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History of Life. Ch. 14. History of Life. Fossil Evidence of Change Paleontologist - a scientist who studies fossils Fossil - preserved evidence of an organism Trace fossils - indirect evidence of organism. ex footprints, burrows, feces Molds and Casts - impression of an organism
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History of Life Ch. 14
History of Life • Fossil Evidence of Change • Paleontologist - a scientist who studies fossils • Fossil - preserved evidence of an organism • Trace fossils - indirect evidence of organism. ex footprints, burrows, feces • Molds and Casts - impression of an organism • Replacement - original organism is replaced with mineral crystals • Petrified - Empty pore spaces are filled by minerals • Amber - Preserved tree sap hardened • Original Material - Mummification or freezing
Fossils • Fossil Formation - formed in sedimentary rocks
Dating Fossils • Relative Dating - determine the age of rocks by comparing them to those in layers around it • Law of superposition - younger layers are deposited on top of older layers, similar to stacking the daily paper on top of each other • Radiometric dating - uses the decay of radioactive isotopes of measure the age of a rock • Half-life - amount of time it takes for half of the original isotope to decay, typically use carbon 14 for dating
Time • Geologic Time Scale - model that expresses the major geological and biological events in Earth's history, divided into precabrian and phanerozoic • Earth formed roughly 4.6 billion years ago • Era - Paleozoic, Mesozoic, and Cenozoic times • Period - smaller division of time (see diagram)
Earth History in a Day • If the entire history of the earth was broken down into 1 Day: • No Life from 12:01 am - 1:00 pm • Microscopic bacteria from 1:00 pm - 8:00 pm • Dinosaurs came at 10:34 pm • Humans at 11:56 pm
Historic Periods • Precambrian - 90% of the earth's history, goes from the beginning of Earth's formation until 542 million years ago • Stromatolites - bacteria that produced oxygen and released it into the atmosphere, because of this Oxygen became plentiful and allowed other organisms to emerge • Paleozoic - Cambrian explosion, most major animal groups diversified, marine species moved to the land. There was a mass extinction that ended this period, 90% of the organisms disappeared
Historic Periods • Mesozoic - The time of the Dinosaurs, birds, and flowering plants. A meteorite struck the earth possibly causing another mass extinction • K-T boundary - the layer of rock that proves of a meteorite impact • Plate Tectonics - the movement of the plates that make up the Earth's surface • Cenozoic - The time of the Mammals, this is when humans as well as most other mammals roamed the Earth
Dinosaurs • How did the dinosaurs die?
The Origin of Life • Spontaneous generation - idea that life arises from nonlife • ex. it was once believed that worms, insects, and fish came from mud • Theory of Biogenesis - states that only living organisms can produce other living organisms • If life can only exist from pre-existing life, then how did the first life-form appear? Which came first the chicken or the egg? Can we even figure this out? Discuss this with your partner and come write your ideas down
Origin of Life • Simple organic molecules - UV light from the sun, electricity from lighting, and the gases present in the atmosphere and early oceans were created through chemical reactions which produced Amino Acids, sugars, and nucleotides • Deep Sea Vents - hydro thermal vents produced sulfur, and other elements which supported a food chain for early organisms
Origin of Life • Meteorites - some believe that this could be the source of life • Clay - Some believe that clay was used by the Amino Acids to hold the chains of AA's together • Genetic code - RNA was life's first coding system, they can also behave like enzymes • There are still holes in this mystery, it remains unresolved
Cell Theory • archea - prokaryotic cells that are restricted to volcanic and other extreme environments, get there nutrients from inorganic molecules like sulfur, they do not need or produce oxygen • Oxygen - was not present in the atmosphere until after 1.8 billion years ago • Cyanobacteria - photosynthesizing prokaryotes, formed the ozone layer, which ultimately made conditions on earth more habitable
Cell Theory • Endosymbiont Theory - prokaryotes lived inside of eukaryotic cells and performed cell functions just as a mitochondria or chloroplast would • These cells evolved into the modern day Eukaryotic cells
Review • Ch. 14 Review • p 411 - 4-8, 10 • p 412 - 14,15,19 • p 413 - 35-40 • p 414-415 - 4,5,8,13,17