Issue Date |
08.12.2012 |
ID |
Michel: 726-729 (A - perforate, B - imperforate );
Scott: 422-425;
Stanley Gibbons: 521-524;
Yvert et Tellier: 602-605;
Category: pR |
Design |
Eldiyar Isakov |
Stamps in set |
4 |
Value |
S23 - Kyrgyzsayrus
S30 - Xenacanthidae
S40 - Longisquama insignis
S52 - Mammuthus
|
Emission/Type |
commemorative |
Issue place |
Bishkek |
Size (width x height) |
40x28mm |
Layout |
4 Sheets of 6 stamps each |
Products |
FDC x1 |
Paper |
chalky |
Perforation |
14.25x14 |
Print Technique |
offset |
Printed by |
Publishing house "Belarusian Printing
House", Belarus |
Quantity |
perforate: 6.000 sets (1.000 sheets)
imperforate: 1.500 sets (250 sheets)
|
Issuing Authority |
Ministry of Transport &
Communication Kyrgyz Rep |
On December 8
th, 2012, the Post Authority of Kyrgyzstan issued a set
of four stamps - "Prehistoric animals", that shows
prehistoric animals who lived on territory of the country
at various points in geologic time from the Triassic to the Quaternary periods.
Note: Similar stamps exist that are imperforate.
Fossils of all these animals are found in Madygen Formation in Kyrgyzstan.
The territory of
Kyrgyzstan along with
China,
Mongolia,
Uzbekistan and
Kazakhstan is a haven for paleontological research.
In the Jurassic Period, 160 million years ago, these areas were inhabited by various prehistoric animals.
During USSR times, Soviet paleontologists found numerous remains of prehistoric animals and fish
in southern Kyrgyzstan Madygen Formation.
These fossils can be seen at the
Paleontologic Museum of Moscow.
Kyrgyzsaurus
is an extinct genus of drepanosaurid archosauromorph known from the
Triassic of southwestern Kyrgyzstan.
|
Kyrgyzsaurus on stamp of Kyrgyzstan 2012
MiNr.: 726, Scott: 422.
|
Kyrgyzsaurus is known only from the holotype specimen, the anterior part of
the skeleton including the skull, cervical and anterior dorsal vertebrae, ribs, pectoral girdle
and skin imprints.
The holotype was collected from the Madygen Formation, dating to the Late Carnian
or the early Ladinian Stage of the Late Middle or the early Late Triassic, about 230-225
million years ago.
Thus, it represents the oldest known drepanosaurid.
Kyrgyzsaurus represents also the first Asian drepanosaurid genus to be named.
Kyrgyzsaurus was first named by V. R. Alifanov and E. N.
Kurochkin in 2011 and the type species is
Kyrgyzsaurus bukhanchenkoi.
The generic name is derived from the name of Kyrgyzstan, and from Greek
sauros, "lizard", thus, the name means "Kyrgyzstan's lizard".
|
Xenacanthidae on stamp of Kyrgyzstan 2012
MiNr.: 727, Scott: 423.
|
Xenacanthidae
is a family of prehistoric sharks in the order
Xenacanthida.
Some teeth of the shark found in the Madygen Formation.
An unusual aspect of this finding was that the teeth found near the eggshell.
Scientists first stumbled upon this neighborhood.
The research team, led by German scientist Jan Fischer, examined the find
and found that eggs and teeth belong to different groups of
sharks:
Xenacanthidae and hybodontidae.
Hybodontidae - extinct relatives of modern sharks
that differ from them only by the presence of small horns on the heads of males.
Xenacanthidae also sharks became extinct about 210-million years ago.
They had the eel-like body shape and protruding spine.
Longisquama
is an extinct genus of lizard-like reptile from Late Triassic (about 200 million years ago).
|
|
Longisquama on stamp of Kyrgyzstan 2012
MiNr.: 728, Scott: 424.
|
Longisquama's reconstruction.
Image credit: Wikimedia
|
There is only one species,
Longisquama insignis, known
from a poorly preserved skeleton and several incomplete fossils
as well as a few individual feather scale impressions from the
Middle to Late Triassic Madygen Formation in Kyrgyzstan.
All specimens are in the collection of the Paleontological Institute of the
Russian Academy of Sciences in Moscow.
This is undoubtedly one of the most amazing animals.
Small size, about 15 centimeters lizard along the back which protruded two rows of long
feather scales.
The length of these scales is as long as the length of the animal.
Longisquama used them instead of a parachute.
Jumping down from the tree, she unfolded a fan of scales and slowly
lowered to the ground similar to a shuttlecock from badminton.
It was one of the first attempts for vertebrates to fly.
There were no other animals that could fly except for insects.
Perhaps insects were the diet of
Longisquama, who preyed it by
jumping down from the trees.
Mammuthus - an extinct genus of mammal elephant's family,
who lived during the Quaternary Period (2.6 million years ago to the present).
|
Mammuthus on stamp of Kyrgyzstan 2012
MiNr.: 729, Scott: 425.
|
Mammoths appeared in the Pliocene and lived between 4.8 million - 4,500 years ago in
Europe, Asia, Africa and North America.
In addition to the numerous bones of mammoths that have been found,
there are also drawings and sculptures of Mammoths made by prehistoric humans.
The major species of these mammals do not exceed the size of modern elephants,
but the North American subspecies
(
Mammuthus imperator) reached the height of 5.5
meters and a weight of 12 tons, and the dwarf species
(
Mammuthus exilis) and (
Mammuthus lamarmorae)
did not exceed 2 meters in height and weight was up to 900 kg.
Mammoths, unlike elephants, had a massive body, shorter legs, long hair and long,
curved tusks.
The main types of mammoths became extinct about 10 thousand years ago during the
last Ice Age.
However, in 1993 an employee of the reserve on the island
Varngelya, Sergey Vardanyan, discovered the remains of mammoths on the
island, whose age has been determined to be between 7000 and 3500 years old.
It remains a special, relatively small subspecies that inhabited the island of
Wrangel at a time when the Egyptian pyramids were standing, and which
disappeared only during the reign of Tutankhamun and the heyday of the
Mycenaean civilization.
Products and associated philatelic items
References:
- Technical details and short press releases:
The Department of Postal Products (Kyrgyzmarkasy):
[1],
[2],
[3],
[4];
diesel.elcat.kg (forum);
colnect;
Ukrafil;
Evening Bishkek (the article doesn't exist anymore).
Acknowledgements:
-
Many thanks to
Dr. Peter Voice from Department of Geological and Environmental Sciences, Western Michigan University,
for review of a draft of this article.