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Re: Silesaurus and Trialestes
_Trialestes romeri_ (Reig, 1963 )
(= _Triassolestes romeri_ Reig, 1963; _Triassolestes_ preoccupied, Tillyard,
1918 [Odonata])
PVL 2561 (holotype): Partial skull lacking the skull roof and braincase,
portions of two forelimbs including a scapula, a humerus, a radius, ulnae, a
radiale and an ulnare, and several cervical and 16 caudal vertebrae. The
forelimb elements of the holotype were associated with the skull; but Reig
(1963) referred the forelimb to _Proterochampsa_ (a crocodylian, according
to Reig), because he believed the forelimb to display crocodylian characters
(elongate carpals), and the partial skull did not. However, the forelimb
was referred back to _Trialestes_ when it was realized that _Proterochampsa_
is not a crocodylomorph (Bonaparte, 1972).
PVL 2559 (referred; Reig, 1963): Partial articulated pes. Clark et al.
(2000) believe this represents the same animal as the holotype.
PVL 3889: (referred; Bonaparte, 1978): Partial postcranium, including
forelimb elements (not the carpus) most of the pelvis and hindlimb, and
several vertebrae.
All specimens come from the Ischigualasto Formation (Late Triassic; Carnian)
of northwestern Argentina.
PVL 3889 exhibits features considered diagnostic for dinosaurs: perforated
acetabulum with a well-developed supraacetabular crest; inturned femoral
head that is more distinct than that in sphenosuchians; mesotarsal ankle
joint; functionally tridactyl pes (Clark et al., 2000).
Says Clark et al. (2000): "Although the forelimbs of both specimens
[holotype and PVL 3889] are very similar, nearly all of their similarities
can be interpreted as plesiomorphic character-states or features that are
found in both crocodylomorphs and basal dinosaurs." The authors note the
"striking" length of the forearm (radius+ulna) relative to the humerus
(~1.15 times). The same ratio in _Silesaurus_ is ~1.1, but no measurements
are given for the putative carpals (Dzik, 2003).
Clark et al. (2000) propose two taxonomic dispositions for the _Trialestes_
material: (1) the material represent a single taxon that combines
dinosaurian and crocodylomorph characteristics; or (2) the specimens
represent two different taxa, one a basal crocodylomorph (PVL 2561) and the
other a basal dinosaur (PVL 3889), but both sharing the same forelimb
proportions. Jaime alluded to a third possibility: (3) the holotype is a
chimera, composed of crocodylomorph and dinosaurian elements. (This reminds
me of what has been claimed by some authors for _Procompsognathus_ - part
crocodylomorph, part dinosaur. I don't know if this idea is still current
for _Procompsognathus_.)
Tim
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