Depositional fluxes, palaeoproductivity, and ice rafting in the NE Atlantic over the past 30 ka

Manighetti, B.; McCave, I N

doi:10.1029/94PA03057

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Depositional fluxes, palaeoproductivity, and ice rafting in the NE Atlantic over the past 30 ka

Author(s): B. Manighetti , I. N. McCave

Publication date Created: June 1995

Publication date (Print): June 1995

Journal: Paleoceanography

Publisher: American Geophysical Union (AGU)

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Most cited references 16

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Origin and consequences of cyclic ice rafting in the Northeast Atlantic Ocean during the past 130,000 years

Hartmut Heinrich (1988)

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Productivity, sedimentation rate, and sedimentary organic matter in the oceans—I. Organic carbon preservation

E. Suess, P.J. Müller (1979)

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Modeling Atmospheric 14C Influences and 14C Ages of Marine Samples to 10,000 BC

Thomas F. Braziunas, Minze Stuiver (1993)

The detailed radiocarbon agevs.calibrated (cal) age studies of tree rings reported in this Calibration Issue provide a unique data set for precise14C age calibration of materials formed in isotopic equilibrium with atmospheric CO2. The situation is more complex for organisms formed in other reservoirs, such as lakes and oceans. Here the initial specific14C activity may differ from that of the contemporaneous atmosphere. The measured remaining14C activity of samples formed in such reservoirs not only reflects14C decay (related to sample age) but also the reservoir14C activity. As the measured sample14C activity figures into the calculation of a conventional14C age (Stuiver & Polach 1977), apparent14C age differences occur when contemporaneously grown samples of different reservoirs are dated.