Holocene North Atlantic surface circulation and climatic variability: evidence from diatom records

M. Witak; A. Wachnicka; A. Kuijpers; S.R. Troelstra; M.A. Prins; A. Witkowski

doi:10.1191/0959683605hl768rp

Holocene North Atlantic surface circulation and climatic variability: evidence from diatom records

M. Witak, A. Wachnicka, A. Kuijpers, S.R. Troelstra, M.A. Prins, A. Witkowski

Research output: Contribution to Journal › Article › Academic › peer-review

Abstract

Diatom analyses have been performed on a 425 cm long Holocene marine sediment sequence from the North Atlantic south of Iceland and a 920 cm sediment core spanning the last c. 7500 years from Skalafjord, Faeroe Islands. Additional core data include stable isotopes and results from magnetic susceptibility measurements, while chronostratigraphic control has been provided by AMS

Original language	English
Pages (from-to)	85-96
Journal	The Holocene
Volume	15
Issue number	1
DOIs	https://doi.org/10.1191/0959683605hl768rp
Publication status	Published - 2005

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title = "Holocene North Atlantic surface circulation and climatic variability: evidence from diatom records",

abstract = "Diatom analyses have been performed on a 425 cm long Holocene marine sediment sequence from the North Atlantic south of Iceland and a 920 cm sediment core spanning the last c. 7500 years from Skalafjord, Faeroe Islands. Additional core data include stable isotopes and results from magnetic susceptibility measurements, while chronostratigraphic control has been provided by AMS",

author = "M. Witak and A. Wachnicka and A. Kuijpers and S.R. Troelstra and M.A. Prins and A. Witkowski",

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T1 - Holocene North Atlantic surface circulation and climatic variability: evidence from diatom records

AU - Witak, M.

AU - Wachnicka, A.

AU - Kuijpers, A.

AU - Troelstra, S.R.

AU - Prins, M.A.

AU - Witkowski, A.

PY - 2005

Y1 - 2005

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AB - Diatom analyses have been performed on a 425 cm long Holocene marine sediment sequence from the North Atlantic south of Iceland and a 920 cm sediment core spanning the last c. 7500 years from Skalafjord, Faeroe Islands. Additional core data include stable isotopes and results from magnetic susceptibility measurements, while chronostratigraphic control has been provided by AMS

U2 - 10.1191/0959683605hl768rp

DO - 10.1191/0959683605hl768rp

M3 - Article

SN - 0959-6836

VL - 15

SP - 85

EP - 96

JO - The Holocene

JF - The Holocene

IS - 1

ER -

Holocene North Atlantic surface circulation and climatic variability: evidence from diatom records

Abstract

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