Multidisciplinary high-resolution correlation of the Permian–Triassic boundary

Biostratigraphic correlation of the ten most important Permian–Triassic boundary sections throughout Tethys enables establishment of four conodont and ammonoid subdivisions within a stratigraphic interval, one to a few metres thick, representing less than 1 Ma. In ascending order, they are conodonts...

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Main Authors: Yin Hongfu, Tong Jinnan
Other Authors: The Pennsylvania State University CiteSeerX Archives
Format: Text
Language:English
Published: 1997
Subjects:
Online Access:http://citeseerx.ist.psu.edu/viewdoc/summary?doi=10.1.1.539.2001
http://dxy.cug.edu.cn/grzy/tjn/PDF files/1998-Yin.pdf
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spelling ftciteseerx:oai:CiteSeerX.psu:10.1.1.539.2001 2023-05-15T15:09:16+02:00 Multidisciplinary high-resolution correlation of the Permian–Triassic boundary Yin Hongfu Tong Jinnan The Pennsylvania State University CiteSeerX Archives 1997 application/pdf http://citeseerx.ist.psu.edu/viewdoc/summary?doi=10.1.1.539.2001 http://dxy.cug.edu.cn/grzy/tjn/PDF files/1998-Yin.pdf en eng http://citeseerx.ist.psu.edu/viewdoc/summary?doi=10.1.1.539.2001 http://dxy.cug.edu.cn/grzy/tjn/PDF files/1998-Yin.pdf Metadata may be used without restrictions as long as the oai identifier remains attached to it. http://dxy.cug.edu.cn/grzy/tjn/PDF files/1998-Yin.pdf text 1997 ftciteseerx 2016-01-08T10:57:06Z Biostratigraphic correlation of the ten most important Permian–Triassic boundary sections throughout Tethys enables establishment of four conodont and ammonoid subdivisions within a stratigraphic interval, one to a few metres thick, representing less than 1 Ma. In ascending order, they are conodonts (Clarkina changxingensis–C. deflecta Zone; Hindeodus typicalis Interval; Isarcicella parva Zone and I. isarcica Zone) and ammonoids (Pseudotirolites–Pleuronodoceras Zone, lower Otoceras Zone, upper Otoceras Zone and Ophiceras Zone). Most of them can be traced to North America and the Arctic region. Carbon isotope investigations of 24 sections along Tethys and in Greenland and Spitzbergen confirm the consistency of d13C negative excursions at the Permian–Triassic boundary, together with an inconsistent Ir anomaly. Eight sections show that in most cases there is a succession of: Ir anomaly (denoting the end-Permian catastrophic environment); d13C excursion (biomass loss, extinction); P=T boundary (origination of newcomers; potentially capable of intercontinental correlation within that short time interval). There is an intercontinental sequence boundary at the top of the Permian, and a transgressive surface at the P=T boundary followed shortly by a maximum flooding surface. An intercontinental anoxia event accompanied the transgression. Three delineations of the mass extinction phases and three population explosions have been recognized and can be more or less correlated in South China and the Southern Alps. Radiometric dating of the volcanogenic boundary clays of Meishan, Shangsi and the main-stage Siberian Tunguss Traps give an almost identical age Text Arctic Greenland Spitzbergen Unknown Arctic Greenland
institution Open Polar
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op_collection_id ftciteseerx
language English
description Biostratigraphic correlation of the ten most important Permian–Triassic boundary sections throughout Tethys enables establishment of four conodont and ammonoid subdivisions within a stratigraphic interval, one to a few metres thick, representing less than 1 Ma. In ascending order, they are conodonts (Clarkina changxingensis–C. deflecta Zone; Hindeodus typicalis Interval; Isarcicella parva Zone and I. isarcica Zone) and ammonoids (Pseudotirolites–Pleuronodoceras Zone, lower Otoceras Zone, upper Otoceras Zone and Ophiceras Zone). Most of them can be traced to North America and the Arctic region. Carbon isotope investigations of 24 sections along Tethys and in Greenland and Spitzbergen confirm the consistency of d13C negative excursions at the Permian–Triassic boundary, together with an inconsistent Ir anomaly. Eight sections show that in most cases there is a succession of: Ir anomaly (denoting the end-Permian catastrophic environment); d13C excursion (biomass loss, extinction); P=T boundary (origination of newcomers; potentially capable of intercontinental correlation within that short time interval). There is an intercontinental sequence boundary at the top of the Permian, and a transgressive surface at the P=T boundary followed shortly by a maximum flooding surface. An intercontinental anoxia event accompanied the transgression. Three delineations of the mass extinction phases and three population explosions have been recognized and can be more or less correlated in South China and the Southern Alps. Radiometric dating of the volcanogenic boundary clays of Meishan, Shangsi and the main-stage Siberian Tunguss Traps give an almost identical age
author2 The Pennsylvania State University CiteSeerX Archives
format Text
author Yin Hongfu
Tong Jinnan
spellingShingle Yin Hongfu
Tong Jinnan
Multidisciplinary high-resolution correlation of the Permian–Triassic boundary
author_facet Yin Hongfu
Tong Jinnan
author_sort Yin Hongfu
title Multidisciplinary high-resolution correlation of the Permian–Triassic boundary
title_short Multidisciplinary high-resolution correlation of the Permian–Triassic boundary
title_full Multidisciplinary high-resolution correlation of the Permian–Triassic boundary
title_fullStr Multidisciplinary high-resolution correlation of the Permian–Triassic boundary
title_full_unstemmed Multidisciplinary high-resolution correlation of the Permian–Triassic boundary
title_sort multidisciplinary high-resolution correlation of the permian–triassic boundary
publishDate 1997
url http://citeseerx.ist.psu.edu/viewdoc/summary?doi=10.1.1.539.2001
http://dxy.cug.edu.cn/grzy/tjn/PDF files/1998-Yin.pdf
geographic Arctic
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genre Arctic
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Spitzbergen
genre_facet Arctic
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Spitzbergen
op_source http://dxy.cug.edu.cn/grzy/tjn/PDF files/1998-Yin.pdf
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http://dxy.cug.edu.cn/grzy/tjn/PDF files/1998-Yin.pdf
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