Negative δ13Ccarb shifts in Upper Ordovician (Hirnantian) Guanyinqiao Bed of South China linked to diagenetic carbon fluxes-Reference-Cited by-同舟云学术

Negative δ13Ccarb shifts in Upper Ordovician (Hirnantian) Guanyinqiao Bed of South China linked to diagenetic carbon fluxes

Published:2017-12 Issue: Volume:487 Page:430-446
ISSN:0031-0182
Container-title:Palaeogeography, Palaeoclimatology, Palaeoecology
language:en
Short-container-title:Palaeogeography, Palaeoclimatology, Palaeoecology

Author:

Chen Can,Wang Jiasheng,Algeo Thomas J.^ORCID,Wang Zhou,Tu Shen,Wang Guangzhe,Yang Junxia

Funder

State Key R&D Project of China

International IMBER Project

National Natural Science Foundation of China

China Scholarship Council

Publisher

Elsevier BV

Subject

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

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

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