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About
Insect Fossils
Modern
insects are among the most diverse of animals, with more
than million species described and represent more than half
of all known eukaryotic organisms. The actual number of extant
species is estimated at between six and ten million, and
occupy essentially all terrestrial Insects, and have even
adapted to multiple environmental niches during their complex
developmental life cycles.
Fossilization
of insects is relatively rare event, normally needing anoxic
conditions (without oxygen
and lacking aerobic
bacteria) such as occur in silty lake bottoms. Exquisite
insect fossils are particularly known from Lagerstätte
sites such as the Eocene Green River formation and Carboniferous
Mazon Creek in the US, the Cretaceous Liaoning Province in
China and Crato Formation of Brazil, and the Jurassic Solnhofen
Limestone of Germany. Like other Arthropods, insects have
an
external skeleton called an exoskeleton, but it is thin and
composed of chitin, along with a tough protein that poorly
fossilizes.
Class
Insecta has nonetheless left a prodigious insect fossil record
owing to their tremendous reproduction
rate. Their
fecundity is a powerful evolutionary mediator, fostering
rapid adaptation and survival
during those geological periods of rapid change known as
extinction events.
The
oldest insect fossil is Rhyniognatha from the Rhynie Chert
of Scotland that is estimated to be
some 400 million
years
old. Because it already had mandibles, a prominent characteristic
of winged insects, it has been inferred that first insects
likely appeared much earlier during the Silurian.