FRINK Linked Data Fragments server

Matches in SemOpenAlex for { <https://semopenalex.org/work/W2094261118> ?p ?o ?g. }

• W2094261118 endingPage "82" @default.
• W2094261118 startingPage "70" @default.
• W2094261118 abstract "A lake sediment core collected from the Staroje Lake, southeastern Belarus, reveals significant changes of the terrestrial and limnic environmental during the Lateglacial and Early Holocene in the periglacial zone of the Late Weichselian Glaciation. The combination of lithological (loss-on-ignition), palaeobotanical (pollen, non-pollen palynomorphs, diatoms) and isotopic (δ18O, δ13C, 14C) proxy parameters was applied for the reconstruction of the vegetation pattern and sedimentation regime. The Lateglacial pre-Interstadial (GS-2) vegetation was dominated by mineral-soil pioneers with scattered occurrence of Pinus and Betula; an Interstadial (GI-1) dominated by Pinus forest with increasing representation of open-ground species since approximately 13,500 cal BP; and Lateglacial Stadial (GS-1) with recurring opening of the vegetation pattern with scattered tree patches including those of Picea. Presence of Pinus stomata confirms the local origin of this plant since the pre-Interstadial. Starting from the Holocene, birch, later accompanied by other deciduous species (Ulmus, Alnus, Quercus, Corylus), took over in the local vegetation structure. Isotopic records (δ18O, δ13C) obtained on bulk carbonates as well as diatom data exhibit several shifts reflecting variations both in terrestrial and limnic environment. Distinct negative excursion of δ18O curve recorded during the first half of the GI-1 event suggests intensive groundwater discharge accompanied by active transportation of detrital carbon in to the basin. Limited basin productivity is also indicated by lithological and diatom records. Since approximately 13,700 cal BP, sedimentation regime in the lake stabilised and productivity of the basin started to increase in positive correlation with LOI data. A considerable decrease in δ18O values punctuated by a rapid jump in the middle of the interval was recorded during the GS-1 Stadial and could be associated with the deterioration of the environmental regime and degradation of the soil layer, increasing erosion activity alongside the rising input of detrital carbonates into the basin. The water table was low, as indicated by diatom data. Recovery of the environmental regime preceded the GS-1/Holocene boundary, as is seen in lithostratigraphical and isotopic data. During the early Holocene, stable isotopes show several episodes with altered levels suggesting instability of the environmental regime, most probably related with the global climatic alterations." @default.
• W2094261118 created "2016-06-24" @default.
• W2094261118 creator A5016220403 @default.
• W2094261118 creator A5021861302 @default.
• W2094261118 creator A5025983070 @default.
• W2094261118 creator A5034512730 @default.
• W2094261118 creator A5077154629 @default.
• W2094261118 creator A5077178170 @default.
• W2094261118 creator A5031289740 @default.
• W2094261118 date "2015-11-01" @default.
• W2094261118 modified "2023-10-15" @default.
• W2094261118 title "Vegetation pattern and sedimentation changes in the context of the Lateglacial climatic events: Case study of Staroje Lake (Eastern Belarus)" @default.
• W2094261118 cites W1516236295 @default.
• W2094261118 cites W1544007163 @default.
• W2094261118 cites W1565184445 @default.
• W2094261118 cites W1618108810 @default.
• W2094261118 cites W1819552095 @default.
• W2094261118 cites W1963984910 @default.
• W2094261118 cites W1967409131 @default.
• W2094261118 cites W1968588309 @default.
• W2094261118 cites W1969502354 @default.
• W2094261118 cites W1971445289 @default.
• W2094261118 cites W1973687673 @default.
• W2094261118 cites W1976031785 @default.
• W2094261118 cites W1977415133 @default.
• W2094261118 cites W1979739429 @default.
• W2094261118 cites W1988206778 @default.
• W2094261118 cites W1991417760 @default.
• W2094261118 cites W1997980854 @default.
• W2094261118 cites W1999712743 @default.
• W2094261118 cites W2002364714 @default.
• W2094261118 cites W2004569583 @default.
• W2094261118 cites W2005045275 @default.
• W2094261118 cites W2005462331 @default.
• W2094261118 cites W2020048343 @default.
• W2094261118 cites W2020599804 @default.
• W2094261118 cites W2021835305 @default.
• W2094261118 cites W2022416339 @default.
• W2094261118 cites W2026673317 @default.
• W2094261118 cites W2030004028 @default.
• W2094261118 cites W2030355458 @default.
• W2094261118 cites W2036026441 @default.
• W2094261118 cites W2036031260 @default.
• W2094261118 cites W2036431121 @default.
• W2094261118 cites W2041006844 @default.
• W2094261118 cites W2043288594 @default.
• W2094261118 cites W2047943497 @default.
• W2094261118 cites W2051773982 @default.
• W2094261118 cites W2053950462 @default.
• W2094261118 cites W2056137997 @default.
• W2094261118 cites W2056244884 @default.
• W2094261118 cites W2057928160 @default.
• W2094261118 cites W2058798025 @default.
• W2094261118 cites W2059128792 @default.
• W2094261118 cites W2064468541 @default.
• W2094261118 cites W2065553263 @default.
• W2094261118 cites W2071184501 @default.
• W2094261118 cites W2080171806 @default.
• W2094261118 cites W2082081375 @default.
• W2094261118 cites W2085581106 @default.
• W2094261118 cites W2085754415 @default.
• W2094261118 cites W2086658485 @default.
• W2094261118 cites W2090166955 @default.
• W2094261118 cites W2090705149 @default.
• W2094261118 cites W2092072437 @default.
• W2094261118 cites W2094417138 @default.
• W2094261118 cites W2099590375 @default.
• W2094261118 cites W2101406394 @default.
• W2094261118 cites W2102276023 @default.
• W2094261118 cites W2105496762 @default.
• W2094261118 cites W2108875511 @default.
• W2094261118 cites W2118247098 @default.
• W2094261118 cites W2125538518 @default.
• W2094261118 cites W2129672566 @default.
• W2094261118 cites W2138834810 @default.
• W2094261118 cites W2140262477 @default.
• W2094261118 cites W2142432396 @default.
• W2094261118 cites W2146933258 @default.
• W2094261118 cites W2158490798 @default.
• W2094261118 cites W2159334146 @default.
• W2094261118 cites W2160138627 @default.
• W2094261118 cites W2160850801 @default.
• W2094261118 cites W2161513873 @default.
• W2094261118 cites W2167752422 @default.
• W2094261118 cites W2168761377 @default.
• W2094261118 cites W2169469431 @default.
• W2094261118 cites W2500288105 @default.
• W2094261118 cites W2745656063 @default.
• W2094261118 cites W2823621924 @default.
• W2094261118 cites W4235955026 @default.
• W2094261118 cites W4249751050 @default.
• W2094261118 cites W62739343 @default.
• W2094261118 doi "https://doi.org/10.1016/j.quaint.2014.06.045" @default.
• W2094261118 hasPublicationYear "2015" @default.
• W2094261118 type Work @default.
• W2094261118 sameAs 2094261118 @default.
• W2094261118 citedByCount "15" @default.
• W2094261118 countsByYear W20942611182015 @default.

• next