Monday, March 26, 2007

Section 14.2 CS

Section 14.2 Cheet Sheet


  • Spontaneous generation – The idea that living material comes from nonliving material.

    • Was disproved by Francesco Redi and Louis Pasteur

      • Redi did the meat/fly experiment

      • Pasteur did the broth experiment

  • Biogenesis – Life comes from life

  • Simple organic molecules must have been formed on early Earth for life to arise.

    • Water vapor, carbon dioxide, nitrogen, and methane and ammonia in the atmosphere may have joined together via energy from the sun, lightning, and Earth's heat to form organic molecules.

    • These molecules would “brew” in a “primordial soup” until simple life arose called protocells.

    • Stanley Miller and Harold Urey tested the hypothesis and created organic molecules.

  • The first life might have been heterotrophs, eating organic molecules found in the oceans, and anaerobic, because there was not an abundant amount of oxygen in the atmosphere.

  • After all the food had been devoured by these heterotrophs, autotrophs would be favored by natural selection and would have evolved, called archaebacteria. These autotrophs would be photosynthetic, producing oxygen.

  • These autotrophs increased the concentration of oxygen in the Earth's atmosphere and allowed aerobically energy producing organisms to evolve.

    • Lightning also may have converted much of the oxygen in the atmosphere to ozone, forming a shield from the dangerous ultraviolet radiation from the sun, which enabled more complex organisms to evolve.

  • Lynn Margulis proposed a theory for how eukaryotes may have evolved, called the endosymbiont theory.

    • Mitochondria evolved from energy making bacteria.

Monday, March 19, 2007

    Science, Section 14.1 Cheat Sheet


  • Early Earth was:

    • extremely hot

      • possibly caused by:

        • surface/atmosphere heating

          • meteorites colliding with the Earth

          • volcanoes erupting

        • internal heating

          • compression of minerals

          • decay of radioactive materials

  • The gas from volcanoes was the primitive atmosphere of the earth.

    • Made up of:

      • Water Vapor

      • CO2

      • Nitrogen

      • Little O2

      • Other gases

  • First organisms appeared between 3.9 and 3.5 billion years ago.

  • 99 percent of all organisms that were on earth are now extinct.

  • Types of Fossils

    • Trace

      • Marking left by an animal

    • Cast

      • When minerals in a rock fill a space left by a decayed organism

    • Imprint

      • When a thin object falls into a sedimentary rock

    • Petrified

      • When minerals penetrate and replace the hard parts of an organism

    • Mold

      • When a dead organism is buried in sediment and decays

    • Amber/Frozen

      • When entire organisms were trapped in ice or tree sap and preserved

  • Fossils can teach scientists about the organism's behavior, as well as the climate and geography of the area the fossil was found in.

  • Fossils primarily occur in sedimentary rocks.

  • There are two ways to find the age of fossils:

    • Relative Dating

      • If the fossil is found in an undisturbed area, the deeper the fossil is, the older it is.

      • The only way scientists can truly have an approximation of the age through this method is to know how old the rock and/or other fossilized organisms are around it.

    • Radiometric Dating

      • Radiometric dating allows scientists to get a better idea of the age of the organism.

      • Radiometric uses common radioactive materials that decay into other materials at a given rate.

      • A radioactive material's half-life is half the amount of time it takes for that material to decay into the other material.

      • Scientists can then find the age of the organism by seeing how much of the radioactive material has decayed.

  • The Geologic Time Scale is a scale of time based on the study of rocks in the Earth.

    • Precambrian – 3.5 billion years ago.

      • 87% of Earth's history.

      • Simple bacterias at first, then to eukaryotes by about 1.8 billion years ago, and by the end, contained multicellular, aquatic eukaryotes like sponges and jellyfish.

    • Paleozoic (Cambrian) – ended 245 million years ago.

      • Large and diverse amounts of organisms, such as fish, worms, and starfish.

      • Plants may have existed since 400 million years ago.

      • A mass extinction marked the end of the Paleozoic, which killed 70 to 90% of all life on Earth.

    • Mesozoic – Began 245 million years ago –

      • Mammals appeared, dinosaurs existed, birds evolved.

      • Three periods: Triassic, Jurassic (Age of the Dinosaurs), Cretaceous.

      • Mass extinction, during Cretaceous period, of dinosaurs in cretaceous allowed mammals and flowering plants to develop.

      • Mass extinction may have took out 2/3 of all living species.

      • Continents may have moved exponentially during this period. This is based on the concept of plate tectonics.

      • Plate tectonics is the idea that Earth's is actually several large “plates”, which are floating on magma, which is moving as well. These plates move and collide to create the surface on which we currently live.

    • Cenozoic – Began 66 Million years ago

      • Modern era

      • Primates evolved

      • Modern humans appeared 200,000 years ago.