Publications home >   American Museum Novitates >
 
Please use this identifier when citing this item: http://hdl.handle.net/2246/2604
Infraorbital bones and their bearing on the phylogeny and geography of osteoglossomorph fishes. American Museum novitates ; no. 2394

File SizeFormat
 
N2394.pdf2595KbAdobe PDFOpen
Download Problems
Title: Infraorbital bones and their bearing on the phylogeny and geography of osteoglossomorph fishes. American Museum novitates ; no. 2394
Authors: Nelson, Gareth J.
Issue Date: 1969
Publisher: New York, N.Y. : American Museum of Natural History
Series/Report no.: American Museum novitates ; no. 2394
Abstract: "The primitive condition of the teleostean infraorbital series probably included seven separate bones from the antiorbital to the dermosphenotic. The anterior four bones probably enclosed more than one neuromast each, but the posterior three bones probably enclosed only one neuromast each. Reduction both of bone and neuromast numbers seems to have occurred during the evolution of most teleostean groups. The primitive condition of seven infraorbital bones occurs in at least some members of all major teleostean groups except the Osteoglossomorpha. It is suggested that the osteoglossomorph condition, typically of six or fewer bones, has resulted from secondary fusion between two of the middle bones of the series. Infraorbital and other evidence, primarily the structure of the caudal fin, indicate that the Recent Osteoglossomorpha constitute a monophyletic group, and suggest certain interrelationships among the members of that group. Nevertheless, some interrelationships remain problematic...
Description: 37 p. : ill. ; 24 cm.
Includes bibliographical references (p. 32-37).
URI: http://hdl.handle.net/2246/2604

Department of Library Services
American Museum of Natural History
Central Park West at 79th St., New York, NY 10024
© American Museum of Natural History, 2006
Powered by DSpace