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dc.contributor.authorMills, MB
dc.contributor.authorMalhi, Y
dc.contributor.authorEwers, RM
dc.contributor.authorKho, LK
dc.contributor.authorTeh, YA
dc.contributor.authorBoth, S
dc.contributor.authorBurslem, DFRP
dc.contributor.authorMajalap, N
dc.contributor.authorNilus, R
dc.contributor.authorHuaraca Huasco, W
dc.contributor.authorCruz, R
dc.contributor.authorPillco, MM
dc.contributor.authorTurner, EC
dc.contributor.authorReynolds, G
dc.contributor.authorRiutta, T
dc.date.accessioned2023-01-18T15:13:05Z
dc.date.issued2023-01-09
dc.date.updated2023-01-18T13:37:54Z
dc.description.abstractLogged and structurally degraded tropical forests are fast becoming one of the most prevalent land-use types throughout the tropics and are routinely assumed to be a net carbon sink because they experience rapid rates of tree regrowth. Yet this assumption is based on forest biomass inventories that record carbon stock recovery but fail to account for the simultaneous losses of carbon from soil and necromass. Here, we used forest plots and an eddy covariance tower to quantify and partition net ecosystem CO2 exchange in Malaysian Borneo, a region that is a hot spot for deforestation and forest degradation. Our data represent the complete carbon budget for tropical forests measured throughout a logging event and subsequent recovery and found that they constitute a substantial and persistent net carbon source. Consistent with existing literature, our study showed a significantly greater woody biomass gain across moderately and heavily logged forests compared with unlogged forests, but this was counteracted by much larger carbon losses from soil organic matter and deadwood in logged forests. We estimate an average carbon source of 1.75 ± 0.94 Mg C ha-1 yr-1 within moderately logged plots and 5.23 ± 1.23 Mg C ha-1 yr-1 in unsustainably logged and severely degraded plots, with emissions continuing at these rates for at least one-decade post-logging. Our data directly contradict the default assumption that recovering logged and degraded tropical forests are net carbon sinks, implying the amount of carbon being sequestered across the world's tropical forests may be considerably lower than currently estimated.en_GB
dc.description.sponsorshipNatural Environment Research Council (NERC)en_GB
dc.description.sponsorshipEuropean Union Horizon 2020en_GB
dc.description.sponsorshipNational Science Foundationen_GB
dc.description.sponsorshipOsaka City University, Japanen_GB
dc.description.sponsorshipSime Darby Foundationen_GB
dc.description.sponsorshipJackson Foundationen_GB
dc.description.sponsorshipNOMIS Foundationen_GB
dc.description.sponsorshipEuropean Research Council (ERC)
dc.description.sponsorshipEhime University, Japan
dc.description.sponsorshipKyoto University, Japan
dc.identifier.citationVol. 120, No. 3, article e2214462120en_GB
dc.identifier.doihttps://doi.org/10.1073/pnas.2214462120
dc.identifier.grantnumberNE/K016377/1en_GB
dc.identifier.grantnumberNE/S007350/1en_GB
dc.identifier.grantnumberNE/P002218/1en_GB
dc.identifier.grantnumber865403en_GB
dc.identifier.grantnumberDEB-9107247en_GB
dc.identifier.grantnumberDEB- 9629601en_GB
dc.identifier.grantnumber06041094en_GB
dc.identifier.grantnumber08NP0901en_GB
dc.identifier.grantnumber09NP0901en_GB
dc.identifier.grantnumber321131en_GB
dc.identifier.urihttp://hdl.handle.net/10871/132265
dc.identifierORCID: 0000-0002-8308-5307 (Riutta, Terhi)
dc.language.isoenen_GB
dc.publisherNational Academy of Sciencesen_GB
dc.relation.urlhttps://www.ncbi.nlm.nih.gov/pubmed/36623189en_GB
dc.relation.urlhttps://doi.org/10.5281/zenodo.7307449en_GB
dc.relation.urlhttps://doi.org/10.5281/zenodo.7307447en_GB
dc.relation.urlhttps://doi.org/10.5281/zenodo.3888375en_GB
dc.rights© 2023 the Author(s). Published by PNAS. This open access article is distributed under Creative Commons Attribution License 4.0 (CC BY).en_GB
dc.subjectcarbon budgeten_GB
dc.subjectcarbon dynamicsen_GB
dc.subjectland useen_GB
dc.subjectloggingen_GB
dc.subjecttropical ecologyen_GB
dc.titleTropical forests post-logging are a persistent net carbon source to the atmosphereen_GB
dc.typeArticleen_GB
dc.date.available2023-01-18T15:13:05Z
dc.identifier.issn0027-8424
exeter.place-of-publicationUnited States
dc.descriptionThis is the final version. Available on open access from the National Academy of Sciences via the DOI in this record. en_GB
dc.descriptionData, Materials, and Software Availability. [field datasets; microclimate data] data have been deposited in [Zenodo] (https://doi.org/10.5281/zenodo.7307449, https://doi.org/10.5281/zenodo.7307447, and https://doi.org/10.5281/ zenodo.3888375). Previously published data were used for this work [L. K. Kho et al. (59), T. Riutta et al. (16), and T. Riutta, et al. (20)].en_GB
dc.identifier.eissn1091-6490
dc.identifier.journalProceedings of the National Academy of Sciencesen_GB
dc.rights.urihttps://creativecommons.org/licenses/by/4.0/en_GB
dcterms.dateAccepted2022-11-16
rioxxterms.versionVoRen_GB
rioxxterms.licenseref.startdate2023-01-09
rioxxterms.typeJournal Article/Reviewen_GB
refterms.dateFCD2023-01-18T15:04:26Z
refterms.versionFCDVoR
refterms.dateFOA2023-01-18T15:13:06Z
refterms.panelCen_GB
refterms.dateFirstOnline2023-01-09


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© 2023 the Author(s). Published by PNAS.
This open access article is distributed under Creative
Commons Attribution License 4.0 (CC BY).
Except where otherwise noted, this item's licence is described as © 2023 the Author(s). Published by PNAS. This open access article is distributed under Creative Commons Attribution License 4.0 (CC BY).