{"refrec":{"BRefID":363579,"RR":"<b>Vachard, D.; Ferriére, J.</b> (1991). Une association à Yabeina (foraminifère fusulinoide) dans le Midien (Permien supérieur) de la région de Whangaroa (Baie d'Orua, Nouvelle-Zélande) = An assemblage with Yabeina (fusulinid foraminifera) from the Midian (upper Permian) of Whangaroa area (Orua Bay), New Zealand). <i>Rev. Micropaleontol. 34(3)</i>: 201-230","BEntID":361297,"PublicFlag":1,"CheckedFlag":0,"wosflag":0,"vabbflag":0,"RefStringPartII":". <i>Rev. Micropaleontol. 34(3)</i>: 201-230","DocTypID":8,"DocType":"Journal article","MarineFlag":1,"FreshFlag":0,"BrackishFlag":0,"TerrestrialFlag":0,"Authorstring":"Vachard, D.; Ferriére, J.","OrigTitleTranslFlag":0,"Authorstringtrunc":"Vachard, D.; Ferriére, J.","Englishabstract":"Describes carbonate microfauna and microflora from the Whangaroa area (Orua Bay, New Zealand). Limestones are exotic blocks embedded in volcanic and volcano-sedimentary units. Algae are dominated by Tubiphytes. Smaller Foraminifera exhibit common Tethyan species. A revision of Nodosariids leads to the creation of Ichthyofrondina Vachard n.gen. Fusulinoids are mainly represented by the general Reichelina, Codonofusiella, Sichotenella and Chusenella. Yabeina parvula is accurately studied; this taxon belongs to a group of species previously known from Japan, Cambodia, Malaysia and British Columbia (near the Canada-USA border). Thanks to these paleobiogeographic relationships, it is deduced that the outcrop is a terrane which belongs to one or several plates of the old Cathaysia and which had migrated 3000 km to the South cross the Paleopacific. 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