Research Library | Digital Repository

Coelacanth fishes from the continental Triassic of the western United States. American Museum novitates ; no. 2036

Show simple item record

dc.contributor.author Schaeffer, Bobb, 1913- en_US
dc.contributor.author Gregory, Joseph Tracy, 1914- en_US
dc.date.accessioned 2005-10-06T17:02:51Z
dc.date.available 2005-10-06T17:02:51Z
dc.date.issued 1961 en_US
dc.identifier.uri http://hdl.handle.net/2246/3465
dc.description 18 p. : ill. ; 24 cm. en_US
dc.description Includes bibliographical references (p. 17-18). en_US
dc.description.abstract "There is now conclusive evidence that coelacanths are present in both the lower and the upper Triassic continental beds of the western United States. The scarcity of their remains is, in part, related to the factors that are responsible for the general rarity of fishes in these formations. The broad, flat, flood-plain environment in which the Moenkopi and Chinle-Dockum sediments were deposited (McKee, 1954; Stewart et al., 1959) was apparently more favorable for the preservation of terrestrial than of aquatic vertebrates. Metoposaur and phytosaur remains are much more abundant and more widely distributed than fish remains. The latter are restricted, as might be expected, to channel and lacustrine deposits. Although isolated actinopterygian scales are reasonably common in such deposits, associated fish remains are extremely rare. At a few localities in the Chinle complete fishes have been found in great abundance. These usually occur in lacustrine deposits in concentrations suggestive of periodic mass mortality. The apparent rarity of coelacanth remains in these concentrations suggests that they were not common in the lakes and ponds of the Chinle flood plain. On the other hand, there is no positive evidence that they were, in general, restricted to rivers and streams. Except for the Moenkopi occurrence, which is quite clearly fluviatile, the paleoecologic picture is unsettled. Isolated coelacanth bones from the Moenkopi formation include distinctive basisphenoids, the morphology of which provides the basis for establishing a new genus and species, Moenkopia wellesi. Specimens thus far recovered from the late Triassic Dockum and Chinle formations are too incomplete to permit generic identification"--P. 15-17. en_US
dc.format.extent 2382731 bytes
dc.format.mimetype application/pdf
dc.language eng en_US
dc.language.iso en_US
dc.publisher New York, N.Y. : American Museum of Natural History en_US
dc.relation.ispartofseries American Museum novitates ; no. 2036 en_US
dc.subject.lcc QL1 .A436 no.2036, 1961 en_US
dc.subject.lcsh Coelacanthiformes, Fossil -- West (U.S.) en_US
dc.subject.lcsh Fishes, Fossil -- West (U.S.) en_US
dc.subject.lcsh Paleontology -- Triassic -- West (U.S.) en_US
dc.subject.lcsh Paleontology -- West (U.S.) en_US
dc.title Coelacanth fishes from the continental Triassic of the western United States. American Museum novitates ; no. 2036 en_US
dc.title.alternative Fishes en_US
dc.type text en_US


Files in this item

This item appears in the following Collection(s)

  • American Museum Novitates
    Novitates (Latin for "new acquaintances"), published continuously and numbered consecutively since 1921, are short papers that contain descriptions of new forms and reports in zoology, paleontology, and geology. New numbers are published at irregular intervals.

Show simple item record

Search Entire Repository

Advanced Search

Browse

My Account