Vertebrate Fossil Record Flashcards

(189 cards)

1
Q

W hat are the features of the vertebrate fossil records

A

Almost exclusively bones and teeth, only made by the vertebrates.
Good against weathering
Soft tissue preservation is rare
Full skeleton is rare.

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2
Q

How are vertebrates reconstructed from bones

A

All bones fit together, sort tissue leaves marks which give an idea at how the bones fit together.
Small holes from blood and nerve sinuses in bones
Shows tendon and muscle attachments
Skin is more difficult to reconstruct and will be more or an estimate
Can tell is there was feathers

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3
Q

How can behaviour be determined from fossils.

A

Can snow reproduction by fossilised eggs and nests
Locomotion -

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4
Q

How can you determine diets from fossils?

A
  • Fossilised stomach contents are rare
  • Teeth show convergent evolution which tells you if they were herbivores or carnivores
  • Gastroliths are smooth pebbles which are picked up by animals that don’t have teeth, they help the animal grind the food int heir stomach
  • coprolites = fossilised faeces
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5
Q

What is palaeogeography?

A

The shifting continents
How land and sea have evolved

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6
Q

What are the 4 geological times?

A

Hadean = 4.55 Ga - 4.0
Archean = 4.0-2.5 Ga
Proterozoic = 2.5-0.54 Ga
Phanerozoic - 0.54- now

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7
Q

What are the smaller period of times?

A

Cambrian = 540-490Ma
Ordovician = 490-443 Ma
Silurian = 443-417 Ma
Devonian = 417-354 Ma
Carboniferous = 354-290 Ma
Permian = 290-248 Ma
Triassic = 248-206 Ma
Jurassic = 206-144 Ma
Cretaceous = 144-65 Ma
Cenozoic = 65-1.8 Ma

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8
Q

How many chordate groups are there

A

3

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9
Q

What are the 3 groups of chordates?

A

Vertebrates (craniates, have a defined head)
Cephalochordates (acraniates) - amphioxus or lancet, they are very small and spend time buried in sediment filter feeders
Urochordates

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10
Q

What are urochordates and their features

A

Tunicates or sea squirts
Non vertebrates
Attaches to rocks in the sea
Large pharynx, hundreds of gill slits

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11
Q

What are the key features of a chordate

A
  • nerve cord dorsal to digestive system
  • dorsal = back
  • notochord - stiff rod running the length of the body
  • myomeres - v shaped blocks of muscles which are segmented, allows flex for swimming
  • pharyngeal slits - for respiration and feeding
  • post anal tail - used in locomotion
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12
Q

What are the key vertebrate characters?

A
  • cranium - brain surrounded by skull
  • well defined sensory organs: nose , ear , eye with associated nervous. Tissue
  • backbone or vertebra
  • bone
  • Haeckel - vertebrate embryos, as an embryo humans have a post anal tail and pharyngeal slits
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13
Q

Pikaia

A
  • early vertebrae fossils
  • mid Cambrian
  • has sigmoidal myomeres
  • primitive notochord
  • distinct head with sensory organs
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14
Q

What is bone?

A
  • only in vertebrate animals
  • living structure = contains blood vessels and nerves in Haversian canals
  • made from collagen and apatite - crystalline calcium phosphate
  • apatite can also make denting - like bone but without trapped cells, enamel , inert crystalline apatite
  • some vertebrates can grow exoskeletal bones eg dermal bone
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15
Q

Haikouichthys and myllokunmingia

A
  • early Cambrian
  • chordate and vertebrate characteristics
  • no bone
  • most likely the first vertebrate
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16
Q

Anatolepis

A
  • late Cambrian to Ordovician
  • widespread
  • dermal bone only , denting around pulp cavity but no enamel
  • early vertebrate fossils
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17
Q

Conodonts

A
  • late Cambrian to end of Triassic
  • conodont elements - possibly teeth
  • fit together to make conodont apparatus
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18
Q

Agnathans, name 2

A

Living jawless fish
- hagfish : primitive eyes, muscular mouth , scavengers , no bone, no fins, large mucous glands
- lampreys: teeth and tongue. Used to attach to prey

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19
Q

What is a crown group

A

Living , share a set of defining morphological characteristics acquired over time

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20
Q

What is a stem group

A

Extinct , have some but not al characteristics

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21
Q

Ordovician agnathans

A
  • first record of complete fossil fish since Cambrian
  • features: large dorsal and ventral head shields, multiple paired gill opening some covered by bronchial plates, lateral lines
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22
Q

Silurian and Devonian agnathans

A

Great radiation of several groups of more or less armoured jawles fish in Silurian
Most extinct

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23
Q

Osteostracans

A
  • large bony head Shield with eye openings , weirdly shaped to help not being eaten
  • up too 10 paired gill openings
  • thick scales on body and tails
  • small pectoral fins and dorsal fin - prevents body tipping sideways and helps hydrodynamic to help move up and down
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24
Q

Gnathostones : 3 types

A

Placoderms: spirulian and Devonian
Chondrichthyes : sharks and rays
Osteichthyes : bony fish and tetrapods

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25
Placoderms
- bone in closed heads and shoulders - paired pelvic fins and pectoral fins and long dorsal fin - armoured plated
26
Chondrichthyes
- shark like scales recorded from late Ordovician and Silurian - endoskeleton of calcified cartilage which doesn’t preserve as well as bone - dermal scales of denting and enamel
27
Osteichthyes
- have swim bladders = gas filled , frees pectoral fins from lift, can hang in the water column - two major groups : ray fins(actinopterygii) , sarcopterygi (tetrapod ancestors) lungfish - ray fins or lobe fins
28
Ray fins
- oldest may be from Devonian - many subsequent diversifications - sturgeons - teleosts - 30,000 living, huge morphological variety
29
Lobe fin fish
- late Silurian - lungfish and coelacanths - tetrapodomorpha
30
Lungfish
- have modified swim bladder which helps them breathe air - can live in stagnant water - gills and lungs - aestivation
31
Coelacanths
- mid Devonian - last fossils in late Cretaceous - living in caves off coral reefs, rare and unchanged
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Tetrapodamorpha
- predatory fish in marine and fresh water - tetrapods evolved from this group - teeth on palate - tetrapod like pectoral fin bone arrangement - extinct by early Permian
33
On land in the Devonian
390 ma - small terrestrial plants in late Silurian and early Devonian - terrestrial invertebrate communities by early Devonian - proper forests by late devonian
34
Origins of the tetrapods Life on land
- spinal support for the body - a gravitational issue (get muscles and ligaments) - locomotion 1 : fins into legs - locomotion 2 : modification of limb girdles to support body, shoulder girdle separates from skull - pelvic girdle enlarges firm attachment of ilium to vertebral column via sacral rib
35
Evolution of eating and breathing in early tetrapods
- reduction in hinge joints in the skull - lower jaw hinges at one point at the back of skull between articulated bone in jaw and quadrate in skull - lung rather than gills
36
Reproduction in early tetrapods
- must return to water (amphibians) - or have desiccation resistant eggs (amniotes)
37
Water balance in early tetrapods
Need to drink a lot or reduce evaporation through skin Semi permeable membrane
38
Tiktaalik
- late Devonian - arctic Canada - robust shoulders and pectoral fins - pelvis is enlarged relative to other finned tetrapodomorphs - lacks ischium an attachment for sacral rib Link between fish and tetrapod
39
On land in the late Carboniferous
- coal swamps along the Pangaea equator - main plants : giant club mosses, lycopods trees (40m tall) , giant horse trails (15m tall), ferns, conifers, seed ferns -no broad leaved trees
40
Nyrany lake , late Carboniferous , Czech Republic
- vertebrate fauna : rare sharks and bony fish; diverse array of early tetrapods (20 species) including embolomeres, temnospondyls, microsaurs , aistopods and nectrideans ; four species of amniote - palaeoenvironment - equatorial enclosed lake surrounded by coal swamps ed by large river systems draining the uplands to N
41
What are the early tetrapods groups
- aistopods - embolomeres - mecttrideans - temnospondyls - eryops
42
Amphibians i
- anurans and urodelans - frog and toads (Anura) - earliest fossils are early Triassic, body modified for jumping - salamander and newts (urodela) - earliest fossils are mid Triassic
43
Key features of amniotes
- protective shell (calcareous or leathery) with underlying semi permeable chorionic membrane - allows for gas exchange , stops water from leaving - amnion - gas transfer to embryo - yolk sac - provides food - allantois - stores waste products - amniotic cavity - fluid filled, for physically protection of the embryo
44
Late Carboniferous amniote groups
- four main patterns of temporal fenestrae in amniote skulls ( anapsid , synapsid , diapsids) arose in the Carboniferous - holes in the skull for reasons unknown, maybe to reduce the weight of the skull - no good fossil record
45
Late Permian climate
Coal swamps disappear from Pangaea , restricted to china Ice caps at the North Pole
46
Permian pelycosaur synapsids
- late Carboniferous to middle Permian group - dominant terrestrial tetrapods (70% of genera) - herbivores and carnivores - some with sail backs - unknown what the function was - some had peg like teeth to strip the vegetation
47
Gergonopsids
- middle to late Permian synapsids - dominant carnivores of late Permian - mouth with wide gape and enormous canine teeth
48
Perm-Triassic mass extinction
95% of al species - 75% of tetrapod families - causes - volcanism , ocean anoxia - surviving major amniotic groups : cynodontia and neodiapsida
49
Triassic early climate
Hottest world climate ; interior of Pangaea arid, warm temperate polar region
50
Triassic diapsids : rhynchosaurs
- herbivores with beak like jaws ,like a parrot , nipping of plants Batteries of small teeth on palate - large claw on hind feet
51
Archosaur
- early Triassic carnivores , some late Triassic herbivores - by mid Triassic major split into : crocodile ancestors, ancestors of pterosaurs , dinosaurs (and birds) - major change in posture from sprawling lizard type legs to erect quadrupedal gait - changes in shape and arrangement of pelvis and ankle bone - more energy efficient
52
Late Triassic amniotic extinctions
- parareptila - synapsids except cynodontia - diapsids - most archosaurs except pterosaurs, crocodiles and dinosaurs - unaffected: testudines, lepidosauromorphs including modern lizards and snakes
53
Mesozoic marine reptile basic facts
- euryapsid skull pattern, evolved amongst the diapsids sometime before earliest Triassic - top marine predators during Mesozoic with sharks and in the late Cretaceous , mosasaurs - not dinosaurs , not closely related - newly formed flooded areas between areas between super continents - seas
54
The ichthyosaurs
- 155 ma history from early Triassic to late Cretaceous Features - dolphin or tuna like morphology (convergent evolution) - sped predators - reversed heterosexual tail - side to side swimming , end of vertical column goes into the bottom of the fluke - limbs modified into paddles - peg like teeth adapted for slippery foods - nostrils not at snout tip - long upper and lower jaws - huge eyes - largest proportion to body among the vertebrate - adapted to low levels of light - gave brith to live young as they couldn’t get onto land - born tail first
55
Grands in ichthyosaur evolution
- increasing in size and generally fishy (fusiform) morphology - increase in number of bones in paddle, separation of hip from spine
56
Plesiosauria
- late Triassic to late Cretaceous - most have long necks and small skulls - pliosaurs = short necks and massive skulls, short teeth - all have limbs modified into flippers ; massive bone support for ventral surface - don’t think they had a tail fluke , not for movement - no type of animal today with this type of morphology - flattened hips - thought they could maybe pull themselves on land
57
Turtles and tortoises
- Chelonia/testudines - diapsid amniotes with anapsid skull pattern - evolved in late Triassic
58
Features of turtles and tortoises
- very solid skull with horny beak with no teeth - skull formed of dorsal domed carapace and ventral flat plastron; opening for head , legs and tail - both aquatic and terrestrial forms - multiple occurrence of tortoise gigantism on oceanic island
59
Odontochelys
- first turtle ? - late Triassic of china - has fixed teeth instead of beak - fully developed plastron but only partial carapace = grew from expansion of ribs - helps explain carapace evolution , and how turtle shoulder girdle is inside ribcage rather than outside like other amniotes
60
Crocodylia, what are the 3 modern groups
- crocs - 3 modern groups : alligators, crocodiles , gharial
61
What are the features of crocodylia
- dermal bone scutes on dorsal surface - aquatic = both fresh and salt water - sprawling giant (mostly)
62
Lepidosaurs
- rhynchocephalians - fossils forms and living tuatara - squamates : lizards - lacertilians , snakes - Serpentes - lizards - generally very poor fossil record in Mesozoic , oldest fossils from late Triassic - mosasaurs - fully marine , late Cretaceous predators, can grow up to 10 metres long , large skulls, deep tails , limbs modified into paddles
63
Snakes
- poor fossil record - evolved from lizards - huge increase in vertebrae - oldest fossils from mid Jurassic - feeding methods = constriction or venom
64
Dinosaur groups in the origin of dinosaurs
- saurishchians - lizard hips - ornithischians - both had upright , digitigrade walking stance - walking on the tips of their digits - associated with running fast
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Early to mid Jurassic climate?
- interior of Pangaea remains arid - circum - Tethys tropical
66
Late Triassic climate?
‘Hot house’ world - warm temperate polar regions
67
Late Cretaceous climate
- climate warmer than today - no polar ice
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Therapod features
Late Triassic to latest Cretaceous carnivores - digitigrade - bipedal locomotion with toes 2-4 elongated - body balanced by long stiff tail but tail doesn’t drag on the ground - arm half length of leg ; 3 or less functional fingers in hand , 4 to 5 digits reduced - steak knife like teeth with serrated margins
69
Jurassic and Cretaceous theropods
- big range of body sizes and morphology -compsognaths = small dino: 70-140cm - ceratosaurs = skull horns and crests - tyrannosaurs = huge, up to 14 metres long, tiny arms , 2-3 fingers
70
Dromaeosaurs
- mid sized theropods with stiff tails - strong 3 fingered hands with mobile wrists - feet with backward pointing 1st toe and huge sickle claw on flexible 2nd toe - major predator at the time - large brains
71
Unusual theropods
- some exhibit very different morphology to typical theropods - not all theropods may have been carnivorous. - some exhibit very different morphology to typical theropods - long claws in therizinosaurus used like ground sloth - grasping for vegetation? - sauropods like teeth or beak in oviraptorids
72
Feathery theropods in china
- early Cretaceous - small theropod dinosaurs with feathers - caudipteryx - symmetrical feathers on tail and arms - sinornthiosaurus - Dromaeosaur with feathers and wishbone - feathers not used for flight , evolved for something else
73
Jurassic feathery theropods
- very elongated fingers - membranous flight membrane supported by styliform element
74
Early sauropods
- walk on all 4 limbs if they wanted to - prosauropods - late Triassic to early Jurassic - bipedal and facultative quadrupedal Features: - small skulls about 5% of body length - lanceolate teeth with serrated edges - tough vegetation strippers - long neck with 10+ cervical vertebrae , balanced by a long tail - have a thumb claw
75
Middle Jurassic sauropods features
- more 12+ and elongated cervical vertebrae - quadrupedal , on pillar like legs - shortened fingers and toes - nostrils and nasal bones moved back on skull - teeth peg like and restricted to front of jaws
76
Late Jurassic and early Cretaceous sauropods (monster herbivores) features
- huge size - pencil like teeth - cavernous vertebrae - hole in the neck vertebrae to reduce weight
77
Brachiosaurus
- late Jurassic to early Cretaceous - herbivore - 23m long , head above 12m ground - estimated 80 tonnes - longer front legs than rear legs - large spines on dorsal vertebrae - large neck muscles
78
Problems being big dino
- locomotion - pilllar like legs ( graviportal) - very thick bones - galloping impossible for modern elephants - huge weight estimated 50-100 tonnes for the largest sauropods, near maximum theoretically possible for terrestrial animals without all legs meeting in middle (~ 150 tonnes) - small surface area to body mass - overheating problems - getting enough to eat - sauropods are all herbivores and need to spend most of their time eating - blood supply to their brain - long neck mean blood supply to head is difficult - might have huge heart or valves in their arteries
79
Morrison formation floodplain USA
- swampy floodplain crossed by sediment rich rivers draining from ancestral Rocky Mountains to west - osteichthyans : 7 genera of actinopterygians - lissamphibia ( 7 frogs , 4 salamanders) - 3 turtles - Lepidosaurs ( 7 lizards, 1 snake , 3 sphenodonts) - 8 crocodiles - 4 pterosaurs - dinosaurs - saurichians ( 12 theropods , 14 sauropods); ornithischians ( 7 ornithopods, 1 stegosaur , 3 ankylosaurs) - mammals : 37, including7 multituberculates , all extinct groups
80
Ornithischians dinos
- bird hip pelvic hip bone - first fossils late Triassic - all herbivores - ornithopods and ceratopsians - stegosaurs and ankylosaurs
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Ornithopods features
- Jurassic to late Cretaceous - bipedal locomotion = ran on hind limbs - fusion of. Pubis and ischium - smaller front limbs - efficient chawing mechanisms - flexiblity in their jaw - probable cheeks
82
Hadrosaurs
- duck bill dinosaurs - “cows” of late Cretaceous — abundant and wide spread - modification of maxilla and premaxilla to form “bill” - tooth batteries for tough vegetation , eg conifer needles - thought to. Have moved on four limbs - hoof like features - communal nests with eggs, evidence of parental care - used ness for a long time - head crests containing hollow tubes - for signalling? - sexual dimorphism - reptile like skin
83
Ceratopsians
- “horned face” dinos - firstly bipedal , lattterly quadrupedal - hued modified skulls with pronounced beaks , and head frills and horns in late Cretaceous species - neural spines = large muscles attachments to keep huge head up - nests and eggs = parental care, elongated eggs - unknown what horns and crests were really for
84
Thyreophora
- armoured ornithischians - mid Jurassic to late Cretaceous - quadrupedal - stegosaurs and ankylosaurs - stegosaurs = bony dermal plates , tiny tubular skulls and tiny brains - dermal plates were not fused into the spine -bone spines at the end of the tail - ankylosaurs - huge amounts of dermal bone, some with tail club
85
Pterosaurs
- diapsids with uncertain origins - sister group to the dinosaurs - first for powered flight - first fossils late Triassic - 2 groups : phamphorhynchoids = all had long tails and teeth , late Triassic , pterodactyloids = late Jurassic , short tails and some are toothless - short body - laid eggs - coating of hair = for heating? , could have been endothermic - large sternum - reduced and fused hipbones - hip solid with new bone - prepubescent -pneumatic bones - 5 long toes , 4 fingers - pteroid bones = hollow ish to reduce weight - fight membranes attached to elongated 4th finger - pterodactyl bone and legs - flight driven by very bird like muscle arrangements - antagonistic pectoral is and supracoracoideus muscles both attached to sternum - good fliers but probably low take off speeds and tricky landing
86
Rhamphorhynchoids
- long tails - most had long widely spaced teeth probably for catching fish - some had smaller peg like teeth
87
Late Jurassic pterodactyloids
- may have been filter feeders - reduced tail vertebrae as with all later pterodactyloids - ctenochasma
88
Late Cretaceous pterodactyloids
- giant - largest flying creature too ever have existed - 11-12m wingspan - no teeth - elongated head crests in some species , function unknown
89
Cretaceous - paleogene extinction event
Wild fires and tsunamis , super heated material in the atmosphere caused n photosynthesis Extinct : - non avian dinosaurs - pterosaurs - some birds and marsupial mammal families - plesiosaurs - mosasaurs - some shark an teleost families - some invertebrates : ammonites, belemnites , some bivalve and plankton groups.
90
Bird evolution basic facts
- global distribution at land and sea - 10,000 species - flying and secondary flightless forms - all lay eggs - all covered in feathers = display and insulation - endothermic - not a good fossil record, small and have more delicate bones
91
Morphology of birds
- considerable modification of skeleton for flight - pneumatic bones - Pygostyle = reduced tail - fusion and reduction of bones in arms and legs - 4 toes - 3 or 2 forwards , 1 or 2 back - large keeled sternum - furcula. = acts as spring between shoulders in flight - swivelling wrists enables wings to be folded against body
92
Archaeopteryx
- ten specimens - late Jurassic age - long tail - identical to modern feathers - toothed jaws = o tooth serrations , interdental plates present - long bony tail - s shaped neck - short back - hand with 3 clawed fingers - separate tibia , fibula , metatarsals - 5 toes - downward pointing pubis - fucula - numeric vertebrae and pubis - feathers = asymmetrical - wings - solhofen lagoons = Germany , bottom of the lagoon is toxic , hyper saline, preserves fossils well
93
Solhofen vertebrates
- mixture of terrestrial animals brought in by streams to N and marine brought in from oceans in S - 4 turtles - theropod dino - ichthyosaur - plesiosaur
94
Evolution of bird flight
- feathers = in modern birds used for flight , insulation and display - variety of morphologies present in saurischian and ornithischians dinos - 2 flight evolution hypotheses: from the ground up (cursorial) , from trees down (arboreal) - arboreal =. Flying squirrels , lizards, frogs and snakes , use of half wings - cursorial evidence = partridge experiments, flapping proceeds gliding , allows for more efficient climbing
95
Confuciusornis
- large. Clawed hands -beak with no teeth - Pygostyle = reduction in tail - sternum with small keel - sexual dimorphism
96
Late Cretaceous US birds
- 2 taxa from shallow marine sediments of western interior basin - hesperornis - long beak with lots of teeth , flightless, reduced sternum and vestigial wing bones - ichthyornis =. Flying toothed shorebird
97
Bird evolution in Cretaceous
- claws on wings lost - finger number reduction - teeth lost - reduction and fusion of tail bones into Pygostyle - fusion of leg bones into tibiotarus and a tarsometatarsus - evolution of alula or bastard wing for better flight control at low speeds - many became extinct
98
Modern birds
- 2 groups separated on jaw structure - neognaths - most modern birds - palaeognaths = Tinamous and ratites : have symmetrical feathers on wings lost, all found in southern hemisphere , may have originated in northern in paleocene or Eocene
99
Eocene birds from messel , Germany
- palaeoenvironment : stagnant lake deposits surrounded by tropical forest - bird fauna includes ratites and a variety of neognaths including phorusrhacids , Gaston is , owls , swifts , no passerines
100
Mammalian characteristics
- endothermic = high energy requirements allows for polar living , also in birds - hair = keratin derived from skin - mammary glands = secrete mil - large brains - extended care of young - dentary squamsoal jaw articulation - 3 small bones in the middle ear - 3 cussed molar teeth
101
Jaw evolution in synapsids
Reduction in post dentary jaw bone size and change in position in Permian to Triassic synapsids - dentary bone increases in synapsids - simultaneous changed in bones forming jaw joint with post dentary bone size reduction: - early cynodonts - joint formed between quadrate in skull and articular in back of lower jaw - like modern reptiles and birds - later cynodonts have double jaw joints - mammals = joint between squamosal and dentary - jaw bones involved in old joint pushed behind new joint into the middle ear , malleus is articular , incus is quadrate , tympanic is angular - we can hear our jaw moving when we eat
102
Cynodonts
- first appeared in the Permian - survived the p-tr extinction and radiated in Triassic - both carnivorous and herbivorous examples - in early Triassic : lower jaw formed mostly of dentary , semi erect gait Later cynodont changed: - fully erect gait achieved by articulating head of femur bent inwards - deeper acetabulum - reduction and loss of lumbar ribs , related to evolution of the diaphragm , improved breathing - expansion of occultation of cheek bones , chewing greater food processing abilities
103
More cynodont changes related to chewing
jaw mechanics: - synapsid external adductor muscle gave rise to new temporal is and masseter muscles - increase in adductor muscle volume - increase bowing of zygomatic arch - all allow back to front and side to side chewing motion - reduction of tooth placement cycles : mammals once , reptiles continuous - more powerful bite
104
Early mammaliaform groups and Mesozoic mammals
- first true mammals from late Triassic = very poorly known - several lineages by late Jurassic but almost all fossils are isolated jaws and teeth of tiny animals(20-30mm skulls) - most very small , carnivorous , shrew like
105
Morganucodontids - Jurassic ‘shrews’
Big group of Mesozoic mammals ; common in early Jurassic in Europe , china, South Africa Last member mid Jurassic England Features: - expanded brain case enclosed entirely by bone - eye socket and temporal fenestra linked - no post orbital bar - cheek teeth divided into premolars and molars , increased specialisation - teeth replaced once = juvenile and adult set - loss of lumbar ribs - probably warm blooded insectivores with mammary glands - quite small mammals - still had ribs on neck bones - eye sucked and linked fenestra
106
Multiberculates
Largest group of Mesozoic mammals, belong to crown group mammals , late Jurassic. To Eocene , global distribution Features: - small rodent like omnivores - large incisors; no canines ; long gap to cheek teeth (as modern rodents) - last premolars modified into shearing blade - one species has epipubic or ‘marsupial’ bones in front of pelvis (as have modern marsupials and monotremes) - diasteamer = used to mix saliva
107
Changing views of Jurassic and Cretaceous mammals
- traditional view : mammals diversity suppressed in ‘dino-dominated’ Mesozoic - not entirely true - very poor fossil record - new Jehovah discoveries indicate Mesozoic mammas inhabited many ecological niches - from swimming , burrowing , to gliding
108
Volaticotherium
- similar to today’s flying squirrel - Jurassic to Cretaceous - had some with dexterous feet - all quite small mammals
109
Changing views of Jurassic and Cretaceous mammals
- traditional view : mammals diversity suppressed in ‘dino-dominated’ Mesozoic - not entirely true = very poorly known fossil record - new Jehol discoveries indicate Mesozoic mammals inhaitated many ecological niches - from swimming, burrowing to gliding - volaticotherium = similar to today’s flying squirrel - had some with dexterous feet - all quite small mammals
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Major modern mammal groups
Three groups form a sort of reproductive continuum: - monotremes = lay eggs - marsupials = give birth to tiny young; later development in external pouch - placentals = advanced development in uterus like in humans Latter two are sister groups - the therians
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Monotremes
- egg laying mammals - 2 modern groups : duck billed platypus in Australia only , echidnas (spiny anteaters) in Australia and New Guinea Features: - lay eggs ; enchidnas brood these in pouches - lots of ‘primitive’ skeletal elements, including epipubic bones in pelvis and small ribs on neck(cervical) vertebrae - no teeth as adults , juvenile platypus has molars - platypus = eat little invertebrates, sensitive beak , lay eggs in burrow
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Fossil monotremes
- sparse record in southern hemisphere only - gondwanan distribution - opalized early Cretaceous jaws and teeth , Australia - platypus like teeth , paleocene , Argentina Obdurodon , Oligocene and Miocene , Australia - fossil platypus
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Therain mammals
- marsupials or metatherians - placentals or eutherians - teeth: marsupials and placentals have tribosphenic molars - marsupials have four molars and three premolars - crown group - placentals have three molars and four premolars
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Marsupials
- give birth to tiny young ; later development in external pouch - pouch supported by epipubic bones in pelvis = also used to help posture? - dentition of up to 5 incisors ( more than placentals) 1 canine and 7 cheek teeth - some marsupial babies so tiny and underdeveloped at birth they breathe through their skin - no lungs - ‘Joey’ has developed forelimbs to enable it to climb into pouch - this form of reproduction significantly reduces dangers associated with long pregnancy
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Modern marsupials- Americans
- South America = opossums , shrew opossums - North America = Virginia opossum only - numbat, possum , koala , wombat
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Mesozoic metatherians
- first fossils metatherians in china in early Cretaceous , then North America - mid Cretaceous teeth and jaw fragments - by latest Cretaceous marsupials also found in Peru ( an opossum and another species) - majority still in North America , many became extinct in the k-pg event
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Marsupials worldwide
Marsupials worldwide in early cenozoic , endemic faunas develop in southern America (parallel with placentals) and Australia , where they have always been the main group
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South American cenozoic marsupials
- 15 families of insectivores, carnivores and some herbivores including opossums , shrew opossums and 2 groups of extinct large carnivores - borhyaenids - thylacosmilids (late Miocene - Pliocene) - marsupials sabre tooth’s
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Australian cenozoic marsupials
- greater diversity of morphologies and sizes than living fauna - most modern groups present by Oligocene - extinct taxa include: ditrotodontoids ( wombat like herbivores up to the size of a hippo , extinct Holocene) Marsupial lions eg. Thlacoleo ( related to wombats , extinct late Pleistocene ) - major faunal change in Pleistocene associated with drying of continent and associated spread to grasslands - big kangaroos replace diprotodontoids
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Parallel evolution of placental and Australian marsupial mammals
- marsupials match almost all placental feeding adaptions except flying insectivore and any aquatic lifestyles - marsupials are declining in numbers today in Australia under all sorts of pressures including imported placental competition and predation - however not being out competed in the americas
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Jurassic eutherian mammals
- juramaia , middle to late Jurassic , china - jaws with 3 molars and 5 premolars - not a member of the crown group placentals
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Cretaceous placental mammals
- 10 or so families from Cretaceous in north and South America , Mongolia and china - eomaia , early Cretaceous , china , jaws with 3 molars and premolars , epipubic bones present , probable sister group to the placentals
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Paleogene palaeoenvironments
- climate of paleocene and Eocene = very warm and no ice caps - lush forests covered most of lands surface from tropics to poles - in Oligocene Antarctica split from Australia ; drake passage formed and the cold circum - Antarctic current developed - Antarctica got much colder ; glaciers formed ; global climate cooled
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Mid paleocene mammals , Montana
- no larger than a sheep - of those groups present 75% are extinct today
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Messed lakes , Eocene , Germany
Vertebrae fauna : - osteichthyans : actinopterygians ( 2 genera of Holsteins. , teleosts) - lissamphibia ( 3 frogs , 1 salamander) - reptiles : 3 turtles , Lepidosaurs ( 7 lizards , 4 snakes ) 6 crocodiles - 12 birds - 2 marsupials Placentals : - 4 insectivores , 3 bats , 1 primate - 1 pangolin - 1 anteater - 3 rodents - 2 carnivores - 1 creodont - perissodactyls ( 1 horse , 1 rhino) - 2 atriodactyls
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Carnivore characters
- modification of teeth for carnivorous diet - carnassials - expanded , blade shaped upper premolar 4 and lower molar 1 , acts like shears for cutting meat - large canine teeth for puncturing prey - peg like incisors for gripping prey and grooming - some bone crushing forms have broad premolars and molars with thick enamel - short simple gut - result of eating high energy food - large brains ; complex hunting behaviour - forward facing eyes for binocular vision - good sense of smell
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Laurasiatherians
Bats - tetrapods take to the air - 1240 species , 25% of all mammals Carnivores - dominant predatory group of mammals today - 280 species
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Early carnivores
- late paleocene and early Eocene - small cat like arboreal and ground living carnivores - small powerful limbs and plants grade feet - by late Eocene and early Oligocene carnivores diverged into two groups separated by morphology of ossified auditory bulla , claw retract ability and muzzle length : the deli forms and the carnivores
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Feliform evolution
Eocene = civets Civets diverged into cats in Oligocene Civets diverge into hyenas in Miocene Oligocene - mongooses
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Cats - felids
Early cat genera in Oligocene , gave rise to two groups in the early Miocene , cats with conical canines and sabre tooth cats Large cats have reduced range today Features : - molars reduced to two in each jaw , don’t have much chewing ability - digitigrade - on the tips of their toes - retractable claws - long tails , generally for balancing
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Sabre tooth cats
- mega fauna - elongated blade shaped canines , flattened laterally - Large incisors - sabre teeth developed independently in three mammal groups in cenozoic : niimravids , felids. Marsupias - had a very wide gape , as the sabre teeth would get in their way so had to open wide to actually get anything in their mouth - lots of fossils have broken sabre teeth so means they could be damaged easily - uncertain to all knowledge as there is none today
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Caniform evolution
Plantigrade locomotion evolved in Eocene , from that bears and pandas diverged in Eocene From plantigrade raccoons diverged in Oligocene From plantigrade mustelids diverged in Miocene Miocene = dogs from digitigrade Pinnipeds in Oligocene
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Dogs - canids
- long legged digitigrade carnivores and omnivores - pack behaviour common - two post carnassial grinding molars - better sense of smell than cats - more molars teeth ,better ability to crush food up
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Pinnipeds
- return to the sea - seals , sea lions , walrus - carnivores adapted for aquatic life - sea and fresh water - blubber under skin for insulation - well developed for diving reflex - limbs modified into paddles - reduction in size of the proximal bones , expansion of distal bones - long fingers and webbing between toes - flexible spine - large canines ; other teeth alike - walrus uses long canines for digging - earliest pinnipeds from early Miocene of North America
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Bats - Chiroptera
- widespread and abundant flying mammals - two groups : microchiropterans ( echolocating ) and megachiropterans - fruit bats. - ear region modified for echolocation - flight membrane of ski spread between elongated fingers 2-5 ; claw on thumb (micros) and finger 2 (mega) for climbing - nocturnal - powerful anticoagulant in saliva of vampire bats - long humerus and radius ; ulna reduced and fused to radius - shorter girdle modified for attachment of large flight muscle - expanded scapula - broad ribs and sternum with small keel - feet turned backwards for hanging upside down - fist bat fossils from late paleocene - whole specimen rare for fossils - fragmented teeth and sometimes abundant in cave deposits
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What are the 2 groups of modern cetaceans
Baleen whales - mysticetes - toothed whales - odontocetes
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Features of modern cetaceans
- nostrils are on the top of the skull - blowholes , air breathing mammals , more efficient at the top of the head - teeth simplified or lost completely - modification of the ear bones for hearing underwater - no hind limbs or pelvis (vestigial in right whales) - front limbs modified into steering paddle - horizontal tail fluke - cervical vertebrae partly or completely fused - no neck - hairless streamline body - thick insulating fat layer ( blubber) under skin - terrestrial ancestry : breathe air; give birth in water and suckle young with milk - beluga whales have a neck
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Toothed whales
- orca, sperm whales, hubby beaked whale , dolphin - echolocation : high frequency sound focussed by (melon) on top of their skull , goes a long distance , sound comes from throat , used to locate and stun prey - one nasal opening , resulting in asymmetrical skull - numerous conical teeth in dolphins , spade shaped in peorpoises , can help catch slippery fish - tooth loss in sperm whales in their upper jaw - beaked whales have no teeth , some have a few - all swallow whole as they cannot chew
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Baleen whales
- no teeth , filter feeder using keratin baleen plates hanging from upper jaw - use large tongue or expandable throat used to push water through baleen plates - prey range from krill to schooling fish - hugely elongated skull bones and lower jaw , both nostrils present - large to giant size - blue whale up to 33m long and 136 tonnes - biggest animal ever
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Cetaceans evolution
- share ancestry with artiodactyls - first cetaceans from early Eocene - archaeocetes gave rise to early mysticetes and odontocetes in late Oligocene - modern cetaceans groups radiated in late Miocene
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Archaeocetes
- first fossils found only in Pakistan and north west India - after protocetids found worldwide - from fully terrestrial pakicetids to fully marine , protocetids in around 4 million years in Eocene - incredibly rapid evolutionary transformation - protocetids gave rise to basilosaurs in late mid Eocene
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Pakicetids
Fossils found in early Eocene in river deposits - terrestrial animals with 4 fully functioning limbs , maybe to wade in streams - share details of ear structure with later whales - pointed incisors - cheek teeth occlude - able to chew food - cetacean evolution
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Abulocetids
- cetaceans evolution - fossils found in early to mid Eocene estuarine deposits - fully functioning in legs but reduced in size compared to pakicetids - large jaw and teeth
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Remingtinocetids
- cetaceans evolution - fossils found in earliest to middle Eocene in coastal deposits - very large skull - small eyes - body like those of the Abulocetids
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Protocetids
- fossils found in early to late Eocene in coastal and fully marine deposits in Pakistan , India , Egypt , Nigeria , south east us - first whales with wide geographical distribution - probably ancestral to all the later whales Features: - hind eggs with 4 long toes , probably webbed - front legs with 5. Fingers , middle 3 weight bearing with small hoofs - locomotion may be like modern sea lions - reduced number of teeth , occlusion of cheek teeth , chewing ability - dorsal - ventral flattened caudal vertebrae in some later species : tail fluke
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Basilosaurs
- cetaceans evolution - first fossils found in marine sediment in late Eocene , world wide distribution by late Eocene Features : - very small hind limbs and pelvic bones not connected to vertebrae - functioning knee and several toes - front limbs modified to flippers , limited mobility of wrist and elbow - large number of elongated lumbar vertebrae - dorsal ventrally flattened tail vertebrae = tail fluke - large size , up to 20 m
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Nostrils to blowholes evolution
- major change in position from mid Eocene to Miocene - elongation of snout or shortening of snout which moved the nostrils to the top - squashing bones helped this move
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Perisodactyls and artiodactyls
- ungulates - larger hoofed herbivores - distantly related laurasiatherians groups : Perissodactyla = odd number of toes Artiodactyla = even number of toes - not that closely related - both evolved in early Eocene from unknown ancestors, replaced earlier mammal groups as main herbivores - share many features of diet and locomotion - 6 genera of perissodactyls vs 79 of artiodactyls - caecal fermentation vs rumination
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Neogene climate
- similar climate belt to today but warmer - palm trees and crocodiles in the uk - Australia was wetter - grasses radiated in Miocene = productive for food for herbivores , biomass is more then if they were in a forest - savanna replaced paleogene broadleaf forest
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Perissodactyla
- horses, rhinos , tapirs - two extinct groups : brontotheres and chalicotheres - brontotheres - browsers that appeared in early Eocene , extinct by the early Oligocene , cow sized , strange bone on the snout - chalicotheres - bizarre beast with back legs shorter than front , fed on the leaves ; small hooves on fingers , claws on toes , probably walked in knuckles . Extinct by the end of Pleistocene
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Horses features
- unguligrade locomotion for fast running : reduction in bone in the distal part of bones - short proximal leg bones - elongation of those remaining - single hoofed toes in both front and back legs - cheek teeth adaption for brazing grass : continuously growing , deep rooted , high crowned - complex folding of enamel and denting on surface - diastema present = mixing food with saliva
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Eocene horses
- small mammals ( terrier sized) with hoofed toes - three hind , 3 front - just like early tapirs - complete tooth rows , molars small and low crowned - had canine teeth
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Later horse evolution
Happened mostly in North America Main features - size increases - lengthening of distal leg bones - reduction in digits - increase in relative proportion of front of skull - increase in tooth length and size of grinding surface
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Rhinoceroses
- probably evolved from early tapirs in Eocene - early rhinos small and hornless - similar in shape to early horses and tapirs - radiation into a number of groups in Oligocene and miocene including indricotheres - largest land mammal of all time , up to 7 m tall and possibly 15 tonnes in weight
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Later rhinos
- rhinos with horns made from keratin radiated in Miocene Include - Pleistocene woolly rhino from Europe and Russia - modern rhino - found in Africa ( black and white rhinos) and Asia ( Indian , Sumatran and Javanese ) are all highly endangered
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Artiodactyls
Even number of toes ungulates Groups: - basal artiodactyls - bundonts = pigs and hippos - selenodonts - camels, giraffes , cattle , deer, antelope
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Artiodactyls `
Even number of toes ungulates Groups Groups : - basal artiodactyls - bunodonts - pigs and hippos - selenodonts - camels , giraffes , cattle , deer, antelope
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Basal artiodactyls
- early Eocene to Oligocene - five fingers - 4 toes - weight on hoofed toes , 3,4 - fibula , ulna and clavicles present ( later lost)
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Pigs
Radiated in late Eocene but only 8 genera today Characters - bunodont molars = square in sections with bulbous cusps ; reflection of omnivorous diet - large canines ( tusks) with triangular cross section used for digging , display, fighting and defence - 4 toes, only central 2 touch the ground in pigs
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Selenodonts
- successful group today , 70+ - characterised by having selenodont ( moon tooth) cheek teeth for chewing tough vegetation - some form of ruminating stomachs 2 groups - camels and strict groups - deer ,cattle, cheep, antelopes = ruminants
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Ruminant
- appeared late Eocene - selenodont cheek teeth = for chewing tough vegetation - upper incisors lost = replaced by horny pad ; reduced or lost upper canines - 2 groups : traguloids and pecorinos - traguloids - most early genera and extinct mouse deer ; 4 toes but only 2 reach the ground ; no horns ; 3 chambered stomach - per oceans - giraffe , deer , cattle , sheep , antelope ; 2 toes ; all have bone horns ; 4 chambered stomach ; mid Miocene radiation - linked with radiation of grasses
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The bovids
- Cattle, sheep, antelope - most successful ungulates today: 50 genera, 115 species - The. Most important group of vertebrates to humans domestic sheep. , goats and cows
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Primate skull characteristics
- big brains ; high encephalisation quotient - reduced snout - decreased reliance on sense of smell - forward facing eyes = stereoscopic vision for arboreal existence - excellent colour vision - post orbital bar behind eye for protection ; post orbital septa in tarsiers , makes and apes
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Characteristics of primates
- body of primates not particularly specialised - pendactylyl = five fingers five toes ; primitive placental mammal characters shared with rodents for example - grasping hands and feet ; opposable thumb and big toes - nails rather than hooves or claws on at least one digit ; monkeys and apes have nails on all digits - very flexible limbs = monkeys and apes have complete rotation of arm around shoulder for arboreal living
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Plesiadapiforms
Primitate evolution - paleocene to mid Eocene Features - elongated skulls with eyes on side of the head - large incisors and diastema ( rodent like) - no post orbital bar - most have claws only - most didn’t have an opposable toes
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Living strepsirrhines ( primate)
- lemurs - lorises - pottos - bush babies - all have moist nose , tooth comb and toilet claw on the second toes of the hind legs - evolved from adaptiformes in paleogene ( adaptiformes early Eocene to late Miocene )
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Haplorhine primates
- anthropoids = monkey and apes ‘ higher primates’ - tarsiiformes = omomyids (extinct) and tarsiers; adaptions to leaping , powerful hind limbs
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Early anthropoids ( primates)
- either Asia or African origin - extinct groups in Eocene and Oligocene - platyrrhines ( new world monkeys) and catarrhines ( old world monkeys and hominids) split in the Eocene
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Platyrrhines ( new world monkeys)
- long tails ; some prehensile - poor thumb and finger grip - eg spider monkey
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Cercopithecoids ( old world monkeys)
- none have prehensile tails - better thumb and finger grips - eg Barbary macaque
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Apes
- chimps - gorillas - orangutan - gibbons - humans - big bodies - no tails - big brains - possession of future - not instinctive
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Ape evolution
- proconsul , lower Miocene , east Africa Features - no tails - relatively large brains - 150cm3 - stretched elbow joints for brachiation - small molars - large canines - primitive features
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Branching between gorilla and human
- DNA difference : gorilla - human = 1.62% Chimp - human = 1.24% - indicates the split between gorilla and humans happened between 8.4 and 6.2 ma and between chimps and humans only 6.2-4.6 ma - this evolution took place exclusively in Africa
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Homo sapiens characters
- upright walking -bipedalism - really big brains - highest encephalisation quotient - speech - possession of culture
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Bipedalism
- entrance of spinal chord in skull ( foramen magnum ) beneath , not behind skull - s shaped spine = bad backs - short bowl shaped pelvis - long leg bones ; straight hinge knee ; flat feet with straight toes ; big toe not opposable
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Trends in primate evolution
- increase in brain size in relation to body size - evolution of increasing behavioural complexity - eyes move to front of face for stereoscopic vision - increasing protection of eye sockets with bone - decrease in muzzle length - decrease in olfactory sense -nails replace claws - increase in gripping ability with opposable thumbs and toes - increase in parental investment in young
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Human evolution
- Darwin suggested in 1871 that humans evolved from apes - corroborated by fossil and molecular evidence - DNA differences between chimps and human : 1.24% - indicates the split between chimps and humans between 4.6 and 6.2 ma in the latest Miocene or earliest Pliocene
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Fossil humans ( hominids)
- currently at least 17 species ranging in age from latest Miocene to present - highly competitive field to find fossils - many species known from fragmentary material ; tendency to name each new bit of bone as new species - in Pliocene and Pleistocene at least three co existing hominins in Africa - only one species today
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Oldest hominins
- 6-5 ma - includes sahelanthropus ; 6 ma , chad ; complete skull - fossils show hominin looks similar to chimp/gorilla - shows bipedalism occurred well before big brians - show the split between chimp and us happened 6 ma
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Ardipithecus
- Ethiopia , 4.4 ma - skull volume 300-350cm3 ; chimps 400cm3; us 1400cm3 - for amen magnum directly beneath brain case = bipedalism - projecting jaws giving a dish shaped face - flat nose - small canines - 1.2 m tall ; around 50kg - long arms in relation to body ;; human like hand ; opposable big toe ; adaptions to arboreal life
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Australopithecus afarensis
Human evolution - east Africa , 3.7-2.9 ma -skull volume 415 cm3 - hips show efficient bipedalism - retains relatively long arms - still partly arboreal? - curved finger and toe bones - diastema between canines and incisors - ‘lucy’. 40%complete female skeleton found in 1978 - features : 1.2 m tall , conical rib age = ape like pot belly
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Laetoli footprints
- human evolution - volcanic ash field in Tanzania ; set like cement after rain - 3 individuals ; one child , 2 adults , one walking in the footsteps of the other - proves bipedalism in hominins at 3.75 ma
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Australopithecus africanus
Human evolution - South Africa ; 2.8-2.4 ma - 1.3 m tall - 45 kg - skull volume 445 cm3 - flatter face
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‘Robust’ Australopiths
- lived alongside other australopiths and early homo species - bodies like other contemporary australopiths - 1.75 m tall , 50kg - robust skull with sagittal crest - huge jaw muscles - huge premolars and molars with thick enamel - diet of tough plant food on grassland ; ‘gracile’ Australopiths - fruit and leaf eaters in more wooded areas - showed sexual dismorphism which is higher than in humans
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Genus homo
- characterised by really large brains and small teeth - first are homo habilis and h.rudolfensis ; some classify as Australopithecus due to brain capacity being not much larger than contemporary australopiths - Kenya 2.4 -1.5 ma ; ~ 1.3 m tall ; skull volume ~ 700 cm3 - oldowantools from 2.4 ma - simple capers made by h.habilis
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Homo erectus
- evolved in Africa - 1.7 ma , then moved quickly across the world , first hominin found outside Africa , 200ka - skull volume ~ 830 cm3 , later 900-1100 cm3 ( Chinese erectus) - primate skull features - strong brow ridges , heavy jaw with no clear chin - fully modern bipedal body - 1.6 m tall at 12 yrs - increased in sophisticated tools - acheulean tool culture appeared around 1.5 ma in Africa - tools used to hunt large animals - evidence of fire used eg cooking
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Homo neanderthalensis
- adapted in ice age , climate of Europe and Near East , lived alongside and hunted wholly mammoths and rhinos etc - appeared in Europe around 200ka , disappeared 35 ka , at the same time the modern human arrived - interbreeding or genocide? - very robust bodies - relatively short legs - strong joints - Inuit patterns - skull = strong brow ridges , projected face, big nasal cavity , weak chin , large teeth , skull volume on average larger than modern humans 1500cm3 - Neanderthal culture : burial of bodies ; rituals ; coking ; building of animal hide shelters ; mousterian toolkits - 60 different types including saws and needles for sewing clothes - could Neanderthals converse with modern humans? = hyoid bone and FOXP2 gene suggest yes
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Homo sapiens
- world domination - evolved in Africa ~ 200ka - reached Australia by 50ka - Europe and Russia by 35ka - americas by 12ka , possibly 32 ka - Polynesia 2-1ka - art from 70ka , shows evidence for abstract thinking - agriculture from 10ka in Middle East and later C.america and china = population explosion - cities from 6 ka in Iraq , today host huge populations