Natural and anthropogenic impacts on Lake Ladoga and its catchment area through the late glacial and Holocene according to a new paleolimnological record

A ca. 12,700 year-long pollen and diatom record, as well as data on lithology, geochemistry, and grain size were obtained from two sediment cores retrieved in the southwest part of Lake Ladoga. Changes in phosphorus content during the Holocene were recorded from this sequence dated by the radiocarbo...

Ausführliche Beschreibung

Gespeichert in:
Bibliographische Detailangaben
Veröffentlicht in:Journal of paleolimnology 2024-08, Vol.72 (2), p.241-259
Hauptverfasser: Sapelko, Tatyana, Ignatyeva, Natalia, Kuznetsov, Denis, Ludikova, Anna, Guseva, Maria, Revunova, Anna, Zazovskaya, Elya, Pozdnyakov, Shamil
Format: Artikel
Sprache:eng
Schlagworte:
Online-Zugang:Volltext
Tags: Tag hinzufügen
Keine Tags, Fügen Sie den ersten Tag hinzu!
container_end_page 259
container_issue 2
container_start_page 241
container_title Journal of paleolimnology
container_volume 72
creator Sapelko, Tatyana
Ignatyeva, Natalia
Kuznetsov, Denis
Ludikova, Anna
Guseva, Maria
Revunova, Anna
Zazovskaya, Elya
Pozdnyakov, Shamil
description A ca. 12,700 year-long pollen and diatom record, as well as data on lithology, geochemistry, and grain size were obtained from two sediment cores retrieved in the southwest part of Lake Ladoga. Changes in phosphorus content during the Holocene were recorded from this sequence dated by the radiocarbon method. An increase in phosphorus, loss-on-ignition and the Fe/Mn ratio was recorded during the climatic optimum of the Holocene ca. 7500–7250 cal yr BP. At the same time, pollen data showed the spread of broad-leaved forests. The peak in phosphorus in the upper part of the core associated with anthropogenic activities is smaller to the peak corresponding to the Holocene climatic optimum. This may indicate that climatic factors affect the ecosystems of large lakes more significantly than anthropogenic ones. According to our new pollen data, first human impact is recorded in Lake Ladoga sediments ca. 2580 cal yr BP.
doi_str_mv 10.1007/s10933-024-00329-9
format Article
fullrecord <record><control><sourceid>proquest_cross</sourceid><recordid>TN_cdi_proquest_miscellaneous_3153761148</recordid><sourceformat>XML</sourceformat><sourcesystem>PC</sourcesystem><sourcerecordid>3102212561</sourcerecordid><originalsourceid>FETCH-LOGICAL-c233t-3d4fa68bb305580b6d4378c6c702ddd847c4b9fdc48668e0c9fad73f493810e73</originalsourceid><addsrcrecordid>eNp9kcFu1DAQhi0EEkvbF-BkiQuX0LGdxM4RVUCRVuVCz9GsPcmmJHawHSEehbett1sJiQMHe6TR9_0a6WfsrYAPAkBfJwGdUhXIugJQsqu6F2wnGl1WtdAv2Q46KSqppXnN3qT0AACd0c2O_bnDvEWcOXpXXj7GsIaR_GT5tKxoc-LB8z3-oPK5MOITOJW1xWyPC_nMMRLyk7mNxzKJz5iJjzPa6Tn4NszBkieO1oboJj_yHDhyT7_4ijOFeVp8YcbJFiPSCbpkrwacE109zwt2__nT95vbav_ty9ebj_vKSqVypVw9YGsOBwVNY-DQulppY1urQTrnTK1tfegGZ2vTtobAdgM6rYa6U0YAaXXB3p9z1xh-bpRyv0zJ0jyjp7ClXolG6VaI2hT03T_oQ9iiL9cVCqQUsmlFoeSZsjGkFGno1zgtGH_3AvpTW_25rb601T-11XdFUmcpFdiPFP9G_8d6BDkgmXE</addsrcrecordid><sourcetype>Aggregation Database</sourcetype><iscdi>true</iscdi><recordtype>article</recordtype><pqid>3102212561</pqid></control><display><type>article</type><title>Natural and anthropogenic impacts on Lake Ladoga and its catchment area through the late glacial and Holocene according to a new paleolimnological record</title><source>SpringerLink Journals</source><creator>Sapelko, Tatyana ; Ignatyeva, Natalia ; Kuznetsov, Denis ; Ludikova, Anna ; Guseva, Maria ; Revunova, Anna ; Zazovskaya, Elya ; Pozdnyakov, Shamil</creator><creatorcontrib>Sapelko, Tatyana ; Ignatyeva, Natalia ; Kuznetsov, Denis ; Ludikova, Anna ; Guseva, Maria ; Revunova, Anna ; Zazovskaya, Elya ; Pozdnyakov, Shamil</creatorcontrib><description>A ca. 12,700 year-long pollen and diatom record, as well as data on lithology, geochemistry, and grain size were obtained from two sediment cores retrieved in the southwest part of Lake Ladoga. Changes in phosphorus content during the Holocene were recorded from this sequence dated by the radiocarbon method. An increase in phosphorus, loss-on-ignition and the Fe/Mn ratio was recorded during the climatic optimum of the Holocene ca. 7500–7250 cal yr BP. At the same time, pollen data showed the spread of broad-leaved forests. The peak in phosphorus in the upper part of the core associated with anthropogenic activities is smaller to the peak corresponding to the Holocene climatic optimum. This may indicate that climatic factors affect the ecosystems of large lakes more significantly than anthropogenic ones. According to our new pollen data, first human impact is recorded in Lake Ladoga sediments ca. 2580 cal yr BP.</description><identifier>ISSN: 0921-2728</identifier><identifier>EISSN: 1573-0417</identifier><identifier>DOI: 10.1007/s10933-024-00329-9</identifier><language>eng</language><publisher>Dordrecht: Springer Netherlands</publisher><subject>anthropogenic activities ; Anthropogenic factors ; Aquatic ecosystems ; Bacillariophyceae ; carbon radioisotopes ; Catchment area ; Catchment areas ; Climate Change ; Cores ; Diatoms ; Earth and Environmental Science ; Earth Sciences ; Forests ; Freshwater &amp; Marine Ecology ; Geochemistry ; Geology ; Grain size ; Holocene ; Holocene epoch ; Human impact ; Human influences ; Lakes ; Lithology ; Original Paper ; Paleontology ; Papal visits ; Phosphorus ; phosphorus content ; Physical Geography ; Pollen ; Radiocarbon dating ; Sediment ; Sedimentation &amp; deposition ; Sedimentology ; Sediments ; Taiga &amp; tundra ; Topography ; watersheds</subject><ispartof>Journal of paleolimnology, 2024-08, Vol.72 (2), p.241-259</ispartof><rights>The Author(s), under exclusive licence to Springer Nature B.V. 2024. Springer Nature or its licensor (e.g. a society or other partner) holds exclusive rights to this article under a publishing agreement with the author(s) or other rightsholder(s); author self-archiving of the accepted manuscript version of this article is solely governed by the terms of such publishing agreement and applicable law.</rights><lds50>peer_reviewed</lds50><woscitedreferencessubscribed>false</woscitedreferencessubscribed><cites>FETCH-LOGICAL-c233t-3d4fa68bb305580b6d4378c6c702ddd847c4b9fdc48668e0c9fad73f493810e73</cites></display><links><openurl>$$Topenurl_article</openurl><openurlfulltext>$$Topenurlfull_article</openurlfulltext><thumbnail>$$Tsyndetics_thumb_exl</thumbnail><linktopdf>$$Uhttps://link.springer.com/content/pdf/10.1007/s10933-024-00329-9$$EPDF$$P50$$Gspringer$$H</linktopdf><linktohtml>$$Uhttps://link.springer.com/10.1007/s10933-024-00329-9$$EHTML$$P50$$Gspringer$$H</linktohtml><link.rule.ids>314,776,780,27901,27902,41464,42533,51294</link.rule.ids></links><search><creatorcontrib>Sapelko, Tatyana</creatorcontrib><creatorcontrib>Ignatyeva, Natalia</creatorcontrib><creatorcontrib>Kuznetsov, Denis</creatorcontrib><creatorcontrib>Ludikova, Anna</creatorcontrib><creatorcontrib>Guseva, Maria</creatorcontrib><creatorcontrib>Revunova, Anna</creatorcontrib><creatorcontrib>Zazovskaya, Elya</creatorcontrib><creatorcontrib>Pozdnyakov, Shamil</creatorcontrib><title>Natural and anthropogenic impacts on Lake Ladoga and its catchment area through the late glacial and Holocene according to a new paleolimnological record</title><title>Journal of paleolimnology</title><addtitle>J Paleolimnol</addtitle><description>A ca. 12,700 year-long pollen and diatom record, as well as data on lithology, geochemistry, and grain size were obtained from two sediment cores retrieved in the southwest part of Lake Ladoga. Changes in phosphorus content during the Holocene were recorded from this sequence dated by the radiocarbon method. An increase in phosphorus, loss-on-ignition and the Fe/Mn ratio was recorded during the climatic optimum of the Holocene ca. 7500–7250 cal yr BP. At the same time, pollen data showed the spread of broad-leaved forests. The peak in phosphorus in the upper part of the core associated with anthropogenic activities is smaller to the peak corresponding to the Holocene climatic optimum. This may indicate that climatic factors affect the ecosystems of large lakes more significantly than anthropogenic ones. According to our new pollen data, first human impact is recorded in Lake Ladoga sediments ca. 2580 cal yr BP.</description><subject>anthropogenic activities</subject><subject>Anthropogenic factors</subject><subject>Aquatic ecosystems</subject><subject>Bacillariophyceae</subject><subject>carbon radioisotopes</subject><subject>Catchment area</subject><subject>Catchment areas</subject><subject>Climate Change</subject><subject>Cores</subject><subject>Diatoms</subject><subject>Earth and Environmental Science</subject><subject>Earth Sciences</subject><subject>Forests</subject><subject>Freshwater &amp; Marine Ecology</subject><subject>Geochemistry</subject><subject>Geology</subject><subject>Grain size</subject><subject>Holocene</subject><subject>Holocene epoch</subject><subject>Human impact</subject><subject>Human influences</subject><subject>Lakes</subject><subject>Lithology</subject><subject>Original Paper</subject><subject>Paleontology</subject><subject>Papal visits</subject><subject>Phosphorus</subject><subject>phosphorus content</subject><subject>Physical Geography</subject><subject>Pollen</subject><subject>Radiocarbon dating</subject><subject>Sediment</subject><subject>Sedimentation &amp; deposition</subject><subject>Sedimentology</subject><subject>Sediments</subject><subject>Taiga &amp; tundra</subject><subject>Topography</subject><subject>watersheds</subject><issn>0921-2728</issn><issn>1573-0417</issn><fulltext>true</fulltext><rsrctype>article</rsrctype><creationdate>2024</creationdate><recordtype>article</recordtype><recordid>eNp9kcFu1DAQhi0EEkvbF-BkiQuX0LGdxM4RVUCRVuVCz9GsPcmmJHawHSEehbett1sJiQMHe6TR9_0a6WfsrYAPAkBfJwGdUhXIugJQsqu6F2wnGl1WtdAv2Q46KSqppXnN3qT0AACd0c2O_bnDvEWcOXpXXj7GsIaR_GT5tKxoc-LB8z3-oPK5MOITOJW1xWyPC_nMMRLyk7mNxzKJz5iJjzPa6Tn4NszBkieO1oboJj_yHDhyT7_4ijOFeVp8YcbJFiPSCbpkrwacE109zwt2__nT95vbav_ty9ebj_vKSqVypVw9YGsOBwVNY-DQulppY1urQTrnTK1tfegGZ2vTtobAdgM6rYa6U0YAaXXB3p9z1xh-bpRyv0zJ0jyjp7ClXolG6VaI2hT03T_oQ9iiL9cVCqQUsmlFoeSZsjGkFGno1zgtGH_3AvpTW_25rb601T-11XdFUmcpFdiPFP9G_8d6BDkgmXE</recordid><startdate>20240801</startdate><enddate>20240801</enddate><creator>Sapelko, Tatyana</creator><creator>Ignatyeva, Natalia</creator><creator>Kuznetsov, Denis</creator><creator>Ludikova, Anna</creator><creator>Guseva, Maria</creator><creator>Revunova, Anna</creator><creator>Zazovskaya, Elya</creator><creator>Pozdnyakov, Shamil</creator><general>Springer Netherlands</general><general>Springer Nature B.V</general><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>C1K</scope><scope>F1W</scope><scope>FR3</scope><scope>H94</scope><scope>H95</scope><scope>H96</scope><scope>L.G</scope><scope>M7N</scope><scope>P64</scope><scope>7S9</scope><scope>L.6</scope></search><sort><creationdate>20240801</creationdate><title>Natural and anthropogenic impacts on Lake Ladoga and its catchment area through the late glacial and Holocene according to a new paleolimnological record</title><author>Sapelko, Tatyana ; Ignatyeva, Natalia ; Kuznetsov, Denis ; Ludikova, Anna ; Guseva, Maria ; Revunova, Anna ; Zazovskaya, Elya ; Pozdnyakov, Shamil</author></sort><facets><frbrtype>5</frbrtype><frbrgroupid>cdi_FETCH-LOGICAL-c233t-3d4fa68bb305580b6d4378c6c702ddd847c4b9fdc48668e0c9fad73f493810e73</frbrgroupid><rsrctype>articles</rsrctype><prefilter>articles</prefilter><language>eng</language><creationdate>2024</creationdate><topic>anthropogenic activities</topic><topic>Anthropogenic factors</topic><topic>Aquatic ecosystems</topic><topic>Bacillariophyceae</topic><topic>carbon radioisotopes</topic><topic>Catchment area</topic><topic>Catchment areas</topic><topic>Climate Change</topic><topic>Cores</topic><topic>Diatoms</topic><topic>Earth and Environmental Science</topic><topic>Earth Sciences</topic><topic>Forests</topic><topic>Freshwater &amp; Marine Ecology</topic><topic>Geochemistry</topic><topic>Geology</topic><topic>Grain size</topic><topic>Holocene</topic><topic>Holocene epoch</topic><topic>Human impact</topic><topic>Human influences</topic><topic>Lakes</topic><topic>Lithology</topic><topic>Original Paper</topic><topic>Paleontology</topic><topic>Papal visits</topic><topic>Phosphorus</topic><topic>phosphorus content</topic><topic>Physical Geography</topic><topic>Pollen</topic><topic>Radiocarbon dating</topic><topic>Sediment</topic><topic>Sedimentation &amp; deposition</topic><topic>Sedimentology</topic><topic>Sediments</topic><topic>Taiga &amp; tundra</topic><topic>Topography</topic><topic>watersheds</topic><toplevel>peer_reviewed</toplevel><toplevel>online_resources</toplevel><creatorcontrib>Sapelko, Tatyana</creatorcontrib><creatorcontrib>Ignatyeva, Natalia</creatorcontrib><creatorcontrib>Kuznetsov, Denis</creatorcontrib><creatorcontrib>Ludikova, Anna</creatorcontrib><creatorcontrib>Guseva, Maria</creatorcontrib><creatorcontrib>Revunova, Anna</creatorcontrib><creatorcontrib>Zazovskaya, Elya</creatorcontrib><creatorcontrib>Pozdnyakov, Shamil</creatorcontrib><collection>CrossRef</collection><collection>Aqualine</collection><collection>Bacteriology Abstracts (Microbiology B)</collection><collection>Ecology Abstracts</collection><collection>Industrial and Applied Microbiology Abstracts (Microbiology A)</collection><collection>Virology and AIDS Abstracts</collection><collection>Water Resources Abstracts</collection><collection>Technology Research Database</collection><collection>Environmental Sciences and Pollution Management</collection><collection>ASFA: Aquatic Sciences and Fisheries Abstracts</collection><collection>Engineering Research Database</collection><collection>AIDS and Cancer Research Abstracts</collection><collection>Aquatic Science &amp; Fisheries Abstracts (ASFA) 1: Biological Sciences &amp; Living Resources</collection><collection>Aquatic Science &amp; Fisheries Abstracts (ASFA) 2: Ocean Technology, Policy &amp; Non-Living Resources</collection><collection>Aquatic Science &amp; Fisheries Abstracts (ASFA) Professional</collection><collection>Algology Mycology and Protozoology Abstracts (Microbiology C)</collection><collection>Biotechnology and BioEngineering Abstracts</collection><collection>AGRICOLA</collection><collection>AGRICOLA - Academic</collection><jtitle>Journal of paleolimnology</jtitle></facets><delivery><delcategory>Remote Search Resource</delcategory><fulltext>fulltext</fulltext></delivery><addata><au>Sapelko, Tatyana</au><au>Ignatyeva, Natalia</au><au>Kuznetsov, Denis</au><au>Ludikova, Anna</au><au>Guseva, Maria</au><au>Revunova, Anna</au><au>Zazovskaya, Elya</au><au>Pozdnyakov, Shamil</au><format>journal</format><genre>article</genre><ristype>JOUR</ristype><atitle>Natural and anthropogenic impacts on Lake Ladoga and its catchment area through the late glacial and Holocene according to a new paleolimnological record</atitle><jtitle>Journal of paleolimnology</jtitle><stitle>J Paleolimnol</stitle><date>2024-08-01</date><risdate>2024</risdate><volume>72</volume><issue>2</issue><spage>241</spage><epage>259</epage><pages>241-259</pages><issn>0921-2728</issn><eissn>1573-0417</eissn><abstract>A ca. 12,700 year-long pollen and diatom record, as well as data on lithology, geochemistry, and grain size were obtained from two sediment cores retrieved in the southwest part of Lake Ladoga. Changes in phosphorus content during the Holocene were recorded from this sequence dated by the radiocarbon method. An increase in phosphorus, loss-on-ignition and the Fe/Mn ratio was recorded during the climatic optimum of the Holocene ca. 7500–7250 cal yr BP. At the same time, pollen data showed the spread of broad-leaved forests. The peak in phosphorus in the upper part of the core associated with anthropogenic activities is smaller to the peak corresponding to the Holocene climatic optimum. This may indicate that climatic factors affect the ecosystems of large lakes more significantly than anthropogenic ones. According to our new pollen data, first human impact is recorded in Lake Ladoga sediments ca. 2580 cal yr BP.</abstract><cop>Dordrecht</cop><pub>Springer Netherlands</pub><doi>10.1007/s10933-024-00329-9</doi><tpages>19</tpages></addata></record>
fulltext fulltext
identifier ISSN: 0921-2728
ispartof Journal of paleolimnology, 2024-08, Vol.72 (2), p.241-259
issn 0921-2728
1573-0417
language eng
recordid cdi_proquest_miscellaneous_3153761148
source SpringerLink Journals
subjects anthropogenic activities
Anthropogenic factors
Aquatic ecosystems
Bacillariophyceae
carbon radioisotopes
Catchment area
Catchment areas
Climate Change
Cores
Diatoms
Earth and Environmental Science
Earth Sciences
Forests
Freshwater & Marine Ecology
Geochemistry
Geology
Grain size
Holocene
Holocene epoch
Human impact
Human influences
Lakes
Lithology
Original Paper
Paleontology
Papal visits
Phosphorus
phosphorus content
Physical Geography
Pollen
Radiocarbon dating
Sediment
Sedimentation & deposition
Sedimentology
Sediments
Taiga & tundra
Topography
watersheds
title Natural and anthropogenic impacts on Lake Ladoga and its catchment area through the late glacial and Holocene according to a new paleolimnological record
url https://sfx.bib-bvb.de/sfx_tum?ctx_ver=Z39.88-2004&ctx_enc=info:ofi/enc:UTF-8&ctx_tim=2025-02-08T10%3A55%3A54IST&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=Natural%20and%20anthropogenic%20impacts%20on%20Lake%20Ladoga%20and%20its%20catchment%20area%20through%20the%20late%20glacial%20and%20Holocene%20according%20to%20a%20new%20paleolimnological%20record&rft.jtitle=Journal%20of%20paleolimnology&rft.au=Sapelko,%20Tatyana&rft.date=2024-08-01&rft.volume=72&rft.issue=2&rft.spage=241&rft.epage=259&rft.pages=241-259&rft.issn=0921-2728&rft.eissn=1573-0417&rft_id=info:doi/10.1007/s10933-024-00329-9&rft_dat=%3Cproquest_cross%3E3102212561%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=3102212561&rft_id=info:pmid/&rfr_iscdi=true