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fossils
evidence of life preserved in rock
include remains or organisms & traces
how to become fossil easily
have preservable parts
buried by sediment
escape physical, chemical, & biological destruction
Environment in fossil preservation
marine & transitional: more favorable
higher rate of deposition
little to no erosion
anerobic environments
continental: less favorable
lower rates of deposition
frequently erosional
types of fossil preservation
preservation of unaltered hard parts
preservation of unaltered soft parts
chemical alteration of hard/soft parts
permineralization
carbonization
replacement
recrystallization
imprints of hard parts
internal molds
external molds
casts
trace fossils or ichnofossils
preservation of unaltered hard parts
shells of invertebrates & single-celled organisms, vertebrate bones & teeth
preservation of unaltered soft parts
freezing, mummification, amber, tar
permineralization
used in unaltered hard parts
minerals occurs in porous structures before surrounding decays
solidifies structure
decay continues as structure mineralizes
carbonization
unaltered soft parts
preserves soft parts with carbon film
commonly in plants
replacement
unaltered hard parts
simultaneous substitution
slow decay of hard part matches with slow mineralization
recrystallization
unaltered hard parts
common with shells/carbonate material
crystals secreted to form shell
increase size but keep same chemistry
preserves overall shape, but destroys fine structure
imprints of hard parts
casts & molds (impressions)
surrounding sediment lithifies before organism decays
decay leaves a mold
can be internal or external
commonly in shells & bone
trace fossils
markings in sediment made by organisms
ex: burrows, tracks, nests, eggs
can provide environmental info
also provide info about the individual that made the traces
Lagerstatte
sedimentary formations that preserve exceptional paleontological info