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Vocabulary-style flashcards covering key concepts from the notes on fossils, fossilisation, and dating methods.
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Fossil record
The history of life preserved in rocks, which is incomplete due to biases in fossil formation, preservation, discovery, and access.
Fossil
Any preserved trace or remains left by an ancient organism.
Body fossils
Preserved parts of organisms, such as bones, teeth, shells, hair, or skin.
Trace fossils
Preserved evidence of activity, such as footprints, casts, faeces, tooth marks, or burrows.
Artefacts
Objects deliberately made or modified by humans, used as evidence of past activity.
Relative dating
Dating that places specimens in order from oldest to youngest without giving an exact age.
Stratigraphy
Study and analysis of rock layers (strata) to determine relative ages.
Index fossils
Widely distributed fossils that existed for a short time, used to correlate and date strata.
Absolute dating
Dating that provides an approximate numerical age (in years) rather than a precise date.
Radiocarbon dating (Carbon-14 dating)
Absolute dating using decay of Carbon-14 to Nitrogen-14; half-life about 5730 years; effective up to ~60,000 years.
Potassium-Argon dating
Radiometric dating using decay of potassium-40 to argon-40; half-life ~1.25–1.3 billion years; useful for very old rocks.
Potassium-40
Radioactive isotope that decays to Argon-40.
Argon-40
Noble gas produced by the decay of Potassium-40.
Isotope
Variant of an element with the same number of protons but different numbers of neutrons.
Fossilisation
Process of becoming a fossil, requiring rapid burial, hard parts, low oxygen, dry/alkaline soils, and undisturbed conditions.
Rapid burial
Quick covering of remains by sediment or ash, aiding preservation.
Hard body parts
Bones, teeth, shells and other durable parts that survive long-term preservation.
Absence of oxygen (anoxia)
Low-oxygen conditions that slow decay and help fossil preservation.
Dry, alkaline soils
Soil conditions that promote mineral preservation; acidic soils can dissolve minerals in bones.
Incomplete fossil record reasons
Destruction, non-discovery, inaccessibility, incomplete fossilisation, or too few specimens.
Fluorine analysis
Technique that compares fluorine uptake in bones to estimate how long they've been buried.
AMS (Accelerator Mass Spectrometry)
A dating method that counts individual atoms, allowing very small samples to be dated.
Half-life
Time required for half of a radioactive substance to decay.
Atmospheric C-14 variation
Fluctuations in C-14 levels in the atmosphere that affect radiocarbon dating accuracy.
Correlation of rock strata
Matching layers of rock from different areas to determine their relative ages.
Principle of superposition
In undisturbed strata, younger layers lie above older layers.
Disturbances in rock layers
Events (tectonic activity, re-burial) that disrupt original layering and complicate dating.