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Stable oxygen isotope ratios of planktonic foraminifera in MIS 16 of IODP Site 306-U1313

B. David A. Naafs, Jens Hefter, Patrizia Ferretti, Ruediger Stein, Gerald H. Haug

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Abstract

Naafs, Bernhard David A; Hefter, Jens; Ferretti, Patrizia; Stein, Ruediger; Haug, Gerald H (2011): Stable oxygen isotope ratios of planktonic foraminifera in MIS 16 of IODP Site 306-U1313 [dataset]. PANGAEA, https://doi.org/10.1594/PANGAEA.762822, In supplement to: Naafs, BDA et al. (2011): Sea surface temperatures did not control the first occurrence of Hudson Strait Heinrich Events during MIS 16. Paleoceanography, 26, PA4201, https://doi.org/10.1029/2011PA002135

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What this paper is about

Naafs, Bernhard David A; Hefter, Jens; Ferretti, Patrizia; Stein, Ruediger; Haug, Gerald H (2011): Stable oxygen isotope ratios of planktonic foraminifera in MIS 16 of IODP Site 306-U1313 [dataset]. PANGAEA, https://doi.org/10.1594/PANGAEA.762822, In supplement to: Naafs, BDA et al. (2011): Sea surface temperatures did not control the first occurrence of Hudson Strait Heinrich Events during MIS 16. Paleoceanography, 26, PA4201, https://doi.org/10.1029/2011PA002135

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Available abstract

Naafs, Bernhard David A; Hefter, Jens; Ferretti, Patrizia; Stein, Ruediger; Haug, Gerald H (2011): Stable oxygen isotope ratios of planktonic foraminifera in MIS 16 of IODP Site 306-U1313 [dataset]. PANGAEA, https://doi.org/10.1594/PANGAEA.762822, In supplement to: Naafs, BDA et al. (2011): Sea surface temperatures did not control the first occurrence of Hudson Strait Heinrich Events during MIS 16. Paleoceanography, 26, PA4201, https://doi.org/10.1029/2011PA002135

Key concepts: Foraminifera, Plankton, Isotopes of oxygen, Oceanography, Geology, Oxygen isotope ratio cycle, Paleontology, Stable isotope ratio

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