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Chapter 29- Resource Acquisition, Nutrition, and Transport in Vascular Plants Following the Big Ideas Energy and Homeostasis- Acquisition of water and nutrients by plants involve specialized mechanisms and structures. Overview: Underground Plants The success of plants depends on their ability to gather and conserve resources from their environment The transport of materials is central to the integrated functioning of the whole plant Stone plants (Lithops) are adapted to life in the desert Two succulent leaf tips are exposed above ground; the rest of the plant lives below ground Concept 29.1: Adaptations for acquiring resources were key steps in the evolution of vascular plants The evolution of adaptations enabling plants to acquire resources from both above and below ground sources allowed for the successful colonization of land by vascular plants The algal ancestors of land plants absorbed water, minerals, and CO2 directly from surrounding water Early nonvascular land plants lived in shallow water and had aerial shoots Natural selection favored taller plants with flat appendages, multicellular branching roots, and efficient transport Transport in plants-The evolution of xylem and phloem in land plants made possible the development of extensive root and shoot systems that carry out long-distance transport H2O & minerals transport in xylem transpiration evaporation, adhesion & cohesion negative pressure (tension) Sugars transport in phloem bulk flow Calvin cycle in leaves loads sucrose into phloem positive pressure Gas exchange photosynthesis CO2 in; O2 out stomates respiration O2 in; CO2 out roots exchange gases within air spaces in soil Why does over-watering kill a plant? Shoot Architecture and Light Capture Stems serve as conduits for water and nutrients and as supporting structures for leaves Shoot height and branching pattern affect light capture There is a trade-off between growing tall and branching Phyllotaxy, the arrangement of leaves on a stem, is specific to each species Most angiosperms have alternate phyllotaxy with leaves arranged in a spiral The angle between leaves is 137.5 and likely minimizes shading of lower leaves Figure 29.3 42 16 34 21 19 27 6 14 Shoot apical meristem 26 5 18 31 11 40 3 8 13 Buds 32 24 29 10 23 28 7 20 22 9 4 2 15 1 17 12 25 1 mm Emerging phyllotaxy of Norway spruce The productivity of each plant is affected by the depth of the canopy, the leafy portion of all the plants in the community Shedding of lower shaded leaves when they respire more than photosynthesize, selfpruning, occurs when the canopy is too thick Leaf orientation affects light absorption In low-light conditions, horizontal leaves capture more sunlight In sunny conditions, vertical leaves are less damaged by sun and allow light to reach lower leaves Root Architecture and Acquisition of Water and Minerals Soil is a resource mined by the root system Root growth can adjust to local conditions For example, roots branch more in a pocket of high nitrate than in a pocket of low nitrate Roots are less competitive with other roots from the same plant than with roots from different plants Roots and the hyphae of soil fungi form mutualistic associations called mycorrhizae Concept 29.2: Different mechanisms transport substances over short or long distances- The Apoplast and Symplast: Transport Continuums The apoplast consists of everything external to the plasma membrane It includes cell walls, extracellular spaces, and the interior of vessel elements and tracheids The symplast consists of the cytosol of the living cells in a plant, as well as the plasmodesmata Three transport routes for water and solutes are The apoplastic route, through cell walls and extracellular spaces The symplastic route, through the cytosol The transmembrane route, across cell walls Figure 29.4 Cell wall Apoplastic route Cytosol Symplastic route Transmembrane route Key Plasmodesma Plasma membrane Apoplast Symplast Short-Distance Transport of Solutes Across Plasma Membranes Plasma membrane permeability controls short-distance movement of substances Both active and passive transport occur in plants In plants, membrane potential is established through pumping H by proton pumps In animals, membrane potential is established through pumping Na by sodiumpotassium pumps Figure 29.5 Solute transport across plant cell plasma membranes EXTRACELLULAR FLUID H Hydrogen ion H H CYTOPLASM H H H Proton pump H H S H H H H H H H H H H H H/sucrose cotransporter (a) H and membrane potential Sucrose (neutral solute) (b) H and cotransport of neutral solutes H H H H H H/NO3− cotransporter H H Nitrate H H Potassium ion K K H (c) H and cotransport of ions K H K K K K Ion channel (d) Ion channels Plant cells use the energy of H+ gradients to cotransport other solutes by active transport Plant cell membranes have ion channels that allow only certain ions to pass Short-Distance Transport of Water Across Plasma Membranes To survive, plants must balance water uptake and loss Osmosis determines the net uptake or water loss by a cell and is affected by solute concentration and pressure © 2014 Pearson Education, Inc. Water potential is a measurement that combines the effects of solute concentration and pressure Water potential determines the direction of movement of water Water flows from regions of higher water potential to regions of lower water potential Potential refers to water’s capacity to perform work Water potential is abbreviated as and measured in a unit of pressure called the megapascal (MPa) 0 MPa for pure water at sea level and at room temperature How Solutes and Pressure Affect Water Potential Both pressure and solute concentration affect water potential This is expressed by the water potential equation: S P The solute potential (S) of a solution is directly proportional to its molarity Solute potential is also called osmotic potential Pressure potential (P) is the physical pressure on a solution Turgor pressure is the pressure exerted by the plasma membrane against the cell wall, and the cell wall against the protoplast The protoplast is the living part of the cell, which also includes the plasma membrane Figure 29.6 Initial flaccid cell: 0.4 M sucrose solution: Plasmolyzed cell at osmotic equilibrium with its surroundings P 0 S −0.9 −0.9 MPa P 0 S −0.7 −0.7 MPa Pure water: P 0 S 0 0 MPa P 0 S −0.9 −0.9 MPa (a) Initial conditions: cellular environmental Turgid cell at osmotic equilibrium with its surroundings P 0.7 S −0.7 0 MPa (b) Initial conditions: cellular environmental Long-Distance Transport: The Role of Bulk Flow Efficient long-distance transport of fluid requires bulk flow, the movement of a fluid driven by pressure Water and solutes move together through tracheids and vessel elements of xylem and sieve-tube elements of phloem Efficient movement is possible because mature tracheids and vessel elements have no cytoplasm, and sieve-tube elements have few organelles in their cytoplasm Concept 29.3: Plants roots absorb essential elements from the soil Water, air, and soil minerals contribute to plant growth 80–90% of a plant’s fresh mass is water 96% of plant’s dry mass consists of carbohydrates from the CO2 assimilated during photosynthesis 4% of a plant’s dry mass is inorganic substances from soil Macronutrients and Micronutrients More than 50 chemical elements have been identified among the inorganic substances in plants, but not all of these are essential to plants There are 17 essential elements, chemical elements required for a plant to complete its life cycle Soil Management Ancient farmers recognized that crop yields would decrease on a particular plot over the years Soil management, by fertilization and other practices, allowed for agriculture and cities In natural ecosystems, nutrients are recycled through decomposition of feces and humus, dead organic material Soils can become depleted of nutrients as plants and the nutrients they contain are harvested Fertilization replaces mineral nutrients that have been lost from the soil Adjusting Soil pH Soil pH affects cation exchange and the chemical form of minerals Cations are more available in slightly acidic soil, as H+ ions displace mineral cations from clay particles The availability of different minerals varies with pH For example, at pH 8 plants can absorb calcium but not iron At present, 30% of the world’s farmland has reduced productivity because of soil mismanagement Soil Texture Soil particles are classified by size; from largest to smallest they are called sand, silt, and clay Topsoil is formed when mineral particles released from weathered rock mix with living organisms and humus Soil solution consists of water and dissolved minerals in the pores between soil particles After a heavy rainfall, water drains from the larger spaces in the soil, but smaller spaces retain water because of its attraction to clay and other particles Loams are the most fertile topsoils and contain equal amounts of sand, silt, and clay Topsoil Composition A soil’s composition refers to its inorganic (mineral) and organic chemical components Inorganic components of the soil include positively charged ions (cations) and negatively charged ions (anions) Most soil particles are negatively charged Anions (for example, NO3–, H2PO4–, SO42–) do not bind with negatively charged soil particles and can be lost from the soil by leaching Cations (for example, K, Ca2, Mg2) adhere to negatively charged soil particles; this prevents them from leaching out of the soil through percolating groundwater During cation exchange, cations are displaced from soil particles by other cations Displaced cations enter the soil solution and can be taken up by plant roots Figure 29.10 Soil particle K K 2 Ca K Mg 2 Ca2 H H2O CO2 H2CO3 HCO3− H Root hair Cell wall Organic components of the soil include decomposed leaves, feces, dead organisms, and other organic matter, which are collectively named humus Humus forms a crumbly soil that retains water but is still porous It also increases the soil’s capacity to exchange cations and serves as a reservoir of mineral nutrients Living components of topsoil include bacteria, fungi, algae and other protists, insects, earthworms, nematodes, and plant roots These organisms help to decompose organic material and mix the soil Concept 29.4: Plant nutrition often involves relationships with other organisms Plants and soil microbes have a mutualistic relationship Dead plants provide energy needed by soildwelling microorganisms Secretions from living roots support a wide variety of microbes in the near-root environment Soil bacteria exchange chemicals with plant roots, enhance decomposition, and increase nutrient availability Rhizobacteria The soil layer surrounding the plant’s roots is the rhizosphere Rhizobacteria thrive in the rhizosphere, and some can enter roots The rhizosphere has high microbial activity because of sugars, amino acids, and organic acids secreted by roots Rhizobacteria known as plant-growth-promoting rhizobacteria can play several roles Produce hormones that stimulate plant growth Produce antibiotics that protect roots from disease Absorb toxic metals or make nutrients more available to roots Bacteria in the Nitrogen Cycle Nitrogen can be an important limiting nutrient for plant growth The nitrogen cycle transforms atmospheric nitrogen and nitrogen-containing compounds Plants can only absorb nitrogen as either NO3– or NH4 Most usable soil nitrogen comes from actions of soil bacteria Figure 29.11 ATMOSPHERE N2 SOIL N2 N2 ATMOSPHERE Proteins from humus (dead organic material) SOIL Nitrogen-fixing bacteria NH3 (ammonia) H (from soil) Microbial decomposition Amino acids Denitrifying bacteria Ammonifying NH4 (ammonium) bacteria NO2− Nitrifying (nitrite) Nitrifying bacteria bacteria Nitrate and nitrogenous organic compounds exported in xylem to shoot system NH4 NO3− (nitrate) Root Conversion to NH4+ Ammonifying bacteria break down organic compounds and release ammonium (NH4+) Nitrogen-fixing bacteria convert N2 gas into NH3 NH3 is converted to NH4+ Conversion to NO3– Nitrifying bacteria oxidize NH4+ to nitrite (NO2–) then nitrite to nitrate (NO3–) Different nitrifying bacteria mediate each step Nitrogen is lost to the atmosphere when denitrifying bacteria convert NO3– to N2 Bacterial root nodules Found on roots of legumessymbiotic relationship! Inside the root nodule, Rhizobium bacteria assume a form called bacteroids, which are contained within vesicles formed by the root cell The plant obtains fixed nitrogen from Rhizobium, and Rhizobium obtains sugar and an anaerobic environment Each legume species is associated with a particular strain of Rhizobium Mycorrhizae increase absorption The hyphae of mycorrhizal fungi extend into soil, where their large surface area and efficient absorption enable them to obtain mineral nutrients, even if these are in short supply or are relatively immobile. Mycorrhizal fungi seem to be particularly important for absorption of phosphorus, a poorly mobile element, and a proportion of the phosphate that they absorb has been shown to be passed to the plant. Mycorrhizae Symbiotic relationship between fungi & plant symbiotic fungi greatly increases surface area for absorption of water & minerals increases volume of soil reached by plant increases transport to host plant Epiphytes, Parasitic Plants, and Carnivorous Plants Some plants have nutritional adaptations that use other organisms in nonmutualistic ways Three unusual adaptations are Epiphytes Parasitic plants Carnivorous plants Epiphytes grow on other plants and obtain water and minerals from rain, rather than tapping their hosts for sustenance Parasitic plants absorb water, sugars, and minerals from their living host plant Some species also photosynthesize, but others rely entirely on the host plant for sustenance Some species parasitize the mycorrhizal hyphae of other plants Carnivorous plants are photosynthetic but obtain nitrogen by killing and digesting mostly insects Figure 29.15a Staghorn fern, an epiphyte Figure 29.15b Parasitic plants Mistletoe, a photosynthetic parasite Dodder, a nonphotosynthetic parasite (orange) Indian pipe, a nonphotosynthetic parasite of mycorrhizae Figure 29.15c Carnivorous plants Sundew Pitcher plants Venus flytraps Concept 29.5: Transpiration drives the transport of water and minerals from roots to shoots via the xylem Plants can move a large volume of water from their roots to shoots Most water and mineral absorption occurs near root tips, where root hairs are located and the epidermis is permeable to water Root hairs account for much of the absorption of water by roots After soil solution enters the roots, the extensive surface area of cortical cell membranes enhances uptake of water and selected minerals The concentration of essential minerals is greater in the roots than in the soil because of active transport Water flow through root Porous cell wall water can flow through cell wall route & not enter cells plant needs to force water into cells Casparian strip Controlling the route of water in root Endodermis cell layer surrounding vascular cylinder of root lined with impermeable Casparian strip forces fluid through selective cell membrane filtered & forced into xylem cells Water & mineral absorption Water absorption from soil osmosis aquaporins Mineral absorption active transport proton pumps active transport of H+ aquaporin root hair proton pumps H2O Mineral absorption Proton pumps active transport of H+ ions out of cell chemiosmosis H+ gradient creates membrane potential difference in charge drives cation uptake creates gradient cotransport of other solutes against their gradient Transport in Plants Transpiration pull-cohesion tension theory states that for every molecule of water evaporated from the leaf, another molecule is drawn in at the root 2006-2007 Pulling Xylem Sap: The Cohesion-Tension Hypothesis According to the cohesion-tension hypothesis, transpiration and water cohesion pull water from shoots to roots Xylem sap is normally under negative pressure, or tension Transpirational pull is generated when water vapor in the air spaces of a leaf diffuses down its water potential gradient and exits the leaf via stomata As water evaporates, the air-water interface retreats farther into the mesophyll cell walls and becomes more curved Due to the high surface tension of water, the curvature of the interface creates a negative pressure potential This negative pressure pulls water in the xylem into the leaf The pulling effect results from the cohesive binding between water molecules The transpirational pull on xylem sap is transmitted from leaves to roots Ascent of xylem fluid Transpiration pull generated by evaporation from the leaf Cohesion and adhesion in the ascent of xylem sap: Water molecules are attracted to each other through cohesion Cohesion makes it possible to pull a column of xylem sap Water molecules are attracted to hydrophilic walls of xylem cell walls through adhesion Adhesion of water molecules to xylem cell walls helps offset the force of gravity Thick secondary walls prevent vessel elements and tracheids from collapsing under negative pressure Drought stress or freezing can cause cavitation, the formation of a water vapor pocket by a break in the chain of water molecules Xylem Sap Ascent by Bulk Flow: A Review Bulk flow is driven by a water potential difference at opposite ends of xylem tissue Bulk flow is driven by evaporation and does not require energy from the plant; like photosynthesis, it is solar powered Bulk flow differs from diffusion It is driven by differences in pressure potential, not solute potential It occurs in hollow dead cells, not across the membranes of living cells It moves the entire solution, not just water or solutes It is much faster Concept 29.6: The rate of transpiration is regulated by stomata Leaves generally have broad surface areas and high surface-to-volume ratios These characteristics increase photosynthesis and increase water loss through stomata Guard cells help balance water conservation with gas exchange for photosynthesis About 95% of the water a plant loses escapes through stomata Each stoma is flanked by a pair of guard cells, which control the diameter of the stoma by changing shape Stomatal density is under genetic and environmental control Control of Stomates Uptake of K+ ions by guard cells Guard cell proton pumps create a membrane potential that drives the uptake of K+ ions from epidermal cell surrounding the guard cells water enters by osmosis guard cells become turgid Loss of K+ ions by guard cells Epidermal cell water leaves by osmosis guard cells become flaccid H2O K+ H2O K+ Nucleus Chloroplasts H2O K+ H2O K+ K+ H2O K+ H2O K+ H2O K+ H2O Thickened inner cell wall (rigid) H2O K+ H2O K+ H2O K+ H2O K+ Stoma open Stoma closed water moves into guard cells water moves out of guard cells Blue light causes stomates to open Control of transpiration Balancing stomate function always a compromise between photosynthesis & transpiration leaf may transpire more than its weight in water in a day…this loss must be balanced with plant’s need for CO2 for photosynthesis Stimuli for Stomatal Opening and Closing Generally, stomata open during the day and close at night to minimize water loss Stomatal opening at dawn is triggered by Blue Light CO2 depletion An internal “clock” in guard cells All eukaryotic organisms have internal clocks; circadian rhythms are 24-hour cycles Drought stress can cause stomata to close during the daytime The hormone abscisic acid (ABA) is produced in response to water deficiency and causes the closure of stomata Osmoregulation in Hydrophytes (Aquatic plants) poorly developed root systems and supportive xylem tissues no stomata (for submerged leaves) thin & finely divided leaves no cuticle Adaptations That Reduce Evaporative Water Loss Xerophytes are plants adapted to arid climates Some desert plants complete their life cycle during the rainy season Others have leaf modifications that reduce the rate of transpiration Some plants use a specialized form of photosynthesis called crassulacean acid metabolism (CAM) where stomatal gas exchange occurs at night © 2014 Pearson Education, Inc. Figure 29.20 Oleander (Nerium oleander) Thick cuticle Upper epidermal tissue 100 m Ocotillo (Fouquieria splendens) Trichomes Crypt Stoma Lower epidermal tissue (“hairs”) Old man cactus (Cephalocereus senilis) Osmoregulation- Plant Responses to Water Limitations Wilting or curling leaves reduces sunlight exposure and water evaporation Stomata are on the underside of the leaf, thick waxy cuticle is on the top Adaptations like needles and fat photosynthesizing stems that store water Deep tap roots or shallow fibrous roots Hairs or scales on leaves that reduce wind evaporation Pits on underside of leaf where stomata are to reduce water loss by raising water potential around stoma area Thick fleshy leaves that store water Small leaves Stomata that only open at night Multiple layered epidermis and small intercellular spaces Concept 29.7: Sugars are transported from sources to sinks via the phloem The products of photosynthesis are transported through phloem by the process of translocation In angiosperms, sieve-tube elements are the conduits for translocation Phloem sap is an aqueous solution that is high in sucrose It travels from a sugar source to a sugar sink A sugar source is an organ that is a net producer of sugar, such as mature leaves A sugar sink is an organ that is a net consumer or storer of sugar, such as a tuber or bulb A storage organ can be both a sugar sink in summer and sugar source in winter Sugar must be loaded into sieve-tube elements before being exported to sinks Depending on the species, sugar may move by symplastic or both symplastic and apoplastic pathways Companion cells enhance solute movement between the apoplast and symplast In most plants, phloem loading requires active transport Proton pumping and cotransport of sucrose and H+ enable the cells to accumulate sucrose At the sink, sugar molecules diffuse from the phloem to sink tissues and are followed by water Sometimes there are more sinks than can be supported by sources Self-thinning is the dropping of sugar sinks such as flowers, seeds, or fruits Transport of sugars in phloem Loading of sucrose into phloem flow through cells via plasmodesmata proton pumps cotransport of sucrose into cells down proton gradient Pressure flow in phloem Bulk flow hypothesis “source to sink” flow direction of transport in phloem is dependent on plant’s needs phloem loading active transport of sucrose into phloem increased sucrose concentration decreases H2O potential water flows in from xylem cells increase in pressure due to increase in H2O causes flow Vessel (xylem) Sieve Source cell tube (leaf) 1 Loading of sugar (phloem) H2O Bulk flow by negative pressure Pressure Flow: The Mechanism of Translocation in Angiosperms Phloem sap flows from source to sink at rates as great as 1 m/hr, much too fast to be accounted for by either diffusion or cytoplasmic streaming. In studying angiosperms, researchers have concluded that sap moves through a sieve tube by bulk flow driven by positive pressure (thus the synonym pressure flow. The building of pressure at the source end and reduction of that pressure at the sink end cause water to flow from source to sink, carrying the sugar along. Xylem recycles the water from sink to source. The pressure flow hypothesis explains why phloem sap always flows from source to sink. Sucrose H2O 1 2 Bulk flow by positive pressure Figure 29.22 2 Uptake of water 3 Unloading of sugar Sink cell (storage root) 3 4 H2O 4 Recycling of water Sucrose can flow 1m/hr Experimentation Testing pressure flow hypothesis using aphids to measure sap flow & sugar concentration along plant stem Maple sugaring Connecting the Concepts With the Big Ideas Energy and Homeostasis Plants depend on water’s special properties of adhesion and cohesion to accomplish movement of water via transpiration pull when stomata are open. Plants employ stomata and root hairs to facilitate gas exchange. Negative feedback allows plants to regulate their transpiration based on water availability Related methods of osmoregulation are used throughout the plant kingdom, showing their common ancestry. Important cooperative relationships that assist plants in their acquisition of nutrients include mycorrhizae and bacterial root nodules.