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- W2616153957 abstract "Abstract The relationship between seawater temperature and the average Mg/Ca ratios in planktic foraminifera is well established, providing an essential tool for reconstructing past ocean temperatures. However, many species display alternating high and low Mg-bands within their shell walls that cannot be explained by temperature alone. Recent experiments demonstrate that intrashell Mg variability in Orbulina universa , which forms a spherical terminal shell, is paced by the diurnal light/dark cycle. Whether Mg-heterogeneity is also diurnally paced in species with more complex shell morphologies is unknown. Here we show that high Mg/Ca-calcite forms at night in cultured specimens of the multi-chambered species Neogloboquadrina dutertrei . Our results demonstrate that N. dutertrei adds a significant amount of calcite, and nearly all Mg-bands, after the final chamber forms. These results have implications for interpreting patterns of calcification in N. dutertrei and suggest that diurnal Mg-banding is an intrinsic component of biomineralization in planktic foraminifera." @default.
- W2616153957 created "2017-05-26" @default.
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- W2616153957 date "2017-05-15" @default.
- W2616153957 modified "2023-10-01" @default.
- W2616153957 title "Link between light-triggered Mg-banding and chamber formation in the planktic foraminifera Neogloboquadrina dutertrei" @default.
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- W2616153957 doi "https://doi.org/10.1038/ncomms15441" @default.
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