chapter 10 (relatedness) Flashcards
process of fossilisation
- animal/plant dies
- the body is covered in sediment the soft tissues decomposed and the hard body structures become fossilised by permineralisation
- the sedimentary layers accumulate and the resultant pressure forms sedimentary rock
- the earth’s movement raise the layers of the rocks to the surface
- the rock erodes exposing fossilised body structures.
increase the likelihood of fossilisation
areas of rapid sediment accumulation , constant cool temperatures, low oxygen availability, low light exposure
relative dating
a dating technique used to determine the relative ages of fossil by comparing its position to other fossils or rock in surrounding rock strata
absolute dating
a dating technique used to determine the absolute age of a fossil by measuring the relative amounts of radioisotopes to their products
index fossils
- a group of widespread fossils which existed for a short period and have a known age
- can be used to reference and easily determine the age of unknown fossils
- best index fossils: physically distinctive, have a large population, existed in many geographical areas, lived within a known short period of time
transitional fossil
a fossil that shows traits that are common to both its ancestral group and its descendant group
mould fossil
- fossil formed when a living thing decomposes underneath sediment
- creating a cavity in the shape of the dead organism
cast fossil
fossil formed when a mould fossil is filled with sediment
trace fossil
- fossil or structure indicating the presence of organisms
- rather than the organisms themselves (e.g. nests, footprints, and burrows)
Radioisotope series
- Carbon-14 - nitrogen-14
5 730 years 1 000 - 50 000 years
Organic materials - Uranium-235 - lead-207
700 million years 1 million - 4.5 billion years
(used together with U-238 - Pb-206 dating)
Uranium-containing materials (shells, corals) - Uranium-238 - lead-206
4.5 billion years 1 million - 4.5 billion years
(used together with U-235 - Pb-207 dating)
Uranium-containing materials (shells, corals) - Potassium-40 - argon-40
1.3 billion years 100 000 + years
Igneous (volcanic) rocks
Homologous structures
- are physical evidence of divergent evolution
- the evolutionary process where two or more populations of a single species accumulate enough genetic differences to be classified as different species.
Analogous structures
are structures that serve similar biological functions but are not derived from a common ancestor
Vestigial structures
are structures found within organisms that once served a purpose for an organism’s ancestors but due to changing selection pressures have lost their original function and are no longer required for survival.
(e.g human coccyx/tailbone)
Molecular homology
is the study of the similarities between organisms at a DNA and amino acid level