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- W2916451831 abstract "Lake Ladoga in northwestern Russia is Europe's largest lake. The postglacial history of the Ladoga basin is for the first time documented continuously with high temporal resolution in the upper 13.3 m of a sediment core (Co1309) from the northwestern part of the lake. We applied a multiproxy approach including radiographic imaging, (bio‐)geochemical and granulometric analyses. Age control was established combining radiocarbon dating with varve chronology, the latter anchored to a correlated radiocarbon age from a lake close by. The age‐depth model reveals the onset of glacial varve sedimentation at 13 910±140 cal. a BP , when Lake Ladoga was part of the Baltic Ice Lake. Linear extrapolation of published retreat rates of the Scandinavian Ice Sheet provides a formation age of the Luga moraine close to Lake Ladoga's southern shore of 14.5–15.9 cal. ka BP , older than previously assumed. Varve sedimentation covers the Bølling/Allerød interstadial, the Younger Dryas stadial and the Early Holocene. Varve‐thickness variations, conjoined with grain‐size and geochemical variations, inform about the relative position of the Scandinavian Ice Sheet and the climate during the deglaciation phase. The upper limit of the varved succession marks the change from glaciolacustrine to normal lacustrine sedimentation and post‐dates the drainage of the Baltic Ice Lake as well as the formation of the Salpausselkä II moraine north of Lake Ladoga, by c . 250 years. The Holocene sediment record is divided into three periods in the following order: (i) a lower transition zone between the Holocene boundary and c . 9.5 cal. ka BP , characterized by mostly massive sediments with low organic content, (ii) a phase with increased organic content from c . 9.5 to 4.5 cal. ka BP corresponding to the Holocene Thermal Maximum, and (iii) a phase with relatively stable sedimentation in a lacustrine environment from c . 4.5 cal. ka BP until present." @default.
- W2916451831 created "2019-03-02" @default.
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- W2916451831 date "2019-02-21" @default.
- W2916451831 modified "2023-10-18" @default.
- W2916451831 title "Deglaciation history of Lake Ladoga (northwestern Russia) based on varved sediments" @default.
- W2916451831 cites W1622734766 @default.
- W2916451831 cites W185551405 @default.
- W2916451831 cites W1884435078 @default.
- W2916451831 cites W1972016341 @default.
- W2916451831 cites W1972832574 @default.
- W2916451831 cites W1973480744 @default.
- W2916451831 cites W1974947172 @default.
- W2916451831 cites W1976693889 @default.
- W2916451831 cites W1979178500 @default.
- W2916451831 cites W1982002268 @default.
- W2916451831 cites W1984879127 @default.
- W2916451831 cites W1985490719 @default.
- W2916451831 cites W1997917137 @default.
- W2916451831 cites W2007331923 @default.
- W2916451831 cites W2010078738 @default.
- W2916451831 cites W2011062887 @default.
- W2916451831 cites W2012193261 @default.
- W2916451831 cites W2016353087 @default.
- W2916451831 cites W2016895904 @default.
- W2916451831 cites W2018049277 @default.
- W2916451831 cites W2018649455 @default.
- W2916451831 cites W2022978299 @default.
- W2916451831 cites W2023167767 @default.
- W2916451831 cites W2025259577 @default.
- W2916451831 cites W2029031509 @default.
- W2916451831 cites W2034034969 @default.
- W2916451831 cites W2036645183 @default.
- W2916451831 cites W2037587407 @default.
- W2916451831 cites W2040609969 @default.
- W2916451831 cites W2040871137 @default.
- W2916451831 cites W2051322392 @default.
- W2916451831 cites W2052493774 @default.
- W2916451831 cites W2052996746 @default.
- W2916451831 cites W2067319544 @default.
- W2916451831 cites W2077303431 @default.
- W2916451831 cites W2077332076 @default.
- W2916451831 cites W2080962981 @default.
- W2916451831 cites W2082092064 @default.
- W2916451831 cites W2085954304 @default.
- W2916451831 cites W2087071932 @default.
- W2916451831 cites W2088596611 @default.
- W2916451831 cites W2089441856 @default.
- W2916451831 cites W2092227809 @default.
- W2916451831 cites W2092904577 @default.
- W2916451831 cites W2094842475 @default.
- W2916451831 cites W2096526453 @default.
- W2916451831 cites W2098126983 @default.
- W2916451831 cites W2100693889 @default.
- W2916451831 cites W2109269291 @default.
- W2916451831 cites W2109773409 @default.
- W2916451831 cites W2118247098 @default.
- W2916451831 cites W2129523241 @default.
- W2916451831 cites W2130256271 @default.
- W2916451831 cites W2131810031 @default.
- W2916451831 cites W2133204386 @default.
- W2916451831 cites W2133989996 @default.
- W2916451831 cites W2139646874 @default.
- W2916451831 cites W2139857660 @default.
- W2916451831 cites W2141961466 @default.
- W2916451831 cites W2153754396 @default.
- W2916451831 cites W2156627317 @default.
- W2916451831 cites W2158918602 @default.
- W2916451831 cites W2159334146 @default.
- W2916451831 cites W2165166287 @default.
- W2916451831 cites W2170755303 @default.
- W2916451831 cites W2176696981 @default.
- W2916451831 cites W2176932226 @default.
- W2916451831 cites W2205590205 @default.
- W2916451831 cites W2327082204 @default.
- W2916451831 cites W2354709762 @default.
- W2916451831 cites W2396989526 @default.
- W2916451831 cites W2464593274 @default.
- W2916451831 cites W2568882059 @default.
- W2916451831 cites W2749330834 @default.
- W2916451831 cites W2799641219 @default.
- W2916451831 cites W2799855403 @default.
- W2916451831 cites W2897145051 @default.
- W2916451831 cites W2911892324 @default.
- W2916451831 cites W2914403075 @default.
- W2916451831 cites W3016659376 @default.
- W2916451831 cites W4210964572 @default.
- W2916451831 cites W4236650783 @default.