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- W2006456435 abstract "The shell microstructure of Ordovician Cornulites species is in general similar to Silurian species. The earliest cornulitid from Baltica, C. semiapertus Öpik, 1930 (Darriwilian), has vesicles, lamellar shell structure, but no pseudopunctae. The earliest Cornulites with pseudopunctae appears in the Katian. The initial shell structure of cornulitids may have been microlamellar, but without pseudopunctae." @default.
- W2006456435 created "2016-06-24" @default.
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- W2006456435 date "2010-06-01" @default.
- W2006456435 modified "2023-09-27" @default.
- W2006456435 title "Shell microstructure of<i>Cornulites</i><i>semiapertus</i>Öpik, 1930 and other early cornulitids from the Ordovician of North Estonia" @default.
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- W2006456435 doi "https://doi.org/10.1080/11035897.2010.483309" @default.
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