Stratigraphic occurrence of selected marine palynomorph species recorder in the Paleogene of ODP Hole 105-647A (Table 3) ...

• Main Authors: Head, Martin J, Norris, Geoffrey
• Format: Dataset
• Language: English
• Published: PANGAEA 1989
• Subjects: Sample code/label; Epoch; Nannofossil zone; Adnatosphaeridium robustum; Dinoflagellate cyst; Rhombodinium sp.; Operculodinium sp.; Hystrichostrogylon membraniphorum; Cribroperidinium giuseppei; Impagidinium spp.; Systematophora ancyrea; Thalassiphora pelagica; Palaeocystodinium golzowense; Spiniferites spp.; Dracodinium sp.; Dracodinium condylos; Ceratiopsis sp.; Cordosphaeridium gracilis; Spiniferites pseudofurcatus; Corrudinium sp.; Impagidinium sp.; Impagidinium dispertitum; Lingulodinium machaerophorum; Operculodinium spp.; Areoligera senonensis; Eatonicysta ursulae; Nematosphaeropsis sp.; Apectodinium sp.; Membranophoridium sp.; Wetzeliella articulata; Diphyes colligerum; Homotryblium sp.; Hystrichokolpoma globulum; Deflandrea sp.; Cordosphaeridium inodes; Phthanoperidinium sp.; Kisselovia crassoramosa; Kisselovia coleothrypta; Rhombodinium glabrum; Heteraulacacysta sp.; Systematophora sp.; Hystrichokolpoma unispina; Dinopterygium cladoides; Adnatosphaeridium multispinosum; Kisselovia edwardsii; Tectatodinium sp.; Samlandia chlamydophora; Impagidinium pallidum; Homotryblium tenuispinosum; Lithosphaeridium sp.; Rockall Plateau; Labrador Sea
• Online Access: https://dx.doi.org/10.1594/pangaea.745253; https://doi.pangaea.de/10.1594/PANGAEA.745253

Dinoflagellate cysts were recovered throughout the Paleogene succession of Hole 647A, which contains an almost complete deep-water record of early Eocene through early late Oligocene sedimentation in the Labrador Sea. Dinoflagellate cyst biostratigraphy is in general accord with that provided by other microfossil groups and is consistent with a lower Eocene age, as determined by nannofossils, for basal sediments in Hole 647A. These sediments overlie oceanic crust of Chron 24 age.Dinocyst assemblages indicate outer neritic to oceanic conditions throughout, although the persistent occurrence of Wetzeliellaceae specimens in the lower Eocene suggests a greater influence from shelf environments during this time. Lower Eocene dinocyst assemblages are similar to coeval assemblages from the Rockall Plateau, but those from the middle to upper Eocene have mixed affinities and may be related to the intensification of the proto-Gulf Stream from middle Eocene time. Oligocene dinocyst assemblages suggest the influence of ... : species abundance: A = abundant, C = common, R = rare, - = not observed, cf. = confer ...