Topic 9 Flashcards

1
Q

What does an entity need to be considered alive?

A

Organization, metabolism, response to stimuli, homeostasis, adaptation, and reproduction

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2
Q

Are viruses alive?

A

Viruses are infectious parasitic entities that span the boundary between living and non-living.

Viruses have nucleic acids that replicate, mutate, and respond to natural selection, but LACK metabolism, homeostasis, and cannot reproduce outside of the host cell

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3
Q

3 Eons of geologic Record

A

Archaean, Proterozoic, and Phanerozoic

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4
Q

Phanerozoic

A

The last half billion years encompassing multicellular eukaryotic life.

3 eras: plaeozoic, mesozoic, and cenozoic

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5
Q

Factors for an Organism to undergo Fossilization

A

Existed for a long time
Abundant and widespread
hard rather than sof-bodied
aquatic
inshore marine, not offshore
not a decomposing organism

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6
Q

Mold Fossils

A

Form when a hollow space (impression) remains after the organism decays or resolve. Ex: cast fossils creating a mold

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7
Q

Replacement/Petrified fossils

A

The original tissues of the organism are replaced by minerals, preserving the detailed structure of the organism

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8
Q

Trace Fossils

A

Provide evidence of organism’s behaviour, such as tracks, burrows, or feces

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9
Q

Preserved Fossils

A

retain much of the original organic material of the organisms, such as carbon films, amber, tar or peat, or being frozen

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10
Q

Sedimentary Strata

A

Layers (strata) revealing the relative ages of fossils but not the absolute ages.

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11
Q

Challenges to Relative Dating

A

Common to have gaps in sedimentary sequence

Sediments can be tipped or even inverted by makor land movements

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12
Q

Radiometric Dating

A

Absolute dating of fossils using radioactive decay of isotopes of various elements providing a means to an age

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13
Q

Plate Tectonics Theory

A

considers that the Earth’s crust is composed of large plates that have been slowly moving since about 3.4 billion years ago causing continental drift to impact Earth’s biodiversity and the distribution of fossils

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14
Q

Supercontinent name

A

Pangaea
250 million years ago

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15
Q

“Big Five” Phanerozoic mass extinctions and main 2 examples

A

mass extinctions where 50% of the Earth’s species became extinct.
1. Permian extinction
2. Cretaceous extinction

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16
Q

Permian mass exctinction

A

Defines the boundary between the Palaeozoic and Mesozoic eras 252 million years ago caused by volcanic activity and coincided with the formation of Pangaea

17
Q

Cretaceous mass extinction

A

66 million years ago, separating the Mesozoic from the Cenozoic. About 20% of all families went extinct, many being terrestrial plants and animals. Lost non-avian dinos.
Coincides with worldwide geologic deposits from a meteorite impact at Chicxulub, Mexico

18
Q

Holocene extinction

A

Probable human-caused mass extinction ongoing now as a result of human population growth and overconsumption of natural resources

19
Q

Consequence of mass extinctions

A

Lost of biodiversity altering ecological communities and niches available for organisms. Entire lineages can be lost by mass extinctions

20
Q

Adaptive radiation

A

The rapid evolution of diversely adapted species from an ancestral species occurring when a change in the environment makes new niches available.

21
Q

Causes of Adaptive Radiation

A

Mass extinctions, evolution of novel characteristics, and colonization of new regions with little competition

22
Q

When did the Earth form?

A

Approximately 4.6 billion years ago during the Hadean Eon

23
Q

Early Earth Conditions (first billion years)

A

Unstable crust floated on molten magma as earth cooled

24
Q

Early Earth Conditions (first billion years)

A

Unstable crust floated on molten magma as earth cooled, steaming gases formed an atmosphere without oxygen, and when temperature dropped, water vapour condensed into raid which collected in basins

25
How did life begin?
Life originated from a series of chemical reactions that led to the formation of living organisms
26
Chemical and physical processes on early Earth that le tot the formation of simple sells
1. Abiotic synthesis of small organic molecules 2. Polymerization of small organic molecules into organic polymers 3. Formation of protocells 4. Emergence of self-replicating molecules
27
2 Possible Sources of organic molecules on Early Earth
1. Terrestrial orgins: spontaneous osynthesis driven by energy sources 2. Extraterrestrial origins: objects hit earth
28
Miller-Urey Experiment (1953)
Demonstrated the amino acids could be synthesized by simulating early Earth conditions. It showed methane, ammonia, hydrogen, and water vapour when exposed to electric sparks could form organic molecules in reduced atmospheres
29
How did polymerization of small organic molecules to larger ones occur?
Likely occurred on hot surfaces such as clay, sand, or rock, where evaporation of water concentrated small organic molecules, triggering the spontaneous formation of organic polymers
30
Protocells
simple, cell-like structures that form when organic molecules become enclosed within vesicles. hypothetical precursors to modern cells.
31
RNA World Hypothesis
Idea that suggests RNA, not DNA, was the first self-replication molecule. Simpler than DNA, it can still self-replicate and perform catalysis (acting like enzymes to speed up chemical reactions
32
Prokaryotes
The oldest fossil evidence of life hypothesized to have existed up to 3.9 bya Single-celled organisms with DNA not contained in the nucleus and lacking membrane-bound organelles.
33
Domains of Prokaryotes
Bacteria and Archaea
34
Stromatolites
The oldest known fossils, rocks formed by the accumulation of sedimentary layers of prokaryote species in shallow marine environments
35
Great Oxygenation Event (GOE)
When oxygen began accumulating in the atmosphere and oceans, dramatically altered Earth’s environmental and caused the extinction of many prokaryotic groups 2.7 to 2.3 bya because prokaryotes has an anaerobic metabolism.