An integrated biostratigraphy (conodonts and foraminifers) and chronostratigraphy (paleomagnetic reversals, magnetic susceptibility, elemental chemistry, carbon isotopes and geochronology) for the Permian-Upper Triassic strata of Guandao section, Nanpanjiang Basin, south China
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Lehrmann D. J., Stepchinski L., ALTINER D., Orchard M. J., Montgomery P., Enos P., ...More
JOURNAL OF ASIAN EARTH SCIENCES, vol.108, pp.117-135, 2015 (SCI-Expanded)
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Publication Type:
Article / Article
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Volume:
108
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Publication Date:
2015
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Doi Number:
10.1016/j.jseaes.2015.04.030
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Journal Name:
JOURNAL OF ASIAN EARTH SCIENCES
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Journal Indexes:
Science Citation Index Expanded (SCI-EXPANDED), Scopus
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Page Numbers:
pp.117-135
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Keywords:
Permian-Triassic, Biostratigraphy, Conodonts, Foraminifera, Carbon isotopes, Paleomagnetic, Geochronology, China, GEOMAGNETIC POLARITY TIMESCALE, GUIZHOU PROVINCE, GREAT BANK, LAGENIDE FORAMINIFERS, ZIRCON GEOCHRONOLOGY, STRATOTYPE SECTION, MARINE ECOSYSTEMS, BIOTIC RECOVERY, MASS EXTINCTION, POINT GSSP
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Middle East Technical University Affiliated:
Yes
Abstract
The chronostratigraphy of Guandao section has served as the foundation for numerous studies of the end-Permian extinction and biotic recovery in south China. Guandao section is continuous from the Permian-Triassic boundary to the Upper Triassic.