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Biodiversity
variety of all living things on earth and what sustains this
functional traits
diversity of a characteristic that effects survival/growth/production
response traits
affect how a species responds to environment
effect traits
influence what the species can do in the ecosystem
nekton
can actively swim against the water column
plankton
cannot actively swim against the water column
allometry
study of relationship of body size to shape, anatomy, and physiology
monophyletic group (clade)
common ancestor and all descendants
paraphyletic group
common ancestor and some, but not all, descendants
polyphyletic group
doesn’t all share a common anscestor
synapomorphy
shared and derived trait used to define a clade
speciation
origin of species over generations
dispersal
movement of organisms among site and regions
ecological drift
random fluctuations in species abundance
ecological selection
environmental tolerances and interactions that favor a species in particular conditions
alpha diversity
measure of diversity in species in a particular area
beta diversity
measure of difference in species diversity between areas
gamma diversity
measure of overall diversity of species for the different areas of a region
levels of biological organization
organism-population-community-ecosystem-biome
4 filters of communities
species pool-dispersal-environmental filtering-biological interactions
rarefraction curve
measures differences/simularities in DNA
gene flow
transfer of genetic material throughout populations
extrinsic factors
environmental factors: range/age
intrinsic factors
factors in relation to organisms: size/reproduction
allopatric
speciation due to a physical barrier
peripatric
one small group breaks away and speciates away from the original group
parapatric
species spreads out over a large area to form their own small groups and speciate
sympatric
gene flow is restricted by something other than a physical barrier
thermocline
temperature difference through the water column
halocline
salinity gradient through the water column
pycnocline
density gradient through the water column due to temp and salinity
coriolis effect
earths rotation impacts water movement away from the equator
ekman transport
each layer of water moves 45 degrees right of the wind = net movement of 90 degrees
center of gyres
little-no movement creating buildup of debris/trash
langmuir circulation
two cells circuling towards eachother creating downwelling and windrows
windrows
visual lines across ocean due to langmuir circulation and downwelling that leaves debris along the cells
reynolds number (Re)
describes the relative importance of inertial vs. viscous forces
inertial forces
tendancy to resist change in motion
high inertia
organisms can stop swiming and coast along with less energy use
viscous forces
fluids resistance to flow
high viscosity
coasting difficult through “thick” water so more energy is used
high Re
inertial forces dominate (larger organisms)
low Re
viscous forces dominate (smaller organisms)
boundary layer
thin layer of fluid on surface of organism where there is limited flow
no slip condition
velocity is zero at the surface of organisms body
laminar flow
smooth and orderly movement with thick and stable boundary layer
turbulent flow
chaotic and irregular movement with thin and unsteady boundary layer
form drag
resistance due to physical shape
skin friction drag
resistance due to surface texture
autotrophs
create their own energy
heterotrophs
obtain their energy from something else
photoautotroph
produce energy from light
chemoautotrophy
produce energy from carbon fixation (no light)
mixotrophy
can get energy from others or make their own
allometric scaling
describing how a variable of an organism changes in relation to their overall size
isometric allometry
variable increases in proportion to body size
positive allometry
variable increases faster than body size
negative allometry
variable increases slower than body size
basal metabolic rate
energy needed when an organism is at rest
active metabolic rate
energy needed when an organism is active
metabolic scaling theory
size related to metabolic rates specific to the size of the organisms
metabolic rate of small organisms
higher with faster growth, shorter generations and faster population responses
metabolic rate of bigger organisms
lower with slower growth, longer generations, and slower population turnover
Metabolic Scope for Growth (MSfG)
energy left over after paying for basic metabolism and movement
MSfG equation
food energy - (basal + metabolic rates)
ecological niche
theoretical rage of conditions a species can survive and reproduce
fundamental niche
full range of environmental conditions/resources an organism could be within
realized niche
realistic range of the environment an organism actually occupies after consideration of interactions with others
Regulators
maintain body aspect through internal processes
conformers
maintain body aspects through exchange with surroundings
ectotherms
regulate their own body temperature
ectotherm adaptations to loosing heat to environment
insulation/blood flow/large body sizes
ectotherms
body temperature conforms to seawater
heterothermy
uses both endo and ectothermy
osmoregulators
actively maintain constant internal salinity
stenohaline
tolerate narrow salinity ranges
euryhaline
tolerate wide salinity ranges
osmoconformers
internal salinity matches environment