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New Diplodocoidea phylogenetic analysis
From: Ben Creisler
bh480@scn.org
In case this advance online publication has not been
mentioned:
WHITLOCK, J. A. (2011)
A phylogenetic analysis of Diplodocoidea (Saurischia:
Sauropoda).
Zoological Journal of the Linnean Society (advance online
publication)
doi: 10.1111/j.1096-3642.2010.00665.x
http://onlinelibrary.wiley.com/doi/10.1111/j.1096-
3642.2010.00665.x/abstract
Diplodocoidea includes some of the first well-known
sauropod dinosaurs, including such late 19th century and
early 20th century discoveries as Apatosaurus,
Diplodocus, and Dicraeosaurus. As a consequence of their
long history of study, the basic set of suprageneric
diplodocoid interrelationships is well resolved, and the
diagnostic features of each genus are well established.
However, intergeneric relationships are less resolved,
including the relationships of putatively basal taxa like
Amphicoelias and Haplocanthosaurus, the flagellicaudatan
Suuwassea, and the highly specialized rebbachisaurids.
For the rebbachisaurids, this uncertainty is coupled with
a recent surge in the discovery of new taxa. Comparative
cladistic methods demonstrate that character and taxon
sampling need to be improved before greater phylogenetic
resolution can be expected. Here, I present a new
phylogenetic analysis that resolves many of the
outstanding questions regarding the relationships within
Diplodocoidea and examines palaeobiogeographical trends
within the group. Suuwassea is recovered as a basal
dicraeosaurid (the only Laurasian member of the group),
and two distinct clades of rebbachisaurids are
identified: a group closely allied with Nigersaurus and a
clade associated with Limaysaurus. Amphicoelias,
Amazonsaurus, and Haplocanthosaurus are provisionally
placed as successively less-derived taxa at the base of
Diplodocoidea. A North American origin for Diplodocoidea
and Flagellicaudata is hypothesized based on the
geographical and temporal distribution of those taxa.
Rebbachisaurid taxa demonstrate a South American/African
vicariance pattern, but the timing of the event pre-dates
the proposed final rifting of those continents by c. 40
million years; the meaning of this discrepancy is
uncertain.