Tropical Response to the 8200 Yr B.P. Cold Event? Speleothem Isotopes Indicate a Weakened Early Holocene Monsoon in Costa Rica

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dc.contributor.authorLachniet, Matthew S.
dc.contributor.authorAsmerom, Yemane
dc.contributor.authorBurns, Stephen J.
dc.contributor.authorPolyak, Victor J.
dc.contributor.authorSeltzer, Geoffrey O.
dc.date.accessioned2008-04-28T14:45:17Z
dc.date.available2008-04-28T14:45:17Z
dc.date.issued2004
dc.format.extent182053 bytes
dc.format.extent957-960
dc.format.mimetypeapplication/pdf
dc.identifier0091-7613
dc.identifier.citationLachniet, Matthew S., Asmerom, Yemane, Burns, Stephen J., Polyak, Victor J., and Seltzer, Geoffrey O. 2004. "<a href="https://repository.si.edu/handle/10088/3687">Tropical Response to the 8200 Yr B.P. Cold Event? Speleothem Isotopes Indicate a Weakened Early Holocene Monsoon in Costa Rica</a>." <em>Geology</em>, (11) 957-960.
dc.identifier.issn0091-7613
dc.identifier.urihttp://hdl.handle.net/10088/3687
dc.language.isoen_US
dc.relation.ispartofGeology (11)
dc.titleTropical Response to the 8200 Yr B.P. Cold Event? Speleothem Isotopes Indicate a Weakened Early Holocene Monsoon in Costa Rica
dc.typearticle
sro.description.unitSTRI
sro.identifier.itemID51736
sro.identifier.refworksID51444
sro.identifier.urlhttps://repository.si.edu/handle/10088/3687

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