Chironomids can be reliable proxies for Holocene temperatures. A comment on Velle et al. (2010)

Brooks, Stephen J. and Axford, Yarrow and Heiri, Oliver and Langdon, Peter G. and Larocque-Tobler, Isabelle. (2012) Chironomids can be reliable proxies for Holocene temperatures. A comment on Velle et al. (2010). Holocene, 22 (12). pp. 1495-1500.

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Velle et al. (2010) discussed discrepancies between Scandinavian Holocene chironomid-inferred temperature estimates, which they attribute to the response of chironomids to environmental variables other than temperature and to taxonomic shortcomings. They suggest ways in which the reliability of chironomid-based paleotemperature reconstructions could be improved by taking into account ecological complexity. While we agree with many of their recommendations, based on the results of other work, we think their paper is unnecessarily pessimistic regarding the ability of existing chironomid-based temperature inference models to provide reliable estimates of past temperature. We offer a critique of the main points discussed by Velle et al. (2010) and provide evidence that chironomid-based temperature inference models can reliably reconstruct mean July air temperature in the Lateglacial and Holocene over millennial and centennial timescales.
Faculties and Departments:05 Faculty of Science > Departement Umweltwissenschaften > Geowissenschaften > Geoökologie (Heiri)
UniBasel Contributors:Heiri, Oliver
Item Type:Article, refereed
Article Subtype:Further Journal Contribution
Publisher:Sage Publications
Note:Publication type according to Uni Basel Research Database: Journal item
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Last Modified:16 Nov 2020 14:41
Deposited On:16 Nov 2020 14:41

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