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photo-
obtain energy from sunlight, light energy to make ATP
chemo-
breaking/forming of chemical bonds to release energy for respiration or fermentation to generate ATP
auto-
make organic matter from inorganic carbon (CO2)
hetero-
obtain carbon from organic compounds
nutrients
substances required for cells to build molecules required to sustain life
essential nutrients
the organism cannot synthesize it and must acquire it from another source
beneficial nutrients
stimulate growth and development but are not required or could be substituted
macronutrients
essential nutrients that are required in large amounts
micronutrients
essential nutrients required in smaller amounts
what are the essential macronutrients
carbon, hydrogen, oxygen, phosphorus, sulfur
mineral nutrients
inorganic compounds from soil or water, elements
vitamin nutrients
organic compounds from other living things, water or fat soluble
how does a stationary organism acquire nutrients
grow in search of new resources, root mines minerals and water as it grows
plant nutrient needs
require light, water, and 20 essential nutrients; carbon: used for glucose to construct cellulose; nitrogen: proteins and nucleic acids, limiting growth factor; phosphorus: synthesize nucleic acids and phospholipids, food energy → chemical energy, liming growth factor; potassium: regulates stomata, water balance, limits growth
nutrient deficiencies
concentration of nutrient decreases between typical range, leads to visual characteristics, nitrogen deficiency is most common
excessive nutrients
can be toxic to certain tissues or cell types
herbivores
plant based, digestive systems that can handle large amounts of plant material
carnivores
eat other animals
omnivores
eat both plants and animals
3 organic precursors that animals can synthesis molecules from for energy
carbohydrates, proteins, fats
carbohydrates
organic carbon for herbivores/omnivores, carnivores rely on protein and lipids
proteins
dietary sources of nitrogen and sulfur
fats
chemical energy, absorption of fat-soluble vitamins and production of fat-soluble hormones
essential nutrients for animals (must be eaten)
amino acids, fatty acids, vitamins, minerals
essential amino acids
protein building blocks, meat sources, grain/legume
essential fatty acids
fat building blocks, humans only have 2
why is it easier to overdose on fat-soluble vitamins
water-soluble dissolve in water and are excreted in urine, fat-soluble is stored in adipose tissue and can cross cell membranes easily, allowing them to build up
why is sodium essential for animals but not plants
animals use sodium for electrical signaling and it drives nutrient absorption, plants use
diffusion
molecules move from area of high to low concentration, no energy required, down concentration gradient
facilitated diffusion
through protein channels embedded in cell membrane, specific, for molecules too large or polar to cross nonpolar cell membrane,
active transport
movement of molecules using energy against concentration gradient, requires energy
proton pumps
protein complexes that use energy from ATP to “pump” protons across membrane, electrochemical gradient, source of energy to move molecules against gradient
co-transport
movement of two molecules at the same time, one “down” which releases energy to move the other against, protein channels called co-transporters
does co transport require an energy source
active transport powered by proton gradients, not ATP directly
importance of concentration gradient in nutrient acquisition
naturally diffuse from high to low, energy not required, higher the concentration = faster rate of diffusion, ex. plant roots, animal digestive tracts
importance of distance in nutrient acquisition
longer distance = slower rate of diffusion, evolution selects shorter travel, ex. circulatory systems: nutrient absorbing capillaries are next to absorption surface
importance of surface area for nutrient absorption
larger = more nutrients can be absorbed, ex. plant roots have root hairs, mammalian digestive tracts’ small intestine is highly folded with microvilli
formation of soil
weathering of rock by mechanical, chemical, and biological processes, made of living and nonliving components: humus, rock fragments, water, gasses
humus in soil
organic matter, plant roots, microorganisms, decomposing plants/animals, 5% of soil volume
rock fragments in soil
inorganic, slowly broken down into smaller particles that vary in size, 40-45% of soil
water and gasses in soil
dissolved in soil particles, 50% of volume
soil texture
determined by proportions of differently sized particles in the soil, affects ability of plant roots to penetrate soil and ability of soil to hold water
categories of soil texture
gravel, sand, silt, clay, loam
factors that affect soil formation
parent material, climate, topography, biological factors, time
soil composition
require certain ions and minerals from soil, mediated by root hairs, properties directly affect ion availability
sand
low water availability, low nutrient availability, high oxygen availability, high root penetration ability
clay
high water availability, high nutrient availability, low oxygen availability, low root penetration ability
organic matter
high water availability, high nutrient availability, high oxygen availability, high root penetration ability
clay and anions
anions are easily dissolved in soil water, do not stick to clay, absorbed by root hairs, also easily leached from soil
presence/absence of clay
prevent leaching of cations from soil, also prevents absorption of cations by clay
root hairs
increase surface area for absorption
proton pumps in plants
used by root hairs to move nutrients into cell, line epidermal tissue, pump H+ into soil, positive charge outside with high concentration, low concentration inside and negative charge; drives ion channels and co-transporters, requires ATP
ion channels in plants
cation exchange: H+ displaces cations from clay and enters root via cation channels (passive)
co-transporters in plants
anion uptake: protons move back in through anion co-transporters, against gradient (active)
mycorrhizal fungi
80-90% of plants form mutualistic relationships with, ecto-wrap around epidermis, endo- hyphae penetrate cell walls, decomposing dead matter and enhanced absorption and plant for nitrogen and phosphorus, fungi gets sugars from root, increases the surface area, not oxygen sensitive
Rhizobia in legumes
mutualistic relationship, fix atmospheric N2 into ammonia inside root nodules, bacteria obtain carbon compounds and plants obtain ammonia, nitrogenase inactived by O2
carnivorous plants
digest insects to obtain N, P, and K in nutrient poor soils
leghemoglobin in legume root nodule
regulates the amount of oxygen available
mobile nutrients
nitrogen, magnesium, potassium, move from old to new tissue when deficient, symptoms appear in older leaves first
immobile nutrients
calcium, iron, cannot be relocated, symptoms in new leaves first
water potential
potential energy of water, determined by solute potential and pressure potential
increase water potential
removing solutes, adding pressure
decrease water potential
adding solutes, removing pressure
directional flow
(highest) soil to root to stem to leaf to atmosphere (lowest), water upward
osmosis
diffusion of water down its concentration gradient
when does water stop moving
when the water potential is equal on both sides of the membrane
cell in an environment with higher solute concentration than the cell
lose water, plasmolyzed
cell in environment with lower solute concentration
cell gain water, turgid
hypotonic
solution on one side of membrane where solute concentration is less than other side of membrane
hypertonic
solution on one side of membrane where solute concentration is greater than on other side
how does soil becoming too dry affect gradient
can result in decreased solute potential and or decreased pressure potential, too low = water into soil
symplast
water moves cell-to-cell through cytoplasm via plasmodesmata, “shared cytoplasm”
transmembrane
water repeatedly crosses plasma membranes through aquaporins, membrane-regulated
apoplast
water travels through porous cell walls without entering cytoplasm, fastest route, Casparian ship forces apoplastic water to cross a membrane
why does air becoming drier increase the rate of transpiration
drier air has a lower water potential than the air inside a leaf, this increases water potential gradient between leaf and atmosphere, leading to a higher rate of transpiration
what are the three hypotheses for water movement in xylem
root pressure pushes water up, capillary action draws water up with xylem, cohesion-tension properties pulls water up (tall trees)
root pressure
water enters roots by osmosis and builds positive pressure, push water a few meters, guttation at night, not strong enough for tall trees
capillary action
driven by cohesion, adhesion, and surface tension, narrow tubes, insufficient for tall trees, pulls water up within a xylem tube
cohesion-tension
transpiration creates negative pressure in leaves, pulls water upward like a straw through entire plant, cohesion keeps this continuous, xylem walls reinforced with lignin to withstand tension, open stomata and water between mesophyll cells utilized
transpiration
evaporation of water from stomata, passive, energy source is extreme difference in water potential between water in soil (high) and water in atmosphere (low)
solute potential
dissolving solutes makes solute potential more negative, through active transport of ions and accumulating sugars
pressure potential
tension from transpiration makes more negative, positive when there is turgor pressure, manipulated through opening and closing of stomata
sugar source
any tissue that produces or releases sugars; mature leaves, stems during growing season, storage organs at start of new growing season, where sugar is coming from
sugar sink
any tissue that uses or stores sugars, growing tissues, storage tissues during growing season, where sugar is going to
translocation
movement of sugars through plant phloem to where they are needed
what is the pressure flow model
for sugar translocation, depends on how solute potential and pressure potential change as sugars move
at the source of pressure flow model
sugars move in phloem, high concentration of sugar creates low solute potential, which draws in water from xylem raising the pressure potential, pushing phloem sap toward sink via bulk flow
sugar source at start of growing season
roots
sugar source in the middle of growing season
mature leaves
at the sink of pressure flow model
sugars are removed, raising the solute potential, water exits the phloem and returns to the xylem, lowering the pressure potential
proton pumps in pressure flow model
use ATP to pump protons out of companion cells, form electrochemical gradient allows for proton-sucrose cotransporter to use the gradient to pull H+ back in along with sucrose against gradient
when sugar is moving down concentration gradient
sugar diffuses down its concentration gradient from the companion cell and into the phloem sieve-tube elements through the plasmodesmata
co transporters in pressure flow model
use energy of protons moving down their gradient to move sucrose against its gradient, symporters bring H+ and sucrose into companion cells
facilitated diffusion in pressure flow model
sucrose in companion cells, down gradient into sieve tube elements
if sink has lower sucrose concentration than the phloem
diffusion is sufficient for unloading
if sink has higher sucrose concentration than the phloem
active transport is required
driving force for fluid movement in xylem
transpiration from leaves, cohesion and tension of water (passive)
driving force for fluid movement in phloem
active transport of sucrose from source cells into phloem sieve tube (energy)
cells facilitating fluid movement in xylem
non-living vessel elements and tracheids
cells facilitating fluid movement in phloem
living sieve tube elements