III. Ecology

Key focus of this chapter: population and communities.

This chapter focuses on population and communities and gives concise summaries of the important things about ecosystem and biosphere.

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A.  Hierarchical levels of organization

 

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B.  Species

1.       Historic biologists

a.    Aristotle (384 – 322 B.C.)

• Scala naturae (“scale of nature”) – a historical hierarchy that ranked organisms from simpler to more complex forms.

• Aristotle considered species fixed and unchanging; this is a historical view, not modern evolutionary biology.

b.    Carolus Linnaeus (1707 – 1778)

• Binomial nomenclature – two-part scientific names (genus and species).

• Linnaeus classified organisms by shared traits and initially regarded species as fixed; modern taxonomy also uses evolutionary relationships.

c.    Georges Cuvier (1769 – 1832)

Paleontology – the study of fossils

• Catastrophism – sudden geological events can cause extinctions and help explain changes seen among fossil-bearing rock strata.

d.   James Hutton (1726 – 1797)

• Gradualism – major geological change can result from the slow accumulation of small, continuous processes.

e.    Charles Lyell (1797 – 1875)

• Uniformitarianism – geological processes operating today also operated in the past over long periods of time.

f.     Jean Lamarck (1744 – 1829)

• Inheritance of acquired characteristics – Lamarck’s historical hypothesis that acquired traits could be inherited.

• Use and disuse were central to Lamarck’s model; this is not accepted as the general mechanism of evolutionary adaptation.

g.    Charles Darwin (1809 – 1882)

• Voyage of HMS Beagle; observations from the Galápagos Islands contributed to Darwin’s ideas about evolution.

-       Reproductive isolation is a key mechanism in speciation, but Darwin’s observations were not the first experimental proof of a new species.

• On the Origin of Species

-       Descent with modification from common ancestors

-       Natural selection is a major mechanism of adaptive evolution

Natural selection

-       Individuals with heritable traits that increase reproductive success tend to contribute more offspring to the next generation.

• Artificial selection

-       Selective breeding by humans increases the frequency of chosen heritable traits.

 

 

 

 

 

 

 

 

 

 

 

 

 

 

2.      Evolution and structure

• Evolution: a change in allele frequencies in a population across generations.

 

Fig. 1 Divergent and convergent evolution

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3.         Geographic separation

• Allopatric speciation

-        New species arise after geographic isolation reduces gene flow between populations.

• Sympatric speciation

-        New species arise without a geographic barrier, often through reproductive isolation within the same area.

-        Populations initially occupy the same geographic region.

 

                                               

C.   Population

1.    Variation of evolution

a.        Mutation – the ultimate source of new alleles and new genetic variation.

b.       Sexual recombination – reshuffles existing alleles into new genotype combinations.

   

2.   Alteration of genetic composition

a.        Genetic drift

Random changes in allele frequencies, especially strong in small populations; drift can reduce genetic variation.

Bottleneck effect

- A sudden reduction in population size can leave a nonrepresentative sample of the original gene pool.

Founder effect

- A new population founded by a few individuals may have allele frequencies different from the source population.

 

b.       Gene flow

-        Movement of alleles into or out of a population through migration of individuals or gametes.

 

c.       Natural selection

Primary mechanism of adaptive evolution.

• Geographic variation / cline

-        A cline is a gradual geographic change in phenotype or allele frequency across an environmental gradient.

• Evolutionary fitness

-          Directional selection: favors one extreme phenotype, shifting the population distribution toward that extreme.

-          Disruptive (diversifying) selection: favors both extreme phenotypes over intermediate phenotypes.

-          Stabilizing selection: favors intermediate phenotypes and selects against extremes.

 

Fig. 2

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3.     Population dynamics

a.    Exponential growth

• Population grows at an approximately constant per-capita rate when resources are abundant (J-shaped curve).

• Growth occurs when additions to the population exceed losses.

 

b.    Logistic growth

• Sigmoid (S-shaped) growth curve.

• Growth is rapid at low density but slows as density-dependent limits increase near carrying capacity.

• Carrying capacity (K): the population size an environment can sustain over time under given conditions.

Life histories

               

 

 

 

 

 

 

 

 

 

 

D. Community ecology

1.      Niche and habitat

• Niche: a species’ ecological role and the range of resources and environmental conditions it uses.

• Habitat: the physical environment or place where an organism lives.

 

2.     Species interactions

 

 

3.     Defensive adaptation

Defensive adaptations that reduce predation or herbivory.

 

 

4.    Innate and learned behaviors

a.    Fixed action pattern (FAP)

• An innate, stereotyped sequence of behavior triggered by a specific sign stimulus.

• E.g., egg-rolling behavior in greylag geese or stereotyped courtship displays.

 

b.       Imprinting

• Rapid learning during a sensitive period early in life.

• Combines an innate predisposition with experience-dependent learning.

• Young animals learn a particular stimulus or individual, which can influence later social or reproductive behavior.

• E.g., young geese following a parent; conservation programs have used surrogate leaders for imprinted cranes.

c.       Habituation

• Decreased response to a repeated, harmless stimulus.

• E.g., an animal gradually stops responding to a repeatedly presented harmless sound.

 

d.      Spatial learning

• Learning and remembering spatial relationships, landmarks, routes, or locations.

 

e.       Associative learning

Learning that forms an association between two stimuli or between a behavior and its consequence.

 

 

 

f.     Extinction

• Extinction: a conditioned response weakens when the conditioned stimulus is repeatedly presented without the unconditioned stimulus; operant behavior can also weaken when reinforcement stops.

 

 

 

5.     Ecological succession

Ecological succession is the sequential change in community composition and structure over time, often after new substrate forms or a disturbance occurs.

 

a.           Primary succession

• Begins on newly exposed substrate where soil is absent.
• Examples: fresh lava or land exposed by a retreating glacier.

• Pioneer organisms often include microbes, lichens, algae, and mosses that help build soil and alter the environment.

Communities

 

 

 

b.           Secondary succession

• Begins after a disturbance where soil and some biological legacies remain.

• Examples include areas recovering after fire, storms, logging, or abandonment of farmland.

 

 

E.  Ecosystem

1.       Biotic and Abiotic factors

• Biotic factors: living organisms and their interactions within an ecosystem.

Abiotic factors

-        Nonliving physical and chemical components of the environment.

-        E.g., water, temperature, sunlight, wind, pH, and nutrients.

 

2.     Energy flow in ecosystem

a.    Food chain

• Biomagnification: persistent toxins can become more concentrated at successively higher trophic levels.

 

 

 

 

 

 

 

 

 

 

 

 

Fig. 3

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3.     Nutrient cycles

Biogeochemical cycles move water and chemical elements between biotic and abiotic reservoirs.

 

a.    Water cycle

Essential to all living organisms

• Evaporation and transpiration -> condensation -> precipitation -> runoff, infiltration, and return to surface waters.

 

b.    Phosphorus cycle

• Phosphorus is a component of ATP, nucleic acids, and phospholipids.

• Weathering releases phosphate -> plant uptake -> consumers -> decomposition and return to soil/water; sedimentation provides long-term storage.

 

c.    Carbon cycle

• Carbon forms the backbone of organic molecules in living organisms.

• Photosynthesis removes CO2 from air or water; respiration, decomposition, and combustion return CO2 to the environment.

 

d.   Nitrogen cycle

• Nitrogen is required for amino acids, proteins, nucleic acids, and other biomolecules.

• N2 -> nitrogen fixation -> NH3/NH4+ -> nitrification -> NO2- -> NO3-; assimilation incorporates inorganic nitrogen into biomass, and denitrification returns N2 to the atmosphere.

 

 

 

 

 

 

Fig. 4 Nitrogen cycles   

 

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4.    Temperature and osmoregulation

a.     Climate

Microclimate

-                Local atmospheric conditions near the ground or around organisms that can differ from the broader regional climate.

-   Can strongly affect individual organisms and local populations.

• Macroclimate

 

-                Broad regional or global climate patterns.

-                Strongly influences the geographic distribution of species and biomes.

 

b. Thermoregulation

• Endotherms

-                Generate substantial metabolic heat and can maintain body temperature within a relatively narrow range.

-                E.g., most mammals and birds. “Warm-blooded” is an informal term.

• Ectotherms

-                Rely mainly on external heat sources; body temperature often varies with environmental conditions.

-                E.g., most reptiles, amphibians, fishes, and invertebrates. “Cold-blooded” is an informal and often misleading term.

 

5.     Osmoregulation in bony fish

a.    Freshwater fish

• Freshwater bony fish are hyperosmotic to the environment: water enters by osmosis, they drink little, excrete copious dilute urine, and actively take up ions across the gills.

 

b.       Saltwater fish

• Marine bony fish are hypoosmotic to seawater: they lose water by osmosis, drink seawater, excrete excess salts through the gills, and produce relatively little urine.

 

 

 

 

F.   Biosphere

1. Aquatic zones

a.        Lake zones

 

 

 

 

 

 

 

 

 

 

b.       Marine zones

 

 

 

2.     Climate and lake mixing

a.    Rain shadow

• Moist air rises on the windward side of a mountain, expands and cools, causing condensation and precipitation.

• Drier air descends on the leeward side, compresses and warms, lowering relative humidity and creating a rain-shadow region.

 Eg/ Death Valley (Sierra Nevada)

 

Fig. 5 Rain shadow

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b.    Seasonal lake turnover

In many temperate dimictic lakes, spring and fall turnover mix oxygen-rich surface water with nutrient-rich deeper water.

• Turnover occurs when temperature and density differences weaken enough for wind-driven mixing of the water column.

Spring turnover

-        Surface water warms toward about 4°C, approaches the density of deeper water, and the lake mixes.

Fall turnover

-        Surface water cools toward about 4°C, becomes denser, and wind-driven mixing circulates the lake.

 

 

3.     Terrestrial biomes

Fig. 6

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1. Which of the following is NOT a factor that influences regional climate?

A.   Ocean currents

B.   Altitude

C.   Latitude

D.  Atmospheric circulation

E.   None of above

 

2. In a community, when two species benefit each other, it is called __________ .

A.   Mutualism

B.   Commensalism

C.   Competition

D.  Parasitism

E.   Predation