by
Paul Sereno

Photo
by Paul Sereno
The claw on the hand of this predator
was probably
10 inches long in life with its
horny covering.
Asia's
Cretaceous Meat-eaters
Asia's most famous Cretaceous
meat-eaters are all tyrannosaurs.
And like the most famous North
American tyrannosaur, Tyrannosaurus
rex, they all lived during
the Late Cretaceous. The most
common was Tarbosaurus,
a huge predator and close cousin
of T. rex.
Little
is known about the large predators
that roamed Asia's Cretaceous
world before the "tyrant" meat-eaters
rose to dominance. The first clues
were unearthed 40 years ago along
the eastern edge of the Alashan
Desert in Inner Mongolia by the
Sino-Soviet Expedition. Jaws and
powerfully-built forelimbs with
huge sickle-shaped claws were
unearthed and named Chilantaisaurus,
an Early Cretaceous predator.

Two
pieces of the jaw that fit together
and encase several sockets and
teeth
of a new, large-bodied predator.
The
red and green rocks that compose
the buttes and ridges surrounding
Camp II date back to the Early
Cretaceous.
"There
it is, whew!" Paul said as he
panted a little from the climb.
Paul lifted a 5-inch hand claw
from the surface. Brushes and
awls whirled, as several team
members followed the bones of
the forelimb into the rock. This
was no Chilantaisaurus.
The claw, although robust, was
not an enormous, highly recurved,
sickle-shaped bone. Yet, it and
the other bones of the hand we
exposed clearly did not belong
to the diminutive forelimb of
a tyrannosaur. Was it a relative
of North America's high-spined
meat-eater Acrocanthosaurus?
Unfortunately, the bones of this
new predator were extremely fragile.
We could not clean them further
in the field without risk of damage.
Our curiosity must wait until
the jackets are opened and the
bones properly exposed in the
lab!

This
tooth, with serrations on only
one of its edges, reveals the
presence of a dromaeosaur, a small
Deinonychus-like predator.
Small
predators were also present in
the Early Cretaceous, and we began
to find their teeth and fragile
limb bones in great numbers. One
tooth type was common and peculiar;
it had serrations only on one
of its edges. That kind of tooth
belongs to a dromaeosaur, a family
of sickle-toed predators that
includes Velociraptor,
known from Late Cretaceous deposits
elsewhere in the Gobi. Another
tooth type from a large predator
was also common and similar to
that in the jaws of Acrocanthosaurus.
Ancient
injury

Unlike
5-toed humans, two-legged dinosaurs
stand on only three toes,
the middle one always the longest.
Dave has an extraordinary knack
for finding footprints. "Did you
just stumble on it? I mean, how
did you find it?" we questioned
him as we gazed down at the three-toed
footprint cast. When you have
bones in mind, you can easily
walk right over anything else.
But Dave often has footprints
in mind, especially when he sees
a ledge-forming sandstone. He
went looking for footprints, overturning
heavy slabs of rock.
The
footprints he discovered were
casts made by sand that infilled
a deep trackway in mud made by
a large two-legged dinosaur. Compared
to a human foot, the print was
huge, its three toes broadly splayed.
The toes of the print were broader
than those commonly made by predators,
suggesting that the trackmaker
was a large ornithopod, something
like Iguanodon . We had
one in mind, a large ornithopod
called Probactosaurus,
first described from similar-aged
rocks on the opposite (east) side
of the Gobi's Alashan Desert.
The space between each print allowed
Dave to measure its stride-length.
Not
more than a stone's throw away,
Andy spied the ribs of a skeleton
protruding from the wall of the
valley. Soon we had exposed enough
of its bones to identify it as
an ornithopod, perhaps a close
relative of Probactrosaurus.
Could it have been the trackmaker?
Perhaps. It's rare to find tracks
and a potential trackmaker in
the same beds, because the conditions
for preserving prints and bones
can be quite different.
The
swollen woven bone on this rib
shaft, compared to that of a normal
rib, marks the site of an ancient
injury which this dinosaur survived.
The
ribs grabbed our attention for
another reason-a section of the
shaft of one of the ribs was swollen.
Looking closer, we could see that
the enlarged shaft was made of
woven bone that forms after an
injury. This ornithopod had suffered
a broken rib! The natural repair
of a broken bone means that the
dinosaur survived the accident,
dying later for other reasons.
The fossils really came alive
for us when we saw such vivid
evidence of dramatic events in
the life of a dinosaur, that took
place more than 100 million years
ago.
Puzzling
turtles
The pea-green color of the rock
and the presence of flaky shales
gave us the idea that we were
about to prospect an ancient swamp
or marshland. Shales are made
of mud laid down in quiet environments
located at some distance from
the churning water of a stream.
Chipping away at the shale with
his rock hammer, Fabrice found
twigs that had turned into black
coal embedded in the layers.
Minutes
after leaving on our first prospecting
session, several team members
found bones of what we soon would
learn was a common swamp inhabitant-turtles.
Pieces of shell and limb bones
littered the valleys.
Professor
Zhao reported finding most of
a skeleton. We followed him back
to the site, as he quickly scaled
a butte more than 100 feet in
height. Incredible! The man is
66 years old and is prospecting
the top of the tallest butte in
the area! His turtle was spread
over several square feet. We were
amazed at how many bones of the
skeleton we were able to find,
plucking the tiniest toe bones
(called "phlanges") from the eroded
surface.
"Here's
a claw!" shouted Jeff with delight,
holding the quarter-inch long
bone between two fingers. All
of us had encountered turtle bones,
but no one had found one, as it
was in life-- shell intact. These
turtles were just too delicate,
their shells made of dozens of
individual plates that seemed
to drift apart after death in
the mud of the swamp.
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