Please use this identifier to cite or link to this item:
Title: O Caloviano do flanco norte do Guilhim (Algarve oriental): biostratigrafia e paleobiogeografia
Author: Marques, B.
Rocha, R. B.
Keywords: Stratigraphy
Issue Date: 13-Aug-2008
Abstract: Stratigraphical study of Telheiro and Cancela sections (northern slope of Guilhim hill) allowed its dating: these may be reported to the Lower Callovian, as ammonite associations typical of Rehmanni and Pictava horizons have been collected there. Hence Gracilis zone can be recognized in Algarve. Ammonites are also associated to Dinoflagellates. These microfossils have been found for the first time in the Callovian of Portugal. Callovian paleogeogtaphy is reapprised, and the limits between mesogean submediterranean and mediterranean provinces are more accurately recognized. Algarve belongs to the mediterranean province according to the typically mesogean character of the fauna where Phylloceratidae are dominant.
Appears in Collections:FCT: DCT - Ciências da Terra

Files in This Item:
File Description SizeFormat 
CT_09_02.pdf2,9 MBAdobe PDFView/Open

FacebookTwitterDeliciousLinkedInDiggGoogle BookmarksMySpace
Formato BibTex MendeleyEndnote Degois 

Items in DSpace are protected by copyright, with all rights reserved, unless otherwise indicated.