Age determination of sediment core HZM, lake Holzmar (Tables 1, 2)

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Hauptverfasser: Hajdas, Irena, Zolitschka, Bernd, Ivy-Ochs, Susan D, Beer, Jürg, Bonani, Georges, Leroy, Suzanne A G, Negendank, Jörg F W, Ramrath, Matthias, Suter, Martin
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Sprache:en
Veröffentlicht: PANGAEA 1995
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author Hajdas, Irena
Zolitschka, Bernd
Ivy-Ochs, Susan D
Beer, Jürg
Bonani, Georges
Leroy, Suzanne A G
Negendank, Jörg F W
Ramrath, Matthias
Suter, Martin
author_facet Hajdas, Irena
Zolitschka, Bernd
Ivy-Ochs, Susan D
Beer, Jürg
Bonani, Georges
Leroy, Suzanne A G
Negendank, Jörg F W
Ramrath, Matthias
Suter, Martin
collection Datos científicos de ciencias marinas y ambientales
contents AMS radiocarbon ages have been determined on terrestrial macrofossils selected from the annually laminated sediments of lake Holzmaar (Germany). The radiocarbon chronology of this lake covers the last 12.6 ka. Comparison of the radiocarbon dated varve chronology with tree ring data shows that an additional 878 years have to be added to the varve chronology. The corrected 14C varve chronology of Holzmaar reaches back to ca. 13.8 ka cal. BP and compares favourably with the results from Soppensee (Switzerland) (Hajdas et al., 1993, doi:10.1007/BF00209748). The corrected ages for the onset and the end of the Younger Dryas biozone are 11,940 cal. BP and 11,490 cal. BP, respectively. The ash layer of the Laacher See volcanic eruption is dated at 12,201 ± 224 cal. BP and the Ulmener Tephra layer is dated at 10,904 cal. BP.
format Dataset Open Access
id pangaea_https___doi_org_10_1594_PANGAEA_734887
institution PANGAEA
language en
publishDate 1995
publisher PANGAEA
record_format pangaea
spellingShingle Age determination of sediment core HZM, lake Holzmar (Tables 1, 2)
Hajdas, Irena
Zolitschka, Bernd
Ivy-Ochs, Susan D
Beer, Jürg
Bonani, Georges
Leroy, Suzanne A G
Negendank, Jörg F W
Ramrath, Matthias
Suter, Martin
Age, 14C calibrated, CALIB (Stuiver & Polach, 1977); Age, dated; Age, dated, standard deviation; Age model, varve counting; Changes in the Geo-Biosphere during the last 15000 years; COMPCORE; Composite Core; DEPTH, sediment/rock; GeoBio15k; Holzmaar; HZM; Isotope ratio mass spectrometry; Mass; Sample code/label; Sample code/label 2; Sampling/drilling in lake; δ13C, organic carbon; δ13C, standard deviation
AMS radiocarbon ages have been determined on terrestrial macrofossils selected from the annually laminated sediments of lake Holzmaar (Germany). The radiocarbon chronology of this lake covers the last 12.6 ka. Comparison of the radiocarbon dated varve chronology with tree ring data shows that an additional 878 years have to be added to the varve chronology. The corrected 14C varve chronology of Holzmaar reaches back to ca. 13.8 ka cal. BP and compares favourably with the results from Soppensee (Switzerland) (Hajdas et al., 1993, doi:10.1007/BF00209748). The corrected ages for the onset and the end of the Younger Dryas biozone are 11,940 cal. BP and 11,490 cal. BP, respectively. The ash layer of the Laacher See volcanic eruption is dated at 12,201 ± 224 cal. BP and the Ulmener Tephra layer is dated at 10,904 cal. BP.
title Age determination of sediment core HZM, lake Holzmar (Tables 1, 2)
topic Age, 14C calibrated, CALIB (Stuiver & Polach, 1977); Age, dated; Age, dated, standard deviation; Age model, varve counting; Changes in the Geo-Biosphere during the last 15000 years; COMPCORE; Composite Core; DEPTH, sediment/rock; GeoBio15k; Holzmaar; HZM; Isotope ratio mass spectrometry; Mass; Sample code/label; Sample code/label 2; Sampling/drilling in lake; δ13C, organic carbon; δ13C, standard deviation
url https://doi.org/10.1594/PANGAEA.734887