Definition
Photosynthesis /foʊtoʊˈsɪnθəsɪs/; from the Greek φώτο- [photo-],
"light," and σύνθεσις [synthesis], "putting together",
"composition") is a chemical process
that converts carbon
dioxide into organic
compounds, especially sugars, using the energy from sunlight. Photosynthesis
occurs in plants, algae, and many species of bacteria, but not in archaea. Photosynthetic organisms are
called photoautotrophs, since they can create their own food. In
plants, algae, and cyanobacteria, photosynthesis uses carbon
dioxide and water, releasing oxygen as
a waste product. Photosynthesis is vital for all aerobic life
on Earth. In addition to
maintaining normal levels of oxygen in the atmosphere, photosynthesis is the source of energy for
nearly all life on earth, either directly, through primary production, or indirectly, as the ultimate source of
the energy in their food, the exceptions being chemoautotrophs that
live in rocks or around deep sea hydrothermal vents. The rate of energy capture by
photosynthesis is immense, approximately 100 terawatts, which is about six times larger than the power consumption of human
civilization. As
well as energy, photosynthesis is also the source of the carbon in all the
organic compounds within organisms' bodies. In all, photosynthetic organisms
convert around 100–115 petagramsof carbon
into biomass per
year.
Although
photosynthesis can happen in different ways in different species, some features
are always the same. For example, the process always begins when energy from
light is absorbed by proteins called photosynthetic reaction centers that
contain chlorophylls. In plants, these proteins are held inside organelles called chloroplasts, while in bacteria they are embedded in the plasma
membrane. Some of the
light energy gathered by chlorophylls is stored in the form of adenosine triphosphate (ATP).
The rest of the energy is used to remove electrons from
a substance such as water. These electrons are then used in the reactions that
turn carbon dioxide into organic compounds. In plants, algae and cyanobacteria,
this is done by a sequence of reactions called the Calvin
cycle, but different
sets of reactions are found in some bacteria, such as the reverse Krebs cycle in Chlorobium. Many photosynthetic organisms haveadaptations that
concentrate or store carbon dioxide. This helps reduce a wasteful process
called photorespiration that
can consume part of the sugar produced during photosynthesis.
The first
photosynthetic organisms probably evolved about 3,500 million years ago, early in the evolutionary history of life, when all forms of life on Earth were microorganisms and
the atmosphere had much more carbon dioxide. They most likely used hydrogen or hydrogen
sulfide as sources of electrons, rather than water. Cyanobacteria
appeared later, around 3,000 million years ago, and drastically changed the Earth when they
began to oxygenate the atmosphere, beginning about 2,400 million years ago. This new atmosphere allowed the evolution of complex life such
as protists.
Eventually, no later than a billion years ago, one of these protists formed a symbiotic
relationship with a cyanobacterium, producing the ancestor
of many plants and algae. The chloroplasts in modern plants are the
descendants of these ancient symbiotic cyanobacteria.
Overview
Photosynthesis changes sunlight into chemical
energy, splits water to liberate O2, and fixes CO2 into sugar.
Photosynthetic
organisms are photoautotrophs, which means that they are
repositories of energy, they are able to synthesize food directly from carbon dioxide, water, and
using energy from light. They accrue it as part of their potential
energy. However, not all
organisms that use light as a source of energy carry out photosynthesis, since photoheterotrophs use
organic compounds, rather than carbon dioxide, as a source of carbon. In
plants, algae and cyanobacteria, photosynthesis releases oxygen. This is called oxygenic photosynthesis. Although there are some differences between
oxygenic photosynthesis in plants, algae and cyanobacteria, the overall process is
quite similar in these organisms. However, there are some types of bacteria
that carry out anoxygenic
photosynthesis, which consumes carbon dioxide but does not release
oxygen.
Carbon dioxide is
converted into sugars in a process called carbon
fixation. Carbon fixation
is a redox reaction,
so photosynthesis needs to supply both a source of energy to drive this
process, and the electrons needed to convert carbon dioxide into a carbohydrate, which is a reduction reaction. In general outline, photosynthesis is the
opposite of cellular respiration, where glucose and other compounds are
oxidized to produce carbon dioxide, water, and release chemical energy.
However, the two processes take place through a different sequence of chemical
reactions and in different cellular compartments.
Carbon dioxide + electron donor + light
energy → carbohydrate + oxidized electron donor
In oxygenic photosynthesis
water is the electron donor and, since its hydrolysis releases
oxygen, the equation for this process is:
carbon dioxide + water + light energy →
carbohydrate + oxygen + water
Often 2n water molecules are cancelled on
both sides, yielding:
carbon dioxide + water + light energy →
carbohydrate + oxygen
Other processes substitute other compounds
(such as arsenite) for water in the electron-supply
role; the microbes use sunlight to oxidize arsenite to arsenate: The equation for this reaction is:
CO2 +
(AsO33–) + photons → (AsO43–) + CO
carbon dioxide + arsenite + light energy →
arsenate + carbon monoxide (used to build other compounds in subsequent
reactions)
Photosynthesis occurs in two stages. In the
first stage, light-dependent
reactions or light reactions capture
the energy of light and use it to make the energy-storage molecules ATP and NADPH. During the second stage, the light-independent reactions use
these products to capture and reduce carbon dioxide.
Most organisms that utilize photosynthesis to
produce oxygen use visible
light to do so, although at least three use infrared
radiation.
Photosynthetic
Membranes and Organelles
Chloroplast ultrastructure:
1. outer membrane
2. intermembrane space
3. inner membrane (1+2+3: envelope)
4. stroma (aqueous fluid)
5. thylakoid lumen (inside of thylakoid)
6. thylakoid membrane
7. granum (stack of thylakoids)
8. thylakoid (lamella)
9. starch
10. ribosome
11. plastidial DNA
12. plastoglobule (drop of lipids)
1. outer membrane
2. intermembrane space
3. inner membrane (1+2+3: envelope)
4. stroma (aqueous fluid)
5. thylakoid lumen (inside of thylakoid)
6. thylakoid membrane
7. granum (stack of thylakoids)
8. thylakoid (lamella)
9. starch
10. ribosome
11. plastidial DNA
12. plastoglobule (drop of lipids)
The proteins that
gather light for photosynthesis are embedded within cell
membranes. The simplest way
these are arranged is in photosynthetic bacteria, where these proteins are held
within the plasma membrane. However, this membrane may be tightly folded
into cylindrical sheets calledthylakoids, or bunched up into round vesicles called intracytoplasmic membranes.[16] These
structures can fill most of the interior of a cell, giving the membrane a very
large surface area and therefore increasing the amount of light that the
bacteria can absorb.[15]
In plants and
algae, photosynthesis takes place in organelles called chloroplasts. A typical plant
cell contains about 10 to 100 chloroplasts. The
chloroplast is enclosed by a membrane. This membrane is composed of a
phospholipid inner membrane, a phospholipid outer membrane, and an intermembrane
space between them. Within the membrane is an aqueous fluid called the stroma.
The stroma contains stacks (grana) of thylakoids, which are the site of
photosynthesis. The thylakoids are flattened disks, bounded by a membrane with
a lumen or thylakoid space within it. The site of photosynthesis is the
thylakoid membrane, which contains integral and peripheral membrane protein complexes,
including the pigments that absorb light energy, which form the photosystems.
Plants absorb
light primarily using the pigment chlorophyll, which is the reason that most plants have a
green color. Besides chlorophyll, plants also use pigments such as carotenes and xanthophylls. Algae also use chlorophyll, but various other
pigments are present as phycocyanin,carotenes, and xanthophylls in green
algae, phycoerythrin in red
algae (rhodophytes) and fucoxanthin in brown
algae and diatoms resulting
in a wide variety of colors.
These pigments are
embedded in plants and algae in special antenna-proteins. In such proteins all
the pigments are ordered to work well together. Such a protein is also called a light-harvesting complex.
Although all cells
in the green parts of a plant have chloroplasts, most of the energy is captured
in the leaves. The cells in the interior tissues of a
leaf, called the mesophyll, can contain between 450,000 and
800,000 chloroplasts for every square millimeter of leaf. The surface of the
leaf is uniformly coated with a water-resistant waxy cuticle that
protects the leaf from excessive evaporation of
water and decreases the absorption of ultraviolet or blue light to
reduce heating. The transparent epidermis layer
allows light to pass through to thepalisade mesophyll
cells where most of the photosynthesis takes place
Light
reactions
Light-dependent reactions of photosynthesis at
the thylakoid membrane
In the light reactions, one molecule of the pigment chlorophyll absorbs
one photon and
loses one electron. This electron is passed to a modified form
of chlorophyll called pheophytin, which passes the electron to a quinonemolecule, allowing the start of a
flow of electrons down an electron transport chain that
leads to the ultimate reduction of NADP to NADPH. In addition, this creates a proton gradient across
the chloroplast membrane; its dissipation is used by ATP
synthase for the concomitant synthesis of ATP.
The chlorophyll molecule regains the lost electron from a water molecule
through a process called photolysis, which releases a dioxygen (O2)
molecule. The overall equation for the light-dependent reactions under the
conditions of non-cyclic electron flow in green plants is:
2 H2O + 2 NADP+ +
3 ADP + 3 Pi + light → 2 NADPH + 2 H+ +
3 ATP + O2
Not all wavelengths of
light can support photosynthesis. The photosynthetic action spectrum depends on
the type ofaccessory pigments present.
For example, in green plants, the action
spectrum resembles the absorption spectrumfor chlorophylls and carotenoids with
peaks for violet-blue and red light. In red algae, the action spectrum overlaps
with the absorption spectrum of phycobilins for
red blue-green light, which allows these algae to grow in deeper waters that
filter out the longer wavelengths used by green plants. The non-absorbed part
of the light spectrum is what gives photosynthetic organisms their
color (e.g., green plants, red algae, purple bacteria) and is the least
effective for photosynthesis in the respective organisms.
1. Z scheme
The
"Z scheme"
In plants, light-dependent
reactions occur in the thylakoid
membranes of the chloroplasts and use light
energy to synthesize ATP and NADPH. The light-dependent reaction has two forms:
cyclic and non-cyclic. In the non-cyclic reaction, the photons are captured in the light-harvesting antenna complexes of photosystem II by chlorophyll and other accessory pigments (see diagram at right). When a chlorophyll molecule at
the core of the photosystem II reaction center obtains sufficient excitation
energy from the adjacent antenna pigments, an electron is transferred to the
primary electron-acceptor molecule, pheophytin, through a process called photoinduced charge separation. These electrons are shuttled
through an electron transport
chain, the so-called Z-scheme shown in the diagram, that initially functions to generate
a chemiosmotic
potential across the
membrane. An ATP synthase enzyme uses the
chemiosmotic potential to make ATP during photophosphorylation, whereas NADPH is a product of the terminal redox reaction in the Z-scheme. The electron enters a chlorophyll
molecule in Photosystem
I. The electron is excited due to the light absorbed by the photosystem.
A second electron carrier accepts the electron, which again is passed down
lowering energies of electron acceptors. The
energy created by the electron acceptors is used to move hydrogen ions across
the thylakoid membrane into the lumen. The electron is used to reduce the
co-enzyme NADP, which has functions in the light-independent reaction. The
cyclic reaction is similar to that of the non-cyclic, but differs in the form
that it generates only ATP, and no reduced NADP (NADPH) is created. The cyclic
reaction takes place only at photosystem I. Once the electron is displaced from
the photosystem, the electron is passed down the electron acceptor molecules
and returns to photosystem I, from where it was emitted, hence the name cyclic reaction.
2. Water photolysis
The NADPH is the main reducing agent in chloroplasts, providing a source of energetic
electrons to other reactions. Its production leaves chlorophyll with a deficit
of electrons (oxidized), which must be obtained from some other reducing agent.
The excited electrons lost from chlorophyll in photosystem
I are replaced from the electron transport chain by plastocyanin.
However, since photosystem
IIincludes the first steps of the Z-scheme, an external source of electrons is required to reduce
its oxidized chlorophyll a molecules. The source of electrons in green-plant and
cyanobacterial photosynthesis is water. Two water molecules are oxidized by
four successive charge-separation reactions by photosystem II to yield a
molecule of diatomic oxygen and four hydrogen ions; the electron
yielded in each step is transferred to a redox-active tyrosine residue that then
reduces the photoxidized paired-chlorophyll a species called P680 that serves as the primary
(light-driven) electron donor in the photosystem II reaction center. The
oxidation of water is catalyzed in photosystem II
by a redox-active structure that contains four manganese ions and a calcium
ion; this oxygen-evolving
complex binds two water molecules and stores the four oxidizing
equivalents that are required to drive the water-oxidizing reaction. Photosystem
II is the only known biological enzyme that carries out this oxidation of water. The hydrogen
ions contribute to the transmembrane chemiosmotic potential that leads to ATP
synthesis. Oxygen is a waste product of light-dependent reactions, but the
majority of organisms on Earth use oxygen for cellular respiration, including photosynthetic organisms.
Light-Independent reactions
1. The Calvin cycle
In the light-independent or dark reactions the enzyme RuBisCO captures CO2 from the atmosphere and in a
process that requires the newly formed NADPH, called the Calvin-Benson Cycle,
releases three-carbon sugars, which are later combined to form sucrose and
starch. The overall equation for the light-independent reactions in green
plants is:
3 CO2 + 9 ATP + 6 NADPH + 6 H+ → C3H6O3-phosphate
+ 9 ADP + 8 Pi + 6
NADP+ + 3 H2O
Overview of the
Calvin cycle and carbon fixation
To
be more specific, carbon fixation produces an intermediate product, which is
then converted to the final carbohydrate products. The carbon skeletons
produced by photosynthesis are then variously used to form other organic
compounds, such as the building material cellulose, as
precursors for lipid and amino acid biosynthesis, or as a fuel in cellular respiration. The
latter occurs not only in plants but also in animals when the energy from plants gets passed
through a food chain.
The
fixation or reduction of carbon dioxide is a process in which carbon dioxide combines with a five-carbon sugar, ribulose
1,5-bisphosphate (RuBP), to
yield two molecules of a three-carbon compound, glycerate
3-phosphate (GP), also
known as 3-phosphoglycerate (PGA). GP, in the presence of ATP and NADPH from the light-dependent stages, is
reduced toglyceraldehyde 3-phosphate (G3P). This product is also referred to
as 3-phosphoglyceraldehyde (PGAL) or even as triose phosphate. Triose is a 3-carbon sugar (see carbohydrates). Most (5
out of 6 molecules) of the G3P produced is used to regenerate RuBP so the
process can continue (see Calvin-Benson cycle). The 1 out of 6 molecules of the
triose phosphates not "recycled" often condense to form hexose phosphates, which ultimately yield sucrose, starch and cellulose. The
sugars produced during carbon metabolism yield carbon skeletons that can be used
for other metabolic reactions like the production of amino acids and lipids.
2. Carbon concentrating mechanisms
a.
On land
In hot and
dry conditions, plants close their stomata to prevent the loss of water. Under
these conditions, CO2 will
decrease, and oxygen gas, produced by the light reactions of photosynthesis,
will decrease in the stem, not leaves, causing an increase of photorespiration by the oxygenase activity of ribulose-1,5-bisphosphate
carboxylase/oxygenase and
decrease in carbon fixation. Some plants have evolved mechanisms to increase the CO2 concentration in the leaves under these
conditions.
C4 plants chemically fix carbon dioxide in the
cells of the mesophyll by adding it to the three-carbon
moleculephosphoenolpyruvate (PEP), a
reaction catalyzed by an enzyme called PEP
carboxylase, creating the four-carbon organic acid oxaloacetic acid.
Oxaloacetic acid or malate synthesized by this process is then
translocated to specialized bundle
sheath cells where
the enzyme RuBisCO and other Calvin cycle enzymes are
located, and where CO2 released bydecarboxylation of the four-carbon acids is then fixed
by RuBisCO activity to the three-carbon sugar 3-phosphoglyceric acids. The
physical separation of RuBisCO from the oxygen-generating light reactions
reduces photorespiration and increases CO2fixation and, thus, photosynthetic capacity of the leaf.[21] C4 plants can produce more sugar than C3 plants in conditions of high light and
temperature. Many important crop plants are C4 plants, including maize, sorghum,
sugarcane, and millet. Plants that do not use PEP-carboxylase in carbon
fixation are called C3 plants because the primary carboxylation
reaction, catalyzed by RuBisCO, produces the three-carbon sugar
3-phosphoglyceric acids directly in the Calvin-Benson cycle. Over 90% of plants
use C3 carbon
fixation, compared to 3% that use C4 carbon fixation.
Xerophytes, such as cacti and most succulents, also use
PEP carboxylase to capture carbon dioxide in a process calledCrassulacean acid metabolism (CAM). In contrast to C4 metabolism, which physically separates the CO2 fixation to PEP from the Calvin cycle,
CAM temporally separates
these two processes. CAM plants have a different leaf anatomy from C3 plants, and fix the CO2 at night, when their stomata are open.
CAM plants store the CO2 mostly in
the form of malic acid via carboxylation of phosphoenolpyruvate to oxaloacetate, which is then reduced
to malate. Decarboxylation of malate during the day releases CO2 inside the leaves, thus allowing carbon
fixation to 3-phosphoglycerate by RuBisCO. Sixteen thousand species of plants
use CAM.
b. In water
Cyanobacteria possess carboxysomes, which
increase the concentration of CO2 around RuBisCO to increase the rate of
photosynthesis. This operates by carbonic anhydrase, producing hydrocarbonate ions (HCO3–),
which are then pumped into the carboxysome, before being processed by a
different carbonic anhydrase to produce CO2. Pyrenoids in algae andhornworts also act to concentrate CO2 around rubisco.
Order
and kinetics
The overall process of photosynthesis takes
place in four stages:
Stage
|
Description
|
Time scale
|
1
|
Energy
transfer in antenna chlorophyll (thylakoid membranes)
|
|
2
|
Transfer
of electrons in photochemical reactions (thylakoid membranes)
|
|
3
|
Electron
transport chain and ATP synthesis (thylakoid membranes)
|
|
4
|
Carbon
fixation and export of stable products
|
Efficiency
Plants usually
convert light into chemical
energy with a photosynthetic efficiency of
3–6%. Actual plants' photosynthetic efficiency
varies with the frequency of the light being converted, light intensity,
temperature and proportion of carbon dioxide in the atmosphere, and can vary
from 0.1% to 8%. By comparison, solar panels convert light into electric
energy at an efficiency of approximately 6–20% for
mass-produced panels, and above 40% in laboratory devices.
Evolution
Plant cells with visible chloroplasts (from a
moss,Plagiomnium
affine)
Early
photosynthetic systems, such as those from green and purple sulfur and green and purple
nonsulfur bacteria, are thought to
have been anoxygenic, using various molecules as electron
donors. Green and purple
sulfur bacteria are thought to have used hydrogen and sulfur as
an electron donor. Green nonsulfur bacteria used various amino and
other organic
acids. Purple nonsulfur
bacteria used a variety of nonspecific organic molecules. The use of these
molecules is consistent with the geological evidence that the atmosphere was
highly reduced at that time.
Fossils of what
are thought to be filamentous photosynthetic
organisms have been dated at 3.4 billion years old.
The main source of oxygen in
the atmosphere is oxygenic
photosynthesis, and its first
appearance is sometimes referred to as the oxygen catastrophe. Geological evidence suggests that oxygenic
photosynthesis, such as that in cyanobacteria, became important during thePaleoproterozoic era
around 2 billion years ago. Modern photosynthesis in plants and most
photosynthetic prokaryotes is oxygenic. Oxygenic photosynthesis uses water as
an electron donor, which is oxidized to
molecular oxygen (O2) in the photosynthetic reaction center.
1. Symbiosis and the origin of chloroplasts
Several groups of animals have formed symbiotic relationships with
photosynthetic algae. These are most common in corals, sponges and sea anemones. It is
presumed that this is due to the particularly simple body plans and large surface
areas of these animals compared to their volumes. In addition, a few marine mollusks Elysia
viridis and Elysia chlorotica also maintain a symbiotic relationship with chloroplasts
they capture from the algae in their diet and then store in their bodies. This
allows the mollusks to survive solely by photosynthesis for several months at a
time. Some of the genes from the plant cell nucleus have even been
transferred to the slugs, so that the chloroplasts can be supplied with
proteins that they need to survive.
An even closer form of symbiosis may explain the origin
of chloroplasts. Chloroplasts have many similarities with photosynthetic bacteria, including
a circular chromosome,
prokaryotic-type ribosomes, and similar
proteins in the photosynthetic reaction center. The endosymbiotic
theory suggests that
photosynthetic bacteria were acquired (by endocytosis)
by early eukaryotic cells to form the
first plant cells. Therefore, chloroplasts may be photosynthetic
bacteria that adapted to life inside plant cells. Like mitochondria,
chloroplasts still possess their own DNA, separate from the nuclear DNA of their plant
host cells and the genes in this chloroplast DNA resemble those in cyanobacteria. DNA in chloroplasts codes for redox proteins such as photosynthetic reaction centers. TheCoRR Hypothesis proposes that this Co-location is
required for Redox Regulation.
2. Cyanobacteria and the evolution of photosynthesis
The biochemical capacity to use water as the source for
electrons in photosynthesis evolved once, in a common ancestor of extant cyanobacteria. The
geological record indicates that this transforming event took place early in
Earth's history, at least 2450–2320 million years ago (Ma), and, it is
speculated, much earlier. Available evidence
from geobiological studies of Archean (>2500 Ma)sedimentary rocks indicates that life existed 3500 Ma, but the question of
when oxygenic photosynthesis evolved is still unanswered. A clear
paleontological window on cyanobacterial evolution opened about 2000
Ma, revealing an already-diverse biota of blue-greens. Cyanobacteria remained principal primary producers throughout the Proterozoic Eon (2500–543 Ma), in part because the redox structure of the
oceans favored photoautotrophs capable of nitrogen fixation. Green algae joined blue-greens
as major primary producers on continental shelves near the end of theProterozoic, but only
with the Mesozoic (251–65 Ma)
radiations of dinoflagellates, coccolithophorids, and diatoms did primary production in marine shelf waters take modern form. Cyanobacteria
remain critical to marine ecosystems as primary producers in oceanic gyres, as agents of
biological nitrogen fixation, and, in modified form, as the plastids of marine algae.
A 2010 study by researchers at Tel Aviv University discovered that the Oriental hornet (Vespa
orientalis) converts sunlight into electric power using a pigment called xanthopterin.
This is the first scientific evidence of a member of the animal kingdom
engaging in photosynthesis.
Discovery
Although some of the steps in photosynthesis
are still not completely understood, the overall photosynthetic equation has
been known since the 19th century.
Jan
van Helmont began the research of the process in the
mid-17th century when he carefully measured the mass of
the soil used by a plant and the mass of the plant as it grew. After noticing
that the soil mass changed very little, he hypothesized that the mass of the
growing plant must come from the water, the only substance he added to the
potted plant. His hypothesis was partially accurate — much of the gained mass
also comes from carbon dioxide as well as water. However, this was a signaling
point to the idea that the bulk of a plant's biomass comes
from the inputs of photosynthesis, not the soil itself.
Joseph
Priestley, a chemist and
minister, discovered that, when he isolated a volume of air under an inverted
jar, and burned a candle in it, the candle would burn out very quickly, much
before it ran out of wax. He further discovered that a mouse could similarly
"injure" air. He then showed that the air that had been
"injured" by the candle and the mouse could be restored by a plant.
In 1778, Jan
Ingenhousz, court physician
to the Austrian Empress,
repeated Priestley's experiments. He discovered that it was the influence of
sunlight on the plant that could cause it to revive a mouse in a matter of
hours.
In 1796, Jean
Senebier, a Swiss pastor,
botanist, and naturalist, demonstrated that green plants consume carbon dioxide
and release oxygen under the influence of light. Soon afterward, Nicolas-Théodore de Saussure showed
that the increase in mass of the plant as it grows could not be due only to
uptake of CO2 but also to the incorporation of water. Thus,
the basic reaction by which photosynthesis is used to produce food (such as
glucose) was outlined.
Cornelis
Van Niel made key discoveries explaining the chemistry
of photosynthesis. By studying purple sulfur bacteria and
green bacteria he was the first scientist to demonstrate that photosynthesis is
a light-dependent redox reaction,
in which hydrogen reduces carbon dioxide.
Robert Emerson discovered two light reactions
by testing plant productivity using different wavelengths of light. With the
red alone, the light reactions were suppressed. When blue and red were
combined, the output was much more substantial. Thus, there were two
photosystems, one absorbing up to 600 nm wavelengths, the other up to 700
nm. The former is known as PSII, the latter is PSI. PSI contains only
chlorophyll a, PSII contains primarily chlorophyll a with most of the available
chlorophyll b, among other pigment. These include phycobilins, which are the
red and blue pigments of red and blue algae respectively, and fucoxanthol for
brown algae and diatoms. The process is most productive when absorption of
quanta are equal in both the PSII and PSI, assuring that input energy from the
antenna complex is divided between the PSI and PSII system, which in turn
powers the photochemistry.
Robert Hill thought
that a complex of reactions consisting of an intermediate to cytochrome b6 (now
a plastoquinone), another is from cytochrome f to a step in the
carbohydrate-generating mechanisms. These are linked by plastoquinone, which
does require energy to reduce cytochrome f for it is a sufficient reductant.
Further experiments to prove that the oxygen developed during the
photosynthesis of green plants came from water, were performed by Hill in 1937
and 1939. He showed that isolated chloroplasts give
off oxygen in the presence of unnatural reducing agents like ironoxalate, ferricyanide or benzoquinone after
exposure to light. The Hill reaction is as follows:
2 H2O + 2 A + (light,
chloroplasts) → 2 AH2 + O2
where A is the electron acceptor. Therefore,
in light, the electron acceptor is reduced and oxygen is evolved.
Samuel
Ruben and Martin
Kamen used radioactive
isotopes to determine that the oxygen liberated in
photosynthesis came from the water.
Melvin
Calvin and Andrew
Benson, along with James
Bassham, elucidated the
path of carbon assimilation (the photosynthetic carbon reduction cycle) in
plants. The carbon reduction cycle is known as the Calvin
cycle, which ignores
the contribution of Bassham and Benson. Many scientists refer to the cycle as
the Calvin-Benson Cycle, Benson-Calvin, and some even call it the
Calvin-Benson-Bassham (or CBB) Cycle.
Nobel
Prize-winning scientist Rudolph
A. Marcus was able to discover the function and
significance of the electron transport chain.
Otto Heinrich Warburg and Dean
Burk discovered the I-quantum photosynthesis
reaction that splits the CO2, activated by the respiration.
Louis N.M. Duysens and Jan Amesz discovered
that chlorophyll a will absorb one light, oxidize cytochrome f, chlorophyll a
(and other pigments) will absorb another light, but will reduce this same
oxidized cytochrome, stating the two light reactions are in series.
Factors
There are three main factors affecting
photosynthesis and several corollary factors. The three main are:
1. Light intensity (irradiance), wavelength and temperature
In the early 20th century, Frederick Frost Blackman along with Albert Einstein investigated the effects of light intensity (irradiance) and
temperature on the rate of carbon assimilation.
§ At constant
temperature, the rate of carbon assimilation varies with irradiance, initially
increasing as the irradiance increases. However, at higher irradiance, this
relationship no longer holds and the rate of carbon assimilation reaches a
plateau.
§ At constant
irradiance, the rate of carbon assimilation increases as the temperature is
increased over a limited range. This effect is seen only at high irradiance
levels. At low irradiance, increasing the temperature has little influence on
the rate of carbon assimilation.
These two experiments illustrate vital points: First, from research it is known that,
in general, photochemical reactions are not affected by temperature. However,
these experiments clearly show that temperature affects the rate of carbon
assimilation, so there must be two sets of reactions in the full process of
carbon assimilation. These are, of course, the light-dependent
'photochemical' stage and the light-independent,
temperature-dependent stage. Second,
Blackman's experiments illustrate the concept of limiting factors. Another
limiting factor is the wavelength of light. Cyanobacteria, which reside several
meters underwater, cannot receive the correct wavelengths required to cause
photoinduced charge separation in conventional photosynthetic pigments. To
combat this problem, a series of proteins with different pigments surround the
reaction center. This unit is called a phycobilisome.
2. Carbon dioxide levels and photorespiration
As carbon dioxide concentrations rise, the rate at which
sugars are made by the light-independent
reactions increases until limited by other factors. RuBisCO,
the enzyme that captures carbon dioxide in the light-independent reactions, has
a binding affinity for both carbon dioxide and oxygen. When the concentration
of carbon dioxide is high, RuBisCO will fix carbon dioxide. However,
if the carbon dioxide concentration is low, RuBisCO will bind oxygen instead of
carbon dioxide. This process, called photorespiration, uses
energy, but does not produce sugars.
RuBisCO oxygenase
activity is disadvantageous to plants for several reasons:
1. One product of
oxygenase activity is phosphoglycolate (2 carbon) instead of 3-phosphoglycerate (3 carbon).
Phosphoglycolate cannot be metabolized by the Calvin-Benson cycle and
represents carbon lost from the cycle. A high oxygenase activity, therefore,
drains the sugars that are required to recycle ribulose 5-bisphosphate and for
the continuation of the Calvin-Benson cycle.
2. Phosphoglycolate
is quickly metabolized to glycolate that is toxic to a plant at a high
concentration; it inhibits photosynthesis.
3. Salvaging
glycolate is an energetically expensive process that uses the glycolate
pathway, and only 75% of the carbon is returned to the Calvin-Benson cycle as
3-phosphoglycerate. The reactions also produce ammonia (NH3),
which is able to diffuse out of the plant,
leading to a loss of nitrogen.
A highly
simplified summary is:
2 glycolate + ATP
→ 3-phosphoglycerate + carbon dioxide + ADP + NH3
The
salvaging pathway for the products of RuBisCO oxygenase activity is more
commonly known as photorespiration, since it
is characterized by light-dependent oxygen consumption and the release of
carbon dioxide.
Photosynthesis Experiments Using Leaf Discs
Objectives:
1. Reinforce methods of experimental design and statistical
analysis.
2. Test some parameters that might have an effect on
photosynthesis
3. Learn how leaf anatomy is adapted to optimize photosynthetic
efficiency.
I. Introduction:
Photosynthesis is the process by which light
energy is converted into chemical bond energy by autotrophic organisms. During
the light dependent reactions of photosynthesis light energy is used to
generate ATP and to reduce NADP+ to NADPH. During the light independent
reactions of photosynthesis, carbon dioxide is synthesized into glucose using
chemical bond energy stored in ATP and the reducing power of NADPH. In
eukaryotic autotrophs, both sets of reactions take place in a specialized
organelle, the chloroplast. In autotrophic bacteria (cyanobacteria) the light
dependent reactions occur on the plasma membrane and the light independent
reactions occur in the liquid cytoplasm.
The entire process of photosynthesis can be summarized:
LIGHT
6 CO2 + 6 H2O C6H12O6 + 6 O2
The rate at which photosynthesis occurs might
depend upon both the quality (i.e. wavelength or color) and quantity (i.e.
brightness) of light, as well as other parameters.
Leaf Anatomy: In most plants, the primary organ in which
photosynthesis occurs is the leaf. In your experiment today, you will
eventually be using portions of leaves to test hypotheses about photosynthesis.
First we will examine leaf anatomy.
With a microscope,
examine a prepared slide of a cross-section of a leaf. The prepared slide may
be labeled: "Typical dicot leaf" or "privet leaf" or "Ligustrum
leaf, c.s."
OBSERVE the cross-section on MEDIUM (100x) or
HIGH (400x) power.
The cross-section of
the leaf is several cell layers thick. Each layer of cells has a different
function and a different morphology ('form fits function').
In the
cross-section, the uppermost and bottom most layers of cells are the upper
epidermis and lower epidermis, respectively. Each of these epidermal
layers is just one cell thick. These cells have relatively thick walls and they
secrete a layer of wax called the cuticle on the surface of the leaf.
What do you think would be a function of the cuticle?
Observe the cells
which make up the lower epidermis; you may see gaps in this array of cells.
These gaps are called stomata; each one (a stoma) is surrounded by two guard
cells. Each pair of guard cells is able to open and close a stoma, thus
regulating the entrance and exit of air, and thus of oxygen , carbon dioxide,
and water. For example, the stomata may close if the leaf becomes too hot or
dry, in order to stop water loss from the leaf. Air which enters the leaf
through the stomata first encounters a layer of cells called the spongy
parenchyma. The spongy parenchyma is so-named because, like a sponge, it
has relatively large air spaces amongst the cells. In the leaf, these spaces
allow for the circulation of air throughout the leaf.
Above the spongy
parenchyma lies a layer of cells that are rectangular and tightly packed. This
layer is called the palisade parenchyma. Can you tell which layer of
parenchyma has more chloroplasts per cell ?
Draw
and label palisade and spongy parenchyma, epidermis, air space, stomata,
cuticle.
II. Methods
1. Cut 5 discs from
the green part of a leaf of the Dieffenbachia seguine plant with a paper
punch. Handle them carefully; the discs consist of live cells, and in this
condition they can be easily damaged.
2. Put the 5 discs
in the syringe, and replace the plunger.
3. Fill the syringe
with buffer. The buffer is 0.1 M NaHCO3 (0.1 moles [8.4 g] of sodium
bicarbonate, or baking soda, dissolved in 1 liter of water). The buffer has
already had most of the dissolved gasses (mostly air) removed from it. Sodium
bicarbonate dissociates into a sodium ion and a hydrogen carbonate ion in
water, like this:
NaHCO3
Na+ + HCO3-
Hydrogen carbonate in the presence of hydrogen
ions can from carbonic acid, H2CO3 which can break down into carbon dioxide and
water.
CO2 + H2O H2CO3 H+ + HCO3-
4. Expel any
airspace in the syringe.
5.
Seal the tip of the syringe by pressing it hard against a rubber stopper or
your finger. Pressing against a rubber stopper gives a better seal. Now back
off the plunger, swirl the disks, and immediately expel any new air space. Gas
will have expanded and moved out of the leaf discs.
6. Repeat step 5
until no more bubbles form, and the leaf discs all sink. Once all the discs
have sunk they can be used in your experiment.
7. The syringe can stand on its plunger. Place it in the light
source provided. Watch to see whether the leaf discs rise, and record in
seconds how long it takes for each one to rise.
Answer the following questions about what you have just done:
At first, why do the leaf discs float?
When you pull back on the plunger, where have the bubbles come
from?
Why do the leaf discs eventually sink in the syringe?
Why do the leaf discs rise when placed in the light?
What is the purpose of the sodium bicarbonate in this experiment?
Now that you have familiarized yourself with the methods, examine
these problems:
Problem 1: Is the rate of photosynthesis higher under bright light than
under dim light?
Describe an experiment that could be designed to answer this
question. After designing and carrying out your experiment, take what you have
learned about the methods, and move on to Problem 2.
Problem 2: Is pigmentation necessary for photosynthesis ?
Describe and carry out an experiment to answer this question.
III. Results
Put data in a data table as you collect it. Templates for
statistical tests are available in class and at the Biology Department's
Statistics web site : (www.radford.edu/~biol-web/stats.html). Study the
examples for entering data in the spreadsheet template. Open the template and
enter your data as instructed.
Graph the data. Describe your results.
IV. Conclusions.
State whether or not your hypotheses were
supported. Tell about how your experiment could be improved. What other factors
might affect photosynthesis that could be tested with this method?
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