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• W2590017457 abstract "Major and trace elements, minerals, and grain-size were analysed from the early to mid-Holocene (12 to 4 ky BP) period of a sediment core from the Alpine lake Oberer Landschitzsee (ObLAN, 2076 m a.s.l.), which is located on predominantly crystalline bedrock on the southern slopes of the Austrian Central Alps. Geochemistry and mineralogy were compared with diatom-inferred (Di-) ‘date of autumn mixing’ (Amix), DOC, pH, and selected indicator pollen species from the same sediment core. Principal components analysis (PCA) indicated a positive correlation between processes triggered by temperature and precipitation (e.g., lake mixing, DOC). PCA grouped indicators of physical weathering and enhanced catchment run-off (sand, quartz, feldspar), elements of weathering (e.g., Ti, Rb, Mn) under dryer conditions (clay to silt fractions), and elements that probably were related to changes in redox conditions (Cu, Fe, S, Zn). The duration and height of the snow-pack played an important role in this high-alpine environment, affecting weathering, erosion, pH, and lake stratification. Low Alnus viridis pollen abundance, together with markers for increased elements of erosion, indicated extensive snow-pack. Changes in S coupled with As, and elements indicating increased weathering, reflected climate oscillations. LOI was affected by productivity and erosion. High (late) Di–Amix coupled with increased Di-DOC indicated prolonged summers with increased productivity. Cold and wet (snow-rich) phases and subsequent melting caused low pH and a decoupling of the significant linear correlation between sedimentary Ca and Di-pH. Weathering and leaching during climate deteriorations opposed the long-term trend in a loss of cations and forced in-lake alkalinity generation during the following lake warming. Overall, the multi-proxy study indicated complex climate-driven processes within different time-scales (long-term trends, climate oscillations, seasonality). The climate oscillations within 12–5 ky BP corresponded well with the cool and wet phases known from central Europe suggesting a dominant common Atlantic climate impact. When Mediterranean climate established between 5 and 4 ky BP, its influence on the southern slopes of the Alps increased." @default.
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• W2590017457 date "2006-04-01" @default.
• W2590017457 modified "2023-09-24" @default.
• W2590017457 title "Climatic Changes from 12,000 to 4,000 Years Ago in the Austrian Central Alps Tracked by Sedimentological and Biological Proxies of a Lake Sediment Core" @default.
• W2590017457 cites W10257938 @default.
• W2590017457 cites W1494431475 @default.
• W2590017457 cites W1503681152 @default.
• W2590017457 cites W1513473536 @default.
• W2590017457 cites W1532351434 @default.
• W2590017457 cites W1600236695 @default.
• W2590017457 cites W1604853763 @default.
• W2590017457 cites W1618303758 @default.
• W2590017457 cites W1971445289 @default.
• W2590017457 cites W1973846070 @default.
• W2590017457 cites W1974452893 @default.
• W2590017457 cites W1975715178 @default.
• W2590017457 cites W1976727495 @default.
• W2590017457 cites W1978677683 @default.
• W2590017457 cites W1981934382 @default.
• W2590017457 cites W1982878828 @default.
• W2590017457 cites W1988614095 @default.
• W2590017457 cites W1990899433 @default.
• W2590017457 cites W1993712538 @default.
• W2590017457 cites W1997582493 @default.
• W2590017457 cites W1999881354 @default.
• W2590017457 cites W2000444336 @default.
• W2590017457 cites W2001691937 @default.
• W2590017457 cites W2004864414 @default.
• W2590017457 cites W2005498841 @default.
• W2590017457 cites W2008470587 @default.
• W2590017457 cites W2008875043 @default.
• W2590017457 cites W2010889515 @default.
• W2590017457 cites W2016184904 @default.
• W2590017457 cites W2017241772 @default.
• W2590017457 cites W2017977879 @default.
• W2590017457 cites W2022437015 @default.
• W2590017457 cites W2025231098 @default.
• W2590017457 cites W2025742812 @default.
• W2590017457 cites W2027037613 @default.
• W2590017457 cites W2036997678 @default.
• W2590017457 cites W2045554807 @default.
• W2590017457 cites W2056522327 @default.
• W2590017457 cites W2061517952 @default.
• W2590017457 cites W2070735656 @default.
• W2590017457 cites W2071311147 @default.
• W2590017457 cites W2072732165 @default.
• W2590017457 cites W2076814911 @default.
• W2590017457 cites W2084428435 @default.
• W2590017457 cites W2084850065 @default.
• W2590017457 cites W2091416174 @default.
• W2590017457 cites W2092519422 @default.
• W2590017457 cites W2093426121 @default.
• W2590017457 cites W2094251003 @default.
• W2590017457 cites W2100512609 @default.
• W2590017457 cites W2102023541 @default.
• W2590017457 cites W2103737089 @default.
• W2590017457 cites W2106996339 @default.
• W2590017457 cites W2112434101 @default.
• W2590017457 cites W2115198043 @default.
• W2590017457 cites W2116629615 @default.
• W2590017457 cites W2124137575 @default.
• W2590017457 cites W2127038511 @default.
• W2590017457 cites W2130213531 @default.
• W2590017457 cites W2133471115 @default.
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• W2590017457 cites W2148596338 @default.
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• W2590017457 cites W2490945171 @default.
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• W2590017457 doi "https://doi.org/10.1007/s10933-005-2351-2" @default.
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