United Kingdom 1991 "150th
Anniversary of Dinosaurs' Identification by Owen"
Issue Date |
20.08.1991 |
ID |
Michel: 1350-1354 Scott: 1387-1391 Stanley
Gibbons: 1573-1577 Yvert: 1556-1560 UPU: N/A Category: pF |
Author |
Bryan Kneale |
Stamps in set |
5 |
Value |
22 p., Iguanodon (Only Iguanodon was known to Owen.)
26 p., Stegosaurus
31 p., Tyrannosaurus
33 p., Protoceratops
37 p., Triceratops
Outline of the animal and human for scale. |
Size (width x height) |
37x35mm |
Layout |
sheets of 100 stamps |
Products |
FDC x 1 PP x1 |
Paper |
unwatermarked phosphor-coated. Gum:PV/1 Dextrin |
Perforation |
14.5 x 14 |
Print Technique |
Inphotograviibe |
Printed by |
Harrison & Sons Limited |
Quantity |
|
Issuing Authority |
Royal Mail of Great Britain |
In August 1991 Royal Mail issued a set of 5 stamps in order to
commemorate great British paleontologist Sir Richard Owen who entered
the world "Dinosaur" in English language in 1841.He coined the name for
a lecture to the British Association
Advancement of Science on Friday 30th July 1841. Dinosaur fossils had
been disicovered many centuries earlier, but it took the genius of
Richard Owen, the best comparative anatomist of the time, to unlock
some of the mysteries of these early finds, which consisted only of odd
teeth and bones. Owen was particularly struck by the fact that three
types (Megalosaurus, Iguanodon and Hylaeosaurus) were not only very
large, but had bodies designed (so he thought) rather like those of
massive modern mammals such as elephants and rhinoceroses. Professor
Owen named these three species dinosaurs to suggest that they were the
most remarkable type of reptile to walk the ancient earth. We now know
that Owens view of dinosaurs as elephantine reptiles was wrong, but he
was absolutely right about how truly remarkable these creatures were.
The idea of commemorate Owen's Dinosauria was suggested by British
paleontologist & professor of Geology & Zoology and
popularizer of science - Lambert Beverly Halstead (13 June 1933 - 30
April 1991). His idea got a wide support from many leading scientist of
Geology and Paleontology. After the theme was accepted by Royal Mail,
four designers (Mrs. Jenny Halstead, John Larkin, Christopher Wormall
and Bryan Kneale) asked to produce some stamps draft. The draft of Mr.
Bryan Kneale is selected by Design Department of Royal Mail and Stamps
Advisory Commitee.
Richard Owen (l8041892) was a medical anatomist who trained at
Edinburgh and St Bartholomews Hospital, London continued to prosper
and, after the completion of the Natural History Museum in 1881, Sir
Richard Owen (as he was later to become) was appointed as the first
Superintendent of Collections. Owens broad and expert knowledge of both
living and fossil animals made him a natural choice to review British
fossil reptiles during the late 1830s. The need for such a review had
become pressing because in the early years of the nineteenth century an
explosion in the rate of discovery and description of fossils had occurred.
Great
excitement and interest had arisen in collecting and
studying fossils of all types through the work of the Frenchman Baron
Georges Cuvier (1769-l832). ln the 1790s and early 1800s Cuvierhad been
able to prove, for the first time, not only that fossils were
the remains of once living creatures rather than simply being curious
stones which could be dug from the ground, but also that some fossil
reptiles must have been monstrously large. Understanding the true
nature of these early finds was difficult because the fossil remains
were almost always isolated teeth and fragments of bone. Here Owens
skill as an anatomist proved to be most important, for heg was able to
deduce from a vast array of material in private collections scattered
throughout the country that some of the fossil reptiles discovered in
Britain during the 1820s and 1830s were not only very large, but quite
unlike those living today.
He concentrated on three types of giant
reptile: Megalosaurus (big reptile), Iguanodon (iguana tooth) and
Hylaeosaurus (forest reptile). Each of these animals was very large (in Owens estimation
about 9 metres long) and had massive, pillar-like legs, short powerful
toes and a backbone built for great strength. All these features seemed
to Owen to belong to. lanndliving creatures bearing a strong
resemblance to the maassive tropical mammals of today, such as
rhinoceroses and elephants. He therefore classified them as a distinct
tribe or suborder erof Saurian Reptiles for which l would propose the
name of Dinosauria. He considered them to be important, believing that
they represented the ultimate stage in reptilian design, mimicking as
nearly as was possible the form of the largest living tropical mammals,
at a time in the past when the world was ruled by reptiles. The
combination of Owens fame and the concept of the dinosaur
captured the public imagination and received a further boost in the
early 1850s. In 1852 Joseph Paxtons Crystal Palace, which had formed
the centrepiece of the Great Exhibition of 1851 in Hyde Park, was
dismantled and moved to a new permanent site at Sydenham. During the
planning for the reopening, it was suggested that the grounds around
the Palace should be landscaped and a populated with life-sized models
of prehistoric animals. Benjamin Waterhouse Hawkins was commissioned to
build the models and, working closely with Owen created four life-sized
restorations of the dinosaurs in brick, reinforced with iron bars and
covered with concrete (two models of Iguanodon, and one each of
Megalosaurus and Hylaeosaurus). After the official reopening of the
Crystal Palace by Queen Victoria in June l854, dinosaurs and other
prehistoric monsters and, although the Palace itself burned downin
1936, the incredible monsters survived and can still he seen to this
day. Since the 1850s considerable advances have been made in the study
of dinosaurs, largely through the discovery of complete, or nearly
complete skeletons. These have shown that Owens view of dinosaurs as
gigantic, scaly, rhinoceros-like creatures was inaccurate, as were his
models. Considering the lamentable state of the material with which he
had to work, this was centiirely excusable, and it is amazing that he
managed to see clearly how different these animals were from anything
else then known. If Owen had a failing, it was that he could not
imagine just how bizarre and utterly different his dinosaurs could be
from anything that has lived before or since.
Iguanodon
(Only
Iguanodon of all
dinosaurs depicting on these stamps was known to Owen.)
Named
in 1825 by English geologist Gideon Mantell, based on sime teeths
found by his wife, Mrs. Mary Ann Mantell, in 1822 in Sussex, southern
England. Iguanodon was the second dinosaur formally named, after
Megalosaurus. Together with Megalosaurus and Hylaeosaurus, it was one
of the three genera originally used to define Dinosauria. It
had a
large thumb spike which could have been used to collect vegetation or
to defend itself. A better specimen was discovered in a quarry in
Maidstone, Kent, in 1834 (lower Lower Greensand Formation), which
Mantell soon acquired. He was able to identify it as an Iguanodon from
its distinctive teeth.The Maidstone slab allowed the first skeletal
reconstructions and artistic renderings of Iguanodon. As such, he made
some mistakes, the most famous of which was the placement of what he
thought was a horn on the nose.The discovery of much better specimens
in later years revealed that the horn was actually a modified thumb.
The largest find of Iguanodon remains to date occurred on 28 February
1878 in a coal mine at Bernissart in Belgium, at a depth of
322m when two mineworkers, accidentally hit on a skeleton that they
initially took for petrified wood. With the encouragement of Alphonse
Briart, supervisor of mines at nearby Morlanwelz, Louis de Pauw on 15
May 1878 started to excavate the skeletons and in 1882 Louis Dollo
reconstructed them. At least 38 Iguanodon individuals were uncovered,
most of which were adults. Many of them went on public display
beginning in July 1883 and are still present for viewing. The exhibit
makes an impressive display in the Royal Belgian Institute of Natural
Sciences, in Brussels. A replica of one of these is on display at the
Oxford University Museum of Natural History and at the Sedgwick Museum
in Cambridge. Most of the remains were referred to a new species,
Iguanodon. bernissartensis, a larger and much more robust animal than
the English remains had yet revealed, but one specimen was referred to
the nebulous, gracile Iguanodon. mantelli (now Dollodon bampingi). The
skeletons were some of the first complete dinosaur skeletons known.
Stegosaurus
Stegosaurus, meaning "roof lizard" in reference to
its
bony plates is a genus of armored stegosaurid dinosaur. They lived
during the Late Jurassic period some 155 to 150 million years ago in
what is now western North America. In 2006, a specimen of Stegosaurus
was announced from Portugal, showing that they were present in Europe
as well. Due to its distinctive tail spikes and plates, Stegosaurus is
one of the most recognizable dinosaurs.
A large, heavily built, herbivorous quadruped, Stegosaurus had a
distinctive and unusual posture, with a heavily rounded back, short
forelimbs, head held low to the ground and a stiffened tail held high
in the air. Its array of plates and spikes has been the subject of much
speculation. The spikes were most likely used for defense, while the
plates have also been proposed as a defensive mechanism, as well as
having display and thermo regulatory functions. Stegosaurus had a
relatively low brain-to-body mass ratio. It had a short neck and small
head, meaning it most likely ate low-lying bushes and shrubs.
Tyrannosaurus
Tyrannosaurus
is a genus of coelurosaurian theropod
dinosaur. It lived throughout what is now western North America, with a
much wider range than other tyrannosaurids. Fossils are found in a
variety of rock formations dating to the Maastrichtian age of the upper
Cretaceous Period, 67 to 65.5 million years ago.
Like other
tyrannosaurids, Tyrannosaurus was a bipedal carnivore with a massive
skull balanced by a long, heavy tail. Relative to the large and
powerful hindlimbs, Tyrannosaurus forelimbs were small, though
unusually powerful for their size, and
bore two clawed digits. Although other theropods rivaled or exceeded
Tyrannosaurus rex in size, it was the largest known tyrannosaurid and
one of the largest known land predators, measuring up to 12.8 m in
length, up to 4 metres tall at the hips, and up to 6.8 metric tons in
weight. By far the largest carnivore in its environment, Tyrannosaurus
rex may have been an apex predator, preying upon hadrosaurs and
ceratopsians, although some experts have suggested it was primarily a
scavenger. The debate over Tyrannosaurus as apex predator or scavenger
is among the longest running in paleontology.
Protoceratops
Protoceratops is a genus of sheep-sized (1.5 to 2 m
long) herbivorous ceratopsian dinosaur, from the Upper Cretaceous
Period of what is now Mongolia. It was a member of the
Protoceratopsidae, a group of early horned dinosaurs. Unlike later
ceratopsians, however, it was a much smaller creature that lacked
well-developed horns and retained some primitive traits not seen in
later genera. Protoceratops had a large neck frill, which may have
served to protect the neck, to anchor jaw muscles, to impress
other members of the species, or combinations of these functions.
Described by Walter W. Granger and W.K. Gregory in 1923, In the 1920s,
Roy Chapman Andrews discovered fossilized eggs in Mongolia that were
interpreted as belonging to this dinosaur, but which turned out to be
those of Oviraptor.
Triceratops
Triceratops is a genus of herbivorous
ceratopsid
dinosaur which lived during the late Maastrichtian stage of the Late
Cretaceous Period, around 68 to 65 million years ago in what is now
North America. It was one of the last dinosaur genera to appear before
the great CretaceousPaleogene extinction event. The term Triceratops,
which literally means "three-horned face". Bearing a large bony frill
and three horns on its large four-legged body, and conjuring
similarities with the modern rhinoceros, Triceratops is one of the most
recognizable of all dinosaurs and the best known ceratopsid. It shared
the landscape with and was preyed upon by the fearsome Tyrannosaurus,
though it is less certain that the two did battle in the manner often
depicting in traditional museum displays and popular images.
The function of the frills and three distinctive facial
horns has long inspired debate. Traditionally these have been viewed as
defensive
weapons against predators. More recent theories, noting the presence of
blood vessels in the skull bones of ceratopsids, find it more probable
that these features were primarily used in identification, courtship
and dominance displays, much like the antlers and horns of modern
reindeer, mountain goats, or rhinoceros beetles.The theory finds
additional support if Torosaurus represents the mature form of
Triceratops, as this would mean the frill also developed holes
(fenestrae) as individuals reached maturity, rendering the structure
more useful for display than defense.
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