E. Carboniferous (359-300 mya) - inverts Arthropleura -largest terrestrial arthropod - 2m.

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Transcript of E. Carboniferous (359-300 mya) - inverts Arthropleura -largest terrestrial arthropod - 2m.

E. Carboniferous (359-300 mya)

- inverts

Arthropleura -largest terrestrial arthropod - 2m

E. Carboniferous (359-300 mya)

- inverts

- radiation of insects

- evolution of flight

Meganeura monyi - largest insect ever

wingspan of 70 cm

E. Carboniferous (359-300 mya)

- inverts

- plants

The early Carboniferous saw a reduction in the Devonian forests and a dominance of small plants - lycopods and their kin.

Lepidodendron

Psaronius - fern

Lebachia - progymnosperm

Cordaites - progymnosperm

E. Carboniferous (359-300 mya)

- inverts

- plants

The early Carboniferous saw a reduction in the Devonian forests and a dominance of small plants - lycopods and their kin.

As the period proceeds, the giant lycopsid swamp forests evolve across the tropical continent of Euramerica.

There was lots of photosynthesis, but this was not balanced by decomposition (because much of the biomass was preserved in sediment, not broken down by decay). So, oxygen production by photosynthesis exceeded oxygen consumption by decomposition... and oxygen levels were probably very high...this may have allowed the enormous size of invertebrates.

E. Carboniferous (359-300 mya)

- inverts

- plants

E. Carboniferous (359-300 mya)

- inverts

- plants Coal deposits in shallow tropical swamps

E. Carboniferous (359-300 mya)

- inverts

- plants

- vertebrates

sharks replace placoderms as dominant in oceans;

The golden age of sharks - 45 Families

(currently 21)

E. Carboniferous (359-300 mya)

- inverts

- plants

- vertebrates

sharks replace placoderms as dominant in oceans;

ray finned fishes dominate in fresh water

- vertebrates

radiation of stem tetrapods!!

- vertebrates

radiation of stem tetrapods!!

- vertebrates

radiation of stem tetrapods!!

"Anthracosaurs"

E. Carboniferous (359-300 mya)

- inverts

- plants

- vertebrates

sharks replace placoderms as dominant in oceans;

ray finned fishes dominate in fresh water

stem tetrapods radiate!

"crown" tetrapods

Seymouriamorpha

Temnospondyls

Ichthyostegans

E. Carboniferous (359-300 mya)

- inverts

- plants

- vertebrates

stem tetrapods

Temnospondyls

a very diverse radiation of tetrapods, from alligator-like salamanders to large, scaled, frog-like creatures. Cowens places these ancestral to Amphibia only, but recent analyses put them as a sister clade to all crown tetrapods.

Temnospondyls

a very diverse radiation of tetrapods, from alligator-like salamanders to large, scaled, frog-like creatures. Cowens places these ancestral to Amphibia only, but recent analyses put them as a sister clade to all crown tetrapods.

Seymouriamorpha

Radiate in Permian

but earliest fossils from the Carboniferous... larvae have external gills, which pulls them out of the amniota...

- vertebrates

radiation of stem tetrapods!!

The Amniote Divide

The amniotic egg was a big advance

- amnion protects the embryo - yolk sac provides nourishment - allantoic sac holds waste produced by embryo

Resist desiccation

Provision embryo

allows for colonization of dry habitats

Primitive Amniotes

Hylonomus lyelli – an early reptile

Carboniferous of Nova Scotia

E. Carboniferous

- The Amniote Radiations

Anapsid ancestor

Hylonomus

Casineria

ANAPSID (turtles?)

DIAPSID

SYNAPSID

I. The Precambrian

- Vendian

II. Paleozoic

A. Cambrian (544-490 mya)

B. Ordovician (490-443 mya)

C. Silurian (443-417 mya)

D. Devonian (417-354 mya)

E. Carboniferous (359-300 mya)

F. Permian (300-251 mya)

F. Permian (300-251 mya)

Pangaea forms

The fusion of land masses reduced the amount of humid coastline and increased the extent of dry inland areas. This favored the amniote radiations over "amphibian" clades.

F. Permian

- The Amniote Radiations Diversify

Anapsid ancestor

Hylonomus

ANAPSID (turtles)

DIAPSID

SYNAPSID

F. Permian (300-251 mya)

Synapsids dominate through the early Permian

Mammals

Cynodonts

Gorgonopsids

Therapsids

Pelycosaurs

Dicynodonts

F. Permian (300-251 mya)

Pelycosaurs dominate early

include the great sail-finned animals like Dimetrodon

F. Permian (300-251 mya)

Early Therapsids, like Gorgonopsids, dominate in the mid-late Permian

Dinocephalians

Moschops

F. Permian (300-251 mya)

Dicynodonts come to numerical dominance in the late Permian

abundant herbivores

F. Permian (300-251 mya)

and the first Cynodonts appear

F. Permian (300-251 mya)

large herbivorous anapsids were also present

F. Permian (300-251 mya)

Diapsids were small and lizard-like; the Synapsids ruled terrestrial communities

F. Permian (300-251 mya)

- Plants!!

F. Permian (300-251 mya)

- Plants!!

- the dry climate reduced the great Carboniferous swamp forests; lycopods shrink...

- Ferns, and gymnosperms ("seed ferns", Ginkos, Cycads, and Conifers) gain prominence...

- In particular Glossopteris - a seed fern - that produces seeds on its leaves like sori of ferns...

The evolution of gymnosperms introduced two important adaptive features:

- pollen (male gametophyte) - no more swimming sperm; reduced reliance on open water habitats

- seed - protective seed coat reduced desiccation of embryo, and nutritious endosperm provisioned the embryo with energy. (Like the amniote egg).

F. Permian (300-251 mya)

The great Permian extinction!!!!

A huge mantle plume rises towards the surface...

F. Permian (300-251 mya)

The great Permian extinction!!!!

then it pops like a zit!!

F. Permian (300-251 mya)

The great Permian extinction!!!!

A huge mantle plume rises towards the surface...

resulting in a great bubble of flowing lava... the Siberian flats (200,000 squ. mi)

F. Permian (300-251 mya)

F. Permian (300-251 mya)

- results:

90-95% of marine species go extinct...

trilobites

placoderms

acanthodians

F. Permian (300-251 mya)

- results:

90-95% of marine species go extinct...

trilobites

placoderms

acanthodians

70% of all land families

pelycosaurs

III. Mesozoic Era

A. Triassic Period (250 - 205 mya)

III. Mesozoic Era

A. Triassic Period (250 - 205 mya)

- climate:

Dry; low sea levels; one large supercontinent

beginning to break up

III. Mesozoic Era

A. Triassic Period (250 - 205 mya)

- inverts:

- marine communities - gastropods and molluscs begin to dominate in these initially depauperate faunas... the 'modern marine fauna', including modern reef-builders

III. Mesozoic Era

A. Triassic Period (250 - 205 mya)

- Plants:

- recovery from the mass extinction is slow; lycopsids

dominate early, but soil formation is very slow...

- dry climate selects for seed plants with pollen;

the Gymnosperms...

Petrified Forest N. P.

III. Mesozoic Era

A. Triassic Period (250 - 205 mya)

- Verts:

- Medium sized therapsids dominate early... like Lystrosaurus

Triassic survivors

Mammals

Gorgonopsids

Therapsids

Pelycosaurs

Dicynodonts

Cynodonts

III. Mesozoic Era

A. Triassic Period (250 - 205 mya)

- Verts:

- Medium sized therapsids dominate early... like Lystrosaurus

- Temnospondyls resurgent (Mastodonosaurus - 6m)

III. Mesozoic Era

A. Triassic Period (250 - 205 mya)

- Verts:

- radiation of the diapsids, but only Ichthyosaurs abundant early

Diapsida

Younginiformes

Ichthyosaurs

Lepidosaurs: Lizards, Snakes, Sphenodonts, Plesiosaurs)

Archosaurs: Dinosaurs, Pterosaurs, Crocodilians, Birds

III. Mesozoic Era

A. Triassic Period (250 - 205 mya)

- Verts:

- the opening of the shallow Tethys Sea between Laurasia and Gondwanaland created a very productive marine environment, which was exploited by a diverse group of evolving marine reptiles:

III. Mesozoic Era

A. Triassic Period (250 - 205 mya)

- Verts:

- marine reptiles:

Ichthyosaurs

Placodonts

Archeosaurs:

Tanystropheus

Lepidosaurs:

Nothosaurus

III. Mesozoic Era

A. Triassic Period (250 - 205 mya)

- Verts:

- marine reptiles:

Lepidosaurs:

Nothosaurus

Shonisaurus - 45m largest reptile

(Blue Whale = 33m, 110 ft)

III. Mesozoic Era

A. Triassic Period (250 - 205 mya)

- Verts:

- As the Triassic proceeds, the Archosaurs displace the Therapsids.

Crocodylomorphs

(Ornithosuchans and Phytosaurs)

Pterosaurs

Dinosaurs

crucrotarsi

Ornithodira

(Marasuchas)

III. Mesozoic Era

A. Triassic Period (250 - 205 mya)

- Verts:

- As the Triassic proceeds, the Archosaurs displace the Therapsids.

- Crocodylomorphs:

III. Mesozoic Era

A. Triassic Period (250 - 205 mya)

- Verts:

- As the Triassic proceeds, the Archosaurs displace the Therapsids.

- In the late Triassic, the first Dinosaur radiations occur.

Ornithichians

Prosauropods

Sauropods

Theropods

Saurichians

III. Mesozoic Era

A. Triassic Period (250 - 205 mya)

- Verts:

- As the Triassic proceeds, the Archosaurs displace the Therapsids.

- In the late Triassic, the first Dinosaur radiations occur.

Ornithichians

Prosauropods

Sauropods

Theropods

Ornithischians

III. Mesozoic Era

A. Triassic Period (250 - 205 mya)

- Verts:

- As the Triassic proceeds, the Archosaurs displace the Therapsids.

- In the late Triassic, the first Dinosaur radiations occur.

Ornithichians

Prosauropods

Sauropods

Theropods

Saurischians

III. Mesozoic Era

A. Triassic Period (250 - 205 mya)

- Verts:

- As the Triassic proceeds, the Archosaurs displace the Therapsids.

- In the late Triassic, the first Dinosaur radiations occur.

Oldest Dinosaurs are the Theropod-like Eoraptor

III. Mesozoic Era

A. Triassic Period (250 - 205 mya)

- Verts:

- As the Triassic proceeds, the Archosaurs displace the Therapsids.

- In the late Triassic, the first Dinosaur radiations occur.

The first radiation of large dinosaurs were the herbivorous Prosauropods

By the late Triassic, all large herbivores were Sauropodomorphs.

III. Mesozoic Era

A. Triassic Period (250 - 205 mya)

- Verts:

- the first mammaliforms... Morganucodontids

III. Mesozoic Era

B. Jurassic (200-146 mya)

- Climate:

A global greenhouse - lush tropical habitats and rich shallow seas lead to the period of maximum Dinosaur domination.

III. Mesozoic Era

B. Jurassic (200-146 mya)

- Marine Reptiles:

Ichthyosaurs still present...

III. Mesozoic Era

B. Jurassic (200-146 mya)

- Marine Reptiles:

but now joined by Plesiosaurs and Pliosaurs (both Lepidosaurs)

III. Mesozoic Era

B. Jurassic (200-146 mya)

- Marine Reptiles:

and marine crocodylians....

III. Mesozoic Era

B. Jurassic (200-146 mya)

- Herbivores:

Ornithichian Stegosaurs

III. Mesozoic Era

B. Jurassic (200-146 mya)

- Herbivores:

Sauropods - the first of the real giants

1, small head and peg-like teeth (and elongated cervical vertebrae)

2, addition of extra cervical vertebrae to the neck

3, apron-like pubis

4, fore limbs as long as or longer than hind limbs, making the back slope posteriorly

5, teeth restricted to front of mouth 6, armor.

III. Mesozoic Era

B. Jurassic (200-146 mya)

- Herbivores:

Sauropods - the first of the real giants

Ultrasaurus (maybe a Brachiosaurus) stood 98 ft long, 140 tons

III. Mesozoic Era

B. Jurassic (200-146 mya)

- Herbivores:

Sauropods - the first of the real giants

Diplodocus - 90 ft long 11 tons

III. Mesozoic Era

B. Jurassic (200-146 mya)

- Carnivores:

1. three-toed foot2. digits IV and V lost on hand3. long arms4. semilunate carpal5. fused pelvis6. large hole in lacrimal bone in skull7. ?no unique derived characters?8. giant, hook-like claw on digit II of pes9. flight feathers

III. Mesozoic Era

B. Jurassic (200-146 mya)

- Carnivores:

- Ceratosaurs

Ceratosaurus

III. Mesozoic Era

B. Jurassic (200-146 mya)

- Carnivores:

- Carnosaurs Allosaurus

III. Mesozoic Era

B. Jurassic (200-146 mya)

- Carnivores:

- Avialae Archaeopteryx

III. Mesozoic Era

B. Jurassic (200-146 mya)

- Carnivores:

- Avialae Archaeopteryx

First fossil - 1860 - a flight feather (asymmetrical)

The 'London' Specimen - 1861 The 'Berlin' Specimen - 1877

10th specimen described in 2005 - shows intermediately rotated halux

10th specimen described in 2005 - shows intermediately rotated halux and hyperextended 2nd digit (like Deinonychosaurs - their sister clade)

10th specimen described in 2005 - shows intermediately rotated halux and hyperextended 2nd digit (like Deinonychosaurs - their sister clade)

A. Herrerasaurus- five digits are present, Digit V shaded yellow and hidden on other side of hand.

B. Coelophysis. Note that digit V is gone.

C. Deinonychus. Note loss of both digits V and IV

D. Archaeopteryx. Note very close correspondence in proportions and relative lengths of bones to Deinonychus.

E. Hoatzin embryo. Number of bones reduced in digit III.

F. Hoatzin adult. Most of the bones of the hand fused

Hand Morphology

Ornitholestes(theropod dinosaur)

Archaeopteryx

Sinornis(a Cretaceous bird)

Modern chicken

Another Set of Examples

Archaeopteryx

Chicken

III. Mesozoic Era

B. Jurassic (200-146 mya)

- Pterosaurs

They were present in the Triassic, but reached their greatest diversity in the Jurassic, with over 80 species recorded.

However, they would attain their greatest size in the Cretaceous.

III. Mesozoic Era

B. Jurassic (200-146 mya)

- Pterosaurs

They were present in the Triassic, but reached their greatest diversity in the Jurassic, with over 80 species recorded.

However, they would attain their greatest size in the Cretaceous.

III. Mesozoic Era

B. Jurassic (200-146 mya)

- Mammals:

Docodonts.... a group of beaver-like animals... the most impressive fossil of the group was found in Feb 2006

- oldest animal with fur

- demonstrates that mammals were radiating into a variety of habitats

III. Mesozoic Era

A. Triassic Period (250 - 205 mya)

B. Jurassic (205 - 146 mya)

C. Cretaceous (145 - 65 mya)

III. Mesozoic Era

A. Triassic Period (250 - 205 mya)

B. Jurassic (205 - 146 mya)

C. Cretaceous (146 - 65 mya)

- the warming trend of the Jurassic continues, and results in very high sea levels and the expanse of shallow seas over significant portions of continents

III. Mesozoic Era

A. Triassic Period (250 - 205 mya)

B. Jurassic (205 - 146 mya)

C. Cretaceous (146 - 65 mya)

- Plants:

Evolution of Angiosperms

Initially in low abundance

Come to dominate by end of Cretaceous

Gymnosperms

III. Mesozoic Era

A. Triassic Period (250 - 205 mya)

B. Jurassic (205 - 146 mya)

C. Cretaceous (146 - 65 mya)

- Plants:

Evolution of Angiosperms

Initially in low abundance

Come to dominate by end of Cretaceous

Gymnosperms

Angiosperms

Archaefructus sinensis

Science 2002

III. Mesozoic Era

A. Triassic Period (250 - 205 mya)

B. Jurassic (205 - 146 mya)

C. Cretaceous (146 - 65 mya)

- Plants:

Evolution of Angiosperms

Initially in low abundance

Come to dominate by end of Cretaceous

Gymnosperms

III. Mesozoic Era

A. Triassic Period (250 - 205 mya)

B. Jurassic (205 - 146 mya)

C. Cretaceous (146 - 65 mya)

- Plants:

Evolution of Angiosperms

Initially in low abundance

Come to dominate by end of Cretaceous

Gymnosperms

III. Mesozoic Era

A. Triassic Period (250 - 205 mya)

B. Jurassic (205 - 146 mya)

C. Cretaceous (146 - 65 mya)

- Inverts:

radiation of pollinators

radiation of pollinators and herbivores

ground beetles do not

C. Cretaceous

- Verts:

-Crocodylians

Sarcosuchus

11m

C. Cretaceous (146 - 65 mya)

- Inverts:

- Verts:

Ornithischians:

Stegosaurs give way to a variety of new

Ornithischian groups:

Ornithischians:

Ankylosaurs

Ornithischians:

Ceratopsians

Ornithischians:

Iguanodonts

Ornithischians:

Hadrosaurs

Ornithischians:

Pachycephalosaurs

C. Cretaceous (146 - 65 mya)

- Inverts:

- Verts:

Ornithischians:

Saurischians - Sauropods

The Titanosaurs (and they were still big)

The Titanosaurs

Andesaurus

40m (?) 80 tons (?)

incomplete skeleton

The Titanosaurs

Argentinasaurus

Largest one known with confidence, but there are bigger single bones....

35m 80-100 tons

incomplete skeleton but a hip girdle, vertebrae, and tibia

C. Cretaceous

- Theropods: carnivores get big!!

Carnosaurs

- Giant Allosaur cousins like:

Giganotosaurus

Longer than the largest Tyrannosaurus rex by 2m

40-45 ft... from Argentina (1995)

C. Cretaceous

Carnosaurs

- Giant Allosaur cousins like:

Carcharodontosaurus

40 ft - slightly smaller than T. rex

from Niger (1927)

C. Cretaceous

Carnosaurs

- Tyrannosaurs:

- Albertosaurus

C. Cretaceous

Carnosaurs

- Tyrannosaurs:

- Gorgosaurus

C. Cretaceous

Carnosaurs

- Tyrannosaurs:

- Tyrannosaurus (3 sp.)

C. Cretaceous

Carnosaurs

- Tyrannosaurs:

- Tyrannosaurus (3 sp.)

C. Cretaceous

Carnosaurs

- Tyrannosaurs:

- Tyrannosaurus (3 sp.)

Soft tissue from a femur?. 2005

C. Cretaceous

Carnosaurs

- Tyrannosaurs:

- Dilong paradoxicus

Feathered

C. Cretaceous

- Deinonychians

Deinonychus

Velaciraptor

III. Mesozoic

C. Cretaceous

- theropods (still)

- Deinonychians

Velociraptor

C. Cretaceous

- non-bird feathered dinosaurs: Sinosauropteryx prima (1996)

first non-bird dinosaur with feathers... a Cretaceous contemporary of birds

- Protobirds

- Protobirds: Sinornithosaurus (Jurassic)

- Protobirds: Microraptor (Cretaceous)

Protobirds:

- Deinonychians

Velociraptor

- Protobirds: Unenlagia (Cretaceous)

- Protobirds: Caudipterxy (Cretaceous)

- Protobirds: Protarchaeopteryx (Cretaceous)

- Protobirds: Eoalulavis (Cretaceous)

- Pterosaurs:

- Pterosaurs:

Pteranodon - wingspan 7.5 m

- Pterosaurs:

Quetzalcoatlus - largest ptersaur; 40 ft wingspan....

- Quetzalcoatlus - largest flying animal

Quetzalcoatlus - largest ptersaur; 40 ft wingspan....

- Mammals...

- Mammals...

- Multituberculates Dominate in Cretaceous

- over 200 species

The K-T Boundary

The K-T Boundary

hmm... a new star in the constellation of Orion...

THAT'S weird...

The K-T Boundary

The K-T Boundary

WHAT THE HELL!!!

It's the Ceratopsians... they're attacking...!!!

The K-T Boundary

The K-T Boundary

The K-T Boundary

The K-T Boundary