NEW SPECIES OF THE GENUS PARKIELLA (FORAMINIFERA) FROM THE LATE CRETACEOUS CENTRAL PACIFIC-OCEAN - BIOSTRATIGRAPHY, BIOGEOGRAPHY, AND THE CRETACEOUS-PALEOGENE BOUNDARY
Jgv. Widmark et M. Kucera, NEW SPECIES OF THE GENUS PARKIELLA (FORAMINIFERA) FROM THE LATE CRETACEOUS CENTRAL PACIFIC-OCEAN - BIOSTRATIGRAPHY, BIOGEOGRAPHY, AND THE CRETACEOUS-PALEOGENE BOUNDARY, Journal of micropalaeontology, 17, 1998, pp. 51-60
Two new species, Parkiella angulocamerata sp. nov. and P. globocamerat
a sp. nov., are described from the Late Cretaceous (late Maastrichtian
) Central Pacific Ocean, DSDP Sites 465 and 171. Examination under the
SEM revealed apertural features that were not documented in the origi
nal description of Parkiella. An 'L'-shaped aperture was originally co
nsidered as a diagnostic character of Parkiella; we suggest that this
is a preservational artefact and question its diagnostic value. The ex
istence of internal toothplates determine both Parkiella described her
e as members of the family Turrilinidae Cushman 1927. Both species wer
e found to be endemic to the tropical Pacific Ocean. They occurred in
sequence throughout the Maastrichtian section at Site 465 with a minim
um (one sample) stratigraphic overlap. Parkiella globocamerata is one
of the few deep-sea benthic foraminiferal species that indeed became e
xtinct at the Cretaceous/Palaeogene (K/Pg) boundary. However, we docum
ent a decrease in both relative abundance and accumulation rate of the
species already prior to the K/Pg transition. We propose that the int
erval between the LO (Last Occurrence) of P. angulocamerata ara and th
e LO of P. globocamerata nra is indicative of uppermost Cretaceous (Mi
cula prinsii Zone) strata in the tropical Pacific.