The Lateglacial and Early Holocene vegetation dynamics: New multi-proxy data from the central Belarus

Stančikaitė, Miglė; Zernitskaya, Valentina; Kluczynska, Gražyna; Valūnas, Darius; Gedminienė, Laura; Uogintas, Domas; Skuratovič, Žana; Власов, Борис Павлович; Gastevičienė, Neringa; Ežerinskis, Žilvinas; Šapolaitė, Justina; Šeirienė, Vaida

doi:10.1016/j.quaint.2021.05.004

Cited by 7 publications

(14 citation statements)

References 91 publications

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“…Due to sparse radiocarbon dating results in the Lipowo profile, the lower, geochronological boundary should be taken with some caution. The lower limit was established on the basis of pollen analysis correlated with the results of studies from the Kaniewo profile (Mirosław‐Grabowska et al , 2020) and central Belarus (Stančikaitė et al , 2022). We think that pollen analysis is in this case more precise, so the stratigraphic scheme is built on this result.…”

Section: Discussionmentioning

confidence: 79%

“…Climate cooling inferred from pollen analysis might be interpreted as the second cool oscillation (GI‐1b), although this should be taken with some caution due to insufficient absolute dating results. An alternative interpretation is that it could belong to the Younger Dryas – this second interpretation is less probable, however, due to absence of Picea in the pollen record and the clear increase of Juniperus , which is characteristic of the Younger Dryas (Stančikaitė et al , 2022).…”

Section: Discussionmentioning

confidence: 99%

“…Therefore, every chronologically well‐supported high‐resolution multiproxy archive of regional importance could aid in improving the understanding of the Late Glacial climatic evolution and the ecosystem reactions in the Northern Hemisphere (Zernitskaya et al , 2014). Late Glacial sediments of lakes located beyond the limit of the maximal extent of the last glaciation (LGM) have been investigated in eastern and central Belarus (Zernitskaya et al , 2014; Stančikaitė et al , 2022). Deposits of this age have also been recognised in western Lithuania (Kisieliene et al , 2005; Guobyte and Satkunas, 2011).…”

Section: Introductionmentioning

confidence: 99%

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Late Pleniglacial – Late Glacial climate oscillations detected in the organic lacustrine succession at the Lipowo site, north‐eastern Poland

Rychel

Sokolowski

Sieradz

et al. 2022

J Quaternary Science

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The profile of the Lipowo palaeolake (NE Poland) preserves a record of environmental and climate changes from the Last Glacial Termination (16.5k cal ka BP), stretching from the Oldest Dryas to the youngest Allerød warm oscillation. In this interdisciplinary study of the lacustrine succession at Lipowo, we used biological and geochemical indicators and multiproxy analyses to reconstruct environmental changes in the lake ecosystem, such as mollusc, zooplankton and vegetation development, trophic state, water temperature and water level. Four cold and four warm climate oscillations of different durations were identified on this basis: the Older Dryas climate deterioration and two short‐term coolings within the Allerød Interstadial, separated by warm periods in the Bølling and Allerød. The covering of the lake series by diamicton deposits from the melting of dead‐ice blocks is a particularly interesting and rare phenomenon for a postglacial area. The hydrological system of the catchment was generally closed, with a periodically opening and existing flow‐through lake. Over the period of the lake's existence, vegetation changed in general from steppe tundra to forest with birch and pine. For most of this time, the palaeolake was mainly oligotrophic, with increased productivity and a higher trophic level only notable during the middle Bølling.

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Section: Discussionmentioning

confidence: 79%

Section: Discussionmentioning

confidence: 99%

Section: Introductionmentioning

confidence: 99%

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Late Pleniglacial – Late Glacial climate oscillations detected in the organic lacustrine succession at the Lipowo site, north‐eastern Poland

Rychel

Sokolowski

Sieradz

et al. 2022

J Quaternary Science

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“…Figure 1. Key section Seltso (marked with an asterisk) and sites used for comparison: 1-Protva River, core PR-10 [38,39]; 2-Lake Dolgoye [25,40]; 3-Lake Seliger, core SP-2 [40,41]; 4-Lake Terebenskoye [42]; 5-Zmeinoe Mire [43]; 6-Lake Sudoble [44,45]; 7-Lake Velikoye [46]; 8-Lake Staroje [47].…”

Section: Methodsmentioning

confidence: 99%

“…Detritus gyttja with higher organic contents formed there in the Late Preboreal. In Lake Velikoye [46], a layer of light grey sandy gyttja accumulated during the Younger Dryas. A transition to greyish-blue gyttja in this core corresponds to the Late Glacial-Holocene boundary.…”

Section: Changes In the Composition Of Lacustrine Sedimentsmentioning

confidence: 99%

Short-Term Climatic Oscillations in the Central Region of the East-European Plain at the Beginning of the Holocene Based on Palynological Studies of Lacustrine Deposits

Borisova,

Naryshkina,

Panin

2024

Quaternary

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The Preboreal (11.75–10.70 ka BP) is still the least paleogeographically studied time interval in the central part of the East European Plain. High-resolution multi-proxy studies of lacustrine sediments at the Seltso site located in the Desna River floodplain (Dnieper River basin) were conducted. Radiocarbon dating, loss-on-ignition determination, sedimentological and palynological studies and identification of Non-Pollen Palynomorphs in lacustrine sediments allow us to reconstruct changes in vegetation caused by rapid warming at the Younger Dryas–Holocene boundary, short-term climatic fluctuations within the Preboreal and subsequent resumption of warming. Initial Preboreal warming reached its maximum at about 11.5 ka BP when a relatively dry continental climate existed. Between 11.4 and 11.2 ka BP, a short-term cooling corresponding to the Preboreal Oscillation in Greenland occurred, as indicated by a significant reduction of woody vegetation and expansion of open plant communities. In the Late Preboreal, approximately 11.2–10.7 ka BP, warming resumed, which was accompanied by a decrease in the climate continentality. Comparison with high-resolution lithological and palynological data from eight reliably dated sections of the central East European Plain indicates that in northwestern and central Europe, the impact of the Preboreal Oscillation cooling on the vegetation and the lake ecosystems’ development was probably somewhat stronger.

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Late-Weichselian (Vistulian) environmental changes in NE Poland – Evidence from Lake Suchar Wielki

Fiłoc,

Kupryjanowicz,

Suchora

et al. 2024

CATENA

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The Lateglacial and Early Holocene vegetation dynamics: New multi-proxy data from the central Belarus

Cited by 7 publications

References 91 publications

Late Pleniglacial – Late Glacial climate oscillations detected in the organic lacustrine succession at the Lipowo site, north‐eastern Poland

Late Pleniglacial – Late Glacial climate oscillations detected in the organic lacustrine succession at the Lipowo site, north‐eastern Poland

Short-Term Climatic Oscillations in the Central Region of the East-European Plain at the Beginning of the Holocene Based on Palynological Studies of Lacustrine Deposits

Late-Weichselian (Vistulian) environmental changes in NE Poland – Evidence from Lake Suchar Wielki

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