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    A Delayed Climatic Response to Solar Forcing at 2800 cal. BP: Multi-Proxy Evidence from Three Irish Peatlands

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    Publication date
    2007
    Author
    Swindles, Graeme T.
    Plunkett, G.
    Roe, H.M.
    Keyword
    late Holocene
    Ireland
    Solar forcing
    2800 cal. BP event
    raised bogs
    tephra
    multiproxy study
    14C production rate
    palaeohydrology
    palaeoclimate
    Peer-Reviewed
    Yes
    
    Metadata
    Show full item record
    Abstract
    Multiproxy 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.
    URI
    http://hdl.handle.net/10454/2699
    Version
    No full-text available in the repository
    Citation
    Swindles, 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.
    Link to publisher’s version
    http://hol.sagepub.com/cgi/reprint/17/2/177
    Type
    Article
    Collections
    Life Sciences Publications

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