LEAF MARGIN ANALYSIS: A NEW EQUATION FROM HUMID TO MESIC FORESTS IN CHINA

Leaf margin analysis (LMA) is a widely used method that applies present-day linear correlation between the proportion of woody dicotyledonous species with untoothed leaves (P) and mean annual temperature (MAT) to estimate paleotemperatures from fossil leaf floras. Previous works demonstrate that LMA...

Ausführliche Beschreibung

Gespeichert in:
Bibliographische Detailangaben
Veröffentlicht in:Palaios 2010-04, Vol.25 (4), p.234-238
Hauptverfasser: SU, TAO, XING, YAO-WU, LIU, YU-SHENG (CHRISTOPHER), JACQUES, FRÉDÉRIC M.B, CHEN, WEN-YUN, HUANG, YONG-JIANG, ZHOU, ZHE-KUN
Format: Artikel
Sprache:eng
Schlagworte:
Online-Zugang:Volltext
Tags: Tag hinzufügen
Keine Tags, Fügen Sie den ersten Tag hinzu!
container_end_page 238
container_issue 4
container_start_page 234
container_title Palaios
container_volume 25
creator SU, TAO
XING, YAO-WU
LIU, YU-SHENG (CHRISTOPHER)
JACQUES, FRÉDÉRIC M.B
CHEN, WEN-YUN
HUANG, YONG-JIANG
ZHOU, ZHE-KUN
description Leaf margin analysis (LMA) is a widely used method that applies present-day linear correlation between the proportion of woody dicotyledonous species with untoothed leaves (P) and mean annual temperature (MAT) to estimate paleotemperatures from fossil leaf floras. Previous works demonstrate that LMA shows regional constraints and to date, no equation has been modeled directly from Chinese forests. Fifty humid to mesic Chinese forests were chosen to understand the relationship between percentage of untoothed leaf species and MAT in China. Consistent with previous studies, the Chinese data indicate that P shows a strong linear correlation with MAT, but the actual relationship is a little different from those recognized from other regions. Among the several currently used LMA equations, the one resulting from North and Central American and Japanese data, rather than the widely used East Asian LMA equation, yields the closest values to the actual MATs of the Chinese samples (mean absolute error = 1.9 °C). A new equation derived from the Chinese forests is therefore developed, where MAT = 1.038 + 27.6 × P. This study not only demonstrates the similarity of the relationship between P and MAT in the Northern Hemisphere, but also improves the reliability of LMA for paleoclimate reconstructions of Chinese paleofloras.
doi_str_mv 10.2110/palo.2009.p09-129r
format Article
fullrecord <record><control><sourceid>jstor_proqu</sourceid><recordid>TN_cdi_proquest_miscellaneous_923191171</recordid><sourceformat>XML</sourceformat><sourcesystem>PC</sourcesystem><jstor_id>40606490</jstor_id><sourcerecordid>40606490</sourcerecordid><originalsourceid>FETCH-LOGICAL-a433t-c26fee40c595ec0754495bbd6913447a49251b432b961744045fa895f58a343c3</originalsourceid><addsrcrecordid>eNqNkE1r20AQhpfSQt0kf6BQ2FsPRe7Mfkja3oQrxwJbopZN6GmRlFWxUbzurk3pv88KhV6b0xzmed8ZHkI-IswZInw9N4OdMwA1P4OKkCn3hsxQ8TSSnPG3ZAZpyiPkEt-TD94fAVCCZDNSrPNsSTfZ9r4oaVZm6591UX-jGS3zB5r_2Ge7oirpcltt6Gq_Kb7TXUU3eV0s6LLa5vWupiG3WBVldkve9c3gzd3LvCH7Zb5brKJ1dV8ssnXUCM4vUcfi3hgBnVTSdJBIIZRs28dYIRciaYRiElvBWatiTIQAIfsmVbKXacMF7_gN-Tz1np39fTX-op8OvjPD0JyMvXqtGEeFmOD_SUhQhksQSDaRnbPeO9Prszs8Ne6vRtCjYD0K1qNgHQTrUXAIfZpCR3-x7l9CQAyxUGPpl2n_y1jfHcypM3-sGx710V7dKSgKfaEZeJIoHmiY6PZg7cm85oFntl-OwA</addsrcrecordid><sourcetype>Aggregation Database</sourcetype><iscdi>true</iscdi><recordtype>article</recordtype><pqid>907154320</pqid></control><display><type>article</type><title>LEAF MARGIN ANALYSIS: A NEW EQUATION FROM HUMID TO MESIC FORESTS IN CHINA</title><source>BioOne Complete</source><source>Jstor Complete Legacy</source><creator>SU, TAO ; XING, YAO-WU ; LIU, YU-SHENG (CHRISTOPHER) ; JACQUES, FRÉDÉRIC M.B ; CHEN, WEN-YUN ; HUANG, YONG-JIANG ; ZHOU, ZHE-KUN</creator><creatorcontrib>SU, TAO ; XING, YAO-WU ; LIU, YU-SHENG (CHRISTOPHER) ; JACQUES, FRÉDÉRIC M.B ; CHEN, WEN-YUN ; HUANG, YONG-JIANG ; ZHOU, ZHE-KUN</creatorcontrib><description>Leaf margin analysis (LMA) is a widely used method that applies present-day linear correlation between the proportion of woody dicotyledonous species with untoothed leaves (P) and mean annual temperature (MAT) to estimate paleotemperatures from fossil leaf floras. Previous works demonstrate that LMA shows regional constraints and to date, no equation has been modeled directly from Chinese forests. Fifty humid to mesic Chinese forests were chosen to understand the relationship between percentage of untoothed leaf species and MAT in China. Consistent with previous studies, the Chinese data indicate that P shows a strong linear correlation with MAT, but the actual relationship is a little different from those recognized from other regions. Among the several currently used LMA equations, the one resulting from North and Central American and Japanese data, rather than the widely used East Asian LMA equation, yields the closest values to the actual MATs of the Chinese samples (mean absolute error = 1.9 °C). A new equation derived from the Chinese forests is therefore developed, where MAT = 1.038 + 27.6 × P. This study not only demonstrates the similarity of the relationship between P and MAT in the Northern Hemisphere, but also improves the reliability of LMA for paleoclimate reconstructions of Chinese paleofloras.</description><identifier>ISSN: 0883-1351</identifier><identifier>EISSN: 1938-5323</identifier><identifier>DOI: 10.2110/palo.2009.p09-129r</identifier><language>eng</language><publisher>SEPM Society for Sedimentary Geology, 4111 S Darlington, Suite 100, Tulsa, OK 74135-6373, U.S.A: SEPM Society for Sedimentary Geology</publisher><subject>algorithms ; Angiospermae ; Asia ; China ; Climate models ; Correlations ; Datasets ; Dicotyledoneae ; Far East ; Flora ; Fossils ; Global climate models ; leaf margin analysis ; Leaves ; living taxa ; modern analogs ; morphology ; Paleobotany ; Paleoclimatology ; paleotemperature ; Plantae ; Research s ; Spermatophyta ; statistical analysis ; Tropical regions ; Vegetation</subject><ispartof>Palaios, 2010-04, Vol.25 (4), p.234-238</ispartof><rights>SEPM (Society for Sedimentary Geology)</rights><rights>GeoRef, Copyright 2020, American Geosciences Institute. Reference includes data from GeoScienceWorld @Alexandria, VA @USA @United States. Reference includes data supplied by SEPM (Society for Sedimentary Geology) @Tulsa, OK @USA @United States</rights><rights>2010 SEPM (Society for Sedimentary Geology)</rights><lds50>peer_reviewed</lds50><woscitedreferencessubscribed>false</woscitedreferencessubscribed><citedby>FETCH-LOGICAL-a433t-c26fee40c595ec0754495bbd6913447a49251b432b961744045fa895f58a343c3</citedby></display><links><openurl>$$Topenurl_article</openurl><openurlfulltext>$$Topenurlfull_article</openurlfulltext><thumbnail>$$Tsyndetics_thumb_exl</thumbnail><linktopdf>$$Uhttps://bioone.org/doi/pdf/10.2110/palo.2009.p09-129r$$EPDF$$P50$$Gbioone$$H</linktopdf><linktohtml>$$Uhttps://www.jstor.org/stable/40606490$$EHTML$$P50$$Gjstor$$H</linktohtml><link.rule.ids>314,777,781,800,26959,27905,27906,52344,57998,58231</link.rule.ids></links><search><creatorcontrib>SU, TAO</creatorcontrib><creatorcontrib>XING, YAO-WU</creatorcontrib><creatorcontrib>LIU, YU-SHENG (CHRISTOPHER)</creatorcontrib><creatorcontrib>JACQUES, FRÉDÉRIC M.B</creatorcontrib><creatorcontrib>CHEN, WEN-YUN</creatorcontrib><creatorcontrib>HUANG, YONG-JIANG</creatorcontrib><creatorcontrib>ZHOU, ZHE-KUN</creatorcontrib><title>LEAF MARGIN ANALYSIS: A NEW EQUATION FROM HUMID TO MESIC FORESTS IN CHINA</title><title>Palaios</title><description>Leaf margin analysis (LMA) is a widely used method that applies present-day linear correlation between the proportion of woody dicotyledonous species with untoothed leaves (P) and mean annual temperature (MAT) to estimate paleotemperatures from fossil leaf floras. Previous works demonstrate that LMA shows regional constraints and to date, no equation has been modeled directly from Chinese forests. Fifty humid to mesic Chinese forests were chosen to understand the relationship between percentage of untoothed leaf species and MAT in China. Consistent with previous studies, the Chinese data indicate that P shows a strong linear correlation with MAT, but the actual relationship is a little different from those recognized from other regions. Among the several currently used LMA equations, the one resulting from North and Central American and Japanese data, rather than the widely used East Asian LMA equation, yields the closest values to the actual MATs of the Chinese samples (mean absolute error = 1.9 °C). A new equation derived from the Chinese forests is therefore developed, where MAT = 1.038 + 27.6 × P. This study not only demonstrates the similarity of the relationship between P and MAT in the Northern Hemisphere, but also improves the reliability of LMA for paleoclimate reconstructions of Chinese paleofloras.</description><subject>algorithms</subject><subject>Angiospermae</subject><subject>Asia</subject><subject>China</subject><subject>Climate models</subject><subject>Correlations</subject><subject>Datasets</subject><subject>Dicotyledoneae</subject><subject>Far East</subject><subject>Flora</subject><subject>Fossils</subject><subject>Global climate models</subject><subject>leaf margin analysis</subject><subject>Leaves</subject><subject>living taxa</subject><subject>modern analogs</subject><subject>morphology</subject><subject>Paleobotany</subject><subject>Paleoclimatology</subject><subject>paleotemperature</subject><subject>Plantae</subject><subject>Research s</subject><subject>Spermatophyta</subject><subject>statistical analysis</subject><subject>Tropical regions</subject><subject>Vegetation</subject><issn>0883-1351</issn><issn>1938-5323</issn><fulltext>true</fulltext><rsrctype>article</rsrctype><creationdate>2010</creationdate><recordtype>article</recordtype><recordid>eNqNkE1r20AQhpfSQt0kf6BQ2FsPRe7Mfkja3oQrxwJbopZN6GmRlFWxUbzurk3pv88KhV6b0xzmed8ZHkI-IswZInw9N4OdMwA1P4OKkCn3hsxQ8TSSnPG3ZAZpyiPkEt-TD94fAVCCZDNSrPNsSTfZ9r4oaVZm6591UX-jGS3zB5r_2Ge7oirpcltt6Gq_Kb7TXUU3eV0s6LLa5vWupiG3WBVldkve9c3gzd3LvCH7Zb5brKJ1dV8ssnXUCM4vUcfi3hgBnVTSdJBIIZRs28dYIRciaYRiElvBWatiTIQAIfsmVbKXacMF7_gN-Tz1np39fTX-op8OvjPD0JyMvXqtGEeFmOD_SUhQhksQSDaRnbPeO9Prszs8Ne6vRtCjYD0K1qNgHQTrUXAIfZpCR3-x7l9CQAyxUGPpl2n_y1jfHcypM3-sGx710V7dKSgKfaEZeJIoHmiY6PZg7cm85oFntl-OwA</recordid><startdate>201004</startdate><enddate>201004</enddate><creator>SU, TAO</creator><creator>XING, YAO-WU</creator><creator>LIU, YU-SHENG (CHRISTOPHER)</creator><creator>JACQUES, FRÉDÉRIC M.B</creator><creator>CHEN, WEN-YUN</creator><creator>HUANG, YONG-JIANG</creator><creator>ZHOU, ZHE-KUN</creator><general>SEPM Society for Sedimentary Geology</general><general>Society for Sedimentary Geology</general><general>SEPM (Society for Sedimentary Geology)</general><scope>AAYXX</scope><scope>CITATION</scope><scope>7SN</scope><scope>C1K</scope></search><sort><creationdate>201004</creationdate><title>LEAF MARGIN ANALYSIS: A NEW EQUATION FROM HUMID TO MESIC FORESTS IN CHINA</title><author>SU, TAO ; XING, YAO-WU ; LIU, YU-SHENG (CHRISTOPHER) ; JACQUES, FRÉDÉRIC M.B ; CHEN, WEN-YUN ; HUANG, YONG-JIANG ; ZHOU, ZHE-KUN</author></sort><facets><frbrtype>5</frbrtype><frbrgroupid>cdi_FETCH-LOGICAL-a433t-c26fee40c595ec0754495bbd6913447a49251b432b961744045fa895f58a343c3</frbrgroupid><rsrctype>articles</rsrctype><prefilter>articles</prefilter><language>eng</language><creationdate>2010</creationdate><topic>algorithms</topic><topic>Angiospermae</topic><topic>Asia</topic><topic>China</topic><topic>Climate models</topic><topic>Correlations</topic><topic>Datasets</topic><topic>Dicotyledoneae</topic><topic>Far East</topic><topic>Flora</topic><topic>Fossils</topic><topic>Global climate models</topic><topic>leaf margin analysis</topic><topic>Leaves</topic><topic>living taxa</topic><topic>modern analogs</topic><topic>morphology</topic><topic>Paleobotany</topic><topic>Paleoclimatology</topic><topic>paleotemperature</topic><topic>Plantae</topic><topic>Research s</topic><topic>Spermatophyta</topic><topic>statistical analysis</topic><topic>Tropical regions</topic><topic>Vegetation</topic><toplevel>peer_reviewed</toplevel><toplevel>online_resources</toplevel><creatorcontrib>SU, TAO</creatorcontrib><creatorcontrib>XING, YAO-WU</creatorcontrib><creatorcontrib>LIU, YU-SHENG (CHRISTOPHER)</creatorcontrib><creatorcontrib>JACQUES, FRÉDÉRIC M.B</creatorcontrib><creatorcontrib>CHEN, WEN-YUN</creatorcontrib><creatorcontrib>HUANG, YONG-JIANG</creatorcontrib><creatorcontrib>ZHOU, ZHE-KUN</creatorcontrib><collection>CrossRef</collection><collection>Ecology Abstracts</collection><collection>Environmental Sciences and Pollution Management</collection><jtitle>Palaios</jtitle></facets><delivery><delcategory>Remote Search Resource</delcategory><fulltext>fulltext</fulltext></delivery><addata><au>SU, TAO</au><au>XING, YAO-WU</au><au>LIU, YU-SHENG (CHRISTOPHER)</au><au>JACQUES, FRÉDÉRIC M.B</au><au>CHEN, WEN-YUN</au><au>HUANG, YONG-JIANG</au><au>ZHOU, ZHE-KUN</au><format>journal</format><genre>article</genre><ristype>JOUR</ristype><atitle>LEAF MARGIN ANALYSIS: A NEW EQUATION FROM HUMID TO MESIC FORESTS IN CHINA</atitle><jtitle>Palaios</jtitle><date>2010-04</date><risdate>2010</risdate><volume>25</volume><issue>4</issue><spage>234</spage><epage>238</epage><pages>234-238</pages><issn>0883-1351</issn><eissn>1938-5323</eissn><abstract>Leaf margin analysis (LMA) is a widely used method that applies present-day linear correlation between the proportion of woody dicotyledonous species with untoothed leaves (P) and mean annual temperature (MAT) to estimate paleotemperatures from fossil leaf floras. Previous works demonstrate that LMA shows regional constraints and to date, no equation has been modeled directly from Chinese forests. Fifty humid to mesic Chinese forests were chosen to understand the relationship between percentage of untoothed leaf species and MAT in China. Consistent with previous studies, the Chinese data indicate that P shows a strong linear correlation with MAT, but the actual relationship is a little different from those recognized from other regions. Among the several currently used LMA equations, the one resulting from North and Central American and Japanese data, rather than the widely used East Asian LMA equation, yields the closest values to the actual MATs of the Chinese samples (mean absolute error = 1.9 °C). A new equation derived from the Chinese forests is therefore developed, where MAT = 1.038 + 27.6 × P. This study not only demonstrates the similarity of the relationship between P and MAT in the Northern Hemisphere, but also improves the reliability of LMA for paleoclimate reconstructions of Chinese paleofloras.</abstract><cop>SEPM Society for Sedimentary Geology, 4111 S Darlington, Suite 100, Tulsa, OK 74135-6373, U.S.A</cop><pub>SEPM Society for Sedimentary Geology</pub><doi>10.2110/palo.2009.p09-129r</doi><tpages>5</tpages></addata></record>
fulltext fulltext
identifier ISSN: 0883-1351
ispartof Palaios, 2010-04, Vol.25 (4), p.234-238
issn 0883-1351
1938-5323
language eng
recordid cdi_proquest_miscellaneous_923191171
source BioOne Complete; Jstor Complete Legacy
subjects algorithms
Angiospermae
Asia
China
Climate models
Correlations
Datasets
Dicotyledoneae
Far East
Flora
Fossils
Global climate models
leaf margin analysis
Leaves
living taxa
modern analogs
morphology
Paleobotany
Paleoclimatology
paleotemperature
Plantae
Research s
Spermatophyta
statistical analysis
Tropical regions
Vegetation
title LEAF MARGIN ANALYSIS: A NEW EQUATION FROM HUMID TO MESIC FORESTS IN CHINA
url https://sfx.bib-bvb.de/sfx_tum?ctx_ver=Z39.88-2004&ctx_enc=info:ofi/enc:UTF-8&ctx_tim=2025-01-19T05%3A53%3A53IST&url_ver=Z39.88-2004&url_ctx_fmt=infofi/fmt:kev:mtx:ctx&rfr_id=info:sid/primo.exlibrisgroup.com:primo3-Article-jstor_proqu&rft_val_fmt=info:ofi/fmt:kev:mtx:journal&rft.genre=article&rft.atitle=LEAF%20MARGIN%20ANALYSIS:%20A%20NEW%20EQUATION%20FROM%20HUMID%20TO%20MESIC%20FORESTS%20IN%20CHINA&rft.jtitle=Palaios&rft.au=SU,%20TAO&rft.date=2010-04&rft.volume=25&rft.issue=4&rft.spage=234&rft.epage=238&rft.pages=234-238&rft.issn=0883-1351&rft.eissn=1938-5323&rft_id=info:doi/10.2110/palo.2009.p09-129r&rft_dat=%3Cjstor_proqu%3E40606490%3C/jstor_proqu%3E%3Curl%3E%3C/url%3E&disable_directlink=true&sfx.directlink=off&sfx.report_link=0&rft_id=info:oai/&rft_pqid=907154320&rft_id=info:pmid/&rft_jstor_id=40606490&rfr_iscdi=true