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Vocabulary flashcards covering key terms from the video notes on energy flow, productivity, biogeochemical cycles, biomes, aquatic zones, and ecological interactions.
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Gross Primary Productivity (GPP)
The rate at which producers convert solar energy into stored chemical energy via photosynthesis; typically measured in kcal/m2/year.
Net Primary Productivity (NPP)
GPP minus the energy used by producers for aerobic respiration; the amount of energy stored as biomass that supports consumers.
Photosynthesis
The process by which producers convert light energy into chemical energy stored as sugars.
Respiration (aerobic respiration)
The process by which cells break down stored energy to fuel metabolism, releasing energy for growth and maintenance.
Primary producers
Organisms that produce their own organic matter from inorganic sources (autotrophs).
Autotrophs
Organisms that sustain themselves without consuming organic material from others; they produce their own food.
Primary consumers
Herbivores that eat primary producers.
Secondary consumers
Carnivores that eat herbivores.
Tertiary consumers
Carnivores that eat other carnivores.
Omnivores
Organisms that eat both plants and animals.
Detritivores
Organisms that feed on dead organic material, especially detritus.
Decomposers
Organisms that break down dead matter, returning nutrients to the ecosystem.
Phycobiliproteins
Colored pigments in cyanobacteria that help photosynthesis by absorbing light colors chlorophyll does not absorb.
Fluorescence
Property of some compounds to absorb one color of light and emit another color.
Carbon cycle
The movement of carbon between sources and sinks (air, water, organisms, soil); includes photosynthesis, respiration, decomposition and fossil fuel burning.
Reservoir
A source or storage pool where a substance accumulates for varying lengths of time in biogeochemical cycles.
Fossil fuels
Carbon-rich energy sources (coal, oil, natural gas) formed over millions of years and released as CO2 when burned.
Decomposition
The breakdown of dead organic matter by decomposers, returning nutrients to the environment.
Nitrogen cycle
The movement of nitrogen through sources and sinks in ecosystems; largest reservoir is the atmosphere.
Nitrogen fixation
Process by which atmospheric N2 is converted into ammonia or related compounds usable by plants.
Nitrification
Oxidation of ammonia to nitrite and nitrate by specialized bacteria.
Assimilation
Uptake of nitrates or ammonium into plant tissues and incorporation into organic compounds.
Ammonification
Conversion of organic nitrogen from decaying matter into ammonia.
Denitrification
Conversion of nitrates back into nitrogen gas, returning N2 to the atmosphere.
Phosphorus cycle
Movement of phosphorus through ecosystems; largest reservoir is ocean sediments; no atmospheric component; often a limiting nutrient.
Ocean sediments
Major phosphorus reservoir in the phosphorus cycle.
No atmospheric component
Phosphorus cycle lacks a gaseous phase in its return flow, unlike carbon or nitrogen cycles.
Hydrologic cycle
Movement of water through Earth’s systems (solid, liquid, gaseous); largest reservoir is the ocean.
Lotic
Rapidly moving freshwater systems (streams, rivers).
Lentic
Still or slow-moving freshwater systems (lakes, ponds).
Photic zone
Sunlit layer of a body of water where photosynthesis can occur.
Littoral zone
Nearshore zone of a lake or sea where light reaches the bottom; rich in biodiversity.
Benthic zone
Bottom zone of a body of water where organisms live on or in the substrate.
Limnetic zone
Open-water zone in a lake away from the shore; away from the littoral zone.
Profundal zone
Deep, aphotic zone below the limnetic zone in a lake.
Epipelagic zone
The uppermost pelagic zone in the ocean where sunlight is abundant.
Mesopelagic zone
Twilight zone of the open ocean, below the epipelagic, with limited light.
Competitive Exclusion Principle
Two species competing for the same limiting resource cannot coexist indefinitely.
Resource partitioning
Dividing resources in different ways, places, or times to reduce competition.
Mutualism
A symbiotic relationship in which both species benefit.
Commensalism
A symbiotic relationship in which one species benefits and the other is unaffected.
Parasitism
A symbiotic relationship in which one organism benefits at the expense of the other.
Gross Primary Productivity (GPP)
Total energy captured by producers through photosynthesis.
Net Primary Productivity (NPP)
Energy available to consumers after respiration; it determines the carrying capacity of ecosystems for consumers. (\text{NPP} = \text{GPP} - \text{R})
NPP's Geographic Distribution
Highest near the equator (tropics) and lowest near the poles and in deserts.
Trophic level
The position an organism occupies in a food chain (e.g., producer, herbivore, carnivore).
Energy Pyramid
A model illustrating how energy flows through trophic levels, where sunlight provides energy to producers, and only about 10\% of energy passes to the next trophic level.
10% Rule
Only approximately 10\% of energy passes to the next trophic level; the rest is lost to respiration, heat, and maintenance.
Carbon Cycle's Largest Reservoir
The ocean (dissolved CO_2 and carbonates).
Photosynthesis (Carbon Cycle)
Plants, algae, and phytoplankton absorb CO_2 and turn it into glucose.
Respiration (Carbon Cycle)
Organisms break down glucose and release CO_2 back into the atmosphere.
Decomposition (Carbon Cycle)
Decomposers break down dead matter, releasing CO2 or methane (CH4).
Sedimentation & Fossilization (Carbon Cycle)
Carbon gets stored in sediments or fossil fuels for millions of years.
Combustion (Carbon Cycle)
Burning fossil fuels releases stored carbon quickly as CO_2.
Modern Carbon
Currently cycling through organisms, air, and oceans.
Fossil Carbon
Stored for millions of years in coal, oil, and natural gas.
Nitrogen Cycle's Largest Reservoir
The atmosphere (78\% nitrogen gas, N_2).
Nitrogen Fixation
Specialized bacteria or lightning convert N2 gas into ammonia (NH3) or ammonium (NH4^+), which plants can use. (\text{N}2 \rightarrow \text{NH}3/\text{NH}4^+).
Nitrification
Bacteria convert ammonia (NH3) into nitrite (NO2^-), then nitrate (NO3^-). Nitrate is the main form plants absorb. (\text{NH}3 \rightarrow \text{NO}2^- \rightarrow \text{NO}3^-) .
Assimilation (Nitrogen Cycle)
Plants absorb nitrate (NO3^-) and incorporate it into proteins and nucleic acids. Animals get nitrogen by eating plants. (\text{NO}3^- \rightarrow \text{plant proteins}).
Ammonification
Decomposers break down organic matter (dead plants/animals, waste) into ammonia/ammonium. (\text{organic N} \rightarrow \text{NH}3/\text{NH}4^+).
Denitrification
Bacteria convert nitrate (NO3^-) back into N2 gas, returning it to the atmosphere. (\text{NO}3^- \rightarrow \text{N}2 \text{ gas}).
Phosphorus Cycle's Largest Reservoir
Rocks and ocean sediments.
Phosphorus Cycle's Atmospheric Phase
None; phosphorus is naturally scarce.
Weathering (Phosphorus Cycle)
Rocks release phosphate (PO_4^{3-}) into soil/water.
Assimilation (Phosphorus Cycle)
Plants absorb phosphate; animals get it by eating plants.
Limiting Nutrient (Phosphorus)
Phosphorus is a limiting nutrient because ecosystems often can't grow unless it's available.
Hydrologic Cycle's Largest Reservoir
Oceans (97\% of Earth’s water).
Power Source of the Hydrologic Cycle
The sun.
Evaporation
Water from oceans/lakes turns into vapor.
Transpiration
Plants release water vapor from leaves.
Condensation
Water vapor forms clouds.
Precipitation
Water falls as rain, snow, or sleet.
Runoff
Water flows across land into rivers/lakes.
Infiltration
Water soaks into soil, replenishing groundwater.
Biome
A large ecological area defined by climate, flora, and fauna.
High NPP Biomes
Tropical rainforests, estuaries, wetlands.
Low NPP Biomes
Deserts, tundra, open ocean (except upwellings).
Photic Zone
The sunlit layer of water where photosynthesis can occur.
Aphotic Zone
The dark layer of water without photosynthesis; organisms here rely on detritus or chemosynthesis.
Lentic Systems
Aquatic systems with still or slow-moving water (e.g., ponds, lakes, wetlands).
Lotic Systems
Aquatic systems with flowing water (e.g., rivers, streams).
Littoral Zone (Lakes)
The near-shore, shallow part of a lake where plants are rooted.
Limnetic Zone (Lakes)
The open water part of a lake where light penetrates, supporting phytoplankton.
Profundal Zone (Lakes)
The deep, dark part of a lake with little oxygen.
Benthic Zone (Lakes)
The bottom sediments of a lake, inhabited by decomposers.
Epipelagic Zone (Sunlight Zone)
The surface to approximately 200 \text{ m} of the ocean, with enough light for photosynthesis; most marine life lives here.
Mesopelagic Zone (Twilight Zone)
The oceanic zone from 200 \text{–}1,000 \text{ m} with faint light and no photosynthesis.
Bathypelagic Zone (Midnight Zone)
The oceanic zone from 1,000 \text{–}4,000 \text{ m} with complete darkness, where organisms use bioluminescence.
Abyssopelagic Zone
The oceanic zone from 4,000 \text{–}6,000 \text{ m} with near-freezing temperatures and high pressure.
Hadal Zone
Deep ocean trenches below 6,000 \text{ m} with extreme conditions.
Estuaries
Transition areas where rivers meet the sea (freshwater + saltwater mix), highly productive and critical nurseries.
Wetlands
Areas saturated with water seasonally or permanently (swamps, marshes, bogs), known for high NPP, biodiversity, and ecosystem services.
Terrestrial Biomes
Distinct ecological areas defined by similar climate, soil, and vegetation types.
Primary Determinants of Biome Type
Temperature and precipitation.
Tropical Rainforest Biome
Hot, wet year-round climate; nutrient-poor soil; broadleaf evergreen trees; very high NPP.
Savanna (Tropical Grassland) Biome
Warm year-round climate with distinct wet and dry seasons; fertile soil; scattered trees and grasses; moderate to high NPP.
Desert Biome
Hot or cold, very dry climate (less than 25 \text{ cm} rainfall per year); mineral-rich soil, low organic matter; succulents; very low NPP.
Temperate Grassland (Prairie/Steppe) Biome
Moderate rainfall, cold winters, hot summers; very fertile, thick topsoil; grasses; moderate NPP.
Temperate Deciduous Forest Biome
Four distinct seasons, moderate rainfall; nutrient-rich soil due to seasonal leaf fall; deciduous trees; moderate to high NPP.