Fossil Preservation (Chapter 3) Flashcards
Taphonomy
- “death study”
- study of biological & geological processes that occur between death of organism & its final state in rock
- biological processes: predation, scavenging
- geological processes: weathering, diagensis
body fossils
actual body of organism; e.g. trilobite’s skeleton
trace fossil
records of activities done by organisms; e.g. trilobite’s trail
hard part
- shell, bone, or woody tissues
- e.g. shell of Lingula rectilate
- good chance of preservation
soft part
- organic tissues
- e.g. body of Lingula rectilate
- poor chance of preservation
calcium carbonate preservation
argonite material recrystallizes to calcite since former is unstable; can also be preservation of origninal material
silica preservation
- permineralization (pore filled) of woody tissues by silica
- orginal preservation of organisms (e.g. diatoms)
phosphate preservation
- of soft parts - early mineralization at low rate of burial & high organic content
- usually replacement of elements in chemcial composition
- allow preservation of original morphological details
iron oxides preservation
- of soft parts - rapid burial & low organic content & presence of sulfates in sediments
- coating of pyrite around soft parts may leads to replacement of hard parts composed of calcium carbonate by pyrite
siderite preservation
- siderite mineral (combination of iron & carbonate) replaces original material & preserve shape or outline of organism
- e.g. fossilized claw of Protocallianassa mortowi
carbonization preservation
- parts (esp. soft parts) are heated & compressed, only carbon film remains
- process likely to occur in anoxic, organic-rich environment; e.g. swamps
- sediments → shales
clay preservation
- clay filled up spaces of organism & take shape even when original material disappeared
- especially good for shelly organism, e.g. ammonite
amber preservation
- way of preserving fossils by envelop material in fossilized resin (amber)
- usually well-preserved since amber is resilient & can preserve both hard & soft parts
original shell/ unaltered preservation
- original material/shell is intact without chemical alteration in mineralogy
- usually due to burial after sof parts decayed
mold
original body has decayed but left an impression on surrounding sediments
cast
orginal body has decayed and its space is replaced later with another material, a perfect replica
internal vs. external cast
- internal - minerals filled in species of a hollow organic structure/cavity which decayed later
- external - minerals filled in mold and recreate outer surface of organism that left the mold.