Climate of the Past Discussions www.clim-past-discuss.net 1814-9340 1814-9359 6 4 2010 10.5194/cpd-6-1351-2010 http://www.clim-past-discuss.net/6/1351/2010/ http://www.clim-past-discuss.net/6/1351/2010/cpd-6-1351-2010.html http://www.clim-past-discuss.net/6/1351/2010/cpd-6-1351-2010.pdf 1351 1389 2010-07-16 Refugia of marine fish in the Northeast Atlantic during the Last Glacial Maximum: concordant assessment from archaeozoology and palaeotemperature reconstructions A. J. Kettle kettle@oswego.edu A. Morales-Muñiz E. Roselló-Izquierdo D. Heinrich L. A. Vøllestad Department of Earth Science, SUNY-Oswego, Oswego, New York, USA Laboratorio de Arqueozoologia, Universidad Autonoma de Madrid, Madrid, Spain Boesselstrasse 9, 24937 Flensburg, Germany Center for Ecological and Evolutionary Synthesis, Department of Biology, University of Oslo, Oslo, Norway Archaeozoological finds of the remains of marine and amphihaline fish from the Last Glacial Maximum (LGM) ca. 21 ka ago show evidence of very different species ranges compared to the present. We show how an ecological niche model (ENM) based on palaeoclimatic reconstructions of sea surface temperature and bathymetry can be used to effectively predict the spatial range of marine fish during the LGM. The results indicate that the ranges of marine fish species that are now in Northwestern Europe were almost completely displaced southward from the modern distribution. Significantly, there is strong evidence that there was an invasion of fish of current economic importance into the Western Mediterranean through the Straits of Gibraltar, where they were exploited by Palaeolithic human populations. There has been much recent interest in the marine glacial refugia to understand how the ranges of the economically important fish species will be displaced with the future climate warming. Recent ENM studies have suggested that species ranges may not have been displaced far southward during the coldest conditions of the LGM. However, archaeozoological evidence and LGM ocean temperature reconstructions indicate that there were large range changes, and certain marine species were able invade the Western Mediterranean. 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