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dc.contributor.authorBrehm, N.en
dc.contributor.authorChristl, M.en
dc.contributor.authorKnowles, T. D. J.en
dc.contributor.authorCasanova, E.en
dc.contributor.authorEvershed, R. P.en
dc.contributor.authorAdolphi, F.en
dc.contributor.authorMuscheler, R.en
dc.contributor.authorSynal, H. -A.en
dc.contributor.authorMekhaldi, F.en
dc.contributor.authorPaleari, C. I.en
dc.contributor.authorLeuschner, H. -H.en
dc.contributor.authorBayliss, A.en
dc.contributor.authorNicolussi, K.en
dc.contributor.authorPichler, T.en
dc.contributor.authorSchlüchter, C.en
dc.contributor.authorPearson, C. L.en
dc.contributor.authorSalzer, M. W.en
dc.contributor.authorFonti, P.en
dc.contributor.authorNievergelt, D.en
dc.contributor.authorHantemirov, R.en
dc.contributor.authorBrown, D. M.en
dc.contributor.authorUsoskin, I.en
dc.contributor.authorWacker, L.en
dc.date.accessioned2022-05-12T08:31:05Z-
dc.date.available2022-05-12T08:31:05Z-
dc.date.issued2022-
dc.identifier.citationTree-Rings Reveal Two Strong Solar Proton Events in 7176 and 5259 BCE / N. Brehm, M. Christl, T. D. J. Knowles et al. // Nature Communications. — 2022. — Vol. 13. — Iss. 1. — 1196.en
dc.identifier.issn2041-1723-
dc.identifier.otherAll Open Access, Gold, Green3
dc.identifier.urihttp://elar.urfu.ru/handle/10995/112237-
dc.description.abstractThe Sun sporadically produces eruptive events leading to intense fluxes of solar energetic particles (SEPs) that dramatically disrupt the near-Earth radiation environment. Such events have been directly studied for the last decades but little is known about the occurrence and magnitude of rare, extreme SEP events. Presently, a few events that produced measurable signals in cosmogenic radionuclides such as 14C, 10Be and 36Cl have been found. Analyzing annual 14C concentrations in tree-rings from Switzerland, Germany, Ireland, Russia, and the USA we discovered two spikes in atmospheric 14C occurring in 7176 and 5259 BCE. The ~2% increases of atmospheric 14C recorded for both events exceed all previously known 14C peaks but after correction for the geomagnetic field, they are comparable to the largest event of this type discovered so far at 775 CE. These strong events serve as accurate time markers for the synchronization with floating tree-ring and ice core records and provide critical information on the previous occurrence of extreme solar events which may threaten modern infrastructure. © 2022, The Author(s).en
dc.description.sponsorshipThe Laboratory of Ion Beam Physics is partially funded by its consortium partners PSI, EAWAG, and EMPA. N.B. is funded by the Swiss National Science Foundation (SNSF grant #SNF 197137). The establishment of the BRAMS Facility was jointly funded by the NERC, BBSRC and the University of Bristol and the measurements in this work were partly funded by an ERC Proof of Concept grant awarded to R.P.E. and financing E.C. postdoctoral contract (LipDat H2020 ERC-2018-PoC/812917). We thank Bisserka Gaydarska for sub-sampling the inter-laboratory replicates from M49, M234, Q2729 and Q2750, Cathy Tyers for reviewing the dating of the Irish and German samples, and Alexander Land for assistance in dating sample M49. P.F. received funding from the SNF Sinergia project CALDERA (no. 183571). R.H. is funded by Russian Science Foundation (grant № 21-14-00330). I.U. acknowledges the support from the Academy of Finland (grant 321882 ESPERA). C.L.P.’s and M.W.S.’s work on bristlecone pine was funded by the M.H. Wiener Foundation (ICCP Project). K.N. acknowledges the support provided by the Austrian Science Fund FWF (grant I-1183-N19).en
dc.format.mimetypeapplication/pdfen
dc.language.isoenen
dc.publisherNature Researchen1
dc.publisherSpringer Science and Business Media LLCen
dc.relationinfo:eu-repo/grantAgreement/RSF//21-14-00330en
dc.rightsinfo:eu-repo/semantics/openAccessen
dc.sourceNat. Commun.2
dc.sourceNature Communicationsen
dc.subjectCONCENTRATION (COMPOSITION)en
dc.subjectRADIOCARBON DATINGen
dc.subjectRADIONUCLIDEen
dc.subjectSOLAR RADIATIONen
dc.subjectTREE RINGen
dc.subjectGERMANYen
dc.subjectIRELANDen
dc.subjectRUSSIAN FEDERATIONen
dc.subjectSWITZERLANDen
dc.subjectUNITED STATESen
dc.titleTree-Rings Reveal Two Strong Solar Proton Events in 7176 and 5259 BCEen
dc.typeArticleen
dc.typeinfo:eu-repo/semantics/articleen
dc.typeinfo:eu-repo/semantics/publishedVersionen
dc.identifier.doi10.1038/s41467-022-28804-9-
dc.identifier.scopus85125976476-
local.contributor.employeeBrehm, N., Laboratory of Ion Beam Physics, ETHZ, Otto-Stern Weg 5 HPK, Zurich, 8093, Switzerland; Christl, M., Laboratory of Ion Beam Physics, ETHZ, Otto-Stern Weg 5 HPK, Zurich, 8093, Switzerland; Knowles, T.D.J., Bristol Radiocarbon Accelerator Mass Spectrometry Facility, Bristol University, Bristol, BS81TS, United Kingdom; Casanova, E., Bristol Radiocarbon Accelerator Mass Spectrometry Facility, Bristol University, Bristol, BS81TS, United Kingdom, UMR7209 Archéologie et Archéobotanique: Sociétés, Pratiques et Environnements, Muséum National d’Histoire Naturelle, CP56, 43 Rue Buffon, Paris, 75005, France; Evershed, R.P., Bristol Radiocarbon Accelerator Mass Spectrometry Facility, Bristol University, Bristol, BS81TS, United Kingdom; Adolphi, F., Alfred Wegener Institute, Helmholtz Centre for Polar and Marine Research, Bremerhaven, 27568, Germany; Muscheler, R., Department of Geology – Quaternary Sciences, Lund University, Lund, 22362, Sweden; Synal, H.-A., Laboratory of Ion Beam Physics, ETHZ, Otto-Stern Weg 5 HPK, Zurich, 8093, Switzerland; Mekhaldi, F., Department of Geology – Quaternary Sciences, Lund University, Lund, 22362, Sweden, British Antarctic Survey, Ice Dynamics and Paleoclimate, Cambridge, CB3 0ET, United Kingdom; Paleari, C.I., Department of Geology – Quaternary Sciences, Lund University, Lund, 22362, Sweden; Leuschner, H.-H., Albrecht von Haller Institute for Plant Sciences, Department of Palynology and Climate Dynamics, Georg-August-University, Wilhelm-Weber-Str. 2a, Göttingen, 37073, Germany; Bayliss, A., Historic England, Cannon Bridge House, 25 Dowgate Hill, London, EC4R 2YA, United Kingdom; Nicolussi, K., Department of Geography, Universität Innsbruck, Innrain 52, Innsbruck, 6020, Austria; Pichler, T., Department of Geography, Universität Innsbruck, Innrain 52, Innsbruck, 6020, Austria; Schlüchter, C., Institute of Geological Sciences, University of Bern, Baltzerstrasse 1+3, Bern, 3012, Switzerland; Pearson, C.L., University of Arizona, the Laboratory for Tree-Ring Research, 1215 E. Lowell Street, Tucson, AZ 85721-0045, United States; Salzer, M.W., University of Arizona, the Laboratory for Tree-Ring Research, 1215 E. Lowell Street, Tucson, AZ 85721-0045, United States; Fonti, P., Swiss Federal Research Institute WSL, Zürcherstrasse 111, Birmensdorf, 8903, Switzerland; Nievergelt, D., Swiss Federal Research Institute WSL, Zürcherstrasse 111, Birmensdorf, 8903, Switzerland; Hantemirov, R., Laboratory of Dendrochronology, Institute of Plant and Animal Ecology, Ural Branch of Russian Academy of Sciences, 8 Marta Street, 202, Ekaterinburg, 620144, Russian Federation, Laboratory of Natural Science Methods in Humanities, Ural Federal University, 19 Mira Street, Ekaterinburg, 620002, Russian Federation; Brown, D.M., School of Natural and Built Environment, The Queen’s University, Belfast, BT7 1NN, United Kingdom; Usoskin, I., Sodankylä Geophysical Observatory and Space Physics and Astronomy Research Unit, University of Oulu, Oulu, FIN-90014, Finland; Wacker, L., Laboratory of Ion Beam Physics, ETHZ, Otto-Stern Weg 5 HPK, Zurich, 8093, Switzerlanden
local.issue1-
local.volume13-
dc.identifier.wos000765815800009-
local.contributor.departmentLaboratory of Ion Beam Physics, ETHZ, Otto-Stern Weg 5 HPK, Zurich, 8093, Switzerland; Bristol Radiocarbon Accelerator Mass Spectrometry Facility, Bristol University, Bristol, BS81TS, United Kingdom; Alfred Wegener Institute, Helmholtz Centre for Polar and Marine Research, Bremerhaven, 27568, Germany; Department of Geology – Quaternary Sciences, Lund University, Lund, 22362, Sweden; British Antarctic Survey, Ice Dynamics and Paleoclimate, Cambridge, CB3 0ET, United Kingdom; Albrecht von Haller Institute for Plant Sciences, Department of Palynology and Climate Dynamics, Georg-August-University, Wilhelm-Weber-Str. 2a, Göttingen, 37073, Germany; Historic England, Cannon Bridge House, 25 Dowgate Hill, London, EC4R 2YA, United Kingdom; Department of Geography, Universität Innsbruck, Innrain 52, Innsbruck, 6020, Austria; Institute of Geological Sciences, University of Bern, Baltzerstrasse 1+3, Bern, 3012, Switzerland; University of Arizona, the Laboratory for Tree-Ring Research, 1215 E. Lowell Street, Tucson, AZ 85721-0045, United States; Swiss Federal Research Institute WSL, Zürcherstrasse 111, Birmensdorf, 8903, Switzerland; Laboratory of Dendrochronology, Institute of Plant and Animal Ecology, Ural Branch of Russian Academy of Sciences, 8 Marta Street, 202, Ekaterinburg, 620144, Russian Federation; Laboratory of Natural Science Methods in Humanities, Ural Federal University, 19 Mira Street, Ekaterinburg, 620002, Russian Federation; School of Natural and Built Environment, The Queen’s University, Belfast, BT7 1NN, United Kingdom; Sodankylä Geophysical Observatory and Space Physics and Astronomy Research Unit, University of Oulu, Oulu, FIN-90014, Finland; UMR7209 Archéologie et Archéobotanique: Sociétés, Pratiques et Environnements, Muséum National d’Histoire Naturelle, CP56, 43 Rue Buffon, Paris, 75005, Franceen
local.identifier.pure29822845-
local.description.order1196-
local.identifier.eid2-s2.0-85125976476-
local.fund.rsf21-14-00330-
local.identifier.wosWOS:000765815800009-
local.identifier.pmid35256613-
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