Not logged in
PANGAEA.
Data Publisher for Earth & Environmental Science

Kostrova, Svetlana S; Biskaborn, Boris K; Pestryakova, Luidmila A; Fernandoy, Francisco; Lenz, Marlene M; Meyer, Hanno (2021): Oxygen isotope composition of diatoms from Lake Emanda (northeastern Siberia, Russia) [dataset]. PANGAEA, https://doi.org/10.1594/PANGAEA.933228

Always quote citation above when using data! You can download the citation in several formats below.

Published: 2021-06-30DOI registered: 2021-07-30

RIS CitationBibTeX Citation ShareShow MapGoogle Earth

Abstract:
The sedimentary sequence of core Co1412 from Lake Emanda (65°17′N; 135°45′E; 671 m a.s.l) has been retrieved in August 2017 using gravity and percussion piston corers (UWITEC Ltd., Austria) and investigated within the German-Russian 'Paleolimnological Transect' (PLOT) project. Well preserved diatoms occur only in the upper 125-cm interval of a 6.1-m sediment core covering the last 13.2 cal. ka BP. Diatoms were purified to >98% SiO₂ and <0.8% Al₂O₃ suitable for oxygen isotope analysis. The δ¹⁸O diatom values were corrected for contamination and range between +22.5‰ and +27.8‰. A new dataset on diatom oxygen isotope composition provides insights into the climate and environmental dynamics in an extreme continental setting in northeastern Siberia. The δ¹⁸O diatom record reveals an obvious shift of 2‰ in the δ¹⁸O diatom record at 11.7−11.5 cal. ka BP reflecting the onset of the Holocene. Relatively high δ¹⁸O diatom during the Early Holocene suggests relatively warm and/or dry climate with associated evaporation effects. The absolute maximum in δ¹⁸O diatom 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 δ¹⁸O diatom 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).
Keyword(s):
Climate change; diatoms; eastern Siberia; lake sediments; stabe isotopes
Related to:
Kostrova, Svetlana S; Biskaborn, Boris K; Pestryakova, Luidmila A; Fernandoy, Francisco; Lenz, Marlene M; Meyer, Hanno (2021): Climate and environmental changes of the Lateglacial transition and Holocene in northeastern Siberia: Evidence from diatom oxygen isotopes and assemblage composition at Lake Emanda. Quaternary Science Reviews, 259, 106905, https://doi.org/10.1016/j.quascirev.2021.106905
Funding:
Federal Ministry of Education and Research (BMBF), grant/award no. 03G0859: Paleolimnological Transect
Coverage:
Latitude: 65.294200 * Longitude: 135.759200
Minimum DEPTH, sediment/rock: 0.045 m * Maximum DEPTH, sediment/rock: 1.225 m
Event(s):
Co1412 (Lake Emanda) * Latitude: 65.294200 * Longitude: 135.759200 * Location: northeastern Siberia * Method/Device: Sediment corer (SEDCO) * Comment: Retrieved: August 2017 using gravity and percussion piston corers (UWITEC Ltd., Austria)
Parameter(s):
#NameShort NameUnitPrincipal InvestigatorMethod/DeviceComment
1CoreCoreKostrova, Svetlana S
2DEPTH, sediment/rockDepth sedmKostrova, Svetlana SGeocode
3AGEAgeka BPKostrova, Svetlana SGeocode
4Silicon dioxide in diatomsSiO2 diatom%Kostrova, Svetlana Scontent of the oxide in the purified diatom sample
5Aluminium oxide in diatomsAl2O3 diatom%Kostrova, Svetlana Scontent of the oxide in the purified diatom sample
6Diatoms, δ18ODiatoms δ18O‰ SMOWMeyer, HannoElemental analyzer (PDZ Europa)measured value in ISOLOAB facility
7ContaminationContamination%Kostrova, Svetlana S
8Diatoms, δ18O, correctedDiatoms δ18O corr‰ SMOWKostrova, Svetlana Scontamination corrected value
Status:
Curation Level: Enhanced curation (CurationLevelC)
Size:
276 data points

Download Data

Download dataset as tab-delimited text — use the following character encoding:

View dataset as HTML