An absolute paleotemperature record from 10 to 6 Ka inferred from fluid inclusion D/H ratios of a stalagmite from Vancouver Island, British Columbia, Canada

Details An absolute paleotemperature record from 10 to 6 Ka inferred from fluid inclusion D/H ratios of a stalagmite from Vancouver Island, British Columbia, Canada An absolute paleotemperature record from 10 to 6 Ka inferred from fluid inclusion D/H ratios of a stalagmite from Vancouver Island, British Columbia, Canada

Feb 2008

adsabs.harvard.edu/cgi-bin/nph-data_query?bibcode=2008gecoa..72.1014z&link_type=ejournal

Geochimica et Cosmochimica Acta, v. 72, iss. 4, p. 1014-1026.

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