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New papers: Kentrosaurus lectotype and dino tracks
From: Ben Creisler
bh480@scn.org
In case these recent papers have not been mentioned yet:
Mallison, Heinrich (2011)
The real lectotype of Kentrosaurus aethiopicus Hennig,
1915.
Neues Jahrbuch für Geologie und Paläontologie -
Abhandlungen 259 (2): 197-206 (February 2011)
DOI: 10.1127/0077-7749/2011/0114
http://www.ingentaconnect.com/content/schweiz/njbgeol/2011
/00000259/00000002/art00004
A detailed study of the relevant literature reveals that
contra recent use the lectotype of the stegosaur
Kentrosaurus aethiopicus Hennig, 1915 is a partial
individual from excavation 'St' at Kindope, Tendaguru,
Tanzania in the collection of the Museum für Naturkunde
Berlin (MB. R.4800.1-37). This significantly influences
the diagnosis of the taxon, defining several characters
based on the lectotype instead of referred specimens,
notably the sub-vertical neural spines of the medial
third of the tail, and the hook-shaped, anteriorly
inclined neural spines in the posterior caudals.
===
P. L. Falkingham, K. T. Bates, L. Margetts and P. L.
Manning (2011)
The ?Goldilocks? effect: preservation bias in vertebrate
track assemblages.
Journal of the Royal Society Interface (advance online
publication)
doi: 10.1098/​rsif.2010.0634
FREE PDF at:
http://rsif.royalsocietypublishing.org/content/early/2011/
01/12/rsif.2010.0634.abstract
Finite-element analysis was used to investigate the
extent of bias in the ichnological fossil record
attributable to body mass. Virtual tracks were simulated
for four dinosaur taxa of different sizes (Struthiomimus,
Tyrannosaurus, Brachiosaurus and Edmontosaurus), in a
range of substrate conditions. Outlines of autopodia were
generated based upon osteology and published soft-tissue
reconstructions. Loads were applied vertically to the
feet equivalent to the weight of the animal, and
distributed accordingly to fore- and hindlimbs where
relevant. Ideal, semi-infinite elastic?plastic substrates
displayed a ?Goldilocks? quality where only a narrow
range of loads could produce tracks, given that small
animals failed to indent the substrate, and larger
animals would be unable to traverse the area without
becoming mired. If a firm subsurface layer is assumed, a
more complete assemblage is possible, though there is a
strong bias towards larger, heavier animals. The depths
of fossil tracks within an assemblage may indicate
thicknesses of mechanically distinct substrate layers at
the time of track formation, even when the lithified
strata appear compositionally homogeneous. This work
increases the effectiveness of using vertebrate tracks as
palaeoenvironmental indicators in terms of inferring
substrate conditions at the time of track formation.
Additionally, simulated undertracks are examined, and it
is shown that complex deformation beneath the foot may
not be indicative of limb kinematics as has been
previously interpreted, but instead ridges and
undulations at the base of a track may be a function of
sediment displacement vectors and pedal morphology.
====
Also of interest:
For French readers, there are news story about a new
theropod found in Aix-en-Provence (a region famous for
fossil dino eggs) in southern France. It's not been named
yet, but it's based on part of a skull, described as up
to 6 meters long in total length, and about 70 million
years old.
http://www.citylocalnews.com/aix/2011/02/01/un-nouveau-
dino-decouvert
http://www.maxisciences.com/dinosaure/une-nouvelle-espece-
de-dinosaure-decouverte-a-aix-en-provence_art12277.html