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・ Diploon
・ Diplopanax
・ Diplopedia
・ Diplopeltis
・ Diplopeltis huegelii
・ Diplophos
・ Diplophos rebainsi
・ Diplopia
・ Diplopodia
・ Diplopodomyces
・ Diplopogon
・ Diplopoma
・ Diplopoma crenulatum
・ Diplopora
・ Diplopora oregonensis
Diploporus
・ Diploprion bifasciatum
・ Diploprora
・ Diplopseustis
・ Diplopseustis constellata
・ Diplopseustis metallias
・ Diplopseustis nigerialis
・ Diplopseustis pallidalis
・ Diplopseustis perieresalis
・ Diplopseustis prophetica
・ Diplopseustis selenalis
・ Diploptalis
・ Diploptera
・ Diplopterys
・ Diplopterys cabrerana


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Diploporus : ウィキペディア英語版
Diploporus

''Diploporus'' is an extinct genus of conifer in the yew family Taxaceae, containing the single species ''Diploporus torreyoides'' known from the middle Eocene of north central Oregon〔 and the Late Paleocene of south central North Dakota. The species was first described from a series of isolated fossil seeds in chert.〔
==History and classification==
''Diploporus torreyoides'' has been identified from a single location in the Clarno Formation, the Clarno nut beds, type locality for both the formation and the species. The nut beds are approximately east of the unincorporated community of Clarno, Oregon and currently considered to be middle Eocene in age, based on averaging zircon fission track radiometric dating which yielded an age of 43.6 and 43.7 ± 10 million years ago and Argon–argon dating radiometric dating which yielded a 36.38 ± 1.31 to 46.8 ± 3.36 mya date.〔 The average of the dates resulted in an age range of 45 to 43 mya. The beds are composed of silica and calcium carbonate cemented tuffaceous sandstones, siltstones, and conglomerates which preserve either a lake delta environment, or alternatively periodic floods and volcanic mudflows preserved with hot spring activity.〔 An unidentified species of ''Diploporus'' has been reported from the Sentinel Butte Formation near the town of Almont, North Dakota and the Beicegal Creek, North Dakota.〔 The age of the formation is based on the recovery of late Tiffanian mammals in the upper section of the formation along with the floral and palynological assemblages of the formation.
The species was described from a group of seventy five type specimens, the holotype specimen UF8542, which is currently preserved in the paleobotanical collections of the University of Florida and a large series of paratypes, totaling seventy-four specimens. The paratypes are in the collections of the National Museum of Natural History, the University of Florida, and the Oregon Museum of Science and Industry. The fossils were part of approximately 20,000 specimens collected from 1942 to 1989 by Thomas Bones, A. W. Hancock, R. A. Scott, Steven R. Manchester, and a number of high school students.〔
The ''Diploporus'' specimens were studied by paleobotanist Steven R. Manchester of the University of Florida. He published his 1994 type description for ''Diploporus torreyoides'' in the journal ''Palaeontographica Americana''〔 In his type description Manchester noted the generic name is derived from the Greek words ''Diplo'' meaning "two" and ''poros'' meaning "passage" in reference to the paired vascular scars. The specific epithet ''torreyoides'', reflects the similarities between ''Diploporus'' and the living genus ''Torreya''.〔

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