Late Glacial to Holocene coastal changes of SE Rügen Island (Baltic Sea, NE Germany)

2005 ◽  
Vol 67 (2) ◽  
pp. 132-141 ◽  
Author(s):  
Gösta Hoffmann ◽  
Jens Barnasch
Keyword(s):  
Baltic Sea ◽  
Late Glacial ◽  
Ne Germany ◽  
Coastal Changes

Late-glacial and post-glacial deposition in a large, low relief, epicontinental basin: the northern Baltic Sea

Sedimentology ◽  
2007 ◽  
Vol 54 (6) ◽  
pp. 1323-1344 ◽  
Author(s):  
JOONAS J. VIRTASALO ◽  
AARNO T. KOTILAINEN ◽  
MATTI E. RÄSÄNEN ◽  
ANTTI E. K. OJALA
Keyword(s):  
Baltic Sea ◽  
Late Glacial

Stages of the Baltic Sea evolution in the geochemical record and radiocarbon dating of sediment cores from the Arkona Basin

2014 ◽  
Vol 43 (3) ◽  
Author(s):  
Robert Kostecki
Keyword(s):  
Baltic Sea ◽  
Environmental Changes ◽  
Sediment Cores ◽  
Late Glacial ◽  
Sudden Increase ◽  
The Baltic Sea ◽  
Geochemical Composition ◽  
Arkona Basin ◽  
The Baltic ◽  
Ancylus Lake

AbstractFour sediment cores from the southern part of the Arkona Basin were analyzed in terms of their geochemical composition, age and stratigraphy. The main stages of the Baltic Sea: the Baltic Ice Lake, the Ancylus Lake and the Littorina Sea were identified in all the analyzed cores. The data confirmed the high water fluctuation and significant environmental changes during the Baltic Sea evolution in the Late-Glacial and the Holocene. The signs of the second regression of the Baltic Ice Lake, dated at around 11 000 cal BP, were identified at a depth of 24 m b.s.l. Regression of the Ancylus Lake, dated at 9300 cal BP, was identified at a depth of 23 m b.s.l. The most pronounced period was the transition stage between the Ancylus Lake and the Littorina Sea. The record of the Littorina Sea onset in the sediments of the Arkona Basin is marked as a sudden increase in loss on ignition, biogenic silica, magnesium, calcium, iron and strontium. The age of the Littorina Sea in the Arkona Basin was estimated as younger than 8200 cal BP.

Fault system evolution in the Baltic Sea area west of Rügen, NE Germany

2018 ◽  
Vol 469 (1) ◽  
pp. 83-98 ◽  
Author(s):  
André Deutschmann ◽  
Martin Meschede ◽  
Karsten Obst
Keyword(s):  
Baltic Sea ◽  
Fault System ◽  
The Baltic Sea ◽  
System Evolution ◽  
Ne Germany ◽  
The Baltic ◽  
Sea Area

scholarly journals Methane distribution in Holocene marine sediments in the Bornholm Basin, southern Scandinavia

1969 ◽  
Vol 26 ◽  
pp. 21-24 ◽  
Author(s):  
Jørn Bo Jensen ◽  
Rudolf Endler
Keyword(s):  
Baltic Sea ◽  
Marine Sediments ◽  
Sustainable Use ◽  
Late Glacial ◽  
Scientific Basis ◽  
Geological Mapping ◽  
The Baltic Sea ◽  
Methane Cycle ◽  
The North ◽  
The Baltic

The Baltic Sea is an ideal natural laboratory to study the methane cycle in the framework of diagenetic processes. In this paper we present preliminary geological mapping results from project Baltic Gas, a research project with the overall aim to contribute to the development of a scientific basis for long term sustainable use and protection of the Baltic Sea ecosystem. The Baltic Sea is a marginal sea with a strong permanent haline stratification, which leads to oxygen-poor bottom waters, and which is sometimes interrupted by oxygen- rich saltwater flowing in from the North Sea. The history of the Baltic Sea has resulted in deposition of organic-rich Holocene marine sediments that overlie glacial, late-glacial and early Holocene organic-poor sediments.

scholarly journals Holocene biogenic sediments of the Curonian Spit (south-eastern Baltic Sea coast)

Baltica ◽  
2015 ◽  
Vol 28 (1) ◽  
pp. 41-50 ◽  
Author(s):  
Alexander Sergeev ◽  
Vadim Sivkov ◽  
Vladimir Zhamoida ◽  
Daria Ryabchuk ◽  
Albertas Bitinas ◽  
...  
Keyword(s):  
Baltic Sea ◽  
Coastal Erosion ◽  
Radiocarbon Dating ◽  
Late Glacial ◽  
Curonian Spit ◽  
Geological Evolution ◽  
Protection Potential ◽  
Late Glacial And Holocene ◽  
Sea Coast ◽  
Eastern Baltic

This article is devoted to the results of study of organic rich sediments of the Curonian Spit marine coast. Radiocarbon dating of relict tree stumps, as well as buried peat and palaeosols, found in the Russian part of the Curonian Spit (around the villages of Lesnoy and Rybachy) and in the vicinity of Zelenogradsk indicate the formation of these sediments during the large age scale since 7300 by 300 cal. BP and represent different stages of the Curonian Spit formation in Holocene. Organic rich sediments are objects of interest in terms of environmental protection, potential accumulators of oil (or its products) pollution, indicators of intensity of coastal erosion, also they play a suitable role for the understanding and reconstruction of the geological evolution of the whole Curonian Spit and Lagoon during the Late Glacial and Holocene.

scholarly journals Late-glacial and Holocene palaeoenvironments in the Baltic Sea based on a sedimentary record from the Gda´n%%KERN_ERR%%sk Basin

2011 ◽  
Vol 48 (1) ◽  
pp. 13-21 ◽  
Author(s):  
A Grigoriev ◽  
V Zhamoida ◽  
M Spiridonov ◽  
A Sharapova ◽  
V Sivkov ◽  
...  
Keyword(s):  
Baltic Sea ◽  
Late Glacial ◽  
The Baltic Sea ◽  
Sedimentary Record ◽  
The Baltic ◽  
Late Glacial And Holocene
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