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Coryphaenoides Hextii
''Coryphaenoides'' is a genus of rattails which is found in all oceans of the world. They are found in deep waters and ''C. yaquinae'', recorded to , is the only member in the family known from the hadal zone. The generic name means "similar to ''Coryphaena''". Species There are currently 66 recognized species in this genus: * '' Coryphaenoides acrolepis'' ( T. H. Bean, 1884) (Pacific grenadier) * '' Coryphaenoides affinis'' Günther, 1878 * ''Coryphaenoides alateralis'' N. B. Marshall & Iwamoto, 1973 * ''Coryphaenoides altipennis '' Günther, 1877 * ''Coryphaenoides anguliceps'' ( Garman, 1899) (Loose-scale grenadier) * ''Coryphaenoides ariommus'' C. H. Gilbert & W. F. Thompson, 1916 (Humboldt grenadier) * '' Coryphaenoides armatus'' ( J. Hector, 1875) (Abyssal grenadier) * ''Coryphaenoides asper'' Günther, 1877 * ''Coryphaenoides asprellus'' ( H. M. Smith & Radcliffe, 1912) * '' Coryphaenoides boops'' ( Garman, 1899) (Short-snout grenadier) * '' Coryphaenoides brevi ...
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Oligocene
The Oligocene ( ) is a geologic epoch of the Paleogene Period and extends from about 33.9 million to 23 million years before the present ( to ). As with other older geologic periods, the rock beds that define the epoch are well identified but the exact dates of the start and end of the epoch are slightly uncertain. The name Oligocene was coined in 1854 by the German paleontologist Heinrich Ernst Beyrich from his studies of marine beds in Belgium and Germany. The name comes from the Ancient Greek (''olígos'', "few") and (''kainós'', "new"), and refers to the sparsity of extant forms of molluscs. The Oligocene is preceded by the Eocene Epoch and is followed by the Miocene Epoch. The Oligocene is the third and final epoch of the Paleogene Period. The Oligocene is often considered an important time of transition, a link between the archaic world of the tropical Eocene a