An experiment to assess the effects of diatom dissolution on oxygen isotope ratios
(2015)
Journal Article
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... Read More about An experiment to assess the effects of diatom dissolution on oxygen isotope ratios.