456 CHAPTER 17
The other major diapsid group, the archosaurs, includes the most
spectacular and diverse of the Mesozoic amniotes. Most of the late
Permian and Triassic archosaurs were fairly generalized predators
1 m or so in length (FIGURE 17.25B). From this generalized body
plan, numerous specialized forms evolved. Among the most highly
modified archosaurs are the pterosaurs, one of the three major ver-
tebrate groups that evolved powered flight. The wing consisted of a
membrane extending to the body from the rear edge of a greatly
elongated fourth finger (FIGURE 17.25C). The pterosaurs diversified
greatly: one, with a wingspan of 11 m (36 ft), was the largest flying
vertebrate known, while others were as small as sparrows.
Dinosaurs evolved from archosaurs related to the one pictured in Fig-
ure 17.25B. Dinosaurs are not simply any old large, extinct reptiles, but
members of the orders Saurischia and Ornithischia, which differ in the
form of the pelvis. Both orders included bipedal forms and quadrupeds
that were derived from bipedal ancestors. Both orders arose in the Trias-
sic and became diverse in the Jurassic.
More than 39 families, about 550 genera, and well over 1000 species of
dinosaurs are recognized (FIGURE 17.26). The Ornithischia—herbivores
with specialized, sometimes very numerous, teeth—included the well-
known stegosaurs, with dorsal plates that probably served for thermo-
regulation, and the ceratopsians (horned dinosaurs), of which Tr ic e rat o p s
is the most widely known. Among the Saurischia, the sauropods, herbi-
vores with small heads and long necks, include the largest animals that
have ever lived on land, such as Apatosaurus (= Brontosaurus); Brachio-
saurus, which weighed more than 80,000 kg; and Argentinosaurus, which
reached about 40 m in length. Saurischians also included carnivorous, bipedal
theropods, such as Velociraptor, the renowned Tyrannosaurus rex (late Cretaceous),
which stood 15 m high and weighed about 7000 kg, and many smaller theropods.
All dinosaurs became extinct at the end of the Cretaceous except for a single group of the-
ropods. They radiated extensively in the Cenozoic and today include about 10,000 species
that we know as the birds. Aside from birds, the only living archosaurs are the 22
species of crocodilians.
The late Paleozoic also included the synapsids (see Figure 17.24), with a single
temporal opening. They gave rise to the therapsids, sometimes called “mammal-
like reptiles,” which flourished until the middle Jurassic, and gave rise in the late
Triassic and early Jurassic to forms that are almost fully mammalian in their features
(see Chapter 20). Many clades of mammals, including more than 300 known gen-
era, arose and became extinct in the Jurassic and especially the Cretaceous (FIGURE
- 27). Although most were small in size, many were ecologically and morphologi-
cally specialized, and convergent with living mammals that evolved similar traits
independently (FIGURE 17.28) [56]. Only three of the many Mesozoic mammal
Futuyma Kirkpatrick Evolution, 4e
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(A) An ichthyosaur
(B) Lagosuchus talampayensis
Tail
Elongated
fourth ngers
Tail
Elongated
fourth ngers
(C) Pterodactylus
FIGURE 17.25 Some Mesozoic reptiles. (A) A marine
ichthyosaur (Greek, “fish lizard”), convergent in form with
sharks and porpoises. (B) Lagosuchus, a Triassic thecodont
archosaur (Greek, “ruling lizard”), showing the body form
of the stem group from which dinosaurs evolved. (C) A
pterosaur (Greek, “wing lizard”).
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