The Baltic Sea as a model system for studying postglacial colonization and ecological differentiation, exemplified by the red alga Ceramium tenuicorne

2002 ◽  
Vol 11 (10) ◽  
pp. 2083-2095 ◽  
Author(s):  
T. M. Gabrielsen ◽  
C. Brochmann ◽  
J. Rueness
2017 ◽  
Vol 60 (2) ◽  
Author(s):  
Priit Kersen ◽  
Tiina Paalme ◽  
Liina Pajusalu ◽  
Georg Martin

AbstractThere is a growing need for diversification of seaweed aquaculture practices in Europe. In the Baltic Sea, very few seaweed species are utilised commercially, and only the kelp


2005 ◽  
Vol 62 (8) ◽  
pp. 1887-1904 ◽  
Author(s):  
Marjatta Säisä ◽  
Marja-Liisa Koljonen ◽  
Riho Gross ◽  
Jan Nilsson ◽  
Jaana Tähtinen ◽  
...  

The genetic structure and phylogeography of Atlantic salmon (Salmo salar) across the Baltic Sea basin and neighbouring areas (eastern Atlantic Ocean, North Sea, Barents Sea, White Sea, and two Russian lakes, Onega and Ladoga) were studied to resolve the partly contradictory hypotheses of the species' postglacial colonization history. Thirty-eight populations (total of 2180 individuals) were studied for nine DNA microsatellite loci. Within the Baltic Sea, the anadromous populations formed three clear groups, corresponding to the northern (Gulf of Bothnia), eastern (Gulf of Finland and eastern Baltic Main Basin), and southern regions (western Baltic Main Basin). The genetic differences among these three groups were clearly greater (GGB 5.6%; GGB being the proportion of diversity components between regions within basins) than were those among population groups in the eastern Atlantic Ocean (GGB 2.2%) from Ireland to the White Sea. The isolation-by-distance model explained part of the differentiation within, but not between, the regions. The results strongly indicate colonization of the Baltic Sea by at least three glacial lineages. Potential refugium areas for each lineage are proposed.


2005 ◽  
Vol 36 (4-5) ◽  
pp. 397-409 ◽  
Author(s):  
Erik Kjellström ◽  
Ralf Döscher ◽  
H.E. Markus Meier

A climate change experiment with a fully coupled high resolution regional atmosphere–ocean model for the Baltic Sea is compared to an experiment with a stand-alone regional atmospheric model. Both experiments simulate 30-yr periods with boundary data from the same global climate model system. This particular global model system simulates very high sea surface temperatures during summer for the Baltic Sea at the end of this century under the investigated emission scenario. We show that the sea surface temperatures are less warm in the coupled regional model compared to the global model system and that this difference is dependent on the atmospheric circulation. In summers with a high NAO index and thereby relatively strong westerly flow over the North Atlantic the differences between the two models are small, while in summers with a weaker, more northerly flow over the Baltic Sea the differences are very large. The higher sea surface temperatures in the uncoupled experiment lead to an intensified hydrological cycle over the Baltic Sea, with more than 30% additional precipitation in summer taken as an average over the full 30-yr period and over the entire Baltic Sea. The differences are mostly local, over the sea, but there are differences in surrounding land areas.


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