%0 Journal Article
%T Middle Oxfordian ammonite biostratigraphy of the Lower Santiago Formation at Taman, San Luis Potosi, Mexico - with notes on Mexico-Caribbean ochetoceratins
%A Ol¨®riz
%A Federico
%A VillaseŁżor
%A Ana B.
%A L¨®pez-Palomino
%A Isabel
%J Revista mexicana de ciencias geol¨®gicas
%D 2008
%I Universidad Nacional Aut¨®noma de M¨¦xico
%X bed-by-bed sampling of ammonites from clayey to calcareous siltstones of the basal part of the santiago formation at the type section in tam¨˘n, san luis potosi (mexico) is first reported. ammonites belonging to assemblages described by burckhardt (1912), usually interpreted as middle to upper oxfordian, are restricted to the lowermiddle oxfordian plicatilis zone, antecedens subzone. perisphinctes (dichotomosphinctes) durangensis (burckhardt, 1912) is revised and its biostratigraphic interpretation constrained by its co-occurrence with gregoryceras. evidence for the occurrence of perisphinctes (perisphinctes), perisphinctes (otosphinctes), and passendorferia or sequeirosia is first reported from mexico -within a precise biostratigraphic context. burckhardt's oxfordian ochetoceratins are re-examined and their affinity with cuban counterparts is approached. from a paleobiogeographical point of view, metapopulation dynamics and potentially involved events (e.g., temporary, ancillary, selective vicariancy and subsequent ecological capture) well apply for understanding the biogeographical significance of the ammonite assemblies described.
%K ammonites
%K oxfordian
%K santiago formation
%K taman
%K mexico.
%U http://www.scielo.org.mx/scielo.php?script=sci_abstract&pid=S1026-87742008000200006&lng=en&nrm=iso&tlng=en