Abstract. Species of the fusiform peridiniacean dinoflagellate cyst
genera Svalbardella Manum, 1960, emend. (Eocene–Oligocene) and Palaeocystodinium Alberti, 1961
(Late Cretaceous–Miocene), have been examined from the high to middle
latitudes of the Northern Hemisphere: Spitsbergen, Norwegian-Greenland Sea,
Labrador Sea, western North Atlantic, and the North Sea basin. The genus
Svalbardella is emended to comprise species with smooth or finely ornamented surfaces
and for which one or both horns are bluntly rounded. Svalbardella clausii sp. nov. has a narrow
range restricted to the lowermost Chattian (close to the NP24–NP25 boundary
and within Chron C9n), and it therefore appears a useful stratigraphical
marker. This species has a wide distribution across the North Atlantic,
having been reported from the North Sea basin, western North Atlantic, and
the Labrador Sea. Svalbardella clausii sp. nov. overlaps stratigraphically with the reoccurrence
interval of Svalbardella cooksoniae Manum, 1960, and spans the Oi-2b cooling maximum. Its presence
may therefore be related to the establishment of cooler surface waters at
this time. Svalbardella kareniae sp. nov. has a discordant occurrence: Lower Oligocene and Lower
Miocene of the Norwegian Sea at Deep Sea Drilling Project Site 338 and Ocean
Drilling Program Site 643, respectively, and mid-Oligocene of the North Sea.
Its distribution suggests that Svalbardella kareniae sp. nov. favours more open marine
conditions. Palaeocystodinium obesum Fensome et al., 2009, described from offshore eastern Canada
where it has a highest occurrence in the Lower Oligocene, is emended to
include specimens with a finely ornamented periphragm and traces of
tabulation in addition to the archeopyle.