Carbon Cycle etc... Flashcards
How do mineral ions in the soil move into the plant?
Diffusion: flow down a concentration gradient into root
Fungal hyphae: symbiotic relationship (fungus absorbs minerals for plant in exchange for sugars)
Mass flow: water flows into plant INTO high solute concentrations by osmosis (creates negative pressure in soil around root); minerals hydrogen bond to water and move passively with water into plant
ACTIVELY
*Protein pumps in root cells (lots of mitochondria) actively transport mineral ions against concentration gradient (like potassium ions) OR *Protein pumps actively pump H+ ions into surrounding soil (these bind to negatively charged ions in soil and diffuse back into root with H+ ions); displaces (forces out) positively charged minerals from clay so they can be absorbed (diffusion) into root cells – this is INDIRECT active transport
Root structure/function
Epidermis: protection; root hairs increase surface area for
absorption
Cortex: transports (diffusion) water/ ions to stele (vascular tissue)
Stele
Endodermis/ Casparian Strip: impermeable to water and
ions; controls rate of uptake – must be pumped
Pericycle/ cambium: lateral root development
Vascular bundle
Xylem (X-shaped; water and mineral ion transport from roots
to stems to leaves)
Phloem (phloem = more out/ surrounding xylem; sugar and
amino acid transport)
Dicots
Vascular bundles form a ring structure
Xylem is more internal in vascular bundle and more “porous” looking (phloem = outer)
Monocots
Vascular bundles are scattered
Xylem is more internal in vascular bundle and more “porous” looking
Why do stomata open/close?
When dehydrated, mesophyll cells release abscisic acid, causes guard
cells (around stomata) to LOSE potassium, water follows by osmosis,
decreasing water pressure/making guard cells flaccid = closing stomata
* K+ ions actively transported into guard cells, water follows by osmosis,
guard cells turgid = opens stomata
How does CO2 in air affect transpiration?
MORE CO2 in air = decreased transpiration (stomata do NOT need to be open as much to get CO2 in)
How does Translocation work?
Sugars (as sucrose)/ amino acids actively transported (companion cells) into phloem tissue (called sieve tubes - at leaves/ stems = SOURCE); water diffuses from xylem into phloem (creating sap); sap volume/ pressure drives sap downward (mass flow); companion cells actively transport organic molecules (sugar stored as starch) into “SINK” (fruit, seeds, roots) and water moves back into xylem (osmosis)
Sieve elements
long/narrow and joined together to form long tube; anucleate; thick/rigid cell walls to withstand high pressure; connected by sieve plates (have pores)
Companion Cells
loading and unloading of organic
compounds from sieve tubes; increased surface area; lots of
mitochondria and transport proteins; plasmodesmata (connect
cytoplasm to sieve elements)
Aphids
Used to calculate translocation rates.
Apical Meristems
Adds Vertical Growth
Primary Growth
Primary xylem and Phloem
New leaves and flowers
Lateral Meristems
Occurs at cambium
Lateral growth
Secondary growth
Secondary xylem and phloem
Produces bark on trees
Auxin
Inhibits lateral buds
Auxin changes patterns of gene expression
stimulates cell elongation
Used for phototropism
Pollination
Movement of pollen from anther to stigma
Fertilization
Fusion of haploid nuclei
PRACTICE DRAWING SEEDS AND FLOWERS
do it bro
Seed Germination
- Absorption of water – production of gibberellic acid (GA/ gibberellin)
- GA turns on genes that synthesize amylase
- Amylase hydrolyzes starch (into maltose)
- Maltose hydrolyzed for glucose (ATP) or polymerized for cellulose (cell wall formation)
- Cotyledons provide stored food for energy until leaves/photosynthesis
- Seed coat will eventually rupture and radicle (seed root) will emerge and grow into ground
Phytochrome
Pr converted to Pfr in the daylight
Pfr promotes flowering in long day plants
Pfr inhibits flowering in short day plants
Long day plants
Burst of light during night of short days
Detritivore
organisms that ingest nonliving organic matter/ feces (ingest THEN digest - earthworms)
Saprotrophs
organisms that live in/ on nonliving organic matter – secreting enzymes into it to digest it then absorb the digested products (digest THEN ingest – bacteria, fungi)
Saprotrophs recycle nutrients (complex organic compounds broken down into simple, inorganic substances which go back into the soil/ water/ atmosphere) in ecosystems for autotrophs to use to make organic compounds again - heterotrophs also release inorganic substances back into the environment as a byproduct of metabolic reactions/ processing organic compounds (cellular respiration releases CO2)
Carbon Cycle
Photosynthesis: CO2 removed from
atmosphere/ water by plants; “fixed” to make organic compounds (sugars, proteins, lipids) = largest flux
Feeding: Heterotrophs obtain organic
compounds by feeding
Cellular respiration: Organisms
breakdown organic compounds to
release energy (and release CO2 and heat
as byproducts)
Decomposition (aerobic):
Saprotrophs break down organic material
and release CO2 (and carbon to soil, air, etc.)
-Decomposition (anaerobic):
Methanogenic archaeans breakdown organic
compounds and release methane (CH4) which forms deposits underground or is oxidized to CO2 and H2O in atmosphere
Saprotrophs inhibited by anaerobic conditions and organic acids produced in anaerobic conditions (lower pH) and organic matter not fully decomposed forms peat (in waterlogged soils) - compressed peat can form COAL (fossil fuel)
Combustion: Burning of fossil fuels/ biofuels releases CO2 into atmosphere (significant increases in CO2 in atmosphere)
Bodies of Water (largest carbon sinks): CO2 dissolves in bodies of water (diffusion) and combines with H2O to form carbonic acid. Carbonic acids dissociates into carbonate ions and hydrogen ions. Hydrogen ions lower pH (acidic). Carbonate ions used by molluscs and corals for shells/ exoskeletons (which can compact to form limestone rock). Increased temps and lower pH cause corals to expel symbiotic algae (bleaching) and cause LESS carbonate ions to be incorporated into shells and exoskeletons so they are weaker too.
Sustainable Ecosystems
To be sustainable over LONG periods of time, ecosystems must have:
-Energy availability (light source/ sun)
-Nutrient availability (decomposers) - recycling of carbon, nitrogen, oxygen etc.
-Waste recycling/ Water
Greenhouse gases
Absorb IR radiation
Trap and re-emit heat, warming earth