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The isotopic signature of planktonic foraminifera from NE Atlantic surface sediments: implications for the reconstruction of past oceanic conditions

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The isotopic signature of planktonic foraminifera from NE Atlantic surface sediments: implications for the reconstruction of past oceanic conditions. / Ganssen, G. M.; Kroon, Dirk.

In: Journal of the Geological Society, Vol. 157, 2000, p. 693-699.

Research output: Contribution to journalArticle

Harvard

Ganssen, GM & Kroon, D 2000, 'The isotopic signature of planktonic foraminifera from NE Atlantic surface sediments: implications for the reconstruction of past oceanic conditions', Journal of the Geological Society, vol. 157, pp. 693-699.

APA

Ganssen, G. M., & Kroon, D. (2000). The isotopic signature of planktonic foraminifera from NE Atlantic surface sediments: implications for the reconstruction of past oceanic conditions. Journal of the Geological Society, 157, 693-699.

Vancouver

Ganssen GM, Kroon D. The isotopic signature of planktonic foraminifera from NE Atlantic surface sediments: implications for the reconstruction of past oceanic conditions. Journal of the Geological Society. 2000;157:693-699.

Author

Ganssen, G. M. ; Kroon, Dirk. / The isotopic signature of planktonic foraminifera from NE Atlantic surface sediments: implications for the reconstruction of past oceanic conditions. In: Journal of the Geological Society. 2000 ; Vol. 157. pp. 693-699.