Ecology Flashcards
Ernst Haeckel
coined the term “ecology”, the scientific study of the interactions between organisms and the environment
ecological system
ecological systems have biotic and abiotic components that interact
homeostasis: physiology/morphology/behavior
organisms maintain a set of conditions
population
group of individuals (2nd lowest group of ecological hierarchy)
community
interaction of populations of individuals of different species (just the biotic part)
ecosystem
interaction of the abiotic and biotic parts of a community
landscape = sets of ecosystems together
biosphere
highest group of ecological hierarchy, contains all ecosystems
climate (macro/micro)
largely dictated by where the sun hits the Earth
climate = average long-term conditions vs weather = short-term conditions
macroclimate: patterns on the global, regional, and landcsape level
microclimate: very fine, localized patterns, such as those encountered by the community of organisms that live in the microhabitat beneath a fallen log
climate diagram
compares temperature and precipitation, constant red line implies little variation in climate
monsoon
typically in hot areas close to oceans, temp is high all year along and heavy rain occurs in a particular season
seasonality
climate changes throughout the year, predictable weather patterns
result of which hemisphere is getting greater sun exposure
weather
weather = short-term conditions vs climate = average long-term conditions
angle of incidence (of the sun)
direct overhead exposure more likely to occur at the Equator
prevailing winds
winds do not just move north and south because the Earth spins (faster at the equator than everywhere else)
prevailing winds drive oceanic currents
gyre
large patterns of ocean movements (circular motion driven by prevailing winds)
currents
California - along CA coast, cold water coming down from Alaska, pushes water off coast and causes upwelling
Gulf Stream - from Caribbean north along East Coast and to Europe, keeps E Coast warmer than it would be otherwise
Antarctic circumpolar - goes all the way around the Antarctic, emphasizes how much more water there is in S hemisphere than N hemisphere
topography
“lay of the land” - in CA, precipitation occurs on windward side of mountains, prevailing winds come from the West and create cold air
windward/leeward
windward side is closer to the ocean/coast, leeward side is over hills/mountains
rain shadow
occurs on leeward side of mountains
dispersal
organism dispersal can be predicted based on directions of prevailing winds, storms, and jet streams
definition is movement of individuals or gametes away from their area of origin or from centers of high population density
contributes greatly to the global distribution of organisms
Mediterranean climate
we have one here in the Bay Area, the actual Mediterranean, and S Hemisphere
Northern and Southern Med climates have different patterns
biome (von Humboldt)
von Humboldt - biogeographer who traveled extensively, saw characteristic sets of plants in different locations, which changed on mountains according to elevation
canopy
upper layer of forest
forest is based on vertical layer of vegetation`
disturbance
event such as a storm, fire, or human activity that changes a community, removing organisms from it and altering resource ability
disturbance rather than stability tends to be the rule
tropical forest
rainfall is relatively constant, about 200-400 cm annually in tropical rainforests
tropical dry forest - precipitation is highly season
temperature is high year round with little seasonal variation
tropical forest vegetation is usually vertically layered with intense competition for light
highest biodiversity of any terrestrial biome
desert
occur in bands near 30 degrees north and south latitude or at other latitudes in the interior of continents
temperature is variable seasonally and daily, can be very high or very low
dominated by low widely scattered vegetation, many plants do CAM photosynthesis
savanna
occurs in equatorial and subequatorial regions
dry season can last up to eight or nine months
warm year-round, but with more seasonal variation than tropical forests
scattered trees are thorny with small leaves; fires are common in the dry season
grasses and forbs make up most of the ground cover, most animals are large and plant-eating or predators
chaparral
occurs in midlatitude coastal regions on several continents and is widely distributed
fall, winter, and spring are cool and summer is warm
dominated by
temperate grassland
eg plains and prairies of central North America
precipitation is often highly seasonal with relatively dry winters and wet summers; periodic drought is common
winters are generally cold while summers are hot
dominant plants are grasses and forbs, many grasses have adaptations to help survive drought
native mammals include large grazers like bison and wild horses
northern coniferous forest (taiga)
largest terrestrial biome on Earth, extending in a broad band across N America and Eurasia to the edge of the arctic tundra
precipitation varies
winters are usually cold and summer may be hot
dominated by cone-bearing trees, such as pine, spruce; conical shape of conifers prevents too much snow from accumulating and breaking their branches
lots of migratory birds
temperate broadleaf forest
found mainly at midlatitudes in the Northern Hemisphere
precipitation highest in fall, sometimes winter snow
cold winters, hot and humid summers
mature TBF has distinct vertical layers, including a closed canopy
dominant plants are deciduous trees, which drop their leaves before winter when low temps would reduce photosynthesis
many mammals hibernate in winter
tundra
covers expansive areas of the Arctic and alpine tundra on very high mountaintops
low precipitation
winters are very cold, summers also cold
vegetation is mostly herbaceous - mosses, grasses, forbs; permanently frozen layer of soil called permafrost restricts the growth of plant roots
large grazing species and predators
oceans
make up the largest marine biome, covering about 75% of Earth’s surface
water evaporated from the oceans provides most of the planet’s rainfall
ocean temperatures have a major effect on global climate and wind patterns
(aquatic biomes are classified by marine or freshwater)
coral reefs
formed largely from the calcium carbonate skeletons of corals
shallow reef-building corals live in the photic zone of relatively stable tropical marine environments with high water clarity
require high oxygen levels and a solid substrate for attachment
corals are main organisms, but overall biodiversity is very high
intertidal zones
periodically submerged and exposed by the tides, wice daily on most marine shores
upper zones experience longer exposure to air and greater variations in temperature and salinity
oxygen and nutrient levels are generally high and renewed with each turn of the tides
high diversity and biomass of attached marine algae
many heterotrophs
estuaries
transition area between river and sea; seawater flows up the estuary channel during a rising tide and flows back down during the falling tide
salinity varies within estuaries, from fresh water to seawater
nutrients from the river make estuaries very productive biomes
complex networks of tidal channels, islands, etc
saltmarsh grasses and algae
rivers
most prominent physical characteristic is speed and volume of flow
river - water generally warmer and more turbid than streams
salt and nutrient content increases from oxygen-rich headwaters to the mouth
headwater streams may be rich in phytoplankton or rooted aquatic plants, also a great diversity of fishes and invertebrates
lakes
standing body of water covering large areas
oligotrophic - nutrient poor and generally oxygen rich
eutrophic - nutrient rich and often depleted of oxygen in the deepest zone, covered with ice in winter
littoral zone - shallow, well-lit waters close to shore
limnetic zone - far from shore, too deep to support rooted aquatic plants, but has phytoplankton and drifting heterotrophs
wetlands
habitat inundated by water at least some of the time and that supports plants adapted to water-saturated soil
both water and soils are periodically low in dissolved oxygen
basin wetlands - develop in shallow basins
riverine wetlands - developing along river and stream banks
water-saturated soils favor the growth of plants
zonation
many aquatic biomes are physically and chemically stratified
photic, aphotic make up pelagic
benthic
abyssal
photic/aphotic
photic zone - upper part of pelagic zone, where there is sufficient light for photosynthesis
aphotic zone - lower zone where little light penetrates
pelagic/benthic
pelagic zone - made up of photic and aphotic zone, above benthic and abyssal zone
benthic zone - bottom of all auatic zones, deep or shallow; made up of sand and organic and inorganic sediments, occupied by communities of organisms collectively called the benthos
major source of food for benthic species is detritus
abyssal
part of the ocean 2000-6000 m below the surface
deep in the aphotic zone
continental shelf
“surface” of land in aquatic biomes
hydrothermal vents
dark, hot environments where food producers are chemoautotrophic prokaryotes
located on mid-ocean ridges, deep sea
marine benthic zone
thermocline (thermal stratification)
narrow layer of abrupt temperature change that separates the uniformly warm upper layer of a lake/ocean from the more uniformly cold deeper waters
lakes tend to be especially layered except for turnover in temperate lakes
turnover
temperate lakes undergo a semiannual mixing of their waters as a result of changing temperature profiles
sends oxygenated water from a lake’s surface to the bottom and brings nutrient-rich water from the bottom to the surface in both spring and autumn
continental drift
plate tectonics have enabled us to figure out the history of the continents
continental drift has changed the makeup and nature of organisms on continents, which had to move or adapt or go extinct
biotic zones (Wallace)
Wallace recognized that different places on Earth had different sets of organisms, he called these biogeographic regions
only recently did we associate that with plate tectonics
biotic exchange
occurs when continents come together
eg we got marsupials in N America from S America when the continents came together, and S America got bears etc from here
vicariance (compare with dispersal)
occurs when the range of a species or lineage is split apart
immigration/emigration
immigration - influx of new individuals from other areas
emigration - movement of individuals out of a population and into other locations
geographic range
how widespread a species is
eg Devil’s hole pupfish has a very small range, while humpback whale has a very large range
generation time
amount of time taken for a cohort to go from birth to when all the individuals are dead
sex ratio
ratio of male to female
exponential growth (multiplicative)
describes population growth in an idealized, unlimited environment
you know what exponential growth is why’d you even make this dumbass flashcard
territoriality
defense of a bounded physical space against encroachment by other individuals
often results in uniform patterns of dispersion
habitat patches
clumped dispersion
habitats are patchy even on a small scale
organisms are not distributed randomly in space
help prevent extinction because even if one patch undergoes a disturbance, the species is distributed in other patches as well
habitat occupancy
set of patches vary over time in whether they’re occupied or not
BD model
B = births D = deaths Nt+1 = Nt + B - D ∆N/∆t = B - D ignores immigration and emigration (for now)
population growth equations
b = per capita birth rate (fecundity) m = per capita death rate (mortality) r = per capita rate of increase r = b - m r = 0, zero population growth (ZPG) ∆N/∆t = rN rinst = instantaneous, intrinsic or innate dN/dt = rinstN, a maximum rate of increase
fecundity, fertility
fertility - TFR total fertility rate is the expected number of children born per woman in her child-bearing years
fecundity - average number of young per female of age x
reproductive table
fertility schedule - age-specific summary of the reproductive rates in a population
constructed by measuring the reproductive output of a cohort from birth until death
tallies the number of female offspring produced by each age-group for sexual species
cohort
randomly selected group of individuals of the same age
survivorship curve (3 types)
Type I - flat at the start, reflecting low death rates during early and middle life, and then drops steeply as death rates increase among older age groups (examples are many large mammals including humans) - inverted L, opposite of type III
Type II - intermediate, with constant death rate over the organism’s life span (occurs in squirrels, rodents, plants, etc.) looks like a downward slope like my GPA
Type III - looks like an L which is what I’ll be taking on this midterm, drops sharply at the start reflecting very high death rates for those few individuals that survive the early period of die-off
life cycle
the stages that an organism goes through in its life, not to be confused with life table etc
carrying capacity (K)
maximum number of organisms supported by a particular environment and its resources
logistic growth (sigmoid, S-shape)
per capita rate of increase approaches zero as the population size nears the carrying capacity