Photosynthesis K-12 Experiments
Photosynthesis Background
Leaf. The primary site of photosynthesis in plants.
Photosynthesis is an important biochemical process in which plants, algae, protistans, and some bacteria convert the energy of sunlight to chemical energy and store it in the bonds of sugar, glucose.
Ultimately, nearly all living things depend on energy produced from
photosynthesis for their nourishment, making it vital to life on Earth. It is also responsible for producing the oxygen that makes up a large portion of the Earth's atmosphere. Organisms that produce energy through photosynthesis are called photoautotrophs.
Plants are the most visible representatives of photoautotrophs, but it
should be emphasized that bacteria and algae as well contribute to the
conversion of free energy into usable energy.
Plant photosynthesis
Most plants are photoautotrophs (exceptions include the famous venus fly trap),
which means that they are able to synthesize food directly from
inorganic compounds using light energy -for example the sun, instead of
eating other organisms or relying on nutrients derived from them. This
is distinct from chemoautotrophs that do not depend on light energy, but use energy from inorganic compounds - like flies and other insects.
The energy for photosynthesis ultimately comes from absorbed photons and involves a reducing agent, which is water in the case of plants, releasing oxygen as a waste product. The light energy is converted to chemical energy, in the form of ATP and NADPH, using the light-dependent reactions and is then available for carbon fixation. Most notably plants use the chemical energy to fix carbon dioxide into carbohydrates and other organic compounds through light-independent reactions. The overall equation for photosynthesis in green plants is:
- n CO2 + 2n H2O + light energy → (CH2O)n + n O2 + n H2O
Where n is defined according to the structure of the resulting carbohydrate. However, hexose sugars and starch are the primary products, so the following generalised equation is often used to represent photosynthesis:
- 6 CO2 + 12 H2O + light energy → C6H12O6 + 6 O2 + 6 H2O
More specifically, photosynthetic reactions usually produces an
intermediate product, which is then converted to the final hexose
carbohydrate products. These carbohydrate products 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 not only occurs in plants, but also in animals when the energy from plants get passed through a food chain.
In general outline, cellular respiration is the opposite of
photosynthesis: glucose and other compounds are oxidised to produce
carbon dioxide, water, and chemical energy. However, both processes
actually take place through a different sequence of reactions and in
different cellular compartments.
Plants capture light primarily using the pigment chlorophyll, which is the reason that most plants have a green color. The function of chlorophyll is often supported by other accessory pigments such as carotenoids and xanthophylls. Both chlorophyll and accessory pigments are contained in organelles (compartments within the cell) called chloroplasts. 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,
contain about half a million 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 as well as decreasing the absorption of ultraviolet or blue light to reduce heating. The transparent, colourless epidermis layer allows light to pass through to the palisade mesophyll cells where most of the photosynthesis takes place.
Photosynthesis in algae and bacteria
Algae range from multicellular forms like kelp to microscopic,
single-celled organisms. Although they are not as complex as land
plants, photosynthesis takes place biochemically the same way. Like
plants, algae have chloroplasts and chlorophyll, but various accessory
pigments are present in some algae such as phycoerythrin in red algae
(rhodophytes) , resulting in a wide variety of colours. All algae
produce oxygen, and many are autotrophic. However, some are heterotrophic, relying on materials produced by other organisms.
Photosynthetic bacteria do not have chloroplasts (or any
membrane-bound organelles), instead, photosynthesis takes place
directly within the cell. Cyanobacteria
contain thylakoid membranes very similar to those in chloroplasts and
are the only prokaryotes that perform oxygen-generating photosynthesis,
in fact chloroplasts are now considered to have evolved from an endosymbiotic
bacterium, which was also an ancestor of and later gave rise to
cyanobacterium. The other photosynthetic bacteria have a variety of
different pigments, called bacteriochlorophylls, and do not produce oxygen. Some bacteria such as Chromatium, oxidize hydrogen sulfide instead of water for photosynthesis, producing sulfur as waste.
Molecular production
Light to chemical energy
- Main article: Light-dependent reaction
A photosystem: a light-harvesting cluster of photosynthetic pigments in a chloroplast thylakoid membrane.
The 'Z-scheme' of electron flow in light-dependent reactions.
The light energy is converted to chemical energy using the light-dependent reactions. The products of the light dependent reactions are ATP from photophosphorylation and NADPH from photoreduction. Both are then utilized as an energy source for the light-independent reactions.
Z scheme
In plants, the light-dependent reactions occur in the thylakoid membranes of the chloroplasts and use light energy to synthesize ATP and NADPH. The photons are captured in the antenna complexes of photosystem I and II by chlorophyll and accessory pigments (see diagram at right). When a chlorophyll a
molecule at a photosystem's reaction center absorbs energy, an electron
is excited and transferred to an electron-acceptor molecule through a
process called Photoinduced charge separation. These electrons are shuttled through an electron transport chain that initially functions to generate a chemiosmotic potential across the membrane, the so called Z-scheme shown in the diagram. An ATP synthase enzyme uses the chemiosmotic potential to make ATP during photophosphorylation while NADPH is a product of the terminal redox reaction in the Z-scheme.
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 II includes the first steps of the Z-scheme, an external source of electrons is required to reduce its oxidized chlorophyll a molecules. This role is played by water during a reaction known as photolysis and results in water being split to give electrons, oxygen and hydrogen ions. Photosystem II is the only known biological enzyme
that carries out this oxidation of water. Initially, the hydrogen ions
from photolysis contribute to the chemiosmotic potential but eventually
they combine with the hydrogen carrier molecule NADP+ to form NADPH. Oxygen is a waste product of light-independent reactions, but the majority of organisms on Earth use oxygen for cellular respiration, including photosynthetic organisms.
Oxygen and photosynthesis
With respect to oxygen and photosynthesis, there are two important concepts.
- Plant and algal cells also use oxygen for cellular respiration, although they have a net output of oxygen since much more is produced during photosynthesis.
- Oxygen is a product of the photolysis reaction not the
fixation of carbon dioxide, during the light-independent reactions.
Consequently, the source of oxygen during photosynthesis is water, not
carbon dioxide.
Bacterial variations
The concept that oxygen production is not directly associated with the fixation of carbon dioxide was first proposed by Cornelius Van Niel in the 1930s, who studied photosynthetic bacteria. Aside from the cyanobacteria,
bacteria only have one photosystem and use reducing agents other than
water. They get electrons from a variety of different inorganic
chemicals including sulfide or hydrogen, so for most of these bacteria oxygen is not produced.
Others, such as the halophiles (an Archeae) produced so called
purple membranes where the bacteriorhodopsin could harvest light and
produce energy. The purple membranes was one of the first to be used to
demonstrate the chemiosmotic theory: light hit the membranes and the pH
of the solution that contained the purple membranes dropped as protons
were pumping out of the membrane.
Carbon fixation
- Main article: Carbon fixation
The fixation of carbon dioxide is a light-independent process in which carbon dioxide combines with a five-carbon sugar, ribulose bisphosphate (RuBP), to give two molecules of a three-carbon compound, glycerate 3-phosphate (GP). This compound is also sometimes known as 3-phosphoglycerate (PGA). GP, in the presence of ATP and NADPH from the light-dependent stages, is reduced to glyceraldehyde 3-phosphate (G3P). This product is also referred to as 3-phosphoglyceraldehyde (PGAL) or even as triose phosphate (a three-carbon sugar). This is the point at which carbohydrates are produced during photosynthesis. Some of the triose phosphates condense to form hexose phosphates, sucrose, starch and cellulose or are converted to acetylcoenzyme A to make amino acids and lipids. Others go on to regenerate RuBP so the process can continue (see Calvin cycle).
Discovery
Although some of the steps in photosynthesis are still not
completely understood, the overall photosynthetic equation has been
known since the 1800s.
Jan van Helmont began the research of the process in the mid-1600s 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. This was a partially accurate
hypothesis - much of the gained mass also comes from carbon dioxide as
well as water. However, this was a signalling 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 sun and light on the plant that could cause it to
rescue a mouse in a matter of hours.
In 1796, Jean Senebier, a French pastor, showed that CO2 was the "fixed" or "injured" air and that it was taken up by plants in photosynthesis. Soon afterwards, 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.
Modern scientists built on the foundation of knowledge from those
scientists centuries ago and were able to discover many things.
Cornelius 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.
Further experiments to prove that the oxygen developed during the
photosynthesis of green plants came from water, were performed by Robert Hill in 1937 and 1939. He showed that isolated chloroplasts give off oxygen in the presence of unnatural reducing agents like iron oxalate, 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 his partner Andrew Benson were able to puzzle out each stage in the dark or light-independent phase of photosynthesis, known as the Calvin cycle.
A Nobel Prize winning scientist, Rudolph A. Marcus, was able to discover the function and significance of the electron transport chain.
Bioenergetics of photosynthesis
Photosynthesis is a physiological phenomenon that converts solar energy into photochemical energy. This physiological phenomenon may be described thermodynamically in terms of changes in energy, entropy and free energy. The energetics of photosynthesis, driven by light, causes a change in entropy that in turn yields a usable source of energy for the plant.
The following chemical equation summarizes the products and reactants of photosynthesis in the typical green photosynthesizing plant:
CO2 + H2O → O2 + (CH2O) + 112 kcal/mol CO2
On earth, there are two sources of free energy: light energy from the
sun, and terrestrial sources, including volcanoes, hot springs and
radioactivity of certain elements. The biochemical value of
electromagnetic radiation has led plants to use the free energy from
the sun in particular. Visible light,
which is used specifically by green plants to photosynthesize, may
result in the formation of electronically excited states of certain
substances called pigments (Gregory). For example, Chlorophyll a
is a pigment which acts as a catalyst, converting solar energy into
photochemical energy that is necessary for photosynthesis (Govindjee).
With the presence of solar energy, the plant has a usable source of
energy, which is termed the free energy (G) of the system. However,
thermal energy is not completely interconvertible, which means that the
character of the solar energy may lead to the limited convertibility of
it into forms that may be used by the plant. This relates back to the
work of Josiah Willard Gibbs: the change in free energy (ΔrG) is related to both the change in entropy (ΔrS) and the change in enthalpy (ΔrH) of the system (Rabinowitch).
Gibbs free energy equation: ΔrG = ΔrH – TΔrS... where ΔH is enthalpy, ΔS is entropy, and T is temperature.
Steelmans free energy equation: ΔtG × Δ<super>lH – SΔn<super>12S = nx</super>±12.332
Past experiments have shown that the total energy produced by
photosynthesis is 112 kcal/mol. However in the experiment, the free
energy due to light was 120 kcal/mol. An overall loss of 8 kcal/mol was
due to entropy, as described by Gibbs equation (Gonindjee). In other
words, since the usable energy of the system is related directly to the
entropy and temperature of the system, a smaller amount of thermal energy
is available for conversion into usable forms of energy (including
mechanical and chemical) when entropy is great (Rabinowitch). This
concept relates back to the second law of thermodynamics in that an increase in entropy is needed to convert light energy into energy suitable for the plant.
Overall, in conjunction with the oxidation-reduction reaction
nature of the photosynthesis equation, and the interrelationships
between entropy and enthalpy, energy in a usable form will be produced
by the photosynthesizing green plant.
Factors affecting photosynthesis
There are three main factors affecting photosynthesis and several corollary factors. The three main are:
Light intensity (Irradiance), wavelength and temperature
In the early 1900s Frederick Frost Blackman investigated the effects of light intensity (irradiance) and temperature on the rate of photosynthesis.
- At constant temperature, the rate of photosynthesis varies with
irradiance, initially increasing as the irradiance increases. However
at higher irradiance this relationship no longer holds and the rate of
photosynthesis reaches a plateau.
- At constant irradiance, the rate of photosynthesis increases as the
temperature is increased over a limited range. This effect is only seen
at high irradiance levels. At low irradiance, increasing the
temperature has little influence on the rate of photosynthesis.
These two experiments illustrate vital points: firstly, from research it is known that photochemical reactions are not generally affected by temperature.
However, these experiments clearly show that temperature affects the
rate of photosynthesis, so there must be two sets of reactions in the
full process of photosynthesis. These are of course the light-dependent 'photochemical' stage and the light-independent, temperature-dependent stage. Secondly, Blackman's experiments illustrate the concept of limiting factors.
Another limiting factor is the wavelength of light. Cyanobacteria which
reside several metres 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 flourescent pigments surround the reaction centre. This
unit is called a phycobilisome.
Carbon dioxide
As carbon dioxide concentrations rise, the rate at which sugars are
made by the light-independent reactions increases until limited by
other factors. One reason for this is that RuBisCO,
the enzyme fixing the carbon dioxide in the light-dependent reactions,
has a binding affinity for both carbon dioxide and oxygen. Thus, an
increase in the concentration of carbon dioxide increases the
probability of RuBisCO fixing carbon dioxide instead of oxygen.
A reduced RuBisCO oxygenase activity is advantageous to plants for several reasons.
- One product of oxygenase activity is phosphoglycolate (2 carbon) instead of 3-phosphoglycerate
(3 carbon). Phosphoglycolate cannot be metabolised by the Calvin 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 cycle.
- Phosphoglycolate is quickly metabolised to glycolate that is toxic
to a plant at a high concentration; it inhibits photosynthesis.
- Salvaging glycolate is an energetically expensive process that uses
the glycolate pathway and only 75% of the carbon is returned to the
Calvin cycle as 3-phosphoglycerate.
-
- A highly simplified summary is:
-
-
- 2 glycolate + ATP → 3-phophoglycerate + carbon dioxide + ADP +NH3
The salvaging pathway for the products of RuBisCO oxygenase activity is more commonly known as photorespiration since it is characterised by light dependent oxygen consumption and the release of carbon dioxide.
Corollary factors
In detail
Metabolic pathways involved in photosynthesis:
References
Govindjee. Bioenergetics of Photosynthesis. New York: Academic Press, 1975.
Gregory, R.P.F. Biochemistry of Photosynthesis. Belfast: Universities Press, 1971.
Rabinowitch, Eugene and Govindjee. Photosynthesis. New York: John Wiley & Sons, Inc., 1969.
Campbell, N., & Reece, J. Biology 7th ed. San Francisco: Benjamin Cummings., 2005
See also
External links
This article is licensed under the GNU Free Documentation License. It uses material from Wikipedia Encyclopedia article "Photosynthesis"
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