CHAPTER 23 ECOSYSTEMS AND BIOMES
SECTION 1 Energy flow in the ecosystem
3 types of energy Roles
1. Producer
- and organism able to capture the energy of sunlight and store it as food
energy
and organism that can make its own
food
2. Consumer
- and organism that obtains energy buy feeding on other organisms
primary consumers
are heterotrophs
heterotroph - can not make their own food the depend on producers for
food and energy
herbivore -in Latin "herba" means herb or
plant "vorare" means eat these are plant
eaters
secondary consumers eat the heterotrophs
tertiary consumers can eat the heterotrophs and secondary
consumers
carnivores - in Latin "carnis" means flesh these
are consumers that only eats animals
omnivores - in Latin "omni" means all these
are consumers that eats plants and animals
scavenger - a carnivore that feed on the bodies of dead organisms
3. Decomposers
- organisms that break down wastes and dead organism and return the raw material
to the environment
they return simple molecules to the
environment. fungi and bacteria mostly
when an organism eats it obtains energy
FOOD CHAIN - is a series of events in which one organism
eats another and obtains energy
grass ---------------> mouse --------------------> hawk
producer ----> first level consumer -------> second
level consumer
shows the possible path along which energy can move through an ecosystem
FOOD WEB - consists of many overlapping food chain in an ecosystem.
/
a more realistic way to show the flow of energy through an ecosystem
ENERGY PYRAMIDS - A diagram that shows the amount of energy that
moves from one feeding level to another in a food web.
.
- Most energy is available at the producer level
- At each level in the pyramid there is less available energy
than at the level below
- only about 10% of energy at one level of the food web is transferred
to the next higher level
- 90% of the energy is used for the organism's life
processes or is lost as heat to the environment
- not enough energy to support many feeding levels
- energy is lost at each level so it limits the number of
consumers the ecosystem can support
SECTION 2 CYCLES OF MATTER
ENERGY IS NOT RECYCLED ecosystem must be constantly supplied
with energy usually from sunlight
MATTER CYCLES THROUGH AN ECOSYSTEM OVER AND OVER samples of cycles
1. water 2. oxygen 3. carbon 4. nitrogen 5. other substances
matter is made of atoms
atoms make up molecules
water cycle -
the process of evaporation, condensation and precipitation
evaporation - the process by which molecules of liquid water
absorb energy and change to the gas state
condensation - the process by which a gas changes to a liquid
precipitation - as more water vapor condenses
carbon oxygen cycle
- In this process the plants (producers) use carbon from the carbon dioxide to
produce (food) other carbon-containing molecules.
- oxygen is also release as a result of photosynthesis
-other organism take in oxygen from the atmosphere and use it in their life
processes and they intern give off carbon dioxide the producers use

NITROGEN CYCLE - nitrogen
moves form the air to the soil, into living things, and back into the air.
air is 78% nitrogen
most organisms can't use the nitrogen
gas in the air
NITROGEN GAS - is call "free
nitrogen" it is not combined with other kinds of atoms
FIXED NITROGEN - has been
combined with other kinds of atoms
most organisms can only use this form of nitrogen

NITROGEN FIXATION - the process of changing
free nitrogen gas into a usable form of nitrogen
NODULES
- bacteria live in bumps of roots of legumes (plants) like beans, peas
alfalfa, peanuts beans
Mutualism - both species benefit
example:
bacteria feed on the plant's sugar and the plant is supplied with nitrogen in a
usable form
crop rotation - farmers will plant different crops
every year.
example - soy beans one year to
add nitrogen to the soil so they don't have to fertilize so much on next years
corn crop
BACK TO NITROGEN GAS
fixed nitrogen can be used by organism to build protein
.
Decomposers break down proteins in wastes and dead organism
nitrogen returns to soil
bacteria eventually break down nitrogen completely and
it goes back to the air
SECTION 3 BIOGEOGRAPHY
BIOGEOGRAPHY - the study of where organisms live
bio - means life
geo - means Earth
graph - means description
CONTINENTAL DRIFT - the very slow motion of the continents
Pangaea - the continents of
earth were connected
DISPERSAL - the movement of organism from one place to another
can be caused by wind, water, or living things, including
humans
native species - species that have naturally evolved in an
area
exotic species - organism that is carried into a new location by
people
LIMITS TO DISPERSAL - three factors that limit dispersal of a
species are physical barriers, competition and climate
physical barriers - mountains, water, deserts hard to cross
competition - competition for resources with the species already
there organism must find a unique niche to survive.
climate - the typical weather pattern in a area over a long period
of time
SECTION
4 EARTH'S BIOMES
http://www.blueplanetbiomes.org/world_biomes.htm
BIOME - is a group of ecosystems with similar climates and organisms
helps ecologist describe the world
generally
scientist focus on 6 major land biomes and 2 major water biomes
climate conditions - temperature
and rainfall determine the biome in an area
climate limits the distribution of plants
plants determine the kinds of animal that live there
1. rainforest 2.desert 3.
grassland 4. deciduous forest 5. boreal
forest (TAIGA) (coniferous) 6.tundra 7.mountains and ice (don't fall into any category)
1.
freshwater 2. Marine
1. rainforest - greatest diversity of species. > ½ of tropical forests have
been destroyed, near the equator, latitudes 23.5 degrees N and 23.5 degrees S.
winter is
absent, and only two seasons are present (rainy and dry).
The length of daylight
is 12 hours and varies little.
Temperature is on average 20-25° C and varies:
by no more than 5 degrees.
Precipitation is evenly distributed annual rainfall exceeding 2000 mm.
Soil is nutrient-poor, acidic. Decomposition
is rapid soils have heavy leaching.
Canopy tall leafy roof is multi-layered, continuous, allowing little light penetration.
understory - second layer of shorter trees and
vines grow well in shade
some plants thrive in near-darkness of the forest floor
Flora is highly diver1 square kilo as many as 100 different tree species.
Trees are 25-35 m tall,
shallow roots, mostly evergreen. orchids, vines, ferns,
Fauna include numerous birds, bats, small
mammals, and insects.

2.desert
Temperatures - annual temp
range 20-25° C. max ranges from 43.5-49° C. Minimum
temperatures sometimes drop to -18° C.
Precipitation - 1.5 cm. < 28 cm
a year. Evap. rates can exceed rainfall rates
Soil - course, shallow, rocky, sand particles with good drainage, no subsurface water.
are coarse cause there's less chemical weathering.
Canopy - Canopy in most deserts is very
rare
Flora - small, thick and covered with a
thick cuticle (outer layer). cacti, the leaves are spines and photosynthesis in the stems. yuccas,
prickly pears,
false mesquite,
Fauna - small nocturnal (active at
night) carnivores. burrowers and kangaroo rats.
insects, arachnids, reptiles and birds. The animals stay inactive in protected
hideaways during the hot day and come out to forage at dusk, dawn or at night,
when the desert is cooler
3.
grassland - (determined
by temperature, rainfall, and soil conditions). seasonal drought,
fires, and grazing by large mammals all prevent woody shrubs and trees from
invading and becoming established.
PRAIRIE
Temperatures - Summer temperatures can be well over 38°
C (100 degrees Fahrenheit), while winter temperatures can be as low as -40° C
(-40 degrees Fahrenheit
Precipitation most in the late spring
& early summer. annual ave ~ 50.8 to 88.9 cm (20-35 inches)
Soil- very rich
Flora grasses include purple needlegrass, blue
grama, buffalo grass, Flowers include asters, blazing stars,
coneflowers, goldenrods, sunflowers, clovers
Fauna - wolves, prairie dogs, jack
rabbits, deer, mice, coyotes, foxes, skunks, badgers, blackbirds, grouses,
meadowlarks, quails, sparrows, hawks, owls, snakes, grasshoppers, leafhoppers,
and spiders.
SAVANNA - cover almost half of Africa large areas of
Australia, South America, and India.
Climate is warm or hot climates
annual rainfall is from about 50.8 to 127 cm (20-50 inches) per year. rainfall
is concentrated in six or eight months of the year, followed by a long period of
drought when fires can occur
STEEPES are dry areas of grassland hot summers and cold
winters.
receive 25.4-50.8 cm (10-20 inches) of rainfall a year. Steppes
occur in the interiors of North America and Europe. graze livestock, grow wheat
and other crops. Overgrazing, plowing, and excess salts left behind by
irrigation waters have harmed some steppes. Strong winds blow loose soil from
the ground after plowing, especially during droughts. causes the dust
storms of the Great Plains of the U.S.
4. deciduous forest
- Temperate forests occur in eastern North America, northeastern Asia, and
western and central Europe. Well-defined seasons with a distinct winter.
Moderate climate and a growing season of 140-200 days during 4-6 frost-free
months.
Temperature varies from -30° C to 30° C.
Precipitation (75-150 cm) is distributed evenly throughout the year.
Soil is fertile, enriched with decaying litter.
Canopy is moderately dense and allows light to penetrate, diversified
understory of vegetation and animals.
Flora is characterized by 3-4 tree species per square kilometer. Trees
have broad leaves that are lost annually include oak, hickory,
maple, basswood, cottonwood, elm, willow, and spring-flowering herbs.
Fauna squirrels, rabbits, skunks, birds, deer, mountain lion,
bobcat, timber wolf, fox, and black bear.

5. boreal
forest (coniferous) - Boreal forests, or taiga, the largest
terrestrial biome.
between 50 and 60 degrees north latitudes, two-thirds in Siberia
with the rest in Scandinavia, Alaska, and Canada. Seasons are divided into
short, moist, and moderately warm summers and long, cold, and dry winters. The
length of the growing season in boreal forests is 130 days.
Temperatures are very low.
Precipitation is primarily in the form of snow,
40-100 cm annually.
Soil is thin, nutrient-poor, and acidic.
Canopy permits low light penetration,
understory is limited.
Flora - cold-tolerant evergreen
conifers needle-like leaves, pine, fir, and spruce. needles have a
waxy coat to prevent evaporation
Fauna include woodpeckers, hawks, moose, bear,
weasel, lynx, fox, wolf, deer, hares, chipmunks, shrews, and bats.

6.tundra - Extremely cold, dry climate, Low biotic diversity, Simple plants, swampy, Short
growing and reproduction seasons, Energy and
nutrients in the form of dead organic material, Large population changes
Temperatures cold, desert-like conditions. The
growing season ranges from 50 to 60 days. The average winter temperature is
-34° C (-30° F), but the average summer temperature is 3-12° C (37-54° F
Precipitation Rainfall may vary in different
regions of the arctic. Yearly precipitation, including melting snow, is 15 to 25
cm (6 to 10 inches
Soil - formed slowly. A layer of permanently
frozen subsoil called permafrost exists, consisting mostly of gravel and
finer material. When water saturates the upper surface, bogs and ponds may form,
providing moisture for plants
Flora - low shrubs, sedges, reindeer mosses,
liverworts, grasses, 400 varieties of flowers, and lichen no deep
root systems in the vegetation of the arctic tundra, about 1,700 kinds of
plants
Fauna - lemmings, voles, caribou, arctic
hares and squirrels, arctic foxes, wolves, and polar bears, Migratory birds:
ravens, snow buntings, falcons, loons, ravens, sandpipers, terns, snow birds,
and various species of gulls, mosquitoes, flies, moths, grasshoppers,
blackflies and arctic bumble bees
7.mountains and ice ( don't fall into any category) conditions change from the base to its summit
1.
freshwater - has a low salt concentration—usually
less than 1%. ponds and lakes, streams and
rivers, and wetlands. Ponds and Lakes - may have limited species
diversity since they are often isolated Lakes and ponds three
different “zones” determined by depth and distance from the shoreline.
littoral zone. top zone, warmest, shallow and can absorb more
of the Sun’s heat. many algae (like diatoms), rooted and floating
plants, snails, clams, insects, fishes, crustaceans, and amphibians,
dragonflies, midges, the egg and larvae stages are found here. turtles, snakes,
and ducks.
limnetic zone - near-surface open water well-lighted
dominated by phytoplankton and zooplankton. fish also occupy this zone.
Temperature varies in ponds and lakes seasonally. During the summer, the
temperature can range from 4° C near the bottom to 22° C at the top. During
the winter, the temperature at the bottom can be 4° C while the top is 0° C
(ice).
Streams and Rivers - flowing water moving in one direction.
headwaters is were they start
by springs, snowmelt or lakes,
mouths where they end, temperature
is cooler, clearer,
has higher oxygen levels, and freshwater fish such as trout and heterotrophs
middle part of stream/river, the width
increases, species diversity—numerous aquatic green plants and algae
can be found.
mouth water gets murky
from sediments picked up, decreasing light penetration through the water.
less light, less diversity of flora, and because of the lower oxygen levels, fish
that require less oxygen live here catfish and carp
2. Marine -
cover ~ 3/4 Earth’s surface (oceans, coral reefs, & estuaries).
algae supply much of the world’s oxygen supply and take in a huge
amount of carbon dioxide. evaporation of seawater provides rainwater for the
land.
Oceans -largest ecosystems, separated
into zones: intertidal, pelagic, abyssal, and benthic. have a great
diversity of species.
intertidal zone
is submerged and exposed, by waves and tides.
the communities are
constantly changing. upper area has algae and small animals, such as herbivorous
snails, crabs, sea stars, and small fishes.
the bottom is exposed
during the lowest tides, many invertebrates, fishes, and seaweed. on sandier
shores is not as stratified as in the rocky areas.
Waves keep mud and sand
constantly moving, thus very few algae and plants can establish themselves—the
fauna include worms, clams, predatory crustaceans, crabs, and shorebirds.
(surface)
pelagic zone open ocean.
generally cold there is thermal stratification with a constant mixing of
warm and cold ocean currents.
The flora in the pelagic zone include surface
seaweeds.
The fauna include many species of fish and some mammals, such as
whales and dolphins. Many feed on the plankton.
Neritic zone -
extends over the continental shelf (benthic zone) below the pelagic zone,
The bottom
of the zone consists of sand, slit, and/or dead organisms.
temperature
decreases as depth increases
since light cannot
penetrate through the deeper water.
Flora represented seaweed
fauna - very nutrient-rich,
bacteria,
fungi, sponges, sea anemones, worms, sea stars, and fishes.
abyssal zone deep ocean. very cold (around 3°
C), highly pressured, high in oxygen content, but low in nutritional
content. supports many species of invertebrates and fishes.
hydrothermal vents,
are found along the ocean floors. Chemosynthetic bacteria
thrive near these vents because of the large amounts of hydrogen sulfide and
other minerals they emit. bacteria start a food web
Coral Reefs - in warm shallow waters. as barriers along
continents Great Barrier Reef , fringing islands, and atolls. dominant
organisms in are corals. fauna include microorganisms,
invertebrates, fishes, sea urchins, octopuses, and sea stars.
SECTION 5
SUCCESSION
SUCCESSION - series of predictable
changes that occur in a community over time
PRIMARY SUCCESSION - a series of changes that occur
in an area where no ecosystem previously existed
area of rock,
volcanic area
PIONEER SPECIES - first species to
populate an area
can grow on bare rocks with little or no soil
help make
soil
lichen and mosses
provide nutrient that enrich the thin layer of soil
SECONDARY SUCCESSION - a series of changes that occur after
a disturbance in an existing ecosystem (fire, logging, tornadoes, farming
etc)
occurs in a place where an ecosystem
has previously existed
occurs more rapidly than primary
succession