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The Gyanyima Limestone is one of the isolated carbonate build‐ups that have a probable Neotethyan seamount origin, distributed along the Yarlung‐Zangbo Suture in southern Tibet. The limestone yields a highly diversified foraminiferal fauna consisting of nine fusuline and 37 taxa of non‐fusuline foraminifers. This foraminiferal fauna is dominated by Reichelina pulchra, Colaniella parva and the characteristic...
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