Late Pennsylvanian seasonality reflected in the 18O and elemental composition of a brachiopod shell

Mii Horng-Sheng Mii, E. L. Grossman

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50 Citations (Scopus)

Abstract

To evaluate the potential for the study of Late Pennsylvanian seasonality, detailed isotopic and elemental analyses were performed on a single specimen of the brachiopod Neospirifer dunbari. Contours of 18O, Mg, Na, and S concentrations parallel growth bands and reveal a record of 1 1/2 to 2 cycles. Mg, S, and Na contents varied inversely with δ18O. This trend is opposite to the expected diagenetic trend and is consistent with the temperature dependences of Mg content and δ18O, thus implying preservation of shell chemistry. The ~1.2‰ range in δ18O values suggests a seasonal temperature variation of 5 to 6°C. This high seasonality for the tropical epicontinental sea of Kansas supports climate-model predictions of enhanced continentality in Pangean climate. -Authors

Original languageEnglish
Pages (from-to)661-664
Number of pages4
JournalGeology
Volume22
Issue number7
DOIs
Publication statusPublished - 1994 Jan 1

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Pennsylvanian
brachiopod
seasonality
shell
inland sea
climate modeling
temperature
climate
prediction
trend

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  • Geology

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Late Pennsylvanian seasonality reflected in the 18O and elemental composition of a brachiopod shell. / Horng-Sheng Mii, Mii; Grossman, E. L.

In: Geology, Vol. 22, No. 7, 01.01.1994, p. 661-664.

Research output: Contribution to journalArticle

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