E. Schrank, NONMARINE CRETACEOUS PALYNOLOGY OF NORTHERN KORDOFAN, SUDAN, WITH NOTES ON FOSSIL SALVINIALES (WATER FERNS), Geologische Rundschau, 83(4), 1994, pp. 773-786
A palynological investigation of 164 samples from 18 water wells in no
rthern Kordofan, Sudan, enabled the recognition of five informal zones
based on pollen and spore assemblages ranging in age from Albian to M
aastrichtian. The youngest (late Campanian- Maastrichtian) assemblages
are restricted to the Bagbag Basin, whereas Albian - Cenomanian (to T
uronian) sediments are widespread to the east and west of the Bagbag a
rea. Impressions of Salvinia floating leaves from outcrops of the uppe
r Hamrat el Wuz Formation, western part of the study area, are among t
he oldest occurrences of this water fern and indicate a Campanian - Ma
astrichtian age for these sediments. The vertical distribution of hygr
ophilous (pteridophytic spores) versus xerophilous (ephedroids and pos
sibly small, weakly sculptured tricolporates) elements in the palynofl
oras suggests widespread moist of even aquatic habitats in the Albian
- Cenomanian and Campanian - Maastrichtian. A shift towards drier cond
itions occurred in the late Cenomanian - Turonian. Throughout the Cret
aceous, however, there may have been extensive arid/semiarid areas of
non-deposition and seasonally dry periods. Some characteristics of the
local palynofloras are attributed to its inner continental position.
Rare Albian - Cenomanian and Campanian - Maastrichtian dinoflagellates
could be interpreted as lacustrine phytoplankton rather than as evide
nce for marine influence.