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A trip through geologic time: Fossils
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Uniformitarianism The present is the key to the past. The same geologic processes that operate today operated in the past Fossil fish- not a goldfish
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Fossils: evidence of past life Fossil Formation: 1. organism dies 2. organism buried in sediment 3. sediments slowly harden into rock preserving the parts of the organism
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Most important conditions for fossil formation Rapid burial Hard parts
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Types of Fossils Mold and Cast 1.organism dies, gets buried, decomposes – leaves behind a hole the shape of the original organism ( the mold) 2.Water washes in sediments which fill in the mold and solidify to form a rock with the same external structure as the organism had (the cast) Trilobite fossil
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Petrified: (mineralized) fossils- organism dies, every molecule of the organism is replaced by a molecule of a mineral This shows the internal structure as well as the external structure. Petrified Wood
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Actual Fossils The actual organism frozen in ice or amber (tree sap) Termites in amber Frog in amber Baby mammoth frozen in ice
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Trace Fossils:evidence that an organism has been there coprolyte Dinosaur footprint gastroliths Dinosaur tracks Worm casings
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Carbon films: an extremely thin coating of carbon on rock Leaf fossil
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Index Fossil: fossils of widely distributed organisms that lived during only one short period.
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http://cartage.org.lb/en/themes/sciences/Paleontology/Foss ilsAndFossilisation/AmberFossils/AmberFossils/AmberFossils. htm http://news.bbc.co.uk/2/hi/6284214.stm http://www.envs.emory.edu/faculty/MARTIN/ichnology/tf- eggs.htm http://en.wikipedia.org/wiki/Gastrolith http://www.clas.ufl.edu/users/pciesiel/gly3603c/fossils.html http://pubs.usgs.gov/gip/geotime/fossils.html Picture bibliography
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