Holocene history of human impacts inferred from annually laminated sediments in Lake Szurpiły, northeast Poland
Annually laminated lake sediments provide high-resolution and accurate timescales for reliable paleoenvironmental reconstructions. We investigated human activity in a low-human-impact region of Poland, taking advantage of varved sediments from Lake Szurpiły, which span the last 8200 years. Multiple...
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creator | Kinder, Małgorzata Tylmann, Wojciech Bubak, Iwona Fiłoc, Magdalena Gąsiorowski, Michał Kupryjanowicz, Mirosława Mayr, Christoph Sauer, Laurentius Voellering, Ulrich Zolitschka, Bernd |
description | Annually laminated lake sediments provide high-resolution and accurate timescales for reliable paleoenvironmental reconstructions. We investigated human activity in a low-human-impact region of Poland, taking advantage of varved sediments from Lake Szurpiły, which span the last 8200 years. Multiple sediment variables indicated that catchment evolution and lacustrine responses, mainly to changes in forest cover, were divided into four phases. Because of sparse or only seasonal occupation of settlements in NE Poland, human impact in the region was insignificant until ca. 939 ± 55 BC (lacustrine phase I). During Phase II (939 ± 55 BC–AD 1392 ± 38), we recorded an increase in human indicators, reflecting the direct influence of a Yatvingian community. Afterwards, between AD 1392 ± 38 and 1770 ± 30 (phase III), permanent settlements and agricultural land use stabilized. The beginning of the last period (phase IV) was clearly identified by all sediment variables, which responded simultaneously to local human activities. Disappearance of laminae from AD 1858 ± 22 until about AD 1997 indicated disturbance of pre-existing, stable depositional conditions, followed by environmental recovery in the last 20 years. Such recovery may have been related to recent socio-economic changes and establishment of a park that reduced human influence on the lake. |
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We investigated human activity in a low-human-impact region of Poland, taking advantage of varved sediments from Lake Szurpiły, which span the last 8200 years. Multiple sediment variables indicated that catchment evolution and lacustrine responses, mainly to changes in forest cover, were divided into four phases. Because of sparse or only seasonal occupation of settlements in NE Poland, human impact in the region was insignificant until ca. 939 ± 55 BC (lacustrine phase I). During Phase II (939 ± 55 BC–AD 1392 ± 38), we recorded an increase in human indicators, reflecting the direct influence of a Yatvingian community. Afterwards, between AD 1392 ± 38 and 1770 ± 30 (phase III), permanent settlements and agricultural land use stabilized. The beginning of the last period (phase IV) was clearly identified by all sediment variables, which responded simultaneously to local human activities. Disappearance of laminae from AD 1858 ± 22 until about AD 1997 indicated disturbance of pre-existing, stable depositional conditions, followed by environmental recovery in the last 20 years. Such recovery may have been related to recent socio-economic changes and establishment of a park that reduced human influence on the lake.</description><identifier>ISSN: 0921-2728</identifier><identifier>EISSN: 1573-0417</identifier><identifier>DOI: 10.1007/s10933-019-00068-2</identifier><language>eng</language><publisher>Dordrecht: Springer Netherlands</publisher><subject>Agricultural land ; Catchment area ; Climate Change ; Earth and Environmental Science ; Earth Sciences ; Economic conditions ; Economics ; Freshwater & Marine Ecology ; Geology ; Holocene ; Human impact ; Human influences ; Lake deposits ; Lake sediments ; Lakes ; Laminates ; Land use ; Original Paper ; Paleontology ; Physical Geography ; Recovery ; Sediment ; Sedimentology ; Sediments ; Socioeconomic aspects</subject><ispartof>Journal of paleolimnology, 2019-04, Vol.61 (4), p.419-435</ispartof><rights>The Author(s) 2019</rights><rights>Journal of Paleolimnology is a copyright of Springer, (2019). All Rights Reserved. © 2019. This work is published under http://creativecommons.org/licenses/by/4.0/ (the “License”). Notwithstanding the ProQuest Terms and Conditions, you may use this content in accordance with the terms of the License.</rights><lds50>peer_reviewed</lds50><oa>free_for_read</oa><woscitedreferencessubscribed>false</woscitedreferencessubscribed><citedby>FETCH-LOGICAL-c2782-1791419e21eeed000391c0be08fa61c4b173ea135cce2c72a07c1d97bb820f4d3</citedby><cites>FETCH-LOGICAL-c2782-1791419e21eeed000391c0be08fa61c4b173ea135cce2c72a07c1d97bb820f4d3</cites><orcidid>0000-0002-5379-5367</orcidid></display><links><openurl>$$Topenurl_article</openurl><openurlfulltext>$$Topenurlfull_article</openurlfulltext><thumbnail>$$Tsyndetics_thumb_exl</thumbnail><linktopdf>$$Uhttps://link.springer.com/content/pdf/10.1007/s10933-019-00068-2$$EPDF$$P50$$Gspringer$$Hfree_for_read</linktopdf><linktohtml>$$Uhttps://link.springer.com/10.1007/s10933-019-00068-2$$EHTML$$P50$$Gspringer$$Hfree_for_read</linktohtml><link.rule.ids>314,780,784,27924,27925,41488,42557,51319</link.rule.ids></links><search><creatorcontrib>Kinder, Małgorzata</creatorcontrib><creatorcontrib>Tylmann, Wojciech</creatorcontrib><creatorcontrib>Bubak, Iwona</creatorcontrib><creatorcontrib>Fiłoc, Magdalena</creatorcontrib><creatorcontrib>Gąsiorowski, Michał</creatorcontrib><creatorcontrib>Kupryjanowicz, Mirosława</creatorcontrib><creatorcontrib>Mayr, Christoph</creatorcontrib><creatorcontrib>Sauer, Laurentius</creatorcontrib><creatorcontrib>Voellering, Ulrich</creatorcontrib><creatorcontrib>Zolitschka, Bernd</creatorcontrib><title>Holocene history of human impacts inferred from annually laminated sediments in Lake Szurpiły, northeast Poland</title><title>Journal of paleolimnology</title><addtitle>J Paleolimnol</addtitle><description>Annually laminated lake sediments provide high-resolution and accurate timescales for reliable paleoenvironmental reconstructions. We investigated human activity in a low-human-impact region of Poland, taking advantage of varved sediments from Lake Szurpiły, which span the last 8200 years. Multiple sediment variables indicated that catchment evolution and lacustrine responses, mainly to changes in forest cover, were divided into four phases. Because of sparse or only seasonal occupation of settlements in NE Poland, human impact in the region was insignificant until ca. 939 ± 55 BC (lacustrine phase I). During Phase II (939 ± 55 BC–AD 1392 ± 38), we recorded an increase in human indicators, reflecting the direct influence of a Yatvingian community. Afterwards, between AD 1392 ± 38 and 1770 ± 30 (phase III), permanent settlements and agricultural land use stabilized. The beginning of the last period (phase IV) was clearly identified by all sediment variables, which responded simultaneously to local human activities. Disappearance of laminae from AD 1858 ± 22 until about AD 1997 indicated disturbance of pre-existing, stable depositional conditions, followed by environmental recovery in the last 20 years. Such recovery may have been related to recent socio-economic changes and establishment of a park that reduced human influence on the lake.</description><subject>Agricultural land</subject><subject>Catchment area</subject><subject>Climate Change</subject><subject>Earth and Environmental Science</subject><subject>Earth Sciences</subject><subject>Economic conditions</subject><subject>Economics</subject><subject>Freshwater & Marine Ecology</subject><subject>Geology</subject><subject>Holocene</subject><subject>Human impact</subject><subject>Human influences</subject><subject>Lake deposits</subject><subject>Lake sediments</subject><subject>Lakes</subject><subject>Laminates</subject><subject>Land use</subject><subject>Original Paper</subject><subject>Paleontology</subject><subject>Physical Geography</subject><subject>Recovery</subject><subject>Sediment</subject><subject>Sedimentology</subject><subject>Sediments</subject><subject>Socioeconomic aspects</subject><issn>0921-2728</issn><issn>1573-0417</issn><fulltext>true</fulltext><rsrctype>article</rsrctype><creationdate>2019</creationdate><recordtype>article</recordtype><sourceid>C6C</sourceid><sourceid>AFKRA</sourceid><sourceid>AZQEC</sourceid><sourceid>BENPR</sourceid><sourceid>CCPQU</sourceid><sourceid>DWQXO</sourceid><sourceid>GNUQQ</sourceid><recordid>eNp9kMFKxDAQhoMouK6-gKeAV6uZtLtpjrKoKywoqOeQplO3a5vUpD2sR9_N9zK7Fbx5Ghi-_5_hI-Qc2BUwJq4DMJmmCQOZMMbmecIPyARmIq4yEIdkwiSHhAueH5OTEDYRkrmYTUi3dI0zaJGu69A7v6Wuouuh1ZbWbadNH2htK_QeS1p511Jt7aCbZksb3dZW93EfsKxbtHuUrvQ70ufPwXf199f2klrn-zXq0NMn12hbnpKjSjcBz37nlLze3b4slsnq8f5hcbNKDBc5T0BIyEAiB0Qs47upBMMKZHml52CyAkSKGtKZMciN4JoJA6UURZFzVmVlOiUXY2_n3ceAoVcbN3gbTyq-KxdzLkWk-EgZ70LwWKnO1632WwVM7cyq0ayKZtXerOIxlI6hEGH7hv6v-p_UD6THfaU</recordid><startdate>20190401</startdate><enddate>20190401</enddate><creator>Kinder, Małgorzata</creator><creator>Tylmann, Wojciech</creator><creator>Bubak, Iwona</creator><creator>Fiłoc, Magdalena</creator><creator>Gąsiorowski, Michał</creator><creator>Kupryjanowicz, Mirosława</creator><creator>Mayr, Christoph</creator><creator>Sauer, Laurentius</creator><creator>Voellering, Ulrich</creator><creator>Zolitschka, Bernd</creator><general>Springer Netherlands</general><general>Springer Nature B.V</general><scope>C6C</scope><scope>AAYXX</scope><scope>CITATION</scope><scope>7QH</scope><scope>7QL</scope><scope>7SN</scope><scope>7T7</scope><scope>7U9</scope><scope>7UA</scope><scope>8FD</scope><scope>8FE</scope><scope>8FH</scope><scope>AFKRA</scope><scope>AZQEC</scope><scope>BBNVY</scope><scope>BENPR</scope><scope>BHPHI</scope><scope>BKSAR</scope><scope>C1K</scope><scope>CCPQU</scope><scope>DWQXO</scope><scope>F1W</scope><scope>FR3</scope><scope>GNUQQ</scope><scope>H94</scope><scope>H95</scope><scope>H96</scope><scope>HCIFZ</scope><scope>L.G</scope><scope>LK8</scope><scope>M7N</scope><scope>M7P</scope><scope>P64</scope><scope>PCBAR</scope><scope>PQEST</scope><scope>PQQKQ</scope><scope>PQUKI</scope><orcidid>https://orcid.org/0000-0002-5379-5367</orcidid></search><sort><creationdate>20190401</creationdate><title>Holocene history of human impacts inferred from annually laminated sediments in Lake Szurpiły, northeast Poland</title><author>Kinder, Małgorzata ; 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We investigated human activity in a low-human-impact region of Poland, taking advantage of varved sediments from Lake Szurpiły, which span the last 8200 years. Multiple sediment variables indicated that catchment evolution and lacustrine responses, mainly to changes in forest cover, were divided into four phases. Because of sparse or only seasonal occupation of settlements in NE Poland, human impact in the region was insignificant until ca. 939 ± 55 BC (lacustrine phase I). During Phase II (939 ± 55 BC–AD 1392 ± 38), we recorded an increase in human indicators, reflecting the direct influence of a Yatvingian community. Afterwards, between AD 1392 ± 38 and 1770 ± 30 (phase III), permanent settlements and agricultural land use stabilized. The beginning of the last period (phase IV) was clearly identified by all sediment variables, which responded simultaneously to local human activities. Disappearance of laminae from AD 1858 ± 22 until about AD 1997 indicated disturbance of pre-existing, stable depositional conditions, followed by environmental recovery in the last 20 years. Such recovery may have been related to recent socio-economic changes and establishment of a park that reduced human influence on the lake.</abstract><cop>Dordrecht</cop><pub>Springer Netherlands</pub><doi>10.1007/s10933-019-00068-2</doi><tpages>17</tpages><orcidid>https://orcid.org/0000-0002-5379-5367</orcidid><oa>free_for_read</oa></addata></record> |
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subjects | Agricultural land Catchment area Climate Change Earth and Environmental Science Earth Sciences Economic conditions Economics Freshwater & Marine Ecology Geology Holocene Human impact Human influences Lake deposits Lake sediments Lakes Laminates Land use Original Paper Paleontology Physical Geography Recovery Sediment Sedimentology Sediments Socioeconomic aspects |
title | Holocene history of human impacts inferred from annually laminated sediments in Lake Szurpiły, northeast Poland |
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