Jurassic (callovian) paleotemperatures from Scotland
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Abstract
Isotopic paleotemperature analyses of belemnites and ammonites from the Belemnite Sands and Oxford Clay of Staffin Bay, Isle of Skye, are presented. Ammonites are depleted in18O compared with co-existing belemnites, which give mean temperatures of around 22°C, consistent with the Skye belemnite analysed by Urey et al. [1]. Possible reasons for the ammonite-belemnite difference are discussed.
Publication type | Article |
---|---|
Publication Subtype | Journal Article |
Title | Jurassic (callovian) paleotemperatures from Scotland |
Series title | Earth and Planetary Science Letters |
DOI | 10.1016/0012-821X(70)90008-7 |
Volume | 9 |
Issue | 5 |
Year Published | 1970 |
Language | English |
Publisher | Elsevier |
Description | 6 p. |
First page | 421 |
Last page | 426 |
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