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Titlebook: Lake Systems from the Ice Age to Industrial Time; Milan Beres,Maren Scheidhauer,François Marillier Book 2003 Birkhäuser Verlag, Basel 2003

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Milan Beres,Maren Scheidhauer,Franç Marillieral construct of deviant sexual arousal has, up till recently, held sway over competing etiological accounts such that it has contributed to the development of a number of unimodal theories which leave little room for additional explanatory constructs (Abel, Barlow, Blanchard, & Guild, 1977). As the
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A 600-year sedimentary record of flood events from two sub-alpine lakes (Schwendiseen, Northeasternccurred on June 14, 1910 is observed in the sedimentary record as the thickest detrital horizon. These short-lived climatic events archived in the sediments of both lakes are superimposed on a longer-term environmental trend characterized by fluctuating conditions in organic productivity. The format
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60 years of glaciolacustrine sedimentation in Steinsee (Sustenpass, Switzerland) compared with histverlain by a about 0.5 m thick graded unit deposited during a catastrophic lake outburst. The uppermost halves of the cores are characterized by very fine laminae of sand to silty clay. Cs-137 dating of these deposits confirmed the annual character of the laminae that are, therefore, true glacial va
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Evolution des assemblages de Chironomidae (Insecta: Diptera) pendant le Tardiglaciaire dans le Lac ervals correspond to the Older Dryas and the Intra Allerød Cold Phase (I.A.C.P.). The beginning of the Younger Dryas is shown by a strong and rapid change in chironomid assemblages. The pelagic primary production appeared much reduced whereas the benthic production was rather favored. The progressiv
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,Les conditions d’établissement et de conservation des sites préhistoriques littoraux de la rive sudthic sites farther from the coast line are not affected by recent erosion. On the contrary, other sites, those protected until 19. century, were destroyed at the level of the present coastline, so that almost all architectural vestiges and all archeological strata have disappeared in the lake. Becau
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