A TIMELINE FOR THE PLANET click for Home Page
The fossil record is hopelessly patchy. Unfortunately it’s also the main source of
information for palaeontologists as they try to piece together ancient
events. You could have two populations
of identical beasts roaming around in two different areas. One we know about, and the other we
don’t. One left a good fossil
record. The other left little, or even
none at all.
This is why palaeontologists are constantly reminding
each other that “absence of evidence is not evidence of absence”.
The primitive mammals that came through the K-T
extinction (more) found an almost empty
environment just waiting for them to exploit more. Most of what we know about these animals
comes from
Another gap in the record covers the period between
the Ediacaran and Cambrian periods. Not one of the Ediacara creatures, or even
descendents thereof, seemed to have survived into the Cambrian period. This led to theories of a mass extinction to
end all mass extinctions. Now however a
jellyfish-like creature has been found from well into the Cambrian, which
palaeontologists are persuaded is a genuine descendent from an Ediacara
creature. Not only that but it appears
to be a genuine ancestor of modern comb jellies. Apparently comb jellies are an entire
‘phylum’ of animals, so this is big news.
The place to look for good fossil sites is the middle
of a large continent. Many of the most
exciting finds have been from
An area subject to plate tectonic activity, such as
Most fossils are bones which have been turned into
stone. This needs fairly special
conditions and most bones simply rot away.
I’ve not so far found a succinct description of how fossilisation
works. This may be because there are
many different types of fossil, and many different ways in which they can be
made.
So the following is the best I can do. To get fossilised, a bone needs to be buried
in gravel or some such. Then there needs
to be more similar material piled on top of it, until the layer with the fossil
in becomes compressed into sedimentary rock.
The bone needs to have mineral-rich water trickling over it. This is quite easy. As the rainwater trickles down, it dissolves
minerals from the pebbles and such that it passes over. As the mineral-rich water seeps into the
pores in the bones, some gets left behind.
The bony material gradually gets dissolved away at the same time. This leaves more pores to get filled with
mineral. And eventually the entire bone
becomes stone. The process may take
100,000 years or so.
The conditions for producing this kind of fossil is
actually quite common. So fossilised
bones are found all over the place, and are the mainstay of palaeontology.
But a fossil skeleton can only tell you so much. Fortunately conditions very occasionally
occur, in which much more is preserved.
For this the entire corpse needs to be buried in a mudslide or a bog, so
that all air is instantly excluded. If
all the air remains excluded for long enough, then the complete body can be
preserved. It may be squashed, and it
may have been swept away from where it died.
But you can get the most intricate details preserved for hundreds or
even thousands of millions of years.
These conditions are extremely rare. The early finds were entirely
accidental. First there was the Burgess
Shale, made famous by Stephen Jay Gould more. Next came the Ediacara Fauna, which came
from shortly before the Cambrian Explosion.
But then palaeontologists started to learn where to
look for such cornucopias. And now all
sorts of goodies are being found, such dinosaur feathers, dinosaur lungs and many others exciting
things.