AP Environmental Science - Topic 1: Ecosystems, Biomes, and Biogeochemical Cycles

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Vocabulary flashcards covering ecological hierarchy, species interactions, aquatic and terrestrial biome characteristics, and the processes of the carbon and nitrogen biogeochemical cycles.

Last updated 5:53 PM on 9/4/26
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42 Terms

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Individual

A single organism within an ecosystem, such as one elk.

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Population

A group of individuals of the same species living in the same area, such as an elk herd.

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Community

All of the living organisms belonging to different species present in a given area.

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Ecosystem

All the living (biotic) organisms and nonliving (abiotic) components, such as plants, animals, rocks, soil, water, and air, interacting in a specific area.

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Biome

A large regional community of plants and animals defined by its specific climate, primarily based on average yearly temperature and precipitation.

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Mutualism

A close and long-term symbiotic interaction between two species in which both organisms benefit (+/++/+).

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Commensalism

A symbiotic relationship in which one species benefits while the other is unaffected (+/0+/0).

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Predation

An interaction in which one organism uses another organism as an energy source (+/+/-).

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True Predators

Carnivores that kill and eat their prey for energy.

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Herbivores

Organisms that eat plants to obtain energy.

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Parasites

Organisms that live on or inside a host organism to gain energy, often without killing the host.

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Parasitoids

Organisms that lay eggs inside a host organism, which then hatch so the larvae can consume the host for energy.

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Symbiosis

Any close and long-term interaction between two organisms of different species, including mutualism, commensalism, and parasitism.

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Resource Partitioning

The practice of different species using a shared limited resource in different ways, places, or times to reduce competition and survive.

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Types of Resource Partitioning

The three strategies species use to share limited resources: temporal partitioning (using resources at different times), spatial partitioning (using different areas of a habitat), and morphological partitioning (using different resources based on evolved physical features).

<p>The three strategies species use to share limited resources: temporal partitioning (using resources at different times), spatial partitioning (using different areas of a habitat), and morphological partitioning (using different resources based on evolved physical features).</p>
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Temporal Partitioning

A form of resource partitioning where competing species utilize the same resource at different times, such as hunting during the night versus during the day.

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Spatial Partitioning

A form of resource partitioning where competing species utilize different physical spaces or depths within a shared habitat.

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Morphological Partitioning

A form of resource partitioning where competing species evolve distinct physical body features to reduce resource competition.

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Lake Zonation

The distinct ecological zones of a freshwater lake defined by light penetration and depth, including the shallow littoral zone with rooted plants, open photic limnetic zone with phytoplankton, deep aphotic profundal zone, and bottom benthic zone.

<p>The distinct ecological zones of a freshwater lake defined by light penetration and depth, including the shallow littoral zone with rooted plants, open photic limnetic zone with phytoplankton, deep aphotic profundal zone, and bottom benthic zone.</p>
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Littoral Zone

The shallow water area of a freshwater lake near the shore where sunlight reaches the bottom and emergent rooted plants grow.

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Limnetic Zone

The open, well-lit surface water layer of a lake where light penetrates to support photosynthesis and phytoplankton, but no rooted plants.

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Profundal Zone

The deep layer of a freshwater lake where sunlight cannot penetrate, preventing photosynthesis.

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Benthic Zone

The nutrient-rich, murky bottom sediment layer of a body of water inhabited by decomposers and invertebrates.

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Wetland

An ecosystem with soil submerged or saturated in water for at least part of the year, shallow enough to support emergent vegetation adapted to wet soil.

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Estuary

A coastal aquatic zone where freshwater rivers flow into the ocean, creating a mix of fresh and salt water with high nutrient levels and biological productivity.

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Intertidal Zone

The narrow band of ocean coastline located between high tide and low tide, where organisms must adapt to wave action and exposure during low tide.

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Ocean Zonation

The vertical and horizontal spatial zones of marine biomes, including the coastal intertidal zone, sunlit photic zone, dark aphotic zone, and bottom benthic zone.

<p>The vertical and horizontal spatial zones of marine biomes, including the coastal intertidal zone, sunlit photic zone, dark aphotic zone, and bottom benthic zone.</p>
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Photic Zone

The upper layer of an aquatic biome that receives sufficient sunlight for photosynthesis.

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Aphotic Zone

The deep layer of an aquatic biome that does not receive sunlight, requiring organisms to rely on detritus or chemosynthesis for energy.

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Carbon Sink

A carbon reservoir that absorbs and stores more carbon than it releases into the atmosphere, such as oceans, plants, and soil.

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Carbon Source

A reservoir or process that releases more carbon into the atmosphere than it absorbs, such as fossil fuel combustion, deforestation, and livestock agriculture.

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Photosynthesis and Cellular Respiration Equations

The complementary biochemical pathways cycling carbon between living things: Photosynthesis (Solar energy+6H2O+6CO2C6H12O6+6O2\text{Solar energy} + 6\text{H}_2\text{O} + 6\text{CO}_2 \rightarrow \text{C}_6\text{H}_{12}\text{O}_6 + 6\text{O}_2) converts atmospheric carbon to glucose, while Respiration (Energy+6H2O+6CO2C6H12O6+6O2\text{Energy} + 6\text{H}_2\text{O} + 6\text{CO}_2 \rightarrow \text{C}_6\text{H}_{12}\text{O}_6 + 6\text{O}_2) breaks down glucose to release energy and return carbon dioxide.

<p>The complementary biochemical pathways cycling carbon between living things: Photosynthesis ($$\text{Solar energy} + 6\text{H}_2\text{O} + 6\text{CO}_2 \rightarrow \text{C}_6\text{H}_{12}\text{O}_6 + 6\text{O}_2$$) converts atmospheric carbon to glucose, while Respiration ($$\text{Energy} + 6\text{H}_2\text{O} + 6\text{CO}_2 \rightarrow \text{C}_6\text{H}_{12}\text{O}_6 + 6\text{O}_2$$) breaks down glucose to release energy and return carbon dioxide.</p>
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Photosynthesis

The chemical process performed by plants, algae, and phytoplankton that converts carbon dioxide (CO2CO_2), water (H2OH_2O), and solar energy into glucose (C6H12O6C_6H_{12}O_6) and oxygen (O2O_2).

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Cellular Respiration

The process performed by living organisms that uses oxygen (O2O_2) to break down stored glucose (C6H12O6C_6H_{12}O_6) for energy, releasing carbon dioxide (CO2CO_2) and water (H2OH_2O).

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Sedimentation

A slow geological process in the carbon cycle where dissolved calcium carbonate precipitates as sediment and settles on the ocean floor.

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Nitrogen Cycle Diagram

The biogeochemical cycle illustrating the movement of nitrogen through various chemical states (N2N_2, NH3NH_3, NH4+NH_4^+ , NO2NO_2^- , NO3NO_3^- , N2ON_2O) across reservoirs including the atmosphere, soil bacteria, plants, and animals.

<p>The biogeochemical cycle illustrating the movement of nitrogen through various chemical states ($$N_2$$, $$NH_3$$, $$NH_4^+$$ , $$NO_2^-$$ , $$NO_3^-$$ , $$N_2O$$) across reservoirs including the atmosphere, soil bacteria, plants, and animals.</p>
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Nitrogen Fixation

The conversion of atmospheric nitrogen gas (N2N_2) into biologically available forms such as ammonia (NH3NH_3) or nitrate (NO3NO_3^-) via soil bacteria, root nodule symbionts, lightning, or synthetic process.

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Nitrification

The two-step biological process by soil bacteria that converts ammonium (NH4+NH_4^+) into nitrite (NO2NO_2^-) and then into nitrate (NO3NO_3^-).

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Ammonification

The process in which decomposers and soil microbes break down waste and dead biomass, converting organic nitrogen back into ammonium (NH4+NH_4^+).

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Assimilation (Nitrogen Cycle)

The uptake of soil nitrates (NO3NO_3^-) or ammonium (NH4+NH_4^+) by plant roots, or consumption of plants by animals, incorporating nitrogen into biological molecules like proteins and DNA.

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Denitrification

The conversion of soil nitrates (NO3NO_3^-) into nitrous oxide (N2ON_2O) and nitrogen gas (N2N_2) by anaerobic soil bacteria, returning nitrogen to the atmosphere.

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Eutrophication

The ecological process where excess nutrient runoff (such as nitrates) stimulates excessive algal growth, causing algal blooms that block sunlight and deplete dissolved oxygen upon bacterial decomposition.