Coping with Environmental Variation
Learning goals:
* understand how stress influences organismal function and distribution
* know the difference between acclimitization and adaptation
Each species has a range of environmental tolerances that determines
its potential geographic distribution; i.e. the geographic ranges of
species are related to constraints imposed by the environment
Some physical environmental limitations are obvious: e.g. freezing
temperatures, very low water availability; others are more subtle: e.g.
soil and water chemistry
The physical environment influences an organism’s success in two
main
ways:
1) Affects ability to obtain energy and resources, maintain metabolic
functions, grow and reproduce
2) Extreme environmental conditions affect survival
A species’ abundance varies across environmental gradients,
reflecting
its tolerances to the environment. Actual distribution reflects
additional constraints due to biotic interactions (e.g. competition,
predation).
A species’ climate envelope is the range of condition over which
it
occurs- useful tool for predicting responses to climate change
Physiological processes (e.g. photosynthesis, metabolic respiration)
have a set of optimal conditions for functioning. Deviations from
the optimum reduce the rate of the process.
Stress—a
decrease in
the rate of important physiological processes due to
environmental change, lowering the potential for survival, growth, or
reproduction.
Many organisms can adjust to stress through behavior or
physiology—called acclimatization;
usually a short-term, reversible process
Over multiple generations of an organism, natural selection can result
in adaptation to
environmental stress, which is a unique, genetically-based solution to
the stress
Individuals with traits that make them best able to cope with stress
are favored, increasing the frequency of the unique adaptations in the
population
Both adaptation and acclimatization enhance survival and reproductive
success, but adaptation is a long-term, genetic response of a
population to environmental stress; acclimatization can be an adaptation
Populations with unique adaptations are called ecotypes
Acclimatization and Adaptation are not “free;” they
involve
tradeoffs with other functions, and require investment of energy and
resources that could be used for other functions such as reproduction
Coping with variation in
temperature
Learning goals
* know what impact temperature extremes can have on organisms
* understand the exchanges in energy that influence the temperature of
an organism (primarily plants and animals)
* learn some of the ways plants and animals can alter the exchange of
energy to warm or cool themselves
Fluctuations in temperature varies considerably among different
environments- e.g. seasonal temperature swing in a boreal forest
can exceed 80 ºC (144 ºF); tropical rain forest 15º C
(22 ºF), and tropical oceans as little as 3 ºC (5 ºF)
Life is usually restricted to organismal temperatures between 0 and 50
ºC, but has been recorded in organisms at -5 and 90 ºC.
Some organisms can survive periods of extreme heat or cold by entering
a state of dormancy, in which little or no metabolic activity occurs
Temperature controls physiological activity through its effects on
chemical reactions, especially enzyme function
Enzymes are proteins that enhance biological reactions
* structure degrades (denature) at high temperature
* their activity decreases at low temperature
Temperature also affects the properties of cell and organelle
membranes; composed of two layers of lipid molecules. At low
temperatures, the lipids solidify, embedded proteins can’t
function, and the cells leak metabolites
The temperature of organisms is determined by exchanges of energy with
the external environment; The balance between inputs and outputs
of energy determines whether the temperature of any object will
increase or decrease.
Organisms can adjust their exchange of energy with the environment
through behavioral, morphological, and physiological modifications to
avoid adverse temperatures
Energy exchange with the environment can be by:
Conduction—transfer of energy from warmer to cooler molecules.
Convection—heat energy is carried by moving water or air.
Latent heat transfer - water absorbs heat as it changes state from
liquid to gas
Energy gains and losses for plant leaves
Temperature change in a plant can be expressed as:
∆ (change in) Hplant= SR + IRin- IRout
+/- Hconv +/- Hcond – Het
(eq. 4.1)
where:
SR = Solar radiation
IR = Infrared radiation
Hconv = Convective heat transfer
Hcond = Conductive heat transfer
Het = Heat transfer by evapotranspiration
Plants adjustment of energy exchange
1) Transpiration (Het)- rate controlled by specialized guard
cells surrounding stomate;
2) changing albedo- reflection of solar radiation, by producing hairs
on the leaf surface
3) altering convective heat loss- altering boundary layer (zone next
to an object where the velocity decreases in response to frictional
drag and turbulence)
depth of the boundary layer is dependent on wind speed and leaf
dimensions: small leaves have a smaller boundary layer than large
leaves- lose