Unit 4: Ecosystems Flashcards

1
Q

Niche

A

the ecological role a species plays in an ecosystem

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2
Q

Competitive Exclusion Principle

A
  1. no two species can occupy the same niche without competing
  2. if two species compete for the same limited resources, one will outcompete the other
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3
Q

Resource Partitioning

A

When two or more species divide resources/avoid competition based on differences in behavior or morphology (body physiology)

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4
Q

Amensalism

A

In this interaction, one species suffers while the other is unaffected.

Ex: allopathy where one species releases a chemical substance to inhibit the growth of another species. Penicillium secretes penicillin, which kills various bacteria.

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5
Q

Competition (two types)

A

This interaction is based upon a competition for resources.

There are two types:
In intraspecific competition, organisms from the same species compete for the same resource.
In interspecific competition, organisms of different species compete for the same resource, usually aggressively.

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6
Q

Commensalism

A

In this interaction, one species benefits from the interaction while the other is neither helped nor harmed

Ex:
small birds and large grazing herbivores. The small birds perch on the backs of large herbivores while they graze in grassy fields. The movement of the large herbivores stirs up insects out of the grass which the small birds then feed on.

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7
Q

Mutualism

A

In this interaction, both species benefit
Ex: bees and flowers

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8
Q

Neutralism

A

While this interaction is almost always implied rather than stated in most superficial interactions, it is crossing paths where neither organism is affected by the other

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9
Q

Parasitism

A

In this interaction, one species benefits while the other is harmed. Parasites generally attach to a host as a consistent source of nutrition. Parasites may be exoparasites, existing outside the host, or endoparasites, existing inside the host. The parasite does not want to kill its host, as this would remove the source of food

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10
Q

Predation

A

In this interaction, one species benefits while the other is harmed. Predators obtain food at the expense of their prey

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11
Q

Saprophytism

A

In this interaction, a dead or decaying organism is fed upon by another organism. Most of these detritivores replenish essential environmental nutrients as part of the biogeochemical cycles

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12
Q

What makes a species invasive by nature?

A
  • All invasive species were once introduced species (they are non-native by nature)
  • Can be introduced purposefully (as with the cane toad) or accidentally (as with the zebra mussel)
  • They outcompete native species for resources & lack a natural predator in their introduced environment
  • Invasives are often generalists and r-selected species meaning: 1. they have lots of offsprings in short amounts of time 2. they reach reproductive maturation early in their life spans
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13
Q

Ecosystem

A

All the organisms in a community (biotic) interacting with abiotic factors (water, air, nutrients)

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14
Q

What is needed in an ecosystem for it to function?

A
  • the capture of energy (photosynthesis -> primary productivity)
  • the transfer of energy
  • the cycling of matter (biogeochemical cycles)
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15
Q

Net primary productivity (NPP)

A

Gross primary productivity (GPP) – Respiration

Units : kcal / m^2 / yr

GPP = rate of photosynthesis in a given area
Respiration = rate of energy used by primary producers (plants)
NPP = “surplus” or what’s left over after photosynthesizers (plants) have carried out respiration. Passed on to higher trophic levels

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16
Q

Ecological pyramid

A

primary producers -> primary consumers -> secondary consumers -> tertiary consumers

10% of energy is transferred between trophic levels of the food chain

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17
Q

Inefficiency of Energy Transfer

A
  • Based on the 2nd Law of Thermodynamics
  • Loss of energy between levels of food chain
  • energy is lost largely due to heat but also because of waste and cellular respiration
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18
Q

Bioaccumulation

A

Absorption of a substance by a living organism

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19
Q

Biomagnification

A

Increase in concentration of a substance per unit of body tissue that occurs in successively higher trophic levels/increase in concentration of chemicals in each organism up the food chain.

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20
Q

A substance will biomagnify if

A
  1. It’s oil/fat soluble (can be built up/stored in body tissues)
  2. It’s persistent (stays in the body for a long time)
  3. It’s biologically active

Ex:
pesticides (like DDT), heavy metals (lead, cadmium, mercury), environmental toxins (like PCBs)

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21
Q

Removal of a keystone species results in

A

“trophic cascades” (a.k.a. “downgrades” → ecosystem collapses & biodiversity declines)

trophic cascades = an ecological phenomenon triggered by the addition or removal of top predators and involving reciprocal changes in the relative populations of predator and prey through a food chain, which often results in dramatic changes in ecosystem structure and nutrient cycling.

22
Q

Biomes

A

The land surface of the Earth is divided into a number of geographic areas distinguished by particular types of dominant flora and fauna.

flora and fauna = collection of all plants and animals living in a particular region

23
Q

Factors that can affect the location of biomes include

A
  • Latitude: how far north and south from equator
  • Temperature: represented as a line graph on a climate graph
  • Rainfall: represented as a bar graph on a climate graph

(Climatic conditions are depicted in climatographs (a.k.a. climate graphs or climate diagrams))

24
Q

Each biome is characterized by

A

amount of precipitation and the average annual temperatures recorded

25
Q

The big 6

A

CHNOPS

Carbon
Hydrogen
Nitrogen
Oxygen
Phosphorus
Sulfur

26
Q

Biogeochemical Cycles

A

Movements of matter within & between ecosystems involving biological, geological, and chemical processes.

27
Q

What roles do matter and energy play?

A
  • ENERGY comes from the Sun, FLOWS through biotic & abiotic components, then emits back into space. It is never lost, just transformed!
  • MATTER never leaves but CYCLES in a variety of forms.
    Remember: Earth is an open system w/ respect to energy but closed w/ respect to matter
28
Q

How do the 1st and 2nd Laws of Thermodynamics apply to cycles of energy and matter?

A

1st Law states that matter and energy are never created nor destroyed, but transformed.

2nd Law states that when these transformations happen, they are never 100% efficient or useful; some energy is lost as “waste heat”

29
Q

Reservoirs

A

A pool or holding place for a nutrients

30
Q

Sinks

A

Reservoirs that accept more nutrients than they release

31
Q

The 6 processes of the carbon cycle

A

6 processes drive this cycle:
- Photosynthesis
- Respiration
- Exchange
- Sedimentation & Burial
- Extraction
- Combustion

1: Photosynthesis
- Plants hold carbon for a short amount of time.
- They take in CO2 in this process and make glucose (C6H12O6)
- Plants are carbon sinks

2: Respiration
- Consumers & decomposers (via metabolic processes) release CO2 into the atmosphere and soil.
- does not contribute to carbon emissions in the air
- the soil is a carbon sink

3: Exchange
- CO2 moves back and forth from the ocean & atmosphere (a.k.a. “diffusion”).
- The ocean is the largest sink of carbon

4: Sedimentation & Burial
- Organisms die, decompose, get buried, and become fossil fuels.
- In both cases, carbon is held or “sequestered” in these reservoirs for a long time (millions of years!)
- Sedimentary rock (ex: limestone) is the largest reservoir of inorganic carbon.

5: Extraction
- Fossil fuels are removed from underground via mining, drilling/fracking.
- This quickly releases CO, CH4 and CO2
- Fossil fuels are sources of “new” carbon

6: Combustion
- Combustion of fossil fuels releases CH4 and CO2 in the atmosphere
- This quickly adds “new” carbon to the atmosphere

32
Q

Explain how carbon cycles through ecosystems

A

Plants and other photosynthetic organisms capture atmospheric carbon dioxide (CO₂) during photosynthesis, using it to produce glucose and other organic compounds, which serve as energy sources for themselves and the consumers that eat them. When organisms respire, they release CO₂ back into the atmosphere. Additionally, when plants and animals die, decomposers break down their remains, returning carbon to the soil or releasing it as CO₂. Some carbon is stored long-term in fossil fuels and sediments, which can re-enter the cycle through combustion or erosion. This dynamic movement of carbon helps sustain life, regulate global temperatures, and maintain the balance of ecosystems. Further, the ocean and atmosphere constantly exchange carbon (but not always equal amounts).

33
Q

anthropogenic impacts on the carbon cycle?

A
  1. Increased extraction & combustion of fossil fuels via human activities (such as driving gasoline-powered cars) releases more CO2 & CH4
  2. Deforestation increases the amount of CO2 in atmosphere b/c of the removal of carbon “sinks”
    Both contribute to accelerating climate change b/c greenhouse gases are released/there’s more greenhouse gasses in the atmosphere
34
Q

Why do living things need nitrogen?

A

Nitrogen atoms are needed to build nucleic acids (for DNA and RNA synthesis) and amino acids (for protein synthesis)

35
Q

What is the significance behind how molecular nitrogen is chemically found?

A

N2 is not biologically “useful” so it needs to be chemically “fixed” to make it useful

36
Q

Steps of the Nitrogen Cycle

A

First way:
Step 1: Nitrogen fixation
- Abiotic form: Lightning converts N2 to nitrate (NO3-)
- Nitrate = most “useable form” of nitrogen
- nitrogen gets fixed in one step because of lightning
- Equation: N2 –(by lightning)—> NO3-

Second way:
Step 1: Nitrogen fixation
- Biotic form: Nitrogen-fixing bacteria (often found in the roots of legume/bean plants) convert nitrogen gas (N2) from the atmosphere into ammonia (NH3) and/or ammonium (NH4+) in the soil
- Equation: N2 —(by bacteria on roots of legumes)—>NH3 and NH4+

Step 2: Nitrification
- Nitrifying bacteria in the soil convert ammonium (NH4+) and/or ammonia (NH3) to nitrites (NO2-) and then nitrates (NO3-)
- Nitrate = most “useable form” of nitrogen
- Equation: NH3 and/or NH4+ —(by nitrifying soil bacteria)—-> NO2- & NO3-

Step 3: Assimilation
- Plants and animals incorporate the nitrates into their tissues when they eat or make their food

Step 4: Ammonification/Mineralization
- When animals and plants die, decomposers break down the amino acids into NH4+ and return it to the soil
- Nitrifying bacteria again convert the NH4+ to NO3- or NO2-
- Equation: NH3 and/or NH4+ —(by nitrifying soil bacteria)—-> NO2- & NO3-

Step 5: Denitrification
- Denitrifying bacteria in the soil convert NO3- into N2O, which then converts to N2 in the atmosphere
- Equation: NO3- —(by denitrifying bacteria)—-> N2O —-> N2

37
Q

Explain the nitrogen cycle

A

Nitrogen gas (N₂), which makes up about 78% of the atmosphere, is not directly usable by most organisms. The atmosphere is the largest reservoir of nitrogen. Nitrogen-fixing bacteria in the soil or in the roots of legumes convert N₂ into ammonia (NH₃) or ammonium (NH₄⁺) in a process called nitrogen fixation. Other bacteria convert ammonia into nitrites (NO₂⁻) and then nitrates (NO₃⁻) through nitrification, forms that plants can absorb and use to build proteins and DNA. The absorption of nitrites and nitrates by plants and animals is called assimilation. Animals obtain nitrogen by consuming plants or other animals. When organisms die or excrete waste, decomposers return nitrogen to the soil as ammonia through ammonification. Some bacteria convert nitrates back into nitrogen gas in a process called denitrification, completing the cycle. This intricate process ensures nitrogen is continuously available for living organisms and maintains ecosystem balance.

38
Q

What are the anthropogenic impacts on the nitrogen cycle?

A
  1. Using synthetic fertilizers adds nitrates (NO3-) to an ecosystem when they runoff into bodies of water
    → lead to algal blooms
    Fertilizers are NOT the same as pesticides!
  2. Discharging animal waste/untreated sewage into bodies of water adds nitrates (NO3-) → lead to algal blooms
  3. Cars & power plants emit NO2 into the air → leads to the formation of ozone (O3) that accumulates in the troposphere (“bad” ozone). This contributes to global warming and is a harmful gas.
39
Q

Explain the water (hydrologic) cycle

A

It begins with evaporation, where solar energy causes water from oceans, lakes, and rivers to change from liquid to vapor. Plants also contribute through transpiration, releasing water vapor from their leaves. This water vapor rises, cools, and condenses into droplets, forming clouds in a process called condensation. When these droplets grow large enough, they fall to Earth as precipitation—rain, snow, sleet, or hail. Precipitated water can infiltrate the soil through infiltration, recharging underground aquifers in a process known as percolation. Some water flows over the land as surface runoff, returning to rivers, lakes, and oceans. Meanwhile, water stored as ice or snow can enter the cycle through sublimation (direct change from solid to vapor) or melting into liquid water. This cycle, driven by solar energy and gravity, ensures the distribution and renewal of Earth’s water supply.

40
Q

What are the anthropogenic impacts on the hydrologic (water) cycle?

A
  1. Deforestation
    Reduce transpiration from plants → More runoff → erosion
  2. Paving over land surfaces
    Water is less likely to permeate through the soil in that particular area → increases runoff & erosion
41
Q

Why do livings things need phosphorus?

A

Phosphorus is needed to form:
- DNA
- Cell membranes (phospholipid bilayer!)
- Bones and teeth

42
Q

Why is phosphorus a limiting factor in plant growth?

A

Phosphorus doesn’t cycle in the air so it takes longer for plants and animals to access it via the water and soil.
Found in nature as PO4-3 (phosphate) in a mineral called apatite

43
Q

How does phosphorus cycle in the lithosphere & biosphere?

A
  1. Weathering of rocks leaches out PO4-3 (phosphate)
  2. Plants and animals assimilate PO4-3 They die & decomposers release the PO4-3 back into the soil
  3. Animal excretions (ex: guano from birds and bats) contain phosphate that returns to the soil

lithosphere = earth’s crust and biosphere = where life exists

44
Q

How does phosphorus cycle in the hydrosphere?

A
  1. Weathering/erosion causes leaching of phosphate into streams/rivers.
  2. Aquatic plants and phytoplankton assimilate the phosphate and the cycle continues.

hydrosphere = water bodies

45
Q

Explain the Phosphorus Cycle

A

1: Weathering of Rocks
Phosphorus begins in rocks and minerals as phosphate ions (PO₄³⁻). Through weathering caused by rain, wind, and other natural forces, phosphate is released into soil and water.
2: Absorption by Plants
Plants absorb phosphate ions from the soil through their roots. Phosphorus is an essential nutrient for plants, forming part of DNA, RNA, and ATP (energy molecules). Plants take up available phosphate (not phosphorus) dissolved in soil water. Phosphorus is stable and insoluble (cannot be taken up by plants).
3. Movement Through the Food Chain
Phosphorus moves through the food chain as herbivores eat plants and carnivores eat herbivores. It becomes part of their body structures, such as bones and teeth, and their metabolic processes.
4. Return to Soil and Water
When plants, animals, and other organisms die, decomposers (bacteria and fungi) break down their organic material, returning phosphorus to the soil.
5. Leaching and Runoff
Excess phosphorus in the soil can dissolvfe in water and be carried away to nearby water bodies through runoff.
6. Sedimentation in Water Bodies
Phosphorus settles at the bottom of water bodies, becoming part of sediment.
7. Geological Uplift
Over millions of years, geological processes lift phosphate-rich sedimentary rocks back to the Earth’s surface. Tectonic activity exposes these rocks to weathering, restarting the phosphorus cycle.

46
Q

What are the anthropogenic impacts on the phosphorus cycle?

A
  1. Using synthetic fertilizers adds phosphates (PO4-3) to an ecosystem when they runoff into bodies of water
    → lead to algal blooms
    Fertilizers are NOT the same as pesticides!
  2. Discharging animal waste/untreated sewage into bodies of water adds phosphates (PO4-3)
47
Q

Tundra

A
  • Location: 60° to 75° North (Arctic tundra). Areas below the ice caps in the Arctic; tend to be present in mountainous areas in North America, Europe, and Siberia
  • Climate: Tundras have low precipitation which makes them similar to a desert Extremely cold temperatures in the winter, but can warm up in the summer
  • Soil Fertility: Low; tundras have short growing seasons and a large amount of frost which makes it difficult for plants to grow; however, certain species such as lichens and mosses are able to withstand the temperatures in a tundra. The permafrost covers the ground under the surface which leaves little space for species to grow.
  • General Plant Adaptions: Small, low-growing plants like mosses and lichens conserve heat. Many plants grow in clumps for protection against cold.
  • General Animal Adaptions: Thick fur or fat layers (e.g., polar bears, caribou). Migration and hibernation are common strategies.
  • Anthropogenic Effects:
    1. Removal of permafrost: rising temperatures is decreasing the amount of permafrost in the ground which releases carbon dioxide and methane that contribute to overall global warming.
    2. Mining/Industrialization: the drilling of oil and gas in tundras leads to the deaths of animals in their habitats as well as the removal of vegetation which is vital for their survival.
    3. Hunting: a surge in the amount of caribou and foxes that are hunted ruins the balance of the ecosystem and leads to disrupted food webs which ultimately impact other animals in the environment.
48
Q

Tropical Rainforests

A
  • Location: found between the latitudes 23.5°N and 23.5°S.
  • Climate: The average temperature is approximately 25-30°C (77-86ºF) throughout the year.
  • Soil Fertility: Nutrient-poor and non-fertile soil
  • General Plant Adaptions: Broad leaves for capturing sunlight, drip tips to shed excess water, and buttress roots for stability in thin soils.
  • General Animal Adaptions: High biodiversity with specialized traits like prehensile tails (monkeys), camouflage (tree frogs), or symbiosis (ants and acacia trees).
  • Anthropogenic Effects: Deforestation for agriculture, logging, and mining reduces biodiversity and increases carbon emissions.
49
Q

Coral Reefs

A
  • Location: 30° North to 30° South (tropical and subtropical waters).
  • Climate: Warm, stable water temperatures (18-29°C) with lots of sunlight. Water is typically clear and nutrient-poor.
  • Soil Fertility: N/A; relies on nutrient cycling within the water. Surrounding water is typically nutrient-poor.
  • General Plant Adaptations: Symbiotic algae (zooxanthellae) live in coral tissues, providing energy through photosynthesis.
  • General Animal Adaptations: Bright coloration for communication and camouflage; mutualism between species (e.g., clownfish and anemones).
  • Anthropogenic Effects: Coral bleaching due to warming oceans, overfishing, and pollution (especially plastic and runoff from agriculture).
50
Q

Wetlands

A
  • Location: Found at all latitudes except Antarctica.
  • Climate: Varies by location. Tropical wetlands are warm and humid, while temperate wetlands experience seasonal temperature changes. Rainfall varies but is typically abundant to maintain waterlogged conditions.
  • Soil Fertility: Generally rich in nutrients; supports diverse plant life. Anaerobic conditions in waterlogged soils can slow decomposition.
  • General Plant Adaptations: Aerenchyma tissue in roots and stems helps transport oxygen in waterlogged conditions. Floating leaves (e.g., water lilies) aid photosynthesis.
  • General Animal Adaptations: Amphibians (e.g., frogs) thrive in wet environments. Wading birds have long legs and beaks for foraging.
  • Anthropogenic Effects: Drained for agriculture and urban development, pollution, and invasive species reduce their extent and biodiversity.
51
Q

Temperate Deciduous Forests

A
  • Location: 30° to 50° North and South.
  • Climate: Four distinct seasons with moderate temperatures. Warm summers (20-25°C) and cold winters (-1°C to 10°C). Precipitation is evenly distributed (75-150 cm/year).
  • Soil Fertility: Moderate to high; decaying leaf litter enriches the soil with nutrients.
  • General Plant Adaptations: Deciduous trees shed leaves in fall to conserve water during winter and regrow in spring for photosynthesis.
  • General Animal Adaptations: Animals hibernate or migrate in winter. Many are generalists, capable of eating a variety of foods (e.g., bears, deer). Thick coat in winter that helps animals like deer stay warm, and a lighter coat in summer to keep cool.
  • Anthropogenic Effects: Urbanization, deforestation, and pollution threaten habitats. Acid rain alters soil chemistry.