Water Reptiles of the Past and Present — John Shaqi
Water Reptiles of the Past and PresentWilliston, Samuel Wendell
Science
Water Reptiles of the Past and Present
Williston, Samuel Wendell
Aquatic reptiles; Aquatic reptiles, Fossil
From the uppermost Cretaceous beds of America, the Lance, Judith
River, or Belly River beds as they are variously called, have come
the remains of a marvelous reptilian fauna. These beds may be grouped
together though not all contemporaneous, and there is dispute about
their age, some excellent paleontologists insisting that the uppermost
are really of Eocene age. From Colorado east of Denver, from eastern
Wyoming, from Montana, and especially from the vicinity of Edmonton
in Canada, as also occasionally in western Texas and New Mexico,
have come many marvelous specimens of dinosaurs, huge bipedal
carnivorous dinosaurs, great spoon-billed aquatic dinosaurs, armored
stegosaurian dinosaurs, and many kinds of the great horned dinosaurs,
the Ceratopsia, so far known only from these beds. Here at the very
close of the Age of Reptiles, at the close of the Age of Dinosaurs,
are found the ultimate specializations of all the chief groups of
dinosaurs except the long-necked quadrupedal dinosaurs which gave up
the ghost in Lower Cretaceous times. Many were provided with horns and
spines, some indeed seemed to have bristled with spines throughout,
a sure sign that they were approaching the end of their career. The
modern type of crocodiles had usurped the ancient forms of the early
Cretaceous, and reached the largest size of their race perhaps, though
but few specimens are known. Here also in these beds we find the
first representatives of lizards and snakes in America, though snakes
have been described from earlier strata, perhaps, in Brazil. Those
archaic, old-fashioned rhynchocephalians described on a later page as
the Choristodera appeared also for the first time in these beds, and
persisted for a little while in the Eocene, in Europe and America. And
with all these there has very recently been described the last of the
plesiosaurs, whose race went out with the dinosaurs at the very close
of the Mesozoic. It is needless to say that the turtles also occur,
for, as a general rule, wherever vertebrate fossils are found, in rocks
of the land or the sea, marine or fresh-water, there will be some bones
of turtles among them.
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