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These
dinosaurs are only known from material that cannot be used
to determine taxa, so are unnamed, unless stated otherwise...
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These
dinosaurs have yet to be formally described, and may never
be...
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The
dinosaurs below are either misidentified or synonyms (see FAQ) |
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"Angloposeidon"
A
bit about Isle of Wight Brachiosaurs
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This
dinosaur, unofficially known as "Angloposeidon",
is known from a single cervical vertebra, which measures
somewhere in the region of 75cm in length, and is relatively
complete though it is partially crushed. There is enough
present, however, to assign it to the Brachiosauridae, with
many similarities with the North American genus Sauroposeidon,
although there is enough differences to determine it as
a new taxon, although there is a chance it may belong to
one of the already known brachiosaurids from the Isle of
Wight.
This
represents the largest known brachiosaurid vertebra known
from Europe, and is similar in scale to Brachiosaurus
from Tanzania, Africa. This would make the entire animal
somewhere in the region of 20 metres in length.
The specimen, MIWG 7306, is currently on display at Dinosaur
Isle.
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All
information on this specimen taken from Naish
et al, 2004
mon
Clabby 2006
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indet.
tetanuran theropod (MIWG 6350)
Known from some partial pubic bones and a femoral fragment, this theropod has just enough material for it to be identified as being different to all the other theropod dinosaurs known from the Isle of Wight. It appears to be a basal tetanuran or indeterminate classification, although it is not a coelurosaur (see below)
The pubes curve gently backwards, the two medial flanges of which form an apron (in other words, bony shelves project inwards from the inner surfaces of both pubic shafts) that is separated for about half of its length by a long slit. A blunt pubic boot, consisting of the conjoined ends of both pubes, is present. The projecting anterior part is missing, but its posterior part is wide and tapers less than the pubic boots of coelurosaurs. the halves of the ubic boot are not fully joined, suggesting this was not a fully grown specimen, even though via compparison with similar theropods, that this dinosaur would have been just over 5 metres in length!
The femur fragment consists of the distal end. Both condyles are preserved, as is a deep extensor groove on the fragment's anterior surface
All
information on this specimen taken from Benson et al, 2009, via Tet Zoo
Simon
Clabby 2006 |
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"indet.
sauropod"
Sauropod
dinosaur, known from a well-preserved chevron (V-shaped bone
attached to the ventral surface of caudal vertebrae, sometimes
called haemal arches), with fragile plate-like anterior
process and less pronounced dorsal process, was found near Grange
Chine in 1975. Although similar to Diplodocus, the midline
slit is shorter and narrower, so may belong to a dicraeosaurid.
However, the 'sled-like' morphology supporting a diplodocoid
assignation is now thought to have been primitive for neosauropods,
rather than derived, so may not be a diplodocoid at all
Also,
BMNH R9224, a 170mm long caudal vertebra from Brighstone
Bay, BMNH R11187, a first metatarsal and MIWG.6593, a fragmentary
ischium.
All
information on this specimen taken from Martill
and Naish, 2001d
Simon
Clabby 2006
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indet. Rebbachisaurid Mannion, 2008
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sauropod dinosaur, known from isolated teeth,
already figured in Naish
and Martill 2001d, but only identified as such in Sereno
and Wilson 2005 and Fowler, in press.and an incomplete
scapular, which displays the extreme dorsoventral expansion
of the scapular blade and the hook-like acromial
process that are characteristic of rebbachisaurids. |
Simon
Clabby 2006 Clabby 2006
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?'Titanosaurus
lydekkeri' Huene, 1929
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The
only ?'Titanosaurus' (gigantic lizard) specimen
is an isolated anterior caudal vertebra from the distal
half of the tail, which was, unusually for an Isle of
Wight dinosaur, found in the Upper Greensand. the vertebra
consists of a centrum, which is strongly procoelous and
may have had transverse processes, indicated by broken
ridge-like areas close to the top, has a slight transverse
compression and convex dorsoventral lateral surfaces that
merge smoothly into the ventral surface. There is no ventral
excavation, and there is an absence of ventrolateral ridges.
There is no horizontal ridge at the neurocentral junction,
and the base of each prezygapophysis is preserved, although
little detail can be seen. There is also a partial neural
arch.
Although this appears to be to a titanosaur, there are
no distinguishing features that diagnose it as any specific
genus.
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All
information on this specimen taken from Martill
and Naish, 2001d and Wilson
and Upchurch, 2003
Simon
Clabby 2006 Clabby 2006
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Indet.
Velociraptorines
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The
presence of dromaeosaurs in the Wessex
fauna has been predicted for some time based on the known
palaeobiogeographical distribution of this group of dinosaurs.
However, until 2003 their remains had not been recognized.
During the course of work on the microvertebrate fauna of
the Wessex Formation,
Island resident and research palaeontologist Steve Sweetman
identified a number of teeth in his collection (one of which
he found in 1972) that are attributable to velociraptorine
dromaeosaurs. A search of other local collections revealed
three further specimens bringing the total to seven. The
specimens have been donated to the collections of the Isle
of Wight Museum Service.
The
largest of the teeth are similar in size to the teeth of
the dromaeosaurine dromaeosaur Utahraptor, from the
Cedar Mountain Formation of Utah, which is the same age
as the Wessex Formation of
the Isle of Wight. It is possible therefore that the Isle
of Wight velociraptorine dromaeosaur could have been of
similar size to Utahraptor, making it the largest
velociraptorine yet discovered. Uncertainty concerning the
number of taxa represented by the specimens and other considerations
have prevented the naming of a taxon based on the teeth
but they do represent the first unequivocal record of dromaeosaurs
in the Wessex Formation,
although Ornithodesmus
is most probably a dromaeosaur too, but that assignation
is debatable.
The
known teeth have a DSDI (Denticle-Size Difference Index
[See here for how this
is worked out]) of between 1.37 and 1.6. There are unflexed
mesial carinae that divide the mesial margin of the crown
symmetrically. Where present, mesial denticles are smaller
than those present on the distal carinae. Uniformly sized
denticles are present along most of the mesial and distal
carinae but shrink progressively towards the tooth tip and
base. A wear facet at the tooth tip is present, having removed
the most apical denticles and breached the enamel, and is
orientated obliquely towards the mesial carina, and more
denticles have been removed from the mesial carinae than
from the distal carinae. The denticle bases on the distal
carinae are apicobasally compressed and strongly rectangular
in outlinecompared to the mesial carinae, which are either
labiolingually compressed or approximately square in basal
profile. The distal denticle tips are apicobasally inflated
and convex, and in lateral profile are almost axe-like.
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All
information on these specimens taken from Sweetman,
2004 and from personal communication with Steve Sweetman.
Simon
Clabby 2006
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Unpublished
Dinosaurs and Other Relevant Finds
- Dollodon,
one of the many ornithopods previously called Iguanodon
- At least
one tyrannosauroid, distinct from Eotyrannus
- A diplodocoid,
distinguished from indet. sauropod,
which was originally classed as a diplodocoid
- Indet.
theropod, of unknown affinity. Had massive hands though...
- Suchosaurus
- Previously classified as a crocodilian, the type material
(teeth) has been reassigned to the spinosauroidea, and may be
synonymous with Baryonyx.
However, until anything is published, it's uncertain if the
Isle of Wight Suchosaurus is the same or just indet.
crocodilian material lumped within the genus.
- Dinosaur
eggshell, although a possible dinosaur egg was reported by van
Straelen in 1928 from the Wealden of the Isle of Wight which
is considered dubious by some authors (Carpenter
and Alf, 1994).
Please
note that this list is not meant to represent any material that
is awaiting publication. If you recognise any of the dinosaurs
as being the subject of your upcoming paper, please contact
me.
Simon
Clabby 2006
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Cetiosaurus
brevis Owen,
1842
Pronounced
'SEET-ee-oh-SAW-russ Brev-ISS'
An
alleged sauropod, known on the Isle of Wight from several vertebrae
from Sandown Bay and Culver Cliff and very fragmentary vertebrae
and limb elements from the Wessex
Formation of Brook. If all these belonged to the same individual,
then they would have been the second most complete Isle of Wight
sauropod, diagnosed on the basis of a low centrum Length: Height
(l:h) ratio, a derived condition present in the anterior caudal
centra of eusauropods. However, recently it has been demonstrated
that all the material assigned to C. brevis by Owen belongs
to Iguanodon (which also has
a low l:h ratio in the posterior dorsals), with the exception
of BMNH R25442550 which represent an indeterminate sauropod.
Most specimens are too poorly preserved to be identified precisely
and may not even be confidently assigned to the Sauropoda.
All
information on this specimen taken from Martill
and Naish, 2001d and Upchurch
and Martin, 2002
For
information on actual Cetiosaurus
fossils, visit DinoWight
EXTRA
Simon
Clabby 2006
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Megalosaurus
Buckland,
1824
Pronounced
'Meg-a-low-SAW-russ'
If
it's on the Isle of Wight, then it's most likely Neovenator,
as most Megalosaurus
material across the world has turned out to be something else,
e.g. Dilophosaurus, Allosaurus, Plateosaurus,
etc.
For
information on actual Megalosaurus
fossils, visit DinoWight
EXTRA
Simon
Clabby 2006
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Polacanthoides
Nopsca, 1929
Pronounced
'Pole-a-CAN-THOI-dees'
Known
from an isolated tibia, humerus and possibly a scapula, almost
certainly Polacanthus
Simon
Clabby 2006
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stegosauria indet (Regnosaurus?)
Pronounced
'Regg-no-SAW-russ'
Known only
from a pubis on the Island, this specimen has been better described
from material found on the mainland in Surrey. The pubis, although
incomplete, has a stout prepubic process and a slender postpubic
process, similar to Iguanodon,
but the prepubic process shows no flaring and there is no anterior
recess next to the position of the acetabulum, which suggests stegosaur.However, the acetabular surface of "Regnosaurus" laterally, posteriorly and
dorsally, in stegosaurs this surface faces
wholly laterally. It is therefore more likely that this specimen is from an Iguanodontoid.
All
information on this specimen taken from Naish and Martill, 2001c and Galton, 2009
Simon
Clabby 2006 |
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Vectensia
Delair, 1982
Pronounced
'Veck-TEN-see-ah'
nomen
nudem, known only from a triangular flat sided bony spike,
about 25cm (10 inches) long, but possibly Polacanthus
Simon
Clabby 2006
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Vectisaurus
Hulke, 1879
Pronounced
'Veck-TISS-or-uss'
Juvenile
specimen of Mantellisaurus
Simon
Clabby 2006
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