Preserved stable isotopic signature of subaerial diagenesis in the 1.2-b.y. Mescal Limestone, central Arizona: Implications for the timing and development of a terrestrial plant cover: Reply

Mark A. Beeunas; L. Paul Knauth

doi:10.1130/0016-7606(1985)96<1595:PSISOS>2.0.CO;2

Preserved stable isotopic signature of subaerial diagenesis in the 1.2-b.y. Mescal Limestone, central Arizona: Implications for the timing and development of a terrestrial plant cover: Reply

Mark A. Beeunas, L. Paul Knauth

Earth and Space Exploration, School of (SESE)

Research output: Contribution to journal › Letter › peer-review

Original language	English (US)
Number of pages	1
Journal	Bulletin of the Geological Society of America
Volume	96
Issue number	12
DOIs	https://doi.org/10.1130/0016-7606(1985)96<1595:PSISOS>2.0.CO;2
State	Published - Jan 1 1985

ASJC Scopus subject areas

Geology

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10.1130/0016-7606(1985)96<1595:PSISOS>2.0.CO;2

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Preserved stable isotopic signature of subaerial diagenesis in the 1.2-b.y. Mescal Limestone, central Arizona: Implications for the timing and development of a terrestrial plant cover: Reply. / Beeunas, Mark A.; Knauth, L. Paul.
In: Bulletin of the Geological Society of America, Vol. 96, No. 12, 01.01.1985.

Research output: Contribution to journal › Letter › peer-review

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Preserved stable isotopic signature of subaerial diagenesis in the 1.2-b.y. Mescal Limestone, central Arizona: Implications for the timing and development of a terrestrial plant cover: Reply

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