patterns of evolution Flashcards

lecture 12 - Mark Briffa

1
Q

macroevolution

A

speciation events or splits from a lineage

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2
Q

microevolution

A

changes within a species or within a lineage

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3
Q

the fossil record - problems

A
  • new branches should appear to be gradual as microevolutionary changes accumulate
  • but in fossil recoed new species appear suddenly

explanations :

  1. major gaps in fossil record - gradual transitions ar absent
  2. evolutionary chnages happen suddenly in short bursts
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4
Q

punctuated equillibrium

A

the idea that evolution occurs in spurts instead of following the slow, but steady path that Darwin suggested

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5
Q

phyletic gradualism

A

model of evolution which theorizes that most speciation is slow, uniform and gradual

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6
Q

phylogeny

A

the history of the evolution of a species or group, especially in reference to lines of descent and relationships among broad groups of organisms

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7
Q

adaptive radiation

A

rapid increase in the number of species with a common ancestor, characterized by great ecological and morphological diversity

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8
Q

convergent evolution

A

the process whereby distantly related organisms independently evolve similar traits to adapt to similar necessities

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9
Q

analogous characters

A

having similarities in functions but different evolutionary origins

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10
Q

homologous characters

A

derived from the same common ancestor

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11
Q

co-evolution

A

the process of reciprocal evolutionary change that occurs between pairs of species or among groups of species as they interact with one another

happens when two or more species directly influence each other’s evolution = exert selection pressure on each other

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12
Q

co-adaptations

A

the process by which two or more species, genes or phenotypic traits undergo adaptation as a pair or group

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13
Q

trilobites and predators ( arms race )

A
  • hard exoskeleton appeared in Cambrain arthropods
  • the sea became dangerous at the time
  • trilobites under strong selection pressure to avoid predatation
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14
Q

fossils

A
  1. transformed body parts
    - shell, bones, teeth
  2. activity ( ‘trace fossils’ )
    - burrows, footprints
  3. preserved remains ( ‘sub fossils’ )
    - shells, remains in amber
  4. organic cheicals
    - any body parts
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15
Q

step one : how fossils are formed

A

body survives long enough after death to undergo fossilisation

  • soft parts are destroyed quickly
  • few fossils of soft bodied organisms
  • even hard parts are likely to be destroyed
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16
Q

step two : how fossils are formed

A

remains must become buied in sediment at the bottom of a water column

  • fossils are only found in sedimentary rocks

the chance of fossilisation depends on proxiity to sediment

  • terrestrial = low
  • in water/on sediment = medium
  • in sediment = high
17
Q

step three : how fossils are formed

A

permineralization

  • sediement covered by more layers
  • compacts into rock - may deform or destory the fossil
    (or)
  • hard minerals leach out and rocks impregnate the remains
  • original compounds replaced and leach out
18
Q

step four : how fossils are formed

A

exposure ( the ‘unlikely’ event )

  • fossil means something dug up
  • tectonic pressures can move the fossil around
  • re-expose it in a terrestrial area
  • can also be lost forever
19
Q

radio-carbon dating - dating fossils

A
  • 5730 years after death 1/2 the C14 to N14
    ( C14 half life = 5730 )
  • can work out date of death by examining the ratio
  • only for fossils up to 40,000 years
20
Q

volcanic ash - dating fossils

A
  • many sediments contain volcanic ash (‘tephra’)
  • Potassium and Argon ( unstable isotopes ) in ash
  • decay ore slowly that C14 - fossils older than 100,00 years
21
Q

paleomagnetic dating - dating fossils

A
  • currents in Earths core change direction of magnetic field ‘normal’/’reserved’
  • determines allignment of magnetic particles when rocks form
  • age rocks by comparing the polarity to cores of rock from sea bed
22
Q

relative dating - dating fossils

A

compare fossils to fossils of known age and other strata that lookk similar

23
Q

paleontology

A

study of fossils

24
Q

Cretaceous

A

65 - 144 mya

extinction of most dinosaurs

Sinosauropteryx ( dinos )
- melanosomes : contain the pigments in hairs and feathers

25
Q

Jurassic

A

144 - 206 mya

’ quarry dinos ‘

very large herbivores

4 species, up to 26m, estimated weight 50 - 113 tonnes

26
Q

Triassic

A

206 - 251 mya

ichthyosaur ( ‘fish lizard ‘ ) evolved from terrestrial reptiles that returned to the sea

predated earliest dinosaurs by 20 my just before last dinos

cetaceans were not the first group to return to the sea

27
Q

Permian

A

251 - 290 mya

terrestrial tetrapods, arthropods, plants and algae

fusulinds - protists with a hard shell

ammonites - molluscs with a hard shell

28
Q

Carboniferous

A

290 - 354 mya

coal deposits due to apperance of bark bearing trees

no lignin digesting bacteria

atomspheric O2 80% higher than today

allowed gigantism to evolve on land and in the sea

29
Q

Devonian

A

354 - 417 mya

lungfish ( first appeared )
- ansestor of tetrapods

tetrapod colonisation of land

first fossil insects

first angiosperms ( flowering plants )

Rhynie Chert ( sedimentary deposit )
- contains evidence of vascular plant and fungal filaments growing in plant tissue
30
Q

Silurian

A

417 - 443 mya

cooksonia, one of the earliest terrestrial plant fossils

31
Q

Ordovician

A

443 - 490 mya

Naultiloids - shell producing cephalopods
straight or curled shells - divided into chambers
- extant species

32
Q

Cambrian ‘ expolosion ‘

A

490 - 543 mya

Trilobites

  • heavily armoured marine arthropods
  • earliest example of animals using weapons
  • rapid evolution
  • 15000 + species recognised
  • 9 orders
  • most animal classes first appear in the Cambrian