Decadal post-fire succession of soil invertebrate communities is dependent on the soil surface properties in a northern temperate forest.
Identifieur interne : 000A44 ( Main/Exploration ); précédent : 000A43; suivant : 000A45Decadal post-fire succession of soil invertebrate communities is dependent on the soil surface properties in a northern temperate forest.
Auteurs : Apolline Auclerc [États-Unis] ; James M. Le Moine [États-Unis] ; Pierre-Joseph Hatton [États-Unis] ; Jeffrey A. Bird [États-Unis] ; Knute J. Nadelhoffer [États-Unis]Source :
- The Science of the total environment [ 1879-1026 ] ; 2019.
Abstract
Although fires are common disturbances in North American forests, the extent to which soil invertebrate assemblages recover from burning remains unclear. Here, we examine long-term (14- to 101-yr) recoveries of soil invertebrate communities from common cut and burn treatments conducted at 6 to 26-yr intervals since 1911 in a deciduous forest in the upper Great Lakes region (USA). We characterize soil surface macro-invertebrate communities during both fall and spring across a long-term, experimental fire chronosequence to characterize invertebrate community recovery at decadal time-scales and community changes between seasons. We posited that changes in invertebrate community structure might, in turn, impact decomposition process. We sampled active organisms at the soil surface using pitfall traps. We described understory vegetation, measured soil properties, and conducted a 4-year litter bag study with big-toothed aspen leaves (Populus grandidentata). Invertebrate community responses followed a habitat accommodation model of succession showing that invertebrate succession is dependent on the soil surface properties. The fall and spring measures revealed that the densities of active invertebrates were highest 101 years after fire. For a given pair of stands, a pattern of sharing higher percentage of taxa was denoted when stands were of similar age. Some species such as the beetle Stelidota octomaculata appeared to be indicator of the chronosequence succession stage because it tracks the successional increase of Quercus and acorn production at the study site. We also found a significant positive correlation between leaf decomposition of soil macrofaunal accessible leaves and millipedes density across the chronosequence. We show that vegetation cover changes and related shifts in habitat structure occurring during post-fire succession are important in shaping communities assemblages. This finding highlights the importance of simultaneously considering abiotic-biotic factors together with above- and belowground measurements to better characterize controls on successional community dynamics after disturbance.
DOI: 10.1016/j.scitotenv.2018.08.041
PubMed: 30180314
Affiliations:
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Electronic address: apolline.auclerc@univ-lorraine.fr.</nlm:affiliation><country xml:lang="fr">États-Unis</country><wicri:regionArea>Laboratoire Sols et Environnement, Université de Lorraine, Inra, LSE, F-54000 Nancy, France; University of Michigan, Department of Ecology and Evolutionary Biology, Ann Arbor, MI</wicri:regionArea><placeName><region type="state">Michigan</region><settlement type="city">Nancy</settlement></placeName><orgName type="university">Université de Lorraine</orgName></affiliation></author><author><name sortKey="Le Moine, James M" sort="Le Moine, James M" uniqKey="Le Moine J" first="James M" last="Le Moine">James M. Le Moine</name><affiliation wicri:level="2"><nlm:affiliation>University of Michigan, Department of Ecology and Evolutionary Biology, Ann Arbor, MI, USA; Northern Arizona University, Center for Ecosystem Science & Society, Flagstaff, AZ, USA.</nlm:affiliation><country xml:lang="fr">États-Unis</country><wicri:regionArea>University of Michigan, Department of Ecology and Evolutionary Biology, Ann Arbor, MI, USA; Northern Arizona University, Center for Ecosystem Science & Society, Flagstaff, AZ</wicri:regionArea><placeName><region type="state">Arizona</region></placeName></affiliation></author><author><name sortKey="Hatton, Pierre Joseph" sort="Hatton, Pierre Joseph" uniqKey="Hatton P" first="Pierre-Joseph" last="Hatton">Pierre-Joseph Hatton</name><affiliation wicri:level="2"><nlm:affiliation>University of Michigan, Department of Ecology and Evolutionary Biology, Ann Arbor, MI, USA; School of Earth & Environmental Sciences, Queens College, CUNY, New York, NY, USA.</nlm:affiliation><country xml:lang="fr">États-Unis</country><wicri:regionArea>University of Michigan, Department of Ecology and Evolutionary Biology, Ann Arbor, MI, USA; School of Earth & Environmental Sciences, Queens College, CUNY, New York, NY</wicri:regionArea><placeName><region type="state">État de New York</region></placeName></affiliation></author><author><name sortKey="Bird, Jeffrey A" sort="Bird, Jeffrey A" uniqKey="Bird J" first="Jeffrey A" last="Bird">Jeffrey A. 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Nadelhoffer</name><affiliation wicri:level="2"><nlm:affiliation>University of Michigan, Department of Ecology and Evolutionary Biology, Ann Arbor, MI, USA.</nlm:affiliation><country xml:lang="fr">États-Unis</country><wicri:regionArea>University of Michigan, Department of Ecology and Evolutionary Biology, Ann Arbor, MI</wicri:regionArea><placeName><region type="state">Michigan</region></placeName></affiliation></author></analytic><series><title level="j">The Science of the total environment</title><idno type="eISSN">1879-1026</idno><imprint><date when="2019" type="published">2019</date></imprint></series></biblStruct></sourceDesc></fileDesc><profileDesc><textClass></textClass></profileDesc></teiHeader><front><div type="abstract" xml:lang="en">Although fires are common disturbances in North American forests, the extent to which soil invertebrate assemblages recover from burning remains unclear. Here, we examine long-term (14- to 101-yr) recoveries of soil invertebrate communities from common cut and burn treatments conducted at 6 to 26-yr intervals since 1911 in a deciduous forest in the upper Great Lakes region (USA). We characterize soil surface macro-invertebrate communities during both fall and spring across a long-term, experimental fire chronosequence to characterize invertebrate community recovery at decadal time-scales and community changes between seasons. We posited that changes in invertebrate community structure might, in turn, impact decomposition process. We sampled active organisms at the soil surface using pitfall traps. We described understory vegetation, measured soil properties, and conducted a 4-year litter bag study with big-toothed aspen leaves (Populus grandidentata). Invertebrate community responses followed a habitat accommodation model of succession showing that invertebrate succession is dependent on the soil surface properties. The fall and spring measures revealed that the densities of active invertebrates were highest 101 years after fire. For a given pair of stands, a pattern of sharing higher percentage of taxa was denoted when stands were of similar age. Some species such as the beetle Stelidota octomaculata appeared to be indicator of the chronosequence succession stage because it tracks the successional increase of Quercus and acorn production at the study site. We also found a significant positive correlation between leaf decomposition of soil macrofaunal accessible leaves and millipedes density across the chronosequence. We show that vegetation cover changes and related shifts in habitat structure occurring during post-fire succession are important in shaping communities assemblages. This finding highlights the importance of simultaneously considering abiotic-biotic factors together with above- and belowground measurements to better characterize controls on successional community dynamics after disturbance.</div></front></TEI><pubmed><MedlineCitation Status="PubMed-not-MEDLINE" Owner="NLM"><PMID Version="1">30180314</PMID><DateCompleted><Year>2018</Year><Month>10</Month><Day>03</Day></DateCompleted><DateRevised><Year>2018</Year><Month>10</Month><Day>04</Day></DateRevised><Article PubModel="Print-Electronic"><Journal><ISSN IssnType="Electronic">1879-1026</ISSN><JournalIssue CitedMedium="Internet"><Volume>647</Volume><PubDate><Year>2019</Year><Month>Jan</Month><Day>10</Day></PubDate></JournalIssue><Title>The Science of the total environment</Title><ISOAbbreviation>Sci Total Environ</ISOAbbreviation></Journal><ArticleTitle>Decadal post-fire succession of soil invertebrate communities is dependent on the soil surface properties in a northern temperate forest.</ArticleTitle><Pagination><MedlinePgn>1058-1068</MedlinePgn></Pagination><ELocationID EIdType="pii" ValidYN="Y">S0048-9697(18)33010-9</ELocationID><ELocationID EIdType="doi" ValidYN="Y">10.1016/j.scitotenv.2018.08.041</ELocationID><Abstract><AbstractText>Although fires are common disturbances in North American forests, the extent to which soil invertebrate assemblages recover from burning remains unclear. Here, we examine long-term (14- to 101-yr) recoveries of soil invertebrate communities from common cut and burn treatments conducted at 6 to 26-yr intervals since 1911 in a deciduous forest in the upper Great Lakes region (USA). We characterize soil surface macro-invertebrate communities during both fall and spring across a long-term, experimental fire chronosequence to characterize invertebrate community recovery at decadal time-scales and community changes between seasons. We posited that changes in invertebrate community structure might, in turn, impact decomposition process. We sampled active organisms at the soil surface using pitfall traps. We described understory vegetation, measured soil properties, and conducted a 4-year litter bag study with big-toothed aspen leaves (Populus grandidentata). Invertebrate community responses followed a habitat accommodation model of succession showing that invertebrate succession is dependent on the soil surface properties. The fall and spring measures revealed that the densities of active invertebrates were highest 101 years after fire. For a given pair of stands, a pattern of sharing higher percentage of taxa was denoted when stands were of similar age. Some species such as the beetle Stelidota octomaculata appeared to be indicator of the chronosequence succession stage because it tracks the successional increase of Quercus and acorn production at the study site. We also found a significant positive correlation between leaf decomposition of soil macrofaunal accessible leaves and millipedes density across the chronosequence. We show that vegetation cover changes and related shifts in habitat structure occurring during post-fire succession are important in shaping communities assemblages. This finding highlights the importance of simultaneously considering abiotic-biotic factors together with above- and belowground measurements to better characterize controls on successional community dynamics after disturbance.</AbstractText><CopyrightInformation>Copyright © 2018 Elsevier B.V. All rights reserved.</CopyrightInformation></Abstract><AuthorList CompleteYN="Y"><Author ValidYN="Y"><LastName>Auclerc</LastName><ForeName>Apolline</ForeName><Initials>A</Initials><AffiliationInfo><Affiliation>Laboratoire Sols et Environnement, Université de Lorraine, Inra, LSE, F-54000 Nancy, France; University of Michigan, Department of Ecology and Evolutionary Biology, Ann Arbor, MI, USA. Electronic address: apolline.auclerc@univ-lorraine.fr.</Affiliation></AffiliationInfo></Author><Author ValidYN="Y"><LastName>Le Moine</LastName><ForeName>James M</ForeName><Initials>JM</Initials><AffiliationInfo><Affiliation>University of Michigan, Department of Ecology and Evolutionary Biology, Ann Arbor, MI, USA; Northern Arizona University, Center for Ecosystem Science & Society, Flagstaff, AZ, USA.</Affiliation></AffiliationInfo></Author><Author ValidYN="Y"><LastName>Hatton</LastName><ForeName>Pierre-Joseph</ForeName><Initials>PJ</Initials><AffiliationInfo><Affiliation>University of Michigan, Department of Ecology and Evolutionary Biology, Ann Arbor, MI, USA; School of Earth & Environmental Sciences, Queens College, CUNY, New York, NY, USA.</Affiliation></AffiliationInfo></Author><Author ValidYN="Y"><LastName>Bird</LastName><ForeName>Jeffrey A</ForeName><Initials>JA</Initials><AffiliationInfo><Affiliation>School of Earth & Environmental Sciences, Queens College, CUNY, New York, NY, USA.</Affiliation></AffiliationInfo></Author><Author ValidYN="Y"><LastName>Nadelhoffer</LastName><ForeName>Knute J</ForeName><Initials>KJ</Initials><AffiliationInfo><Affiliation>University of Michigan, Department of Ecology and Evolutionary Biology, Ann Arbor, MI, USA.</Affiliation></AffiliationInfo></Author></AuthorList><Language>eng</Language><PublicationTypeList><PublicationType UI="D016428">Journal Article</PublicationType></PublicationTypeList><ArticleDate DateType="Electronic"><Year>2018</Year><Month>08</Month><Day>07</Day></ArticleDate></Article><MedlineJournalInfo><Country>Netherlands</Country><MedlineTA>Sci Total Environ</MedlineTA><NlmUniqueID>0330500</NlmUniqueID><ISSNLinking>0048-9697</ISSNLinking></MedlineJournalInfo><KeywordList Owner="NOTNLM"><Keyword MajorTopicYN="N">Burn plots</Keyword><Keyword MajorTopicYN="N">Disturbance</Keyword><Keyword MajorTopicYN="N">Fire chronosequence</Keyword><Keyword MajorTopicYN="N">Multi-taxa</Keyword><Keyword MajorTopicYN="N">Recovery</Keyword><Keyword MajorTopicYN="N">Soil cover</Keyword></KeywordList></MedlineCitation><PubmedData><History><PubMedPubDate PubStatus="received"><Year>2018</Year><Month>05</Month><Day>30</Day></PubMedPubDate><PubMedPubDate PubStatus="revised"><Year>2018</Year><Month>08</Month><Day>03</Day></PubMedPubDate><PubMedPubDate PubStatus="accepted"><Year>2018</Year><Month>08</Month><Day>03</Day></PubMedPubDate><PubMedPubDate PubStatus="pubmed"><Year>2018</Year><Month>9</Month><Day>6</Day><Hour>6</Hour><Minute>0</Minute></PubMedPubDate><PubMedPubDate PubStatus="medline"><Year>2018</Year><Month>9</Month><Day>6</Day><Hour>6</Hour><Minute>1</Minute></PubMedPubDate><PubMedPubDate PubStatus="entrez"><Year>2018</Year><Month>9</Month><Day>6</Day><Hour>6</Hour><Minute>0</Minute></PubMedPubDate></History><PublicationStatus>ppublish</PublicationStatus><ArticleIdList><ArticleId IdType="pubmed">30180314</ArticleId><ArticleId IdType="pii">S0048-9697(18)33010-9</ArticleId><ArticleId IdType="doi">10.1016/j.scitotenv.2018.08.041</ArticleId></ArticleIdList></PubmedData></pubmed><affiliations><list><country><li>États-Unis</li></country><region><li>Arizona</li><li>Michigan</li><li>État de New York</li></region><settlement><li>Nancy</li></settlement><orgName><li>Université de Lorraine</li></orgName></list><tree><country name="États-Unis"><region name="Michigan"><name sortKey="Auclerc, Apolline" sort="Auclerc, Apolline" uniqKey="Auclerc A" first="Apolline" last="Auclerc">Apolline Auclerc</name></region><name sortKey="Bird, Jeffrey A" sort="Bird, Jeffrey A" uniqKey="Bird J" first="Jeffrey A" last="Bird">Jeffrey A. Bird</name><name sortKey="Hatton, Pierre Joseph" sort="Hatton, Pierre Joseph" uniqKey="Hatton P" first="Pierre-Joseph" last="Hatton">Pierre-Joseph Hatton</name><name sortKey="Le Moine, James M" sort="Le Moine, James M" uniqKey="Le Moine J" first="James M" last="Le Moine">James M. Le Moine</name><name sortKey="Nadelhoffer, Knute J" sort="Nadelhoffer, Knute J" uniqKey="Nadelhoffer K" first="Knute J" last="Nadelhoffer">Knute J. Nadelhoffer</name></country></tree></affiliations></record>Pour manipuler ce document sous Unix (Dilib)
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