

Funder

American Chemical Society Petroleum Research Fund

National Science Foundation

NASA Astrobiology Institute

Publisher

American Geophysical Union (AGU)

Subject

General Medicine

Link

https://onlinelibrary.wiley.com/doi/pdf/10.1029/2021AV000563

Reference73 articles.

1. Chitinozoan biostratigraphy of a new Upper Ordovician stratigraphic framework for Anticosti Island, Canada

2. Quantifying early marine diagenesis in shallow-water carbonate sediments

3. Abrupt global-ocean anoxia during the Late Ordovician–early Silurian detected using uranium isotopes of marine carbonates

4. Katian (Upper Ordovician) δ13C chemostratigraphy and sequence stratigraphy in the United States and Baltoscandia: A regional comparison

5. Mg and Ca isotope signatures of authigenic dolomite in siliceous deep-sea sediments

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1. C, N, Hg isotopes and elemental chemostratigraphy across the Ordovician–Silurian transition in the Argentine Precordillera: Implications for the link between volcanism and extinctions;Gondwana Research;2024-09

2. Steep oceanic DIC δ13C depth gradient during the Hirnantian Glaciation;Earth-Science Reviews;2024-08

3. Modelling sulfate concentrations in the global ocean through Phanerozoic time;Journal of the Geological Society;2024-04-29

4. Linking carbon cycle perturbations to the Late Ordovician glaciation and mass extinction: A modeling approach;Earth and Planetary Science Letters;2024-04

5. Constraining reducing conditions in the Prague Basin during the late Silurian Lau/Kozlowskii extinction event;Journal of the Geological Society;2024-02-21

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