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dc.contributor.authorVedovato, LB
dc.contributor.authorCarvalho, LCS
dc.contributor.authorAragão, LEOC
dc.contributor.authorBird, M
dc.contributor.authorPhillips, OL
dc.contributor.authorAlvarez, P
dc.contributor.authorBarlow, J
dc.contributor.authorBartholomew, DC
dc.contributor.authorBerenguer, E
dc.contributor.authorCastro, W
dc.contributor.authorFerreira, J
dc.contributor.authorFrança, FM
dc.contributor.authorMalhi, Y
dc.contributor.authorMarimon, B
dc.contributor.authorJúnior, BHM
dc.contributor.authorMonteagudo, A
dc.contributor.authorOliveira, EA
dc.contributor.authorPereira, LO
dc.contributor.authorPontes-Lopes, A
dc.contributor.authorQuesada, CA
dc.contributor.authorSilva, CVJ
dc.contributor.authorEspejo, JES
dc.contributor.authorSilveira, M
dc.contributor.authorFeldpausch, TR
dc.date.accessioned2023-04-27T10:23:29Z
dc.date.issued2023-02-14
dc.date.updated2023-04-27T08:41:19Z
dc.description.abstractDrought and fire reduce productivity and increase tree mortality in tropical forests. Fires also produce pyrogenic carbon (PyC), which persists in situ for centuries to millennia, and represents a legacy of past fires, potentially improving soil fertility and water holding capacity and selecting for the survival and recruitment of certain tree life-history (or successional) strategies. We investigated whether PyC is correlated with physicochemical soil properties, wood density, aboveground carbon (AGC) dynamics and forest resistance to severe drought. To achieve our aim, we used an Amazon-wide, long-term plot network, in forests without known recent fires, integrating site-specific measures of forest dynamics, soil properties and a unique soil PyC concentration database. We found that forests with higher concentrations of soil PyC had both higher soil fertility and lower wood density. Soil PyC was not associated with AGC dynamics in non-drought years. However, during extreme drought events (10% driest years), forests with higher concentrations of soil PyC experienced lower reductions in AGC gains (woody growth and recruitment), with this drought-immunizing effect increasing with drought severity. Forests with a legacy of ancient fires are therefore more likely to continue to grow and recruit under increased drought severity. Forests with high soil PyC concentrations (third quartile) had 3.8% greater AGC gains under mean drought, but 33.7% greater under the most extreme drought than forests with low soil PyC concentrations (first quartile), offsetting losses of up to 0.68 Mg C ha–1yr–1 of AGC under extreme drought events. This suggests that ancient fires have legacy effects on current forest dynamics, by altering soil fertility and favoring tree species capable of continued growth and recruitment during droughts. Therefore, mature forest that experienced fires centuries or millennia ago may have greater resistance to current short-term droughts.en_GB
dc.description.sponsorshipCoordination of Improvement of Personnel in Higher Education, Brazil (CAPES)en_GB
dc.description.sponsorshipNatural Environment Research Council (NERC)en_GB
dc.description.sponsorshipFAPESPen_GB
dc.description.sponsorshipRoyal Societyen_GB
dc.description.sponsorshipNational Council for Science and Technology Development of Brazil (CNPq)en_GB
dc.format.extent1024101-
dc.identifier.citationVol. 6, article 1024101en_GB
dc.identifier.doihttps://doi.org/10.3389/ffgc.2023.1024101
dc.identifier.grantnumber88881.128127/2016-01en_GB
dc.identifier.grantnumberPVE 177/2012en_GB
dc.identifier.grantnumberNE/N011570/1en_GB
dc.identifier.grantnumberNE/N012542/1en_GB
dc.identifier.grantnumber2012/51872-5en_GB
dc.identifier.grantnumberNE/K016431/1en_GB
dc.identifier.grantnumber2012/51509-8en_GB
dc.identifier.grantnumberNE/S011811/1en_GB
dc.identifier.grantnumberICA/R1/180100en_GB
dc.identifier.grantnumberPELD/441244/2016-5en_GB
dc.identifier.grantnumberPELD/441572/2020-0en_GB
dc.identifier.grantnumber441659/2016-0en_GB
dc.identifier.grantnumber441573/2020-7en_GB
dc.identifier.grantnumberCNPq/PPBio/457602/2012-0en_GB
dc.identifier.grantnumber458022/2013-6en_GB
dc.identifier.grantnumber2016/21043-8en_GB
dc.identifier.grantnumber4067/2022-0en_GB
dc.identifier.grantnumber314416/2020-0en_GB
dc.identifier.urihttp://hdl.handle.net/10871/133030
dc.identifierORCID: 0000-0002-6631-7962 (Feldpausch, Ted R)
dc.identifierScopusID: 55323559100 (Feldpausch, Ted R)
dc.language.isoenen_GB
dc.publisherFrontiers Mediaen_GB
dc.rights© 2023 Vedovato, Carvalho, Aragão, Bird, Phillips, Alvarez, Barlow, Bartholomew, Berenguer, Castro, Ferreira, França, Malhi, Marimon, Marimon Júnior, Monteagudo, Oliveira, Pereira, Pontes-Lopes, Quesada, Silva, Silva Espejo, Silveira and Feldpausch. This is an open-access article distributed under the terms of the Creative Commons Attribution License (CC BY). The use, distribution or reproduction in other forums is permitted, provided the original author(s) and the copyright owner(s) are credited and that the original publication in this journal is cited, in accordance with accepted academic practice. No use, distribution or reproduction is permitted which does not comply with these terms.en_GB
dc.subjecthistorical firesen_GB
dc.subjectsoil fertilityen_GB
dc.subjectwood densityen_GB
dc.subjectcarbon sequestrationen_GB
dc.subjectsoil pyrogenic carbonen_GB
dc.subjectwater deficiten_GB
dc.subjectforest compositionen_GB
dc.titleAncient fires enhance Amazon forest drought resistanceen_GB
dc.typeArticleen_GB
dc.date.available2023-04-27T10:23:29Z
dc.identifier.issn2624-893X
exeter.article-numberARTN 1024101
dc.descriptionThis is the final version. Available on open access from Frontiers Media via the DOI in this recorden_GB
dc.descriptionData availability statement: The datasets presented in this article are not readily available but the raw data supporting the conclusions of this article will be available under reasonable request to the authors. Requests to access the datasets should be directed to TF, T.R.Feldpausch@exeter.ac.uk.en_GB
dc.identifier.eissn2624-893X
dc.identifier.journalFrontiers in Forests and Global Changeen_GB
dc.relation.ispartofFrontiers in Forests and Global Change, 6
dc.rights.urihttps://creativecommons.org/licenses/by/4.0/en_GB
dcterms.dateAccepted2023-01-06
rioxxterms.versionVoRen_GB
rioxxterms.licenseref.startdate2023-02-14
rioxxterms.typeJournal Article/Reviewen_GB
refterms.dateFCD2023-04-27T10:15:17Z
refterms.versionFCDVoR
refterms.dateFOA2023-04-27T10:23:36Z
refterms.panelCen_GB
refterms.dateFirstOnline2023-02-14


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© 2023 Vedovato, Carvalho, Aragão, Bird, Phillips, Alvarez, Barlow, Bartholomew, Berenguer, Castro, Ferreira, França, Malhi, Marimon, Marimon Júnior, Monteagudo, Oliveira, Pereira, Pontes-Lopes, Quesada, Silva, Silva Espejo, Silveira and Feldpausch. This is an open-access article distributed under the terms of the Creative Commons Attribution License (CC BY). The use, distribution or reproduction in other forums is permitted, provided the original author(s) and the copyright owner(s) are credited and that the original publication in this journal is cited, in accordance with accepted academic practice. No use, distribution or reproduction is permitted which does not comply with these terms.
Except where otherwise noted, this item's licence is described as © 2023 Vedovato, Carvalho, Aragão, Bird, Phillips, Alvarez, Barlow, Bartholomew, Berenguer, Castro, Ferreira, França, Malhi, Marimon, Marimon Júnior, Monteagudo, Oliveira, Pereira, Pontes-Lopes, Quesada, Silva, Silva Espejo, Silveira and Feldpausch. This is an open-access article distributed under the terms of the Creative Commons Attribution License (CC BY). The use, distribution or reproduction in other forums is permitted, provided the original author(s) and the copyright owner(s) are credited and that the original publication in this journal is cited, in accordance with accepted academic practice. No use, distribution or reproduction is permitted which does not comply with these terms.