DINOSAUR, any member of a group of about 350
well-known genera of archosaurian reptiles that first
appeared in the late Middle or early Late Triassic
period, about 200 million years ago. They comprise two
orders, the "bird-hipped" Ornithischia and the
"reptile-hipped" Saurischia. The earliest known
dinosaurs, such as Staurikosaurus and Herrerasaurus
from South America, are too primitive to be classified
within either order.
Dinosaurs arose at a time when the land was
dominated by crocodilelike phytosaurs (see
PHYTOSAUR), giant amphibians and archosaurian
carnivores, and large therapsids (see THERAPSID).
The first dinosaurs were small, lightly built, bipedal
carnivores or omnivores that were probably quicker and
more agile than their contemporaries, most of which
became extinct by the end of the Triassic period. During the Jurassic period
and
Cretaceous period the dinosaurs evolved into myriad adaptive types, many
of which
reached colossal size, including Argentinosaurus, a long-necked vegetarian
weighing about 100 tons, 20 tons more than Seismosaurus, another sauropod
previously thought to be the heaviest dinosaur; and Gigantosaurus carolinii,
a land
carnivore of about 8 tons. Both of these dinosaurs roamed South America
30 million
years before Tyrannosaurus rex, their carnivorous North-American counterpart,
came into existence.
Remains of dinosaurs were first discovered in England in the 1820s. By
the 1840s
several genera were well enough known that the great comparative anatomist
Richard Owen gave them the name Dinosauria, a term coined from the Greek
words
deinos, "terrifying" and sauros, "lizard." In doing so, he recognized the
uniqueness
of their great size, their terrestrial habits, their upright posture, and
the inclusion of
at least five vertebrae in their hip girdles. It was not, however, until
the exploration of
the western U.S. in the 1880s and after the recovery of complete dinosaur
skeletons
from the badlands there that dinosaurs were recognized as having been largely
bipedal?a most unusual stance for a reptile, and one that led to much speculation
about their locomotion, behavior, and physiology.
In the 1880s, H. G. Seeley (1839?1909) saw that Dinosauria could be divided
into
two groups based on the form of the hip girdle. The Ornithischia had pubic
bones
that, like those of birds, faced posteriorly. The more conventional Saurischia
had
pubic bones that faced anteriorly. Ironically, it was the "reptile-hipped"
Saurischia
from which birds evolved, specifically from small carnivorous dinosaurs
related to
Deinonychus and Compsognathus. The reversal of the pubis was an evolutionary
convergence in birds and ornithischians.
Dinosaurs are distinguished by an erect posture in which the limbs are
brought
more or less under the body in the fashion of birds and mammals, rather
than
sprawling to the side as in crocodiles, lizards, and turtles. They share
this
characteristic with pterosaurs (see PTEROSAUR), their closest relatives,
as well as
with their descendants the birds. Their footprints show that the bipedal
dinosaurs
walked as birds do, putting one foot in front of the other, toed slightly
inward. Their
hands were prehensile, with thumbs somewhat opposable to the other digits.
Their
brains were generally larger than average for reptiles, particularly in
the carnivores
and duck-billed dinosaurs.
Ornithischian Dinosaurs
The earliest ornithischians include the poorly known Triassic form Pisanosaurus
from South America, and Early Jurassic genera such as Heterodontosaurus
and
Scutellosaurus. By the Early Jurassic the ornithischians had already split
into
several major lineages. One lineage, known collectively as Thyreophora,
includes
the plated stegosaurs and the armored ankylosaurs, and ranges from the
Early
Jurassic through the Late Cretaceous. A second group, the Ornithopoda,
includes
the duck-billed hadrosaurs and their relatives the iguanodonts, as well
as the horned
ceratopsians and their relatives the pachycephalosaurs. The Ornithopoda
also
ranged from the Early Jurassic through the Late Cretaceous.
Ornithischian dinosaurs are distinguished by their "birdlike" hip girdles,
and also by
the presence of a predentary bone on the tip of the lower jaw. All ornithischians
were herbivorous, and the predentary bone appears to have served, much
like the
incisors of camels and horses, to crop vegetation. It also connected the
two halves
of the lower jaws and enabled them to transmit and absorb force during
chewing. In
duck-billed dinosaurs and ceratopsians, the jaws held dozens of teeth tightly
arranged to form a single beveled battery of chewing surface. As in all
other
vertebrates except mammals, the teeth were continually replaced through
life as the
roots were resorbed and new crowns developed.
Saurischian Dinosaurs
Saurischian dinosaurs include two major groups: (1) the herbivorous
Sauropodomorpha, which comprise the giant, long-necked Sauropoda such as
Diplodocus and Apatosaurus, plus the less-well-known Prosauropoda, which
include
Plateosaurus; and (2) the carnivorous Theropoda, which comprise all the
large and
small meat-eaters from Coelophysis, Compsognathus, and Deinonychus up through
the giant meat-eaters such as Allosaurus and Tyrannosaurus, as well as
their
descendants the birds. Larger, bulkier sauropods, called Supersaurus and
Ultrasaurus, which are related to Brachiosaurus or Diplodocus, have been
found in
Colorado.
Saurischians have long necks and large claws on the first digits of their
hands and
feet; the fourth and fifth fingers of the hand are reduced or absent (as
in birds, which
retain only the first three digits). The sauropods became very large and
quadrupedal,
and evolved some interesting adaptations for feeding on high vegetation.
In
Diplodocus, for example, the neck and tail are both very long; the lower
(haemal)
arches of the tail vertebrae, at the point where the tail would normally
reach them,
are canoe-shaped instead of tongue-shaped, and appear to have assisted
the
animal in using the tail as a prop for the hindlimbs in a tripod stance
as it fed on
high vegetation, with its forelimbs raised off the ground. In Brachiosaurus,
by
contrast, the neck is very long but the tail is short, so the tripod stance
was
impossible; however, Brachiosaurus had forelimbs that were longer than
its
hindlimbs, and this length plus the long neck enabled it to reach high
vegetation by
different means than Diplodocus used.
Large carnivorous theropods such as Tyrannosaurus had very large heads
with great
jaws filled with recurved, doubly serrated teeth. Their forelimbs were
reduced but
their hips and hindlimbs were massive, and clearly the predator had little
to do
beyond grasping its prey in its jaws, planting its feet, and tearing and
ripping the
flesh until the prey suffered massive shock and blood loss. Smaller theropods
such
as Deinonychus must have been much more agile hunters that chased down
prey
and attacked in packs, ripping with teeth and claws. However, some lineages
of
small theropods, such as Struthiomimus and its relatives, were toothless,
as were
all but the first birds (see; HESPERORNIS) and may have been more omnivorous
in
their habits.
Warm-Bloodedness
Were the dinosaurs warm-blooded? The evidence is mixed. Like birds and
mammals, dinosaurs had rapid rates of growth, and their bones show evidence
of
secondary reworking (Haversian canal systems). They could not sprawl like
most
living reptiles, and their obligate erect posture implies continual expense
of
metabolic energy. Their footprints and long limbs show that they were capable
of
high speeds. In addition, the birds, which are technically living dinosaurs,
are
warm-blooded. Probably no single thermal strategy can describe all dinosaurs:
In
these respects such mammals as bats, cats, elephants, and whales differ
considerably, and the dinosaurs were probably equally varied. New evidence
that
dinosaurs were warm-blooded and that their brooding behavior was similar
to that of
modern birds came with the 1995 discovery of the remains of a nesting dinosaur
in
the Gobi Desert. The 8-foot-long ostrichlike dinosaur of the genus Oviraptor
was
found with its legs folded beneath its body and its forelimbs surrounding
a clutch of
at least 15 eggs.
Extinction
Dozens of explanations for dinosaurian extinction have been offered, most
of them
fanciful or outside the resolution of evidence. Until recently dinosaurs
were
considered to have died off gradually through the Late Cretaceous. The
recent
discovery at the Cretaceous-Tertiary boundary of the rare element iridium
and of
shocked quartz granules, both signatures of the impact of a large asteroid
or comet,
fueled speculation that such an impact could have triggered climatic catastrophes
that ended the dinosaur?s reign. Although such events, which are known
to be
common in geologic history, might have had some environmental consequences,
the vast majority of dinosaurs were long extinct by that time. Moreover,
other
organisms such as crocodiles, turtles, fishes, birds, and amphibians, which
might
have been expected to suffer equally from such a cataclysm, survived with
only
minor losses?a pattern that has yet to be explained by any catastrophe
hypothesis. It is known that through the Late Cretaceous the climate was
becoming
more unstable and seasonal, and waves of extinctions had long been affecting
both
marine and terrestrial life. Although the effects of extraterrestrial impact
cannot be
ruled out, they do little to explain the observed evidence of extinction
and survival at
the end of the Cretaceous.
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