Unit 1 APES

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109 Terms

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Carbon cycle

Movement of carbon between sources and sinks

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carbon sinks definition

a carbon reservoir that stores more carbon that it releases

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carbon sinks examples

Ocean, plants, soil

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carbon reservoir definition

processes that add carbon to the atmosphere

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carbon reservoir examples

fossil fuel combustion, deforestation

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Photosynthesis in carbon cycle

removes CO2 from atmosphere and convert + store it as glucose. Carbon sink.

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Cellular respiration in the carbon cycle

the breakdown of glucose and release of energy; releases carbon dioxide into the environment

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Direct exchange

CO2 moves directly between atmosphere and the ocean by dissolving into and out of ocean water at the surface

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sedimentation in the carbon cycle

when marine organisms die, their bodies sink to ocean floor where they're broken down into sediments that contain carbon

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burial in the carbon cycle

sediments are compressed into sedimentary rock or fossil fuels by pressure

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Nitrogen cycle

The movement of nitrogen between sources and sinks/reservoirs

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The main nitrogen reservoir/sink

atmosphere

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Why organisms need nitrogen

DNA, amino acids to make proteins

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nitrogen fixation

Process of converting nitrogen gas into ammonia

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NH3

ammonia

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NO3

Nitrate

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bacterial fixation

certain bacteria that live in the soil, or in symbiotic relationship with plant root nodules convert N2 into ammonia (NH3)

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synthetic fixation

humans combust FFs to convert N2 gas into nitrate

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assimilation

plants and animals taking nitrogen and incorporating it into their body

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ammonification

decomposers and soil bacteria convert organic waste into ammonia

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nitrification

conversion of ammonia into nitrate and then nitrite by soil bacteria

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denitrification

conversion of nitrate into nitrous oxide which returns to atmosphere

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Ammonia volatilization

excess fertilizer use can lead to NH3 gas entering the atmosphere

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Phosphorus cycle

movement of phosphorus between sources and reservoirs/sinks

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Major reservoir of phosphorus

rocks and sediment

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Why organisms need phosphorus

DNA, ATP (energy), bone and tooth enamel

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Major natural source of phosphorus

weathering of rocks

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Synthetic source of phosphorus

mining of phosphate minerals and adding to products like synthetic fertilizers

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mini loop in carbon cycle

photosynthesis and cellular respiration

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mini loop in phosphorus cycle

assimilation and excretion/decomposition

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mini loop in nitrogen cycle

assimilation and ammonification

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What causes geological uplift?

Tectonic plate collision forcing up rock layers that form mountains.

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What is the role of weathering in the phosphorus cycle?

Weathering releases phosphate from rock.

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the water cycle

movement of water in different states between sources and sinks

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largest water reservoir

ocean

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largest freshwater reservoirs

polar ice caps and groundwater

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two main sources of water

surface water and ground water

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transpiration

Evaporation of water from the leaves of a plant

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process of transpiration

leaf opens in stomata open, allowing water to evaporate from the plant and creating low pressure in the leaf which draws water up from roots.

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evapotranspiration

the amount of water that enters the atmosphere from transpiration and evaporation combined.

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runoff

water that flows over the ground surface rather than soaking into the ground

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infiltration

Downward movement of water through soil.

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Individual

one organism

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Population

group of individuals of the same species

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community

all living organisms in an area

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ecosystem

all living and nonliving things in an area

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Biome

A group of ecosystems with similar climate conditions that determine species that live there

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Symbiosis

A close, long term relationship between two different species

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competition

the struggle between organisms to survive in a habitat with limited resources.

Limits population size ( - , -)

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Predation

An interaction in which one organism kills another for energy ( +, -)

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Mutualism

A relationship between two species that benefits both organisms (+ , +)

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Commensalism

a relationship between two organisms that benefits one organism and doesnt impact the other. (+, 0)

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4 types of predation

True predation, Herbivores, Parasites, Parasitoids

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herbivores

eat plants for energy

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true predators

carnivores; kill and eat prey for energy

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parasite

an organism that uses a host organism for energy

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parasitoid

an organism that lay eggs inside a host organism

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resource partitioning

When species divide a niche to avoid competition for resources; reduces competition

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temporal partitioning

two species reduce competition by using a resource at different times

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spacial partitioning

two species reduce competition by using different areas of a shared habitat

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morphological partitioning

two species reduce competition by using different resources based on different evolved body features

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climate

overall yearly temperature and precipitation

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biomes are defined by

annual temperature and rainfall

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Characteristics of aquatic biomes

salinity, depth, flow, temperature

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Characteristics of rivers

high oxygen due to flow mixing water and air, nutrient rich due to sediments

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Characteristics of lakes

standing bodies of fresh water

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4 zones in freshwater biomes

Littoral, limnetic, profundal, benthic

<p>Littoral, limnetic, profundal, benthic</p>
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wetlands

an area with soil submerged or saturated in water for at least part of the year, but shallow enough for emergent plants

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emergent plants

roots are submerged in water, but rest of plant sticks out

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limnetic zone

well-lit, open-water area of a lake or pond

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littoral zone

a shallow zone in a freshwater habitat where light reaches the bottom and nurtures plants

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profundal zone

a region of water where sunlight does not reach, below the limnetic zone in very deep lakes

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benthic zone

the muddy bottom of a lake, pond, or ocean

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Estuaries

areas where rivers empty into the ocean, mixing freshwater and saltwater

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coral reef

The most diverse marine biome on Earth, found in warm, shallow waters beyond the shoreline.

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intertidal zones

narrow band of coastline between low and high tides

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desiccation

drying out

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open ocean

Low productivity/area as only algae & phytoplankton can survive in most of ocean

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importance of open ocean

algae and plankton absorb atmospheric CO2 and release O2

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aphotic zone

abyssal zone, area of ocean too deep for sunlight

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source zone of rivers

high elevation collects precipitation and snowmelt. Cold, fast-moving, high dissolved oxygen levels, low nutrients

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transition zone of rivers

wider, slower, less dissolved oxygen levels, more sediment, warmer, nutrient-rich when compared to source zone.

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floodplain zone of rivers

where water spills out, forming wetlands and temporary lakes. More sediment, less dissolved oxygen.

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biosphere

combination of all ecosystems on earth

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taiga

Biome in which the winters are cold but summers are mild enough to allow the ground to thaw

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temperate rainforests

a coastal biome typified by moderate temperatures and high precipitation

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temperate seasonal forests

A biome with warmer summers and colder winters than temperate rainforests and dominated by deciduous trees.

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tropical rainforests characteristics.

Near the equator. Warm with lots of precipitation. Little seasonal temperature variation. Most diverse biome.

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shrubland

Arid terrestrial biome characterized by shrubs and tending to occur along coasts that have dry summers and receive most of their rainfall in the winter.

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temperate grassland

biome characterized by deep, nutrient-rich soil that supports many grass species

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savanna

An area of grassland with scattered trees and bushes

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desert

An extremely dry area with little water and few plants

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tundra

An extremely cold, dry biome.

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primary productivity

the rate that solar energy is converted into organic compounds via photosynthesis over a unit of time

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respiration loss

plants use up some of the energy they generate via photosynthesis by doing cellular respiration

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gross primary productivity

The total amount of solar energy that producers in an ecosystem capture and convert to energy via photosynthesis

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net primary productivity

the amount of energy (biomass) left over for consumers after plants have used some for respiration

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ecological efficency

the proportion of incoming solar energy that is captured by plants and converted into biomass

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higher primary productivity =

more diversity

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NPP =

GPP-RL