De Eurasian Lakes with Respect to Temperature and Continentality: Development and Application of New Chironomid-Based Climate-Inference Models in Northern Russia
Quaternary Science Reviews 30 (2011) 1122e1141 Contents lists available at ScienceDirect Quaternary Science Reviews journal homepage: www.elsevier.com/locate/quascirev The distribution and abundance of chironomids in high-latitude Eurasian lakes with respect to temperature and continentality: development and application of new chironomid-based climate-inference models in northern Russia A.E. Self a,b,*, S.J. Brooks a, H.J.B. Birks b,c,d, L. Nazarova e, D. Porinchu f, A. Odland g, H. Yang b, V.J. Jones b a Department of Entomology, Natural History Museum, Cromwell Road, London SW7 5BD, UK b Environmental Change Research Centre, Department of Geography, University College London, Gower Street, London WC1E 6BT, UK c Department of Biology, Bjerknes Centre for Climate Research, University of Bergen, P.O. Box 7803, N-5020 Bergen, Norway d School of Geography and the Environment, University of Oxford, South Parks Road, Oxford OX1 3QY, UK e Alfred Wegener Institute for Polar and Marine Research, Telegrafenberg A 43, 14473 Potsdam, Germany f Department of Geography, The Ohio State University, 1036 Derby Hall, 154 N. Oval Mall, Columbus, OH 43210, USA g Institute of Environmental Studies, Telemark University College, N-3800 Bø, Norway article info abstract Article history: The large landmass of northern Russia has the potential to influence global climate through amplification Received 10 June 2010 of climate change. Reconstructing climate in this region over millennial timescales is crucial for Received in revised form understanding the processes that affect the global climate system. Chironomids, preserved in lake 18 January 2011 sediments, have the potential to produce high resolution, low error, quantitative summer air temperature Accepted 19 January 2011 reconstructions.
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