Extensive marine anoxia associated with the Late Devonian Hangenberg Crisis

Author:

Zhang FeifeiORCID,Dahl Tais W.ORCID,Lenton Timothy M.,Luo GenmingORCID,Shen Shu-zhong,Algeo Thomas J.ORCID,Planavsky Noah,Liu JiangsiORCID,Cui YingORCID,Qie WenkunORCID,Romaniello Stephen J.ORCID,Anbar Ariel D.

Funder

National Science Foundation of China

DFF

Strategic Priority Research Program of Chinese Academy of Sciences

National Key R & D Project of China

Carlsberg Foundation

Strategic Priority Research Program

NERC

Packard Foundation

Montclair State University

NASA Astrobiology

NSF Frontiers in Earth System Dynamics

Publisher

Elsevier BV

Subject

Space and Planetary Science,Earth and Planetary Sciences (miscellaneous),Geochemistry and Petrology,Geophysics

Reference56 articles.

1. Sedimentary Corg:P ratios, paleocean ventilation, and Phanerozoic atmospheric pO2;Algeo;Palaeogeogr. Palaeoclimatol. Palaeoecol.,2007

2. Terrestrial-marine teleconnections in the Devonian: links between the evolution of land plants, weathering processes, and marine anoxic events;Algeo;Philos. Trans. R. Soc. Lond. B, Biol. Sci.,1998

3. Land plant evolution and weathering rates changes in the Devonian;Algeo;Earth Sci., J. China Univ. Geosci.,2010

4. Late Devonian oceanic anoxic events and biotic crises: “rooted” in the evolution of vascular land plants;Algeo;GSA Today,1995

5. A modern framework for the interpretation of 238U/235U in studies of ancient ocean redox;Andersen;Earth Planet. Sci. Lett.,2014

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