SPECTROMETRY 14C AGES MEASURED IN PLANKTONIC FORAMINIFERA: PALEOCEANOGRAPHIC IMPLICATIONS - Archive ouverte HAL Accéder directement au contenu
Article Dans Une Revue Paleoceanography Année : 1988

SPECTROMETRY 14C AGES MEASURED IN PLANKTONIC FORAMINIFERA: PALEOCEANOGRAPHIC IMPLICATIONS

Résumé

Carbon 14 dates obtained by accelerator mass spectrometry (AMS) on foraminiferal samples from deep-sea sediment cores must be corrected for the difference in 14C composition between the atmosphere and the sea surface. In the modem ocean, the "apparent age" of carbonate shells formed in surface waters varies between 300 and 1200 years and depends mainly on latitude. The time variation of this parameter during climate oscillations of the last 40,000 years may have been significant: there should have been small changes for most of the ocean between 40øS and 40øN, but an increase of the apparent age by several hundred years should be expected at high latitudes in response to subpolar/subtropical front movements. The North Atlantic is likely to have experienced the most significant changes, due to large variations in the mode and rate of North Atlantic Deep Water production. These hypothetical changes may be measured by coupled AMS 14C dating of contemporaneous planktonic foraminifera and terrestrial organic matter (pollen, charcoal, wood, etc.) which occur in the same core or are stratigraphically linked by the same volcanic ash layer. The A(14C atmosphere, 14C sea surface) can be viewed as a new paleoceanographic tracer which may provide additional information about high latitude surface waters complementary to those obtained with 13C/12C and Cd/Ca ratios measured in planktonic foraminifera.
Fichier principal
Vignette du fichier
Paleoceanography - December 1988 - Bard - Correction of accelerator mass spectrometry 14C ages measured in planktonic.pdf (888.8 Ko) Télécharger le fichier
Origine : Fichiers éditeurs autorisés sur une archive ouverte

Dates et versions

hal-03549486 , version 1 (31-01-2022)

Identifiants

Citer

Edouard Bard. SPECTROMETRY 14C AGES MEASURED IN PLANKTONIC FORAMINIFERA: PALEOCEANOGRAPHIC IMPLICATIONS. Paleoceanography, 1988, 3 (6), pp.635-645. ⟨10.1029/PA003i006p00635⟩. ⟨hal-03549486⟩

Collections

CEA CNRS CDF
21 Consultations
102 Téléchargements

Altmetric

Partager

Gmail Facebook X LinkedIn More