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Climate Forcings and Their Influence on Alpine History as Reconstructed Through the Application of Synchrotron‐based X‐ray Microfluorescence on Layered Stalagmites

Bibliographic Data

ID8352820
AuthorsSilvia Frisia (0000-0001-6568-2696, Museo delle Scienze), Andrea Borsato (0000-0003-3858-4462, Museo delle Scienze), Jean Susini (0009-0002-1267-0549, European Synchrotron Radiation Facility), Andréa Somogyi (0000-0002-3814-4152, European Synchrotron Radiation Facility)
Year2005
Volume47
Issue2
Pages209-219
Publication date2005-05-01
Open AccessYes
TypeARTICLE
VenueArchaeometry (JOURNAL)
Journal identifiersISSN: 0003-813X • E-ISSN: 1475-4754
PublisherWiley (PUBLISHER • GB)
DOI10.1111/j.1475-4754.2005.00197.x
OpenAlexW2037007375
LanguageEN
References cited26

Solar variability and volcanic activity strongly interact with climate and the environment. Synchrotron radiation X‐ray microfluorescence (micro‐XRF) to an annually laminated Alpine stalagmite confirmed that annual laminae result from hydrological variability and changes in the duration of soil microbial degradation. The latter is modulated by solar variability. At the centennial timescale, growth rate and solar activity appear to be correlated with temperature change, with low temperatures at solar minima. By combining micro‐XRF and absorption spectroscopy techniques (XANES), we also found that speleothems are a new archive of aerosol sulphate related to volcanic activity. Peaks in S‐concentration from c. 5.2 to 5.0 ka bp in an Alpine stalagmite suggest that multiple volcanic sulphate aerosol emissions enhanced Mid‐Holocene summer cooling, thus favouring the preservation of the Alpine Iceman mummy in a persistent ice casket

Aerosol · Atmospheric sciences · Climatology · Geochemistry · Geography · Holocene · Ice core · Meteorology · Stalagmite · Synchrotron · Volcano · Archaeology and ancient environmental studies · Building materials and conservation · Geology · Geology and Paleoclimatology Research · Oceanography

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Highly citedNo

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