
Tyrannosaurus rex and its
prey, a fallen Triceratops—a
detail from a 1998 mural by artist M.W. Skrepnick.
The full mural is displayed in Carnegie Museum
of Natural History’s Dinosaur Hall.
By R.J. Gangwere
Carnegie Museum of Natural History is known locally
and internationally for its research in biodiversity.
Each year, the museum sends scientists into the field
to locate and identify all the living species in a
particular area, and to examine how living plants and
animals relate to each
other. Its “Bioblitzes”—24 hours
spent in Pittsburgh’s parks, studying all the
plants and animals—have turned up 1,200-1,800
species each year for several years. And week-long “BioForays” at
the museum’s Powdermill Nature Reserve have studied
the ecological relationships among many species. Internationally,
the museum’s department of Invertebrate Zoology
(insects) is on a five-year mission with Harvard University
and the Smithsonian to document threatened native species
on the island of Hispaniola—a Caribbean environment
where some flora and fauna are on the brink of extinction.
Soon, the museum’s expertise in biodiversity
will be showcased for all the world to see in a collection
of exhibits called Dinosaurs in Their World, which
is driving the museum’s biggest expansion since
1907. In fact, Carnegie Museum of Natural History
expects the “world” aspect of its new
display—the
ecological environments in which dinosaurs lived—to
be a tourist attraction for dinosaur lovers everywhere,
and one that will draw visitors to Pittsburgh.
“The idea for Dinosaurs in Their World came
to us when we reacted to the way the American Museum
of Natural History recently restored its dinosaur halls,” says
Bill DeWalt, director of Carnegie Museum of Natural History. “They developed
their permanent halls around the scientific method of evolutionary descent [or
cladistics]—explaining how you differentiate one kind of vertebrate from
another. It’s scientific in a way that I think only a very small percentage
of the public can get much benefit from.
“
We are trying to do something more appealing to a greater percentage of the public—that
is, put dinosaurs into their world and emphasize biological diversity and how
that changes through the years, rather than how dinosaurs evolved one from another.
Ours is a more ecological approach.”
“
Dinosaurs in Their World is about more than just the animals and plants that
make up the ecosystem,” says Curator of Vertebrate Paleontology Chris
Beard. “It’s
really about the world itself, which was evolving and changing under the
feet of the dinosaurs. At the start of that time, modern continents did not
exist
but were all part of a giant land mass that scientists call ‘Pangaea’ [all
earth]. Before we even talk about the plants and animals that made up the
biodiversity of the dinosaurs’ worlds, the museum has to talk about
those different worlds themselves.”
The subject is hard to grasp. With
an expected lifespan of 60 to 80 years, a recorded “civilized” history
that dates back only 5,000 years, and humanoid ancestors that evolved a
mere three million years ago, the average person
has a limited sense of the time involved in evolution. It takes a geologist
or a paleontologist to comprehend the nature of life on Earth when the
Age of Dinosaurs
began some 248 million years ago and ended about 65 million years ago.
To help us, geologists have divided that long period of the Mesozoic Era
into three different worlds or periods:
the
Triassic, the Jurassic, and the Cretaceous. Dinosaurs in Their World will
represent each
of these periods in its exhibits. Those exhibits will start by explaining
the climate and geology of the period, and then focus on one particular
area where
the scientific collections are excellent and the history of fieldwork by
the museum provides special expertise.
Then, as now, plants of all types
were dominant in terms of sheer biomass, both on land and in the sea.
In addition, the myriads of insects, spiders,
crustaceans, and similar animals are not fully seen in the fossil record.
The
Triassic (248 to 206 million years ago)—42
Million Years of Transition
The Age
of the Dinosaurs was held together at the ends by
two great
mass extinctions of life forms. The “Permian
Extinction” of
248 million years ago set the stage, killing off
over 90 percent of living species in the
seas and on land. What caused this extinction has long been debated,
but there is no argument that the global climate
became inhospitable or toxic to life.
Still, some
marine and terrestrial species survived, and
reptiles began to adapt to the world of the Triassic
Period. Early dinosaurs
appeared
in a
landscape much different from today’s. It was a transitional
period, extremely hot in the middle of the giant land-mass, with
smoking volcanoes and ever-widening
oceans beginning to separate the land into continents. For 42 million
years, this first world saw the progressive breakup of Pangaea
into large pieces, which
is the basis for the theory of Plate Tectonics. As the separate
continents came to exist, terrestrial species began to differentiate
themselves
on each of them.
For the Triassic Period, the Dinosaurs in Their World exhibit will focus on Ghost Ranch, New Mexico, where Carnegie
Museum of Natural
History
Paleontologist Dave
Berman conducted extensive fieldwork in the 1980s, producing
extraordinary collections for the museum. Ghost Ranch
is one of the best North
American sites
of the Triassic
Age, and the museum can tell the story of which animals lived
there, and what life and the ecosystems of that period
were like.
One of the earliest North American dinosaurs
from this period, which lived about 220 million years
ago, was the fast and agile
dinosaur
Coelophysis, a predator
that probably hunted in packs, with powerful rear legs and
razor-sharp teeth. Botanically, plants began to differentiate
during the Triassic Period, and fern-like plants and
conifers developed.
Curator
Zhexi-Luo also points out that the evolutionary line of mammals
began in this period. “Anatomically defined mammals
appeared about the same time as anatomically defined dinosaurs,” explains
Zhexi-Luo, who also serves as interim associate director
of research and collections. “There
is always this shared history of mammals and dinosaurs.”
Luo’s
work in China has yielded some of the earliest mammal fossils,
which were very small at the start. One example
is Hadrocodium, a large-brained but
tiny
creature the
size of
a paperclip,
from the Early Jurassic, and another is the 6-inch, one-ounce
Sinodelphys, the most
primitive ancestor of marsupials (animals with pouches for
raising young). He notes that in the fossil collection is
a Phytosaurus— “A very interesting
animal that put its body and head in the water, and had a
volcano-like nostril on the dorsal side of its head. These
are common from the late Triassic time,
when the dinosaurs originated. And there were lots of crocodiles—and
we have a fine fossil of a baby crocodile from the Triassic.”
The Jurassic (206 to
144 million years ago)—High
Tide for Dinosaurs
Biodiversity in the
long Jurassic Period (about 62 million years) included
the development
of flowering plants. The familiar gingko
tree is one species that survives from this period.
In the air, winged lizards (Pterosaurs)
began to glide, and true birds with feathers began
to evolve from the scales of animals.
To
tell the Jurassic story, the museum has excellent
fossil collections from Dinosaur
National Monument, which Carnegie Paleontologist
Earl Douglass
discovered in 1909. That incredibly rich
site of dinosaur fossils was declared
a national
monument in 1915 by President Woodrow
Wilson, a friend of Andrew Carnegie’s,
and the Carnegie Quarry continued to
operate
there
until 1923. Today the 200,000-acre national
monument extends into Colorado.
Many
of Carnegie Museum of Natural History’s
most dramatic specimens come from this
amazing “bone
bed,” which yielded 20 mountable
skeletons representing 10 different species,
including
the long-necked, long-tailed, plant-eating
sauropods: Apatasaurus, Diplodocus, and
Camarasaurus.
Stegasaurus, with its high backbone
plates, and Allosaurus, the
abundant predator and dominant meat-eater
of its day, likewise come
from Dinosaur National Monument.
The Cretaceous and Extinction
(144-65 million years ago)
Tyrannosaurus
rex, the classic predator and scavenger, evolved
during the Cretaceous Period,
as did another popular dinosaur, Torosaurus,
a plant-eater with long horns and a giant
frill over its eyes.
In the Cretaceous hall of
exhibits, the museum will focus on Lance Creek, Wyoming,
where its Triceratops specimen originated,
and talk about
the work of John Bell Hatcher (“Mr.
Triceratops”),
one of the museum’s most famous
curators from the early 20th century.
Triceratops was one of the last dinosaurs to live
in North
America, and its head was one of the
biggest of any land mammal, with long
horns, hooked
snout, and wide, shield-shaped frill.
The coastal deltas were the home of plant-eating
Triceratops 67 million years ago in what
is now the Great Plains, but then was
covered by a shallow sea. On these huge
deltas,
Triceratops’ home
resembled the warm, wet bayou country
of our modern Gulf Coast. Grass had not
yet evolved,
but the new flowering shrubs that Triceratops ate and the trees that shaded it were
early cousins of today’s plants.
Sequoia, sassafras, and relatives of
the fig grew
here in lush
thickets and groves. Many species of
reptiles, mammals, and birds had evolved
into familiar
forms, and rivers were full of fish:
stingrays, perch, gar, and bowfin, along
with turtles and frogs whose descendants
live today.
In fact, an entire part of
the Cretaceous gallery will be devoted
to the Cretaceous
North American
marine seaway, the vast shallow sea that
extended across the middle of the North
American continent,
covering places that we now know as Kansas,
South Dakota, and Nebraska. This seaway
teamed with marine life, including Mosasaurs (great
lizards that returned to the oceans to
swim), Icthysaurs (fish-like reptiles
that no longer
exist, but that looked like sharks and
dolphins), and Plesiasaurs (the long-necked
reptiles that
gave rise to the Loch Ness monster story).
The
most famous, if not the largest, of all mass extinctions
marks the end
of the Cretaceous
Period, 65 million years ago. One theory
contends that a giant asteroid hit the Earth
near the Yucatan
Peninsula in Mexico, sending debris
into the atmosphere that affected the
photosynthesis
process globally, ending much plant
life and
the animals that depended upon it.
This was the great extinction in which the dinosaurs
died out.
But while many species disappeared,
including marine reptiles and flying
pterosaurs,
there were other groups—such
as flowering plants, snails, and clams,
amphibians, snakes, lizards,
mammals, and crocodilians—that “crossed
the boundary” of the great extinction
to live on and flourish in more modern
times.
Show Me the Fossils
The best proof of what
the world of the dinosaurs was like is to
be found
in
the rare fossil
evidence that only a few museums possess.
All the overwhelming popular attention—the
publicity, the games, and the movies—depends
on this real fossil evidence, and Carnegie
Museum of Natural History, with its
100 years of research
and collections,
has some of the best evidence to be
found anywhere.
Says Carnegie Museum
of Natural History Curator Emeritus
Mary Dawson, “These are animals
that once lived, breathed, walked around,
ate, reproduced, and died—what
can be more astounding than being in
a room with 12 or
13 of such animals that were once alive?
Seeing the real thing is important
for people who
really have an appreciation for life,
for the past, and for the future. That
you get from
originals. You don’t get it from
copies. A plaster cast is just an artifact.
It is not
a fossil.”
Dawson’s associate
at the museum, Curator David Berman,
explains that most people do
not know how rare such fossil evidence
is. “Most
reconstructed dinosaur skeletons, like
our own famous Diplodocus, are composites—made
up of the bones of several animals.
Having one complete specimen, like
our juvenile Camarasaurus,
is extraordinary.” Chris Beard
adds that no matter how much money
a museum has today,
and how badly it may want the real
thing, it’s
usually impossible. “If you want
the Mona Lisa, that object cannot be
obtained because
it hangs in the Louvre,” Beard
says. “We
have our own Mona Lisas in Dinosaur
Hall.”
Dinosaurs in Their World will feature abundant fossil evidence
of the biodiversity
on land
and at sea throughout the Mesozoic
Era. And its exhibits will, of course,
include
great
models, reconstructions, dramatic
graphics, and a small theater.
But who are the real
stars of the show? The fossils. Large or small,
plant
or animal, each
is evidence of the real worlds
that existed millions of years before
us.
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