Evolution of trees and mycorrhizal fungi intensifies silicate mineral weathering.
Identifieur interne : 001F02 ( Main/Curation ); précédent : 001F01; suivant : 001F03Evolution of trees and mycorrhizal fungi intensifies silicate mineral weathering.
Auteurs : Joe Quirk [Royaume-Uni] ; David J. Beerling ; Steve A. Banwart ; Gabriella Kakonyi ; Maria E. Romero-Gonzalez ; Jonathan R. LeakeSource :
- Biology letters [ 1744-957X ] ; 2012.
Descripteurs français
- KwdFr :
- MESH :
- analyse : Sol.
- génétique : Arbres, Mycorhizes.
- microbiologie : Arbres.
- métabolisme : Calcium.
- Angleterre, Microbiologie du sol, Silicates, Spécificité d'espèce, Symbiose, Évolution biologique.
English descriptors
- KwdEn :
- MESH :
- chemical , analysis : Soil.
- chemical , metabolism : Calcium.
- genetics : Mycorrhizae, Trees.
- microbiology : Trees.
- Biological Evolution, England, Silicates, Soil Microbiology, Species Specificity, Symbiosis.
Abstract
Forested ecosystems diversified more than 350 Ma to become major engines of continental silicate weathering, regulating the Earth's atmospheric carbon dioxide concentration by driving calcium export into ocean carbonates. Our field experiments with mature trees demonstrate intensification of this weathering engine as tree lineages diversified in concert with their symbiotic mycorrhizal fungi. Preferential hyphal colonization of the calcium silicate-bearing rock, basalt, progressively increased with advancement from arbuscular mycorrhizal (AM) to later, independently evolved ectomycorrhizal (EM) fungi, and from gymnosperm to angiosperm hosts with both fungal groups. This led to 'trenching' of silicate mineral surfaces by AM and EM fungi, with EM gymnosperms and angiosperms releasing calcium from basalt at twice the rate of AM gymnosperms. Our findings indicate mycorrhiza-driven weathering may have originated hundreds of millions of years earlier than previously recognized and subsequently intensified with the evolution of trees and mycorrhizas to affect the Earth's long-term CO(2) and climate history.
DOI: 10.1098/rsbl.2012.0503
PubMed: 22859556
PubMed Central: PMC3497110
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Banwart</name></author><author><name sortKey="Kakonyi, Gabriella" sort="Kakonyi, Gabriella" uniqKey="Kakonyi G" first="Gabriella" last="Kakonyi">Gabriella Kakonyi</name></author><author><name sortKey="Romero Gonzalez, Maria E" sort="Romero Gonzalez, Maria E" uniqKey="Romero Gonzalez M" first="Maria E" last="Romero-Gonzalez">Maria E. Romero-Gonzalez</name></author><author><name sortKey="Leake, Jonathan R" sort="Leake, Jonathan R" uniqKey="Leake J" first="Jonathan R" last="Leake">Jonathan R. 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Leake</name></author></analytic><series><title level="j">Biology letters</title><idno type="eISSN">1744-957X</idno><imprint><date when="2012" type="published">2012</date></imprint></series></biblStruct></sourceDesc></fileDesc><profileDesc><textClass><keywords scheme="KwdEn" xml:lang="en"><term>Biological Evolution (MeSH)</term><term>Calcium (metabolism)</term><term>England (MeSH)</term><term>Mycorrhizae (genetics)</term><term>Silicates (MeSH)</term><term>Soil (analysis)</term><term>Soil Microbiology (MeSH)</term><term>Species Specificity (MeSH)</term><term>Symbiosis (MeSH)</term><term>Trees (genetics)</term><term>Trees (microbiology)</term></keywords><keywords scheme="KwdFr" xml:lang="fr"><term>Angleterre (MeSH)</term><term>Arbres (génétique)</term><term>Arbres (microbiologie)</term><term>Calcium (métabolisme)</term><term>Microbiologie du sol (MeSH)</term><term>Mycorhizes (génétique)</term><term>Silicates (MeSH)</term><term>Sol (analyse)</term><term>Spécificité d'espèce (MeSH)</term><term>Symbiose (MeSH)</term><term>Évolution biologique (MeSH)</term></keywords><keywords scheme="MESH" type="chemical" qualifier="analysis" xml:lang="en"><term>Soil</term></keywords><keywords scheme="MESH" type="chemical" qualifier="metabolism" xml:lang="en"><term>Calcium</term></keywords><keywords scheme="MESH" qualifier="analyse" xml:lang="fr"><term>Sol</term></keywords><keywords scheme="MESH" qualifier="genetics" xml:lang="en"><term>Mycorrhizae</term><term>Trees</term></keywords><keywords scheme="MESH" qualifier="génétique" xml:lang="fr"><term>Arbres</term><term>Mycorhizes</term></keywords><keywords scheme="MESH" qualifier="microbiologie" xml:lang="fr"><term>Arbres</term></keywords><keywords scheme="MESH" qualifier="microbiology" xml:lang="en"><term>Trees</term></keywords><keywords scheme="MESH" qualifier="métabolisme" xml:lang="fr"><term>Calcium</term></keywords><keywords scheme="MESH" xml:lang="en"><term>Biological Evolution</term><term>England</term><term>Silicates</term><term>Soil Microbiology</term><term>Species Specificity</term><term>Symbiosis</term></keywords><keywords scheme="MESH" xml:lang="fr"><term>Angleterre</term><term>Microbiologie du sol</term><term>Silicates</term><term>Spécificité d'espèce</term><term>Symbiose</term><term>Évolution biologique</term></keywords></textClass></profileDesc></teiHeader><front><div type="abstract" xml:lang="en">Forested ecosystems diversified more than 350 Ma to become major engines of continental silicate weathering, regulating the Earth's atmospheric carbon dioxide concentration by driving calcium export into ocean carbonates. Our field experiments with mature trees demonstrate intensification of this weathering engine as tree lineages diversified in concert with their symbiotic mycorrhizal fungi. Preferential hyphal colonization of the calcium silicate-bearing rock, basalt, progressively increased with advancement from arbuscular mycorrhizal (AM) to later, independently evolved ectomycorrhizal (EM) fungi, and from gymnosperm to angiosperm hosts with both fungal groups. This led to 'trenching' of silicate mineral surfaces by AM and EM fungi, with EM gymnosperms and angiosperms releasing calcium from basalt at twice the rate of AM gymnosperms. Our findings indicate mycorrhiza-driven weathering may have originated hundreds of millions of years earlier than previously recognized and subsequently intensified with the evolution of trees and mycorrhizas to affect the Earth's long-term CO(2) and climate history.</div></front></TEI><pubmed><MedlineCitation Status="MEDLINE" Owner="NLM"><PMID Version="1">22859556</PMID><DateCompleted><Year>2013</Year><Month>03</Month><Day>05</Day></DateCompleted><DateRevised><Year>2018</Year><Month>11</Month><Day>13</Day></DateRevised><Article PubModel="Print-Electronic"><Journal><ISSN IssnType="Electronic">1744-957X</ISSN><JournalIssue CitedMedium="Internet"><Volume>8</Volume><Issue>6</Issue><PubDate><Year>2012</Year><Month>Dec</Month><Day>23</Day></PubDate></JournalIssue><Title>Biology letters</Title><ISOAbbreviation>Biol Lett</ISOAbbreviation></Journal><ArticleTitle>Evolution of trees and mycorrhizal fungi intensifies silicate mineral weathering.</ArticleTitle><Pagination><MedlinePgn>1006-11</MedlinePgn></Pagination><ELocationID EIdType="doi" ValidYN="Y">10.1098/rsbl.2012.0503</ELocationID><Abstract><AbstractText>Forested ecosystems diversified more than 350 Ma to become major engines of continental silicate weathering, regulating the Earth's atmospheric carbon dioxide concentration by driving calcium export into ocean carbonates. Our field experiments with mature trees demonstrate intensification of this weathering engine as tree lineages diversified in concert with their symbiotic mycorrhizal fungi. Preferential hyphal colonization of the calcium silicate-bearing rock, basalt, progressively increased with advancement from arbuscular mycorrhizal (AM) to later, independently evolved ectomycorrhizal (EM) fungi, and from gymnosperm to angiosperm hosts with both fungal groups. This led to 'trenching' of silicate mineral surfaces by AM and EM fungi, with EM gymnosperms and angiosperms releasing calcium from basalt at twice the rate of AM gymnosperms. 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