Exam II Flashcards

(33 cards)

1
Q

Human Population Growth

A

Increasing exponentially. Problems that arise from having this many people: Number of available resources, the rate of resource consumption, rates are regionally and economically based, the change in resources

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2
Q

When/why did humans migrate out of Africa?

A

100,000 years ago, because of their hunter-gatherer lifestyle

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3
Q

Pre-agricultural period

A

100,000 years ago. It took tens of thousands of years for human population to double. At the end of this period, there are 5-10 million people. Marked by a hunter-gatherer culture

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4
Q

Agricultural period (Neolithic Revolution)

A

10,000 years ago. Plants and animals are domesticated
Doubling time is shortened to 1,000 years. There are 500 million people at the end of this period. Population density increases. Specialization of professions begins. High birth rates

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5
Q

Industrial period

A

~1800. Huge technological advances are made. Fossil fuels begin to be used at huge rates. Advances in sanitation and medicine are achieved. Death rates decline. High birth rates maintained for some time

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6
Q

Demographic transition model

A

Pretransition: a pre-economy lifestyle. Birth dates and death rates are high. Mortality transition: economic development occurs. Birth rates are high and death rates are low. Fertility transition: low birth and death rates. The US is at this stage. Stability transition: birth rates and death rates are approximately equal

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7
Q

Age structure

A

Determined by survivorship and age-specific birth rate

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8
Q

Point of crisis

A

Developed by Thomas Malthus. When the available resources can no longer carry any more of a population

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9
Q

Effects of age structure

A

Too young puts pressure on resources; too old puts pressure on the workforce/economy

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10
Q

Resource competition

A

Interspecific competition: competition between two or more species. Intraspecific competition: competition between multiple members of the same species

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11
Q

Niche

A

Ecological niche: the role an organism fills within its habitat. Fundamental niche: the complete range of areas in which an organism could exist. Realized niche: the range in which an organism actually exists due to competition. Niche differentiation: potential competitors will coexist, division of resources will occur

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12
Q

Competition mechanisms

A

Exploitation (quick consumption) and interference (denial)

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13
Q

Trophic levels

A

First trophic level: primary producers (autotrophs)
Second level: primary consumers (herbivores)
Third level: secondary consumers (carnivores)
Fourth level: tertiary consumers (top carnivores)

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14
Q

How much energy is available to the next trophic level?

A

Only ~10%

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15
Q

Keystone species

A

A species that is highly important to a food web

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16
Q

Trophic cascade

A

When a change in one trophic level has effects in other trophic levels

17
Q

Pools

A

Where matter resides in an ecosystem

18
Q

Flux

A

The rate at which matter moves

19
Q

Mass-balancing accounting

A

The process that accounts for the abundance for an element in an ecosystem

20
Q

Capital

A

The total mass of an element in the pool

21
Q

Equilibrium

A

When capital in a pool remains constant

22
Q

Residence time

A

Average time an element stays in a pool

23
Q

Cycling time

A

Average time it takes an element to move through the cycle

24
Q

Hydrological cycle

A

Energy of solar radiation and gravity drive the cycle. Evaporation, transpiration, and precipitation all involved. After precipitation, water can return to the atmosphere via evaporation or transpiration, percolate through soil/rock to become groundwater (aquifer), or join other bodies of water

25
Where is most carbon found?
Most carbon is found in sedimentary rocks,
26
Nitrogen cycle
Nitrogen is the most abundant element in the atmosphere. It enters the biosphere through nitrogen fixation (bacteria convert N2 to NO3-). Soil bacteria carry out nitrification (NO3- to NO2-). Ammonification occurs (NO2- to NH3)
27
Long-term climate patterns
In the past 10,000 years, Earth has gone through periods of ups and downs. In the past 1,000 years, Earth has warmed, cooled, and warmed again
28
Pleistocene
Occurred two million years ago. The cycles of this period lasted ~100,000 years each. 800,000 years ago, a cold period brought severe glaciers, these glaciers covered most of North America.The most recent cool period took place from 110,000 to 12,000 years ago
29
Holocene
Started 10,000 years ago. The Earth is in a warm interglacial period
30
The Little Ice Age
Took place from 1000-1300 CE
31
Neanderthals
Neanderthals lived in Europe during the Ice Age. They lived 130,000 years ago. They had short, squatty bodies and large sinuses
32
Forecasting global warming
Global circulation models (GCMs) forecast climate change and are checked by the process of backcasting. Three baselines: today’s world (0° change), business as usual (4°C increase by 2100), sustainable world (1.8° increase by 2100)
33
Committed warming
0.1°C per decade