The elasmobranch fauna of the late Burdigalian
, Miocene, at Werder-Uesen, Lower Saxony, Germany, and its relationships with Early Miocene faunas in the North Atlantic, Central Paratethys and Mediterranean.
In the early Miocene (Aquitanian and Burdigalian
, 23-16 Ma), occurrences of fossil Itea are widespread and nearly circumboreal in distribution, although only five are from outside of continental Europe.
A model of early calcite cementation in alluvial fans: Evidence from the Burdigalian
sandstones and limestones of the Valle'sPenede's half-graben (NE Spain), Sed.
sandstone sequence of Burdigalian age with strong gas shows.
drilled into the Burdigalian sandstone sequence a short distance from the
Catapsydrax stainforthi BOLLI, LOEBLICH, and TAPPAN are also found in this sub-member belonging to Burdigalian.
The decrease in the number of Echinoderms towards the upper part of the formation is due to the great migration of these species towards the North in Burdigalian sup.
Coralline algae, oysters and echinoids - a liaison in rhodolith formation from the Burdigalian
of the Latium-Abruzzi Platform (Italy) (M.
Based upon benthic foraminifer's dispersion and strontium isotope stratigraphy, Rupelian to Burdigalian age was considered for this formation [1,3,4,6,9].
The age of this member, based upon its foraminifers, is Burdigalian.
The target Burdigalian
Sandstones were encountered between 1,083 and 1,110
Testing the Burdigalian
gas shows encountered in Costisa-1Z is