Speciation, fossilisation and relatedness Flashcards

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1
Q

Speciation

A

is the process by which populations genetically diverge until they become different species

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2
Q

Species

A

are a group of individuals who are able to breed with each other and produce viable and fertile offspring

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3
Q

viable

A

able to survive

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4
Q

fertile

A

the ability to reproduce

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5
Q

Allopatric speciation

A

the geographic separation of a population from a parent population resulting in evolution of a new species

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6
Q

geographic barrier

A

a physical barrier that isolates populations from each other, preventing gene flow and allowing genetic differences to accumulate

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7
Q

The process of allopatric speciation

A
  1. initially a population(s) of the same species becomes seperated by a geographical barrier preventing gene flow
  2. the isolated populations are exposed to different selective pressures, favouring different phenotypes and allowing genetic differences to accumulate
  3. 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.
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8
Q

Allopatric speciation

A

the geographic separation of a population of a population from a parent population resulting in the evolution of a new species

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9
Q

geographic barrier

A

a physical barrier that isolates populations from each other, preventing gene flow and allowing genetic differences to accumulate

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10
Q

Fossil record

A

information from fossils arranged in chronological order helping to map the history of life on Earth, placing species in the appropriate geological time frame

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11
Q

fossils

A

are the preserved remains of long-dead organisms

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12
Q

Process of fossilization

A
  1. usually begins when remnants of an organism are rapidly covered by sediment.
  2. Over time, layers of sediment upon each other and pressure pushes these layers together forming sedimentary rock
  3. When devoid of oxygen, microorganism and other disturbances the remains are preserved
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13
Q

Conditions that contribute to fossilisation

A

areas of rapid sediment accumilation
physical protection from scavengers and decomposers (eg fungi and bacteria)

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14
Q

Permineralised fossils

A

fossil formed when organic matter is gradually replaced by hard minerals

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15
Q

Impression fossils

A

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

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16
Q

Trace fossils

A

fossils of objects or structures indicating the presence of organisms, rather than the organisms themselves ( nests, eggs, footprints)

17
Q

Mummified fossils

A

fossil formed when the body is under conditions that slow down or stop the decaying process
found trapped in caves, ice and in dry caves

18
Q

Absolute dating

A

works out the absolute age of the fossil in years
eg. radiometric dating

19
Q

Relative dating

A

age of fossil determined by relative dating techniques
Describes the age of a fossil compared to other fossils, instead of a fossil’s age in years
Relies on strata which are separate layers within sedimentary rock
fossil succession is the principle that fossils of the same age will be in the same layer of sedimentary rock, and fossils found in a higher or lower sedimentary layer will be younger or older respectively. Also known as the law of superposition

20
Q

transitional fossils

A

fossils that show an intermediate stage of evolution

21
Q

Relatedness between species

A

Evolutionary studies provide evidence that all of life on Earth is related.
Relatedness between species can be shown through similar morphology (physical structures) and shared DNA sequences.
This evidence suggests that related species evolved from a common ancestor in the past.
The more similar the structures or DNA sequences, the more recently the two species diverged from a common ancestor.
These theoretical relationships are often illustrated using phylogenetic trees.

22
Q

Structure of phylogenetic trees

A

Phylogenetic trees usually have a line at the base called the root representing the common ancestor.
Each line on the tree is called a branch.
These branches split away from each other at nodes, which represent a divergence between those two taxa.
The end of a branch is called the leaf. This is where the present–day or extinct species are found, labelled with the species or taxa name