AOS 4 Flashcards
(34 cards)
what is mass extinction
when a larger-than-normal number of groups become extinct on regional and global scale
* evolutionary opportunity for other species to thrive and diversify
evidence for evolution
- fossils
- biogeographical distribution
- comparative
- anatomy - structural morphology
- embryology - developmental biology
- molecular homology - DNA and amino acid sequences
conditions that favour fossilisation
- rapidly buried
- protected from scavengers
- prevented from decomposition by low oxygen levels and low tempratures
- organisms having hard structures (won’t decompose as rapidly)
process of fossilisation
- an organism dies and is rapidly buried
- protected from scavengers
- prevented from decomposition by low oxygen levels + low temperatures
- continued deposits of sediments bury it more and more deeply
- over time the molecules in the organism (usually the hard parts) are replaced by minerals from groundwater
- gradually, the weight of the overlying sediments compresses the original sediment layer so that it becomes rock
- over time the rock is eroded, uplifted through the movement of tectonic plates or excavated
timeline of life on earth
- prokaryotes
- first unicellular eukaryotes
- first multicellular eukaryotes
- first vertebraes (jawless fish)
- first insects
- first land plants
- first amphibians
- first ferns
- first reptiles
- first conifers
- first dinosaurs
- birds
- first mammals
- first flowering plants
- primates
- humans
mineralised/petrified fossils
organic material of a structure replaced by minerals
mold fossils
- form when a mineralised/petrified fossil dissolves and leave an impression of the original
- these can be filled in to make cast fossils
trace fossils
- form when traces of activity are buried before they are erased and turn into rock
- eg footprints, teeth marks, scats (faeces)
purpose of fossil record
- the fossil record reveals that over time changes have occurred in the types of organisms living on this planet
- provides evidence in support of the prediction that ancestral species will appear before the species that descend from them
fossil/faunal succession
- based on the premise that strata accumalates in chronological order
- fossils in lower strata are older than fossils closer to the surface
- fossils in lower strata are less complex than strata closer to surface
relative dating
- sedimentary rocks form in layers (strata)
- newer layers are at the top and the older layers are at the bottom
- can determine relative age from that (as in newer or older - not the specific time)
index fossils
- index fossils can be used to determine the relative ages of rock strata anywhere in the world
- presence of index fossils in rock strata in widely separated regions of the world can identify these rocks as having the same age.
- must be
- abundant
- distributed worldwide
- existed for only a short period of time
transitional fossils
- can tell us about major changes - evidence of evolution
- is the fossilised remains of a life form that exhibits traits common to both an ancestral group and its derived descendant group
- e.g: archaopteryx - dinosaur and modern birds (claws on wings + feathers)
absolute dating techniques
- radiometric dating is the most common way to find the actual age of a fossil (rock)
- measure the relative amounts (decay) of radioactive materials (parent) and their daughter products
- the radioactive isotopes (parents) spontaneously decay or break down over time to form stable daughter products
relative vs absolute dating
relative age provides a comparative age whereas absolute age provides a more precise numerical age
half-life
half life → the time taken for half of the original radioactive isotope to decay
carbon dating
- carbon 14 will decay into nitrogen 14 (half-life of 5700 years)
- living things take in C14 when they eat living things stop taking in C14 when they die
- by comparing the amount of C14 and N14, the time since death can be determined
- limitation: can’t be used to date fossils older than around 50000 - 60000 years, there are very small amounts of carbon 14 left in the organic matter
speciation
the formation of a new species
process of speciation
- variation of characteristics is present in the population
- breeding population becomes isolated
- different selective pressures applied to isolated populations, random genetic drift, mutations
- b/c of natural selection, some characteristics are favoured over others
- those best suited to the environment survive
- survivors reproduce and pass on favourable genes + traits to offspring
- frequency of genes for new traits increases
- overtime, differences and mutations accumulate resulting in speciation
definition of species
organisms that can breed and produce fertile and viable offspring
allopatric speciation
- Initially a population (or populations) of the same species becomes isolated by a geographical barrier.
- Over time the isolated population(s) is exposed to different selective pressures and accumulates
- sufficient differences to the original population so that it forms a new species.
galapagos finches
- 13 volcanic islands w/ a variety of habitats - arid regions and mountainous regions
- after finches had arrived on an island they would become geographically isolated
- differing environmental selection pressures on each of the islands based on food availability (main environmental pressure)
- caused change in beak shape bc of diff food source
- no gene flow
sympatric speciation
- members of a populations living in the same area diverge to become 2 species
- no geographical barrier - both species continue to inhabit the same geographic region
- non-geographical barrier isolates populations from each other (active day/night) - some gene flow
- isolated populations are subject to different selection pressures → different phenotypes are favoured
- over generations, genetic divergence occurs
- responds to diff environmental pressures → different phenotypes and isolated populations change
- when the population come together again - can no longer interbreed - two separate species (2 distinct gene pools and different species)
lord howe island palms
- there was variation in the lord howe island population
- shift in nutrient content in the soils which caused a shift in flowering times
- those that flowered at the same time would interbreed
- over time there was accumulation in the differences and mutations in the palms
- speciation occurs and the two species can no longer interbreed