Late Cretaceous Planktonic Foraminiferal Bioevents in Thetethys and in the Southern Ocean Record: An Overview

Research Article| October 01, 2003 LATE CRETACEOUS PLANKTONIC FORAMINIFERAL BIOEVENTS IN THETETHYS AND IN THE SOUTHERN OCEAN RECORD: AN OVERVIEW Maria Rose Petrizzo Maria Rose Petrizzo 1 Dipartimento di Scienze della Terra "Ardito Desio", Universita' degli Studi di Milano, via Mangiagalli 34, I-20133 Milano, Italy 1E-mail: mrose.petrizzo@unimi.it Search for other works by this author on: GSW Google Scholar Journal of Foraminiferal Research (2003) 33 (4): 330–337. https://doi.org/10.2113/0330330 Article history received: 05 Aug 2002 accepted: 15 Oct 2002 first online: 03 Mar 2017 Cite View This Citation Add to Citation Manager Share Icon Share Facebook Twitter LinkedIn MailTo Tools Icon Tools Get Permissions Search Site Citation Maria Rose Petrizzo; LATE CRETACEOUS PLANKTONIC FORAMINIFERAL BIOEVENTS IN THETETHYS AND IN THE SOUTHERN OCEAN RECORD: AN OVERVIEW. Journal of Foraminiferal Research 2003;; 33 (4): 330–337. doi: https://doi.org/10.2113/0330330 Download citation file: Ris (Zotero) Refmanager EasyBib Bookends Mendeley Papers EndNote RefWorks BibTex toolbar search Search Dropdown Menu toolbar search search input Search input auto suggest filter your search All ContentBy SocietyJournal of Foraminiferal Research Search Advanced Search Abstract The Late Cretaceous planktonic foraminiferal distribution recorded at several drill sites (Deep Sea Drilling Project and Ocean Drilling Program) in the South Atlantic and south Indian Ocean and from sediment outcrops in the Tethyan region (Gubbio and El Kef) have been analyzed in order to investigate the presence of a similar sequence of bioevents occurring at low, middle, and high latitude. Comparative analysis highlights the co-occurrence of several bioevents; some of them are isochronous bioevents occurring in the Tethys and in the Southern Ocean record, whereas others are diachronous across latitudes but can be used for correlation at regional scale, as they show the same stratigraphic distribution in the South Atlantic and Indian Ocean record. Isochronous bioevents are the first and the last occurrence of Helvetoglobotruncana helvetica, and the first appearance of Falsotruncana maslakovae in the lower-middle Turonian. The first occurrence of Heterohelix papula in the Southern Ocean sites, correlated with the first occurrence of large heterohelicids in the Tethyan area, allows the Coniacian/Santonian boundary to be identified. The most reliable bioevents useful for correlation at a regional scale in the Southern Ocean record are the last occurrence of the marginotruncanids in the upper Santonian, the first and the last occurrence of Globigerinelloides impensus from the uppermost Santonian to upper Campanian, the first occurrence of Heterohelix rajagopalani in the middle-upper Campanian, and the appearance of Abathomphalus mayaroensis in the lower Maastrichtian. You do not have access to this content, please speak to your institutional administrator if you feel you should have access.