The
geological time scale is marked by significant geological and biological events, including
the origin of the earth about 4.6 billion years ago, the origin of life about
3.5 billion years ago, the origin of eukaryotic life-forms about 1.5 billion years ago, and the origin of animals about 0.6 billion years ago.
The latter event marks the beginning of the Cambrian period. Animals
originated relatively late in the history of the earth—in only the last 10%
of the earth’s history. During a geologically brief 100-million-year
period, all modern animal phyla (along with other animals that are now extinct)
evolved. This rapid origin and diversification
of animals is often referred to as “the Cambrian explosion”.
Scientists
have asked important questions about this explosion since Charles Darwin. Why did it occur so late in the history of
the earth? The origin of multicellularity seems a relatively simple step compared to
the origin of life itself. Why do no
fossil records document the series of evolutionary changes during the evolution
of the animal phyla? Why did animal life
evolve so quickly? Paleontologists
continue to search the fossil records for answers to these questions.
One
interpretation regarding the absence of fossils during this important
100-million-year period is that early animals were soft-bodies and simply did
not fossilize. Fossilization of
soft-bodied animals is less likely than fossilization of hard-bodied animals,
but it does occur. Conditions that
promote fossilization of soft-bodies animals include very rapid covering by
sediments that creates an anoxic environment that
discourages decomposition. In fact,
fossil beds containing soft-bodied animals have been known for many years.
The
Ediacara fossil formation, which contains the oldest
known animal fossils, consists exclusively of soft-bodied forms. Although named after a site in
A
slightly younger fossil formation containing animal remains is the Tommotian formation—named after a locale in
A
third fossil formation containing soft-bodied animals provides evidence of
the results of the Cambrian explosion. This
fossil formation, called the Burgess
Shale, is in
Fossil
formations like the Burgess Shale show that evolution cannot always be thought
of as a slow progression. The Cambrian
explosion involved rapid evolutionary diversification, followed by the
extinction of many unique animals. Why
was this evolution so rapid? No one
really knows. Many zoologists believe
that it was because so many ecological niches were available with virtually no
competition from existing species. Will
zoologists ever know the evolutionary sequence in the Cambrian explosion? Perhaps another ancient fossil bed of
soft-bodied animals from 600 million-year-old seas is awaiting discovery.