HIGHLIGHTS
- who: Biogeosciences and collaborators from the de Boelelaan, HV, Amsterdam, the Netherlands have published the article: Oxygen isotope composition of the final chamber of planktic foraminifera provides evidence of vertical migration and depth-integrated growth, in the Journal: (JOURNAL)
- what: The authors show that the mean value of δ 18 O of the final chambers (δ 18 OF ) is 0.2 ‰ ± 0.4 ‰ (1σ ) higher than the mean value δ 18 O of The authors show that there is no statistical difference in the δ 18 Osacculifer values of shells of three different size classes of T. sacculifer although . . .
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