{"refrec":{"BRefID":418549,"RR":"<b>Crombé, P.</b> (2025). Early and middle Holocene climate and environmental change, <b><i>in</i></b>: Nilsson Stutz, L. <i>et al.</i> <i>The Oxford handbook of mesolithic Europe. Oxford Handbooks,</i> : pp. 33-50. <a href=\"https://dx.doi.org/10.1093/oxfordhb/9780198853657.013.2\" target=\"_blank\">https://dx.doi.org/10.1093/oxfordhb/9780198853657.013.2</a>","BEntID":416379,"PublicFlag":1,"CheckedFlag":0,"wosflag":0,"vabbflag":0,"RefStringPartII":", <b><i>in</i></b>: Nilsson Stutz, L. <i>et al.</i> <i>The Oxford handbook of mesolithic Europe. Oxford Handbooks,</i> : pp. 33-50. <a href=\"https://dx.doi.org/10.1093/oxfordhb/9780198853657.013.2\" target=\"_blank\">https://dx.doi.org/10.1093/oxfordhb/9780198853657.013.2</a>","DocTypID":17,"DocType":"Book chapters","MarineFlag":0,"FreshFlag":0,"BrackishFlag":0,"TerrestrialFlag":0,"Authorstring":"Crombé, P.","OrigTitleTranslFlag":0,"Authorstringtrunc":"Crombé, P.","Englishabstract":"The Mesolithic corresponds to a period of abrupt global warming resulting in a series of profound environmental changes, such as rapid sea level rise, decreased river discharge and lake levels, increased drought and forest fires, and a radical overturn of both fauna and flora. The latter includes the rapid replacement of cold-tolerant species occurring in an open tundra environment by temperate-boreal species, adapted to the forested environment of the Early and Middle Holocene. 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