Temperature dependence of oxygen isotope fractionation in coccolith calcite: A culture and core top calibration of the genus Calcidiscus
Reconstructions of seawater temperature based on measurement of oxygen isotopes in carbonates mostly derive from analyses of bulk sediment samples or manually picked foraminifera. The temperature dependence of 18O fractionation in biogenic calcite was first established in the 1950s and the objective...
| المؤلفون الرئيسيون: | , , , |
|---|---|
| التنسيق: | Journal article |
| اللغة: | English |
| منشور في: |
2013
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مواد مشابهة
Oxygen isotopes in calcite grown under cave-analogue conditions
حسب: Day, C, وآخرون
منشور في: (2011)
حسب: Day, C, وآخرون
منشور في: (2011)
Oxygen isotopes in calcite grown under cave-analogue conditions
حسب: Day, C, وآخرون
منشور في: (2011)
حسب: Day, C, وآخرون
منشور في: (2011)