A unique geochemical record at the Permian/Triassic boundary

@article{Holser1989AUG,
  title={A unique geochemical record at the Permian/Triassic boundary},
  author={William T. Holser and Hans Peter Sch{\"o}nlaub and M. Jr. Attrep and Klaus Boeckelmann and Peter Klein and Mordeckai Magaritz and Charles J. Orth and Alois Fenninger and Catherine Jenny and Martin Kr{\'a}lik and Hermann Johann Mauritsch and Edwin Pak and J.-M. Schramm and Karl Stattegger and Rupert Schm{\"o}ller},
  journal={Nature},
  year={1989},
  volume={337},
  pages={39-44}
}
A 330-metre core drilled through the marine Permian/Triassic boundary in the Carnic Alps of Austria allows closely correlated studies of geochemistry, petrography and palaeontology across the boundary. The isotope shifts and metal concentrations are extended, multiple and complex, and do not resemble those seen at the Cretaceous/Tertiary boundary. Both the carbon isotope shifts and the chemical events (including an indium anomaly) may have causes related to a major regression of the sea. 

Carbon and Sulfur Isotope Stratigraphy of the Permian and Adjacent Intervals

The Permian was a most unusual period in geologic history. It was marked by repeated largescale climate changes, major extinction events, abrupt and extensive volcanic activity (the Siberian traps),

Geochemical changes at the Permian–Triassic transition in Southern Alps and adjacent area: a review

Compilation of the recent literature from the Southern Alps and adjacent area confirms the geochemical variations of unusual amplitudes during the Permian-Triassic boundary interval (PTBI). A great

Permo-Triassic Boundary Superanoxia and Stratified Superocean: Records from Lost Deep Sea

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The symmetry in lithostratigraphy and redox condition of the boundary sections suggest that the superocean Panthalassa became totally stratified for nearly 20 million years across the Permo-Triassic boundary.

The Permian-Triassic of the Gartnerkofel-1 Core (Carnic Alps, Austria): Sulfur Isotopes

Sulfur isotope ratios in pyrite have high negative values characteristic of each level, confirming a syngenetic origin of the sulfide. Two samples of gypsum have high negative values corresponding to

Geochemistry of the end-Permian extinction event in Austria and Italy: No evidence for an extraterrestrial component

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The carbon-isotope shift at the Permian/Triassic boundary in the southern Alps is gradual

Carbon isotope ratios in marine carbonate rocks have been shown to shift at some of the time boundaries associated with extinction events; for example, Cretaceous/Tertiary1 and Ordovician/ Silurian2.

Siderophile-enriched sediments from the Cretaceous–Tertiary boundary

Siderophilic element concentrations are high in sediments from the Cretaceous–Tertiary boundary. An extraterrestrial source is indicated. Concentrations are too high to be understood in terms of the

Carbon-isotope events across the Precambrian/Cambrian boundary on the Siberian Platform

Variations of marine isotopes with time have been observed through the Phanerozoic1,2, in association with some period boundaries: Pleistocene/Holocene3, Cretaceous/Tertiary4, Permo-Triassic5,6 and

Conodont Survival and Low Iridium Abundances Across the Permian-Triassic Boundary in South China

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Elemental abundances (including Ir), carbon and oxygen ratios in carbonates, mineral content, and thin sections have been measured in samples collected across the conodont-defined Ordovician/Silurian

The Cretaceous/Tertiary boundary carbon and oxygen isotope stratigraphy, diagenesis, and paleoceanography at Zumaya, Spain

Carbon and oxygen isotope analysis of 240 m of Upper Cretaceous and Lower Tertiary limestones and marlstones from Zumaya, Spain, has revealed three distinct, negative carbon isotope excursions of up

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Chronology of Fluctuating Sea Levels Since the Triassic

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Significance of a δ13C anomaly near the Devonian/Carboniferous boundary at the Muhua section, South China

The Muhua section of Guizhou Province, South China is one of three candidates for the Devonian/Carboniferous international boundary stratotype1. Although palaeontological and stratigraphical data