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Comment on The Response of Vegetation on the Andean Flank in Western Amazonia to Pleistocene Climate Change
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| dc.contributor.author | Punyasena, Surangi W. | en |
| dc.contributor.author | Dalling, James W. | en |
| dc.contributor.author | Jaramillo, Carlos A. | en |
| dc.contributor.author | Turner, Benjamin L. | en |
| dc.date.accessioned | 2011-12-20T14:44:52Z | |
| dc.date.available | 2011-12-20T14:44:52Z | |
| dc.date.issued | 2011 | |
| dc.identifier.citation | Punyasena, Surangi W., Dalling, James W., Jaramillo, Carlos A., and Turner, Benjamin L. 2011. "<a href="https%3A%2F%2Frepository.si.edu%2Fhandle%2F10088%2F17531">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> | en |
| dc.identifier.issn | 0036-8075 | |
| dc.identifier.uri | http://hdl.handle.net/10088/17531 | |
| dc.description.abstract | Cárdenas 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. | en |
| dc.relation.ispartof | Science | en |
| dc.title | Comment on The Response of Vegetation on the Andean Flank in Western Amazonia to Pleistocene Climate Change | en |
| dc.type | Journal Article | en |
| dc.identifier.srbnumber | 102676 | |
| dc.identifier.doi | 10.1126/science.1207525 | |
| rft.jtitle | Science | |
| rft.volume | 333 | |
| rft.issue | 6051 | |
| rft.spage | 1825 | |
| rft.epage | 1825 | |
| dc.description.SIUnit | STRI | en |
| dc.description.SIUnit | Peer-reviewed | en |
| dc.citation.spage | 1825 | |
| dc.citation.epage | 1825 |
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