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Recent climate change has driven divergent hydrological shifts in high-latitude peatlands

dc.contributor.authorZhang, H
dc.contributor.authorVäliranta, M
dc.contributor.authorSwindles, GT
dc.contributor.authorAquino-López, MA
dc.contributor.authorMullan, D
dc.contributor.authorTan, N
dc.contributor.authorAmesbury, M
dc.contributor.authorBabeshko, KV
dc.contributor.authorBao, K
dc.contributor.authorBobrov, A
dc.contributor.authorChernyshov, V
dc.contributor.authorDavies, MA
dc.contributor.authorDiaconu, A-C
dc.contributor.authorFeurdean, A
dc.contributor.authorFinkelstein, SA
dc.contributor.authorGarneau, M
dc.contributor.authorGuo, Z
dc.contributor.authorJones, MC
dc.contributor.authorKay, M
dc.contributor.authorKlein, ES
dc.contributor.authorLamentowicz, M
dc.contributor.authorMagnan, G
dc.contributor.authorMarcisz, K
dc.contributor.authorMazei, N
dc.contributor.authorMazei, Y
dc.contributor.authorPayne, R
dc.contributor.authorPelletier, N
dc.contributor.authorPiilo, SR
dc.contributor.authorPratte, S
dc.contributor.authorRoland, T
dc.contributor.authorSaldaev, D
dc.contributor.authorShotyk, W
dc.contributor.authorSim, TG
dc.contributor.authorSloan, TJ
dc.contributor.authorSłowiński, M
dc.contributor.authorTalbot, J
dc.contributor.authorTaylor, L
dc.contributor.authorTsyganov, AN
dc.contributor.authorWetterich, S
dc.contributor.authorXing, W
dc.contributor.authorZhao, Y
dc.date.accessioned2022-11-07T11:15:18Z
dc.date.issued2022-08-24
dc.date.updated2022-11-07T09:00:42Z
dc.description.abstractHigh-latitude peatlands are changing rapidly in response to climate change, including permafrost thaw. Here, we reconstruct hydrological conditions since the seventeenth century using testate amoeba data from 103 high-latitude peat archives. We show that 54% of the peatlands have been drying and 32% have been wetting over this period, illustrating the complex ecohydrological dynamics of high latitude peatlands and their highly uncertain responses to a warming climate.en_GB
dc.format.extent4959-
dc.format.mediumElectronic
dc.identifier.citationVol. 13, article 4959en_GB
dc.identifier.doihttps://doi.org/10.1038/s41467-022-32711-4
dc.identifier.urihttp://hdl.handle.net/10871/131669
dc.identifierORCID: 0000-0002-4667-003X (Amesbury, Matthew)
dc.identifierScopusID: 22953098700 (Amesbury, Matthew)
dc.identifierORCID: 0000-0002-9237-1364 (Roland, Thomas)
dc.language.isoenen_GB
dc.publisherNature Researchen_GB
dc.relation.urlhttps://www.ncbi.nlm.nih.gov/pubmed/36002465en_GB
dc.relation.urlhttps://doi.org/10.12197/2022GA021en_GB
dc.rights© The Author(s) 2022. Open Access. This article is licensed under a Creative Commons Attribution 4.0 International License, which permits use, sharing, adaptation, distribution and reproduction in any medium or format, as long as you give appropriate credit to the original author(s) and the source, provide a link to the Creative Commons license, and indicate if changes were made. The images or other third party material in this article are included in the article’s Creative Commons license, unless indicated otherwise in a credit line to the material. If material is not included in the article’s Creative Commons license and your intended use is not permitted by statutory regulation or exceeds the permitted use, you will need to obtain permission directly from the copyright holder. To view a copy of this license, visit http://creativecommons.org/licenses/by/4.0/.en_GB
dc.titleRecent climate change has driven divergent hydrological shifts in high-latitude peatlandsen_GB
dc.typeArticleen_GB
dc.date.available2022-11-07T11:15:18Z
dc.identifier.issn2041-1723
exeter.article-number4959
exeter.place-of-publicationEngland
dc.descriptionThis is the final version. Available on open access from Nature Research via the DOI in this recorden_GB
dc.descriptionData availability: The peat record data that support the findings of this study can be accessed at the WDC for Geophysics, Beijing (https://doi.org/10.12197/2022GA021).en_GB
dc.identifier.eissn2041-1723
dc.identifier.journalNature Communicationsen_GB
dc.relation.ispartofNat Commun, 13(1)
dc.rights.urihttps://creativecommons.org/licenses/by/4.0/en_GB
dcterms.dateAccepted2022-08-10
dc.rights.licenseCC BY
rioxxterms.versionVoRen_GB
rioxxterms.licenseref.startdate2022-08-24
rioxxterms.typeJournal Article/Reviewen_GB
refterms.dateFCD2022-11-07T11:13:35Z
refterms.versionFCDVoR
refterms.dateFOA2022-11-07T11:15:28Z
refterms.panelCen_GB
refterms.dateFirstOnline2022-08-24


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© The Author(s) 2022. Open Access. This article is licensed under a Creative Commons Attribution 4.0 International License, which permits use, sharing, adaptation, distribution and reproduction in any medium or format, as long as you give appropriate credit to the original author(s) and the source, provide a link to the Creative Commons license, and indicate if changes were made. The images or other third party material in this article are included in the article’s Creative Commons license, unless indicated otherwise in a credit line to the material. If material is not included in the article’s Creative Commons license and your intended use is not permitted by statutory regulation or exceeds the permitted use, you will need to obtain permission directly from the copyright holder. To view a copy of this license, visit http://creativecommons.org/licenses/by/4.0/.
Except where otherwise noted, this item's licence is described as © The Author(s) 2022. Open Access. This article is licensed under a Creative Commons Attribution 4.0 International License, which permits use, sharing, adaptation, distribution and reproduction in any medium or format, as long as you give appropriate credit to the original author(s) and the source, provide a link to the Creative Commons license, and indicate if changes were made. The images or other third party material in this article are included in the article’s Creative Commons license, unless indicated otherwise in a credit line to the material. If material is not included in the article’s Creative Commons license and your intended use is not permitted by statutory regulation or exceeds the permitted use, you will need to obtain permission directly from the copyright holder. To view a copy of this license, visit http://creativecommons.org/licenses/by/4.0/.