Physical and chemical properties, 14C ages and palynology of sediment cores from the Western Baltic Sea
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| Format: | Dataset Open Access |
| Sprache: | en |
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PANGAEA
1986
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| _version_ | 1867171363536502784 |
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| author | Winn, Kyaw Averdieck, Fritz-Rudolf Erlenkeuser, Helmut Werner, Friedrich |
| author_facet | Winn, Kyaw Averdieck, Fritz-Rudolf Erlenkeuser, Helmut Werner, Friedrich |
| collection | Datos científicos de ciencias marinas y ambientales |
| contents | Sea level related radiocarbon, palynological and stratigraphical data from sediment cores in the Western Baltic have been tested against the existing sea level curves for the region. The relative sea level rise curves for the beginning of the Holocene show no significant deviations between the Kiel, Mecklenburg und Lübeck Bays and hence do not support the previously reported differences in the averaged regional subsidence rates for this time interval. Local subsidence and upheaval due to salt tectonics probably played a greater role than previously suspected in the region. The sea level possibly stagnated around -28 m during the early Holocene before rising very rapidly to -14 m. The submarine terraces at -30 m and perhaps also at -27 m were formed during the lacustrine phase of the Western Baltic when the water levels were controlled by the main thresholds in the Great Belt. |
| format | Dataset Open Access |
| id | pangaea_https___doi_org_10_1594_PANGAEA_784896 |
| institution | PANGAEA |
| language | en |
| publishDate | 1986 |
| publisher | PANGAEA |
| record_format | pangaea |
| spellingShingle | Physical and chemical properties, 14C ages and palynology of sediment cores from the Western Baltic Sea Winn, Kyaw Averdieck, Fritz-Rudolf Erlenkeuser, Helmut Werner, Friedrich Baltic Sea; Bay of Kiel, Baltic Sea; BC; Boknis Eck; Box corer; Eckernförder Bucht; Falshoeft Channel, Kiel Bay; Fem_E143c; Fern_44b; Fluegge Channel, Kiel Bay; GC; GIK_LS1; GIK00334; GIK02002; GIK02063; GIK10006-1; GIK10012-1; GIK10030-1; GIK10047-1; GIK10051-1; GIK10056-1; GIK10385-1; GIK10511-1; GIK10517-1; GIK10554-1; GIK10860-1; GIK10869-1; GIK10872; GIK11881-1; GIK11882-1; GIK12519-1; GIK12522-2; GIK12773; GIK12886-1; GIK13367; GIK13368; GIK13371; GIK13704-1; GIK13712-1; GIK13949-1; GIK14361-1; GIK14362-1; GIK14363-1; GIK14365-1; GIK14366-1; GIK14367-1; GIK14368-1; GIK14369-1; GIK14849-1; GIK14850-1; GIK14851-1; GIK14852-1; GIK14858-1; GIK15301-1; GIK15304-1; GIK15309-1; GIK15314-1; GIK15324-1; GIK15342-1; GIK15384-1; GIK15386-1; GIK15391-1; GIK15392-1; GIK15393-1; GIK15396-1; GIK15399-1; GIK15496-1; GIK-cruise; Graet Belt Channel (Western Baltic); Gravity corer; Gravity corer (Kiel type); Great Belt, western Baltic Sea, off Denmark; Hermann Wattenberg; KAL15; Kasten corer 15 cm; LI197x; LI198x; Littorina; Mecklenburg Bay; Neustadt-Luebeck Bay; PL3/81; PL4/79; PL69; Planet II (1967-2004); POS40; POS46/2; POS53; POS54; POS79; Poseidon; SL; SW Sagas Bank, Mecklenburg Bay; VC; Vejsnaes Channel, Kiel Bay; Vejsnaes Shoal, Kiel Bay; Vibro corer; WA197x; Wattenburg Channel, Kiel Bay; Western Baltic Sea; WIL197x; William Sea level related radiocarbon, palynological and stratigraphical data from sediment cores in the Western Baltic have been tested against the existing sea level curves for the region. The relative sea level rise curves for the beginning of the Holocene show no significant deviations between the Kiel, Mecklenburg und Lübeck Bays and hence do not support the previously reported differences in the averaged regional subsidence rates for this time interval. Local subsidence and upheaval due to salt tectonics probably played a greater role than previously suspected in the region. The sea level possibly stagnated around -28 m during the early Holocene before rising very rapidly to -14 m. The submarine terraces at -30 m and perhaps also at -27 m were formed during the lacustrine phase of the Western Baltic when the water levels were controlled by the main thresholds in the Great Belt. |
| title | Physical and chemical properties, 14C ages and palynology of sediment cores from the Western Baltic Sea |
| topic | Baltic Sea; Bay of Kiel, Baltic Sea; BC; Boknis Eck; Box corer; Eckernförder Bucht; Falshoeft Channel, Kiel Bay; Fem_E143c; Fern_44b; Fluegge Channel, Kiel Bay; GC; GIK_LS1; GIK00334; GIK02002; GIK02063; GIK10006-1; GIK10012-1; GIK10030-1; GIK10047-1; GIK10051-1; GIK10056-1; GIK10385-1; GIK10511-1; GIK10517-1; GIK10554-1; GIK10860-1; GIK10869-1; GIK10872; GIK11881-1; GIK11882-1; GIK12519-1; GIK12522-2; GIK12773; GIK12886-1; GIK13367; GIK13368; GIK13371; GIK13704-1; GIK13712-1; GIK13949-1; GIK14361-1; GIK14362-1; GIK14363-1; GIK14365-1; GIK14366-1; GIK14367-1; GIK14368-1; GIK14369-1; GIK14849-1; GIK14850-1; GIK14851-1; GIK14852-1; GIK14858-1; GIK15301-1; GIK15304-1; GIK15309-1; GIK15314-1; GIK15324-1; GIK15342-1; GIK15384-1; GIK15386-1; GIK15391-1; GIK15392-1; GIK15393-1; GIK15396-1; GIK15399-1; GIK15496-1; GIK-cruise; Graet Belt Channel (Western Baltic); Gravity corer; Gravity corer (Kiel type); Great Belt, western Baltic Sea, off Denmark; Hermann Wattenberg; KAL15; Kasten corer 15 cm; LI197x; LI198x; Littorina; Mecklenburg Bay; Neustadt-Luebeck Bay; PL3/81; PL4/79; PL69; Planet II (1967-2004); POS40; POS46/2; POS53; POS54; POS79; Poseidon; SL; SW Sagas Bank, Mecklenburg Bay; VC; Vejsnaes Channel, Kiel Bay; Vejsnaes Shoal, Kiel Bay; Vibro corer; WA197x; Wattenburg Channel, Kiel Bay; Western Baltic Sea; WIL197x; William |
| url | https://doi.org/10.1594/PANGAEA.784896 |