[Date Prev][Date Next][Thread Prev][Thread Next][Date Index][Thread Index][Subject Index][Author Index]
Ornithopod teeth from Alaska
From: Ben Creisler
bh480@scn.org
A new online paper:
Caleb Marshall Brown and Patrick Druckenmiller (2011)
Basal ornithopod (Dinosauria: Ornithischia) teeth from
the Prince Creek Formation (early Maastrichtian) of
Alaska.
Canadian Journal of Earth Sciences (advance online
publication)
doi:10.1139/e11-017
http://www.nrcresearchpress.com/doi/abs/10.1139/e11-017
Abstract
A diverse and prolific record of polar dinosaurs comes
from the Upper Cretaceous (Campanian?Maastrichtian)
sediments of the Prince Creek Formation exposed on
Alaska?s North Slope. Previous assignment of basal
ornithopod material from this formation has been based
solely on teeth, which have either been referred
to "hypsilophodontid" indet. or Thescelosaurus sp. Here,
we re-examine this material and describe several new
specimens, including five isolated premaxillary teeth and
three cheek teeth. The premaxillary teeth are most
similar to those of Thescelosaurus, whereas the cheek
teeth are more similar to its sister taxon Parksosaurus,
for which premaxillary teeth are unknown. Referral of
this new material to Thescelosaurus would represent the
oldest occurrence of this taxon and considerably extend
its stratigraphic range. A more likely possibility is
that the premaxillary teeth are referable to
Parksosaurus, an interpretation that is more parsimonious
from a stratigraphic perspective. Intriguingly, one cheek
tooth previously referred to as "hypsilophodontid" cannot
be referred to either Thescelosaurus or Parksosaurus.
Previously, faunal comparisons of the Prince Creek
Formation have largely been made with non-contemporaneous
formations, including the Campanian-aged Judith River and
Aguja formations, or to the latest Maastrichtian Hell
Creek Formation. On the basis of age and faunal
similarities, a more appropriate comparison should be
made with coeval rocks of the Horseshoe Canyon. This
study expands our knowledge of Cretaceous ornithischian
diversity at polar paleolatitudes and underscores the
importance of small, rare, or easily misidentified
fossils in paleoecological studies.
----------------