A. Sanfilippo et Jp. Caulet, TAXONOMY AND EVOLUTION OF PALEOGENE ANTARCTIC AND TROPICAL LOPHOCYRTID RADIOLARIANS, Micropaleontology, 44(1), 1998, pp. 1-42
Investigation of three-segmented theoperids through successive stratig
raphic levels in Antarctic Paleogene sediment sequences, and a tropica
l reference section, resulted in recognition of four groups characteri
zed by different cephalic structures taxonomically treated as the new
genera, Aphetocyrtis and Clinorhabdus, the new subgenus Lophocyrtis (A
poplanius), and the previously described subgenus Lophocyrtis (Lophocy
rtis). All four lineages are represented in Middle Eocene sediments fr
om the Antarctic. The Antarctic representatives of the tropical Lophoc
yrtis (Lophocyrtis) lineage become extinct at the end of the Middle Eo
cene. The diversity of the two new genera, restricted to the Antarctic
, is at a peak in the Oligocene interval, coincident with the major co
oling event reported during this interval. Most of the new species are
endemic to the Antarctic, and only three have been sporadically found
in rare abundance in tropical areas. One geographic invasion from the
tropics to the Antarctic is documented. The following ten new taxa ar
e described: Aphetocyrtis gnomabax, A., catalexis, A. rossi, Lophocyrt
is (Apoplanius) nomas, L. (A.) keraspera, L. (A.) klydus, Lophocyrtis
(Lophocyrtis) jacchia; hapsis, Lophocyrtis (Lophocyrtis ?) zeira, Clin
orhabdus anantomus and C. ocymora. Species whose definitions have been
emended herein are: Lophocyrtis (Apoplanius) aspera, Lophocyrtis (Lop
hocyrtis) jacchia jacchia, L. (L. ?) barbadense, L. (L. ?) semipolita,
Clinorhabdus longithorax and C. robusta.