Fossils
Window to the past
Freezing
What is freezing ?
This type of fossilization preserves an organism wholly without any
significant alteration to the chemical composition of the organism. The
parts of the organism that are usually preserved are muscles, tendons,
and skin. Generally in a typical fossilization the hard parts of the organism
are preserved by replacement of the organism's soft parts by other stable
organic materials or mineral substance from the environment. This type
of fossilization requires special circumstances to preserve the soft organic
parts by encompassing the organism in an inert environment to prevent any
or little changes within the organism. Freezing is one of the ways to slow
down the decomposition of the soft parts.
What are the conditions for freezing
?
So how did organisms situate themselves into such circumstance for millions
of years? Assuming that the organism is an animal, it probably first fell
into a "melted-out ice" crevice and found themselves entombed
in a fatal and "freezing" predicament. A common example of such
fossilization is a woolly mammoth frozen in a permafrost region of Siberia
and Alaska. They probably died during the late Ice Age. Rarely paleontologists
come across mastodons, woolly rhinoceros, horses, moose, bison, musk oxen,
and other animals.
Index
Amber || Casts & Molds
|| Compactions || Compressions
|| Coprolites & Gastroliths
Drying & Dessication || Freezing
|| Impressions || Molecular
Fossils || Permineralization
Reference || Trace
Fossils || Wax & Asphalt
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