final (part 4 material) Flashcards

(33 cards)

1
Q

What are pools and fluxes? How do you calculate turnover rate and residence time?

A

Pools: storage compartments of matter (e.g., carbon stored in fossil fuels).

Fluxes: movements of matter between pools (e.g., carbon released by burning).

Turnover rate = (Flux out / Pool size) * 100

Residence time = Pool size / Flux out

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2
Q

What is net primary production (NPP) and how might you measure it?

A

Net carbon available to consumers in an ecosystem; measured using biomass growth or satellite-based chlorophyll reflectance

NPP = GPP - autotroph respiration

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3
Q

How does NPP vary across the globe? What are some factors that affect NPP?

A

NPP varies by biome: highest in tropical forests and lowest in deserts and tundra.

Key factors: precipitation, temperature, and nutrient availability; too much rain can reduce NPP due to nutrient leaching

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4
Q

What is consumption efficiency?

A

Consumption efficiency = (Ingested energy / Available energy from previous level)

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5
Q

What is assimilation efficiency?

A

Assimilation efficiency = (Assimilated energy / Ingested energy)

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6
Q

What is production efficiency?

A

Production efficiency = (Energy to growth / Assimilated energy)

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7
Q

What is trophic efficiency?

A

Trophic efficiency = (Energy passed to next level / Energy in current level)

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8
Q

What is biomagnification?

A

Biomagnification is the increasing concentration of toxins (e.g., mercury, DDT) at higher trophic levels.

Especially problematic in gold mining regions and higher latitudes​

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9
Q

What functions do N and P have in organisms?

A

Nitrogen (N): Essential for amino acids, proteins, enzymes, and DNA. It’s a critical component of chlorophyll in plants and is vital for growth.

Phosphorus (P): Needed for ATP (energy transfer), DNA, RNA, and phospholipids in cell membranes. It is crucial for energy storage and genetic material.

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10
Q

What are the different stages of the nitrogen cycle?

A

Fixation: N₂ gas → NH₃ (ammonia), via microbes, lightning, or industrial processes.

Nitrification: NH₄⁺ → NO₂⁻ → NO₃⁻ by microbes.

Assimilation: Plants absorb NH₄⁺ or NO₃⁻.

Ammonification: Organic N → NH₄⁺ from waste/dead matter.

Denitrification: NO₃⁻ → N₂ gas by anaerobic bacteria, releasing N₂ back to the atmosphere.

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11
Q

How does the nitrogen cycle interact with food webs?

A

N enters food webs when plants assimilate ammonium or nitrate.

It cycles through herbivores and predators via feeding.

Decomposers recycle N back into soil from detritus.

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12
Q

What are some ways that human activity affects the nitrogen and phosphorus cycles?

A

Industrial fertilizer production (Haber-Bosch process) increases reactive nitrogen.

Agriculture (N-fixing crops, fertilizer runoff) causes eutrophication.

Fossil fuel combustion adds nitrogen oxides to the atmosphere.

Mining and overuse of phosphorus-rich fertilizers affect aquatic systems.

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13
Q

Where does phosphorus come from and how does it cycle through ecosystems?

A

Comes from rocks and marine sediments, not from the atmosphere.

Weathering releases it into soil → taken up by plants → cycles through food webs.

Returns to soil via waste/decomposition and can bind to soil or leach into water.

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14
Q

How do scientists study decomposition? What are some factors that affect litter decomposition rates?

A

Methods: Use of litter bags, “Soil Your Undies” challenges, controlled field/lab experiments.

Factors: Moisture, temperature, chemical makeup (lignin/tannins vs. proteins/sugars), presence of decomposers (bacteria, fungi, soil invertebrates).

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15
Q

What are some examples of disturbances that would result in primary vs. secondary succession?

A

Primary succession: Glacial retreat, volcanic eruption (e.g., Mt. St. Helens), landslides—no life remains.

Secondary succession: Fires, floods, clear-cutting—some organisms and soil remain.

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16
Q

What life history traits typically characterize early succession/pioneer species vs. late succession/climax species?

A

Early/pioneer species: r-selected traits (fast-growing, short-lived, high reproductive output).

Late/climax species: K-selected traits (slow-growing, long-lived, competitive).

17
Q

Does the successional trajectory in the Glacier Bay example support the Clementsian or Gleasonian views of succession?

A

Gleasonian. The study found multiple pathways and non-uniform outcomes depending on location and proximity to refugia, supporting individualistic species responses, not a fixed climax (Clementsian view).

18
Q

Describe the three models of succession.

A

Facilitation: Early species modify environment, making it suitable for later ones.

Inhibition: Early species prevent others from establishing; later species dominate due to longer life.

Tolerance: All species can colonize, but those tolerant of limited resources dominate over time.

19
Q

How could animals accelerate or impede the succession of plant communities?

A

Accelerate: Soil invertebrates (e.g., nematodes, beetles) enhance decomposition and nutrient cycling.

Impede: Seed predation (e.g., deer mice eating tree seeds) reduces regeneration and slows succession.

20
Q

What is the field of biogeography?

A

Biogeography studies the geographic distribution of species and communities through geological time

21
Q

What is Wallace’s line and its cause?

A

A biogeographic boundary separating Asian and Australian fauna, caused by deep ocean trenches that prevented species migration during low sea levels

22
Q

What is the relationship between vicariance and disjunct ranges?

A

Vicariance: a once continuous range is split by a barrier (e.g., mountains, oceans).

Leads to disjunct ranges: related species found in widely separated locations​

23
Q

What are some unique features of plants in the tropical rainforest biome?

A

Evergreen, thick leaves with drip tips

High chemical defenses in leaves

Shallow roots with buttresses

Lianas (woody climbers), epiphytes, and nitrogen-fixing epiphylls

24
Q

What are hyperdominant Amazonian tree species?

A

A small number of tree species dominate Amazon biomass and stem count.

25
Why are the Andes mountains a geographic barrier for rain forest organisms?
They block dispersal, leading to cross-Andean disjunctions in many species. 70% of woody species in Central America and the Western Amazon show this pattern
26
What is the story of the tropical tree Symphonia globulifera?
A “living fossil,” found in both Africa and the Neotropics. Shows ancient lineages (~15 million years) and long-distance dispersal despite seed sensitivity to saltwater. A model for studying pantropical biogeography and dispersal events
27
Why are museum specimens useful tools in studies of climate change?
Provide historical data on species distributions, phenology, and abundances. Help detect long-term ecological changes using well-documented geographic and temporal records.
28
What are the main conclusions of the Grinnell resurvey project?
Birds: Reduced richness and altered distributions (likely due to warming). Mammals: Less change; more stable distributions. Conclusion: Birds more sensitive to climate change in Mojave than mammals.
29
Why are small mammals in the Mojave desert more resilient to warming than birds?
Birds had a 58% increase in cooling costs, mammals only 17%. 80% of mammals experienced no increased cooling costs due to burrowing and behavioral thermoregulation.
30
What are some of the traits that favor successful leading-edge range expansion?
High dispersal ability, broad thermal tolerance, rapid reproduction, and generalist diets.
31
How is the changing phenology of arctic plants impacting Caribou?
Phenological mismatch: Plants are leafing earlier due to warming, but Caribou calving time hasn’t shifted accordingly → reduced calf survival due to less nutritious forage.
32
What are the main conclusions of the Forest and Chisholm study of bee responses to climate change?
Warmer conditions led to increased parasitism of mason bees by wasps. Parasites benefitted more than bees, showing negative climate effects on mutualisms.
33
What seems to be happening to Amazonian rainforest tree communities in response to climate change?
Trees face increased drought and heat stress. Although higher CO₂ helps trees close stomata, drought still has strong effects. Forests are shifting to more drought-tolerant species, changing carbon cycling dynamics.