Title: Life of the Mesozoic Era
1Chapter 15
Life of the Mesozoic Era
2Mesozoic 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
3Baryonyx
- 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.
4The 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
5Dinosaur 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)
6Mammals 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
7Birds
- 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
8Land 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
9Systems 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
10Isolation
- 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
11Mesozoic 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
12Marine 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
13Brachiopods 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
14Mollusks
- 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
15Ammonoidea
- 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
16Cephalopods
- Cephalopods
- such as the Late Cretaceous ammonoids Baculites
- were important predators
- and excellent guide fossils
17Surviving 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
18Belemnoids
- These extinct squidlike cephalopods
- were abundant during the Cretaceous
- and are excellent guide fossils
- for the Jurassic and Cretaceous
19Cretaceous Hard Chalk Seafloor
- Mollusks were major elements of the Mesozoic
marine invertebrate fauna, particularly during
the Cretaceous
20Mesozoic 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
21Cretaceous Bivalves
- Bivalves were particularly diverse and abundant
during the Mesozoic - Even today they remain important elements in the
marine invertebrate fauna
22Mesozoic 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
23Rudist 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
24Familiar 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
25Echinoids
- 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
26Foraminifera
- 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
27Planktonic 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.
28Burrowing 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
29Escaping 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
30Mesozoic 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
31Coccolithophores
- Coccolithophores from the Gulf of Mexico
- of Miocene age
32Diatoms
- 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
33Diatoms
- Diatoms from Upper Miocene rocks in Java
34Dinoflagellates
- 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
35Increasing 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
36Aquatic 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
37Lungfishes 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
38Living 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
39Bony 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
40Advanced 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
41Labyrinthodont 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
42PlantsPrimary 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
43Ginkgos
- Ginkgos
- have changed very little
- for millions of years
- They were found
- living in some isolated habitats in Asia
- and have been transplanted elsewhere
44Gymnosperms
- 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
45Mesozoic Plants
- The Jurassic landscape was dominated by
- seedless vascular plants,
- particularly ferns,
- as well as gymnosperms
- such as conifers,
- tree ferns,
- and cycads
46Cycads
- Gymnosperms such as these cycads
- are still quite common
47Angiosperms
- 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
48Fossil Angiosperms
- Archaefructus sinensis
- from Lower Cretaceous rocks in China
- is among the oldest known angiosperms
49Fossil Angiosperms
- Reconstruction of Archaefructus sinensis
50Angiosperms 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
51Reproductive Cycle of Angiosperms
52More 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
53The 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
54Reptiles and Birds
- Relationships among fossil and living reptiles
and birds
55The 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
56Reptiles and Birds
57Archosaurs 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
58Archosaurs 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.
59Dinosaurs
- 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
60Misconceptions 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
61Misconceptions 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!
62Active 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
63Questions 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
64Dinosaurs 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
65Distinctive 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
66Dinosaur 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
67Common Ancestor
- Paleontologists are convinced
- that both orders of dinosaurs
- share a common ancestor,
- much like archosaurs
- from the Middle Triassic rocks
- in Argentina.
68Dinosaur 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
69Saurischian 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
70Dinosaur Cladogram
71Small Theropod Dinosaur
- Compsognathus weighed only 2 or 3 kg
- Bones found within its ribcage indicate it ate
lizards
72Tyrannosaurus
- The skull of Tyrannosaurus,
- another theropod,
- measured more than 1 m long
73Theropods 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
74Velociraptor 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
75Deinonychus
- Lifelike restoration of Deinonychus in its
probable attack posture - It was about 3 m long
76Mongolian 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
77Sauropods
- 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
78Sauropod 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
79Ornithischian Dinosaurs
- Scientists recognize five distinct groups of
ornithischians - ornithopods,
- pachycephalosaurs,
- ankylosaurs,
- stegosaurs,
- and ceratopsians
80Dinosaur Cladogram
81Ornithopod 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
82Duck-Billed Dinosaurs
- Two dinosaurs from the Late Cretaceous
- with head crests,
- hollow, bony extensions of the skull
83Duck-Billed Dinosaurs
- Edmontosaurus had no crest
84Ornithopods Were Herbivores
- All ornithopods were herbivores
- and primarily bipedal
- with well-developed forelimbs
- that allowed them to walk
- in a quadrupedal fashion also
85Care 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
86Pachycephalosaurs
- 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
87Ceratopsians
- 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.
88Triceratops
- Skeleton of the ceratopsian Triceratops
89Fossil Herds
- Fossil trackways
- and bone beds
- of ceratopsians
- indicate that these large,
- quadrupedal herbivores
- moved in herds
90Stegosaurs
- 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
91Stegosaurus
- Stegosaurus from the Late Jurassic was about 9 m
long, and had plates on its back and bony spikes
on its tail.
92Ankylosaurs
- 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
93Ankylosaur
- The ankylosaur Euoplocephalus
- Note the heavy armor and bony club at the end of
the tail
- The ankylosaur Sauropelta
94Warm-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
95Opinion 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
96Endothermic 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
97Higher 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
98Predators 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
99Large 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
100Insulation
- 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
101Four-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
102Convincing 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
103Arguments 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
104Less Heat Loss
- With less heat loss
- across their comparatively smaller surface area,
- sauropods probably retained heat more effectively
- than their smaller relatives
105Flying 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
106Pterodactyls
- Pterodactyls, a long-tailed Late Jurassic
pterosaur
- Among several known species,
- wingspan ranged from 50 cm to 2.5 m
107Pteranodon
- The short-tailed pterosaur
- known as Pteranodon
- was a large Cretaceous animal
- with a wingspan of more than 6 m
108Adaptations 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
109Wings
- 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?
110Pterosaurs
- 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
111Too 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
112Smaller Pterosaurs
- Smaller pterosaurs,
- in contrast,
- probably stayed aloft
- by vigorously flapping their wings
- just as present-day small birds do
113Mesozoic 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
114Ichthyosaurs
- 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
115Ichthyosaurs
- Restoration showing ichthyosaurs
- fully aquatic animals
- that evolved from land-dwelling ancestors
116Ichthyosaur
- Life-sized frieze of a 18.2-m-long ichthyosaur
- known as Shonisaurus popularis
- at Berlin-Ichthyosaur State Park, Nevada
117Ichthyosaurs Tail and Forelimbs
- Ichthyosaurs used
- their powerful tail
- for propulsion
- and their flipperlike forelimbs
- for maneuvering
118Ichthyosaurs
- 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
119Mary 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
120Mary Anning
- Mary Anning
- lived in Lyme Regis
- on Englands south coast
- where she began collecting
- and selling fossils
- when she was 11 years old
121Mary Anning
- Unfortunately,
- many scientists of her time
- could not accept that an untutored girl
- could possess such knowledge and skill
122Plesiosaurs
- 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
123Plesiosaurs
- Although the marine reptiles
- plesiosaurs
- were aquatic animals,
- their fipperlike forelimbs
- probably allowed them to come out onto land
124Short-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
125Mosasaurs
- 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
126Tylosaurus
- Tylosaurus was
- a large,
- Late Cretaceous
- mosasaur
- It measured up to 9 m long
127Mosasaur Skull
- Mosasaur skull on display
- in the Museum of Geology and Paleontology,
- University of Florence, Italy
128Mosasaurs 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
129Crocodiles
- 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
130Turtles
- 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
131Lizards, 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
132Snakes
- 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
133From 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
134Birds 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?
135Fossil 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
136Archaeopteryx
- 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
137Archaeopteryx
- In most anatomical details Archaeopteryx more
closely resembled a small theropod - It had claws on its wing and reptilian teeth
- but was a bird
138Archaeopteryx
- 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
139Ancestor/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
140Bird 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
141Protoavis
- 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
142Small 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
143Origin 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
144Origin 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
145Cynodonts 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
146Skeletal 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
147Reptile 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
148Mammalian Jaw
- Skull of a mammal showing the typical mammalian
dentary-squamosal jaw joint
149Cynodont Skull
- The skull of a cynodont
- shows the articular-quadrate jaw joint of reptiles
150Mammalian Middle Ear Bones
- Enlarged view of a mammals middle ear bones
151Reptilian Ear Bone
- Enlarged view of a reptilian ear bone
152Transition 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
153Transitional 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
154Embryos
- 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
155Differentiated 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
156Mammal and Reptile Teeth
157Sets 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
158Tooth 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
159Secondary 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
160Secondary Palate
- Views of the bottoms of skulls
- showing the progressive development
- of the bony secondary palate
161Mesozoic 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!
162Mesozoic 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
163Mosaic Evolution
- In short,
- some mammalian features
- evolved more rapidly than others
- Recall the concept of mosaic evolution