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

Micropaleontology; September 2003; v. 49; no. 3; p. 231-251; DOI: 10.2113/49.3.231
© 2003 Micropaleontology Project
This Article
Right arrow Figures Only
Right arrow Full Text
Right arrow Full Text (PDF)
Right arrow Submit a response
Right arrow Alert me when this article is cited
Right arrow Alert me when eLetters are posted
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
Citing Articles
Right arrow Citing Articles via HighWire
Right arrow Citing Articles via Web of Science (3)
Right arrow Citing Articles via Google Scholar
Google Scholar
Right arrow Articles by Watkins, D. K.
Right arrow Articles by Bergen, J. A.
Right arrow Search for Related Content
GeoRef
Right arrow GeoRef Citation

Article

Late Albian adaptive radiation in the calcareous nannofossil genus Eiffellithus

David K. Watkins1 and James A. Bergen2

1 Department of Geosciences, University of Nebraska, Lincoln, Nebraska 68588-0340, email: dwatkins1{at}unl.edu
2 BP America, Inc., 501 Westlake Park Blvd., Houston, Texas 77079

Well preserved nannofossil assemblages in upper Albian and lower Cenomanian hemipelagic sections from Ocean Drilling Program (ODP) Leg 171B preserve a record of the early history and adaptive radiation of the genus Eiffellithus. Seven distinct taxa are recognized and differentiated, with one previously named taxon (E. monechiae) emended and four new species described: E. praestigium, E. vonsalisiae, E. equibiramus, and E. parvus. Sample census data indicate that most species evolved, rose to dominance, and then rapidly declined to extinction, to be replaced by other members of the genus. Newly evolved species tended to remain at low abundance levels until a significant disruption in the pelagic realm resulted in the precipitous decline of the dominant species. This decline provided open niche space in the pelagic realm into which the new species could rapidly rise to dominance. These major disruptions correspond to significant changes or shifts in the sedimentological and carbon isotopic records associated with the late Albian Oceanic Anoxic Event (OAE-1d), suggesting that major changes in the strength of deep mixing and the structure of the surface water mass drove the early adaptive radiation of Eiffellithus.




This article has been cited by other articles:


Home page
Journal of Foraminiferal ResearchHome page
M. D. Georgescu and B. T. Huber
PARACOSTELLAGERINA NOV. GEN., A MERIDIONALLY COSTELLATE PLANKTONIC FORAMINIFERAL GENUS OF THE MIDDLE CRETACEOUS (LATEST ALBIAN-EARLIEST CENOMANIAN)
Journal of Foraminiferal Research, October 1, 2006; 36(4): 368 - 373.
[Abstract] [Full Text] [PDF]




JOURNAL HOME HELP CONTACT PUBLISHER SUBSCRIBE ARCHIVE SEARCH TABLE OF CONTENTS
Copyright © 2009 by Micropaleontology Project