Quantifying sea surface temperature ranges of the Arabian Sea for the past 20 000 years
The oxygen isotopic composition of planktonic foraminifera tests is one of the widest used geochemical tools to reconstruct past changes of physical parameters of the upper ocean. It is common practice to analyze multiple individuals from a mono-specific population and assume that the outcome reflec...
| Main Authors: | , , , , , , |
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| Format: | Article |
| Language: | English |
| Published: |
Copernicus Publications
2011-12-01
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| Series: | Climate of the Past |
| Online Access: | http://www.clim-past.net/7/1337/2011/cp-7-1337-2011.pdf |