Middle to Upper Ordovician stable carbon isotope stratigraphy and sedimentary facies in the Shunbei and Tahe areas, northern-central Tarim, China

Author:

Ma Dong-ChenORCID,Li Wen-Jie,Chen Zhong-Yang,Fang XiangORCID,Cheng Jun-Feng,Jia Xing-Liang

Funder

National Natural Science Foundation of China

Chinese Academy of Sciences

Chinese Academy of Geological Sciences, Ministry of Natural Resources

SINOPEC Northwest Oil Field Company

Publisher

Elsevier BV

Subject

Paleontology,Stratigraphy,Ecology, Evolution, Behavior and Systematics

Reference73 articles.

1. Did early land plants produce a stepwise change in atmospheric oxygen during the Late Ordovician (Sandbian ∼458 Ma)?;Adiatma;Palaeogeography, Palaeoclimatology, Palaeoecology,2019

2. Darriwilian (Middle Ordovician) δ13Ccarb chemostratigraphy in the Precordillera of Argentina: Documentation of the middle Darriwilian Isotope Carbon Excursion (MDICE) and its use for intercontinental correlation;Albanesi;Palaeogeography, Palaeoclimatology, Palaeoecology,2013

3. Ainsaar, L., Meidla, T., Tinn, O., 2004. Middle and Upper Ordovician stable isotope stratigraphy across the facies belts in the eastern Baltic. In: Hints, O., Ainsaar, L. (Eds.), WOGOGOB-2004 8th Meeting of the Working Group on the Ordovician Geology of Baltoscandia: Conference Materials. Abstract and Field Guidebook, Tartu, pp. 11–12.

4. Darriwilian (Middle Ordovician) carbon isotope stratigraphy in Baltoscandia;Ainsaar;Acta Palaeontologica Sinica,2007

5. The new chronostratigraphic classification of the Ordovician System and its relations to major regional series and stages and to δ13C chemostratigraphy;Bergström;Lethaia,2009

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