Chapter 3 Vocabulary (Carinita)

ecology

the study of how organisms interact with one another and with their nonliving environment; study of connections in nature

organism

any form of life; the most fundamental unit of ecology

species

groups of organisms that resemble one another in appearance, behavior, chemistry, and genetic makeup

population

a group of interacting individuals of the same species occupying a specific area

genetic diversity

in most natural populations, individuals vary slightly in their genetic makeup, which is why they do not all look or act alike

habitat

the place where a population or individual organism normally lives is its habitat

distribution; range

the area over which we can find a species

community; biological community

consists of all the populations of different species that live and interact in a particular area

ecosystem

a community where populations of different species interact with one another and with their nonliving environment of matter and energy

biosphere

the global ecosystem where all life is interconnected; living and dead organisms

atmosphere

a thin envelope or membrane of air around the planet

troposphere

the inner layer of the atmosphere; contains the majority of the planet's air, mostly nitrogen and oxygen

stratosphere

the layer above the troposphere; contains enough ozone to filter out most of the sun's harmful UV radiation, which allows life to exist on land and in the surface layers of bodies of water

hydrosphere

consists of the earth's water; found as liquid water, ice, and water vapor

lithosphere

the earth's crust and upper mantle; contains nonrenewable fossil fuels and minerals we use as well as nutrients needed for plant life

biomes

terrestrial regions inhabited by certain types of life, especially vegetation; examples include various types of deserts, grasslands, and forests

aquatic life zones

marine and freshwater portions of the biosphere; examples include lakes, streams, estuaries, coastlines, coral reefs, and the deep ocean

abiotic

nonliving components of the ecosystem such as water, air, nutrients, and solar energy

biotic

biological components of the ecosystem such as producers, consumers, and decomposers

range of tolerance

range of chemical and physical conditions that must be maintained for populations of a particular species to stay alive and grow, develop, and function normally

limiting factor principle

too much or too little of any abiotic factor can limit or prevent growth of a population, even if all other factors are at or near the optimum range of tolerance

producers; autotrophs

organisms that make their own food from compounds and energy obtained from their environment

photosynthesis

complex plants that takes place in cells of green plants; radiant energy form the sun is used to combine carbon dioxide and water to produce oxygen, carbohydrates, and other nutrient molecules

consumers; heterotrophs

organisms that get energy and nutrients they need by feeding on other organisms and their remains

primary consumers; herbivores

eat producers

secondary consumers; carnivores

feed on herbivores

third and higher level consumers

carnivores that feed on other carnivores

omnivores

feed on both plants and animals

decomposers

specialized organisms that recycle nutrients in ecosystems; secrete enzymes that digest or biodegrade living or dead organisms into simpler inorganic compounds that producers can take up from the soil and water and use as nutrients

detritivores

insects and other scavengers that feed on the wastes or dead bodies of other organisms

aerobic respiration

complex process that occurs in the cells of most living organisms, in which nutrient organic molecules such as glucose combine with oxygen to produce carbon dioxide, water, and energy

chemosynthesis

process in which certain organisms extract inorganic compounds from their environment and convert them into organic nutrient compounds without the presence of sunlight

anaerobic respiration; fermentation

form of cellular respiration in which some decomposers get the energy they need thorough the breakdown of glucose in the absence of oxygen

biological diversity; biodiversity

one of the earth's most important renewable resources; includes functional, ecological, genetic, and species diversity

HIPPO

acronym about five major causes of species decline and premature extinction; habitat destruction, invasive species, pollution, population growth, overexploitation

food chain

a sequence of organisms, each of which is a source of food for the next

trophic level

feeding level depending on whether an organism is a producer or a consumer and on what it eats or decomposes

food web

a complex network of interconnected food chains

biomass

dry weight of all organic matter contained in organisms

ecological efficiency

the percentage of usable energy transferred as biomass form one trophic level to the next

pyramid of energy flow

diagram representing the flow of energy through each trophic level in a food chain or food web; with each energy transfer, only a small part (usually 10%) of the usable energy entering one trophic level is transferred to the organisms at the next trophic

gross primary productivity (GPP)

the rate at which an ecosystem's producers convert solar energy into chemical energy a biomass

net primary productivity (NPP)

rate at which producers use photosynthesis to store energy minus the rate at which they sue some of this stored energy through aerobic respiration; amount of energy producers make

soil

thin covering over most land that is a complex mixture of eroded rock, mineral nutrients, decaying organic matter, water, air, and billions of living organisms, most of them microscopic decomposers

weathering

soil formation begins when bedrock is broken down into rock fragments and particles by physical, chemical, and biological processes

soil horizons

mature soils are arranged in a series of horizontal layers each with a distinct texture and composition that varies with different types of soils

soil profile

a cross-sectional view of the horizons in a soil

humus

partially decomposed bodies of dead plants and animals

infiltration

downward movement of water through soil

leaching

as water seeps down, it dissolves various minerals and organic matter in upper layers and carries them to lower levels

soil texture

determined by the relative amounts of the different sizes and types of mineral particles

nutrients

elements and compounds that organisms need to live, grow, and reproduce

biogeochemical cycles; nutrient cycles

nutrients move through air, water, soil, rock, and living organisms in cycles

hydrologic cycle; water cycle

collects, purifies, distributes, and recycles the earth's fixed supply of water

carbon cycle

carbon, the basic building block of the carbohydrates, fats, proteins, DNA, and other organic compounds necessary for life, circulates through the biosphere

nitrogen cycle

cyclic movement of nitrogen in different chemical forms from the environment to organisms and then back to the environment

sulfur cycle

cyclic movement of sulfur in different chemical forms from the environment to organisms and then back to the environment

clay

smallest particle of soil

silt

medium size particles of soil

sand

large size particles of soil

layers in soil

surface litter layer --> topsoil layer --> subsoil --> parent material (bedrock)

mature soils

soils that have developed over a long time

denitrification

nitrogen leaves the soil as specialized bacteria convert ammonia and ammonium back into nitrite and nitrate ions, and then into nitrogen gas (N2) and nitrous oxide gas (N2O)

crust

soil and rock

litosphere

crust; top of upper mantle

phytoplankton

dominant producers in water; mostly microscopic organisms that float or drift in the the water

substrate

the right surface; a limiting factor

salinity

amounts of various inorganic minerals or salts dissolved in a given volume of water

phosphorus

limiting factor of marine life

nitrogen

limiting factor of terrestrial life

optimum level or range

best level of a limiting factor at which populations are the greatest

microbe

greatest biomass