lecture 4 Flashcards
(22 cards)
Environmental Heterogeneity
• Climate is the part of the physical (abiotic) environment that has the greatest impact on an organism
– Weather
combination of temperature, humidity, precipitation, wind, cloudiness at a specific place and time
Climate
long-term average pattern of weather
Earth’s atmosphere intercepts solar radiation
– Earth’s rotation and movement generate prevailing winds and ocean currents • Together these generate global weather patterns
– Results in environmental heterogeneity (=variability in abiotic factors across space)
• Weather patterns differ at different spatial scales:
– Global → Regional → Local → Micro
Global and regional climate patterns determine the l
the large-scale distribution of plants and animals
Microclimate
– Local climatic conditions do not match the general climate profiles of the larger region
• Because local patterns of microclimate are the actual environmental conditions experienced by organisms → our focus
Aquatic Environment
Dominant environment on Earth
~ 75 % of the planet’s surface is water
• •
•
Low degree of microclimate variability in time and space
Divided by salinity: saltwater and freshwater
Divided by depth
– Solar radiation is:
• Reflected back into atmosphere
• Absorbed or reflected by suspended particles (alive & dead)
• Absorbed by water
Solar radiation declines exponentially with depth
→ Distinct vertical profiles of light, temperature, oxygen, pressure, etc.
Aquatic Environment - Light
• •
Direct impact: plants
– Plants require sunlight for photosynthesis
– Plants are restricted to top 100 m
Indirect impact: animals
– Herbivores are restricted to depths where plants reside
– Animals inhabiting deep water (> 200 m) have adaptations:
• Lack pigment
• Large eyes (maximum light-gathering ability)
• Organs that produce light (bioluminescence)
– Thermocline
region with most rapid decline in temperature
• After temperature continues to decline with depth but at a slower rate
Aquatic Environment - Temperature
•
Exponential decline in solar radiation with depth → decline in temperature with
depth
– Thermocline
– Some form of thermal stratification occurs in all open bodies of water
– Mixing of the water column can break down this gradient (e.g. winds, currents,
seasonal)
– as water cools, it becomes more dense until 4oC (max density) → 4- 0 oC is less
dense
Aquatic Environment - Oxygen
• Oxygen diffuses from the atmosphere into aquatic environments • Oxygen produced by plants during photosynthesis
– Restricts high concentrations of oxygen to surface waters
– Limits respiration and metabolic activity of animals
– Mixing of the water column can break down this gradient
Terrestrial Environment
• Higher degree of microclimate variability in time and space
• Greatest constraint is desiccation (drying out) ~ living cells contain 75 - 95 % water
• Soil is the foundation upon which all terrestrial life depends
• Medium for plant growth
→ provides vertical structure for animal life
• Controls the fate of water in terrestrial environments
• Provides habitat for decomposers (Nature’s recycling system)
Terrestrial Environment
• Moisture-holding capacity of the soil is critical for availability of:
– water
– chemical elements dissolved in soil water
What causes variation in the moisture-holding capacity?
- Climate
- Type of parent material
- Topography
- Aspect
- Presence/absence & type of vegetatio n
Vegetation
- habitat for animals
Eg. Different bird species depend on vegetation of different heights
- Climate
directly influences the physical & chemical reactions in the soil & water availability
- Type of parent material
- material from which soil develops
• Physical and chemical characteristics determine properties of soil
- Topography
eg. Slope, level ground
- Aspect
north vs south-facing sites
• Differ in their exposure to solar radiation
- Presence/absence & type of vegetatio n
– Vegetation alters microclimates: • Light (via shading) • Temperature (via shading) • Moisture (via use) • Wind movement • Structure – habitat for animals
vegetation
provides high diversity of microclimates for terrestrial environments