New technique for study on isotopic fractionation between sea water and foraminiferal growing processes

Cang Shuxi; N. J. Shackleton

doi:10.1007/BF02849675

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New technique for study on isotopic fractionation between sea water and foraminiferal growing processes

OriginalPaper | Updated：2023-05-16

- New technique for study on isotopic fractionation between sea water and foraminiferal growing processes
- New technique for study on isotopic fractionation between sea water and foraminiferal growing processes
- 海洋湖沼学报（英文） 1990年8卷第4期页码：299-305
- Affiliations：
  
  1. Institute of Oceanology Academia Sinica
  2. The Godwin Laboratory Free School Lane
- Author bio：
- Funds：
  
  Contribution No. 1847 from the Institute of Oceanology, Academia Sinica.
- DOI：10.1007/BF02849675
  中图分类号：
- 纸质出版：1990
- Accepted：
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New technique for study on isotopic fractionation between sea water and foraminiferal growing processes[J]. 海洋湖沼学报（英文）, 1990,8(4):299-305.

Shuxi, C., Shackleton, N.J. New technique for study on isotopic fractionation between sea water and foraminiferal growing processes., Chin. J. Ocean. Limnol. 8, 299–305 (1990). https://doi.org/10.1007/BF02849675
New technique for study on isotopic fractionation between sea water and foraminiferal growing processes[J]. 海洋湖沼学报（英文）, 1990,8(4):299-305. DOI： 10.1007/BF02849675.

Shuxi, C., Shackleton, N.J. New technique for study on isotopic fractionation between sea water and foraminiferal growing processes., Chin. J. Ocean. Limnol. 8, 299–305 (1990). https://doi.org/10.1007/BF02849675 DOI：

摘要

Abstract

The stable isotopic δ18O and δ13C composition of foraminiferal shell calcite varies as a function of many factors including temperature and salinity. In order to understand and interpret the variations in the isotopic composition of foraminiferal shell calcite

research has been recently focused on the role of the “vital effects”. Our examination of the lamella structure of several recent planktonic foraminifera indicates that the secretion of sequential lamellae results in multiple lamillae on earlier chambers and a single lamella on the final chamber. We used a very simple procedure to separate the individual whole test of foraminifera into several chambers and measured the isotopic composition of each growth stage chamber. The results indicate that the stable isotopic composition (carbon and oxygen)

particularly that of the last two chambers

of the foraminiferal test varies as a function of the individual growing process.

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references

Berger, W. H. and J. V. Gardner, 1975. On the determination of Pleistiocene temperature from planktonic foraminifera.J. Foram. Res. 5: 102–113.

Berger, W. H., J. S. Killingley and E. Vincent, 1978. Stable isotopes in deep-sea carbonates: Boxcore ERDC-92 West Equatorial Pacific.Oceanol. Acta. 1: 230–216.

Berger, W. H., 1979. Stable isotopes in foraminifera, foraminiferal ecology and paleoecology.SEPM Short Course, 6: 159–198.

Craig, H. and L. I. Gordon, 1965. Denterium and oxygen-18 variations in the ocean and the marine atmos-phere. In “Stable Isotopes in Oceanographic Studies and Paleotemperatures”. pp. 9–310.

Duplessy, J. C., 1978. Isotope Studies in Climatic Changes. Cambridge University Press. pp. 46–67.

Shackleton, N. J., 1987. Oxygen isotope, ice volume and sea level.Quaternary Science Reviews, 6: 183–190.

Spero, H. J. and D. F. Williams, 1988. Extracting environment from planktonic foraminiferal C—13 data.Nature, 335: 717–719.

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