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; March 2008; v. 82; no. 2; p. 351-361; DOI: 10.1666/06-127.1
© 2008 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 ISI Web of Science
Right arrow Alert me to new issues of the journal
Right arrow Download to citation manager
Right arrow reprints & permissions
Google Scholar
Right arrow Articles by Schlögl, J.
Right arrow Articles by Atrops, F.
GeoRef
Right arrow GeoRef Citation

ARTICLE

Early Tithonian Serpulid-Dominated Cavity-Dwelling Fauna, and the Recruitment Pattern of the Serpulid Larvae

Ján Schlögl1, Jozef Michalík2, Kamil Zágorsek3 and François Atrops4

1 Department of Geology and Paleontology, Faculty of Sciences, Comenius University, Mlynska dolina, Pav. G, SK-842 15 Bratislava, Slovakia, <schlogl{at}nic.fns.uniba.sk>
2 Geological Institute of Slovak Academy of Sciences, Dubravska 9, P.O. Box 106, SK-840 05 Bratislava, Slovakia, <geolmich{at}savba.sk>
3 National Museum, Václavské námestí 68, CZ-115 79, Praha 1, Czech Republic, <kamil.zagorsek{at}nm.cz>
4 Centre des Sciences de la Terre, Université Claude Bernard Lyon1, 27-43 Bd 11 Novembre, F-69 622 Villeurbanne, France, <Francois.Atrops{at}univ-lyon1.fr>

A Lower Tithonian cavity-dwelling community from pelagic carbonate platform deposits of the Czorsztyn Unit, Western Carpathians, represents a succession of mostly solitary coelobite organisms, dominated by scleractinian corals and small-sized serpulids during the initial recruitment stage, and by serpulids during the following recruitment stages. These bioconstructors were accompanied with other suspension feeders: thecideidine brachiopods, oysters, bryozoans, sponges, crinoids and sessile foraminifers. The boundary between the first and the second recruitment stage represents an interval of aggregate growth interruption, when a thin sheet of cyclostome bryozoans developed. Corals and serpulids Neovermilia and Vermiliopsis are primary bioconstructors; all other associated organisms profited from the free spaces between the serpulid tubes. The aggregates were already bioeroded, mineralized and encrusted during their growth. Serpulid larvae show a special recruitment pattern. Their tubes were observed attached on the inner surfaces of adult serpulid tubes only. Possible causes of such a larval behaviour involve several physical, biological or chemical factors. Except for the first recruitment stage, the rest of the succession seems to be physically controlled by the gradual infilling of cavities.







JOURNAL HOME HELP CONTACT PUBLISHER SUBSCRIBE ARCHIVE SEARCH TABLE OF CONTENTS
Copyright © 2008 by Paleontological Society