Evolution Flashcards
Define evolution.
The scientific explanation for the mechanisms that drive species to change over time.
What does the fossil record provide?
A significant source of evidence for evolution.
What does the modern evolutionary synthesis do?
Combines evidence from the fossil record with our relatively modern knowledge of how genes are inherited and how changes to genes arise to give a complete picture of the mechanisms of evolution.
What are the measures of time in which evolution has occurred?
Periods, eras, epochs and eons.
What does continental drift cause?
The significant movement of tectonic plates over time.
Explains current biogeography.
What provides evidence for continental drift?
The fossil record.
Give examples of continents that once existed.
Gondwana and
the supercontinent Pangaea.
Describe the association between Oxygen levels and organisms.
Around 300 my, Oxygen level of Earth’s atmosphere rose sharply.
Corresponds with an increase in organisms’ body size in the fossil record.
Corresponds with the Carboniferous period and the rise of photosynthetic plants.
What are the five major lines of evidence supporting evolution?
Palaeontology
Biogeography
Developmental biology
Morphology
Define palaeontology.
The study of prehistoric life, particularly the fossil record.
Define biogeography.
The study of the distribution of species over time.
Define developmental biology.
The study of the process by which organs develop.
Define morphology.
The study of the form and structure of organisms.
Define genetics.
The study of genes, heredity and variation in living organisms.
Give examples of further evidence supporting evolution?
Comparative genomics
Comparative biochemistry
Bioinformatics
Define comparative genomics.
The comparison of genomic features of organisms.
Define comparative biochemistry.
The comparison of proteins of organisms.
Define bioinformatics.
Analysis of large data sets (such as the genomic sequences of different organisms).
Define fossils.
Preserved remains of organisms and their traces.
Commonly hard parts such as teeth, bones and shells. Also include impressions left after soft tissue has decayed, or footprints, burrows or preserved faeces (coprolites).
How does fossilation occur.
Fossilisation requires the absence of oxygen.
Organisms can be covered with sediment such as silt or sand. This can protect the remains from scavengers and slow the decay long enough for fossilisation to occur.
Mineralisation: hard parts of organisms are replaced with minerals and makes fossilisation more likely.
Can be formed as a result of freezing and subsequent dehydration, by soft material such as ash falling on impressions, or from impressions made in sandstone and mudstone.
Where are fossils found?
Not usually found in volcanic rock, as molten lava solidifies at 1000°C.
Not usually found in metamorphic rock as the pressure and heat of metamorphism is likely to destroy fossils.