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New Mesozoic vertebrate articles
From: Ben Creisler bh480@scn.org
New Mesozoic vertebrate articles
Here are some new and not so new articles (new to me at
least) about Mesozoic vertebrates that I don't recall
seeing mentioned on the list.
Note that the first one is only available online and has
not appeared in print in official form. Some other papers
erect new non-dinosaur taxa.
Paton, Haddrath and Baker (2002 online). Complete
mitochondrial DNA genome sequences show that modern birds
are not descended from transitional shorebirds.
Proceedings of the Royal Society: Biological Sciences
(online)
Abstract: To test the hypothesis put forward by
Feduccia of the origin of modern birds from transitional
birds, we sequenced the first two complete mitochondrial
genomes of shorebirds (ruddy turnstone and blackish
oystercatcher) and compared their sequences with those of
already published avian genomes. When corrected for rate
heterogeneity across sites and non-homogeneous nucleotide
compositions among lineages in maximum likelihood (ML),
the optimal tree places palaeognath birds as sister to the
neognaths including shorebirds. This optimal topology is a
re-rooting of recently published ordinal-level avian trees
derived from mitochondrial sequences. Using a penalized
likelihood (PL) rate-smoothing process in conjunction with
dates estimated from fossils, we show that the basal
splits in the bird tree are much older than the Cretaceous-
Tertiary (K-T) boundary, reinforcing previous molecular
studies that rejected the derivation of modern birds from
transitional shorebirds. Our mean estimate for the origin
of modern birds at about 123 million years ago (Myr ago)
is quite close to recent estimates using both nuclear and
mitochondrial genes, and supports theories of continental
break-up as a driving force in avian diversification. Not
only did many modern orders of birds originate well before
the K-T boundary, but the radiation of major clades
occurred over an extended period of at least 40Myr ago,
thus also falsifying Feduccia's rapid radiation scenario
following a K-T bottleneck.
van Dijk, D. Eduard, 2001. Jurassic bipeds that could hop?
Perch? Pounce? Fly? South African Journal of Science.
September-
October, 2001; 97 (9-10): 373-374.
AB: THE DESCRIPTION OF THE ICHNOGENUS Molapopentapodiscus
(Ellenberger, 1970) includes the presumption that forward
progression was by bounding with feet together. That this
genus, and other genera based on footprints or trackways,
were hoppers, has been disputed. Material from KwaZulu-
Natal, South Africa, suggests that more than one Lower
Jurassic biped was a hopper, but with feet adapted also to
other functions.
O'Keefe, Frank Robin, 2001. A cladistic analysis and
taxonomic revision of the Plesiosauria (Reptilia:
Sauropterygia). Acta Zoologica Fennica 213:1-63.
The Plesiosauria (Reptilia: Sauropterygia) is a group of
Mesozoic marine reptiles known from abundant material,
with specimens described from all continents. The group
originated very near the Triassic-Jurassic boundary and
persisted to the end-Cretaceous mass extinction. This
study describes the results of a specimen-based cladistic
study of the Plesiosauria, based on examination of 34 taxa
scored for 166 morphological characters. The Pliosauroidea
is found to by polyphyletic due to the inclusion of the
Polycotylidae; this second clade is instead a member of
the Plesiosauroidea, and thus more closely related to
elasmosaurs than to other `pliosaurs'. Characters of body
proportion such as neck length and head size are very
labile, with the `pliosauromorph' body plan evolving three
times, while extremely long necks evolved in two clades.
Characters from the entire skeleton support these
relationships, although characters of the skull roof and
palate are especially useful. Lastly, a new genus and
species, Hauffiosaurus zanoni, is named based on German
material of Toarcian age.
O'Keefe, Frank Robin. 2002. The evolution of plesiosaur
and pliosaur morphotypes in the Plesiosauria (Reptilia:
Sauropterygia). Paleobiology: Vol. 28, No. 1, pp. 101-112.
ABSTRACT
The dichotomy between short-necked, large-
headed ?pliosaurs? and long-necked, small-
headed ?plesiosaurs? has formed the basis of plesiosaur
taxonomy for over one hundred years. Recent work has cast
doubt on the taxonomic validity of this dichotomy,
suggesting that the pliosaur morphotype may have evolved
independently in more than one clade. This paper
quantifies the variation in body proportion in the clade
Plesiosauria using principal component analysis and
demonstrates that the traditional plesiosaur/pliosaur
dichotomy is an oversimplified view of the range of
morphologies present in the group. The topology of the
clade is mapped into the morphospace, demonstrating that
the pliosaur morphotype evolved three times from two
different regions of morphospace. Both the range of body
morphologies displayed by plesiosaurs and the evolutionary
history of those morphologies, are more complex than
previously supposed.
Wilson, Jeffrey A., Malkani, M. Sadiq, Gingerich, Philip
D., 2001. New crocodyliform (Reptilia, Mesoeucrocodylia)
from the upper Cretaceous Pab Formation of Vitakri,
Balochistan (Pakistan).
Contributions from the Museum of Paleontology
University of Michigan. December 31, 2001; 30 (12): 321-
336.
AB: Fossil remains from the upper part of the Pab
Formation in eastern Balochistan, Pakistan, provide the
first diagnostic remains of a Cretaceous crocodyliform
from the Indian subcontinent, and provide important
information for assessing its biogeographic history.
Specimens collected to date include the well preserved
rostrum of a new genus and species, Pabwehshi
pakistanensis. The rostrum has a foreshortened anterior
snout, with serrated teeth that interlock to form a zig-
zag cutting edge. The anterolaterally directed external
nares are bordered ventrally and laterally by a well-
marked narial fossa. Comparisons with crocodyliforms of
equivalent age indicate that Pabwehshi is a baurusuchid
mesoeucrocodylian related to Baurusuchus from Brazil and
Cynodontosuchus from Argentina. Pabwehshi is the first
baurusuchid known outside South America. It provides
further evidence of a Cretaceous biogeographic link
between South America and Indo-Pakistan.
Hungerbuehler, A., 2002. The Late Triassic Phytosaur
Mystriosuchus Westphali, With A Revision of the Genus.
Palaeontology 45 (2): 377-418. (March 2002).
Abstract:
Mystriosuchus westphali is based on a large, well-
preserved cranium and a snout fragment from the
Stubensandstein (Norian) of south-west Germany. The
hypodigm is redescribed and new or poorly known cranial
structures in phytosaurs are discussed. For the first
time, the presence of a premaxillary crest is
substantiated in a phytosaur. The type specimen shows a
supernumerary occipital element (=?tabular?) that is
probably fused to the parietal in other phytosaurs, and an
orbitosphenoid. A computerised parsimony analysis confirms
the hypothesis that Mystriosuchus is nested within
Pseudopalatinae, the most derived clade of phytosaurs, and
thus does not fall within basal phytosaurs. Mystriosuchus
is characterised by five unique features (slit-like
interpremaxillary fossa, triangular cross-section of the
postorbito-squamosal bar, strongly reduced posttemporal
fenestra, and two features of the cranial sculpture), plus
eight synapomorphies that also occur in some more
distantly related taxa. Mystriosuchus westphali is
diagnosed by, among other apomorphies, a distinct
premaxillary crest, a squamosal-proo¨tic contact, absence
of a posterior process of the squamosal, and a slit-like
posttemporal fenestra. The type species Mystriosuchus
planirostris shows, most significantly, the naris facing
forward anteriorly and upward posteriorly, and the longest
rostrum and the highest degree of depression of the
supratemporal opening in any phytosaur. Mystriosuchus
exemplifies a common pattern in phytosaurids in being a
genus that includes a gracile, elongated, slender-snouted
and a more robust species with a broader, often crested
snout. This study demonstrates that a detailed analysis of
the cranial anatomy and the rigorous application of
cladistic principles to identified character states help
to clarify current inconsistencies in the taxonomy and
nomenclature of phytosaurs.
Li Chun & O. Rieppel, 2002. A new cyamodontoid placodont
from Triassic of Guizhou, China. Chinese Science Bulletin.
47(5): 403-407.
Abstract A new cyamodontoid placodont is named
(Psephochelys polyosteoderma gen. et. sp. nov.) and
described based on a three-dimensionally preserved
specimen. The material comes from the Wayao Member of the
Falang Formation (Carnian, Late Triassic) in Guizhou
Province, southwestern China. The skull of Psephochelys
shows a unique combination of characteristics observed in
Psephoderma and Placochelys, and the carapace is
diagnostic of a new taxon as well. The ventral dermal
armor of Psephochelys differs from all other known
cyamodontoids in that it comprises irregular marginal
osteoderms in loose contact with each other, and gastralia
between them. The cranial suture pattern is in part
difficult to analyze due to apparent co-ossification of
elements, or poor delimitation of sutures. This affects
primarily the demarcation of the nasal from the
prefrontal, and the relation between the anterior part of
the parietal, posterior ends of the frontals, and
postfrontals. However, the postfrontal appears to enter
the anteromedial margin of the upper temporal fenestra, a
characteristic otherwise known from Placodus, but not from
other cyamodontoids. However, given the difficulties of
interpretation of this skull, additional material is
required to unequivocally assess some details of the
pattern of cranial sutures.
Maisch M.W., 2002. A New Basal Lystrosaurid Dicynodont
from the Upper Permian of South Africa. Palaeontology 45
(2):343-359
Abstract:
A new genus and species of late Permian dicynodont,
Kwazulusaurus shakai, is described on the basis of a
complete skull from the late Permian Dicynodon Assemblage
Zone of the South African Beaufort Group. It is an
advanced form which shows characters, such as the shape of
the snout and the loss of the ectopterygoid, that link it
to the early Triassic genus Lystrosaurus. Kwazulusaurus
represents the most basal member of the lystrosaurian
lineage. The phylogeny of progressive pristerodontian
dicynodonts is discussed. It appears possible that the
Kannemeyeriiformes and Lystrosauridae do not form a
monophylum, as previously assumed. Instead a sister-group
relationship between lystrosaurids and dicynodontids plus
kannemeyeriiforms is suggested.