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author Hepp, Daniel A
De Pol-Holz, Ricardo
author_facet Hepp, Daniel A
De Pol-Holz, Ricardo
collection Datos científicos de ciencias marinas y ambientales
contents Hand‐picked plant macrofossils (peat or plant remains) or marine calcareous fossils (mainly foraminifera and shell valves or their fragments) from 23 samples, as well as one wellpreserved but possibly reworked shell valve were dated using accelerator mass spectrometry 14C dating. Radiocarbon ages of samples from core GeoB17721‐1 were determined at the Poznań Radiocarbon Laboratory (Poznań, Poland), whereas radiocarbon ages from peat layers or layers of decayed organic matter in cores 09‐x were determined at the W. M. Keck Carbon Cycle Accelerator Mass Spectrometry Laboratory (University of California, Irvine) (see Table 1 for details). All radiocarbon dates were converted to calendar ages using the CALIB 7.0 program (Stuiver and Reimer, 1993; http://calib. org). The reservoir effect of the marine samples was corrected with ΔR values provided by Scourse et al. (2012) for the German Bight (mean ΔR = 83), with the restriction that the ΔR values were determined on post‐industrial samples.
format Dataset Open Access
id pangaea_https___doi_org_10_1594_PANGAEA_907453
institution PANGAEA
language en
publishDate 2019
publisher PANGAEA
record_format pangaea
spellingShingle Radiocarbon datings of sediments from the Paleo-Ems valley
Hepp, Daniel A
De Pol-Holz, Ricardo
Age, 14C AMS; Age, dated; Age, dated, standard deviation; Age, dated material; Analytical method; Calendar age; Calendar age, maximum/old; Calendar age, minimum/young; Core_09-1; Core_09-2; Core_09-3; Core_09-5; Core_09-6; Core_09-7; Core 09-1; Core 09-2; Core 09-3; Core 09-5; Core 09-6; Core 09-7; Depth, bottom/max; DEPTH, sediment/rock; Depth, top/min; Event label; GeoB17718-3; GeoB17721-1; HE405; HE405/38-1; HE405/44-1; Heincke; Laboratory code/label; North Sea; Optional event label; Radiocarbon dating; SEDCO; Sediment corer; VC; Vibro corer
Hand‐picked plant macrofossils (peat or plant remains) or marine calcareous fossils (mainly foraminifera and shell valves or their fragments) from 23 samples, as well as one wellpreserved but possibly reworked shell valve were dated using accelerator mass spectrometry 14C dating. Radiocarbon ages of samples from core GeoB17721‐1 were determined at the Poznań Radiocarbon Laboratory (Poznań, Poland), whereas radiocarbon ages from peat layers or layers of decayed organic matter in cores 09‐x were determined at the W. M. Keck Carbon Cycle Accelerator Mass Spectrometry Laboratory (University of California, Irvine) (see Table 1 for details). All radiocarbon dates were converted to calendar ages using the CALIB 7.0 program (Stuiver and Reimer, 1993; http://calib. org). The reservoir effect of the marine samples was corrected with ΔR values provided by Scourse et al. (2012) for the German Bight (mean ΔR = 83), with the restriction that the ΔR values were determined on post‐industrial samples.
title Radiocarbon datings of sediments from the Paleo-Ems valley
topic Age, 14C AMS; Age, dated; Age, dated, standard deviation; Age, dated material; Analytical method; Calendar age; Calendar age, maximum/old; Calendar age, minimum/young; Core_09-1; Core_09-2; Core_09-3; Core_09-5; Core_09-6; Core_09-7; Core 09-1; Core 09-2; Core 09-3; Core 09-5; Core 09-6; Core 09-7; Depth, bottom/max; DEPTH, sediment/rock; Depth, top/min; Event label; GeoB17718-3; GeoB17721-1; HE405; HE405/38-1; HE405/44-1; Heincke; Laboratory code/label; North Sea; Optional event label; Radiocarbon dating; SEDCO; Sediment corer; VC; Vibro corer
url https://doi.org/10.1594/PANGAEA.907453