PHYSICAL ENVIRONMENT ECOL 1
Common definitions
Plant:
Autotrophic
Eukaryotic
Multicellular
Generally adapted to a terrestrial existence
Have a cell wall
Take in carbon dioxide
Autotroph: an organism that makes its own food from inorganic molecules
From the greek auto meaning self and trophe meaning nourishing
Animal:
Heterotrophic
Eukaryotic
Multicellular
Take in oxygen with few exceptions
Theory: an explanation of a natural phenomenon supported by many observations
Same results occur over and over using scientific method
Example: gravity is a theory
Physical environment
Water makes all life possible
Fresh water is vital to life but also a finite resource
Most of earth's surface is water (71%)
97% is saline
3% is freshwater mostly in ice snow or groundwater
0.9% of freshwater is from lakes and rivers
Properties of water
Polarity
In a water molecule hydrogen and oxygen have an unequal sharing of electrons
Hydrogen is partially positive, oxygen is partially negative, bent molecular shape at poles
Partial charge attracts other polar molecules, often dissolving them
Universal solvent
Water dissolves more substances than any other liquid
Cohesion
Sticks to itself
Creates surface tension
Adhesive
Sticks to other things
Helps draw water up the plant (i.e., capillary action)
Properties of water in plants
Water absorbed by roots and root hairs
Water molecules pull each other up against gravity (cohesion + adhesion + water potential)
Water molecules exposed to air and evaporation through pores (stomata) in leaf (process is transpiration)
Water and nutrients passively absorbed through roots
Water moves up stem in xylem tissue system and adhesion + cohesion “stickiness”
Water evaporates through stomata
Transportation of water through tall trees
Through fog
Epiphyte: plant or plant-like organism that grows on another plant, but is not parasitic
Nutrients = essential compounds
availability varies by biome
Bedrock: underlying geology (i.e., limestone has different minerals than granite)
Water: movement of nutrients and weathering of rock
Soil type: different types/sizes of soil retain nutrients better
3 classes
Clay, silt, sand
Properties of sand
Largest particle size
Greatest “room in between particles (pore size)
Warm up faster since more air can circulate
Different biomes
Desert soils are mostly sandy
Little precipitation
little/no weathering processes
Release of nutrients from bedrock very slow
Low amounts of organic material
Very nutrient poor
Tropical
Soils are variable (clay loam and sand)
Abundant precipitation
Fast weathering process
High organic materia, quickly reused
Pacific soils do not trap nutrients
Very nutrient poor
Adaptation to nutrient availability
Plants
Succulent, waxy leaves
Root allocation
Spines and hairs
Carnivory
Animals
Structural adaptation (seabirds secrete excess nutrients through nasal cavity
Resource adaptation (adapting to foods where there is less competition)
Metabolic adaptations (freshwater fish produce lots of dilute urine, marine produce little urine that is concentrated
Light and energy
Happens above ground
All living things need energy
Carbon dioxide + water + light energy = glucose + oxygen
CO2 + H2O + sunlight = C6H12O2
Simplified photosynthesis definition:
Conversion of inorganic carbon dioxide into organic compounds using water and light energy
Light is energy
Pigments that absorb energy
Chlorophyll a
Chlorophyll b
Carotenoids
Action spectrum (most effective)
Wavelengths outside of the action spectrum reflect (absorb red and blue, reflects green) (why plants are green)