Issue Date |
24.05.1995 |
ID |
Michel: 789-792, Bl.22 (793);
Scott: 779-782, 780a;
Stanley Gibbons: 663-666, 667;
Yvert et Tellier: 745-748, BF22;
Category: pF
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Design |
Lambert Kreidemann |
Stamps in set |
5 |
Value |
40c - Tortoise Geochelone stromeri (shell)
80c - Diamantornis wardi (eggs)
90c - Prohyrax hendeyi (skull)
N$1.20 - Crocodylus lloydi (skull)
Souvenir-Sheet, 80c - Diamantornis wardi
(the same design as the 80c stamp)
|
Size (width x height) |
stamps: 29 mm x 45mm,
Souvenir-Sheet: 50 mm x 65 mm
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Layout |
Mini-Sheets of 10 stamps,
Souvenir-Sheet with 1 stamp.
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Products |
FDC x 2 |
Paper |
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Perforation |
13.75 x 14.25 |
Print Technique |
Offset |
Printed by |
Government Printer, Pretoria, South Africa |
Quantity |
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Issuing Authority |
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On May 24
th, 1995, the Post Authority of Namibia issued the set
of four stamps and the Souvenir-Sheet depicting some fossil of prehistoric animals
and some modern animals of the country.
All these fossils were found at the Orange River Valley.
Orange River is the longest river in South Africa.
It rises in the Drakensberg mountains in Lesotho,
flowing westwards through South Africa to the Atlantic Ocean.
The river forms part of the international borders between South Africa and Namibia
and between South Africa and Lesotho, as well as several provincial borders within South Africa.
Except for Upington, Kimberly, and Aggeneys, the river does not pass through any major cities,
it plays an important role in the South African economy by providing water for irrigation,
as well as hydroelectric power.
The river was named by Robert Jacob Gordon after the Dutch Royal House.
The following text was written by Dr. Martin Pickford from Geological Survey of Namibia.
The text was published in
the information card attached to the FDC.
The fossils of the Orange River Valley provide us with a rare glimpse of life in southern Namibia
between 20 and 16 million years ago.
40c - Geochelone stromeri
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Geochelone stromeri on stamp of Namibia 1995
MiNr.: 789, Scott: 779.
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In the Lower Miocene Period 19 to 20 million years ago, the coastal region of southern
Namibia was inhabited by giant tortoises, first described in 1926 as
Geochelone stromeri.
In 1992, the first complete carapaces of this species were found during diamond
mining operations at Auchas in the Orange River Valley 50 kilometres upstream from Oranjemund.
The tortoises are associated with fossil mammals and plants that indicate that the area
enjoyed a subtropical climate at the time that they lived, in stark contrast to the extremely
arid conditions that prevail there today.
The specimen depicting on the stamp is almost half a metre long and 25 centimetres high,
and is thus much larger than any tortoise living in southern Namibia today.
80c - Diamantornis wardi
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Diamantornis wardi on stamp of Namibia 1995
MiNr.:790, Scott: 780.
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Fossilised eggshell fragments have been known to occur in the Sperrgebiet (forbidden territory) for many years,
but it was only in 1992 that the first complete eggs were found by the Namibia Palaeontology Expedition at Rooilepel.
At this site 30 kilometres north of Auchas Mine is an extensive cliff of hardened sand dunes 120 metres thick which
contain abundant fossil mammals as well as eggshells dating from about 16 to 17 million years ago.
The eggs of
Diamantornis wardi (Wards Diamond Bird) are one and a half times as voluminous as those of
the living ostrich (1,8 liters as opposed to 1,2 litres) and the shell is much thicker
(3 to 4 millimetres versus 1,2 millimetres), suggesting that the birds that laid them were appreciably larger
than the living ostrich.
90c Prohyrax hendeyi
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Prohyrax hendeyi on stamp of Namibia 1995
MiNr.: 791, Scott: 781.
|
At Arrisdrift, 35 kilometres upstream from Oranjemund, numerous fossils were found in an
abandoned channel of the Orange River during diamond prospecting activities.
The commonest mammals found at the site, dating from 17,5 million years ago, were large dassies
(hyraxes) the size of Dorper sheep.
In 1976, a particularly finely preserved skull was found and this formed the basis for the reconstruction
depicting on the stamp.
These dassies probably lived in herds along the floodplain of the proto-Orange River, much as the springbok today.
At that time, the environment in the Orange River Valley would have been considerably more luxuriant than it is today.
Apart from dassies, Arrisdrift has yielded many other species of mammals ranging in size from mice to elephants.
N$1,20 - Crocodylus lloydi
|
Crocodylus lloydi on stamp of Namibia 1995
MiNr.: 792, Scott: 782.
|
In contrast to the arid situation prevailing today in the lower Orange River Valley,
the environment was probably subtropical and the vegetation more luxuriant during the
Middle Miocene period 17,5 million years ago.
At Arrisdrift, many fossilised crocodile bones and teeth have been excavated
which indicate that the climate was on average warmer then than it is now.
The discovery of the complete skull and jaws of the
Crocodylus lloydi
revealed its similarity in shape and size to the Nile crocodile, the modern distribution
of which is restricted to the tropics and subtropics.
Many of the fossil mammal bones at Arrisdrift show evidence of having been bitten by crocodile,
which must have been one of the major predators in the valley.
The cachet of the FDC show fossil and reconstruction of
Orangemeryx hendeyi
During the Middle Miocene Period, an incredible variety of now extinct mammals comprising at
least 28 species lived in the proto-Orange River Valley.
One of the most peculiar of these was a large ruminant about the size of a gemsbok,
called
Orangemeryx hendeyi.
It belonged to the giraffoid group and possessed branched ossicones (antlerlike horns)
covered in skin.
It was probably a browser, preferring young shoots and leaves out of reach to other
herbivores but which it could exploit because of its long legs and neck.
Many of the
Orangemeryx fossils have tooth marks made by crocodile.
Products and associated philatelic items
FDC |
Mini-Sheet |
Examples of circulated covers |
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References
Acknowledgements:
- Many thanks to Dr. Peter Voice from Department of Geological and Environmental Sciences,
Western Michigan University, for reviewing the draft page and his valuable comments.