Did early land plants produce a stepwise change in atmospheric oxygen during the Late Ordovician (Sandbian ~458 Ma)?-Reference-Cited by-同舟云学术

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Did early land plants produce a stepwise change in atmospheric oxygen during the Late Ordovician (Sandbian ~458 Ma)?

Published:2019-11 Issue: Volume:534 Page:109341
ISSN:0031-0182
Container-title:Palaeogeography, Palaeoclimatology, Palaeoecology
language:en
Short-container-title:Palaeogeography, Palaeoclimatology, Palaeoecology

Author:

Adiatma Y. Datu,Saltzman Matthew R.,Young Seth A.,Griffith Elizabeth M.,Kozik Nevin P.,Edwards Cole T.,Leslie Stephen A.,Bancroft Alyssa M.

Funder

National Science Foundation

Publisher

Elsevier BV

Subject

Paleontology,Earth-Surface Processes,Ecology, Evolution, Behavior and Systematics,Oceanography

Reference92 articles.

1. Quantifying early marine diagenesis in shallow-water carbonate sediments;Ahm;Geochim. Cosmochim. Acta,2018

2. Middle and Upper Ordovician carbon isotope chemostratigraphy in Baltoscandia: a correlation standard and clues to environmental history;Ainsaar;Palaeogeogr. Palaeoclimatol. Palaeoecol.,2010

3. Co-evolution of oceans, climate, and the biosphere during the ‘Ordovician Revolution’: a review;Algeo;Palaeogeogr. Palaeoclimatol. Palaeoecol.,2016

4. The Cenomanian-Turonian oceanic anoxic event, II. Palaeoceanographic controls on organic-matter production and preservation;Arthur;Geol. Soc. Lond. Spec. Publ.,1987

5. Calculation of simultaneous isotopic and trace element variations during water-rock interaction with applications to carbonate diagenesis;Banner;Geochim. Cosmochim. Acta,1990

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