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Compositional turnover and variation in Eemian pollen sequences in Europe
The Eemian interglacial represents a natural experiment on how past vegetation with negligible human impact responded to amplified temperature changes compared to the Holocene. Here, we assemble 47 carefully selected Eemian pollen sequences from Europe to explore geographical patterns of (1) total c...
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Published in: | Vegetation history and archaeobotany 2020, Vol.29 (1), p.101-109 |
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creator | Felde, Vivian A. Flantua, Suzette G. A. Jenks, Cathy R. Benito, Blas M. de Beaulieu, Jacques-Louis Kuneš, Petr Magri, Donatella Nalepka, Dorota Risebrobakken, Bjørg ter Braak, Cajo J. F. Allen, Judy R. M. Granoszewski, Wojciech Helmens, Karin F. Huntley, Brian Kondratienė, Ona Kalniņa, Laimdota Kupryjanowicz, Mirosława Malkiewicz, Małgorzata Milner, Alice M. Nita, Małgorzata Noryśkiewicz, Bożena Pidek, Irena A. Reille, Maurice Salonen, J. Sakari Šeirienė, Vaida Winter, Hanna Tzedakis, Polychronis C. Birks, H. John B. |
description | The Eemian interglacial represents a natural experiment on how past vegetation with negligible human impact responded to amplified temperature changes compared to the Holocene. Here, we assemble 47 carefully selected Eemian pollen sequences from Europe to explore geographical patterns of (1) total compositional turnover and total variation for each sequence and (2) stratigraphical turnover between samples within each sequence using detrended canonical correspondence analysis, multivariate regression trees, and principal curves. Our synthesis shows that turnover and variation are highest in central Europe (47–55°N), low in southern Europe (south of 45°N), and lowest in the north (above 60°N). These results provide a basis for developing hypotheses about causes of vegetation change during the Eemian and their possible drivers. |
doi_str_mv | 10.1007/s00334-019-00726-5 |
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A. ; Jenks, Cathy R. ; Benito, Blas M. ; de Beaulieu, Jacques-Louis ; Kuneš, Petr ; Magri, Donatella ; Nalepka, Dorota ; Risebrobakken, Bjørg ; ter Braak, Cajo J. F. ; Allen, Judy R. M. ; Granoszewski, Wojciech ; Helmens, Karin F. ; Huntley, Brian ; Kondratienė, Ona ; Kalniņa, Laimdota ; Kupryjanowicz, Mirosława ; Malkiewicz, Małgorzata ; Milner, Alice M. ; Nita, Małgorzata ; Noryśkiewicz, Bożena ; Pidek, Irena A. ; Reille, Maurice ; Salonen, J. Sakari ; Šeirienė, Vaida ; Winter, Hanna ; Tzedakis, Polychronis C. ; Birks, H. John B.</creator><creatorcontrib>Felde, Vivian A. ; Flantua, Suzette G. A. ; Jenks, Cathy R. ; Benito, Blas M. ; de Beaulieu, Jacques-Louis ; Kuneš, Petr ; Magri, Donatella ; Nalepka, Dorota ; Risebrobakken, Bjørg ; ter Braak, Cajo J. F. ; Allen, Judy R. 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Our synthesis shows that turnover and variation are highest in central Europe (47–55°N), low in southern Europe (south of 45°N), and lowest in the north (above 60°N). 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John B.</creatorcontrib><title>Compositional turnover and variation in Eemian pollen sequences in Europe</title><title>Vegetation history and archaeobotany</title><addtitle>Veget Hist Archaeobot</addtitle><description>The Eemian interglacial represents a natural experiment on how past vegetation with negligible human impact responded to amplified temperature changes compared to the Holocene. Here, we assemble 47 carefully selected Eemian pollen sequences from Europe to explore geographical patterns of (1) total compositional turnover and total variation for each sequence and (2) stratigraphical turnover between samples within each sequence using detrended canonical correspondence analysis, multivariate regression trees, and principal curves. Our synthesis shows that turnover and variation are highest in central Europe (47–55°N), low in southern Europe (south of 45°N), and lowest in the north (above 60°N). These results provide a basis for developing hypotheses about causes of vegetation change during the Eemian and their possible drivers.</description><subject>Anthropology</subject><subject>Archaeology</subject><subject>Biogeosciences</subject><subject>Climate Change</subject><subject>Detrended canonical correspondence analysis</subject><subject>Earth and Environmental Science</subject><subject>Earth Sciences</subject><subject>Environmental Sciences</subject><subject>Extrinsic and intrinsic processes</subject><subject>Holocene</subject><subject>Human impact</subject><subject>Human influences</subject><subject>Human-environment relationship</subject><subject>Inertia</subject><subject>Last interglacial dataset</subject><subject>Multivariate regression trees</subject><subject>Neutral processes</subject><subject>Paleontology</subject><subject>Pollen</subject><subject>Principal curves</subject><subject>Regression analysis</subject><subject>Short Communication</subject><subject>Variation</subject><subject>Vegetation</subject><issn>0939-6314</issn><issn>1617-6278</issn><issn>1617-6278</issn><fulltext>true</fulltext><rsrctype>article</rsrctype><creationdate>2020</creationdate><recordtype>article</recordtype><recordid>eNp9kcFOwzAMhiMEEmPwApwqcUKi4CRt0hynMdikSVyAa5S26ejUJSVph3h70hWBuHCybH_-ZftH6BLDLQbgdx6A0iQGLOKQEhanR2iCGeYxIzw7RhMQVMSM4uQUnXm_BcCcpzBBq7ndtdbXXW2NaqKud8butYuUKaO9crUaGlFtooXe1cpErW0abSKv33ttCu0Prd7ZVp-jk0o1Xl98xyl6eVg8z5fx-ulxNZ-tY5WkvItJluMi47mgSjDNGS25YBWkIi-zqlA0JaxMdJJDUTGdA1cKaEIFwQKrUrOUTtHNqOs_dNvnsnX1TrlPaVUt7-vXmbRuI30vcQYsGfDrEX9TzR92OVvLoQYEBAbM9jiwVyPbOhvu853c2vCQcI0klFLg4aNJoMhIFc5673T1I4tBDm7I0Q0Z3JAHN-SwBv3eOsBmo92v9D9TX_J6i_U</recordid><startdate>2020</startdate><enddate>2020</enddate><creator>Felde, Vivian A.</creator><creator>Flantua, Suzette G. 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John B.</au><format>journal</format><genre>article</genre><ristype>JOUR</ristype><atitle>Compositional turnover and variation in Eemian pollen sequences in Europe</atitle><jtitle>Vegetation history and archaeobotany</jtitle><stitle>Veget Hist Archaeobot</stitle><date>2020</date><risdate>2020</risdate><volume>29</volume><issue>1</issue><spage>101</spage><epage>109</epage><pages>101-109</pages><issn>0939-6314</issn><issn>1617-6278</issn><eissn>1617-6278</eissn><abstract>The Eemian interglacial represents a natural experiment on how past vegetation with negligible human impact responded to amplified temperature changes compared to the Holocene. 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ispartof | Vegetation history and archaeobotany, 2020, Vol.29 (1), p.101-109 |
issn | 0939-6314 1617-6278 1617-6278 |
language | eng |
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source | JSTOR Archival Journals and Primary Sources Collection; Springer Link |
subjects | Anthropology Archaeology Biogeosciences Climate Change Detrended canonical correspondence analysis Earth and Environmental Science Earth Sciences Environmental Sciences Extrinsic and intrinsic processes Holocene Human impact Human influences Human-environment relationship Inertia Last interglacial dataset Multivariate regression trees Neutral processes Paleontology Pollen Principal curves Regression analysis Short Communication Variation Vegetation |
title | Compositional turnover and variation in Eemian pollen sequences in Europe |
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