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        <rdf:li rdf:resource="http://comments.gmane.org/gmane.science.dinosaurs.general/54854"/>
        <rdf:li rdf:resource="http://comments.gmane.org/gmane.science.dinosaurs.general/54853"/>
        <rdf:li rdf:resource="http://comments.gmane.org/gmane.science.dinosaurs.general/54852"/>
        <rdf:li rdf:resource="http://comments.gmane.org/gmane.science.dinosaurs.general/54845"/>
        <rdf:li rdf:resource="http://comments.gmane.org/gmane.science.dinosaurs.general/54831"/>
        <rdf:li rdf:resource="http://comments.gmane.org/gmane.science.dinosaurs.general/54810"/>
        <rdf:li rdf:resource="http://comments.gmane.org/gmane.science.dinosaurs.general/54794"/>
        <rdf:li rdf:resource="http://comments.gmane.org/gmane.science.dinosaurs.general/54789"/>
        <rdf:li rdf:resource="http://comments.gmane.org/gmane.science.dinosaurs.general/54786"/>
        <rdf:li rdf:resource="http://comments.gmane.org/gmane.science.dinosaurs.general/54785"/>
        <rdf:li rdf:resource="http://comments.gmane.org/gmane.science.dinosaurs.general/54783"/>
        <rdf:li rdf:resource="http://comments.gmane.org/gmane.science.dinosaurs.general/54780"/>
        <rdf:li rdf:resource="http://comments.gmane.org/gmane.science.dinosaurs.general/54775"/>
        <rdf:li rdf:resource="http://comments.gmane.org/gmane.science.dinosaurs.general/54774"/>
        <rdf:li rdf:resource="http://comments.gmane.org/gmane.science.dinosaurs.general/54767"/>
        <rdf:li rdf:resource="http://comments.gmane.org/gmane.science.dinosaurs.general/54761"/>
        <rdf:li rdf:resource="http://comments.gmane.org/gmane.science.dinosaurs.general/54753"/>
        <rdf:li rdf:resource="http://comments.gmane.org/gmane.science.dinosaurs.general/54752"/>
        <rdf:li rdf:resource="http://comments.gmane.org/gmane.science.dinosaurs.general/54749"/>
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    <title>Gmane</title>
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    <link>http://gmane.org</link>
  </image>
  <item rdf:about="http://comments.gmane.org/gmane.science.dinosaurs.general/54854">
    <title>Tetrapods from Permo-Triassic boundary in Russia</title>
    <link>http://comments.gmane.org/gmane.science.dinosaurs.general/54854</link>
    <description>&lt;pre&gt;From: Ben Creisler
bcreisler&amp;lt; at &amp;gt;gmail.com


A new paper in Paleontological Journal:

A. G. Sennikov and V. K. Golubev (2012)
On the faunal verification of the Permo-Triassic boundary in
continental deposits of eastern Europe: 1. Gorokhovets-Zhukov ravine.
Paleontological Journal 46(3): 313-323
DOI: 10.1134/S003103011203015X
http://www.springerlink.com/content/ug2835240107184u/

A reference section of the Permian and Triassic continental deposits
of the Zhukov ravine near the town of Gorokhovets (Vladimir Region) is
described and new tetrapod localities are characterized. The position
of the Permian-Triassic boundary in this section is recognized and its
faunal substantiation based on vertebrates is provided for the first
time. The Zhukov ravine section is unique in the fact that it shows a
thick stratigraphically continuous succession of the Permo-Triassic
boundary beds, with three successive tetrapod zones: the terminal
Permian Chroniosuchus paradoxus and Archosaurus rossicus zones and the
Early Triassic Tupil&lt;/pre&gt;</description>
    <dc:creator>Ben Creisler</dc:creator>
    <dc:date>2012-05-26T15:45:30</dc:date>
  </item>
  <item rdf:about="http://comments.gmane.org/gmane.science.dinosaurs.general/54853">
    <title>Andalgalornis (phorusrhacid "terror bird") neck flexibility</title>
    <link>http://comments.gmane.org/gmane.science.dinosaurs.general/54853</link>
    <description>&lt;pre&gt;From: Ben Creisler
bcreisler&amp;lt; at &amp;gt;gmail.com

New in PLoS ONE:

Claudia P. Tambussi, Ricardo de Mendoza, Federico J. Degrange &amp;amp;
Mariana B. Picasso (2012)
Flexibility along the Neck of the Neogene Terror Bird Andalgalornis
steulleti (Aves Phorusrhacidae).
PLoS ONE 7(5): e37701.
doi:10.1371/journal.pone.00377
http://www.plosone.org/article/info%3Adoi%2F10.1371%2Fjournal.pone.0037701

Background

Andalgalornis steulleti from the upper Miocene–lower Pliocene (≈6
million years ago) of Argentina is a medium-sized patagornithine
phorusrhacid. It was a member of the predominantly South American
radiation of ‘terror birds’ (Phorusrhacidae) that were apex predators
throughout much of the Cenozoic. A previous biomechanical study
suggests that the skull would be prepared to make sudden movements in
the sagittal plane to subdue prey.

Methodology/Principal Findings

We analyze the flexion patterns of the neck of Andalgalornis based on
the neck vertebrae morphology and biometrics. The transitional
cervical vertebrae 5th&lt;/pre&gt;</description>
    <dc:creator>Ben Creisler</dc:creator>
    <dc:date>2012-05-26T04:56:34</dc:date>
  </item>
  <item rdf:about="http://comments.gmane.org/gmane.science.dinosaurs.general/54852">
    <title>Sauropod tracks impact on lagoon sandstone in Australia</title>
    <link>http://comments.gmane.org/gmane.science.dinosaurs.general/54852</link>
    <description>&lt;pre&gt;From: Ben Creisler
bcreisler&amp;lt; at &amp;gt;gmail.com

New in PLoS ONE:

Tony Thulborn (2012)
Impact of Sauropod Dinosaurs on Lagoonal Substrates in the Broome
Sandstone (Lower Cretaceous), Western Australia.
PLoS ONE 7(5): e36208.
doi:10.1371/journal.pone.0036208
http://www.plosone.org/article/info%3Adoi%2F10.1371%2Fjournal.pone.0036208



Existing knowledge of the tracks left by sauropod dinosaurs (loosely
‘brontosaurs’) is essentially two-dimensional, derived mainly from
footprints exposed on bedding planes, but examples in the Broome
Sandstone (Early Cretaceous) of Western Australia provide a
complementary three-dimensional picture showing the extent to which
walking sauropods could deform the ground beneath their feet. The
patterns of deformation created by sauropods traversing
thinly-stratified lagoonal deposits of the Broome Sandstone are
unprecedented in their extent and structural complexity. The stacks of
transmitted reliefs (underprints or ghost prints) beneath individual
footfalls are nested into a hierarch&lt;/pre&gt;</description>
    <dc:creator>Ben Creisler</dc:creator>
    <dc:date>2012-05-26T04:54:03</dc:date>
  </item>
  <item rdf:about="http://comments.gmane.org/gmane.science.dinosaurs.general/54845">
    <title>Microraptor hanqingi, new species from China.</title>
    <link>http://comments.gmane.org/gmane.science.dinosaurs.general/54845</link>
    <description>&lt;pre&gt; &amp;gt; Again, I actually like the idea - since you're the one who pointed it 
out here, I was hoping you had some suggestions for what we'd predict if 
tree-roosting was indeed important to paravians.

The idea was never advanced by me as a testable lifestyle for any 
particular fossil specimen -- that would be a "misunderstanding" -- but 
it falsifies the idea that an animal evolving flight in tree-down 
gliding-first mode will by evolutionary logic show "arboreal 
adaptations" in its skeleton -- beyond the basic capacity to climb a tree...

I suppose predictions made by tree-roosting might include 1) limited 
upstroke early on (that is, even after the appearance of a sophisticated 
gliding wing), 2) that the perching foot would appear subsequent to 
powered flight (full upstroke), not before -- and 3) the capability of 
climbing vertically.

One note -- controlled climbing up is easier than climbing down -- and 
in the hoatzin type wing-claw model, climbing down would appear to be 
problematic, which makes par&lt;/pre&gt;</description>
    <dc:creator>Don Ohmes</dc:creator>
    <dc:date>2012-05-25T22:45:55</dc:date>
  </item>
  <item rdf:about="http://comments.gmane.org/gmane.science.dinosaurs.general/54831">
    <title>Geometric Morphometrics courses</title>
    <link>http://comments.gmane.org/gmane.science.dinosaurs.general/54831</link>
    <description>&lt;pre&gt;Dear colleagues:

This e-mail is to inform you of some courses on Geometric Morphometrics, which may would be of your interest. I would appreciate if you could distribute this information between your colleagues:

"Introduction to Geometric Morphometrics". June 12-15, 2012. Instructors: Dr. Chris Klingenberg (University of Manchester, UK) and Dr. Jesús Marugán-Lobón (Universidad Autónoma de Madrid). Just 5 places left. More information at: http://www.transmittingscience.org/introduction_to_gm.htm

“3D Geometric Morphometrics”. July 17-20, 2012. Instructor: Dra Melissa Tallman (CUNY/AMNH, New York). Early registration until May 31. More information at: http://www.transmittingscience.org/3d_gm.htm

“Geometric Morphometrics and Phylogeny”. September 4-7, 2012. Instructor: Dr. Chris Klingenberg (University of Manchester, UK). More information at: http://www.transmittingscience.org/gm_and_phylogeny.htm

For any questions: courses&amp;lt; at &amp;gt;transmittingscience.org.
These courses will be held in the premises of S&lt;/pre&gt;</description>
    <dc:creator>Soledad Esteban</dc:creator>
    <dc:date>2012-05-25T09:04:52</dc:date>
  </item>
  <item rdf:about="http://comments.gmane.org/gmane.science.dinosaurs.general/54810">
    <title>K/T '3-meter gap' controversy</title>
    <link>http://comments.gmane.org/gmane.science.dinosaurs.general/54810</link>
    <description>&lt;pre&gt;From: Ben Creisler
bcreisler&amp;lt; at &amp;gt;gmail.com


A new online paper:

A.J. (Tom) van Loon (2012)
Time and space in stratigraphy: The ‘3-m gap’ story.
Proceedings of the Geologists' Association (advance online publication)
http://dx.doi.org/10.1016/j.pgeola.2012.03.008
http://www.sciencedirect.com/science/article/pii/S0016787812000296


Even for earth scientists it appears difficult to keep in mind that a
sedimentary succession does not form due to accumulation at a constant
rate, but that long periods of slow accumulation may alternate with
short phases of event sedimentation and/or shorter or longer
time-spans of non-deposition or even erosion. An example of this
incorrect way of thinking is a recently published article in which it
is postulated that the find of a ceratopsian brow horn only 13 cm
below the K/T boundary in the Hell Creek Formation (Montana, USA)
proves that dinosaurs did not become extinct before the K/T impact. It
is argued why the postulated consequence (closure of the so-called 3-m
gap: a zon&lt;/pre&gt;</description>
    <dc:creator>Ben Creisler</dc:creator>
    <dc:date>2012-05-24T16:11:23</dc:date>
  </item>
  <item rdf:about="http://comments.gmane.org/gmane.science.dinosaurs.general/54794">
    <title>Phylogeny of Ankylosaur Dinosaurs - PDF request</title>
    <link>http://comments.gmane.org/gmane.science.dinosaurs.general/54794</link>
    <description>&lt;pre&gt;Hi all,

Once again early access has prevented my institution from getting what we normally get.

If anyone has access to the latest paper on ankylosaur systematics, I would really appreciate a copy of it.


Thank you,

Jason
 

Thompson, R.S., Parish, J.C., Maidment, S.C.R., Barrett, P.M. 2012. Phylogeny of the Ankylosaurian Dinosaurs (Ornithischia: Thyreophora). J.Syst.Paleo. Vol.10(2):301-312

&lt;/pre&gt;</description>
    <dc:creator>Jura</dc:creator>
    <dc:date>2012-05-23T18:03:59</dc:date>
  </item>
  <item rdf:about="http://comments.gmane.org/gmane.science.dinosaurs.general/54789">
    <title>Chechnya "dinosaur eggs" officially debunked</title>
    <link>http://comments.gmane.org/gmane.science.dinosaurs.general/54789</link>
    <description>&lt;pre&gt;From: Ben Creisler
bcreisler&amp;lt; at &amp;gt;gmail.com


Alas, the supposed giant "dinosaur eggs" from Chechnya are only boring rocks--


http://www.rt.com/news/chechen-eggs-rocks-photos-996/

&lt;/pre&gt;</description>
    <dc:creator>Ben Creisler</dc:creator>
    <dc:date>2012-05-23T17:38:32</dc:date>
  </item>
  <item rdf:about="http://comments.gmane.org/gmane.science.dinosaurs.general/54786">
    <title>Dinosaur tracks from Cretaceous of Alaska</title>
    <link>http://comments.gmane.org/gmane.science.dinosaurs.general/54786</link>
    <description>&lt;pre&gt;From: Ben Creisler
bcreisler&amp;lt; at &amp;gt;gmail.com

A new online paper:


Anthony R. Fiorillo, Thomas L. Adams &amp;amp; Yoshitsugu Kobayashi (2012)
Cretaceous Research (advance online publication)
http://dx.doi.org/10.1016/j.cretres.2012.04.013
http://www.sciencedirect.com/science/article/pii/S0195667112000869



An unnamed nonmarine sedimentary package of rocks in southeastern
Alaska in Wrangell-St. Elias National Park and Preserve has provided
the first evidence of dinosaurs for this vast region. The rock unit is
contained within the Wrangellia Terrane and exposures are of limited
geographic extent. The rock unit is considered to be latest Cretaceous
age. Sections are overwhelmingly dominated by extraformational
conglomerates. Fine- to medium-grained light coloured sandstones are
common and medium grey shales occur as minor components of the
sections. Megafloral specimens indicate an abundance of horsetails,
ferns and gymnosperm wood. Rather than two-dimensional impressions,
most ferns are preserved in three dimensions, sugg&lt;/pre&gt;</description>
    <dc:creator>Ben Creisler</dc:creator>
    <dc:date>2012-05-23T17:13:46</dc:date>
  </item>
  <item rdf:about="http://comments.gmane.org/gmane.science.dinosaurs.general/54785">
    <title>Ichthyostega limb joint mobility</title>
    <link>http://comments.gmane.org/gmane.science.dinosaurs.general/54785</link>
    <description>&lt;pre&gt;From: Ben Creisler
bcreisler&amp;lt; at &amp;gt;gmail.com


A new advance paper in Nature:

Stephanie E. Pierce, Jennifer A. Clack &amp;amp; John R. Hutchinson (2012)
Three-dimensional limb joint mobility in the early tetrapod Ichthyostega.
Nature (advance online publication)
doi:10.1038/nature11124
http://www.nature.com/nature/journal/vaop/ncurrent/full/nature11124.html

The origin of tetrapods and the transition from swimming to walking
was a pivotal step in the evolution and diversification of terrestrial
vertebrates. During this time, modifications of the limbs—particularly
the specialization of joints and the structures that guide their
motions—fundamentally changed the ways in which early tetrapods could
move. Nonetheless, little is known about the functional consequences
of limb anatomy in early tetrapods and how that anatomy influenced
locomotion capabilities at this very critical stage in vertebrate
evolution. Here we present a three-dimensional reconstruction of the
iconic Devonian tetrapod Ichthyostega and a quantitativ&lt;/pre&gt;</description>
    <dc:creator>Ben Creisler</dc:creator>
    <dc:date>2012-05-23T17:11:50</dc:date>
  </item>
  <item rdf:about="http://comments.gmane.org/gmane.science.dinosaurs.general/54783">
    <title>EOABELISAURUS</title>
    <link>http://comments.gmane.org/gmane.science.dinosaurs.general/54783</link>
    <description>&lt;pre&gt;
OoooH ... Please .... anybody .... send me a copy
of this paper !!!    Thank you ever so much !!!
- dale       

&lt;/pre&gt;</description>
    <dc:creator>dale mcinnes</dc:creator>
    <dc:date>2012-05-23T15:42:32</dc:date>
  </item>
  <item rdf:about="http://comments.gmane.org/gmane.science.dinosaurs.general/54780">
    <title>Agustinia ligabuei</title>
    <link>http://comments.gmane.org/gmane.science.dinosaurs.general/54780</link>
    <description>&lt;pre&gt;Hi all,

I'm going to ask a potentially very silly question: how certain can we
be that the osteoderms (particularly types 3 and 4) of *Agustinia
ligabuei* Bonaparte, 1999 are actually osteoderms? Is it possible that
they are just misidentified transverse processes / sacral ribs
(compare the base of the osteoderm (but rotate it upside down) in
Bonaparte (1999) to Figure 23.B in Curry Rogers (2009), for example)?
If so, then the sacrum would have to have been at least a third wider
than it is long (though I don't 100% trust the scale bars for the
dimensions of the sacral vertebrae - in Bonaparte (1999), Figure 1
suggests that they are ~11cm long, whilst Figure 2 suggests ~67cm...).
Novas (2009) follows Bonaparte's (1999) Figure 2, and based on his
Figure 5.4 (p. 173; presuming his scaling of the osteoderms is
correct) the breadth of the pelvis (without the ilia) would be ~91cm.

The identity of the Type 2 osteoderm (640mm transverse length) is a
bit more problematic; could it be the fused ischia, viewed dorsa&lt;/pre&gt;</description>
    <dc:creator>Stephen Poropat</dc:creator>
    <dc:date>2012-05-23T13:57:25</dc:date>
  </item>
  <item rdf:about="http://comments.gmane.org/gmane.science.dinosaurs.general/54775">
    <title>White House petition for open access</title>
    <link>http://comments.gmane.org/gmane.science.dinosaurs.general/54775</link>
    <description>&lt;pre&gt;Many of you will already know about this, but at present there is an
unprecedented opportunity to contribute to the legislative push for
open access to federally funded research in the USA -- including, but
not limited to, palaeontology.

The White House OSTP (Office of Science and Technology Policy) has
solicited public comments on open access twice in as many years, which
shows its concern.  Now, following a meeting between the president's
Chief Science Advisor John Holdren and open-access advocates including
John Wilbanks and SPARC's Heather Joseph, the administration wants to
gauge public interest in this issue by means of an online petition:
        http://wh.gov/6TH

YOU DO NOT NEED TO BE AMERICAN TO SIGN THE PETITION.  This is an
international issue, and international signatures are welcomed.  All
that's required is that you are 13 or older, and have an email address
that they can use for the verification email.

The petition needs to hit 25,000 signatures in 30 days in order to
cross the president's &lt;/pre&gt;</description>
    <dc:creator>Mike Taylor</dc:creator>
    <dc:date>2012-05-23T11:54:02</dc:date>
  </item>
  <item rdf:about="http://comments.gmane.org/gmane.science.dinosaurs.general/54774">
    <title>Eoabelisaurus - almost complete Aalenian-Bajocian abelisaurid.</title>
    <link>http://comments.gmane.org/gmane.science.dinosaurs.general/54774</link>
    <description>&lt;pre&gt;Diego Pol &amp;amp; Oliver W. M. Rauhut (2012) A Middle Jurassic abelisaurid from Patagonia and the early diversification of theropod dinosaurs. Proc. R. Soc. B rspb20120660; published ahead of print May 23, 2012, 1471-2954

Abstract = Abelisaurids are a clade of large, bizarre predatory dinosaurs, most notable for their high, short skulls and extremely reduced forelimbs. They were common in Gondwana during the Cretaceous, but exceedingly rare in the Northern Hemisphere. The oldest definitive abelisaurids so far come from the late Early Cretaceous of South America and Africa, and the early evolutionary history of the clade is still poorly known. Here, we report a new abelisaurid from the Middle Jurassic of Patagonia, Eoabelisaurus mefi gen. et sp. nov., which predates the so far oldest known secure member of this lineage by more than 40 Myr. The almost complete skeleton reveals the earliest evolutionary stages of the distinctive features of abelisaurids, such as the modification of the forelimb, which started with a&lt;/pre&gt;</description>
    <dc:creator>Choo, Brian</dc:creator>
    <dc:date>2012-05-23T09:53:43</dc:date>
  </item>
  <item rdf:about="http://comments.gmane.org/gmane.science.dinosaurs.general/54767">
    <title>Palaeochirotherium, new Triassic archosaur tracks from central Germany</title>
    <link>http://comments.gmane.org/gmane.science.dinosaurs.general/54767</link>
    <description>&lt;pre&gt;From: Ben Creisler
bcreisler&amp;lt; at &amp;gt;gmail.com

Many thanks to Jürgen Fichter for bringing this paper to my attention
and for providing a copy. Although the issue is dated 2011, I believe
the true publication date would be 2012, which affects the citation
for the new ichnotaxon: Palaeochirotherium macrodactylum Fichter &amp;amp;
Kunz 2012. Please correct me if I am wrong!

I mentioned the name Palaeochirotherium when it appeared in a German
news story a few weeks back. See below.

Jürgen Fichter &amp;amp; Reiner Kunz (2011 [2012])
Neue Nachweise chirotheroider Fährten in der Detfurth-Formation
(Mittlerer Buntsandstein, Untere Trias) bei Wolfhagen.[New evidence of
chirotheroid tracks in the Detfurth-Formation (Middle Bunter, Lower
Triassic) near Wolfhagen.]
Geologisches Jahrbuch Hessen 137: 5-18

Abstract
New evidence of chirotheroid tracks from a quarry near Wolfhagen with
exposed Detfurth-Formation (Middle Bunter, Lower Triassic) is
described. (Speculative) information about the population of
trackmakers of Protochirotherium wo&lt;/pre&gt;</description>
    <dc:creator>Ben Creisler</dc:creator>
    <dc:date>2012-05-23T03:01:08</dc:date>
  </item>
  <item rdf:about="http://comments.gmane.org/gmane.science.dinosaurs.general/54761">
    <title>Pterosaur flapping frequency question</title>
    <link>http://comments.gmane.org/gmane.science.dinosaurs.general/54761</link>
    <description>&lt;pre&gt;Dear all: I was reading on the flapping frequency of Pteranodon in
Stein (1975), which claims a wing stroke for second for an inferred 15
kg. Pteranodon. However, that weight is no longer considered the adult
weight, as far as I know. Do you know where can I read about the
relationship between wing stroke frequency relative to body mass, if
present?
Thank you in advance,
Augusto.

&lt;/pre&gt;</description>
    <dc:creator>Augusto Haro</dc:creator>
    <dc:date>2012-05-23T02:23:11</dc:date>
  </item>
  <item rdf:about="http://comments.gmane.org/gmane.science.dinosaurs.general/54753">
    <title>Quadrupedal Ornithischian Dinosaur Stance and Gait</title>
    <link>http://comments.gmane.org/gmane.science.dinosaurs.general/54753</link>
    <description>&lt;pre&gt;From: Ben Creisler
bcreisler&amp;lt; at &amp;gt;gmail.com

New in PLoS ONE:


Susannah C. R. Maidment, Deborah H. Linton, Paul Upchurch &amp;amp; Paul M.
Barrett (2012)
Limb-Bone Scaling Indicates Diverse Stance and Gait in Quadrupedal
Ornithischian Dinosaurs.
PLoS ONE 7(5): e36904.
doi:10.1371/journal.pone.0036904
http://www.plosone.org/article/info%3Adoi%2F10.1371%2Fjournal.pone.0036904


Background

most primitive ornithischian dinosaurs were small bipeds, but
quadrupedality evolved three times independently in the clade. The
transition to quadrupedality from bipedal ancestors is rare in the
history of terrestrial vertebrate evolution, and extant analogues do
not exist. Constraints imposed on quadrupedal ornithischians by their
ancestral bipedal bauplan remain unexplored, and consequently, debate
continues about their stance and gait. For example, it has been
proposed that some ornithischians could run, while others consider
that none were cursorial.

Methodology/Principal Findings

Drawing on biomechanical concepts of limb bone sc&lt;/pre&gt;</description>
    <dc:creator>Ben Creisler</dc:creator>
    <dc:date>2012-05-22T22:07:36</dc:date>
  </item>
  <item rdf:about="http://comments.gmane.org/gmane.science.dinosaurs.general/54752">
    <title>Phylogeny of Basal Iguanodonts</title>
    <link>http://comments.gmane.org/gmane.science.dinosaurs.general/54752</link>
    <description>&lt;pre&gt;From: Ben Creisler
bcreisler&amp;lt; at &amp;gt;gmail.com

New in PLoS ONE:

Andrew T. McDonald (2012)
Phylogeny of Basal Iguanodonts (Dinosauria: Ornithischia): An Update.
PLoS ONE 7(5): e36745.
doi:10.1371/journal.pone.0036745
http://www.plosone.org/article/info%3Adoi%2F10.1371%2Fjournal.pone.0036745


The precise phylogenetic relationships of many non-hadrosaurid members
of Iguanodontia, i.e., basal iguanodonts, have been unclear.
Therefore, to investigate the global phylogeny of basal iguanodonts a
comprehensive data matrix was assembled, including nearly every valid
taxon of basal iguanodont. The matrix was analyzed in the program TNT,
and the maximum agreement subtree of the resulting most parsimonious
trees was then calculated in PAUP. Ordering certain multistate
characters and omitting taxa through safe taxonomic reduction did not
markedly improve resolution. The results provide some new information
on the phylogeny of basal iguanodonts, pertaining especially to
obscure or recently described taxa, and support some rece&lt;/pre&gt;</description>
    <dc:creator>Ben Creisler</dc:creator>
    <dc:date>2012-05-22T22:05:58</dc:date>
  </item>
  <item rdf:about="http://comments.gmane.org/gmane.science.dinosaurs.general/54749">
    <title>Chickens are Myrmecophages</title>
    <link>http://comments.gmane.org/gmane.science.dinosaurs.general/54749</link>
    <description>&lt;pre&gt;I have been researching the origins of domesticated chickens and turkeys and I just stumbled on some information that may help to enrich our past discussions about myrmecophagy in alvarezsaurs.

Multiple field reports, including studies of crop contents, indicate that the Red Jungle Fowl, Gallus gallus, which is the ancestral chicken, feeds predominantly on termites in season in its native bamboo forests of India. Both adults and poults capture flying termites but also scratch into the mounds of Odontotermes obesus and consume pupae and  juveniles. Klasing, 2005, states that this is true of many asian Phaisanidae, not only Gallus.

Chicks eat a larger percentage of insect material than adult Gallus, and the breeding cycle of Gallus in the wild correlates with the annual cycle of termite availability, according to Collias and Collias, 1967.

References include Bump and Bohl, 1961, Klasing, 2005, Bebbe, 1990, Collias and Collias, 1967, and Collias and Saichuae, 1967.

This is interesting to me because chickens&lt;/pre&gt;</description>
    <dc:creator>Jason Brougham</dc:creator>
    <dc:date>2012-05-22T20:48:12</dc:date>
  </item>
  <item rdf:about="http://comments.gmane.org/gmane.science.dinosaurs.general/54748">
    <title>Dinosaur Egg Discovered in Space (joke)</title>
    <link>http://comments.gmane.org/gmane.science.dinosaurs.general/54748</link>
    <description>&lt;pre&gt;From: Ben Creisler
bcreisler&amp;lt; at &amp;gt;gmail.com


In the spirit of  all the recent badly distorted  and scientifically
unfounded news reporting on dinosaur-related items such as  sauropod
flatulence as a supposed cause of dinosaur extinction, the theory that
dinosaurs were all aquatic, and especially the purported giant
meter-wide "dinosaur eggs" [concretions!] found in Chechnya, let me be
the first to claim (in honor of the defunct Weekly World News) that a
huge "dinosaur egg" has been discovered in space. A photo can be seen
at:


http://www.universetoday.com/95323/cassini-captures-a-rarely-seen-moon/

&lt;/pre&gt;</description>
    <dc:creator>Ben Creisler</dc:creator>
    <dc:date>2012-05-22T19:10:04</dc:date>
  </item>
  <item rdf:about="http://comments.gmane.org/gmane.science.dinosaurs.general/54745">
    <title>New dinosaur hall to open in Houston, Texas</title>
    <link>http://comments.gmane.org/gmane.science.dinosaurs.general/54745</link>
    <description>&lt;pre&gt;From: Ben Creisler
bcreisler&amp;lt; at &amp;gt;gmail.com


A news story about the paleontology section about to open at the
Houston Museum of Natural Science. This version has photos:

http://www.google.com/hostednews/ap/article/ALeqM5gcKMGNMRlWvDckkKBFGKDPC_sCJA?docId=4a48620a47db4cde9ff9e2f241b646a3

Also, a free version of a NY Times article about the exhibit and
another new museum in Dallas:

http://www.post-gazette.com/stories/news/us/texas-gets-prehistoric-with-two-new-fossil-halls-636767/

&lt;/pre&gt;</description>
    <dc:creator>Ben Creisler</dc:creator>
    <dc:date>2012-05-22T16:55:17</dc:date>
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