{"refrec":{"BRefID":231811,"RR":"<b>Vecoli, M.; Samuelsson, J.</b> (2001). Reworked acritarchs as provenance indicators in the Lower Palaeozoic of Denmark. <i>C. r. Acad. sci., Sér. 2, Sci. terre planètes 332(7)</i>: 465-471. <a href=\"http://dx.doi.org/10.1016/S1251-8050(01)01555-5\" target=\"_blank\">dx.doi.org/10.1016/S1251-8050(01)01555-5</a>","BEntID":223523,"PublicFlag":1,"CheckedFlag":1,"wosflag":0,"vabbflag":null,"RefStringPartII":". <i>C. R. Acad. Sci., Sér. 2, Sci. Terre Planètes 332(7)</i>: 465-471. <a href=\"https://dx.doi.org/10.1016/S1251-8050(01)01555-5\" target=\"_blank\">https://dx.doi.org/10.1016/S1251-8050(01)01555-5</a>","DocTypID":8,"DocType":"Journal article","MarineFlag":1,"FreshFlag":0,"BrackishFlag":0,"TerrestrialFlag":0,"Authorstring":"Vecoli, M.; Samuelsson, J.","OrigTitleTranslFlag":0,"Authorstringtrunc":"Vecoli, M.; Samuelsson, J.","Englishabstract":"Profuse and well-preserved acritarchs were recovered from subsurface Lower Palaeozoic successions cored by the boreholes Slagelse-1 and Pernille-1 (Danish-North German Basin). Together with Llandovery in situ microphytoplankton, reworked Cambrian and Ordovician species occur. The reworked Ordovician acritarchs show a clear Perigondwanan palaeobiogeographic affinity and indicate elastic sedimentary input from a Perigondwanan-related terrane located south of the East European Platform. 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