High-resolution dinoflagellate cyst biostratigraphy of the Santonian-basalCampanian (Upper Cretaceous): new data from Whitecliff, Isle of Wight, England
Im. Prince et al., High-resolution dinoflagellate cyst biostratigraphy of the Santonian-basalCampanian (Upper Cretaceous): new data from Whitecliff, Isle of Wight, England, REV PALAE P, 105(3-4), 1999, pp. 143
Results are presented of a high-resolution study of dinoflagellate cysts fr
om part of the Upper Chalk succession on the Isle of Wight, southern Englan
d. The section was logged in detail, and stage and zonal boundaries were lo
cated using macrofossil data. Lower and middle Santonian samples are domina
ted by species of Senoniasphaera, Canningia, Circulodinium and Heterosphaer
idium. Major changes in the dinocyst assemblages coincide with the base of
the upper Santonian Uintacrinus socialis crinoid Zone, with an increase in
abundance and diversity, and a shift to assemblages dominated by Spiniferit
es spp. and Palaeohystrichophora infusorioides Deflandre. Our palynological
records (114 dinocyst, 4 acritarch species) provide the basis for a new ev
ent stratigraphy. Cyclonephelium filoreticulatum (Slimani) Prince, Jarvis e
t Tocher, comb. nov. temporarily disappears and an acme of Heterosphaeridiu
m? heteracanthum (Deflandre et Cookson) Eisenack et Kjellstrom occur in the
lower Santonian. The total range of Renidinium rigidum Prince, Jarvis et T
ocher, sp. nov. and the FAD of Senoniasphaera protrusa Clarke et Verdier em
end. lie within the middle Santonian. Raetiaedinium truncigerum (Deflandre)
Kirsch and Pervosphaeridium monasteriense Yun first appear, and Hystrichos
trogylon membraniphorum Agelopoulos reappears around the base of the upper
Santonian. The FADs of Pervosphaeridium intervelum Kirsch and Thalassiphora
? spinosa (Clarke et Verdier) Foucher, and the reappearance datums (RADs) o
f Chlamydophorella nyei Cookson et Eisenack, Subtilisphaera pontis-mariae (
Deflandre) Lentin et Williams and Membranilarnacia polycladiata Cookson et
Eisenack occur in the upper Santonian. No major changes in dinocyst assembl
ages occur at the Santonian/Campanian boundary, but a sequence of LADs occu
r in the basal lower Campanian, in the order: Xenascus perforatus (Vozzhenn
ikova) Yun; Spinidinium echinoideum (Cookson et Eisenack) Lentin et William
s; Surculosphaeridium? longifurcatum (Firtion), Davey et al.; Raetiaedinium
truncigerum (Deflandre) Kirsch and S. protrusa; Florentinia ferox (Defland
re) Duxbury; Acanthaulax wilsonii Yun and T.? spinosa, The range of Endoscr
inium campanula (Gocht) Vozzhennikova extends into the upper Santonian. Add
itional taxonomic proposals are: Senoniasphaera Clarke emend.; S rotundata
Clarke et Verdier emend,; Circulodinium latoaculeus (Yun) Prince, Jarvis et
Tocher, comb, nov. (C) 1999 Elsevier Science B.V. All rights reserved.