Description:
This beautiful and striking Mammuthus primigenius molar comes directly
from the vast, harsh wastelands of Siberia. The preservation is
remarkable and natural mineral replacement processes in fossilization
that resulted in a spectrum of light brown hues. At almost 7 lbs
(2.960 kg), its as heavy and dense as the rock it became since tens
of thousands of years ago when humans were still roving bands of
hunter gatherers. The woolly mammoths met extinction at the end
of the Pleistocene (12,000 years ago), probably as a result of climate
change together with the effects of human hunting.
The molars of the woolly mammoth, like those of other mammoths
and elephants were large, specialized structures with a flattened
grinding surface. Low ridges of dense enamel run across the surface
of the teeth, making them ideal for grinding grasses. As with mastodons,
a mammoth will have a series of six cheek teeth (premolars and molars)
on each side of the jaw (a total of 24 teeth for both upper and
lower jaws.) Younger mammoths had three teeth on each side, while
most adults had two, and the old animals had one. As the teeth were
worn down, they were replaced by teeth growing in from the back.
Newer teeth were larger and contained more ridges than older teeth.
I also
need to dispel self-serving disinformation I’ve seen on the
Internet regarding Mammoth teeth from Siberian sedimentary deposits,
compared with those brought up from the sea. The former are clearly
more aesthetic, and the natural preservation and structural integrity
has not been compromised by the adverse chemical effects and dissolution
during sea water submersion as in the latter. The former smells
like the rock that it is and the latter smells like the hydrocarbons
required to restore structure integrity with many shellac-like coating.
At the 2008 Tucson Fossil show, the former were scarce and relatively
expensive, and latter were prevalent and pretty inexpensive. Pitching
fossils as investments reminds me of the coin and pawn shop near
where I grew up. If I thought fossils were good investment vehicles,
I would recommend Mammoth teeth from Siberia, so don’t be
duped by the disinformation. The Mammoth teeth from the North Sea
are just fine, especially since they should be a bargain compared
to those from Siberia, if you don’t mind the smell. The Siberian
teeth are also safer around small children.
We’ve
also seen a suggestion that preservation with burial in frozen Siberia
somehow equates to that on the sea floor. A non-scientist can deny
this silly hypothesis by asking whether the Titanic would look better
if buried in Siberia. The markedly different chemical conditions
lead to concomitantly differential chemical processes and mineral
exchange during fossilization, the complex processes where organic
material becomes, yes, stone. We do agree that melted ice becomes
water, however, contracting in volume during that phase change below
0.0 degrees centigrade. As for the toxicity problem noted above,
adequate protection can probably be acquired by an extra heavy coat
of glossy black enamel, though this may collaterally comprise surface
details and hide the natural hues through absorption of all frequencies
of the visible electromagnetic spectrum. Then again: “how
many ways can you arrange the deck chairs on the Titanic? –
answer: who cares?
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