Nature Geoscience
Nature Geoscience is a monthly journal dedicated to publishing high-quality original research papers across all areas of the geosciences. The journal’s content reflects all the disciplines within the geosciences, including studies of the Earth’s climate system, the solid Earth and the planets. Nature Geoscience covers studies based on all the methods used by geoscientists, ranging from field work and numerical modelling on regional and global scales to theoretical studies and remote sensing. Physical, chemical and biological investigations that contribute to our understanding of the Earth system or the planets are all represented.
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Nature Geoscience
© 2024 Macmillan Publishers Limited, part of Springer Nature. All rights reserved.
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Nature Geoscience
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https://www.nature.com/articles/s41561-024-01430-4
Nature Geoscience, Published online: 25 March 2024; doi:10.1038/s41561-024-01430-4Author Correction: Abrupt Holocene ice loss due to thinning and ungrounding in the Weddell Sea Embayment]]>
Mackenzie M. GriemanChristoph Nehrbass-AhlesHelene M. HoffmannThomas K. BauskaAmy C. F. KingRobert MulvaneyRachael H. RhodesIsobel F. RowellElizabeth R. ThomasEric W. Wolff
doi:10.1038/s41561-024-01430-4
Nature Geoscience, Published online: 2024-03-25; | doi:10.1038/s41561-024-01430-4
2024-03-25
Nature Geoscience
10.1038/s41561-024-01430-4
https://www.nature.com/articles/s41561-024-01430-4
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https://www.nature.com/articles/s41561-024-01395-4
Nature Geoscience, Published online: 25 March 2024; doi:10.1038/s41561-024-01395-4Volcanism after large, caldera-forming eruptions is thought to be muted. Exploration of the partially submerged caldera of Santorini reveals that large explosive eruptions have occurred since the caldera formed.]]>
Ben Kennedy
doi:10.1038/s41561-024-01395-4
Nature Geoscience, Published online: 2024-03-25; | doi:10.1038/s41561-024-01395-4
2024-03-25
Nature Geoscience
10.1038/s41561-024-01395-4
https://www.nature.com/articles/s41561-024-01395-4
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2 release with erosion]]>
https://www.nature.com/articles/s41561-024-01426-0
Nature Geoscience, Published online: 25 March 2024; doi:10.1038/s41561-024-01426-0Author Correction: Co-variation of silicate, carbonate and sulfide weathering drives CO2 release with erosion]]>
2 release with erosion]]>
Aaron BufeNiels HoviusRobert EmbersonJeremy K. C. RugensteinAlbert GalyHima J. Hassenruck-GudipatiJui-Ming Chang
doi:10.1038/s41561-024-01426-0
Nature Geoscience, Published online: 2024-03-25; | doi:10.1038/s41561-024-01426-0
2024-03-25
Nature Geoscience
10.1038/s41561-024-01426-0
https://www.nature.com/articles/s41561-024-01426-0
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https://www.nature.com/articles/s41561-024-01391-8
Nature Geoscience, Published online: 25 March 2024; doi:10.1038/s41561-024-01391-8Daytime surface ocean warming has large-scale patterns associated with the sea surface temperature front, leading to an afternoon slackening of the front and impacts on surface wind variability.]]>
Meghan F. CroninDongxiao ZhangSamantha M. WillsJ. E. Jack Reeves EyreLuAnne ThompsonNathan Anderson
doi:10.1038/s41561-024-01391-8
Nature Geoscience, Published online: 2024-03-25; | doi:10.1038/s41561-024-01391-8
2024-03-25
Nature Geoscience
10.1038/s41561-024-01391-8
https://www.nature.com/articles/s41561-024-01391-8
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https://www.nature.com/articles/s41561-024-01392-7
Nature Geoscience, Published online: 25 March 2024; doi:10.1038/s41561-024-01392-7Evidence for a past large explosive eruption within the Santorini caldera suggests that early stages of silicic caldera cycles can be more hazardous than previously assumed, according to analyses of intra-caldera deposits from the Kameni Volcano.]]>
Jonas PreineJens KarstensChristian HübscherTim DruittSteffen KutterolfParaskevi NomikouMichael MangaRalf GertisserKatharina PankSarah BeetheCarole BerthodGareth CrutchleyIona McIntoshThomas RongeMasako TominagaAcacia ClarkSusan DeBariRaymond JohnstonZenon MateoAlly PecciaChristopher JonesGünther KletetschkaAbigail MetcalfeAlexis BernardHehe ChenShun ChiyonobuTatiana Fernandez-PerezKumar Batuk JoshiOlga KoukousiouraMolly McCantaAntony MorrisParaskevi PolymenakouAdam WoodhouseYuzuru YamamotoKuo-Lung WangHao-Yang LeeXiaohui LiDimitrios Papanikolaou
doi:10.1038/s41561-024-01392-7
Nature Geoscience, Published online: 2024-03-25; | doi:10.1038/s41561-024-01392-7
2024-03-25
Nature Geoscience
10.1038/s41561-024-01392-7
https://www.nature.com/articles/s41561-024-01392-7
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https://www.nature.com/articles/s41561-024-01389-2
Nature Geoscience, Published online: 12 March 2024; doi:10.1038/s41561-024-01389-2Schreibersite is found in meteorites and thought to dwell in planetary cores. Tingting Gu explains how it may also have supported life on the early Earth.]]>
Tingting Gu
doi:10.1038/s41561-024-01389-2
Nature Geoscience, Published online: 2024-03-12; | doi:10.1038/s41561-024-01389-2
2024-03-12
Nature Geoscience
10.1038/s41561-024-01389-2
https://www.nature.com/articles/s41561-024-01389-2
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https://www.nature.com/articles/s41561-024-01411-7
Nature Geoscience, Published online: 12 March 2024; doi:10.1038/s41561-024-01411-7Understanding the ecosystem response to global environmental change requires consideration of geological processes, highlighting the interconnected nature of our Earth system.]]>
doi:10.1038/s41561-024-01411-7
Nature Geoscience, Published online: 2024-03-12; | doi:10.1038/s41561-024-01411-7
2024-03-12
Nature Geoscience
10.1038/s41561-024-01411-7
https://www.nature.com/articles/s41561-024-01411-7
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https://www.nature.com/articles/s41561-024-01379-4
Nature Geoscience, Published online: 12 March 2024; doi:10.1038/s41561-024-01379-4The carbon emissions of large igneous province magmatism are commonly associated with severe environmental crises. We developed a technique that used sedimentary mercury records to estimate these carbon fluxes through time and found that they are smaller and/or slower than assumed, which suggests that the influence of carbon-cycle feedback processes is underestimated in current models.]]>
doi:10.1038/s41561-024-01379-4
Nature Geoscience, Published online: 2024-03-12; | doi:10.1038/s41561-024-01379-4
2024-03-12
Nature Geoscience
10.1038/s41561-024-01379-4
https://www.nature.com/articles/s41561-024-01379-4