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dc.contributor.authorJamieson, SSR
dc.contributor.authorRoss, N
dc.contributor.authorPaxman, GJG
dc.contributor.authorClubb, FJ
dc.contributor.authorYoung, DA
dc.contributor.authorYan, S
dc.contributor.authorGreenbaum, J
dc.contributor.authorBlankenship, DD
dc.contributor.authorSiegert, MJ
dc.date.accessioned2023-11-23T10:03:30Z
dc.date.issued2023-10-24
dc.date.updated2023-11-17T16:32:05Z
dc.description.abstractThe East Antarctic Ice Sheet (EAIS) has its origins ca. 34 million years ago. Since then, the impact of climate change and past fluctuations in the EAIS margin has been reflected in periods of extensive vs. restricted ice cover and the modification of much of the Antarctic landscape. Resolving processes of landscape evolution is therefore critical for establishing ice sheet history, but it is rare to find unmodified landscapes that record past ice conditions. Here, we discover an extensive relic pre-glacial landscape preserved beneath the central EAIS despite millions of years of ice cover. The landscape was formed by rivers prior to ice sheet build-up but later modified by local glaciation before being dissected by outlet glaciers at the margin of a restricted ice sheet. Preservation of the relic surfaces indicates an absence of significant warm-based ice throughout their history, suggesting any transitions between restricted and expanded ice were rapid.en_GB
dc.description.sponsorshipNational Science Foundation (NSF)en_GB
dc.description.sponsorshipNASAen_GB
dc.description.sponsorshipG. Unger Vetlesen Foundationen_GB
dc.description.sponsorshipNatural Environment Research Council (NERC)en_GB
dc.format.extent6507-
dc.format.mediumElectronic
dc.identifier.citationVol. 14, article 6507en_GB
dc.identifier.doihttps://doi.org/10.1038/s41467-023-42152-2
dc.identifier.grantnumberANT-0733025en_GB
dc.identifier.grantnumberANT-1443690en_GB
dc.identifier.grantnumberNNX09AR52Gen_GB
dc.identifier.grantnumberNE/D003733/1en_GB
dc.identifier.grantnumberNE/L002590/1en_GB
dc.identifier.urihttp://hdl.handle.net/10871/134600
dc.identifierORCID: 0000-0002-0090-4806 (Siegert, Martin J)
dc.language.isoenen_GB
dc.publisherNature Researchen_GB
dc.relation.urlhttps://doi.org/10.5067/F5FGUT9F5089; HICARS2en_GB
dc.relation.urlhttps://doi.org/10.5067/9EBR2T0VXUDGen_GB
dc.relation.urlhttps://doi.org/10.5281/zenodo.8159223en_GB
dc.relation.urlhttps://www.ncbi.nlm.nih.gov/pubmed/37875503en_GB
dc.rights© The Author(s) 2023. Open access. 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 licence, and indicate if changes were made. The images or other third party material in this article are included in the article’s Creative Commons licence, unless indicated otherwise in a credit line to the material. If material is not included in the article’s Creative Commons licence 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 licence, visit http://creativecommons.org/licenses/by/4.0/en_GB
dc.titleAn ancient river landscape preserved beneath the East Antarctic Ice Sheeten_GB
dc.typeArticleen_GB
dc.date.available2023-11-23T10:03:30Z
dc.identifier.issn2041-1723
exeter.article-number6507
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 data used for this work is the radio-echo sounding data from the ICECAP project, which is openly accessible via the Blankenship 2017 references38,39 (HICARS1: https://doi.org/10.5067/F5FGUT9F5089; HICARS2: https://doi.org/10.5067/9EBR2T0VXUDG). The mapping data generated in this study (Fig. 3a) are openly available as GIS shapefiles at https://doi.org/10.5281/zenodo.815922373. Source data are provided with this paper—these relate to the data that underlies Figs. 3c and 4. Source data are provided with this paper.en_GB
dc.identifier.eissn2041-1723
dc.identifier.journalNature Communicationsen_GB
dc.relation.ispartofNat Commun, 14(1)
dc.rights.urihttps://creativecommons.org/licenses/by/4.0/en_GB
dcterms.dateAccepted2023-10-02
rioxxterms.versionVoRen_GB
rioxxterms.licenseref.startdate2023-10-24
rioxxterms.typeJournal Article/Reviewen_GB
refterms.dateFCD2023-11-20T09:12:09Z
refterms.versionFCDVoR
refterms.dateFOA2023-11-23T10:03:32Z
refterms.panelBen_GB
refterms.dateFirstOnline2023-10-24


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© The Author(s) 2023. Open access. 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 licence, and indicate if changes were made. The images or other third party material in this article are included in the article’s Creative Commons licence, unless indicated otherwise in a credit line to the material. If material is not included in the article’s Creative Commons licence 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 licence, visit http://creativecommons.org/licenses/by/4.0/
Except where otherwise noted, this item's licence is described as © The Author(s) 2023. Open access. 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 licence, and indicate if changes were made. The images or other third party material in this article are included in the article’s Creative Commons licence, unless indicated otherwise in a credit line to the material. If material is not included in the article’s Creative Commons licence 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 licence, visit http://creativecommons.org/licenses/by/4.0/