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Evolution: The Science behind the theory •Geological time •Fossils •Darwin & Natural Selection •Species changing over time •Anatomical & Embryological evidence •Speciation Summary of Evolution of Life Chemical Evolution (1 billion years) Formation of the earth’s early crust and atmosphere Small organic molecules form in the seas Large organic molecules (biopolymers) form in the seas First protocells form in the seas Biological Evolution (3.7 billion years) Single-cell prokaryotes form in the seas Single-cell eukaryotes form in the seas Variety of multicellular organisms form, first in the seas and later on land How do we know about the past? Fossils What is a fossil? A fossil is an impression, cast, original material or track of any animal or plant that is preserved in rock after the original organic material is transformed or removed. A fossil may be: an original skeleton or shell; a mold or cast; traces such as footprints or worm tubes Material that has replaced the once living thing Types of Fossils Body fossils – actual parts of an organism bones, shells, leaf imprints Types of Fossils Trace fossils – evidence of life having been there tracks, burrows, casts Trace Fossils Mold – reproduction of the inside or outside surface of a living thing Cast – duplicate of the original organism; usually formed by replacement of inside of living thing Trace Fossils Burrows or borings – Spaces dug out by living things & preserved as is or filled in Tracks – impressions of passage of living things Trace Fossils Imprint – Thin objects such as a leaf that falls onto sediment & leaves an imprint then the sediment hardens into rock Petrified Fossils Minerals penetrate & replace the hard parts of an organism producing a copy of them Amber & Ice An entire organism was quickly trapped in ice or tree sap that hardens into amber Where are fossils found? Sedimentary Rock Why sedimentary rock? What conditions promote fossilization? Hard body parts such as skeletal bones or exoskeletons Rapid burial and/or lack of Oxygen Unaltered - insects or plant parts trapped in amber or ice ; original unaltered material from the living organism Replacement – the hard parts of an organism dissolve and are replaced by other minerals Petrification – rock-like minerals seep in slowly and replace the original organic tissues Authigenic- molds or casts of organisms tissue material is decomposed or of markings left behind by an orgasnism Putting it all together Examples of Fossils . . . Sporadoceras Nautilus Orthoceras Squid Trilobites Lobster Fossil Fish Dinosaur Bones