An experiment to assess the effects of diatom dissolution on oxygen isotope ratios
Rationale: Current studies which use the oxygen isotope composition from diatom silica (δ18Odiatom) as a palaeoclimate proxy assume that the δ18Odiatom value reflects the isotopic composition of the water in which the diatom formed. However, diatoms dissolve post mortem, preferentially losing less s...
| Main Authors: | , , , , , , , , |
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| Format: | Article |
| Published: |
Wiley
2016
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| Subjects: | |
| Online Access: | https://eprints.nottingham.ac.uk/31157/ |