Quick
Search: 
 
advanced search
 GSW Home    GeoRef Home    My GSW Alerts    Contact GSW    About GSW    Journals List    Help 
  Journal of Paleontology   Signup for GSW Email News
JOURNAL HOME HELP CONTACT PUBLISHER SUBSCRIBE ARCHIVE SEARCH TABLE OF CONTENTS

Journal of Paleontology; May 2000; v. 74; no. 3; p. 386-393; DOI: 10.1666/0022-3360(2000)074<0386:AVMOSS>2.0.CO;2
© 2000 Paleontological Society
This Article
Right arrow Figures Only
Right arrow Full Text
Right arrow Full Text (PDF)
Right arrow Alert me when this article is cited
Right arrow Alert me if a correction is posted
Right arrow Citation Map
Services
Right arrow Email this article to a friend
Right arrow Similar articles in this journal
Right arrow Similar articles in Web of Science
Right arrow Alert me to new issues of the journal
Right arrow Download to citation manager
Right arrow reprints & permissions
Citing Articles
Right arrow Citing Articles via HighWire
Right arrow Citing Articles via Web of Science (5)
Right arrow Citing Articles via Google Scholar
Google Scholar
Right arrow Articles by ZHANG, X.-G.
Right arrow Articles by PRATT, B. R.
Right arrow Search for Related Content
GeoRef
Right arrow GeoRef Citation

A VARIED MIDDLE ORDOVICIAN SPONGE SPICULE ASSEMBLAGE FROM WESTERN NEWFOUNDLAND

XI-GUANG ZHANG1 and BRIAN R. PRATT1

1 Department of Geological Sciences, University of Saskatchewan, 114 Science Place, Saskatoon, Saskatchewan S7N 5E2, Canada, <xgzhang@sprint.ca>, <brian.pratt@usask.ca>

Abundant and morphologically fairly diverse siliceous sponge spicules of Darriwilian (Middle Ordovician) age were collected from the Table Cove Formation of Port au Port Peninsula, western Newfoundland. Without co-occurrence of appropriate sponge body fossils, it is difficult to refer these disarticulated sponge spicules to existing or to new taxa. However, representatives of demosponges and hexactinellids are recognized. While marked differences are noted between older and younger lithistid dendroclones, for example, spicule form in these Middle Ordovician specimens is similar overall to previously known assemblages of various ages, demonstrating the morphologically conservative nature of the spicular skeleton.




This article has been cited by other articles:


Home page
Journal of PaleontologyHome page
LATE ORDOVICIAN JAWED POLYCHAETE FAUNAS OF THE TYPE CINCINNATIAN REGION, U.S.A
Journal of Paleontology, May 1, 2003; 77(3): 509 - 523.



Home page
Journal of PaleontologyHome page
OCCURRENCE OF THE SILICEOUS SPONGE SPICULE KONYRIUM (HEXACTINELLIDA) IN THE UPPER CAMBRIAN OF THE MACKENZIE MOUNTAINS, NORTHWESTERN CANADA
Journal of Paleontology, May 1, 2002; 76(3): 565 - 569.





JOURNAL HOME HELP CONTACT PUBLISHER SUBSCRIBE ARCHIVE SEARCH TABLE OF CONTENTS
Copyright © 2009 by Paleontological Society