Table 1 : AMS-14C data used for the reconstruction of the Wismar Bay shoreline displacement curve
The Baltic coast of Mecklenburg-Vorpommern is located in the transition Zone between the region of Fennoscandian Uplift and the Central European Depression. In relation to the eustatic sea-level rise, the northeast coast shows a slower inundation, while for the southwestern area a faster transgressi...
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ftpangaea:oai:pangaea.de:doi:10.1594/PANGAEA.778835 2023-05-15T16:13:03+02:00 Table 1 : AMS-14C data used for the reconstruction of the Wismar Bay shoreline displacement curve Lampe, Reinhard Endtmann, Elisabeth Janke, Wolfgang Meyer, Hinrich Lübke, Harald Harff, Jan Lemke, Wolfram LATITUDE: 54.000000 * LONGITUDE: 11.500000 2012-04-05 text/tab-separated-values, 1012 data points https://doi.pangaea.de/10.1594/PANGAEA.778835 https://doi.org/10.1594/PANGAEA.778835 en eng PANGAEA https://doi.pangaea.de/10.1594/PANGAEA.778835 https://doi.org/10.1594/PANGAEA.778835 CC-BY-3.0: Creative Commons Attribution 3.0 Unported Access constraints: unrestricted info:eu-repo/semantics/openAccess CC-BY Supplement to: Lampe, Reinhard; Endtmann, Elisabeth; Janke, Wolfgang; Meyer, Hinrich; Lübke, Harald; Harff, Jan; Lemke, Wolfram (2005): A new relative sea-level curve for the Wismar Bay, N-German Baltic coast. Meyniana, 57, 5-35, https://doi.org/10.2312/meyniana.2005.57.5 Age 14C AMS comment dated dated standard deviation error Facies name/code Sample code/label Site wismarbay Wismar Bay Baltic Sea Germany δ13C Dataset 2012 ftpangaea https://doi.org/10.1594/PANGAEA.778835 https://doi.org/10.2312/meyniana.2005.57.5 2023-01-20T08:53:46Z The Baltic coast of Mecklenburg-Vorpommern is located in the transition Zone between the region of Fennoscandian Uplift and the Central European Depression. In relation to the eustatic sea-level rise, the northeast coast shows a slower inundation, while for the southwestern area a faster transgression is indicated, which can be attributed to crustal movements. To determine the spatial and temporal differences since the onset of the Littorina Transgression, three relative sea-level curves have been established along a transect parallel to the gradient of upliftlsubsidence. The Wismar Bay area is one endpoint of the transect demonstrating today 10 Abb., 2 Tab. a relative sea-level rise of 1.4 mm/a. To determine the relative sea-level curve for the Wismar Bay, two sites were investigated on Rustwerder Spit (Poel) and Redentin. They provided reliable depth-age data, while the stratigraphy was additionally supported by lithological/geochemical, pollen, diatom and macrofossil data. Additional evidence was provided by archaeological submarine surveys and excavations. Comparing the new relative sea-level curve with a curve from the Vorpommern coast, it can be shown that for the period from 4000 cal BC until present, the differences between the two curves are caused by a constant neotectonic movement, while for the older periods an increasing isostatic component must be taken into account. Dataset Fennoscandian PANGAEA - Data Publisher for Earth & Environmental Science ENVELOPE(11.500000,11.500000,54.000000,54.000000) |
institution |
Open Polar |
collection |
PANGAEA - Data Publisher for Earth & Environmental Science |
op_collection_id |
ftpangaea |
language |
English |
topic |
Age 14C AMS comment dated dated standard deviation error Facies name/code Sample code/label Site wismarbay Wismar Bay Baltic Sea Germany δ13C |
spellingShingle |
Age 14C AMS comment dated dated standard deviation error Facies name/code Sample code/label Site wismarbay Wismar Bay Baltic Sea Germany δ13C Lampe, Reinhard Endtmann, Elisabeth Janke, Wolfgang Meyer, Hinrich Lübke, Harald Harff, Jan Lemke, Wolfram Table 1 : AMS-14C data used for the reconstruction of the Wismar Bay shoreline displacement curve |
topic_facet |
Age 14C AMS comment dated dated standard deviation error Facies name/code Sample code/label Site wismarbay Wismar Bay Baltic Sea Germany δ13C |
description |
The Baltic coast of Mecklenburg-Vorpommern is located in the transition Zone between the region of Fennoscandian Uplift and the Central European Depression. In relation to the eustatic sea-level rise, the northeast coast shows a slower inundation, while for the southwestern area a faster transgression is indicated, which can be attributed to crustal movements. To determine the spatial and temporal differences since the onset of the Littorina Transgression, three relative sea-level curves have been established along a transect parallel to the gradient of upliftlsubsidence. The Wismar Bay area is one endpoint of the transect demonstrating today 10 Abb., 2 Tab. a relative sea-level rise of 1.4 mm/a. To determine the relative sea-level curve for the Wismar Bay, two sites were investigated on Rustwerder Spit (Poel) and Redentin. They provided reliable depth-age data, while the stratigraphy was additionally supported by lithological/geochemical, pollen, diatom and macrofossil data. Additional evidence was provided by archaeological submarine surveys and excavations. Comparing the new relative sea-level curve with a curve from the Vorpommern coast, it can be shown that for the period from 4000 cal BC until present, the differences between the two curves are caused by a constant neotectonic movement, while for the older periods an increasing isostatic component must be taken into account. |
format |
Dataset |
author |
Lampe, Reinhard Endtmann, Elisabeth Janke, Wolfgang Meyer, Hinrich Lübke, Harald Harff, Jan Lemke, Wolfram |
author_facet |
Lampe, Reinhard Endtmann, Elisabeth Janke, Wolfgang Meyer, Hinrich Lübke, Harald Harff, Jan Lemke, Wolfram |
author_sort |
Lampe, Reinhard |
title |
Table 1 : AMS-14C data used for the reconstruction of the Wismar Bay shoreline displacement curve |
title_short |
Table 1 : AMS-14C data used for the reconstruction of the Wismar Bay shoreline displacement curve |
title_full |
Table 1 : AMS-14C data used for the reconstruction of the Wismar Bay shoreline displacement curve |
title_fullStr |
Table 1 : AMS-14C data used for the reconstruction of the Wismar Bay shoreline displacement curve |
title_full_unstemmed |
Table 1 : AMS-14C data used for the reconstruction of the Wismar Bay shoreline displacement curve |
title_sort |
table 1 : ams-14c data used for the reconstruction of the wismar bay shoreline displacement curve |
publisher |
PANGAEA |
publishDate |
2012 |
url |
https://doi.pangaea.de/10.1594/PANGAEA.778835 https://doi.org/10.1594/PANGAEA.778835 |
op_coverage |
LATITUDE: 54.000000 * LONGITUDE: 11.500000 |
long_lat |
ENVELOPE(11.500000,11.500000,54.000000,54.000000) |
genre |
Fennoscandian |
genre_facet |
Fennoscandian |
op_source |
Supplement to: Lampe, Reinhard; Endtmann, Elisabeth; Janke, Wolfgang; Meyer, Hinrich; Lübke, Harald; Harff, Jan; Lemke, Wolfram (2005): A new relative sea-level curve for the Wismar Bay, N-German Baltic coast. Meyniana, 57, 5-35, https://doi.org/10.2312/meyniana.2005.57.5 |
op_relation |
https://doi.pangaea.de/10.1594/PANGAEA.778835 https://doi.org/10.1594/PANGAEA.778835 |
op_rights |
CC-BY-3.0: Creative Commons Attribution 3.0 Unported Access constraints: unrestricted info:eu-repo/semantics/openAccess |
op_rightsnorm |
CC-BY |
op_doi |
https://doi.org/10.1594/PANGAEA.778835 https://doi.org/10.2312/meyniana.2005.57.5 |
_version_ |
1765998658222817280 |