15 research outputs found
Application du microscope électronique à balayage (MEB) à la paléontologie et à la sédimentologie
Associations palynologiques définies dans le Trias languedocien (France) : Interprétation stratigraphique.
Morphological diversity of the exine sculpture of some Frasnian spores from the northern Timan: Applications for taxonomy and significance for spore dispersal
Palynology of the Monterey formation (Miocene) phosphatic facies at Lions head, Santa Maria area, California
Organic-rich sedimentation at the Cenomanian-Turonian boundary in oceanic and coastal basins in the North Atlantic and Tethys
New Hettangian tracks from the Causses Basin (LozĂšre, southern France) complement the poor fossil record of earliest Jurassic crocodylomorphs in Europe
The palynostratigraphy of the Upper Maiolica, Selli Level and the Lower Marne a Fucoidi units in the proposed Barremian/Aptian (Lower Cretaceous) GSSP stratotype at Gorgo a Cerbara, UmbriaâMarche Basin, Italy
Megaspores from the Lower Jurassic (Pliensbachian) Rotzo Formation (Monti Lessini, northern Italy) and their palaeoenvironmental implications
Coastal sediments from the Algarve: low-latitude climate archive for the Aptian-Albian
The Late Aptian to Early Albian transition has
previously been identified as a possible example of substantial
climate cooling within the mid-Cretaceous greenhouse
period. To study the response of continental
weathering and terrestrial vegetation to this cooling episode
at low- to mid-latitudes, marine nearshore deposits
from the Algarve Basin (SW Portugal) have been investigated
with a combined approach including palynology,
clay mineralogy and bulk-rock geochemistry. In the Lower
Aptian part of the succession, quartz-rich sandstone facies
is accompanied by high abundances of early diagenetic
kaolinite, which is interpreted to reflect episodes of enhanced
humidity and high meteoric flow-through. In contrast,
the Late Aptian to Early Albian deposits are
characterized by high abundances of detrital clay minerals
(mica and chlorite) indicating the dominance of physical
weathering processes in the source area, most probably
related to low precipitation rates in conjunction with tectonically
enhanced erosion. Palynological data show a
strong dominance of Classopollis pollen associated with
low pteridophyte spore abundances, suggesting warm
semi-arid to arid palaeoenvironments. Changes in sedimentation
patterns from varicoloured lagoonal marls to
thick-bedded shallow-water carbonates are neither expressed
in the spore-pollen assemblages nor in the distributions
of clay minerals which both remain essentially
stable throughout the Late Aptian to Early Albian. These
relatively stable patterns are in contrast with various lines
of evidence, predominantly from high-latitude areas, that
suggest a significant cooling during this time interval. Our
study demonstrates that terrestrial environments of low- to
mid-latitude regions were not significantly affected by the
Late Aptian - Early Albian ââcold snapââ