ECOLOGY: The Study of Ecosystems
Ecology (from the Greek oikos meaning "house" or "dwelling", and logos meaning
"discourse") is the study of the interactions of organisms with each other and
their environment.
The hierarchy. Define each of the following.
- species -
- population -
- community -
- ecosystem -
- biosphere -
Ecology is a SCIENCE, not a sociopolitical movement (e.g., environmentalism).
The Ecologist engages in the hypothetico-deductive method to pose questions
and devise testable hypotheses about ecosystems. Often, this involves the
generation of complex mathematical models to simulate ecosystems. These
models represent idealized systems to which real systems can be compared
for their predictive value. Sometimes, when a very large scale project is
logistically impossible to perform, a computer model is used to predict
expected results.
An ecosystem consists of
- biotic components - the living organisms
- abiotic components - non-living factors, such as light,
temperature, water, nutrients, topography, etc.
Evolution by natural selection is driven by ecological interactions.
Levels of Ecological Study
- ORGANISMAL ECOLOGY - the study of individual organisms' behavior,
physiology, morphology, etc. in response to environmental challenges.
- POPULATION ECOLOGY - the study of factors that affect and change the
size and genetic composition of populations of organisms.
- COMMUNITY ECOLOGY - the study of how community structure and
organization are changed by interactions among living organisms
- ECOSYSTEM ECOLOGY - the study of entire ecosystems, including the
responses and changes in the community in response to the abiotic components
of the ecosystem. This field is concerned with such large-scale topics as
energy and nutrient cycling.
COMPONENTS OF THE BIOSPHERE
The plant community of a particular region depends on the CLIMATE--the
combination of temperature, water, light, and wind. And the flora directly
affects the composition of the fauna.
ABIOTIC COMPONENTS OF ECOSYSTEMS
Temperature
- different organisms have different cellular tolerances for cold and
heat
- organism classification based on temperature source and
regulation:
- ectotherm - obtains heat primarily from the environment
- endotherm - obtains heat primarily from metabolic reactions
- poikilotherm - temperature regulated primarily by environment
- homeotherm - temperature regulated primarily by internal
homeostatic mechanisms
- contributes to erosion & creation of soil
Water
- challenge of water balance in terrestrial and freshwater
environments
- animals that have secondarily returned to marine environments face
osmotic challenges, as the ocean is now saltier than when their
ancestors left it.
- important component in erosion & creation of soils
Sunlight
- intensity
- daily duration
- angle of incidence of the sun (seasonal changes)
- competition for light is an important selective factor in many
environments, and this has driven selection of many species
- photosynthesis wavelengths primarily in the blue & red regions of
spectrum; understory and underwater regions have varying levels of these
wavelengths, with red light being lost first, and blue light last.
- photoperiodicity can be diurnal, seasonal, etc. (Circadian rhythms)
Wind
- contributes to erosion
- affects perceived temperature via evaporation & convection
- affects desiccation rate
- affects growth form of plants
Rocks/Soil
- topography creates habitat
- mineral (inorganic nutrient) content of rock affects flora
- pH of rock/soil affects flora
- substrate composition affects any water in contact with that
substrate
- Here's a nice overview of how SOIL comes to be...
Major Environmental Disturbances
- fire
- severe storms (hurricanes, tornadoes, etc.)
- volcanic activity
- oh, heck. Comets, too.
In short, all of which contribute to CLIMATE.
GLOBAL PATTERNS OF CLIMATE
The ultimate source of climate is the sun, which provides not only the
majority of energy on earth, but also creates climatic events when its
randomizing energy interacts with the earth.
Less than half of the solar radiation striking the earth's atmosphere
successfully penetrates the atmosphere to reach earth.
Terrestrial
irradiance (i.e., solar radiation incident on the earth's surface) ranges
from approximately 250nm (ultraviolet) to 1500nm (near infrared). Shorter
and longer wavelengths are absorbed or reflected by atmospheric ozone,
water vapor.
When the sun is directly overhead in a cloudless sky, irradiance is
most intense and peaks near 540nm ("green").
Environmental conditions and angle of incidence
affect both intensity and spectral distribution of incident sunlight.

- the TROPICS lie between the Tropic of Cancer (23.5o
N) and the Tropic of Capricorn (23.5o
S). These receive the highest annual input of solar energy, and are
the only place on earth that the sun ever shines directly overhead (on
the equinoxes, March 21 and September 21).
- the SUBTROPICS lie between the Tropic of Cancer and
30oN in the northern hemisphere, and between the
Tropic of Capricorn and
30oS in the southern hemisphere. (Miami is in the
subtropics)
- the TEMPERATE regions lie between 30oN and
60oN in the Northern Hemisphere and between 30oS and
60oS in the Southern Hemisphere.
- the POLAR REGIONS lie above 60oN and S
Flora and fauna are profoundly affected by environmental and seasonal changes in solar
intensity and spectral distribution. Note also that because the sun is
tilted 23.5o on its axis (defining those tropical latitudes),
there are seasonal changes solar irradiation in both hemispheres:

Solar warming of earth creates
global air and water vapor movement


- Warm, high levels of precipitation: Tropics
- Relatively warm, arid: subtropics and temperate regions
- Cool, high levels of precipitation: just below polar area;
coniferous forests dominate
- Cold, arid: polar regions (Arctic and Antarctic)
Climate can be affected locally by
proximity to ocean, lakes, rivers
topography
This creates smaller, localized ecosystems within large, ecologically distinct areas known as biomes.
Climate is the primary factor that determines what organisms can live in
any given habitat. Therefore, climate is what causes certain areas of the
earth to become distinctive BIOMES.