Hydrological change in Southern Europe responding to increasing North Atlantic overturning during Gr...
Hydrological change in Southern Europe responding to increasing North Atlantic overturning during Greenland Stadial 1
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United States: National Academy of Sciences
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Language
English
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United States: National Academy of Sciences
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Significance This study presents robust evidence of two hydrological phases within the Greenland Stadial 1 (GS-1) cold event (12.8−11.7 ka B.P.) in Southern Europe. We present a well-dated high-resolution speleothem record (Seso Cave, Central Pyrenees) where temperature and hydrological signals are independently reconstructed. Detailed interpretati...
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Full title
Hydrological change in Southern Europe responding to increasing North Atlantic overturning during Greenland Stadial 1
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TN_cdi_crossref_primary_10_1073_pnas_1503990112
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https://devfeature-collection.sl.nsw.gov.au/record/TN_cdi_crossref_primary_10_1073_pnas_1503990112
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ISSN
0027-8424
E-ISSN
1091-6490
DOI
10.1073/pnas.1503990112