Seasonal changes in sea surface temperat
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Tsuyoshi Watanabe; Amos Winter; Tadamichi Oba
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Article
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2001
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Elsevier Science
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English
β 487 KB
The oxygen isotopic composition (d 18 O) of coral skeletons reΒ―ects a combination of sea surface temperature (SST) and the d 18 O of seawater, which is related to sea surface salinity (SSS). In contrast, the magnesium/calcium (Mg/Ca) ratio of a coral skeleton reΒ―ects SST independent of salinity. By