Lect_note#2_Plant_Nutrient_MRQ_2011 _Long-Distance Transport in the Xylem and Phloem
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Transcript of Lect_note#2_Plant_Nutrient_MRQ_2011 _Long-Distance Transport in the Xylem and Phloem
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Long-Distance Transport
in the Xylem and Phloem
Mochammad Roviq, 2011
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Concept The long-distance transport of water and
solutes - mineral elements and low-molecularweight organic compounds - takesplace in the vascular system of xylem and
phloem. Long-distance transport from the roots to the
shoots occurs predominantly in the nonlivingxylem vessels.
Coniferous trees lack the continuous systemof xylem vessels, and depend on tracheides
which are non-living conducting cells rangingin length from 2 to 6 mm.
In annual plant species too long-distancetransport in the xylem vessels may beinterrupted by tracheides, for example at the
root-shoot junction or in the nodes of thestem.
These structures pose an internal resistanceto xylem volume flow but simultaneouslypermit an intensive xylem phloem solutetransfer
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Root pressure
Xylem transport is driven by thegradient in hydrostatic pressure(root pressure) and by the gradientin the water potential
The gradient in water potentialbetween roots and shoots is quitesteep particularly during the daywhen the stomata are open.
Values become less negative in the
following sequence: atmosphere leaf cells > xylem sap > root cells >external solution
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Direction of long-distance
transport
Solute flow in the xylem from theroots to the shoots is thereforeunidirectional
Under certain conditions in the shoots
a counterflow of water in the xylemmay also occur, for example, fromlow-transpiring fruits back to theleaves
Long-distance transport in the phloem
takes place in the living sieve tubecells and is bidirectional.
The direction of transport isdetermined primarily by thenutritional requirements of the
various plant organs or tissues andoccurs, therefore, from source to sink
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Transfer cells
During long-distancetransport, mineralelements and organicsolutes are transferred
between the xylem andphloem by extensiveexchange processes,referred to as loading andunloading.
The transfer is mediated byspecific cells called transfercells
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Transfer cells are specialised
parenchymal cells. They are different from
the other cells of theplant structure in that,they are concerned withtransport of solutes.
They are present in highnumbers whereveractive absorption andsecretion are evident.
They are mostly found inthe close conjunction
with vascular cambialcells i.e., xylem andphloem
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Composition of the Xylem Sap
Depend on factors such as plant species, mineralelement supply to the roots, assimilation ofmineral nutrients in the roots and nutrient
recycling. Composition and particularly concentration of
solutes are also strongly influenced by the degreeof dilution by water and are therefore dependent
on the transpiration rate and the time of day. Composition and concentration of xylem sap also
change typically during the ontogenesis of plants
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Xylem Volume Flow (Pressurized Exudation at 100 kPa) and Mineral
Element Concentrations in the Xylem Sap of Soil-Grown Nodulated
Soybean During Reproductive Stage
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Exchange Adsorption and Resorption
The interactions between cations are similar to those inthe AFS of the root cortex .
The degree of retardation (penghambatan) of cationtranslocation depends on the valency of the cation (Ca2+>
K
+
), its own activity, the activity of competing cations, thecharge density of the negative groups (dicots > monocots),the pH of the xylem sap which may vary between 5 and 7and the diameter of the xylem vessels.
The translocation rate in the xylem of heavy metal cationsis much enhanced when the ions are complexed, forexample, in the case of copper, zinc or cadmium
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Resorption
Solutes can also be resorbed from the xylem(apoplasm) into the living cells (transport in thecytoplasm and vacuole) along the pathway of thexylem sap from the roots to the leaves
Resorption from the xylem can be the result either oftransient or permanent storage in the xylemparenchyma and other stem tissue, or of xylem-phloem transfer, mediated by specialized cells (xylemparenchyma transfer cells)
The resorption of certain mineral elements from thexylem sap is very pronounced and can have importantconsequences for the mineral nutrition of these plants
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Natrophobic or natrophilic plant species
Na+ is retained mainly in the roots and lowerstem (Phaseolus vulgaris), whereas in natrophilicspecies (e.g. sugar beet) translocation into theleaves readily occurs
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Resorspsi unsur mikro
Resorpsi dari cairan xilem di akar dan batang juga dapat
menjadi faktor penentu dalam distribusi unsur mikro pada
tanaman.
Sehingga ketika pasokan
molibdenum dalammedium hara tinggi, pada
tomat terjadi keracunan
jauh lebih awal daripada
kacang atau bungamatahari
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Release or Secretion
Komposisi cairan xilem di sepanjangjalur transportasi juga dapat berubaholeh pelepasan atau sekresi zat terlarutdari sel-sel di sekitarnya.
Misalnya, nonlegum yang diberi nitrat,konsentrasi nitrat di cairan xilemmenurun sejalan dengan semakinpanjang jalur, sedangkan konsentrasinitrogen organik, khususnya glutaminmeningkat
Dalam legum yang bernodulasi (di manaterjadi fiksasi N2), di sisi lain, rasioamida dengan asam amino bergesermendukung asam amino
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Xylem Unloading in Leaves
Meskipun terjadi resorpsi sepanjang jalur di batang, sebagianbesar zat terlarut dan air diangkut pembuluh xilem ke daun.
Air diangkut dalam pembuluh utama ke bagian yang
mengalami penguapan cepat seperti tepi daun
Konsentrasi zat terlarutdapat naik dibagian
tertentu, misalnya, tepi
daun, tergantung pada
konsentrasi dan komposisi
larutan dalam cairan xilem
yang masuk daun, laju
kehilangan air melalui
transpirasi, dan panjang
jalur yang melalui daun
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Precipitation..
Pencegahan akumulasi zat terlarut yang
berlebihan dalam apoplasm daun dapat
dicapai dengan pembentukan garam low
solubility di apoplasm, terutama untuk
menghilangkan kalsium larut dalamgymnosperms
This mechanism of precipitation
seems to be a safe way of coping with
a continuous xylem import of calcium
which is scarcely exported in the
phloem and where the ionic
concentrations in the symplasm have
to be kept very low.
Calcium oxalate crystals in the
apoplasm of needles. (Left) Micrograph
from the phloem of a needle from
Juniperus chinensis; (right) micrograph
of a stomatal pore of a needle from
Picea abies (L.) Karst.
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Model for scavenging solutes from the xylem sap
(xylem unloading') in leaf cells.
The cells of the bundlesheath are sites of intensivenet proton excretion whichacidifies the apoplasm the
proton gradient across theplasma membrane acting asthe driving force forcotransport of amino acidsand ureides.
The activity of the protonpump in legumes is highbefore pod filling anddisappears during podformation
As- amino acids.
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Effect of Transpiration
Rate on Uptake and
Translocation
Tingkat fluks air di akar(transportasi jarak pendek) dan
di dalam pembuluh xilem(transportasi jarak jauh)ditentukan oleh tekanan akardan laju transpirasi.Peningkatan tingkat transpirasimungkin, atau tidak mungkin,
meningkatkan serapan dantranslokasi unsur mineral dalamxilem tersebut. Peningkatandapat dicapai dengan berbagaicara
A. 'Passive' transport of mineral elements through
the apoplasm into the stele. B. More rapid removal
of mineral elements released into the xylem vessels
. C. Increase in the mass flow of the external
solution to the rhizoplane and eventually into the
apparent free space of the cortex, favoring active
uptake into the symplasm. E, Endodermis; X, xylem;
arrow, water flux (A to C see text).
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Predominantly factors of uptake and
translocation rate:
1. Plant age. In seedlings and young plants witha low leaf surface area, enhancementeffectsof transpiration are usually absent; wateruptake and solute transport in the xylem tothe shoots are determined mainly by the root
pressure. As the age and size of the plantsincrease, the relative importance of thetranspiration rate, particularly for thetranslocation of mineral elements increases.
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2. Time of day
In leaves up to 90% of the total transpiration isstomatal. During the light period, transpiration ratesand thus the potential enhancement of uptake andtranslocation of mineral elements are much higher
than during the dark period.
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4. Type of mineral element. Under otherwisecomparable conditions (e.g. plant age andexternal concentration), the effect of
transpiration rates on the uptake and transportfollows a typically defined ranking order ofmineral elements.
transpirasi meningkatkan penyerapan dan
translokasi molekul tak bermuatan ke tingkatyang lebih besar daripada ion.
Ada hubungan erat antara tingkat transpirasi dantingkat penyerapan herbisida tertentu
translocation rate
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Measured and Calculated Silicon Uptake inRelation to Transpiration (Water Consumption)
of Oat Plants
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Effect of Transpiration Rate on
Distribution within the Shoot
The long-distance transport of a mineral elementexclusively in the xylem should be expected togive a distinct distribution pattern in the shootorgans that depends on both transpiration rates
(e.g., ml g-1 dry weight each day) and duration oftranspiration (e.g. age of the organ).
For example, manganese (where at the sameplant (maple tree) and similar leaf age the *sun
leaves' (high transpiration rates) have muchhigher manganese contents in their dry matterthan 'shade leaves' (low transpiration rates).
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Increasing supply
The distribution of boron is alsorelated to the loss of water
from the shoot organ, as shownby the boron distribution inshoots of rape in response toan increasing boron supply
The typical gradient in thetranspiration rates in the shootorgans (leaves > pods seeds)corresponds to the gradient inboron content.
Effect of increasing boron
application to the soil on the
distribution of boron in the
shoots of rape
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II. Phloem Transport
Principles of Transport and Phloem Anatomy
Composition of the Phloem Sap
Mobility in the Phloem Transfer between the Xylem and Phloem
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Principles of Transport and Phloem
Anatomy
Long-distance transport inthe phloem takes place inliving cells, the sieve
tubes The principles of the
transport mechanism inthe phloem wereproposed as early as 1930by Munch inpressure
flow hypothesis(Druckstromtheorie)based on the principle ofthe osmometer.
Cross-sectional area of a vascular bundle from
the stem of maize. Inset: sieve tube with sieve
plate pores and T-protein'. (From Eschrich,
1976.)
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Release or unloading at the sink
Munch suggested that solutessuch as sucrose areconcentrated in the phloem ofleaves (i.e.,phloem loading) andthe water is sucked into thephloem, creating a positiveinternal pressure.
This pressure induces a massflow in the phloem to the sitesof lower positive pressurecaused by removal of solutes
from the phloem. Flow rate and direction of flow
are therefore closely related tothe release or unloading at thesink.
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Munchpressure flow hypothesis
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This type ofpressure-driven mass flow in thephloem differs from thatin the xylem in three
important ways: (a)Organic compounds arethe dominant solutes inthe phloem sap; (b)transport takes place in
living cells; and (c) theunloading of solutes atthe sink plays animportant role.
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Source-sink regulated transport
An example for a primarilysource-sink regulated transportof a mineral nutrient is shownin for phosphorus.
After application to one of the
two mature primary leaves,the labelled phosphorus istransported to the shoot apexand the roots whereastransport to the other primary
leaf is negligible. In contrast, sodium is not
transported to the shoot apexbut exclusively movesdownwards (basipetally) to the
Retranslocation of labeled phosphorus
(P) and sodium (Na) after application to
the tip of a primary leaf of bean.
Autoradiogram, 24 h after application.
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Composition of the Phloem Sap
Phloem sap has a high pH (7-8) and contains highconcentrations of solutes, on average 15-25% dry matter.
The main component is usually sucrose, which maycomprise up to 90% of the solids. The proportion of sucroseto other solutes depends on the site of phloem sapcollection, it is very high, for example near the ear ofcereals
In addition to sucrose, among the other organic solutesamino acids are usually present in high concentrations theamides glutamine and asparagine may represent up to 90%of this fraction, whereas the concentrations of nitrate andammonium are usually very low
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Comparison of the Levels of Organic and Inorganic Solutes in the
Phloem and Xylem Exudates ofNicotiana glauca
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Mobility in the Phloem
The classification is, ofcourse, only a firstapproximation as certain
factors are ignored, forexample, genotypicaldifferences or the nutritionalstatus of plants.
For the macronutrients,
except calcium (phloemmobility is generally high,and for the micronutrients itis at least intermediate withthe exception of manganese.
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Transfer between the Xylem and
Phloem
In the vascularbundles, phloem andxylem are separated
by only a few cells(Lihat gambarsebelumnya).
In the regulation oflong-distancetransport, exchange
of solutes betweenthe two conductingsystems is veryimportant
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Water and solute flow
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Transfer from xylem to phloem
Dari perbedaan konsentrasi yang ditampilkan didalamnya adalah jelas bahwa transfer dari floemke xilem dapat terjadi downhill, melalui membranplasma dari tabung saringan, jika sebuah gradien
konsentrasi yang cukup ada. Sebaliknya, bagi sebagian besar zat terlarut
organik dan anorganik ditransfer dari xilem kefloem biasanya merupakan uphill transport
melawan gradien konsentrasi antara apoplasm(xilem) dan symplasm sel xilem sekitar parenkimdan sel-sel floem
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Higher demand
The xylem-to-phloem transfer is ofparticular importance for themineral nutrition of plants,because xylem transport isdirected mainly to the sites(organs) of highest transpiration,which are usually not the sites ofhighest demand for mineralnutrients.
This transfer of organic and
inorganic solutes can take place allalong the pathway from roots toshoot, and the stem plays animportant role in this respect mostlikely via transfer cells
Long-distance transport in xylem (X)
and phloem (P) in a stem with a
connected leaf, and xylem-to-phloem
transfer mediated by a transfer cell (T).
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Mineral Nutrients with High Phloem
Mobility
For mineral nutrients withhigh phloem mobility suchas potassium, phosphorus
or nitrogen as amino-N therelative importance ofphloem and xylemtransport into an organmainly depends on thestage of development of
the organ as shown in foramino-N during the life ofan individual leaf.
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Mineral Nutrients of Low Phloem
Mobility; Example Calcium
Because of its low concentrations in the phloem sap (Section 3.3.2)the import of calcium into growth sinks such as shoot apices, youngleaves or fruits takes place nearly exclusively in the xylem, whereas
the import in the phloem is negligible as shown for castor bean inTable 3.11. This is in marked contrast to potassium of which most(terminal bud) and at least half (youngest leaves) of the total netimport takes place in the phloem. For magnesium phloem importcontributes to 25 and 40% of the total import, respectively.
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Environmental Factors
To increase thecalcium contentof growing leavesor fruits,
increasing thetranspirationrates of the fruitsis more effective
than increasingthe calciumsupply in thesubstrate
Effect of Environmental Factors and Growth Rate
on Calcium and Potassium Content of Red Pepper
Fruits
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Root pressure
High root pressure, as indicated by the intensity
of guttation, is closely correlated with an
increased concentration of calcium in expanding
leaves and either the absence of, or only mildsymptoms of, calcium deficiency (tip necrosis).
Magnesium, which is highly phloem mobile, is
only slightly affected by root pressure. Root pressure also strongly depends on root
respiration and oxygen supply to the roots.
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Guttation
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Retranslocation and Cycling of
Nutrients
With exception of calcium and presumably also
manganese, import of nutrients in the xylem and
export (retranslocation) in the phloem is a normal
feature throughout the life of an individual leaf. Several pieces of evidence indicate a rapid xylem-
to-phloem transfer in the leaf blades and
involvement of only a small fraction of the totalleaf content ('cycling' fraction;) in this process.
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Between 82 and 100% of theexported mineral elementsare retranslocated in thephloem back to the roots, anda high proportion of thepotassium and magnesiumcycle, i.e., they are againloaded into the xylem andtransported to the shoots.
For calcium and sodium noprecise data can be given but
cycling is of minorimportance. For cycling ofpotassium, correspondingdata for other plant speciesare 20% in tomato and 30% inwheat and rye.
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Remobilization of Mineral Nutrients
Import and export of mineral nutrients occursimultaneously during the life of plant organssuch as leaves (Table 3.16).
h l l d b h l
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Physiological and biochemical
processes
Remobilization is based on a range of differentphysiological and biochemical processes:
utilization of mineral nutrients stored in vacuoles(potassium, phosphorus, magnesium, amino-N, etc.),
breakdown of storage proteins (e.g., in vacuoles of theparaveinal mesophyll cells of legumes;), or, finally,
breakdown of cell structures (e.g., chloroplasts) and
enzyme proteins thereby transforming structurallybound mineral nutrients (e.g., magnesium inchlorophyll, micronutrients in enzymes) into a mobileform.
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Seed Germination
During the germination of seeds (or storage
organs such as tubers) mineral nutrients are
remobilized within the seed tissue and
translocated in the phloem or xylem, or both,to the developing roots or shoots.
As a rule, seedlings will grow for at least
several days without an external supply ofmineral nutrients
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Vegetative Stage
During vegetative growth, nutrient supply to the roots isoften either permanently insufficient (as in the case of lowsoil nutrient content) or temporarily interrupted (when, forexample, there is a lack or excess of soil moisture).
Remobilization of mineral nutrients from mature leaves to
areas of new growth is thus of key importance for thecompletion of the life cycle of plants under theseexperimental conditions.
This behaviour (strategy) is typical for fast-growing cropspecies whereas for many wild species cessation of growth
occurs under adverse environmental conditions and, thus,redistribution of mineral nutrients plays a lesser importantrole
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Reproductive Stage
Remobilization of mineral nutrients is particularlyimportant during reproductive growth whenseeds, fruits, and storage organs are formed.
At this growth stage root activity and nutrientuptake generally decrease, mainly as a result ofdecreasing carbohydrate supply to the roots ('sinkcompetition'.
Therefore, the mineral nutrient contents ofvegetative parts quite often decline sharplyduring the reproductive stage
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Period Before Leaf Drop (Perennials)
As a rule, and similar to annual species, theextent of remobilization is high for nitrogen,potassium, phosphorus, and zinc, whereas theleaf contents of calcium, boron, iron and
manganese increase until leaf drop Remobilization of mineral nutrients (except
calcium and manganese) from the leaves towoody parts is a typical feature of perennial
species before leaf drop in temperate climates,and is closely related to the discoloration ofleaves in the autumn.
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Terimakasih