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Survivorship curves
It show age-distribution characteristics of species, reproductive strategies, and life history
Reproductive success
It is measured by how many organisms are able to mature and reproduce, with each survivorship curve representing a balance between natural resource limitations and interspecific and intraspecific competition
Carrying capacity (K)
It refers to the number of individuals that can be supported sustainably in a given area
Population dispersal pattern
It is how individuals or species of animal become distributed in different spaces over certain periods of time
Clumped
Some areas within a habitat are dense with organisms, while other areas contain few members
Random
Occurs in habitats where environmental conditions and resources are consistent
Uniform
Space is maximized between individuals to minimize competition
Biotic potential
The maximum reproductive capacity of an organism under optimum environmental conditions
Environmental Resistance
Any factor that inhibits an increase in the number of organisms in the population
J-Curve
It represents a population growth occurs in a new environment when the population density of an organism increases rapidly in an exponential or logarithmic form, but then stops abruptly as environmental resistance or another factor suddenly impacts the population growth
S-Curve
It occurs when, in a new environment, the population density of an organism initially increases slowly but then stabilizes due to the finite amount of resources available
Limiting Factor
It can be any resource or environmental condition that limits the abundance, distribution, and/or growth of a population
Density-dependent limiting factors
These are factors whose effects on the size or growth of the population vary with the density of the population
Density-independent factors
These are factors that limit the size of a population, and their effects are not dependent on the number of individuals in the population
Rule of 70
It helps to explain the time periods involved in exponential population growth occurring at a constant rate
Doubling time
It is the amount of time it takes for a population to double in size
Age-structure diagrams
These are determined by birth rate, generation time, death rate, and sex ratios
Pyramid-shaped age-structure diagram
It indicates that the population has high birth rates and the majority of the population is in the reproductive age group
Bell shape age-structure diagram
It indicates that pre-reproductive and reproductive age groups are more nearly equal, with the post-reproductive group being smallest due to mortality
Urn-Shaped age-structure diagram
It indicates that the post-reproductive group is largest and the pre-reproductive group is smallest, a result of the birth rates falling below the death rate, and is characteristic of declining populations
Total fertility rate (TFR)
The average number of children that each woman will have during her lifetime
Earth Wisdom
Natural cycles that can serve as a model for human behavior
Frontier Worldview
Viewed undeveloped land as a hostile wilderness to be cleared and planted, then exploited for its resources as quickly as possible
Planetary Management
Beliefs that as the planets most important species, we are in charge of Earth
Earth Wisdom
Beliefs that nature exists for all Earths species and we are not in charge of Earth; resources are limited and should not be wasted
Demographic transition
It is the transition from high birth and death rates to lower birth and death rates as a country or region develops from a pre-industrial to an industrialized economic system
Stage 1
Pre-Industrial (High Stationary)
Stage 2
Transitional (Early Expanding)
Stage 3
Industrial (Late Expanding)
Stage 4
Post-Industrial (Low Stationary)
Stage 5
Sub-Replacement Fertility (Declining)
Stage 5: Sub-Replacement Fertility (Declining)
Stage 4: Post-Industrial (Low Stationary)
Stage 3: Industrial (Late Expanding)
Stage 2: Transitional (Early Expanding)
Stage 1: Pre-Industrial (High Stationary)
Present to 2050 C.E.
Estimates are as high as 9.8 billion.
Earth Wisdom
1650 C.E. to present
1300 C.E. to 1650 C.E.
0 C.E. to 1300 C.E.
5000 B.C.E. to 1 B.C.E.
8000 B.C.E. to 5000 B.C.E.
Before Agricultural Revolution
Birth Rate (%) = [(total births/total population)] × 100
Birth Rate Formula
CBR = [(b ÷ p) × 1,000]
Crude Birth Rate Formula
Death Rate (%) = [(total deaths/total population)]× 100
Death Rate Formula
CDR = [(d ÷ p) × 1,000]
Crude Death Rate Formula
Doubling Time = 70/% growth rate
Doubling Time Formula
Emigration = number leaving a population
Emigration Formula
Global Population Growth Rate (%) = [(CBR – CDR)]/10
Global Population Growth Rate Formula
Immigration = number entering a population
Immigration Formula
National Population Growth Rate (%) = [(CBR + immigration) – (CDR + emigration)]/10
National Population Growth Rate Formula
Percent Rate of Change = [(new # - old #)/old #] × 100
Percent Rate of Change Formula
Population Density = total population size/total area
Population Density Formula
Population Growth Rate Formula
dt= 70/r
To find how long it takes for a population to double in size we can use the following formula _
Liebig’s law of the minimum
Based on _, even if all other factors are favorable, the one that is least favorable will dictate the growth, abundance, or distribution of the population of a species.
Positive feedback loops
_ stimulate change and are responsible for sudden or rapid changes within ecosystems.
Negative feedback loops
This often provide stability.
carrying capacity
This point of stabilization is known as the _ of the environment, and it denotes the point at which the upward growth curve begins to level out
density-dependent
This type of population growth is termed “_” since the growth rate depends on the number of organisms in the population.
density-dependent
This type of population growth rate is known as “_,” a regulation of the growth rate is not tied to the population density until the resources are exhausted and the population growth crashes.
Type I - Late Loss
Reproduction occurs fairly early in life, with most deaths occurring at the limit of biological life span.
Type I - Late Loss
Low mortality at birth with a high probability of surviving to advanced age.
Type I - Late Loss
Death rates decrease in younger years due to advances in prenatal care, nutrition, disease prevention, and cures, including immunization.
Type II - Constant Loss
Individuals in all age categories have fairly uniform death rates, with predation being the primary cause of death.
Type II - Constant Loss
Typical of organisms that reach adult stages quickly.
Type III - Early Loss
Typical of species that have great numbers of offspring and reproduce for most of their lifetime.
Type III - Early Loss
Death is prevalent for younger members of the species due to environmental loss and predation and declines with age.
r-Strategists
r-Strategists
r-Strategists
K-Strategists
K-Strategists
K-Strategists
Generalists
Generalists
Specialists
Specialists
Plate tectonic theory
It states that Earth’s lithosphere is divided into a small number of plates that float on and travel independently over the mantle, with much of Earth’s seismic activity occurring at the boundaries of these plates.
Pangaea
In 1915, Alfred Wegener proposed that all present-day continents originally formed one landmass he called _.
Alfred Wegener
In 1915, proposed that all present-day continents originally formed one landmass he called Pangaea.
Seafloor Spreading Theory
geologic process in which tectonic plates —large slabs of Earth's lithosphere —split apart from each other.
lithosphere
The is the solid, outer part of the Earth and is broken into huge sections called plates, which are slowly moving.
plates
The lithosphere is the solid, outer part of the Earth and is broken into huge sections called , which are slowly moving.
Subduction zones
These are areas on Earth where two tectonic plates meet and move toward each other, with one sliding underneath the other and moving down into the mantle.
Convergent Boundaries
These occur where two plates slide toward each other.
Cascade Mountain Range
Example of Convergent Boundaries
Divergent Boundaries
These occur when two plates slide apart from each other.
Divergent Boundaries
It can create massive fault zones in the oceanic ridge system and areas of frequent oceanic earthquakes.
Mid-Atlantic Ridge and the East Pacific Rise
Example of Oceanic Divergent Boundary
East African Great Rift Valley
Example of Continental Divergent Boundary
island arc
When two oceanic plates converge, they create an _ — a curved chain of volcanic islands rising from the deep seafloor and near a continent.
undersea trench
A deep _ is located in front of such arcs where the descending plate dips downward.
Transform boundaries
These occur where plates slide past each other in opposite directions.
The san Andreas fault
Example of Transform boundaries
Soils
These are a thin layer on top of most of Earth’s land surface.
Surface Litter
Leaves and partially decomposed organic debris.
Topsoil
Organic matter, living organisms, and inorganic materials; it is very thick in grass lands.
Zone of leaching
Dissolved and suspended materials move downward.