Preserved stable isotopic signature of subaerial diagenesis in the Mescal Limestone, central Arizona: Implications for the timing of a terrestrial plant cover: Discussion and replyDiscussion

VOLKER C. VAHRENKAMP; VICTOR ROSSINSKY

doi:10.1130/0016-7606(1987)99<595:PSISOS>2.0.CO;2

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Research Article| October 01, 1987

Preserved stable isotopic signature of subaerial diagenesis in the Mescal Limestone, central Arizona: Implications for the timing of a terrestrial plant cover: Discussion and reply: Discussion

VOLKER C. VAHRENKAMP;

VOLKER C. VAHRENKAMP

1

Rosenstiel School of Marine and Atmospheric Science, University of Miami, Rickenbacker Causeway, Miami, Florida 33149

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VICTOR ROSSINSKY, JR.

1

Rosenstiel School of Marine and Atmospheric Science, University of Miami, Rickenbacker Causeway, Miami, Florida 33149

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Author and Article Information

VOLKER C. VAHRENKAMP

1

Rosenstiel School of Marine and Atmospheric Science, University of Miami, Rickenbacker Causeway, Miami, Florida 33149

VICTOR ROSSINSKY, JR.

1

Rosenstiel School of Marine and Atmospheric Science, University of Miami, Rickenbacker Causeway, Miami, Florida 33149

Publisher: Geological Society of America

First Online: 01 Jun 2017

Online ISSN: 1943-2674

Print ISSN: 0016-7606

Geological Society of America

GSA Bulletin (1987) 99 (4): 595–596.

https://doi.org/10.1130/0016-7606(1987)99<595:PSISOS>2.0.CO;2

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Preserved stable isotopic signature of subaerial diagenesis in the Mescal Limestone, central Arizona: Implications for the timing of a terrestrial plant cover: Discussion and reply: Discussion

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Preserved stable isotopic signature of subaerial diagenesis in the Mescal Limestone, central Arizona: Implications for the timing of a terrestrial plant cover: Discussion and reply: Discussion

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