Comment on “The Response of Vegetation on the Andean Flank in Western Amazonia to Pleistocene Climate Change”

dc.contributor.authorPunyasena, Surangi W.
dc.contributor.authorDalling, James W.
dc.contributor.authorJaramillo, Carlos A.
dc.contributor.authorTurner, Benjamin L.
dc.date.accessioned2011-12-20T14:44:52Z
dc.date.available2011-12-20T14:44:52Z
dc.date.issued2011
dc.description.abstractCárdenas et al. (Reports, 25 February 2011, p. 1055) used the presence of Podocarpus pollen and wood to infer =5°C cooling of Andean forests during Quaternary glacial periods. We show that (i) Podocarpus has a wide elevation range in the Neotropics, and (ii) edaphic factors cannot be discounted as a factor governing its distribution. Paleoecologists should therefore reevaluate Podocarpus as a cool-temperature proxy.
dc.format.extent1825–1825
dc.identifier0036-8075
dc.identifier.citationPunyasena, Surangi W., Dalling, James W., Jaramillo, Carlos A., and Turner, Benjamin L. 2011. "<a href="https://repository.si.edu/handle/10088/17531">Comment on “The Response of Vegetation on the Andean Flank in Western Amazonia to Pleistocene Climate Change”</a>." <em>Science</em>, 333, (6051) 1825–1825. <a href="https://doi.org/10.1126/science.1207525">https://doi.org/10.1126/science.1207525</a>.
dc.identifier.issn0036-8075
dc.identifier.urihttp://hdl.handle.net/10088/17531
dc.relation.ispartofScience 333 (6051)
dc.titleComment on “The Response of Vegetation on the Andean Flank in Western Amazonia to Pleistocene Climate Change”
dc.typearticle
sro.description.unitSTRI
sro.identifier.doi10.1126/science.1207525
sro.identifier.itemID102676
sro.identifier.refworksID71756
sro.identifier.urlhttps://repository.si.edu/handle/10088/17531

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