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- W1609451726 abstract "Two metres of sediments were recovered from the Lac du Bouchet (Massif Central, France) to assess the influence of climatic changes on organic lacustrine sedimentation. Palaeoenvironmental reconstruction was realised on the basis of a quantitative evaluation of the different mineral and organic fluxes. The late glacial period is marked by high mineral and low organic fluxes. The transition to the Holocene is mainly characterised by an increased flux of organic components (terrestrial biomass and phytoplankton) and a relative decrease in the mineral fluxes. The respective evolution of phytoplanktonic and terrestrial higher-plant fluxes reflects the local palaeoenvironmental variations concerning both the sedimentation and surrounding basin. The end of the Atlantic period shows a climatic cooling and the transition from Sub-Boreal to Sub-Atlantic underlines the installation of present climatic conditions. Anthropogenic influence is visible from the middle of the Sub-Atlantic. The regional palaeoenvironmental variations are also recorded in other European sites (SchalkenMehrener Maar, Lago di Monticchio), although slight differences occur due to local effects related to the geomorphology of the basins. This palaeoclimatic evolution parallels global climatic changes as recorded by the recognition of similar major trends in tropical sites (Carajas, Amazonia).Key wordsLac du Bouchetorganic fluxespalynofaciesimage analysispalaeoenvironmentLate Quaternary" @default.
- W1609451726 created "2016-06-24" @default.
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- W1609451726 date "1995-01-01" @default.
- W1609451726 modified "2023-09-26" @default.
- W1609451726 title "Organic sedimentation and its relationship with palaeoenvironmental changes over the last 30,000 years (Lac du Bouchet, Haute Loire, France). Comparison with other palaeoclimatic lacustrine examples" @default.
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- W1609451726 doi "https://doi.org/10.1007/bfb0117672" @default.
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