Speciation, fossilisation and relatedness Flashcards
Speciation
is the process by which populations genetically diverge until they become different species
Species
are a group of individuals who are able to breed with each other and produce viable and fertile offspring
viable
able to survive
fertile
the ability to reproduce
Allopatric speciation
the geographic separation of a population from a parent population resulting in evolution of a new species
geographic barrier
a physical barrier that isolates populations from each other, preventing gene flow and allowing genetic differences to accumulate
The process of allopatric speciation
- initially a population(s) of the same species becomes seperated by a geographical barrier preventing gene flow
- the isolated populations are exposed to different selective pressures, favouring different phenotypes and allowing genetic differences to accumulate
- over time, sufficent genetic differences accumulate in the two population as they can no longer interbreed to produce viable, fertile offspring. Hence, two species are formed.
Allopatric speciation
the geographic separation of a population of a population from a parent population resulting in the evolution of a new species
geographic barrier
a physical barrier that isolates populations from each other, preventing gene flow and allowing genetic differences to accumulate
Fossil record
information from fossils arranged in chronological order helping to map the history of life on Earth, placing species in the appropriate geological time frame
fossils
are the preserved remains of long-dead organisms
Process of fossilization
- usually begins when remnants of an organism are rapidly covered by sediment.
- Over time, layers of sediment upon each other and pressure pushes these layers together forming sedimentary rock
- When devoid of oxygen, microorganism and other disturbances the remains are preserved
Conditions that contribute to fossilisation
areas of rapid sediment accumilation
physical protection from scavengers and decomposers (eg fungi and bacteria)
Permineralised fossils
fossil formed when organic matter is gradually replaced by hard minerals
Impression fossils
fossils formed when an organism is encased in material but decompose or is removed and the gap is filled with another substance. Also known as cast and mould fossils