) vegetation (Berry, 1937a; Romero, 1968, 1973; Freile, 1972;
The Clayton Formation, itself, is overlain by the later Paleocene
Porters Creek Formation (not figured), which contains the material that is mined to manufacture the product "Kitty Litter."
Eccentric bulla appear not only in the Kemp Clay, but also upsection in Globorotalia pseudobulloides of the Paleocene
Wills Point Formation.
Planktonic foraminifera from the Ranikot and basal Laki formation(Paleocene
and Eocene) of the Lakhra area Sind Pakistan.
The DIVA results indicate that the Maestrichtian to Paleocene
sediments in the southern and mainly in the southwestern sector of the Anambra basin should be the major sedimentary strata with liquid hydrocarbon potentials, whereas the Lower Cretaceous and particularly the Santonian sediments exhibit the highest potentials for gaseous hydrocarbons.
Orbital tuning of the complete Late Paleocene
and Early Eocene record at Walvis Ridge (South Atlantic) has indicated a link between the timing of the hyperthermals and eccentricity maxima (Lourens et al.
The magnetostratigraphy of the uppermost 100m of the Maastrichtian and the basal 70m of the Paleocene
showed magnetochrons C31 to C27, that correlate well with the magnetostratigraphy of the classic section at Bottaccione, Gubbio, (Alvarez and Lowrie, 1977) and the Agost section 100km farther east (Groot et al., 1989).
) in the continental shelf of the East China Sea; A.
Turtles and Crocodilians Directly above the Cretaceous/Tertiary Boundary in Pulaski County, Illinois.
In the North Pacific the Leg 86 data confirmed a large reduction in aeolian grain size found to occur once before at the Paleocene/Eocene boundary, suggesting that atmospheric circulation in the early Eocene was much more sluggish than in the late Paleocene
. Samples from that same cruise were later used to demonstrate that this grain-size change was one of several significant paleoclimatic changes that occur at the Paleocene/Eocene boundary.
The orbitoidiform larger foraminifera including species of Setia and Orbitosiphon in the Lockhart Limestone and lower part of the Patala Formation represent the late Paleocene
Smaller Benthic Foraminiferal Zone 4 (SBZ4).