{"refrec":{"BRefID":234127,"RR":"<b>Godefroid, J.</b> (1995). <i>Dayia shirleyi</i> ALVAREZ & RACHEBOEUF, 1986, un brachiopode silurien dans les \"Schistes de Mondrepuis\" à Muno (sud de la Belgique). <i>Bull. Kon. Belg. Inst. Natuurwet. Aardwet. = Bull. - Inst. r. sci. nat. Belg., Sci. Terre 65</i>: 269-272","BEntID":225811,"PublicFlag":1,"CheckedFlag":0,"wosflag":0,"vabbflag":null,"RefStringPartII":". <i>Bull. Kon. Belg. Inst. Natuurwet. Aardwet. = Bull. - Inst. r. sci. nat. Belg., Sci. Terre 65</i>: 269-272","DocTypID":8,"DocType":"Journal article","MarineFlag":1,"FreshFlag":0,"BrackishFlag":0,"TerrestrialFlag":0,"Authorstring":"Godefroid, J.","OrigTitleTranslFlag":0,"Authorstringtrunc":"Godefroid, J.","Englishabstract":"At Muno, on the northern border of the Givonne Anticlinorium, numerous <i>Dayia shirleyi</i> ALVAREZ & RACHEBOEUF, 1986 occur in the lower part of the \"Shales of Mondrepuis\" overlying the \"Conglomerate of Pepin\", base of the Gedinnian. The presence of this brachiopod indicates that the lower part of the Lower Gedinnian at Muno is of Silurian (Prídolí) age.","AbstractOtherLang":"A Muno, au bord nord de l'Anticlinorium de Givonne, de nombreuses <i>Dayia shirleyi</i> ALVAREZ & RACHEBOEUF, 1986 proviennent de la partie inférieure des \"Schistes de Mondrepuis\" surmontant le \"Poudingue de Fépin\", base du Gedinnien. 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