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| Main Authors: | , , , , , , |
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| Format: | Dataset Open Access |
| Language: | en |
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PANGAEA
2012
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| Online Access: | https://doi.org/10.1594/PANGAEA.778835 |
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| _version_ | 1867168104376696832 |
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| 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 |
| collection | Datos científicos de ciencias marinas y ambientales |
| contents | 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 Open Access |
| id | pangaea_https___doi_org_10_1594_PANGAEA_778835 |
| institution | PANGAEA |
| language | en |
| publishDate | 2012 |
| publisher | PANGAEA |
| record_format | pangaea |
| spellingShingle | 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 Age; Age, 14C AMS; Age, comment; Age, dated; Age, dated, standard deviation; Age, error; Comment; Facies name/code; Sample code/label; Site; wismarbay; Wismar Bay, Baltic Sea, Germany; δ13C 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. |
| title | Table 1 : AMS-14C data used for the reconstruction of the Wismar Bay shoreline displacement curve |
| topic | Age; Age, 14C AMS; Age, comment; Age, dated; Age, dated, standard deviation; Age, error; Comment; Facies name/code; Sample code/label; Site; wismarbay; Wismar Bay, Baltic Sea, Germany; δ13C |
| url | https://doi.org/10.1594/PANGAEA.778835 |