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

Journal of Paleontology; July 2005; v. 79; no. 4; p. 702-718; DOI: 10.1666/0022-3360(2005)079[0702:FCPLT]2.0.CO;2
© 2005 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 (6)
Right arrow Citing Articles via Google Scholar
Google Scholar
Right arrow Articles by LEROSEY-AUBRIL, R.
Right arrow Articles by FEIST, R.
Right arrow Search for Related Content
GeoRef
Right arrow GeoRef Citation

FIRST CARBONIFEROUS PROTASPID LARVAE (TRILOBITA)

RUDY LEROSEY-AUBRIL1 and RAIMUND FEIST1

1 Laboratoire de Paléontologie, Paléobiologie et Phylogénie, Institut des Sciences de l'Evolution de Montpellier, Université Montpellier II, 34095 Montpellier Cedex 05, F <lerosey{at}isem.univ-montp2.fr> and <rfeist{at}isem.univ-montp2.fr>

The recovery of well-preserved silicified larvae from the early Tournaisian of Montagne Noire, southern France, allows the first description of the early ontogeny of proetoid trilobites, survivors of the end-Devonian Hangenberg extinction event. The fauna comprises various taxa that can only partly and tentatively be assigned to the genera Liobolina, Diacoryphe, and Pedinocoryphe without specific attribution. The close resemblance of these larvae to previously described proetoid larvae from the Ordovician and Devonian emphasizes the ontogenetic homogeneity of this superfamily. Moreover, it supports the view that the Proetida is composed of two clades: the Aulacopleuroidea/Bathyuroidea group and the Proetoidea. The Carboniferous anaprotaspides exhibit an unusually wide size-range that may provide evidence of the acquisition of an extended planktonic period in the early ontogeny of at least some Carboniferous proetoids. This change in the ontogenetic strategy may have enabled proetoid trilobites to survive during the end-Devonian biocrises.




This article has been cited by other articles:


Home page
Journal of PaleontologyHome page
C. CRONIER
LARVAL MORPHOLOGY AND ONTOGENY OF AN UPPER DEVONIAN PHACOPID: NEPHRANOPS FROM THURINGIA, GERMANY
Journal of Paleontology, July 1, 2007; 81(4): 684 - 700.
[Abstract] [Full Text] [PDF]


Home page
PaleobiologyHome page
N. C. Hughes, A. Minelli, and G. Fusco
The ontogeny of trilobite segmentation: a comparative approach
Paleobiology, December 1, 2006; 32(4): 602 - 627.
[Abstract] [Full Text] [PDF]


Home page
Geological MagazineHome page
R. LEROSEY-AUBRIL
Ontogeny of Drevermannia and the origin of blindness in Late Devonian proetoid trilobites
Geological Magazine, January 1, 2006; 143(1): 89 - 104.
[Abstract] [Full Text] [PDF]




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