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dc.contributor.authorSwindles, Graeme T.*
dc.contributor.authorPlunkett, G.*
dc.contributor.authorRoe, H.M.*
dc.date.accessioned2009-05-27T08:16:54Z
dc.date.available2009-05-27T08:16:54Z
dc.date.issued2007
dc.identifier.citationSwindles, G.T., Plunkett, G. and Roe, H.M. (2007). A Delayed Climatic Response to Solar Forcing at 2800 cal. BP: Multi-Proxy Evidence from Three Irish Peatlands. The Holocene. Vol.17, No. 2, pp. 177-182.en
dc.identifier.urihttp://hdl.handle.net/10454/2699
dc.descriptionNoen
dc.description.abstractMultiproxy palaeohydrological records from three raised bogs in Northern Ireland indicate that a major shift to wetter/cooler climatic conditions postdated the rapid decrease in solar activity at 2800 cal. BP by ~100 years. This event is bracketed by two wiggle-match radiocarbon-dated cryptotephra layers in each profile, enabling a high degree of chronological precision. These replicated data corroborate previous findings based on Irish peat humification profiles, and may indicate spatial complexity in the climatic response to solar activity between oceanic and continental areas.en
dc.language.isoenen
dc.relation.isreferencedbyhttp://hol.sagepub.com/cgi/reprint/17/2/177en
dc.subjectlate Holoceneen
dc.subjectIrelanden
dc.subjectSolar forcingen
dc.subject2800 cal. BP eventen
dc.subjectraised bogsen
dc.subjecttephraen
dc.subjectmultiproxy studyen
dc.subject14C production rateen
dc.subjectpalaeohydrologyen
dc.subjectpalaeoclimateen
dc.titleA Delayed Climatic Response to Solar Forcing at 2800 cal. BP: Multi-Proxy Evidence from Three Irish Peatlandsen
dc.status.refereedYesen
dc.typeArticleen
dc.type.versionNo full-text available in the repositoryen


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