The structure of Termination II (penultimate deglaciation and Eemian) in the North Atlantic.

A. Lototskaya, G.M. Ganssen

Research output: Contribution to JournalArticleAcademicpeer-review

Abstract

A study of the 140-100 ka interval in core T90-9P from the North Atlantic (45°N, 25°W), based on analysis of oxygen and carbon isotope records from planktonic and benthonic foraminifera, and from the bulk sediment fine fraction facilitates a detailed paleoceanographic reconstruction of the penultimate deglaciation (Termination II), and of the Eemian interglacial (δ
Original languageEnglish
Pages (from-to)1641-1654
JournalQuaternary Science Reviews
Volume18
DOIs
Publication statusPublished - 1999

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Eemian
deglaciation
interglacial
foraminifera
carbon isotope
oxygen isotope
isotopes
reconstruction
oxygen
sediments
carbon
sediment
analysis
Retaria
Oxygen Isotopes
Bulk
North Atlantic
Sediment
Carbon Isotopes

Cite this

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The structure of Termination II (penultimate deglaciation and Eemian) in the North Atlantic. / Lototskaya, A.; Ganssen, G.M.

In: Quaternary Science Reviews, Vol. 18, 1999, p. 1641-1654.

Research output: Contribution to JournalArticleAcademicpeer-review

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AB - A study of the 140-100 ka interval in core T90-9P from the North Atlantic (45°N, 25°W), based on analysis of oxygen and carbon isotope records from planktonic and benthonic foraminifera, and from the bulk sediment fine fraction facilitates a detailed paleoceanographic reconstruction of the penultimate deglaciation (Termination II), and of the Eemian interglacial (δ

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