|
October
12, 2000
Camp 2
Gadafawa, North

Planning
the next day's activities often occurs after
sundown in light generated by solar-powered
lanterns.
Although it is desert
now, 110 million years ago the Sahara was
a wet, lush environment with huge rivers,
lakes and streams. Long clams, fish, and
crabs inhabited the banks; alongside lived
dinosaurs, pterosaurs, crocodiles and turtles.
We know these creatures lived here from
fossils we find. The rock records evidence
of great waterways in the way the sandstone
layers are cross-bedded.
Although the beds are
the same age as those we've been exploring
at Camp 1, we have very little idea how
rich, or poor, in fossils the localities
surrounding Camp 2 will be.
This is a classic moment
on an expedition: a small group of young
scientists sets out into uncharted geology
to survey an area known hitherto only by
brief descriptions and oral histories.
Here at Camp 2, the
outcrop has risen in relief, transmogrified
into a broken cliff line, burnt umber against
sand..
The Move North
As we journeyed north
from Camp 1, the desert shifted shape. What
was flat outcrop at Camp 1 has transformed
into a burnt umber cliff-line. What had
been sporadic dunes has become a never-ending
undulation. At the base of the outcrop,
white-tipped grass is thick and green.
On our
way up we passed two stocky, black Touareg
tents amidst hundreds of camels grazing.
Our camp is located in a cirque of barkhan
dunes, the highest of which overlooks the
outcrop to the East.

Sand dunes intermingle
with fossil-bearing rocks in the area
under exploration from Camp 2.
Paul calls our drives
into the outcrop a "cat and mouse game"
because the outcrop (exposed rock) intermingles
with dunes. As a result each time we make
a foray into a new area we are skirting
sandstone ledges (hard to drive over) and
sand dunes (easy to get stuck in). The point
of the game: reach the outcrop without getting
stuck in the sand, cut off by dunes, or
driving over sharp rocks.

A stripped-down
camp puts the kitchen between two trucks.
What is prospecting?
What is prospecting?
Looking for fossils. Some people might say
it is looking for something you think might
be there, but you don't know what it is
until you find it.
Once you are in an area
that is the right age (here the rocks
are 110 million years old, Cretaceous age)
and the right type (because dinosaurs
were land animals, we are looking at terrestrial
rocks; rocks that were formed on land),
you look for outcrop - areas where
the rock is exposed.

Prospecting
requires a keen eye - and an occasional
climb. Here, Greg explores steep sandstone
layers laid down by an ancient river.
To find a dinosaur -
or other fossilized animal - something needs
to be poking up out of the rock onto the
surface. Like hunters, paleontologists follow
a trail - fragments of bone traced to the
source.
Paleontologists may
be hunters, but they must be detectives
as well. Once you have found something,
how do you make sense of it? If you are
interested in more than a trophy or a mantelpiece,
you must learn to read clues the bones and
rocks hold, and to construct stories from
them. The full stories come from geology
as well as paleontology - rocks and bones.
What kind of animals
lived at that time here on Africa? How many
species? What was the diversity? How big
- or small - did these animals get? What
was the environment like when these animals
were alive? These are some of our initial
questions.
When we actually excavate
a site, we try to piece together the death
scenario as we excavate. When we are in
prospecting mode, like now, we are (literally)
scratching the surface to find out what
is here.
Next
|