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Early/first life
3.8 bya cyanobacteria
Geological eras
Paleozoic - life
Up to 300 mya
Mesozoic - middle life
300 - 65 mya
Cenozoic - modern life
65 mya - present
Diversity of life
Insects have most species (most biodiversity)
Scientific History
Linnaeus - concept of species
Darwin - evolution
People in galapagos could identify tortoise island based on shell
Finches had diff beaks on diff islands
Natural selection - climate quite diff btw islands
Led to speciation of tortoises when sea level rose
Led to speciation of finches for food sources
Allopatric vs. sympatric speciation
Allopatric: complete isolation that leads to speciation via natural selection
Ex: tortoises
Sympatric: only functionally separated but speciation still occurs via natural selection
Ex: finches
Protists in fossil record
Algae
Phytoplankton
Forams, dinoflagellates, radiolarians
Amoeba
Plant kingdom
Gymnosperm: conifers, dominated mesozoic
Angiosperm: flowering plants, fruits spread seeds, dominate cenozoic (evolved 100 mya)
Animal kingdom, deuterostomes, etc
Mass extinction, evolutionary radiations and adaptive breakthroughs
After mass extinctions, diversity increases bc niches open up
Used to be more niches than organisms to fill them, but now there's an organism or multiple for niches
Evolutionary radiation examples
Jurassic corals
Symbiotic relationship w zooxanthellae
Zooxanthellae cant handle heat
Makes coral vulnerable since coral became dependent
Porous skeletons
Grow more quickly
Take up more space and outcompete coral neighbors
Post cretaceous mammals
Dinos were filling the niches
Extinction of dinos allowed for rise of mammals
Cope's law
Animals get larger as they evolve
Exception: dwarfism on small islands - large size unnecessary
Climate belts on land (tropics, desert, horse lats) & in ocean
Rains in tropics bc humid warm air rises, cools, can't hold water, rains
Horse lats: 30-38 degrees N & S, deserts
Erratic winds - horses got kicked off boats when ran out of wind
Coriolis
Clockwise gyres in northern hemisphere
Counterclockwise gyres in southern hemisphere
Thermohaline Circulation
Great conveyor belt
Surface current moves to N Atlantic
Well oxygenated & nutrient poor
Gets cold & wants to sink
Sea ice forms → surrounding water is salty
Cold + salty water = negatively buoyant → sinking
Deep current becomes anoxic without access to surface
Organic matter sinks to anoxic level, gets buried
Upwelling brinks deep water to surface
Structure of atoms, atomic number & weight etc
Atomic #: # of protons
# of neutrons = # of protons
Except in isotopes
Atomic weight = weight of neutrons + weight of protons
Ooids
Calcium carbonate (limestone) forms around nucleus being moved back and forth by strong currents
Water needs to be supersaturated with carbonate
Conditions exist in bahamas, red sea, australia
Aragonite
Used to be calcite
Sedimentary rocks have fossils
Silica fossils make chert
Carbonate fossils make chalk