New climatic oscillations during MIS 11c in the record of the Skrzynka II site (Eastern Poland) based on palynological and isotope analysis

Górecki, Artur; Żarski, Marcin; Drzewicki, Wojciech; Pleśniak, Łukasz; Zalewska‐Gałosz, Joanna; Hrynowiecka, Anna

doi:10.1016/j.quaint.2021.09.017

Cited by 3 publications

(10 citation statements)

References 55 publications

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“…Sites with Mazovian Interglacial sediments record the presence of paleolakes that developed after the Saanian 2 Glaciation (Elsterian, MIS 12; Żarski 2008, 2009; Żarski et al 2009a) in depressions for med after melted-out dead-ice blocks (Małek and Pidek 2007;Pidek et al 2011;Hrynowiecka et al 2019;Górecki et al 2022). In south-eastern Poland, most Mazovian Interglacial deposits accumulated in small basins located on the surface of fossil moraine plateaus or glaciofluvial plains from the Saanian 2 Glaciation.…”

Section: Lake Deposits Of the Mazovian Interglacial (Holsteinian Mis ...mentioning

confidence: 99%

“…The second region in the Southern Podlasie Lowland with a documented Mazovian palaeolakeland is located in its south-western part -in the vicinity of Łuków, Kock and Wola Okrzejska within the Łuków Plain and in the western part of the Żelechów Heights (Żarski et al 2005a, b, 2009aMałek and Pidek 2007;Pidek et al 2011;Terpiłowski et al 2014;Hrynowiecka et al 2019;Górecki et al 2022).…”

Section: Lake Deposits Of the Mazovian Interglacial (Holsteinian Mis ...mentioning

confidence: 99%

“…In the frame of the Adamów sheet of the Detailed Geological Map of Poland at the scale of 1: 50 000, the Kolonia Domaszewska, Kolonia Bystrzycka, Przytulin and Hermanów sites have been subject to expert palaeobotanic analyses of lake deposits, whose age was attributed to the Mazovian Interglacial (MIS 11c) (Krupiński 2004a(Krupiński , b, 2009Żarski and Krupiński 2005;Winter 2006Winter , 2008Żarski et al 2009b). A complete palaeobotanic expertise was prepared for Hermanów and Skrzynka (Hrynowiecka et al 2019;Górecki et al 2022).…”

Section: Lake Deposits Of the Mazovian Interglacial (Holsteinian Mis ...mentioning

confidence: 99%

“…In 2013, two rotary drillings were made, resulting in successions with intact core structure SKI and SKII. The SKII succession was subject to palynologic analysis (Górecki et al 2022).…”

Section: Skrzynkamentioning

confidence: 99%

“…In Skrzynka, the Mazovian Interglacial (MIS 11c) series is 4.3 m thick and begins with sands with peat intercalations, passing into gyttja, overlain by lake peat and silts (Górecki et al 2022). Below the lacustrine series occur glacial tills of the Sanian 2 Glaciation (Elsterian, MIS 12; Table 4, Text-fig.…”

Section: Lithological Analysismentioning

confidence: 99%

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The maximum extent of the Odranian Glaciation (Saalian, MIS 6) in the South Podlasie Lowland (SE Poland) in the light of sites with lacustrine deposits of the Mazovian Interglacial

Żarski,

Hrynowiecka,

Górecki

et al. 2024

Acta Geologica Polonica

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Based on the analysis of the geological context and palynological studies performed on lake and bog sediments in the Southern Podlasie Lowland, a new concept of the maximum extent of the Odranian Glaciation (Saalian, MIS 6) is presented for the study area. It is depicted by the Siedlce−Łosice−Kornica zone of end moraines, which so far was considered as stadial-rank or as the Wartanian ice sheet limit. To the south of this zone, near Biała Podlaska and in the Łuków Plain, there occur numerous sites with fossil deposits of the Mazovian Interglacial (MIS 11c). Sites with new documentation, i.e., Wólka Domaszewska, Kolonia Bystrzycka, Przytulin, Hermanów, and Skrzynka are located about 30 km to the south and 60 km to the west of the Biała Podlaska area. Palynological analysis unequivocally indicates the presence of a vegetation succession characteristic of the Mazovian Interglacial. In all sites, deposits of the Mazovian Interglacial are covered by lacustrine sediments of the Liviecian Glaciation (Fuhne, MIS 11b-MIS 10) or mineral sediments of the Vistulian Glaciation (Weichselian, MIS 2) and the Holocene. The sediments infill paleolakes carved in glacial tills of the Sanian 2 Glaciation (MIS 12). The lake sediments of the Mazovian Interglacial and the overlying biogenic and mineral deposits occur in the analysed sites directly below the surface. They are never covered by glacial deposits, which suggests that the Odranian ice sheet did not cover the study area. The location of the lake and bog sites with their geological analysis allow for the precise depiction of the eastern limit of the Odranian ice sheet lobe, which in the study area correlates with the limit suggested in the late 19th century. The Odranian ice sheet did not cover Southern Podlasie.

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Section: Lake Deposits Of the Mazovian Interglacial (Holsteinian Mis ...mentioning

confidence: 99%

Section: Lake Deposits Of the Mazovian Interglacial (Holsteinian Mis ...mentioning

confidence: 99%

Section: Lake Deposits Of the Mazovian Interglacial (Holsteinian Mis ...mentioning

confidence: 99%

“…In 2013, two rotary drillings were made, resulting in successions with intact core structure SKI and SKII. The SKII succession was subject to palynologic analysis (Górecki et al 2022).…”

Section: Skrzynkamentioning

confidence: 99%

Section: Lithological Analysismentioning

confidence: 99%

See 3 more Smart Citations

The maximum extent of the Odranian Glaciation (Saalian, MIS 6) in the South Podlasie Lowland (SE Poland) in the light of sites with lacustrine deposits of the Mazovian Interglacial

Żarski,

Hrynowiecka,

Górecki

et al. 2024

Acta Geologica Polonica

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Quaternary Stratigraphy – Sediments, Palaeoenvironments, Fauna and Human Migrations across Central Europe

Danukalova

Fiebig

Pieruccini

et al. 2022

Quaternary International

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Marine Isotope Stage 11c in Europe: Recent advances in marine–terrestrial correlations and their implications for interglacial stratigraphy – a review

Candy,

Oliveira,

Parkes

et al. 2024

Boreas

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The interglacial known as MIS 11c (c. 426 000–396 000 years ago) receives intensive international interest because of its perceived role as an analogue for the current interglacial and its importance for understanding future climate change. Here we review the current understanding of the stratigraphy of this interglacial in Europe. This study considers (i) the evidence for the environmental history of this interglacial as reconstructed from the varved lake records from northern Europe, (ii) the climate history of MIS 11c as preserved in the long pollen records of southern Europe and (iii) a comparison of both of these with marine records from the North Atlantic. The result of this review is a discussion of the evidence for millennial and centennial scale climate change found in European records of MIS 11c, the patterns of warming that are seen across this interglacial and the discrepancy in aspects of the duration of this interglacial that seems to exist between the marine and terrestrial records of this warm period. A review of the recent advances in the study of MIS 11c in Europe confirms its importance for understanding both the past evolution of the Holocene and the future patterns of long‐term climate change.

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New climatic oscillations during MIS 11c in the record of the Skrzynka II site (Eastern Poland) based on palynological and isotope analysis

Cited by 3 publications

References 55 publications

The maximum extent of the Odranian Glaciation (Saalian, MIS 6) in the South Podlasie Lowland (SE Poland) in the light of sites with lacustrine deposits of the Mazovian Interglacial

The maximum extent of the Odranian Glaciation (Saalian, MIS 6) in the South Podlasie Lowland (SE Poland) in the light of sites with lacustrine deposits of the Mazovian Interglacial

Quaternary Stratigraphy – Sediments, Palaeoenvironments, Fauna and Human Migrations across Central Europe

Marine Isotope Stage 11c in Europe: Recent advances in marine–terrestrial correlations and their implications for interglacial stratigraphy – a review

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