(Q107047000)

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The Influence of CaCO3Dissolution on Core Top Radiocarbon Ages for Deep-Sea Sediments

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title

The Influence of CaCO3Dissolution on Core Top Radiocarbon Ages for Deep-Sea Sediments (English)

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1

Wallace S. Broecker

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author name string

Mieczyslawa Klas

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2

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Elizabeth Clark

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3

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Georges Bonani

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4

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Susan Ivy

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5

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Willy Wolfli

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6

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publication date

October 1991

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published in

Paleoceanography

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volume

6

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issue

5

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page(s)

593-608

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Boundary scavenging in the Pacific Ocean: a comparison of10Be and231Pa

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Retreat velocity of the North Atlantic polar front during the last deglaciation determined by 14C accelerator mass spectrometry

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Calibration of the 14C timescale over the past 30,000 years using mass spectrometric U–Th ages from Barbados corals

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Glacial to interglacial changes in ocean chemistry

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Comparison between radiocarbon ages obtained on coexisting planktonic foraminifera

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The relation of deep sea [Atlantic Ocean] sedimentation rates to variations in climate

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Arctic Ocean chronology confirmed by accelerator 14C dating

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Polar ice evidence that atmospheric CO2 20,000 yr BP was 50% of present

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Direct dating of the oxygen-isotope record of the last deglaciation by 14C accelerator mass spectrometry

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Evidence from Fram Strait (78° N) for early deglaciation

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Rates of Benthic Mixing in Deep-Sea Sediment as Determined by Radioactive Tracers

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Structure of the glacial thermocline at Little Bahama Bank

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10.1029/91PA01768

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(Q107047000)

The Influence of CaCO3Dissolution on Core Top Radiocarbon Ages for Deep-Sea Sediments

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