(Table 1) Age determination of sediment core PS1795-2 ...

C14 ages measured on planktonic foraminifera Neogloboquadrina pachyderma shells at the ETH laboratory of Ion Beam Physics in Zuric. C14 age (BP)--delta C13 corrected radiocarbon age based on concentration of 14C measured in sample. BP= Before Present (before 1950 AD). Calibrated C14 ages (Calendar t...

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Bibliographic Details
Main Authors: Sprenk, Daniela, Weber, Michael E, Kuhn, Gerhard, Wennrich, Volker, Hartmann, Thomas, Seelos, Klemens
Format: Dataset
Language:English
Published: PANGAEA 2014
Subjects:
Laboratory code/label
Depth, top/min
Depth, bottom/max
DEPTH, sediment/rock
Age, dated
Age, error
Reservoir effect/correction
Reservoir effect/correction, standard deviation
Calendar age
Calendar age, standard error
Age, minimum/young
Age, maximum/old
Probability
Sample mass
Sample comment
Gravity corer Kiel type
Age, 14C AMS
Age, reservoir corrected Bard, 1988
Age, 14C calibrated
ANT-VIII/5
Polarstern
Paleoenvironmental Reconstructions from Marine Sediments @ AWI AWI_Paleo
Reimer
Neogloboquadrina pachyderma
Planktonic foraminifera
Online Access:https://dx.doi.org/10.1594/pangaea.833417
https://doi.pangaea.de/10.1594/PANGAEA.833417
Description
Summary:C14 ages measured on planktonic foraminifera Neogloboquadrina pachyderma shells at the ETH laboratory of Ion Beam Physics in Zuric. C14 age (BP)--delta C13 corrected radiocarbon age based on concentration of 14C measured in sample. BP= Before Present (before 1950 AD). Calibrated C14 ages (Calendar time intervals) using Clam 2.1, Clam 2.1 (Blaauw, 2010) and the Marine09 calibration curve (Reimer et al., 2011) were used to calculate calendar years before present (cal yr BP). ...

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