Quick
Search: 		  
advanced search
 GSW Home   GeoRef Home   My GSW Alerts   Contact GSW   About GSW   Journals List   Help 
Palynology Email Content Delivery
JOURNAL HOME HELP CONTACT PUBLISHER SUBSCRIBE ARCHIVE SEARCH TABLE OF CONTENTS
Palynology; 2004; v. 28;1; p. 129-141; DOI: 10.2113/28.1.129
© 2004 American Association of Stratigraphic Palynologists
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
Services
Right arrow Email this article to a friend
Right arrow Similar articles in this journal
Right arrow Alert me to new issues of the journal
Right arrow Download to citation manager
Citing Articles
Right arrow Citing Articles via Google Scholar
Google Scholar
Right arrow Articles by DODSWORTH, P.
Right arrow Search for Related Content
GeoRef
Right arrow GeoRef Citation

THE PALYNOLOGY OF THE CENOMANIAN–TURONIAN (CRETACEOUS) BOUNDARY SUCCESSION AT AKSUDERE IN CRIMEA, UKRAINE

PAUL DODSWORTH

Ichron Limited, 5 Dalby Court, Gadbrook Business Centre, Rudheath, Northwich, Cheshire CW9 7TN, U.K.

The Upper Cenomanian ‘black shales’ at Aksudere in Crimea contain a distinct palynological association dominated by prasinophyte phycomata, mainly leiospheres and tasmanitids, and peridinioid dinoflagellate cysts, mainly Trithyrodinium suspectum ukrainense subsp. nov. Prasinophyte dominated assemblages have not previously been reported from Cenomanian–Turonian boundary organic rich deposits. Their presence confirms probable deposition under oxygen-deficient bottom waters in this area.






JOURNAL HOME HELP CONTACT PUBLISHER SUBSCRIBE ARCHIVE SEARCH TABLE OF CONTENTS
Copyright © 2009 by American Association of Stratigraphic Palynologists