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Comparison between radiocarbon ages obtained on coexisting planktonic foraminifera

Data up to Jan 2025

Published1988
Citations62
References16

Total Citations Per Year

Abstract

References (16)

Vertical distribution and isotopic fractionation of living planktonic foraminifera from the Panama Basin

1982 • 693 citations

The chronology of the last Deglaciation: Implications to the cause of the Younger Dryas Event

1988 • 418 citations

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

1979 • 211 citations

Reconstruction of the last deglaciation: deconvolved records of ?18O profiles, micropaleontological variations and accelerator mass spectrometric14C dating

1987 • 183 citations

Radiocarbon measurements on coexisting benthic and planktic foraminifera shells: potential for reconstructing ocean ventilation times over the past 20 000 years

1984 • 110 citations

Precision measurements of 14C in AMS — some results and prospects

1984 • 78 citations

New evidence from the South China Sea for an abrupt termination of the last glacial period

1988 • 77 citations

The impacts of bioturbation on the age difference between benthic and planktonic foraminifera in deep sea sediments

1984 • 74 citations

Limits on the ventilation rate for the deep ocean over the last 12000 years

1986 • 62 citations

Introduction

1988 • 45 citations

Can the Greenland Climatic Jumps be Identified in Records from Ocean and Land?

1988 • 40 citations

Ocean ventilation during the last 12,000 years: Hypothesis of counterpoint deep water production

1987 • 28 citations

14C measurements on foraminifera of deep sea core V28-238 and their preliminary interpretation

1984 • 26 citations

Target preparation for milligram sized 14C samples and data evaluation for AMS measurements

1984 • 23 citations

The Impact of Bioturbation on Ams 14C Dates On Handpicked Foraminifera: A Statistical Model

1987 • 14 citations

Accelerator Radiocarbon Ages on Foraminifera Separated from Deep-Sea Sediments

2011 • 11 citations

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