Ontogenetic isotopic variation in foraminifera: Implications for palaeo proxy

The oxygen isotopic composition (δ 1 8 O) of Marginopora kudakajimaensis (Foraminiferida) is found to differ by 0.5‰ among the individuals living under similar physico-chemical conditions. The δ 1 8 O variation along the growth direction (ontogeny) is much higher, ranging between 1.5 and 2.5‰. In comparison, the ontogenetic variation in carbon isotopes (δ 1 3 C) is relatively small. The range and standard deviation of ontogenetic δ 1 8 O decrease progressively for deeper water species. There is no such systematic change in δ 1 3 C values. The study suggests that as palaeo proxy, the isotopic data not only require correct species discrimination but also a good understanding of the palaeobiology of the species.

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