Climate and environmental changes of the Lategacial transition and Holocene in northeastern Siberia: Evidence from diatom oxygen isotopes and assemblage composition at Lake Emanda

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dc.contributor.authorKostrova, S.S.
dc.contributor.authorBiskaborn, B.K.
dc.contributor.authorPestryakova, L.A.
dc.contributor.authorFernandoy, F.
dc.contributor.authorLenz, M.M.
dc.contributor.authorMeyer, H.
dc.date.accessioned2021-05-14T14:01:38Z
dc.date.available2021-05-14T14:01:38Z
dc.date.issued2021-05
dc.descriptionIndexación Scopuses
dc.description.abstractA new dataset from Lake Emanda provides insights into climate and environmental dynamics in an extreme continental setting in northeastern Siberia. The δ18Odiatom record is supported by diatom assemblage analysis, modern isotope hydrology and atmospheric circulation patterns. The data reveal a relatively cold oligotrophic freshwater lake system persisting for the last ∼13.2 cal ka BP. Most recent δ18Odiatom (+21.5‰) combined with present-day average δ18Olake (−16.5‰) allows calculating Tlake (∼21 °C), reflecting summer conditions. Nonetheless, the δ18Odiatom variability is associated with changes in δ18Olake rather than with Tlake. An obvious shift of ∼2‰ in the δ18Odiatom record at 11.7–11.5 cal ka BP accompanied by significant changes in diatom assemblages reflects the onset of the Holocene. Relatively high δ18Odiatom during the Early Holocene suggests relatively warm and/or dry climate with associated evaporation effects. The absolute maximum in δ18Odiatom of +27.7‰ consistent with high values of diatom indices at ∼7.9–7.0 cal ka BP suggests a Mid Holocene Thermal Maximum. A continuous depletion in δ18Odiatom since ∼5.0 cal ka BP is interpreted as Middle to Late Holocene cooling reaching the absolute minimum at 0.4 cal ka BP (i.e. the Little Ice Age). An overall cooling trend (∼0.3‰ 1000 yr−1) throughout the Holocene follows decreasing solar insolation. The pattern of the Lake Emanda δ18Odiatom record is similar to that obtained from Lake El'gygytgyn suggesting a common “eastern” regional signal in both records, despite their hydrological differences. Presently, atmospheric moisture reaches the study region from the west and east with ∼40% each, as well as ∼20% from the north. © 2021 The Author(s)es
dc.description.urihttps://www-sciencedirect-com.recursosbiblioteca.unab.cl/science/article/pii/S0277379121001128?via%3Dihub
dc.identifier.citationQuaternary Science Reviews, Volume 259, 1 May 2021, Article number 106905es
dc.identifier.doi10.1016/j.quascirev.2021.106905
dc.identifier.issn02773791
dc.identifier.urihttp://repositorio.unab.cl/xmlui/handle/ria/18854
dc.language.isoenes
dc.publisherElsevier Ltdes
dc.subjectChironomidaees
dc.subjectSubfossiles
dc.subjectCladoceraes
dc.subjectClimate changeses
dc.subjectDiatomses
dc.subjectLake sedimentses
dc.subjectStable isotopeses
dc.titleClimate and environmental changes of the Lategacial transition and Holocene in northeastern Siberia: Evidence from diatom oxygen isotopes and assemblage composition at Lake Emandaes
dc.typeArtículoes
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