| Vertebrate Paleontology
Eudibamus cursoris
Dave Berman, Amy Henrici, Stuart Sumida
in the Bromacker Quarry
with colleague Rich Kissel
(second from right)
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Oldest known bipedal reptile
Since
1993, Carnegie Museum of Natural History Curator of Vertebrate Paleontology David Berman, PhD,
and Collection Manager Amy Henrici, along with colleagues Thomas Martens (Museum
der Natur, Gotha, Germany) and Stuart Sumida (California State University),
have been excavating the Bromacker Quarry, an abandoned sandstone quarry
in Germany.
The
Bromacker excavations have yielded fascinating specimens that provide
new information about the dominant life forms of the early part of the Permian period (290–250 million years ago), nearly 80 million
years before the Age of Dinosaurs. Major discoveries at the Bromacker
Quarry include the oldest known bipedal reptile, Eudibamus
cursoris, and other reptile and amphibian species that,
until now, were found only in the Permian deposits of the United States.
The scientific name for this new creature translates as "original
runner on two limbs"—an apt description of Eudibamus cursoris, the oldest known example of a bipedal reptile. Click here for the press release on this discovery.
The superbly preserved
skeletal remains suggest that Eudibamus could sprint upright on
its long, slender hind limbs, using its tail for balance. This evidence
comes from close analysis of the leg and arm proportions of the specimen. Eudibamus' upper limbs are relatively short, while its lower limbs
are comparatively long for its body size. These proportions are associated
with bipedal locomotion, as longer legs increase both an animal's stride
and overall speed.
Eudibamus cursoris
Illustration: Sandra Budd
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Why did this reptile
require such a swift foot? A diminutive herbivore like Eudibamus most likely used its speed to escape predators.
Compared to its contemporaries, Eudibamus belongs to a family of reptiles with an extraordinarily
large geographic range. Berman and his colleagues suggest that the combination
of lightning speed and herbivorous diet contributed to its widespread
success.
Groundbreaking Bromacker Discoveries
Until
their discovery in the Bromacker Quarry, the fossils listed below were
found only in Permian deposits of the United States. The similarity between
these European and American fossils provides undeniable biological evidence
that North America and Europe were once connected as part of a single
massive continent called Pangaea. Earth's continents sit on
a patchwork of interlocking plates, which have been in constant motion
over the past 750 million years. During the Permian period, all of the
plates were joined as the supercontinent Pangaea.
Diadectes absitus was an herbivorous reptile
approximately six feet in length. Previously known from fossils found
throughout the United States, Diadectes was one of the first Bromacker
animals that helped confirm the land connection between Europe and North
America. Trackways of Diadectes footprints occur commonly at the
Bromacker Quarry.

Seymouria sanjuanensis was a carnivorous amphibian
approximately two feet in length. Its presence at the Bromacker Quarry
provides the best biological evidence for the supercontinent Pangaea.
Berman has also collected this animal from rocks of similar age in New
Mexico; however, the Bromacker specimens are the most complete and best-preserved
examples of Seymouria.

Orobates pabsti, an herbivorous reptile approximately five feet in length, was also found.
This superbly preserved reptile is very closely related to Diadectes and represents the most primitive plant-eating land animal ever found.
A more slender body and limb bones distinguish this animal from Diadectes. Much remains to be discovered about this group, which is closely related
to the group of reptiles that gave rise to mammals.

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