Variations in nitrogen-15 natural abundance of plant and soil systems in four remote tropical rainforests, southern China.
Identifieur interne : 001742 ( Main/Exploration ); précédent : 001741; suivant : 001743Variations in nitrogen-15 natural abundance of plant and soil systems in four remote tropical rainforests, southern China.
Auteurs : Ang Wang [République populaire de Chine] ; Yun-Ting Fang ; De-Xiang Chen ; Keisuke Koba ; Akiko Makabe ; Yi-De Li ; Tu-Shou Luo ; Muneoki YohSource :
- Oecologia [ 1432-1939 ] ; 2014.
Descripteurs français
- KwdFr :
- MESH :
- analyse : Isotopes de l'azote.
- composition chimique : Feuilles de plante, Plantes, Sol.
- microbiologie : Plantes.
- Arbres, Biomasse, Chine, Cycle de l'azote, Mycorhizes, Écosystème.
English descriptors
- KwdEn :
- MESH :
- chemical , analysis : Nitrogen Isotopes.
- chemistry : Plant Leaves, Plants, Soil.
- microbiology : Plants.
- Biomass, China, Ecosystem, Mycorrhizae, Nitrogen Cycle, Trees.
Abstract
The foliar stable N isotope ratio (δ(15)N) can provide integrated information on ecosystem N cycling. Here we present the δ(15)N of plant and soil in four remote typical tropical rainforests (one primary and three secondary) of southern China. We aimed to examine if (1) foliar δ(15)N in the study forests is negative, as observed in other tropical and subtropical sites in eastern Asia; (2) variation in δ(15)N among different species is smaller compared to that in many N-limited temperate and boreal ecosystems; and (3) the primary forest is more N rich than the younger secondary forests and therefore is more (15)N enriched. Our results show that foliar δ(15)N ranged from -5.1 to 1.3‰ for 39 collected plant species with different growth strategies and mycorrhizal types, and that for 35 species it was negative. Soil NO3 (-) had low δ(15)N (-11.4 to -3.2‰) and plant NO3 (-) uptake could not explain the negative foliar δ(15)N values (NH4 (+) was dominant in the soil inorganic-N fraction). We suggest that negative values might be caused by isotope fractionation during soil NH4 (+) uptake and mycorrhizal N transfer, and by direct uptake of atmospheric NH3/NH4 (+). The variation in foliar δ(15)N among species (by about 6‰) was smaller than in many N-limited ecosystems, which is typically about or over 10‰. The primary forest had a larger N capital in plants than the secondary forests. Foliar δ(15)N and the enrichment factor (foliar δ(15)N minus soil δ(15)N) were higher in the primary forest than in the secondary forests, albeit differences were small, while there was no consistent pattern in soil δ(15)N between primary and secondary forests.
DOI: 10.1007/s00442-013-2778-5
PubMed: 24085637
Affiliations:
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sortKey="Koba, Keisuke" sort="Koba, Keisuke" uniqKey="Koba K" first="Keisuke" last="Koba">Keisuke Koba</name></author><author><name sortKey="Makabe, Akiko" sort="Makabe, Akiko" uniqKey="Makabe A" first="Akiko" last="Makabe">Akiko Makabe</name></author><author><name sortKey="Li, Yi De" sort="Li, Yi De" uniqKey="Li Y" first="Yi-De" last="Li">Yi-De Li</name></author><author><name sortKey="Luo, Tu Shou" sort="Luo, Tu Shou" uniqKey="Luo T" first="Tu-Shou" last="Luo">Tu-Shou Luo</name></author><author><name sortKey="Yoh, Muneoki" sort="Yoh, Muneoki" uniqKey="Yoh M" first="Muneoki" last="Yoh">Muneoki Yoh</name></author></titleStmt><publicationStmt><idno type="wicri:source">PubMed</idno><date when="2014">2014</date><idno type="RBID">pubmed:24085637</idno><idno type="pmid">24085637</idno><idno type="doi">10.1007/s00442-013-2778-5</idno><idno type="wicri:Area/Main/Corpus">001A92</idno><idno type="wicri:explorRef" wicri:stream="Main" wicri:step="Corpus" wicri:corpus="PubMed">001A92</idno><idno 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last="Fang">Yun-Ting Fang</name></author><author><name sortKey="Chen, De Xiang" sort="Chen, De Xiang" uniqKey="Chen D" first="De-Xiang" last="Chen">De-Xiang Chen</name></author><author><name sortKey="Koba, Keisuke" sort="Koba, Keisuke" uniqKey="Koba K" first="Keisuke" last="Koba">Keisuke Koba</name></author><author><name sortKey="Makabe, Akiko" sort="Makabe, Akiko" uniqKey="Makabe A" first="Akiko" last="Makabe">Akiko Makabe</name></author><author><name sortKey="Li, Yi De" sort="Li, Yi De" uniqKey="Li Y" first="Yi-De" last="Li">Yi-De Li</name></author><author><name sortKey="Luo, Tu Shou" sort="Luo, Tu Shou" uniqKey="Luo T" first="Tu-Shou" last="Luo">Tu-Shou Luo</name></author><author><name sortKey="Yoh, Muneoki" sort="Yoh, Muneoki" uniqKey="Yoh M" first="Muneoki" last="Yoh">Muneoki Yoh</name></author></analytic><series><title level="j">Oecologia</title><idno type="eISSN">1432-1939</idno><imprint><date when="2014" type="published">2014</date></imprint></series></biblStruct></sourceDesc></fileDesc><profileDesc><textClass><keywords scheme="KwdEn" xml:lang="en"><term>Biomass (MeSH)</term><term>China (MeSH)</term><term>Ecosystem (MeSH)</term><term>Mycorrhizae (MeSH)</term><term>Nitrogen Cycle (MeSH)</term><term>Nitrogen Isotopes (analysis)</term><term>Plant Leaves (chemistry)</term><term>Plants (chemistry)</term><term>Plants (microbiology)</term><term>Soil (chemistry)</term><term>Trees (MeSH)</term></keywords><keywords scheme="KwdFr" xml:lang="fr"><term>Arbres (MeSH)</term><term>Biomasse (MeSH)</term><term>Chine (MeSH)</term><term>Cycle de l'azote (MeSH)</term><term>Feuilles de plante (composition chimique)</term><term>Isotopes de l'azote (analyse)</term><term>Mycorhizes (MeSH)</term><term>Plantes (composition chimique)</term><term>Plantes (microbiologie)</term><term>Sol (composition chimique)</term><term>Écosystème (MeSH)</term></keywords><keywords scheme="MESH" type="chemical" qualifier="analysis" xml:lang="en"><term>Nitrogen Isotopes</term></keywords><keywords scheme="MESH" qualifier="analyse" xml:lang="fr"><term>Isotopes de l'azote</term></keywords><keywords scheme="MESH" qualifier="chemistry" xml:lang="en"><term>Plant Leaves</term><term>Plants</term><term>Soil</term></keywords><keywords scheme="MESH" qualifier="composition chimique" xml:lang="fr"><term>Feuilles de plante</term><term>Plantes</term><term>Sol</term></keywords><keywords scheme="MESH" qualifier="microbiologie" xml:lang="fr"><term>Plantes</term></keywords><keywords scheme="MESH" qualifier="microbiology" xml:lang="en"><term>Plants</term></keywords><keywords scheme="MESH" xml:lang="en"><term>Biomass</term><term>China</term><term>Ecosystem</term><term>Mycorrhizae</term><term>Nitrogen Cycle</term><term>Trees</term></keywords><keywords scheme="MESH" xml:lang="fr"><term>Arbres</term><term>Biomasse</term><term>Chine</term><term>Cycle de l'azote</term><term>Mycorhizes</term><term>Écosystème</term></keywords></textClass></profileDesc></teiHeader><front><div type="abstract" xml:lang="en">The foliar stable N isotope ratio (δ(15)N) can provide integrated information on ecosystem N cycling. Here we present the δ(15)N of plant and soil in four remote typical tropical rainforests (one primary and three secondary) of southern China. We aimed to examine if (1) foliar δ(15)N in the study forests is negative, as observed in other tropical and subtropical sites in eastern Asia; (2) variation in δ(15)N among different species is smaller compared to that in many N-limited temperate and boreal ecosystems; and (3) the primary forest is more N rich than the younger secondary forests and therefore is more (15)N enriched. Our results show that foliar δ(15)N ranged from -5.1 to 1.3‰ for 39 collected plant species with different growth strategies and mycorrhizal types, and that for 35 species it was negative. Soil NO3 (-) had low δ(15)N (-11.4 to -3.2‰) and plant NO3 (-) uptake could not explain the negative foliar δ(15)N values (NH4 (+) was dominant in the soil inorganic-N fraction). We suggest that negative values might be caused by isotope fractionation during soil NH4 (+) uptake and mycorrhizal N transfer, and by direct uptake of atmospheric NH3/NH4 (+). The variation in foliar δ(15)N among species (by about 6‰) was smaller than in many N-limited ecosystems, which is typically about or over 10‰. The primary forest had a larger N capital in plants than the secondary forests. Foliar δ(15)N and the enrichment factor (foliar δ(15)N minus soil δ(15)N) were higher in the primary forest than in the secondary forests, albeit differences were small, while there was no consistent pattern in soil δ(15)N between primary and secondary forests.</div></front></TEI><pubmed><MedlineCitation Status="MEDLINE" IndexingMethod="Curated" Owner="NLM"><PMID Version="1">24085637</PMID><DateCompleted><Year>2014</Year><Month>10</Month><Day>09</Day></DateCompleted><DateRevised><Year>2019</Year><Month>03</Month><Day>18</Day></DateRevised><Article PubModel="Print-Electronic"><Journal><ISSN IssnType="Electronic">1432-1939</ISSN><JournalIssue CitedMedium="Internet"><Volume>174</Volume><Issue>2</Issue><PubDate><Year>2014</Year><Month>Feb</Month></PubDate></JournalIssue><Title>Oecologia</Title><ISOAbbreviation>Oecologia</ISOAbbreviation></Journal><ArticleTitle>Variations in nitrogen-15 natural abundance of plant and soil systems in four remote tropical rainforests, southern China.</ArticleTitle><Pagination><MedlinePgn>567-80</MedlinePgn></Pagination><ELocationID EIdType="doi" ValidYN="Y">10.1007/s00442-013-2778-5</ELocationID><Abstract><AbstractText>The foliar stable N isotope ratio (δ(15)N) can provide integrated information on ecosystem N cycling. Here we present the δ(15)N of plant and soil in four remote typical tropical rainforests (one primary and three secondary) of southern China. We aimed to examine if (1) foliar δ(15)N in the study forests is negative, as observed in other tropical and subtropical sites in eastern Asia; (2) variation in δ(15)N among different species is smaller compared to that in many N-limited temperate and boreal ecosystems; and (3) the primary forest is more N rich than the younger secondary forests and therefore is more (15)N enriched. Our results show that foliar δ(15)N ranged from -5.1 to 1.3‰ for 39 collected plant species with different growth strategies and mycorrhizal types, and that for 35 species it was negative. Soil NO3 (-) had low δ(15)N (-11.4 to -3.2‰) and plant NO3 (-) uptake could not explain the negative foliar δ(15)N values (NH4 (+) was dominant in the soil inorganic-N fraction). We suggest that negative values might be caused by isotope fractionation during soil NH4 (+) uptake and mycorrhizal N transfer, and by direct uptake of atmospheric NH3/NH4 (+). The variation in foliar δ(15)N among species (by about 6‰) was smaller than in many N-limited ecosystems, which is typically about or over 10‰. The primary forest had a larger N capital in plants than the secondary forests. Foliar δ(15)N and the enrichment factor (foliar δ(15)N minus soil δ(15)N) were higher in the primary forest than in the secondary forests, albeit differences were small, while there was no consistent pattern in soil δ(15)N between primary and secondary forests.</AbstractText></Abstract><AuthorList CompleteYN="Y"><Author ValidYN="Y"><LastName>Wang</LastName><ForeName>Ang</ForeName><Initials>A</Initials><AffiliationInfo><Affiliation>Research Institute of Tropical Forestry, Chinese Academy of Forestry, Guangzhou, 510520, China.</Affiliation></AffiliationInfo></Author><Author ValidYN="Y"><LastName>Fang</LastName><ForeName>Yun-Ting</ForeName><Initials>YT</Initials></Author><Author ValidYN="Y"><LastName>Chen</LastName><ForeName>De-Xiang</ForeName><Initials>DX</Initials></Author><Author ValidYN="Y"><LastName>Koba</LastName><ForeName>Keisuke</ForeName><Initials>K</Initials></Author><Author ValidYN="Y"><LastName>Makabe</LastName><ForeName>Akiko</ForeName><Initials>A</Initials></Author><Author 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first="Akiko" last="Makabe">Akiko Makabe</name><name sortKey="Yoh, Muneoki" sort="Yoh, Muneoki" uniqKey="Yoh M" first="Muneoki" last="Yoh">Muneoki Yoh</name></noCountry><country name="République populaire de Chine"><noRegion><name sortKey="Wang, Ang" sort="Wang, Ang" uniqKey="Wang A" first="Ang" last="Wang">Ang Wang</name></noRegion></country></tree></affiliations></record>Pour manipuler ce document sous Unix (Dilib)
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