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Life of the Mesozoic Era

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Title: Life of the Mesozoic Era


1
Chapter 15
Life of the Mesozoic Era
2
Mesozoic Life Fascinates
  • The animals existing during the Mesozoic Era
  • fascinate nearly everyone
  • Ever since Sir Richard Owen
  • first used the term dinosaur in 1842,
  • dinosaurs have been the objects of intense
    curiosity
  • No other group of animals
  • has so thoroughly captured the public
    imagination,
  • but dinosaurs were only one type of Mesozoic
    reptile

3
Baryonyx
  • This Mesozoic scene shows the 10 m-long
    carnivorous dinosaur Baryonyx
  • and two large herbivorous dinosaurs
  • in the background.
  • Dinosaurs are the most popular of all extinct
    organisms.

4
The Age of Reptiles
  • Other Mesozoic reptiles include
  • flying reptiles
  • marine reptiles,
  • as well as turtles, crocodiles, lizards, and
    snakes
  • Geologists informally call the Mesozoic
  • "The Age of Reptiles,"
  • calling attention to the importance of reptiles
  • among land-dwelling animals

5
Dinosaur Movies
  • Of course Mesozoic animals,
  • especially dinosaurs,
  • have been popularized in numerous books,
  • TV specials, and movies
  • such as Jurassic Park (1993)
  • and its two sequels,
  • The Lost World (1997)
  • and Jurassic Park III (2001),
  • as well as Dinosaur (2000)

6
Mammals Too
  • The evolution and diversification of Mesozoic
    reptiles was certainly important,
  • but so were several other events
  • such as the origin of mammals during the Triassic
  • Thus mammals and dinosaurs were contemporaries
  • throughout the Mesozoic,
  • but mammals were not particularly diverse
  • and none were very large

7
Birds
  • Birds also made their appearance,
  • most likely evolving
  • from small carnivorous dinosaurs
  • during the Jurassic
  • Remarkable discoveries of feathered dinosaurs in
    China
  • have important implications about dinosaur
    biology
  • and are important for evaluating dinosaur
    relationships with birds

8
Land Plants
  • Important changes took place
  • in land plant communities
  • as the flowering plants evolved
  • during the Cretaceous
  • and soon became widespread and numerous
  • The major groups of Paleozoic land plants
    persisted,
  • but now they constitute less than 10 of all
    species

9
Systems Approach
  • We continue to emphasize
  • the systems approach to Earth and life history
  • The distribution of land and sea
  • profoundly influences oceanic circulation,
  • which in turn partly controls climate
  • The proximity or separation of landmasses
  • partly determines the geographic distribution of
    organisms

10
Isolation
  • Pangaea began fragmenting
  • during the Triassic and continues to do so
  • Organisms had increasingly difficulty
  • migrating between continents as a result
  • In fact, South America and Australia
  • became isolated island continents
  • and their faunas evolving in isolation
  • became quite different from those elsewhere

11
Mesozoic Mass Extinctions
  • Mass extinctions at the end of the Mesozoic,
  • second in magnitude only to the Paleozoic
    extinctions,
  • had a tremendous impact on the biosphere
  • But because dinosaurs were among the victims,
  • these extinctions have received
  • much more attention than any other extinction
  • Just as at the end of the Paleozoic Era,
  • biotic diversity was sharply reduced,
  • but once again many survivors evolved rapidly,
  • giving rise to the Cenozoic fauna

12
Marine Invertebrates and Phytoplankton
  • Following the Paleozoic mass extinctions,
  • the Mesozoic was a time
  • when marine invertebrates repopulated the seas
  • The Early Triassic invertebrate fauna
  • was not very diverse,
  • but by the Late Triassic the seas
  • were once again swarming with invertebrates
  • from planktonic foraminifera
  • to cephalopods

13
Brachiopods Never Fully Recover
  • The brachiopods,
  • that had been so abundant during the Paleozoic,
  • never completely recovered from their near
    extinction
  • Although brachiopods still exist
  • the bivalves
  • have largely taken over their ecological niche

14
Mollusks
  • Mollusks such as
  • cephalopods, bivalves, and gastropods
  • were the most important elements
  • in the Mesozoic marine invertebrate fauna
  • Their rapid evolution
  • and the fact that many cephalopods were nektonic
  • make them excellent guide fossils

15
Ammonoidea
  • The Ammonoidea,
  • cephalopods with wrinkled sutures,
  • constitute three groups
  • the goniatites, ceratites, and ammonites
  • Ammonites, while present during the entire
    Mesozoic,
  • were most prolific during the Jurassic and
    Cretaceous
  • Most ammonites were coiled,
  • some attaining diameters of 2 m,
  • whereas others were uncoiled
  • and led a nearly benthonic existence

16
Cephalopods
  • Cephalopods
  • such as the Late Cretaceous ammonoids Baculites
  • and Helioceros
  • were important predators
  • and excellent guide fossils

17
Surviving Cephalopods
  • Ammonites became extinct
  • at the end of the Cretaceous,
  • but two related groups of cephalopods
  • survived into the Cenozoic
  • the nautiloids,
  • including the living pearly nautilus,
  • and the coleoids, represented by extinct
    belemnoids
  • which were squidlike in appearance
  • and are good Jurassic and Cretaceous guide
    fossils
  • as well as by the living squid and octopus

18
Belemnoids
  • These extinct squidlike cephalopods
  • were abundant during the Cretaceous
  • and are excellent guide fossils
  • for the Jurassic and Cretaceous

19
Cretaceous Hard Chalk Seafloor
  • Mollusks were major elements of the Mesozoic
    marine invertebrate fauna, particularly during
    the Cretaceous

20
Mesozoic Bivalves
  • Mesozoic bivalves diversified
  • to inhabit many epifaunal and infaunal niches
  • Oysters and clams
  • epifaunal suspension feeders
  • became particularly diverse and abundant
  • and despite a reduction in diversity
  • at the end of the Cretaceous,
  • remain important animals in the marine fauna today

21
Cretaceous Bivalves
  • Bivalves were particularly diverse and abundant
    during the Mesozoic
  • Even today they remain important elements in the
    marine invertebrate fauna

22
Mesozoic Reef-Builders
  • Where shallow marine waters were warm and clear,
  • coral reefs proliferated, as they do today
  • An important reef-builder throughout the Mesozoic
  • was a group of bivalves known as rudists
  • Rudists are important
  • because they displaced corals
  • as the main reef-builders during the later
    Mesozoic
  • and are excellent guide fossils
  • for the Late Jurassic and Cretaceous

23
Rudist Bivalves
  • Two genera of Cretaceous reef-building bivalves
    known as rudists
  • These and other rudists replaced corals as the
    main reef-building animals of the Mesozoic

24
Familiar Coral
  • A new and familiar type of coral
  • also appeared during the Triassic,
  • the scleractinians
  • Whether scleractinians evolved from rugose corals
  • or from an as yet unknown soft-bodied ancestor
  • with no known fossil record is still unresolved

25
Echinoids
  • Another invertebrate group
  • that prospered during the Mesozoic
  • was the echinoids
  • Echinoids were exclusively epifaunal
  • during the Paleozoic,
  • but branched out into the infaunal habitat
  • during the Mesozoic
  • Both groups began a major adaptive radiation
  • during the Late Triassic
  • that continued throughout the remainder
  • of the Mesozoic and Cenozoic

26
Foraminifera
  • The foraminifera
  • single-celled consumers
  • underwent an explosive diversification
  • during the Jurassic and Cretaceous
  • They are still diverse and abundant today
  • The planktonic forms
  • in particular
  • diversified rapidly,
  • but most genera
  • became extinct at the end of the Cretaceous

27
Planktonic Foraminifera
  • Many planktonic foraminifera
  • are excellent guide fossils for the Cretaceous,
  • such as species of the genus Globotruncana,
  • which is restricted to the Upper Cretaceous.

28
Burrowing Organisms
  • One of the major differences
  • between the Paleozoic and Mesozoic
  • marine invertebrate faunas
  • was the increased abundance and diversity
  • of burrowing organisms
  • Paleozoic burrowers, with few exceptions,
  • were soft-bodied animals such as worms
  • The bivalves and echinoids,
  • which were epifaunal elements
  • during the Paleozoic,
  • evolved various means of entering infaunal
    habitats

29
Escaping from Predators
  • This trend toward an infaunal existence
  • may reflect an adaptive response
  • to increasing predation
  • from the rapidly evolving fish and cephalopods
  • Bivalves, for instance,
  • expanded into the infaunal niche
  • during the Mesozoic,
  • and escaped predators by burrowing

30
Mesozoic Primary Producers
  • The primary producers in the Mesozoic seas
  • were various types of microorganisms
  • Coccolithophores are an important group
  • of calcareous phytoplankton
  • that first evolved during the Jurassic
  • and became extremely common during the Cretaceous

31
Coccolithophores
  • Coccolithophores from the Gulf of Mexico
  • of Miocene age
  • of Miocene-Pliocene age

32
Diatoms
  • Diatoms
  • which build their skeletons of silica,
  • made their appearance during the Cretaceous,
  • but they are more important
  • as primary producers during the Cenozoic
  • Diatoms are presently most abundant
  • in cooler oceanic waters
  • and some species inhabit freshwater lakes

33
Diatoms
  • Diatoms from Upper Miocene rocks in Java

34
Dinoflagellates
  • Dinoflagellates
  • Which are organic-walled phytoplankton,
  • were common during the Mesozoic and today are the
    major primary producers in warm water
  • An Eocene dinoflagellate from Alabama
  • A Miocene-Piocene dinoflagellate from the Gulf of
    Mexico

35
Increasing Complexity
  • The Mesozoic was a time of
  • generally increasing complexity
  • of the marine invertebrate fauna
  • At the beginning of the Triassic,
  • diversity was low and food chains were short
  • Near the end of the Cretaceous, though,
  • the marine invertebrate fauna was highly complex
  • with interrelated food chains
  • This evolutionary history
  • reflects changing geologic conditions
  • influenced by plate tectonic activity

36
Aquatic and Semiaquatic VertebratesFish and
Amphibians
  • Sharks and the other cartilaginous fishes
  • became more abundant during the Mesozoic,
  • but even so they never came close
  • to matching the diversity of the bony fishes
  • Although an evolutionarily conservative group,
  • sharks, were and still are, important members
  • of the marine fauna, especially among predators

37
Lungfishes and Crossopterygians
  • Few species of lungfishes and crossopterygians
  • existed during the Mesozoic,
  • and the latter declined
  • and was nearly extinct by the end of the era
  • Only one crossopterygian species exists now
  • and the group has no known Cenozoic fossil record

38
Living Fossil
  • Latimeria
  • belongs to a group of fish once thought to have
    gone extinct at the end of the Mesozoic Era
  • A specimen was caught off the coast of East
    Africa in 1938
  • Since then many more have been captured

39
Bony Fish
  • All bony fish,
  • except lungfishes and crossopterygians,
  • belong to 3 groups, which for convenience we call
  • primitive, intermediate, and advanced
  • The primitive bony fishes
  • existed mostly during the Paleozoic,
  • but by Middle Mesozoic time,
  • the intermediate group predominated

40
Advanced Bony Fish
  • The advanced group,
  • more formally known as teleosts,
  • was dominant by Cretaceous time
  • in both marine and freshwater environments
  • With about 20,000 living species
  • they are by far the most diverse
  • and numerous of all living vertebrate animals

41
Labyrinthodont Amphibians
  • The labyrinthodont amphibians
  • were common during the latter part of the
    Paleozoic,
  • but the few surviving Mesozoic species died out
  • by the end of the Triassic
  • Since their greatest abundance
  • during the Pennsylvanian Period,
  • amphibians have made up
  • only a small part of the total vertebrate fauna
  • Frogs and salamanders evolved
  • during the Mesozoic,
  • but both have poor fossil records

42
PlantsPrimary Producers on Land
  • Just as during the Late Paleozoic,
  • seedless vascular plants and gymnosperms
  • dominated Triassic and Jurassic land-plant
    communities,
  • and, in fact, representatives of both groups
  • are still common
  • Among the gymnosperms,
  • the large seed ferns became extinct
  • by the end of the Triassic,
  • but ginkgos remained abundant
  • and still exist in isolated regions

43
Ginkgos
  • Ginkgos
  • have changed very little
  • for millions of years
  • They were found
  • living in some isolated habitats in Asia
  • and have been transplanted elsewhere

44
Gymnosperms
  • Conifers continued to diversify
  • and are now widespread in some terrestrial
    habitats,
  • particularly at high elevations and high
    latitudes
  • A new group of gymnosperms
  • known as cycads made its appearance
  • during the Triassic
  • These palm-like plants
  • became widespread
  • and now exist in tropical
  • and semi-tropical areas

45
Mesozoic Plants
  • The Jurassic landscape was dominated by
  • seedless vascular plants,
  • particularly ferns,
  • as well as gymnosperms
  • such as conifers,
  • tree ferns,
  • and cycads

46
Cycads
  • Gymnosperms such as these cycads
  • are still quite common

47
Angiosperms
  • The long dominance of seedless plants and
    gymnosperms
  • ended during the Early Cretaceous,
  • perhaps the Late Jurassic,
  • when many were replaced
  • by angiosperms,
  • or flowering plants
  • Studies of fossil and living gymnosperms
  • show that some have a close relationship with
    angiosperms,
  • but precise ancestors remain obscure

48
Fossil Angiosperms
  • Archaefructus sinensis
  • from Lower Cretaceous rocks in China
  • is among the oldest known angiosperms

49
Fossil Angiosperms
  • Reconstruction of Archaefructus sinensis

50
Angiosperms Evolved and Adapted
  • Since they evolved, angiosperms have adapted
  • to nearly every terrestrial habitat
  • from mountains to deserts
  • and some have even adapted
  • to shallow coastal waters
  • Several factors account for their phenomenal
    success,
  • but chief among them is their method of
    reproduction
  • Two developments were particularly important
  • the evolution of flowers,
  • which attract animal pollinators, especially
    insects
  • and the evolution of enclosed seeds

51
Reproductive Cycle of Angiosperms
52
More Than 90
  • Seedless vascular plants and gymnosperms
  • are important and still flourish in many
    environments
  • in fact, many botanists regard ferns
  • and conifers as emerging groups
  • Nevertheless, a measure of the angiosperms'
    success is
  • that today with 250,000 to 300,000 species
  • they account for more than 90 of all land plant
    species,
  • and they occupy some habitats
  • in which other land plants do poorly or cannot
    exist

53
The Diversification of Reptiles
  • Reptile diversification began
  • during the Mississippian Period
  • with the evolution of the protorothyrids,
  • the first animals to lay amniotic eggs
  • From this basic stock of so-called stem reptiles,
  • all other reptiles
  • as well as birds and mammals evolved

54
Reptiles and Birds
  • Relationships among fossil and living reptiles
    and birds

55
The Story of Reptile Diversification
  • Recall that pelycosaurs
  • were the dominant land vertebrates
  • of the Pennsylvanian and Permian periods
  • Here we continue our story
  • of reptile diversification
  • with a group called archosaurs

56
Reptiles and Birds
57
Archosaurs and the Origin of Dinosaurs
  • Reptiles known as archosaurs
  • archo meaning "ruling" and sauros meaning
    "lizard
  • include crocodiles, pterosaurs (flying reptiles),
    dinosaurs, and the ancestors of birds
  • Including such diverse animals
  • in a single group implies
  • that they share a common ancestor
  • and indeed they possess several characteristics
    that unite them

58
Archosaurs Teeth
  • For instance, all have teeth set in individual
    sockets,
  • except today's birds,
  • but even the early birds had this feature,
  • and they all lay amniotic eggs
  • One of the most important features is the limbs
  • that indicate semi-upright or upright posture
  • We now turn to a discussion of dinosaurs.

59
Dinosaurs
  • Sir Richard Owen
  • proposed the term dinosaur in 1842
  • to mean "fearfully great lizard"
  • although now "fearfully" has come to mean
  • "terrible," thus the characterization of
    dinosaurs as
  • "terrible lizards"
  • But of course they were not terrible,
  • or at least no more terrible
  • than animals living today,
  • and they were not lizards

60
Misconceptions about Dinosaurs
  • Dinosaurs, more than any other kind of animal,
    have inspired awe,
  • but unfortunately, their popularization
  • in many cartoons, books, and movies
  • has commonly been inaccurate
  • and has contributed to many misunderstandings
  • For instance, many people think
  • that all dinosaurs were large,
  • and because they are extinct
  • they must have been poorly adapted

61
Misconceptions about Dinosaurs
  • It is true that many were quite large,
  • but dinosaurs varied from giants
  • weighing several tens of metric tons
  • to those that weighed no more than 2 or 3 kg
  • To consider them poorly adapted
  • is to ignore the fact
  • that dinosaurs were extremely diverse
  • and widespread for more than 140 million years!

62
Active and Cared for Their Young
  • Although various media
  • now portray dinosaurs as more active animals,
  • the misconception that they were lethargic,
  • dim-witted beasts persists
  • Evidence now available indicates
  • that some were quite active
  • and perhaps even warm-blooded
  • Some species probably cared for their young
  • long after hatching,
  • a behavioral characteristic most often associated
  • with birds and mammals

63
Questions Remain
  • Many questions remain unanswered about dinosaurs,
  • their fossils and the rocks containing them
  • are revealing more and more
  • about their evolutionary relationships and
    behavior

64
Dinosaurs Orders
  • All dinosaurs possess
  • a number of shared characteristics,
  • such as full and upright posture
  • with limbs directly beneath their bodies
  • yet differ enough for us to recognize
  • two distinct orders,
  • the Saurischia
  • and Ornithischia
  • A distinctive pelvic structure
  • characterizes each order

65
Distinctive Pelvic Structure
  • Saurischian dinosaurs
  • have a 1izardlike pelvis
  • and are thus called lizard-hipped dinosaurs
  • Ornithischians
  • have a birdlike pelvis
  • and are called bird-hipped dinosaurs

66
Dinosaur Cladogram
  • Cladogram showing dinosaur relationships
  • showing pelvises of ornithischians and
    saurischians
  • Among the several subgroups of dinosaurs
  • theropods were carnivores
  • and all others were herbivores

67
Common Ancestor
  • Paleontologists are convinced
  • that both orders of dinosaurs
  • share a common ancestor,
  • much like archosaurs
  • from the Middle Triassic rocks
  • in Argentina.

68
Dinosaur Ancestors
  • These dinosaur ancestors were small
  • less than 1 m long
  • long-legged carnivores that walked
  • and ran on their hind limbs,
  • so they were bipedal,
  • as opposed to quadrupedal animals
  • that move on all four limbs

69
Saurischian Dinosaurs
  • The saurischians,
  • or lizard-hipped dinosaurs,
  • include two distinct groups
  • known as theropods and sauropods
  • All theropods
  • were carnivorous bipeds
  • ranging in size from tiny Compsognathus
  • to giants such as Tyrannosaurus
  • and similar but even larger species

70
Dinosaur Cladogram
71
Small Theropod Dinosaur
  • Compsognathus weighed only 2 or 3 kg
  • Bones found within its ribcage indicate it ate
    lizards

72
Tyrannosaurus
  • The skull of Tyrannosaurus,
  • another theropod,
  • measured more than 1 m long

73
Theropods with Feathers
  • Beginning in 1996,
  • Chinese scientists
  • have made remarkable discoveries
  • of theropods with feathers
  • Molecular analysis shows
  • that they were indeed composed
  • of the same material as bird's feathers

74
Velociraptor and Deinonychus
  • The movie Jurassic Park and its sequels
  • popularized some of the smaller theropods
  • such as Velociraptor,
  • a 1.8-m-long predator
  • with large sickle-like claws on the hind feet
  • This dinosaur and its somewhat larger relative
  • Deinonychus,
  • probably used their claws
  • in a slashing type of attack

75
Deinonychus
  • Lifelike restoration of Deinonychus in its
    probable attack posture
  • It was about 3 m long

76
Mongolian Double Fossil
  • A particularly interesting fossil from Mongolia
  • shows a Velociraptor grasping
  • a herbivorous dinosaur called Protoceratops
  • It seems that both animals perished
  • when the Velociraptor attacked

77
Sauropods
  • Included among the sauropods
  • are the truly giant,
  • quadrupedal herbivorous dinosaurs
  • such as Apatosaurus, Diplodocus, and
    Brachiosaurus,
  • the largest known land animals of any kind
  • Brachiosaurus,
  • a giant even by sauropod standards,
  • might have weighed as much as 75 metric tons,
  • and partial remains
  • indicate that even larger sauropods
  • may have existed

78
Sauropod History
  • Sauropods were preceded in the fossil record
  • by considerably smaller dinosaurs
  • known as prosauropods
  • These Late Triassic and Early Jurassic dinosaurs
  • were certainly closely related to sauropods
  • but probably were not their ancestors
  • Sauropods were particularly common during the
    Jurassic,
  • but only a few genera existed during the
    Cretaceous

79
Ornithischian Dinosaurs
  • Scientists recognize five distinct groups of
    ornithischians
  • ornithopods,
  • pachycephalosaurs,
  • ankylosaurs,
  • stegosaurs,
  • and ceratopsians

80
Dinosaur Cladogram
81
Ornithopod Dinosaurs
  • Ornithopods include the duck-billed dinosaurs
  • with flattened bill-like mouths
  • Hadrosaurs were especially numerous during the
    Cretaceous
  • and several species had head crests
  • which might have served a variety of functions

82
Duck-Billed Dinosaurs
  • Two dinosaurs from the Late Cretaceous
  • with head crests,
  • hollow, bony extensions of the skull

83
Duck-Billed Dinosaurs
  • Edmontosaurus had no crest

84
Ornithopods Were Herbivores
  • All ornithopods were herbivores
  • and primarily bipedal
  • with well-developed forelimbs
  • that allowed them to walk
  • in a quadrupedal fashion also

85
Care of the Young
  • Maiasaura, a Late Cretaceous ornithopod, nested
    in colonies in northern Montana
  • In this scene a female leads her young to a
    feeding area

86
Pachycephalosaurs
  • The most distinctive feature
  • of the pachycephalosaurs
  • is their thick-boned,
  • dome-shaped skull
  • Paleontologists note that the thick skull bones
  • are found in juveniles but not adults
  • These bipedal herbivores
  • are known from Late Cretaceous-aged rocks

87
Ceratopsians
  • The fossil record of Ceratopsians,
  • or horned dinosaurs,
  • shows that small Early Cretaceous animals
  • were the ancestors of large Late Cretaceous
    genera
  • such as Triceratops
  • and related genera with huge heads,
  • a large bony frill over the neck,
  • and a horn or horns on the skull
  • They were quite common in North America.

88
Triceratops
  • Skeleton of the ceratopsian Triceratops

89
Fossil Herds
  • Fossil trackways
  • and bone beds
  • of ceratopsians
  • indicate that these large,
  • quadrupedal herbivores
  • moved in herds

90
Stegosaurs
  • The most distinctive features of Stegosaurus
  • a medium-sized, quadrupedal herbivore
  • from the Jurassic Period
  • were a spiked tail,
  • used almost certainly for defense,
  • and plates on the back
  • The exact arrangement
  • of these plates is uncertain,
  • although they are usually depicted in two rows
  • with plates on one side offset from those on the
    other
  • Most paleontologists are convinced
  • that plates functioned
  • to absorb and dissipate heat

91
Stegosaurus
  • Stegosaurus from the Late Jurassic was about 9 m
    long, and had plates on its back and bony spikes
    on its tail.

92
Ankylosaurs
  • The ankylosaurs
  • were the most heavily armored of all dinosaurs
  • All were quadrupedal herbivores
  • and some were quite large
  • Bony armor
  • protected the animal's back, flanks,
  • and top of the head
  • The tail of some species ended in a bony club
  • that could undoubtedly deliver a crippling blow
  • to an attacking predator

93
Ankylosaur
  • The ankylosaur Euoplocephalus
  • Note the heavy armor and bony club at the end of
    the tail
  • The ankylosaur Sauropelta

94
Warm-Blooded Dinosaurs?
  • Were dinosaurs endotherms
  • warm-blooded
  • like today's mammals and birds,
  • or were they ectotherms
  • cold-blooded
  • as are all of today's reptiles?
  • Almost everyone now agrees
  • that some compelling evidence exists for dinosaur
    endothermy

95
Opinion Is Divided
  • Opinion is still divided among
  • (1) those holding that all dinosaurs were
    endotherms
  • (2) those who think only some were endotherms
    and
  • (3) those proposing that dinosaur metabolism,
  • and thus their ability to regulate body
    temperature,
  • changed as they matured
  • Bones of endotherms
  • typically have numerous passageways that,
  • contain blood vessels,
  • but considerably fewer passageways are present in
    bones of ectotherms

96
Endothermic Bone
  • Proponents of dinosaur endothermy
  • note that dinosaur bones
  • are similar to those of living endotherms
  • Yet crocodiles and turtles
  • have this so-called endothermic bone,
  • but they are ectotherms,
  • and some small mammals
  • have bone more typical of ectotherms
  • Perhaps bone structure is related
  • more to body size
  • and growth patterns than to endothermy,
  • so this evidence is obviously not conclusive

97
Higher Metabolic Rates
  • Endotherms must eat more
  • than comparable sized ectotherms
  • because their metabolic rates are so much higher
  • Consequently, endothermic predators
  • require large prey populations
  • and thus constitute a much smaller proportion
  • of the total animal population than their prey,
  • usually only a few percent

98
Predators to Prey Proportion
  • In contrast, the proportion
  • of ectothermic predators to prey
  • might be as high as 50
  • Where data are sufficient
  • to allow an estimate,
  • dinosaur predators made up 3 to 5
  • of the total population
  • Nevertheless, uncertainties in the data
  • make this less than a convincing argument
  • for many paleontologists

99
Large Brain
  • A large brain in comparison to body size
  • requires a rather constant body temperature
  • and thus implies endothermy
  • Some dinosaurs were indeed rather brainy,
  • especially the small- and medium-sized theropods

100
Insulation
  • So brain size might be a convincing argument for
    these dinosaurs,
  • but even more compelling evidence for theropod
    endothermy
  • comes from their probable relationship to birds,
  • and the discoveries in China
  • of dinosaurs with feathers or a feather-like
    covering
  • Today, only endotherms have
  • hair, fur, or feathers for insulation

101
Four-Chambered Heart
  • Some scientists point out
  • that certain duck-billed dinosaurs
  • grew and reached maturity much more quickly
  • than would be expected for ectotherms
  • and conclude that they must have been
    warm-blooded
  • Furthermore, a recently prepared fossil
    ornithopod
  • discovered in 1993
  • has a preserved four-chambered heart
  • much like that of living mammals and birds

102
Convincing Evidence
  • Three-dimensional imaging of this heart,
  • now on display
  • at the North Carolina Museum of Natural Sciences,
  • has convinced many scientists
  • that this animal was an endotherm

103
Arguments for Endothermy
  • Good arguments for endothermy
  • exist for several types of dinosaurs,
  • although the large sauropods
  • were probably not endothermic
  • but nevertheless were capable
  • of maintaining a rather constant body temperature
  • Large animals heat up and cool down
  • more slowly than smaller ones
  • because they have a small surface area
  • compared to their volume

104
Less Heat Loss
  • With less heat loss
  • across their comparatively smaller surface area,
  • sauropods probably retained heat more effectively
  • than their smaller relatives

105
Flying Reptiles
  • Paleozoic insects
  • were the first animals to achieve flight,
  • but the first among vertebrates were pterosaurs,
  • or flying reptiles,
  • which were common in the skies
  • from the Late Triassic
  • until their extinction at the end of the
    Cretaceous

106
Pterodactyls
  • Pterodactyls, a long-tailed Late Jurassic
    pterosaur
  • Among several known species,
  • wingspan ranged from 50 cm to 2.5 m

107
Pteranodon
  • The short-tailed pterosaur
  • known as Pteranodon
  • was a large Cretaceous animal
  • with a wingspan of more than 6 m

108
Adaptations for Flight
  • Adaptations for flight include
  • a wing membrane
  • supported by an elongated fourth finger
  • light hollow bones,
  • and development of those parts of the brain
  • associated with muscular coordination and sight
  • Because at least one pterosaur species
  • had a coat of hair or hairlike feathers,
  • possibly it was an endotherm
  • as perhaps all pterosaurs were

109
Wings
  • In all flying vertebrates,
  • the forelimb has been modified into a wing
  • A long 4th finger supports the pterosaur wing
  • whereas in birds the 2nd and 3rd fingers are
    fused together
  • and in bats, fingers 2 through 5 support the wing
  • Are these wings analogous, homologous, or both?

110
Pterosaurs
  • Pterosaurs are generally depicted in movies
  • as large, aggressive creatures,
  • but some were no bigger than today's
  • sparrows, robins, and crows
  • However, a few species had
  • wingspans of several meters,
  • and one Cretaceous pterosaur found in Texas had
  • a wingspan of at least 12 m!
  • Nevertheless, even the very largest species
  • probably weighed less than a few tens of kilograms

111
Too Weak for Sustained Flapping
  • Experiments and studies of fossils
  • indicate that the wing bones of large pterosaurs
  • such as Pteranodon
  • were too weak for sustained flapping
  • These comparatively large animals
  • probably took advantage of rising air currents
  • to stay airborne,
  • mostly by soaring
  • but occasionally flapping their wings for
    maneuvering

112
Smaller Pterosaurs
  • Smaller pterosaurs,
  • in contrast,
  • probably stayed aloft
  • by vigorously flapping their wings
  • just as present-day small birds do

113
Mesozoic Marine Reptiles
  • Several Mesozoic reptiles
  • adapted to a marine environment
  • including turtles and some crocodiles,
  • as well as the Triassic mollusk-crushing
    placodonts
  • Here, however, we concentrate on
  • the ichthyosaurs, plesiosaurs, and mosasaurs
  • All of these marine predators
  • were thoroughly aquatic,
  • but other than all being reptiles
  • they are not particularly closely related

114
Ichthyosaurs
  • The streamlined, rather porpoiselike ichthyosaurs
  • varied from species measuring only 0.7 m long
  • to 15 m-long giants
  • Although details of their ancestry
  • are still not fully known,
  • they evolved from small animals
  • whose fossils remind one researcher of
  • "a lizard with flippers that still retained
    some key features of their land-dwelling
    ancestors1
  • 1Motani, R. 2000 Rulers of the Jurassic Seas,
    Scientific American, v 283, no 6, p 55

115
Ichthyosaurs
  • Restoration showing ichthyosaurs
  • fully aquatic animals
  • that evolved from land-dwelling ancestors

116
Ichthyosaur
  • Life-sized frieze of a 18.2-m-long ichthyosaur
  • known as Shonisaurus popularis
  • at Berlin-Ichthyosaur State Park, Nevada

117
Ichthyosaurs Tail and Forelimbs
  • Ichthyosaurs used
  • their powerful tail
  • for propulsion
  • and their flipperlike forelimbs
  • for maneuvering

118
Ichthyosaurs
  • They had numerous sharp teeth
  • Preserved stomach contents reveal a diet of
  • fish, cephalopods, and other marine organisms
  • It is doubtful that ichthyosaurs
  • could come onto land,
  • so females must have retained eggs
  • within their bodies
  • and gave birth to live young
  • A few fossils with small ichthyosaurs
  • in the appropriate part of the body cavity
  • support this interpretation

119
Mary Anning
  • An interesting side note in the history of
    paleontology
  • is the story of Mary Anning (1799-1847),
  • who when only about 11 years old discovered
  • and directed the excavation
  • of a nearly complete ichthyosaur
  • in southern England
  • This and subsequent discoveries
  • made her a well-known fossil collector

120
Mary Anning
  • Mary Anning
  • lived in Lyme Regis
  • on Englands south coast
  • where she began collecting
  • and selling fossils
  • when she was 11 years old

121
Mary Anning
  • Unfortunately,
  • many scientists of her time
  • could not accept that an untutored girl
  • could possess such knowledge and skill

122
Plesiosaurs
  • The plesiosaurs,
  • another well-known group of Mesozoic marine
    reptiles,
  • belonged to one of two subgroups
  • short necked and long-necked
  • Most were modest sized animals 3.6 to 6 m long,
  • but one species
  • found in Antarctica
  • measures 15 m

123
Plesiosaurs
  • Although the marine reptiles
  • plesiosaurs
  • were aquatic animals,
  • their fipperlike forelimbs
  • probably allowed them to come out onto land

124
Short-Necked Plesiosaurs
  • Short-necked plesiosaurs might have been bottom
    feeders,
  • but their long-necked cousin
  • may have used their necks
  • in a snakelike fashion
  • to capture fish with their numerous sharp teeth
  • These animals
  • probably came ashore to lay their eggs

125
Mosasaurs
  • Mosasaurs were Late Cretaceous marine lizards
  • related to the present-day
  • Komodo dragon or monitor lizard
  • Some species measured no more than 2.5 m long,
  • but a few such as Tylosaurus were large,
  • measuring up to 9 m
  • Mosasaur limbs resemble paddles
  • and were used mostly for maneuvering
  • whereas the long tail provided propulsion

126
Tylosaurus
  • Tylosaurus was
  • a large,
  • Late Cretaceous
  • mosasaur
  • It measured up to 9 m long

127
Mosasaur Skull
  • Mosasaur skull on display
  • in the Museum of Geology and Paleontology,
  • University of Florence, Italy

128
Mosasaurs Were Predators
  • All mosasaurs were predators,
  • and preserved stomach contents indicate
  • that they ate fish, birds, smaller mosasaurs,
  • and a variety of invertebrates
  • including ammonoids

129
Crocodiles
  • By Jurassic time,
  • crocodiles had become
  • the most common freshwater predators
  • All crocodiles are amphibious,
  • spending much of their time in water,
  • but they are well equipped for walking on land
  • Crocodile evolution has been conservative,
  • involving changes mostly in size
  • from a meter or so in Jurassic forms
  • to 15 m in some Cretaceous species

130
Turtles
  • Turtles, too, have been evolutionarily
    conservative
  • since their appearance during the Triassic
  • The most remarkable feature of turtles
  • is their heavy, bony armor
  • turtles are more thoroughly armored
  • than any other vertebrate animal, living or
    fossil
  • Turtle ancestry is uncertain
  • One Permian animal
  • had eight broadly expanded ribs,
  • which may represent the first stages
  • in the development of turtle armor

131
Lizards, and Snakes
  • Lizards and snakes are closely related,
  • and lizards were in fact ancestral to snakes
  • The limbless condition in snakes
  • some lizards are limbless, too
  • and skull modifications
  • that allow snakes to open their mouths very wide
  • are the main differences between these two groups
  • Lizards are known from Upper Permian strata,
  • but they were not abundant until the Late
    Cretaceous

132
Snakes
  • Snakes first appear during the Cretaceous,
  • but the families to which most living snakes
    belong
  • differentiated since the Early Miocene
  • One Early Cretaceous genus from Israel
  • appears to show characteristics intermediate
  • between snakes and their lizard ancestors

133
From Reptiles to Birds
  • Scientists were aware of a number of
    characteristics
  • shared by reptiles and birds
  • even before they found fossil evidence
  • showing a relationship between the two groups
  • For example, birds and reptiles
  • lay shelled, yolked eggs,
  • and both share a number of skeletal features
  • such as the way the jaw articulates with the skull

134
Birds Do Not Closely Resemble Living Reptiles
  • But of course birds have feathers
  • whereas reptiles have scales
  • or a tough, beaded skin
  • Furthermore, birds do not closely resemble
  • any living reptile,
  • so why do scientists think they are justified
  • when they claim that birds evolved from reptiles?

135
Fossil Feathers
  • Several fossils with feather impressions
  • have been discovered
  • in the Solnhofen Limestone of Germany
  • They definitely have feathers
  • and a wishbone, consisting of fused clavicle
    bones,
  • so typical of birds,
  • and yet in most other skeletal features
  • they most closely resemble
  • small theropod dinosaurs

136
Archaeopteryx
  • Fossil bird, Archaeopteryx
  • from the Jurassic Solnhofen Limestone in Germany
  • has feather impressions in the wings and long
    tail
  • A wishbone and feathers made it a bird

137
Archaeopteryx
  • In most anatomical details Archaeopteryx more
    closely resembled a small theropod
  • It had claws on its wing and reptilian teeth
  • but was a bird

138
Archaeopteryx
  • These animals, known as Archaeopteryx
  • are birds by definition,
  • but their numerous reptilian features
  • convince many scientists
  • that they evolved from
  • some kind of small theropod
  • Even fused clavicles are found in several
    theropods,
  • and recent discoveries in China of theropods
  • with some kind of feathery covering
  • provide more evidence for this relationship

139
Ancestor/Descendant Gap
  • Opponents of the theropod-bird scenario
  • point out that theropods
  • are typically found in Cretaceous-aged rocks,
  • whereas Archaeopteryx is Jurassic
  • However, some of the fossils
  • coming from China
  • are about the same age as Archaeopteryx,
  • thus narrowing the gap
  • between presumed ancestor and descendant

140
Bird Evolution
  • A Mesozoic fossil, from China,
  • is slightly younger than Archaeopteryx
  • and possesses both primitive and advanced
    features
  • It retains abdominal ribs
  • similar to those of Archaeopteryx and theropods,
  • but it has a reduced tail
  • more typical of present-day birds
  • Another Mesozoic bird, from Spain
  • is also a mix of primitive and advanced
    characteristics,
  • but it appears to lack abdominal ribs

141
Protoavis
  • Archaeopteryx's fossil record is not good enough
  • to resolve whether it is the actual ancestor of
    today's birds
  • or an animal that died out without leaving
    descendants
  • Of course, that in no way diminishes the fact
  • that it had both reptile and bird characteristics
  • However, some claim that fossils of two
    crow-sized individuals
  • known as Protoavis
  • represent an even earlier bird than Archaeopteryx

142
Small Theropods?
  • Protoavis Late Triassic fossils have hollow bones
  • and the breastbone structure of birds,
  • but because no feather impressions were found,
  • many paleontologists think they are small
    theropods

143
Origin of Flight Two Hypotheses
  • From the Ground Up
  • Bird ancestors were bipedal, fleet-footed ground
    dwellers
  • whose wings enabled them to leap into the air
  • and glide short distances
  • From the Trees Down
  • Bird ancestors were bipeds that climbed trees
  • and used their rudimentary wings for gliding
  • or parachuting

144
Origin and Early Evolution of Mammals
  • Therapsids,
  • or the advanced mammal-like reptiles
  • diversified into numerous species
  • of herbivores and carnivores
  • These terrestrial vertebrates
  • were the most diverse
  • and numerous land-dwelling vertebrates during the
    Permian
  • One particular group of carnivorous therapsids
  • called cynodonts was the most mammal-like of all
  • and by the Late Triassic gave rise to mammals

145
Cynodonts and the Origin of Mammals
  • We can easily recognize living mammals
  • as warm-blooded animals with hair or fur
  • that have mammary glands and,
  • except for the platypus and spiny anteater,
  • give birth to live young

146
Skeletal Modifications
  • Obviously these criteria are inadequate
  • for classifying fossils
  • for them, we must use skeletal structure only
  • Several skeletal modifications
  • characterize the transition
  • from mammal-like reptiles to mammals
  • but distinctions between the two groups
  • are based largely on details of the middle ear,
  • the lower jaw,
  • and the teeth

147
Reptile and Mammal Jaws
  • Reptiles have only one small bone
  • in the middle ear the stapes
  • while mammals have three
  • the incus, the malleus, and the stapes
  • Also, the lower jaw of a mammal
  • is composed of a single bone called the dentary,
  • but a reptile's jaw is composed of several bones
  • In addition, a reptile's jaw
  • is hinged to the skull at a contact
  • between the articular and quadrate bones,
  • while in mammals the dentary
  • contacts the squamosal bone of the skull

148
Mammalian Jaw
  • Skull of a mammal showing the typical mammalian
    dentary-squamosal jaw joint

149
Cynodont Skull
  • The skull of a cynodont
  • shows the articular-quadrate jaw joint of reptiles

150
Mammalian Middle Ear Bones
  • Enlarged view of a mammals middle ear bones

151
Reptilian Ear Bone
  • Enlarged view of a reptilian ear bone

152
Transition From Cynodonts to Mammals
  • During the transition from cynodonts to mammals,
  • the quadrate and articular bones
  • that had formed the joint
  • between the jaw and skull in reptiles
  • were modified into the incus and malleus
  • of the mammalian middle ear
  • Fossils document the progressive enlargement
  • of the dentary
  • until it became the only element
  • in the mammalian jaw

153
Transitional Cynodonts
  • Likewise, a progressive change
  • from the reptile to mammal jaw joint
  • is documented by fossil evidence
  • In fact, some of the most advanced cynodonts
  • were truly transitional because they had a
    compound jaw joint consisting of
  • (1) the articular and quadrate bones typical of
    reptiles and
  • (2) the dentary and squamosal bones as in mammals

154
Embryos
  • The study of embryos
  • provides evidence for evolution
  • Opossum embryos show
  • that the middle-ear bones of mammals
  • were originally part of the jaw
  • In fact, even when opossums are born,
  • the middle-ear elements are still attached
  • to the dentary
  • but as they develop further,
  • these elements migrate to the middle ear,
  • and a typical mammal jaw joint develops

155
Differentiated Teeth
  • Several other aspects of cynodonts
  • also indicate that they were ancestors of mammals
  • Their teeth were somewhat differentiated
  • into distinct types
  • that performed specific functions
  • In mammals the teeth are fully differentiated
  • into incisors, canines, and chewing teeth,
  • but typical reptiles do not have differentiated
    teeth

156
Mammal and Reptile Teeth
157
Sets of Teeth
  • In addition, mammals have
  • only two sets of teeth during their lifetimes
  • a set of baby teeth and the permanent adult teeth
  • Typical reptiles have teeth
  • replaced continuously throughout their lives,
  • the notable exception being in some cynodonts
  • who in mammal fashion had only two sets of teeth

158
Tooth Occlusion
  • Another important feature of mammal teeth is
    occlusion
  • that is, the chewing teeth meet surface to
    surface
  • to allow grinding
  • Thus, mammals chew their food,
  • but typical reptiles, amphibians, and fish do not
  • However, tooth occlusion
  • is known in some advanced cynodonts

159
Secondary Palate
  • Another mammalian feature,
  • the secondary palate,
  • was partially developed in advanced cynodonts
  • This bony shelf
  • separating the nasal passages from the mouth
    cavity,
  • is an adaptation for eating and breathing at the
    same time,
  • a necessary requirement for endotherms
  • with their high demands for oxygen

160
Secondary Palate
  • Views of the bottoms of skulls
  • showing the progressive development
  • of the bony secondary palate
  • an early therapsid
  • an early mammal
  • a cynodont

161
Mesozoic Mammals
  • Mammals evolved during the Late Triassic,
  • not long after the first dinosaurs appeared
  • but for the rest of the Mesozoic Era
  • most remained small
  • Exceptions
  • the Middle Jurassic-aged aquatic mammal from
    China
  • Repenomamus giganticus,
  • about 1 m long and 12-14 kg,
  • which had the remains of a juvenile dinosaur in
    its stomach!

162
Mesozoic Mammals
  • Most other Mesozoic mammals
  • were about the size of mice and rats
  • and were not very diverse
  • Furthermore, they still retained several
    reptilian characteristics,
  • but had mammalian features as well
  • For instance, the Triassic-aged triconodonts
  • had the fully differentiated teeth typical of
    mammals,
  • but they also had both the reptile and mammal
    types of jaw joints

163
Mosaic Evolution
  • In short,
  • some mammalian features
  • evolved more rapidly than others
  • Recall the concept of mosaic evolution
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