Late Permian global coal hiatus linked to 13C-depleted CO2 flux into the atmosphere during the final consolidation of Pangea: Comment and Reply

D. R. Gröcke; Kevin Faure; Maarten J. de Wit; James P. Willis

doi:10.1130/0091-7613(1996)024<0473:LPGCHL>2.3.CO;2

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Research Article| May 01, 1996

Late Permian global coal hiatus linked to ¹³C-depleted CO₂ flux into the atmosphere during the final consolidation of Pangea: Comment and Reply

D. R. Gröcke;

D. R. Gröcke

1

Department of Earth Sciences, Monash University, Clayton, Victoria 3168, Australia

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Kevin Faure;

Kevin Faure

2

Geological Survey of Japan, Tsukuba, Ibaraki 305, Japan

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Maarten J. de Wit;

Maarten J. de Wit

3

Department of Geological Sciences, University of Cape Town, Rondebosch 7700, South Africa

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James P. Willis

3

Department of Geological Sciences, University of Cape Town, Rondebosch 7700, South Africa

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Author and Article Information

D. R. Gröcke

1

Department of Earth Sciences, Monash University, Clayton, Victoria 3168, Australia

Kevin Faure

2

Geological Survey of Japan, Tsukuba, Ibaraki 305, Japan

Maarten J. de Wit

3

Department of Geological Sciences, University of Cape Town, Rondebosch 7700, South Africa

James P. Willis

3

Department of Geological Sciences, University of Cape Town, Rondebosch 7700, South Africa

Publisher: Geological Society of America

First Online: 02 Jun 2017

Online ISSN: 1943-2682

Print ISSN: 0091-7613

Geological Society of America

Geology (1996) 24 (5): 473–475.

https://doi.org/10.1130/0091-7613(1996)024<0473:LPGCHL>2.3.CO;2

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Late Permian global coal hiatus linked to ¹³C-depleted CO₂ flux into the atmosphere during the final consolidation of Pangea: Comment and Reply

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Late Permian global coal hiatus linked to ¹³C-depleted CO₂ flux into the atmosphere during the final consolidation of Pangea: Comment and Reply