Dating late Quaternary planktonic foraminifer Neogloboquadrina pachyderma from the Arctic Ocean using amino acid racemization

Darrell S Kaufman, Leonid Polyak, Ruth Adler, James E T Channell, Chuang Xuan

Research output: Contribution to journalArticle

32 Citations (Scopus)

Abstract

The long-term rate of racemization for amino acids preserved in planktonic foraminifera was determined by using independently dated sediment cores from the Arctic Ocean. The racemization rates for aspartic acid (Asp) and glutamic acid (Glu) in the common taxon, Neogloboquadrina pachyderma, were calibrated for the last 150 ka using 14C ages and the emerging Quaternary chronostratigraphy of Arctic Ocean sediments. An analysis of errors indicates realistic age uncertainties of about ±12% for Asp and ±17% for Glu. Fifty individual tests are sufficient to analyze multiple subsamples, identify outliers, and derive robust sample mean values. The new age equation can be applied to verify and refine age models for sediment cores elsewhere in the Arctic Ocean, a critical region for understanding the dynamics of global climate change.

Original languageEnglish (US)
Article numberPA3224
JournalPaleoceanography
Volume23
Issue number3
DOIs
StatePublished - Sep 2008

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racemization
planktonic foraminifera
amino acid
aspartic acid
sediment core
chronostratigraphy
acid
outlier
global climate
climate change
Arctic Ocean
dating
sediment
rate

ASJC Scopus subject areas

  • Oceanography
  • Palaeontology

Cite this

Dating late Quaternary planktonic foraminifer Neogloboquadrina pachyderma from the Arctic Ocean using amino acid racemization. / Kaufman, Darrell S; Polyak, Leonid; Adler, Ruth; Channell, James E T; Xuan, Chuang.

In: Paleoceanography, Vol. 23, No. 3, PA3224, 09.2008.

Research output: Contribution to journalArticle

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