Environmental controls on peatland testate amoebae (Protozoa: Rhizopoda) in the North of Ireland: Implications for Holocene palaeoclimate studies

The environmental controls on modern peatland testate amoebae (Protozoa: Rhizopoda) in the North of Ireland were investigated to assess the potential for Holocene palaeoclimate research within this region. Canonical Correspondence Analysis (CCA) revealed that hydrological factors (water table depth...

Ausführliche Beschreibung

Gespeichert in:
Bibliographische Detailangaben
Veröffentlicht in:Journal of paleolimnology 2009-07, Vol.42 (1), p.123-140
Hauptverfasser: Swindles, G. T., Charman, D. J., Roe, H. M., Sansum, P. A.
Format: Artikel
Sprache:eng
Schlagworte:
Online-Zugang:Volltext
Tags: Tag hinzufügen
Keine Tags, Fügen Sie den ersten Tag hinzu!
container_end_page 140
container_issue 1
container_start_page 123
container_title Journal of paleolimnology
container_volume 42
creator Swindles, G. T.
Charman, D. J.
Roe, H. M.
Sansum, P. A.
description The environmental controls on modern peatland testate amoebae (Protozoa: Rhizopoda) in the North of Ireland were investigated to assess the potential for Holocene palaeoclimate research within this region. Canonical Correspondence Analysis (CCA) revealed that hydrological factors (water table depth and moisture content) are the most important abiotic controls on organism distribution. A series of partial CCAs showed that water table depth explains 15.8% and moisture content explains 5.5% of the total variance. Monte-Carlo permutation tests showed that the results are highly significant ( p  
doi_str_mv 10.1007/s10933-008-9266-7
format Article
fullrecord <record><control><sourceid>proquest_cross</sourceid><recordid>TN_cdi_proquest_journals_872826997</recordid><sourceformat>XML</sourceformat><sourcesystem>PC</sourcesystem><sourcerecordid>1894942111</sourcerecordid><originalsourceid>FETCH-LOGICAL-a338t-33efc23416e0d7ca7bbb4968f8f30854fdcba32b432698116bf58324d9d0061c3</originalsourceid><addsrcrecordid>eNp1kM1q3DAURkVpINNJHiA7kVW6cKsfjyVnV0KaGQhJCM1ayPJVx4NH15U0geYt-saRmUJXXQku3_mu7iHkgrMvnDH1NXHWSlkxpqtWNE2lPpAFX6kyqbn6SBasFbwSSuhT8imlHWOs1Wq1IH9uw-sQMewhZDtShyFHHBPFQCewebShpxlSthmo3SN0FujVU8SMb2iv6fN2eMMJe_uZDoHmLdAHjHlL0dNNhJm-ppv9NA7O5gFDoh4jXeOIDgLQyY4W0I3Dfq5P-dAPkM7IibdjgvO_75K8fL_9cbOu7h_vNjff7isrpc6VlOCdkDVvgPXKWdV1Xd022msvmV7VvnedlaKrpWhazXnT-ZWWou7bnrGGO7kkl8feKeKvQznR7PAQQ1lpdPFUqFaVED-GXMSUIngzxfLb-NtwZmbx5ijeFPFmFm9mRhyZVLLhJ8R_xf-H3gHpZIiD</addsrcrecordid><sourcetype>Aggregation Database</sourcetype><iscdi>true</iscdi><recordtype>article</recordtype><pqid>872826997</pqid></control><display><type>article</type><title>Environmental controls on peatland testate amoebae (Protozoa: Rhizopoda) in the North of Ireland: Implications for Holocene palaeoclimate studies</title><source>SpringerLink Journals - AutoHoldings</source><creator>Swindles, G. T. ; Charman, D. J. ; Roe, H. M. ; Sansum, P. A.</creator><creatorcontrib>Swindles, G. T. ; Charman, D. J. ; Roe, H. M. ; Sansum, P. A.</creatorcontrib><description>The environmental controls on modern peatland testate amoebae (Protozoa: Rhizopoda) in the North of Ireland were investigated to assess the potential for Holocene palaeoclimate research within this region. Canonical Correspondence Analysis (CCA) revealed that hydrological factors (water table depth and moisture content) are the most important abiotic controls on organism distribution. A series of partial CCAs showed that water table depth explains 15.8% and moisture content explains 5.5% of the total variance. Monte-Carlo permutation tests showed that the results are highly significant ( p  &lt; 0.002; p  &lt; 0.040 respectively). Transfer functions were generated for water table depth using weighted averaging tolerance downweighted (WA-Tol) regression and for moisture content using weighted averaging partial least squares regression (WA-PLS). The performance of the models was assessed using leave-one-out cross-validation (jacknifing). After removal of outlier samples, the improved transfer functions were found to perform well with an r jack 2 and root mean square error of prediction jack of 0.83, 4.99 cm for water table depth and 0.76, 4.60% for moisture content respectively. The water table transfer function was applied to a fossil peat sequence from this region and reconstruction errors were generated by 1,000 bootstrap cycles. The water table reconstruction was also carried out using an established pan-European transfer function and was found to be similar to that based on the North of Ireland dataset. This demonstrates the persistent and comparable control of hydrological variables on the distribution of testate amoebae taxa across Europe and implies that regional training sets can suffice as long as no-analogue situations are not encountered.</description><identifier>ISSN: 0921-2728</identifier><identifier>EISSN: 1573-0417</identifier><identifier>DOI: 10.1007/s10933-008-9266-7</identifier><language>eng</language><publisher>Dordrecht: Springer Netherlands</publisher><subject>Climate Change ; Earth and Environmental Science ; Earth Sciences ; Freshwater &amp; Marine Ecology ; Geology ; Holocene ; Hydrology ; Limnology ; Moisture content ; Original Paper ; Paleoclimate ; Paleontology ; Peat ; Physical Geography ; Protozoa ; Sedimentology ; Water depth ; Water table ; Wetlands</subject><ispartof>Journal of paleolimnology, 2009-07, Vol.42 (1), p.123-140</ispartof><rights>Springer Science+Business Media B.V. 2008</rights><rights>Springer Science+Business Media B.V. 2009</rights><lds50>peer_reviewed</lds50><woscitedreferencessubscribed>false</woscitedreferencessubscribed><citedby>FETCH-LOGICAL-a338t-33efc23416e0d7ca7bbb4968f8f30854fdcba32b432698116bf58324d9d0061c3</citedby><cites>FETCH-LOGICAL-a338t-33efc23416e0d7ca7bbb4968f8f30854fdcba32b432698116bf58324d9d0061c3</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/s10933-008-9266-7$$EPDF$$P50$$Gspringer$$H</linktopdf><linktohtml>$$Uhttps://link.springer.com/10.1007/s10933-008-9266-7$$EHTML$$P50$$Gspringer$$H</linktohtml><link.rule.ids>314,780,784,27924,27925,41488,42557,51319</link.rule.ids></links><search><creatorcontrib>Swindles, G. T.</creatorcontrib><creatorcontrib>Charman, D. J.</creatorcontrib><creatorcontrib>Roe, H. M.</creatorcontrib><creatorcontrib>Sansum, P. A.</creatorcontrib><title>Environmental controls on peatland testate amoebae (Protozoa: Rhizopoda) in the North of Ireland: Implications for Holocene palaeoclimate studies</title><title>Journal of paleolimnology</title><addtitle>J Paleolimnol</addtitle><description>The environmental controls on modern peatland testate amoebae (Protozoa: Rhizopoda) in the North of Ireland were investigated to assess the potential for Holocene palaeoclimate research within this region. Canonical Correspondence Analysis (CCA) revealed that hydrological factors (water table depth and moisture content) are the most important abiotic controls on organism distribution. A series of partial CCAs showed that water table depth explains 15.8% and moisture content explains 5.5% of the total variance. Monte-Carlo permutation tests showed that the results are highly significant ( p  &lt; 0.002; p  &lt; 0.040 respectively). Transfer functions were generated for water table depth using weighted averaging tolerance downweighted (WA-Tol) regression and for moisture content using weighted averaging partial least squares regression (WA-PLS). The performance of the models was assessed using leave-one-out cross-validation (jacknifing). After removal of outlier samples, the improved transfer functions were found to perform well with an r jack 2 and root mean square error of prediction jack of 0.83, 4.99 cm for water table depth and 0.76, 4.60% for moisture content respectively. The water table transfer function was applied to a fossil peat sequence from this region and reconstruction errors were generated by 1,000 bootstrap cycles. The water table reconstruction was also carried out using an established pan-European transfer function and was found to be similar to that based on the North of Ireland dataset. This demonstrates the persistent and comparable control of hydrological variables on the distribution of testate amoebae taxa across Europe and implies that regional training sets can suffice as long as no-analogue situations are not encountered.</description><subject>Climate Change</subject><subject>Earth and Environmental Science</subject><subject>Earth Sciences</subject><subject>Freshwater &amp; Marine Ecology</subject><subject>Geology</subject><subject>Holocene</subject><subject>Hydrology</subject><subject>Limnology</subject><subject>Moisture content</subject><subject>Original Paper</subject><subject>Paleoclimate</subject><subject>Paleontology</subject><subject>Peat</subject><subject>Physical Geography</subject><subject>Protozoa</subject><subject>Sedimentology</subject><subject>Water depth</subject><subject>Water table</subject><subject>Wetlands</subject><issn>0921-2728</issn><issn>1573-0417</issn><fulltext>true</fulltext><rsrctype>article</rsrctype><creationdate>2009</creationdate><recordtype>article</recordtype><sourceid>AFKRA</sourceid><sourceid>AZQEC</sourceid><sourceid>BENPR</sourceid><sourceid>CCPQU</sourceid><sourceid>DWQXO</sourceid><sourceid>GNUQQ</sourceid><recordid>eNp1kM1q3DAURkVpINNJHiA7kVW6cKsfjyVnV0KaGQhJCM1ayPJVx4NH15U0geYt-saRmUJXXQku3_mu7iHkgrMvnDH1NXHWSlkxpqtWNE2lPpAFX6kyqbn6SBasFbwSSuhT8imlHWOs1Wq1IH9uw-sQMewhZDtShyFHHBPFQCewebShpxlSthmo3SN0FujVU8SMb2iv6fN2eMMJe_uZDoHmLdAHjHlL0dNNhJm-ppv9NA7O5gFDoh4jXeOIDgLQyY4W0I3Dfq5P-dAPkM7IibdjgvO_75K8fL_9cbOu7h_vNjff7isrpc6VlOCdkDVvgPXKWdV1Xd022msvmV7VvnedlaKrpWhazXnT-ZWWou7bnrGGO7kkl8feKeKvQznR7PAQQ1lpdPFUqFaVED-GXMSUIngzxfLb-NtwZmbx5ijeFPFmFm9mRhyZVLLhJ8R_xf-H3gHpZIiD</recordid><startdate>20090701</startdate><enddate>20090701</enddate><creator>Swindles, G. T.</creator><creator>Charman, D. J.</creator><creator>Roe, H. M.</creator><creator>Sansum, P. A.</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>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></search><sort><creationdate>20090701</creationdate><title>Environmental controls on peatland testate amoebae (Protozoa: Rhizopoda) in the North of Ireland: Implications for Holocene palaeoclimate studies</title><author>Swindles, G. T. ; Charman, D. J. ; Roe, H. M. ; Sansum, P. A.</author></sort><facets><frbrtype>5</frbrtype><frbrgroupid>cdi_FETCH-LOGICAL-a338t-33efc23416e0d7ca7bbb4968f8f30854fdcba32b432698116bf58324d9d0061c3</frbrgroupid><rsrctype>articles</rsrctype><prefilter>articles</prefilter><language>eng</language><creationdate>2009</creationdate><topic>Climate Change</topic><topic>Earth and Environmental Science</topic><topic>Earth Sciences</topic><topic>Freshwater &amp; Marine Ecology</topic><topic>Geology</topic><topic>Holocene</topic><topic>Hydrology</topic><topic>Limnology</topic><topic>Moisture content</topic><topic>Original Paper</topic><topic>Paleoclimate</topic><topic>Paleontology</topic><topic>Peat</topic><topic>Physical Geography</topic><topic>Protozoa</topic><topic>Sedimentology</topic><topic>Water depth</topic><topic>Water table</topic><topic>Wetlands</topic><toplevel>peer_reviewed</toplevel><toplevel>online_resources</toplevel><creatorcontrib>Swindles, G. T.</creatorcontrib><creatorcontrib>Charman, D. J.</creatorcontrib><creatorcontrib>Roe, H. M.</creatorcontrib><creatorcontrib>Sansum, P. A.</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>ProQuest SciTech Collection</collection><collection>ProQuest Natural Science Collection</collection><collection>ProQuest Central UK/Ireland</collection><collection>ProQuest Central Essentials</collection><collection>Biological Science Collection</collection><collection>ProQuest Central</collection><collection>Natural Science Collection</collection><collection>Earth, Atmospheric &amp; Aquatic Science Collection</collection><collection>Environmental Sciences and Pollution Management</collection><collection>ProQuest One Community College</collection><collection>ProQuest Central Korea</collection><collection>ASFA: Aquatic Sciences and Fisheries Abstracts</collection><collection>Engineering Research Database</collection><collection>ProQuest Central Student</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>SciTech Premium Collection</collection><collection>Aquatic Science &amp; Fisheries Abstracts (ASFA) Professional</collection><collection>ProQuest Biological Science Collection</collection><collection>Algology Mycology and Protozoology Abstracts (Microbiology C)</collection><collection>Biological Science Database</collection><collection>Biotechnology and BioEngineering Abstracts</collection><collection>Earth, Atmospheric &amp; Aquatic Science Database</collection><collection>ProQuest One Academic Eastern Edition (DO NOT USE)</collection><collection>ProQuest One Academic</collection><collection>ProQuest One Academic UKI Edition</collection><jtitle>Journal of paleolimnology</jtitle></facets><delivery><delcategory>Remote Search Resource</delcategory><fulltext>fulltext</fulltext></delivery><addata><au>Swindles, G. T.</au><au>Charman, D. J.</au><au>Roe, H. M.</au><au>Sansum, P. A.</au><format>journal</format><genre>article</genre><ristype>JOUR</ristype><atitle>Environmental controls on peatland testate amoebae (Protozoa: Rhizopoda) in the North of Ireland: Implications for Holocene palaeoclimate studies</atitle><jtitle>Journal of paleolimnology</jtitle><stitle>J Paleolimnol</stitle><date>2009-07-01</date><risdate>2009</risdate><volume>42</volume><issue>1</issue><spage>123</spage><epage>140</epage><pages>123-140</pages><issn>0921-2728</issn><eissn>1573-0417</eissn><abstract>The environmental controls on modern peatland testate amoebae (Protozoa: Rhizopoda) in the North of Ireland were investigated to assess the potential for Holocene palaeoclimate research within this region. Canonical Correspondence Analysis (CCA) revealed that hydrological factors (water table depth and moisture content) are the most important abiotic controls on organism distribution. A series of partial CCAs showed that water table depth explains 15.8% and moisture content explains 5.5% of the total variance. Monte-Carlo permutation tests showed that the results are highly significant ( p  &lt; 0.002; p  &lt; 0.040 respectively). Transfer functions were generated for water table depth using weighted averaging tolerance downweighted (WA-Tol) regression and for moisture content using weighted averaging partial least squares regression (WA-PLS). The performance of the models was assessed using leave-one-out cross-validation (jacknifing). After removal of outlier samples, the improved transfer functions were found to perform well with an r jack 2 and root mean square error of prediction jack of 0.83, 4.99 cm for water table depth and 0.76, 4.60% for moisture content respectively. The water table transfer function was applied to a fossil peat sequence from this region and reconstruction errors were generated by 1,000 bootstrap cycles. The water table reconstruction was also carried out using an established pan-European transfer function and was found to be similar to that based on the North of Ireland dataset. This demonstrates the persistent and comparable control of hydrological variables on the distribution of testate amoebae taxa across Europe and implies that regional training sets can suffice as long as no-analogue situations are not encountered.</abstract><cop>Dordrecht</cop><pub>Springer Netherlands</pub><doi>10.1007/s10933-008-9266-7</doi><tpages>18</tpages></addata></record>
fulltext fulltext
identifier ISSN: 0921-2728
ispartof Journal of paleolimnology, 2009-07, Vol.42 (1), p.123-140
issn 0921-2728
1573-0417
language eng
recordid cdi_proquest_journals_872826997
source SpringerLink Journals - AutoHoldings
subjects Climate Change
Earth and Environmental Science
Earth Sciences
Freshwater & Marine Ecology
Geology
Holocene
Hydrology
Limnology
Moisture content
Original Paper
Paleoclimate
Paleontology
Peat
Physical Geography
Protozoa
Sedimentology
Water depth
Water table
Wetlands
title Environmental controls on peatland testate amoebae (Protozoa: Rhizopoda) in the North of Ireland: Implications for Holocene palaeoclimate studies
url https://sfx.bib-bvb.de/sfx_tum?ctx_ver=Z39.88-2004&ctx_enc=info:ofi/enc:UTF-8&ctx_tim=2025-01-05T09%3A27%3A04IST&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=Environmental%20controls%20on%20peatland%20testate%20amoebae%20(Protozoa:%20Rhizopoda)%20in%20the%20North%20of%20Ireland:%20Implications%20for%20Holocene%20palaeoclimate%20studies&rft.jtitle=Journal%20of%20paleolimnology&rft.au=Swindles,%20G.%20T.&rft.date=2009-07-01&rft.volume=42&rft.issue=1&rft.spage=123&rft.epage=140&rft.pages=123-140&rft.issn=0921-2728&rft.eissn=1573-0417&rft_id=info:doi/10.1007/s10933-008-9266-7&rft_dat=%3Cproquest_cross%3E1894942111%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=872826997&rft_id=info:pmid/&rfr_iscdi=true