The Ordovician Graptolite Genus Paraglossograptus Mu
- 1 March 1972
- journal article
- research article
- Published by Cambridge University Press (CUP) in Geological Magazine
- Vol. 109 (2) , 99-113
- https://doi.org/10.1017/s0016756800039492
Abstract
Summary: The lacinia in Paraglossograptus Mu is shown to consist of four ladder-like networks which are independent of each other and have no direct connection with spinose thecal apertural processes. The lacinial networks are positioned at the corners of the quadrangular rhabdosome as in Paraglossograptus ? sp. of Whittington & Rickards, which is described here as Paraglossograptus proteus (Harris & Thomas). Paraglossograptus etheridgei (Harris, 1924), the important Ordovician zone fossil, together with P. typicalis Mu and P. latus Hsü, are considered junior synonyms of Reteograptus tentaculatus J. Hall, 1865. P. tentaculatus (J. Hall, 1865), is regarded here as the type species of Paraglossograptus Mu. Detailed comparisons are made between P. tentaculatus and the stratigraphically younger P. proteus (Harris & Thomas), and with Glossograptus holmi Bulman, a species in some ways intermediate between Paraglossograptus and Glossograptus Emmons.Keywords
This publication has 6 references indexed in Scilit:
- Ordovician Graptolite Zones of Western Newfoundland in Relation to Paleogeography of the North AtlanticGSA Bulletin, 1971
- GRAPTOLITES OF NORTH AMERICAPublished by Geological Society of America ,1947
- The lower Ordovician (Tetragraptus zone) at Saint John, New Brunswick, and the new genus ProtistograptusAmerican Journal of Science, 1915
- Bibliographic index of American Ordovician and Silurian fossils, pt. 1Bulletin of the United States National Museum, 1915
- The succession of faunas at Levis, P. QAmerican Journal of Science, 1914
- North American Graptolites: New Species and Vertical RangeThe Journal of Geology, 1896