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Salvinia natans in medieval wetland deposits in Gdańsk, northern Poland: evidence for the early medieval climate warming
Large numbers of sub-fossil remains of the aquatic fern Salvinia natans (L.) All. have been found in several early medieval sites in Gdańsk, N. Poland. This record indicates a population expansion of this species around 7th–8th century A.D., similar to the recently observed rapid spread and high pop...
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Published in: | Journal of paleolimnology 2011-03, Vol.45 (3), p.369-383 |
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creator | Święta-Musznicka, Joanna Latałowa, Małgorzata Szmeja, Józef Badura, Monika |
description | Large numbers of sub-fossil remains of the aquatic fern
Salvinia natans
(L.) All. have been found in several early medieval sites in Gdańsk, N. Poland. This record indicates a population expansion of this species around 7th–8th century A.D., similar to the recently observed rapid spread and high population dynamics of
S. natans
in northern Poland, which recent studies have attributed to climate warming. Our results suggest that in the Vistula deltaic area the
S. natans
expansion in the Early Middle Ages (7th–8th century A.D.) was similarly stimulated by climate warming, while its subsequent decline was mainly due to climate cooling, especially during the Little Ice Age. Warmer winters and springs and a longer growing season seem to be the most important factors forcing the expansion of
S. natans
in medieval times. According to our data, the co-occurrence of
S. natans
with other aquatic plant species was similar in both the medieval and present-day vegetation. Also, the high density of
S. natans
in the medieval population caused impoverishment of the local ecosystems in a way that has been observed in recent water bodies affected by invasive pleustophytes (free-floating plants). |
doi_str_mv | 10.1007/s10933-011-9505-1 |
format | article |
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Salvinia natans
(L.) All. have been found in several early medieval sites in Gdańsk, N. Poland. This record indicates a population expansion of this species around 7th–8th century A.D., similar to the recently observed rapid spread and high population dynamics of
S. natans
in northern Poland, which recent studies have attributed to climate warming. Our results suggest that in the Vistula deltaic area the
S. natans
expansion in the Early Middle Ages (7th–8th century A.D.) was similarly stimulated by climate warming, while its subsequent decline was mainly due to climate cooling, especially during the Little Ice Age. Warmer winters and springs and a longer growing season seem to be the most important factors forcing the expansion of
S. natans
in medieval times. According to our data, the co-occurrence of
S. natans
with other aquatic plant species was similar in both the medieval and present-day vegetation. Also, the high density of
S. natans
in the medieval population caused impoverishment of the local ecosystems in a way that has been observed in recent water bodies affected by invasive pleustophytes (free-floating plants).</description><identifier>ISSN: 0921-2728</identifier><identifier>EISSN: 1573-0417</identifier><identifier>DOI: 10.1007/s10933-011-9505-1</identifier><language>eng</language><publisher>Dordrecht: Springer Netherlands</publisher><subject>Climate Change ; Earth and Environmental Science ; Earth Sciences ; Freshwater & Marine Ecology ; Geology ; Original Paper ; Paleontology ; Physical Geography ; Salvinia natans ; Sedimentology</subject><ispartof>Journal of paleolimnology, 2011-03, Vol.45 (3), p.369-383</ispartof><rights>The Author(s) 2011</rights><lds50>peer_reviewed</lds50><oa>free_for_read</oa><woscitedreferencessubscribed>false</woscitedreferencessubscribed><citedby>FETCH-LOGICAL-a386t-f312a1c5b313a52ec08e1df42e4b79ec01e13302b7398f19d0e8af036e3f5b673</citedby><cites>FETCH-LOGICAL-a386t-f312a1c5b313a52ec08e1df42e4b79ec01e13302b7398f19d0e8af036e3f5b673</cites></display><links><openurl>$$Topenurl_article</openurl><openurlfulltext>$$Topenurlfull_article</openurlfulltext><thumbnail>$$Tsyndetics_thumb_exl</thumbnail><link.rule.ids>314,780,784,27922,27923</link.rule.ids></links><search><creatorcontrib>Święta-Musznicka, Joanna</creatorcontrib><creatorcontrib>Latałowa, Małgorzata</creatorcontrib><creatorcontrib>Szmeja, Józef</creatorcontrib><creatorcontrib>Badura, Monika</creatorcontrib><title>Salvinia natans in medieval wetland deposits in Gdańsk, northern Poland: evidence for the early medieval climate warming</title><title>Journal of paleolimnology</title><addtitle>J Paleolimnol</addtitle><description>Large numbers of sub-fossil remains of the aquatic fern
Salvinia natans
(L.) All. have been found in several early medieval sites in Gdańsk, N. Poland. This record indicates a population expansion of this species around 7th–8th century A.D., similar to the recently observed rapid spread and high population dynamics of
S. natans
in northern Poland, which recent studies have attributed to climate warming. Our results suggest that in the Vistula deltaic area the
S. natans
expansion in the Early Middle Ages (7th–8th century A.D.) was similarly stimulated by climate warming, while its subsequent decline was mainly due to climate cooling, especially during the Little Ice Age. Warmer winters and springs and a longer growing season seem to be the most important factors forcing the expansion of
S. natans
in medieval times. According to our data, the co-occurrence of
S. natans
with other aquatic plant species was similar in both the medieval and present-day vegetation. Also, the high density of
S. natans
in the medieval population caused impoverishment of the local ecosystems in a way that has been observed in recent water bodies affected by invasive pleustophytes (free-floating plants).</description><subject>Climate Change</subject><subject>Earth and Environmental Science</subject><subject>Earth Sciences</subject><subject>Freshwater & Marine Ecology</subject><subject>Geology</subject><subject>Original Paper</subject><subject>Paleontology</subject><subject>Physical Geography</subject><subject>Salvinia natans</subject><subject>Sedimentology</subject><issn>0921-2728</issn><issn>1573-0417</issn><fulltext>true</fulltext><rsrctype>article</rsrctype><creationdate>2011</creationdate><recordtype>article</recordtype><recordid>eNp9UD1PwzAQtRBIlMIPYPPGQsBnx03MhhAUpEogAbPlJJfikjjFTlt156_xv3AJEhvT6e596N0j5BTYBTCWXQZgSoiEASRKMpnAHhmBzOIlhWyfjJjikPCM54fkKIQFY0zlmRyR7bNp1tZZQ53pjQvUOtpiZXFtGrrBvjGuohUuu2D7H3Bama_P8H5OXef7N_SOPnU70hXFta3QlUjrztMIUTS-2f65lY1tTY90Y3xr3fyYHNSmCXjyO8fk9e725eY-mT1OH26uZ4kR-aRPagHcQCkLAcJIjiXLEao65ZgWmYorIAjBeJEJldegKoa5qZmYoKhlMcnEmJwNvkvffaww9Lq1ocQmhsZuFbRiXEiR5nlkwsAsfReCx1ovfYzstxqY3rWsh5Z1bFnvWtYQNXzQhMh1c_R60a28iw_9I_oGWuCBsQ</recordid><startdate>20110301</startdate><enddate>20110301</enddate><creator>Święta-Musznicka, Joanna</creator><creator>Latałowa, Małgorzata</creator><creator>Szmeja, Józef</creator><creator>Badura, Monika</creator><general>Springer Netherlands</general><scope>C6C</scope><scope>AAYXX</scope><scope>CITATION</scope><scope>7SN</scope><scope>7TG</scope><scope>C1K</scope><scope>F1W</scope><scope>H95</scope><scope>H96</scope><scope>KL.</scope><scope>L.G</scope></search><sort><creationdate>20110301</creationdate><title>Salvinia natans in medieval wetland deposits in Gdańsk, northern Poland: evidence for the early medieval climate warming</title><author>Święta-Musznicka, Joanna ; Latałowa, Małgorzata ; Szmeja, Józef ; Badura, Monika</author></sort><facets><frbrtype>5</frbrtype><frbrgroupid>cdi_FETCH-LOGICAL-a386t-f312a1c5b313a52ec08e1df42e4b79ec01e13302b7398f19d0e8af036e3f5b673</frbrgroupid><rsrctype>articles</rsrctype><prefilter>articles</prefilter><language>eng</language><creationdate>2011</creationdate><topic>Climate Change</topic><topic>Earth and Environmental Science</topic><topic>Earth Sciences</topic><topic>Freshwater & Marine Ecology</topic><topic>Geology</topic><topic>Original Paper</topic><topic>Paleontology</topic><topic>Physical Geography</topic><topic>Salvinia natans</topic><topic>Sedimentology</topic><toplevel>peer_reviewed</toplevel><toplevel>online_resources</toplevel><creatorcontrib>Święta-Musznicka, Joanna</creatorcontrib><creatorcontrib>Latałowa, Małgorzata</creatorcontrib><creatorcontrib>Szmeja, Józef</creatorcontrib><creatorcontrib>Badura, Monika</creatorcontrib><collection>SpringerOpen</collection><collection>CrossRef</collection><collection>Ecology Abstracts</collection><collection>Meteorological & Geoastrophysical Abstracts</collection><collection>Environmental Sciences and Pollution Management</collection><collection>ASFA: Aquatic Sciences and Fisheries Abstracts</collection><collection>Aquatic Science & Fisheries Abstracts (ASFA) 1: Biological Sciences & Living Resources</collection><collection>Aquatic Science & Fisheries Abstracts (ASFA) 2: Ocean Technology, Policy & Non-Living Resources</collection><collection>Meteorological & Geoastrophysical Abstracts - Academic</collection><collection>Aquatic Science & Fisheries Abstracts (ASFA) Professional</collection><jtitle>Journal of paleolimnology</jtitle></facets><delivery><delcategory>Remote Search Resource</delcategory><fulltext>fulltext</fulltext></delivery><addata><au>Święta-Musznicka, Joanna</au><au>Latałowa, Małgorzata</au><au>Szmeja, Józef</au><au>Badura, Monika</au><format>journal</format><genre>article</genre><ristype>JOUR</ristype><atitle>Salvinia natans in medieval wetland deposits in Gdańsk, northern Poland: evidence for the early medieval climate warming</atitle><jtitle>Journal of paleolimnology</jtitle><stitle>J Paleolimnol</stitle><date>2011-03-01</date><risdate>2011</risdate><volume>45</volume><issue>3</issue><spage>369</spage><epage>383</epage><pages>369-383</pages><issn>0921-2728</issn><eissn>1573-0417</eissn><abstract>Large numbers of sub-fossil remains of the aquatic fern
Salvinia natans
(L.) All. have been found in several early medieval sites in Gdańsk, N. Poland. This record indicates a population expansion of this species around 7th–8th century A.D., similar to the recently observed rapid spread and high population dynamics of
S. natans
in northern Poland, which recent studies have attributed to climate warming. Our results suggest that in the Vistula deltaic area the
S. natans
expansion in the Early Middle Ages (7th–8th century A.D.) was similarly stimulated by climate warming, while its subsequent decline was mainly due to climate cooling, especially during the Little Ice Age. Warmer winters and springs and a longer growing season seem to be the most important factors forcing the expansion of
S. natans
in medieval times. According to our data, the co-occurrence of
S. natans
with other aquatic plant species was similar in both the medieval and present-day vegetation. Also, the high density of
S. natans
in the medieval population caused impoverishment of the local ecosystems in a way that has been observed in recent water bodies affected by invasive pleustophytes (free-floating plants).</abstract><cop>Dordrecht</cop><pub>Springer Netherlands</pub><doi>10.1007/s10933-011-9505-1</doi><tpages>15</tpages><oa>free_for_read</oa></addata></record> |
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subjects | Climate Change Earth and Environmental Science Earth Sciences Freshwater & Marine Ecology Geology Original Paper Paleontology Physical Geography Salvinia natans Sedimentology |
title | Salvinia natans in medieval wetland deposits in Gdańsk, northern Poland: evidence for the early medieval climate warming |
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