{"refrec":{"BRefID":231701,"RR":"<b>Van Nieuwenhove, N.; Vandenbroucke, T.R.A.; Verniers, J.</b> (2006). Chitinozoan biostratigraphy of the Upper Ordovician Greenscoe section, Southern Lake District, UK. <i>Rev. Palaeobot. Palynol. 139(1-4)</i>: 151-169. <a href=\"http://dx.doi.org/10.1016/j.revpalbo.2005.07.009\" target=\"_blank\">dx.doi.org/10.1016/j.revpalbo.2005.07.009</a>","BEntID":223413,"PublicFlag":1,"CheckedFlag":1,"wosflag":1,"vabbflag":null,"RefStringPartII":". <i>Rev. Palaeobot. Palynol. 139(1-4)</i>: 151-169. <a href=\"https://dx.doi.org/10.1016/j.revpalbo.2005.07.009\" target=\"_blank\">https://dx.doi.org/10.1016/j.revpalbo.2005.07.009</a>","DocTypID":8,"DocType":"Journal article","MarineFlag":1,"FreshFlag":0,"BrackishFlag":0,"TerrestrialFlag":0,"Authorstring":"Van Nieuwenhove, N.; Vandenbroucke, T.R.A.; Verniers, J.","OrigTitleTranslFlag":0,"Authorstringtrunc":"Van Nieuwenhove, N. <i>et al.</i>","Englishabstract":"Nineteen samples taken in the Upper Ordovician Kirkley Bank Formation at the recent Greenscoe section yielded a rich and moderately to well preserved chitinozoan assemblage, in spite of a high Conodont Colour Alteration Index. Within the assemblage, the Baltoscandian Fungochitina spinifera Biozone could be recognized, indicating a strong faunal exchange between the Baltica palaeocontinent and the Avalonian palaeomicrocontinent during the Late Ordovician. 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