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56 Cards in this Set

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evolution definition

cumulative change in the heritable characteristics of a population over successive generations

full plant classification

Kingdom: Plantae


Phylum: Angiospermophyta


Class: Rosids


Order: Rosales


Family: Rosaceae


Genus: Rosa


Species: Acicularis

evidence for evolution

1 fossils:




2 selective breeding:




3 homologous structures:



1 fossils

the sequence in which they appear in the earths rock match with the sequence they were expected to evolveplants then animals

2 selective breeding:

form of artificial selection, humans intervene to produce desired traits in offspringresults in diverse breeds of domesticated animals like dogs (racing, toy), cows (normal vs. wild belgian blue) and horses

3 homologous structures:

homologous structures illustrate adaptive radiation: several new species rapidly diversify from an ancestral source so they use their COMMON STRUCTURES for DIFFERENT FUNCTIONS


pentadactyl limb: human hands, bird wing, whale fins


divergent evolution due to common ancestry



analogous structures



DIFFERENT STRUCTURES FOR COMMON FUNCTION


convergent evolution is the independent evolution of similar features in species with distinct lineages


eg wings in bats, birds butterflies or eyes in humans and octopuses


common selection pressures



peppered moth evolution

soot form factories blacked the bark

soot form factories blacked the bark

Natural selection explanation


and eg

Charles Darwin: survival of the fittest


VARIATION – genetic variation in heritable characteristics (mutation, sexual reproduction)


COMPETITION – There is a struggle for survival (more offspring than the environment can support)


SELECTION – Environmental/evolutionary pressures lead to differential reproduction within a population


ADAPTATION – Individuals with reproductive advantages (best suited) will be more likely to survive and pass these traits on to their offspring


EVOLUTION -cumulative change... make pop. better suited


E.g. antibiotic resistance (MSSA and MRSA), peppered moths, finches on galapagos islands

galapagos islands

beak shape and size of finches illustrate adaptive radiation


different environment on each island=different selective pressures (food, predators)


some east seeds, insects



antibiotic resistance

eg. staphylococcus aureus treated with methicillin 
MRSA and MSSA exist

eg. staphylococcus aureus treated with methicillin


MRSA and MSSA exist

advantaged of binomial nomenclature

1 universally understood


2 can show some similarity between organisms


3 language barrier

domains of life

eukarytote, archaea (P), bacteria (P)

hierarchy of taxa

domain, kingdom, phylum, class, order, family, genus and species.DID KATY PERRY COME OVER FOR GREAT SOUP

human classification

Kingdom: Animalia


Phylum: Chordata


Class: Mammalis


Order: Primate


Family: Hominidae


Genus: Homo


Species: Sapien

natural classification (not selection)

According to a natural classification system, all members of a particular group would have shared a common ancestor


help in identication of species (through a dichotomous key) and allow the prediction of characteristics shared byspecies within a group eg, we find a bat like thing and can prediict stuff about it



reviewing classification

Taxonomists sometimes reclassify groups of species when new evidence shows that a previous taxon contains species that have evolved from different ancestral species.

animal phyla


Porfera


Cnidaria


Platyhelminths


Annelida


Anthropoda


Mollusca


Chordata

plant phyla


Bryophytes


Filicinophytes


Conipherophytes


Angiospermophytes

kingdom animalia, phylum: chordata (vertebrates), what are specific classes

clade def


cladogram def

A clade is a group of organisms that have evolved from
a common ancestor.
Cladograms are tree diagrams that show the sequence o‚f divergence
root=initial comm. ancestor
node= comm. ancestor

A clade is a group of organisms that have evolved froma common ancestor.


Cladograms are tree diagrams that show the sequence of divergence


root=initial comm. ancestor


node= comm. ancestor

cladogram making evidence

Evidence for which species are part of a clade in the base sequence of a gene or the corresponding amino acid sequence of a protein




using morphology is less accurate in reveling common ancestry so things had to be reclassified after DNA CLADISTICS evidence eg FIGWORTS family split

molecular clock

Sequence differences accumulate gradually so there isa positive correlation between the number of differencesbetween two species and the time since they diverged from a common ancestor


mutationsoccur at a roughly constant rate so they can be used as a molecularclock



human cladogram with other primates

definistions


Species:


Population


Community:


Habitat:


Ecosystem


Ecology:

Species:A group of organisms that can potentially interbreed to produce fertile, viable offspring


Population:A group of organisms of the same species, living in the same area at the same time


Community:A group of populations living together and interacting with each other within a given area


Habitat:The environment in which a species normally lives, or the location of a living organism


Ecosystem:A community and its abiotic environment (i.e. habitat)


Ecology:The study of the relationship between living organisms, or between living organisms and their environment

utotrophic or heterotrophic or mix

autotrohps


inorganic nutrients from the abiotic environment


energy for process from photosynthesis




heterotrophs


get organic nutrients from eating other oganisms




mixotrophssome unicellular organisms or venus fly trap



heterotroph types

herbivor, omniovere (panda), carnivore


scavengers: feed on dead (vulture)


DETRIVORES eg earthworms or beetles: non-living organic sources, such as detritus (decaying matter or poop)


SAPOTROPHS eg fungi, mould: secrete digestive enzymes into the food to do external digestions. aka decomposers

nutirent cycle

autotrophs get nutient from abiotic
heterotroph eat them
all die and sapotrophs break down, making nutrient release in soil
autotroph grow in  said soil

autotrophs get nutient from abiotic


heterotroph eat them


all die and sapotrophs break down, making nutrient release in soil


autotroph grow in said soil

components needed for ecosystem

energy (light from sun)


nutrients available


recycling waste

chi-squared test with data obtained by quadrat sampling

testing for association between two species


positive = togetehr cuz symbiosis or predator-prey


negative= competition


1 quadrat rectangular sample count how many of each in diff spots


2 identify hypotheses


3 table of frequenceies --expected and real with totals


3 chi squared formula finds 4 values then average


4 degrees of freedom ONE (row-1 x column -1)


5 if bigger than p value >positive



trophic levels

position occupied in food chain (linear)

position occupied in food chain (linear)

energy lost in ecosystem

not passed from one trophic level to the next cus of


cell respiration & othermetabolic activity (used to stay alive)


heat (byproduct of metabolic activity)


poop


unconsumed parts of an organism




this limits size of food chains as only 10% of energy passed on

heat in ecosystems

Living organisms cannot turn heat into other forms of usable energy

released from organism and lost from ecosystem (unlike nutrients that are recycled)


so ecosystems need external continuous variable energy source ie sun

food chain eg

biomass

Biomass is the total mass of a group of organisms


higher trophic levels have less biomass


ie eating fish gives more energy than eating hawk


due to loss of carbon dioxide, water and other waste products, such as urea to the ecosystem


because tertiary eat more than secondary, spend more energy hunting and losing biomass

energy pyramid

arrow shows flo of energy
10%
must use word producer, primary consumer ec.

arrow shows flo of energy


10%


must use word producer, primary consumer ec.

carbon cycle

photosynthesis
fossilization
combustion
sedimentation
volcanoes

photosynthesis


fossilization


combustion


sedimentation


volcanoes

co2 diffusion

autotrophs need co2 for photosynthesis


levels of co2 in them are always lowe rthan in environment


diffusing from area of high to low


through stomata in terrestrial plants or through cells in aquatic

cell respiration and photsynthesis in ecosystem

autotrophs do both and are balanced at compensation point
when lots of photo bcuz plant >low atmospheric co2 eg summer
when little photo bcuz dead plant> high atmospheric co2 eg winter
forests are carbon sinks

autotrophs do both and are balanced at compensation point


when lots of photo bcuz plant >low atmospheric co2 eg summer


when little photo bcuz dead plant> high atmospheric co2 eg winter


forests are carbon sinks

aquatic ecosystems carbon

co2 dissolves in water


some makes carbonic acid or hyrdogen carbonate


react with ca in rocks to make calcium carbionate


component of hard shells in clam, mussel and CORALS

methanogenesis

Methanogens are anaerobic archaean microorganisms that produce methane as byproduct of metabolic activity


eg. wetlands, mud sediments, rice paddies


also digestive system of cows




after produces, either released into air or deposits in ground (natural gas)

methane in atmostphere

only persists for ~12 years

naturally oxidised to form carbon dioxide and water (CH4 + 2 O2 → CO2 + 2 H2O)

peat formation

normally, sapotrophic bacteria decompose dead organisms


waterlogged conditions are anaerobic


so they becomes ACIDIC and sapotrophs cant live


peat: partially decomposed, carbon rich, waterlogged, acidic anaerobic


heat and pressure removes moisture and you get coal



oil/natural gas formation

decay of marine organisms on the ocean floor

sediments deposited on top creating anaerobic conditions preventing decomposition


heat + pressure turns the hydrocrabons into oil and gas


these accumulate in porous rocks called sandstone



combustion

products are co2 and water
fossil fuels or biomass
living organisms make hydrocarbon as part of biomass
hydrocarbons extracted, purified them burned eg biodiesel

products are co2 and water


fossil fuels or biomass


living organisms make hydrocarbon as part of biomass


hydrocarbons extracted, purified them burned eg biodiesel

carbon fluxes

rate of exchange of carbon between the various carbon sinks / reservoirs

4 sinks: lithosphere (earth crust), hydrosphere, atmosphere, biosphere


rate affected by photo, respiration, decomposition, combustion, deforestation


only ESTIMATION because impossible to directly emasure


measured in gigatonnes

annual atmospheric carbon fluctuation

hawaii


global conforms to nortehnr hemisphere contains cuz more land


co2 levels low in summer as days are long so lots of photo


measures in gigatonnes

most significant greenhouse gases and others
Carbon dioxide and water vapour (cllouds)

others methane nitrogen oxides


less than 1% of atmosphere

factors affecting amount of impact of gas

ability to absorb long wave radiatuon


concentration in atmosphere

greenhouse effect

natural process
traps heat in atmosphere (stops rapid temp fluctuations)
incoming short wave UV from sun
earth survance absorbs teh short UV and reemits it as long IR wave
greenhosue gases absorb and trap  some of those IR

natural process


traps heat in atmosphere (stops rapid temp fluctuations)


incoming short wave UV from sun


earth survance absorbs teh short UV and reemits it as long IR wave


greenhosue gases absorb and trap some of those IR



why rising atmospheric co2 levels

COMBUSTION of fossilized organic matter : factoryies, cars

deforestation


cattle farming



things influenced by change in greenhouse gas concentraions

global temperatures (specifically by CO2)


climate patterns


ENHANCED GREENHOUSE EFFECT - too much trapped heat


more frequent weather storms, droughts, changing ocean currents

co2 and global temp

ice cores in antarctica


analyze gas bubbles farther down = older


fluctuating global temps in ice ages and warm ages show positive correlation



industrial revolution and co2

burning fossil fuels




high fossil fuel emission = high atmospheric co2 = high global temps



ocean acidification

dissolves co2 dissociates and h+ ions raise acidity and react with more carbonate


so mulluscs and coral cant form calcium carbonate shells and dies


8.2 to 8.1 since industrial revolution sows 30 percent acidification


dissapearance of coral reefs


loss in revenue of tourning industry


too much algae





greenhouse debate