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Chapter 50. An Introduction to Ecology & the Biosphere. Overview: The Scope of Ecology. Ecology- study of interactions b/w organisms & environ These interactions determine distribution of organisms & their abundance Ecology reveals the richness of the biosphere.
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Chapter 50 An Introduction to Ecology & the Biosphere
Overview: The Scope of Ecology • Ecology- study of interactions b/w organisms & environ • These interactions determine distribution of organisms & their abundance • Ecology reveals the richness of the biosphere
Concept 50.1: Ecology is the study of interactions b/w organisms & the environment • Ecology has a long history as a descriptive science • It is also a rigorous experimental science
Ecology & Evolutionary Biology • Events that occur in ecological time affect life on the scale of evolutionary time
Organisms & the Environment • The environment of any organism includes: • Abiotic- nonliving • Biotic- living • All organisms part of the indiv’s environment are collectively called the biota • Environmental components affect the distribution & abundance of organisms
LE 50-2 Kangaroos/km2 > 20 10–20 5–10 1–5 0.1–1 < 0.1 Limits of distribution Tasmania
Ecologists use observations & experiments to test explanations for the distribution & abundance of spp
Subfields of Ecology • Organismal ecology- how an organism’s structure, physiology, & (for animals) behavior meet environmental challenges
LE 50-3a Organismal ecology
pop ecology- factors affecting how many indiv’s of a spp live in an area
LE 50-3b pop ecology
LE 50-3c Community ecology
Ecosystem ecology- emphasizes energy flow & chemical cycling for biotic & abiotic factors
LE 50-3d Ecosystem ecology
Landscape ecology- arrays of ecosystems & how they are arranged in a geographic region
LE 50-3e Landscape ecology
The biosphere is the global ecosystem, the sum of all the planet’s ecosystems
Ecology & Environmental Issues • Ecology provides the scientific understanding underlying environmental issues • Rachel Carson is credited w/ starting the modern environmental mvmt
Most ecologists follow the precautionary principle regarding environmental issues • It states that humans need to be concerned w/ how their actions affect the environment
Concept 50.2: Interactions b/w organisms & the environment limit the distribution of spp • Ecologists have long recognized global & regional patterns of distribution of organisms within the biosphere • Many naturalists began to identify broad patterns of distribution by naming biogeographic realms
LE 50-5 Palearctic Nearctic Tropic of Cancer (23.5°N) Oriental Ethiopian Equator Neotropical (23.5°S) Tropic of Capricorn Australian
Biogeography is a good starting point for understanding what limits geographic distribution of spp
LE 50-6 spp absent b/c Area inaccessible or insufficient time Yes Yes Dispersal limits distribution? Habitat selection Yes Predation, parasitism, competition, disease Chemical factors Behavior limits distribution? No Biotic factors (other spp) limit distribution? Water Oxygen Salinity pH Soil nutrients, etc. No Abiotic factors limit distribution? No Tm Light Soil structure Fire Moisture, etc. Physical factors
Dispersal & Distribution • Dispersal- mvmt of indiv’s away from centers of high pop density or from their area of origin • Dispersal contributes to global distribution of organisms
Natural Range Expansions • Natural range expansions show the influence of dispersal on distribution
LE 50-7 New areas occupied Year 1996 1989 1974
spp Transplants • spp transplants include organisms that are intentionally or accidentally relocated from their original distribution • spp transplants can disrupt the communities or ecosystems to which they have been introduced
Behavior & Habitat Selection • Some organisms do not occupy all of their potential range • spp distribution may be limited by habitat selection behavior
Biotic Factors • Biotic factors that affect the distribution of organisms: • Interactions w/ other spp • Predation • Competition
LE 50-8 100 Sea urchin Both limpets & urchins removed 80 Only urchins removed 60 Seaweed cover (%) Limpet 40 Only limpets removed Control (both urchins & limpets present) 20 0 August 1982 February 1984 August 1983 February 1983
Abiotic Factors • Abiotic factors affecting distribution of organisms: • Tm • Water • Sunlight • Wind • Rocks & soil
Tm • Environmental Tm is an important factor in distribution of organisms b/c of its effects on biological processes
Water • Water availability in habitats is another important factor in spp distribution
Sunlight • Light intensity & quality affects photosynthesis • Light is also important to development & behavior of organisms sensitive to photoperiod
Wind • Wind amplifies effects of Tm by increasing heat loss from evaporation & convection • Wind can change morphology of plants
Rocks & Soil • Many chara’s of soil limit distribution of plants & so animals that eat them: • Physical structure • pH • Mineral composition
Climate • 4 major abiotic components of climate: Tm, water, sunlight, & wind • Climate is the prevailing weather in an area • Macroclimate- patterns on the global, regional, & local level • Microclimate- fine patterns, such as those encountered by the community of organisms underneath a fallen log
Global Climate Patterns • Global climate patterns are determined largely by solar energy & the planet’s mvmt in space
Sunlight intensity plays a major part in determining the Earth’s climate patterns
LE 50-10a North Pole 60°N Low angle of incoming sunlight 30°N Tropic of Cancer Sunlight directly overhead at equinoxes 0° (equator) Tropic of Capricorn 30°S Low angle of incoming sunlight 60°S South Pole Atmosphere
Seasonal variations of light & Tm increase steadily toward the poles
LE 50-10b March equinox: Equator faces sun directly; neither pole tilts toward sun; all regions on Earth experience 12 hours of daylight & 12 hours of darkness. 60°N 30°N June solstice: Northern Hemisphere tilts toward sun; summer begins in Northern Hemisphere; winter begins in Southern Hemisphere. 0° (equator) 30°S December solstice: Northern Hemisphere tilts away from sun; winter begins in Northern Hemisphere; summer begins in Southern Hemisphere. Constant tilt of 23.5° September equinox: Equator faces sun directly; neither pole tilts toward sun; all regions on Earth experience 12 hours of daylight & 12 hours of darkness.
Global air circulation & wind patterns play major roles in determining climate patterns
LE 50-10c 60°N 30°N Descending dry air absorbs moisture Descending dry air absorbs moisture 0° (equator) Ascending moist air releases moisture 30°S 60°S 0° 23.5° 23.5° 30° 30° Arid zone Arid zone Tropics
LE 50-10d Arctic Circle 60°N Westerlies 30°N Northeast trades Doldrums 0° (equator) Southeast trades 30°S Westerlies 60°S Antarctic Circle
Regional, Local, & Seasonal Effects on Climate • Various features of the landscape contribute to local variations in climate • Seasonal variation also influences climate