The chironomid-temperature relationship: expression in nature and palaeoenvironmental implications

Fossils of chironomid larvae (non-biting midges) preserved in lake sediments are well-established palaeotemperature indicators which, with the aid of numerical chironomid-based inference models (transfer functions), can provide quantitative estimates of past temperature change. This approach to temp...

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Bibliographic Details
Published in:Biological Reviews
Main Authors: Eggermont, Hilde, Oliver, Heiri
Format: Article in Journal/Newspaper
Language:English
Published: 2012
Subjects:
Biology and Life Sciences
palaeoenvironmental reconstruction
FRESH-WATER MIDGES
lakes
autoecology
chironomids
temperature
PAST ENVIRONMENTAL-CONDITIONS
CHRYSOPHYTE CYST ASSEMBLAGES
SOUTHERN BRITISH-COLUMBIA
SUB-FOSSIL CHIRONOMIDAE
OXY-REGULATORY CAPACITY
NEW-ZEALAND CHIRONOMIDS
VARVED LAKE SILVAPLANA
JULY AIR-TEMPERATURE
CLIMATE-CHANGE
Arctic
New Zealand
Climate change
Subarctic
Online Access:https://biblio.ugent.be/publication/3103258
http://hdl.handle.net/1854/LU-3103258
https://doi.org/10.1111/j.1469-185X.2011.00206.x
https://biblio.ugent.be/publication/3103258/file/3103259
Description
Summary:Fossils of chironomid larvae (non-biting midges) preserved in lake sediments are well-established palaeotemperature indicators which, with the aid of numerical chironomid-based inference models (transfer functions), can provide quantitative estimates of past temperature change. This approach to temperature reconstruction relies on the strong relationship between air and lake surface water temperature and the distribution of individual chironomid taxa (species, species groups, genera) that has been observed in different climate regions (arctic, subarctic, temperate and tropical) in both the Northern and Southern hemisphere. A major complicating factor for the use of chironomids for palaeoclimate reconstruction which increases the uncertainty associated with chironomid-based temperature estimates is that the exact nature of the mechanism responsible for the strong relationship between temperature and chironomid assemblages in lakes remains uncertain. While a number of authors have provided state of the art overviews of fossil chironomid palaeoecology and the use of chironomids for temperature reconstruction, few have focused on examining the ecological basis for this approach. Here, we review the nature of the relationship between chironomids and temperature based on the available ecological evidence. After discussing many of the surveys describing the distribution of chironomid taxa in lake surface sediments in relation to temperature, we also examine evidence from laboratory and field studies exploring the effects of temperature on chironomid physiology, life cycles and behaviour. We show that, even though a direct influence of water temperature on chironomid development, growth and survival is well described, chironomid palaeoclimatology is presently faced with the paradoxical situation that the relationship between chironomid distribution and temperature seems strongest in relatively deep, thermally stratified lakes in temperate and subarctic regions in which the benthic chironomid fauna lives largely ...

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