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Wessiea
''Wessiea'' is an extinct morphogenus of fern not placed in a specific family. ''Wessia'' is known from Late Cretaceous and Middle Miocene age fossils found in Central Washington USA and Southern Alberta Canada. Two species are described in the morphogenus, ''W. oroszii'' and the type species ''W. yakimaensis''.
==History and classification==
The genus was first described from specimens of slicified rhizomes and frond bases in blocks of chert. The chert was recovered from the "Ho ho" site, one of the "county line hole" fossil localities north of Interstate 82 in Yakima County, Washington.〔 The "Ho ho" site works strata which is part of the Museum Flow Package within the interbeds of the Sentinel Bluffs Unit of the central Columbia Plateau N2 Grande Ronde Basalt, Columbia River Basalt Group. The Museum Flow Package interbeds, designated the type locality, are dated to the middle Miocene and are approximately 15.6 million years old.〔
The holotype specimen, rhizomes and fronds #1–3 and 3 E2 #1–3, are preserved in chert block 3A1 and housed in the Burke Museum of Natural History and Culture as specimen number "''UWBM 56441''". The paratype, number 3F1 #2 top on specimen "UWBM 56441", is a rhizome which shows root gaps, roots and frond bases.〔 The specimens of chert were studied by paleobotanists Kathleen B. Pigg of Arizona State University and Gar W. Rothwell of Ohio University. Pigg and Rothwell published their 2001 type description for ''Wessiea yakimaensis'' in the ''American Journal of Botany''.〔 In their type description they note the etymology for the generic name is in honor of Wesley C. Wehr for his numerous contributions to Tertiary paleobotany of western North America. The specific epithet ''yakimaensis'', is a reference to the type locality in the Yakima Canyon.〔 Pigg and Rothwell noted the similarity between ''Wessiea'' and both the modern genus ''Diplazium'' and the fossil genus ''Makotopteris''.〔
The second species is known from ironstones of the Campanian age Horseshoe Canyon Formation, Alberta, recovered at the "Fred's site" locality. The fossils, housed in the Royal Tyrrell Museum of Palaeontology, were dissolved from the ironstone and embedded into a bioplastic for study. After embedding, the fossils were acid peeled by paleobotanists Rudolph Serbet and Gar W. Rothwell for study in thin section slides. Serbert and Rothell published the description of ''W. oroszii'' in a 2006 article. The specific epithet "oroszii" is a patronym honoring s Alfred Orosz, paleontologist for the Royal Tyrrell Museum, and discoverer of the species type locality.〔
抄文引用元・出典: フリー百科事典『 ウィキペディア（Wikipedia）』
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