Paleontologists classify prehistoric biological remains according to the specific geological and chemical mechanisms that preserved them. Match each fossil preservation mode with its defining geological characteristic.
- Trace fossilSedimentary rock records indirect physical evidence of an ancient organism's biological activity, such as footprints, burrows, or coprolites, without preserving body parts.
- Mold and castBuried biological structures dissolve completely to leave a hollow cavity in rock, which subsequently fills with percolating minerals that replicate the external shape.
- CarbonizationIntense compression drives off organic liquids and gases, leaving behind a thin silhouette film of pure elemental residue.
- Amber entombmentWhole, delicate organisms are completely encased and sealed within hardened, fossilized tree resin with original soft tissues intact.
Answer
Trace fossil correctly pairs with sedimentary evidence of biological activity without body parts; Mold and cast correctly pairs with a hollow cavity filled with secondary minerals replicating external morphology; Carbonization correctly pairs with compression expelling volatiles to leave a thin carbon film; Amber entombment correctly pairs with complete organisms sealed in hardened tree resin.
Each fossilization process corresponds directly to distinct physical and geochemical mechanisms: trace fossils capture indirect activity (footprints and burrows); mold and cast formations represent hollow dissolution cavities filled by mineral crystallization; carbonization results from volatile loss under pressure leaving a thin carbonaceous film; and amber entombment seals whole specimens in fossilized resin.
Step-by-Step Solution
Key Concept
Modes of fossil preservation in paleontology and sedimentary stratigraphy
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