18O Fractionation in the coralline aragonite of Porites lobata: Implications in oceanic paleothermometry studies
This study is fundamentally focused on a simple, but relatively unpondered problem: the coral δ18O temperature sensitivity (dδ/dT). Previous paleotemperature studies of corals have involved the use of either: 1) the calcite’s δ18O temperature sensitivity for mollusks (Epstein et al., 1953) or 2) th...
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| Format: | Article |
| Language: | English |
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Universidad Autónoma de Baja California
1994-03-01
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| Series: | Ciencias Marinas |
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| Online Access: | http://www.cienciasmarinas.com.mx/index.php/cmarinas/article/view/974 |