Geology, stratigraphy and palaeoenvironmental evolution of the Stephanorhinus kirchbergensis‐bearing Quaternary palaeolake(s) of Gorzów Wielkopolski (NW Poland, Central Europe)
ABSTRACT The sedimentary succession exposed in the Gorzów Wielkopolski area includes Eemian Interglacial (MIS 5e) or Early Weichselian (MIS 5d–e) deposits. The sedimentary sequence has been the object of intense interdisciplinary study, which has resulted in the identification of at least two palaeo...
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| Veröffentlicht in: | Journal of quaternary science 2020-05, Vol.35 (4), p.539-558 |
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| creator | Sobczyk, Artur Borówka, Ryszard K. Badura, Janusz Stachowicz‐Rybka, Renata Tomkowiak, Julita Hrynowiecka, Anna Sławińska, Joanna Tomczak, Michał Pitura, Mateusz Lamentowicz, Mariusz Kołaczek, Piotr Karpińska‐Kołaczek, Monika Tarnawski, Dariusz Kadej, Marcin Moska, Piotr Krąpiec, Marek Stachowicz, Krzysztof Bieniek, Bartosz Siedlik, Krzysztof Bąk, Małgorzata Made, Jan Kotowski, Adam Stefaniak, Krzysztof |
| description | ABSTRACT
The sedimentary succession exposed in the Gorzów Wielkopolski area includes Eemian Interglacial (MIS 5e) or Early Weichselian (MIS 5d–e) deposits. The sedimentary sequence has been the object of intense interdisciplinary study, which has resulted in the identification of at least two palaeolake horizons. Both yielded fossil remains of large mammals, alongside pollen and plant macrofossils. All these proxies have been used to reconstruct the environmental conditions prevailing at the time of deposition, as well as to define the geological context and the biochronological position of the fauna. Optically stimulated luminescence dating of the glaciofluvial layers of the GS3 succession to 123.6 ± 10.1 (below the lower palaeolake) and 72.0 ± 5.2 ka (above the upper palaeolake) indicate that the site formed during the Middle–Late Pleistocene (MIS 6 – MIS 5). Radiocarbon‐dating of the lacustrine organic matter revealed a tight cluster of Middle Pleniglacial Period (MIS 3) ages in the range of ~41–32 ka cal bp (Hengelo – Denekamp Interstadials). Holocene organic layers have also been found, with 14C ages within a range of 4330–4280 cal bp (Neolithic). Pollen and plant macrofossil records, together with sedimentological and geochemical data, confirm the dating to the Eemian Interglacial. |
| doi_str_mv | 10.1002/jqs.3198 |
| format | Article |
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The sedimentary succession exposed in the Gorzów Wielkopolski area includes Eemian Interglacial (MIS 5e) or Early Weichselian (MIS 5d–e) deposits. The sedimentary sequence has been the object of intense interdisciplinary study, which has resulted in the identification of at least two palaeolake horizons. Both yielded fossil remains of large mammals, alongside pollen and plant macrofossils. All these proxies have been used to reconstruct the environmental conditions prevailing at the time of deposition, as well as to define the geological context and the biochronological position of the fauna. Optically stimulated luminescence dating of the glaciofluvial layers of the GS3 succession to 123.6 ± 10.1 (below the lower palaeolake) and 72.0 ± 5.2 ka (above the upper palaeolake) indicate that the site formed during the Middle–Late Pleistocene (MIS 6 – MIS 5). Radiocarbon‐dating of the lacustrine organic matter revealed a tight cluster of Middle Pleniglacial Period (MIS 3) ages in the range of ~41–32 ka cal bp (Hengelo – Denekamp Interstadials). Holocene organic layers have also been found, with 14C ages within a range of 4330–4280 cal bp (Neolithic). Pollen and plant macrofossil records, together with sedimentological and geochemical data, confirm the dating to the Eemian Interglacial.</description><identifier>ISSN: 0267-8179</identifier><identifier>EISSN: 1099-1417</identifier><identifier>DOI: 10.1002/jqs.3198</identifier><language>eng</language><publisher>Chichester: Wiley Subscription Services, Inc</publisher><subject>Dating ; Ecological succession ; Eemian Interglacial ; Environmental conditions ; Geology ; Holocene ; Interdisciplinary studies ; Organic matter ; OSL dating ; palynology and macrofossil analysis ; Plant fossils ; Pleistocene ; Pollen ; Quaternary ; Quaternary stratigraphy ; radiocarbon dating ; Radiometric dating ; Sediment deposits ; Stone Age ; Stratigraphy</subject><ispartof>Journal of quaternary science, 2020-05, Vol.35 (4), p.539-558</ispartof><rights>2020 John Wiley & Sons, Ltd.</rights><lds50>peer_reviewed</lds50><oa>free_for_read</oa><woscitedreferencessubscribed>false</woscitedreferencessubscribed><citedby>FETCH-LOGICAL-a3508-f2464b639b20d54b92a6e65cd9512d3aaa82f0934f02760be70e88ee4582854d3</citedby><cites>FETCH-LOGICAL-a3508-f2464b639b20d54b92a6e65cd9512d3aaa82f0934f02760be70e88ee4582854d3</cites><orcidid>0000-0002-6878-9007 ; 0000-0001-5983-0402 ; 0000-0001-6782-0714 ; 0000-0003-2552-8269 ; 0000-0002-8170-8240 ; 0000-0003-0660-9530 ; 0000-0002-0802-0570 ; 0000-0003-3829-561X ; 0000-0003-0429-1530 ; 0000-0002-4807-4338 ; 0000-0002-4116-7275 ; 0000-0003-0437-0255 ; 0000-0001-6114-9595 ; 0000-0001-9711-6947 ; 0000-0002-3249-7408</orcidid></display><links><openurl>$$Topenurl_article</openurl><openurlfulltext>$$Topenurlfull_article</openurlfulltext><thumbnail>$$Tsyndetics_thumb_exl</thumbnail><linktopdf>$$Uhttps://onlinelibrary.wiley.com/doi/pdf/10.1002%2Fjqs.3198$$EPDF$$P50$$Gwiley$$H</linktopdf><linktohtml>$$Uhttps://onlinelibrary.wiley.com/doi/full/10.1002%2Fjqs.3198$$EHTML$$P50$$Gwiley$$H</linktohtml><link.rule.ids>314,780,784,1416,27923,27924,45573,45574</link.rule.ids></links><search><creatorcontrib>Sobczyk, Artur</creatorcontrib><creatorcontrib>Borówka, Ryszard K.</creatorcontrib><creatorcontrib>Badura, Janusz</creatorcontrib><creatorcontrib>Stachowicz‐Rybka, Renata</creatorcontrib><creatorcontrib>Tomkowiak, Julita</creatorcontrib><creatorcontrib>Hrynowiecka, Anna</creatorcontrib><creatorcontrib>Sławińska, Joanna</creatorcontrib><creatorcontrib>Tomczak, Michał</creatorcontrib><creatorcontrib>Pitura, Mateusz</creatorcontrib><creatorcontrib>Lamentowicz, Mariusz</creatorcontrib><creatorcontrib>Kołaczek, Piotr</creatorcontrib><creatorcontrib>Karpińska‐Kołaczek, Monika</creatorcontrib><creatorcontrib>Tarnawski, Dariusz</creatorcontrib><creatorcontrib>Kadej, Marcin</creatorcontrib><creatorcontrib>Moska, Piotr</creatorcontrib><creatorcontrib>Krąpiec, Marek</creatorcontrib><creatorcontrib>Stachowicz, Krzysztof</creatorcontrib><creatorcontrib>Bieniek, Bartosz</creatorcontrib><creatorcontrib>Siedlik, Krzysztof</creatorcontrib><creatorcontrib>Bąk, Małgorzata</creatorcontrib><creatorcontrib>Made, Jan</creatorcontrib><creatorcontrib>Kotowski, Adam</creatorcontrib><creatorcontrib>Stefaniak, Krzysztof</creatorcontrib><title>Geology, stratigraphy and palaeoenvironmental evolution of the Stephanorhinus kirchbergensis‐bearing Quaternary palaeolake(s) of Gorzów Wielkopolski (NW Poland, Central Europe)</title><title>Journal of quaternary science</title><description>ABSTRACT
The sedimentary succession exposed in the Gorzów Wielkopolski area includes Eemian Interglacial (MIS 5e) or Early Weichselian (MIS 5d–e) deposits. The sedimentary sequence has been the object of intense interdisciplinary study, which has resulted in the identification of at least two palaeolake horizons. Both yielded fossil remains of large mammals, alongside pollen and plant macrofossils. All these proxies have been used to reconstruct the environmental conditions prevailing at the time of deposition, as well as to define the geological context and the biochronological position of the fauna. Optically stimulated luminescence dating of the glaciofluvial layers of the GS3 succession to 123.6 ± 10.1 (below the lower palaeolake) and 72.0 ± 5.2 ka (above the upper palaeolake) indicate that the site formed during the Middle–Late Pleistocene (MIS 6 – MIS 5). Radiocarbon‐dating of the lacustrine organic matter revealed a tight cluster of Middle Pleniglacial Period (MIS 3) ages in the range of ~41–32 ka cal bp (Hengelo – Denekamp Interstadials). Holocene organic layers have also been found, with 14C ages within a range of 4330–4280 cal bp (Neolithic). Pollen and plant macrofossil records, together with sedimentological and geochemical data, confirm the dating to the Eemian Interglacial.</description><subject>Dating</subject><subject>Ecological succession</subject><subject>Eemian Interglacial</subject><subject>Environmental conditions</subject><subject>Geology</subject><subject>Holocene</subject><subject>Interdisciplinary studies</subject><subject>Organic matter</subject><subject>OSL dating</subject><subject>palynology and macrofossil analysis</subject><subject>Plant fossils</subject><subject>Pleistocene</subject><subject>Pollen</subject><subject>Quaternary</subject><subject>Quaternary stratigraphy</subject><subject>radiocarbon dating</subject><subject>Radiometric dating</subject><subject>Sediment deposits</subject><subject>Stone Age</subject><subject>Stratigraphy</subject><issn>0267-8179</issn><issn>1099-1417</issn><fulltext>true</fulltext><rsrctype>article</rsrctype><creationdate>2020</creationdate><recordtype>article</recordtype><recordid>eNp1kc1uEzEUhS0EEqEg8QiW2KRSp_hnfuwlikooqoCqoC5HdzJ3Mk5ce2rPtAorHqHv0kfgTXgSHNItq7u4n76jo0PIW85OOWPi_eY2nkqu1TMy40zrjOe8ek5mTJRVpnilX5JXMW4YS7-SzcjjEr31690JjWOA0awDDP2OgmvpABbQo7szwbsbdCNYinfeTqPxjvqOjj3SqxGHHpwPvXFTpFsTVn2DYY0umvjn10ODEIxb08sJRgwOwu7Ja2GL83i89yx9-Pn78Z5eG7RbP3gbt4bOv1zTb4ly7QldpPCQ0s-m4Ac8fk1edGAjvnm6R-THx7Pvi0_Zxdfl-eLDRQayYCrrRF7mTSl1I1hb5I0WUGJZrFpdcNFKAFCiY1rmHRNVyRqsGCqFmBdKqCJv5RF5d_AOwd9OGMd646fUwcZaSF3pQkqtEjU_UKvgYwzY1UMwN6lozVm9n6ROk9T7SRKaHdB7Y3H3X67-fHn1j_8LuluSvQ</recordid><startdate>202005</startdate><enddate>202005</enddate><creator>Sobczyk, Artur</creator><creator>Borówka, Ryszard K.</creator><creator>Badura, Janusz</creator><creator>Stachowicz‐Rybka, Renata</creator><creator>Tomkowiak, Julita</creator><creator>Hrynowiecka, Anna</creator><creator>Sławińska, Joanna</creator><creator>Tomczak, Michał</creator><creator>Pitura, Mateusz</creator><creator>Lamentowicz, Mariusz</creator><creator>Kołaczek, Piotr</creator><creator>Karpińska‐Kołaczek, Monika</creator><creator>Tarnawski, Dariusz</creator><creator>Kadej, Marcin</creator><creator>Moska, Piotr</creator><creator>Krąpiec, Marek</creator><creator>Stachowicz, Krzysztof</creator><creator>Bieniek, Bartosz</creator><creator>Siedlik, Krzysztof</creator><creator>Bąk, Małgorzata</creator><creator>Made, Jan</creator><creator>Kotowski, Adam</creator><creator>Stefaniak, Krzysztof</creator><general>Wiley Subscription Services, Inc</general><scope>AAYXX</scope><scope>CITATION</scope><scope>7ST</scope><scope>7TG</scope><scope>8FD</scope><scope>C1K</scope><scope>FR3</scope><scope>KL.</scope><scope>KR7</scope><scope>SOI</scope><orcidid>https://orcid.org/0000-0002-6878-9007</orcidid><orcidid>https://orcid.org/0000-0001-5983-0402</orcidid><orcidid>https://orcid.org/0000-0001-6782-0714</orcidid><orcidid>https://orcid.org/0000-0003-2552-8269</orcidid><orcidid>https://orcid.org/0000-0002-8170-8240</orcidid><orcidid>https://orcid.org/0000-0003-0660-9530</orcidid><orcidid>https://orcid.org/0000-0002-0802-0570</orcidid><orcidid>https://orcid.org/0000-0003-3829-561X</orcidid><orcidid>https://orcid.org/0000-0003-0429-1530</orcidid><orcidid>https://orcid.org/0000-0002-4807-4338</orcidid><orcidid>https://orcid.org/0000-0002-4116-7275</orcidid><orcidid>https://orcid.org/0000-0003-0437-0255</orcidid><orcidid>https://orcid.org/0000-0001-6114-9595</orcidid><orcidid>https://orcid.org/0000-0001-9711-6947</orcidid><orcidid>https://orcid.org/0000-0002-3249-7408</orcidid></search><sort><creationdate>202005</creationdate><title>Geology, stratigraphy and palaeoenvironmental evolution of the Stephanorhinus kirchbergensis‐bearing Quaternary palaeolake(s) of Gorzów Wielkopolski (NW Poland, Central Europe)</title><author>Sobczyk, Artur ; Borówka, Ryszard K. ; Badura, Janusz ; Stachowicz‐Rybka, Renata ; Tomkowiak, Julita ; Hrynowiecka, Anna ; Sławińska, Joanna ; Tomczak, Michał ; Pitura, Mateusz ; Lamentowicz, Mariusz ; Kołaczek, Piotr ; Karpińska‐Kołaczek, Monika ; Tarnawski, Dariusz ; Kadej, Marcin ; Moska, Piotr ; Krąpiec, Marek ; Stachowicz, Krzysztof ; Bieniek, Bartosz ; Siedlik, Krzysztof ; Bąk, Małgorzata ; Made, Jan ; Kotowski, Adam ; Stefaniak, Krzysztof</author></sort><facets><frbrtype>5</frbrtype><frbrgroupid>cdi_FETCH-LOGICAL-a3508-f2464b639b20d54b92a6e65cd9512d3aaa82f0934f02760be70e88ee4582854d3</frbrgroupid><rsrctype>articles</rsrctype><prefilter>articles</prefilter><language>eng</language><creationdate>2020</creationdate><topic>Dating</topic><topic>Ecological succession</topic><topic>Eemian Interglacial</topic><topic>Environmental conditions</topic><topic>Geology</topic><topic>Holocene</topic><topic>Interdisciplinary studies</topic><topic>Organic matter</topic><topic>OSL dating</topic><topic>palynology and macrofossil analysis</topic><topic>Plant fossils</topic><topic>Pleistocene</topic><topic>Pollen</topic><topic>Quaternary</topic><topic>Quaternary stratigraphy</topic><topic>radiocarbon dating</topic><topic>Radiometric dating</topic><topic>Sediment deposits</topic><topic>Stone Age</topic><topic>Stratigraphy</topic><toplevel>peer_reviewed</toplevel><toplevel>online_resources</toplevel><creatorcontrib>Sobczyk, Artur</creatorcontrib><creatorcontrib>Borówka, Ryszard K.</creatorcontrib><creatorcontrib>Badura, Janusz</creatorcontrib><creatorcontrib>Stachowicz‐Rybka, Renata</creatorcontrib><creatorcontrib>Tomkowiak, Julita</creatorcontrib><creatorcontrib>Hrynowiecka, Anna</creatorcontrib><creatorcontrib>Sławińska, Joanna</creatorcontrib><creatorcontrib>Tomczak, Michał</creatorcontrib><creatorcontrib>Pitura, Mateusz</creatorcontrib><creatorcontrib>Lamentowicz, Mariusz</creatorcontrib><creatorcontrib>Kołaczek, Piotr</creatorcontrib><creatorcontrib>Karpińska‐Kołaczek, Monika</creatorcontrib><creatorcontrib>Tarnawski, Dariusz</creatorcontrib><creatorcontrib>Kadej, Marcin</creatorcontrib><creatorcontrib>Moska, Piotr</creatorcontrib><creatorcontrib>Krąpiec, Marek</creatorcontrib><creatorcontrib>Stachowicz, Krzysztof</creatorcontrib><creatorcontrib>Bieniek, Bartosz</creatorcontrib><creatorcontrib>Siedlik, Krzysztof</creatorcontrib><creatorcontrib>Bąk, Małgorzata</creatorcontrib><creatorcontrib>Made, Jan</creatorcontrib><creatorcontrib>Kotowski, Adam</creatorcontrib><creatorcontrib>Stefaniak, Krzysztof</creatorcontrib><collection>CrossRef</collection><collection>Environment Abstracts</collection><collection>Meteorological & Geoastrophysical Abstracts</collection><collection>Technology Research Database</collection><collection>Environmental Sciences and Pollution Management</collection><collection>Engineering Research Database</collection><collection>Meteorological & Geoastrophysical Abstracts - Academic</collection><collection>Civil Engineering Abstracts</collection><collection>Environment Abstracts</collection><jtitle>Journal of quaternary science</jtitle></facets><delivery><delcategory>Remote Search Resource</delcategory><fulltext>fulltext</fulltext></delivery><addata><au>Sobczyk, Artur</au><au>Borówka, Ryszard K.</au><au>Badura, Janusz</au><au>Stachowicz‐Rybka, Renata</au><au>Tomkowiak, Julita</au><au>Hrynowiecka, Anna</au><au>Sławińska, Joanna</au><au>Tomczak, Michał</au><au>Pitura, Mateusz</au><au>Lamentowicz, Mariusz</au><au>Kołaczek, Piotr</au><au>Karpińska‐Kołaczek, Monika</au><au>Tarnawski, Dariusz</au><au>Kadej, Marcin</au><au>Moska, Piotr</au><au>Krąpiec, Marek</au><au>Stachowicz, Krzysztof</au><au>Bieniek, Bartosz</au><au>Siedlik, Krzysztof</au><au>Bąk, Małgorzata</au><au>Made, Jan</au><au>Kotowski, Adam</au><au>Stefaniak, Krzysztof</au><format>journal</format><genre>article</genre><ristype>JOUR</ristype><atitle>Geology, stratigraphy and palaeoenvironmental evolution of the Stephanorhinus kirchbergensis‐bearing Quaternary palaeolake(s) of Gorzów Wielkopolski (NW Poland, Central Europe)</atitle><jtitle>Journal of quaternary science</jtitle><date>2020-05</date><risdate>2020</risdate><volume>35</volume><issue>4</issue><spage>539</spage><epage>558</epage><pages>539-558</pages><issn>0267-8179</issn><eissn>1099-1417</eissn><abstract>ABSTRACT
The sedimentary succession exposed in the Gorzów Wielkopolski area includes Eemian Interglacial (MIS 5e) or Early Weichselian (MIS 5d–e) deposits. The sedimentary sequence has been the object of intense interdisciplinary study, which has resulted in the identification of at least two palaeolake horizons. Both yielded fossil remains of large mammals, alongside pollen and plant macrofossils. All these proxies have been used to reconstruct the environmental conditions prevailing at the time of deposition, as well as to define the geological context and the biochronological position of the fauna. Optically stimulated luminescence dating of the glaciofluvial layers of the GS3 succession to 123.6 ± 10.1 (below the lower palaeolake) and 72.0 ± 5.2 ka (above the upper palaeolake) indicate that the site formed during the Middle–Late Pleistocene (MIS 6 – MIS 5). Radiocarbon‐dating of the lacustrine organic matter revealed a tight cluster of Middle Pleniglacial Period (MIS 3) ages in the range of ~41–32 ka cal bp (Hengelo – Denekamp Interstadials). Holocene organic layers have also been found, with 14C ages within a range of 4330–4280 cal bp (Neolithic). Pollen and plant macrofossil records, together with sedimentological and geochemical data, confirm the dating to the Eemian Interglacial.</abstract><cop>Chichester</cop><pub>Wiley Subscription Services, Inc</pub><doi>10.1002/jqs.3198</doi><tpages>20</tpages><orcidid>https://orcid.org/0000-0002-6878-9007</orcidid><orcidid>https://orcid.org/0000-0001-5983-0402</orcidid><orcidid>https://orcid.org/0000-0001-6782-0714</orcidid><orcidid>https://orcid.org/0000-0003-2552-8269</orcidid><orcidid>https://orcid.org/0000-0002-8170-8240</orcidid><orcidid>https://orcid.org/0000-0003-0660-9530</orcidid><orcidid>https://orcid.org/0000-0002-0802-0570</orcidid><orcidid>https://orcid.org/0000-0003-3829-561X</orcidid><orcidid>https://orcid.org/0000-0003-0429-1530</orcidid><orcidid>https://orcid.org/0000-0002-4807-4338</orcidid><orcidid>https://orcid.org/0000-0002-4116-7275</orcidid><orcidid>https://orcid.org/0000-0003-0437-0255</orcidid><orcidid>https://orcid.org/0000-0001-6114-9595</orcidid><orcidid>https://orcid.org/0000-0001-9711-6947</orcidid><orcidid>https://orcid.org/0000-0002-3249-7408</orcidid><oa>free_for_read</oa></addata></record> |
| fulltext | fulltext |
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| ispartof | Journal of quaternary science, 2020-05, Vol.35 (4), p.539-558 |
| issn | 0267-8179 1099-1417 |
| language | eng |
| recordid | cdi_proquest_journals_2397953398 |
| source | Wiley Online Library All Journals |
| subjects | Dating Ecological succession Eemian Interglacial Environmental conditions Geology Holocene Interdisciplinary studies Organic matter OSL dating palynology and macrofossil analysis Plant fossils Pleistocene Pollen Quaternary Quaternary stratigraphy radiocarbon dating Radiometric dating Sediment deposits Stone Age Stratigraphy |
| title | Geology, stratigraphy and palaeoenvironmental evolution of the Stephanorhinus kirchbergensis‐bearing Quaternary palaeolake(s) of Gorzów Wielkopolski (NW Poland, Central Europe) |
| url | https://sfx.bib-bvb.de/sfx_tum?ctx_ver=Z39.88-2004&ctx_enc=info:ofi/enc:UTF-8&ctx_tim=2025-01-11T13%3A24%3A48IST&url_ver=Z39.88-2004&url_ctx_fmt=infofi/fmt:kev:mtx:ctx&rfr_id=info:sid/primo.exlibrisgroup.com:primo3-Article-proquest_cross&rft_val_fmt=info:ofi/fmt:kev:mtx:journal&rft.genre=article&rft.atitle=Geology,%20stratigraphy%20and%20palaeoenvironmental%20evolution%20of%20the%20Stephanorhinus%20kirchbergensis%E2%80%90bearing%20Quaternary%20palaeolake(s)%20of%20Gorz%C3%B3w%20Wielkopolski%20(NW%20Poland,%20Central%20Europe)&rft.jtitle=Journal%20of%20quaternary%20science&rft.au=Sobczyk,%20Artur&rft.date=2020-05&rft.volume=35&rft.issue=4&rft.spage=539&rft.epage=558&rft.pages=539-558&rft.issn=0267-8179&rft.eissn=1099-1417&rft_id=info:doi/10.1002/jqs.3198&rft_dat=%3Cproquest_cross%3E2397953398%3C/proquest_cross%3E%3Curl%3E%3C/url%3E&disable_directlink=true&sfx.directlink=off&sfx.report_link=0&rft_id=info:oai/&rft_pqid=2397953398&rft_id=info:pmid/&rfr_iscdi=true |