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Autotrophic Assimilation – Photosynthesis

Overview of Autotrophic Assimilation

“Autotrophic assimilation” in biology refers to the ability of certain organisms (autotrophs) to build organic compounds from inorganic starting materials. In most ecosystems, the most important autotrophic process is photosynthesis: the conversion of light energy into chemical energy stored in organic molecules, mainly carbohydrates.

In this chapter the focus is on:

General metabolism and biocatalysis are treated in the parent chapter; here we emphasize what is specific to photosynthetic autotrophic assimilation.

Photosynthetic Organisms and Cellular Structures

Photosynthetic Organisms

Organisms performing photosynthesis include:

All of them convert $\mathrm{CO_2}$ and water into organic matter, using light as the primary energy source and producing $\mathrm{O_2}$ (in oxygenic photosynthesis).

A simplified overall equation for oxygenic photosynthesis is:

$$
6\,\mathrm{CO_2} + 6\,\mathrm{H_2O} \xrightarrow{\text{light}} \mathrm{C_6H_{12}O_6} + 6\,\mathrm{O_2}
$$

Here $\mathrm{C_6H_{12}O_6}$ represents a hexose such as glucose; in reality, plants first form triose phosphates and then a variety of carbohydrates.

Chloroplast Structure (Plants and Algae)

In plants and algae, photosynthesis takes place in chloroplasts. Key structural features that are important for the chemistry:

The physical separation between stroma and thylakoid lumen is crucial for setting up and using proton gradients and for organizing electron transfer chains.

Cyanobacteria lack chloroplasts but have internal membrane systems functionally analogous to thylakoids.

Light-Dependent Reactions: Conversion of Light to Chemical Energy

The light-dependent reactions transform light energy into:

These reactions are located in the thylakoid membrane and involve specialized pigment–protein complexes.

Photosynthetic Pigments and Light Absorption

The primary pigments in oxygenic photosynthesis are:

These pigments are organized into:

From an organic-chemistry viewpoint, conjugated double-bond systems are key; excitation of electrons in these systems enables the primary photophysical and photochemical events.

Photosystems and Electron Transport

In plants and algae, two photosystems cooperate:

Water Splitting and Oxygen Evolution

In PSII:

Net reaction in water splitting:

$$
2\,\mathrm{H_2O} \rightarrow 4\,\mathrm{H^+} + 4\,\mathrm{e^-} + \mathrm{O_2}
$$

The protons are released into the thylakoid lumen, contributing to the proton gradient. Electrons are passed through plastoquinone and other carriers to cytochrome $b_6f$.

Electron Transport and Proton Gradient

Electrons travel from PSII to PSI through carriers including:

At PSI:

The electron transfer chain has two major consequences:

  1. Proton accumulation in the thylakoid lumen
    • From water oxidation
    • From PQ/PQH$_2$ cycling through cytochrome $b_6f$
  2. Reduction of $\mathrm{NADP^+}$ in the stroma:
    $$
    \mathrm{NADP^+ + H^+ + 2\,e^- \rightarrow NADPH}
    $$

The resulting proton-motive force across the thylakoid membrane is used to synthesize ATP.

Photophosphorylation: ATP Synthesis

ATP synthase is embedded in the thylakoid membrane. It couples proton flow from the lumen back into the stroma to the endergonic synthesis of ATP:

$$
\mathrm{ADP + P_i \xrightarrow{\text{ATP synthase}} ATP}
$$

Because the driving force is light, this form of ATP synthesis in chloroplasts is termed photophosphorylation.

Key point: after the light reactions, the stroma contains:

Both are essential for the carbon fixation reactions of the Calvin cycle.

Carbon Fixation: The Calvin–Benson–Bassham Cycle

The Calvin cycle (often simply “Calvin cycle”) is the central pathway for autotrophic assimilation of $\mathrm{CO_2}$ in most plants and many photosynthetic microorganisms. It runs in the stroma of chloroplasts.

The core function:

The cycle can be divided into three phases:

  1. Carboxylation
  2. Reduction
  3. Regeneration

Phase 1: Carboxylation (CO₂ Fixation)

The initial acceptor for $\mathrm{CO_2}$ is a 5-carbon sugar:

The key enzyme:

Rubisco catalyzes the carboxylation:

$$
\mathrm{RuBP (C_5) + CO_2 \rightarrow 2\; 3\text{-phosphoglycerate} \ (2 \times C_3)}
$$

In more detail, the 6-carbon intermediate formed after $\mathrm{CO_2}$ addition is unstable and splits into two molecules of 3-phosphoglycerate (3-PGA), each with three carbons.

From an organic perspective, this is a nucleophilic addition of $\mathrm{CO_2}$ to a sugar phosphate, followed by cleavage.

Phase 2: Reduction

The two 3-PGA molecules are then:

  1. Phosphorylated by ATP:
    $$
    \mathrm{3\text{-PGA} + ATP \rightarrow 1,3\text{-bisphosphoglycerate} + ADP}
    $$
  2. Reduced by $\mathrm{NADPH}$:
    $$
    \mathrm{1,3\text{-bisphosphoglycerate} + NADPH + H^+ \rightarrow glyceraldehyde\text{-}3\text{-phosphate} \ (G3P) + P_i + NADP^+}
    $$

The product glyceraldehyde-3-phosphate (G3P) is a triose phosphate.

Organic viewpoint:

Phase 3: Regeneration of Ribulose-1,5-bisphosphate

Most of the G3P produced is not exported but used to regenerate RuBP. This regeneration involves multiple sugar-phosphate rearrangements:

At the end, ribulose-5-phosphate is formed and then phosphorylated by ATP:

$$
\mathrm{ribulose\text{-}5\text{-phosphate} + ATP \rightarrow ribulose\text{-}1,5\text{-bisphosphate} + ADP}
$$

This closes the cycle and prepares another RuBP molecule to accept $\mathrm{CO_2}$.

Stoichiometry of the Calvin Cycle

To produce one net triose phosphate (G3P) that can leave the cycle:

The overall balanced stoichiometry for synthesis of one G3P is:

$$
3\,\mathrm{CO_2} + 9\,\mathrm{ATP} + 6\,\mathrm{NADPH} + 5\,\mathrm{H_2O}
\rightarrow
\mathrm{G3P} + 9\,\mathrm{ADP} + 8\,\mathrm{P_i} + 6\,\mathrm{NADP^+} + 2\,\mathrm{H^+}
$$

Later, two G3P molecules can be combined to form hexoses like fructose-1,6-bisphosphate and eventually starch or sucrose.

Organic Products of Photosynthesis and Their Fates

The immediate organic product of the Calvin cycle is G3P (a triose phosphate). From this central intermediate, various classes of organic compounds are synthesized.

Carbohydrate Synthesis

From G3P, plants synthesize:

These are precursors for:

Key organic reactions involved:

Precursors for Other Biomolecules

Because G3P can be further metabolized, photosynthesis indirectly provides carbon skeletons for:

Thus, photosynthesis is the primary source of reduced carbon in most ecosystems, feeding into the synthesis of numerous organic functional groups and compounds discussed elsewhere in the course.

Variants of Carbon Fixation: C₃, C₄, and CAM Pathways (Overview)

The Calvin cycle itself produces a 3-carbon compound (3-PGA) as the first stable product of $\mathrm{CO_2}$ fixation; plants relying solely on this are called C$_3$ plants.

To reduce losses due to photorespiration (a side reaction of Rubisco with $\mathrm{O_2}$), certain plants evolved additional $\mathrm{CO_2}$-concentrating mechanisms:

Chemically, both strategies involve additional carboxylation and decarboxylation reactions and temporary storage of carbon as organic acids; the Calvin cycle remains the final stage of $\mathrm{CO_2}$ assimilation into carbohydrates.

Energetics and Redox Aspects

From the standpoint of thermodynamics and redox chemistry, photosynthesis performs:

By convention, the overall process can be described as:

$$
\mathrm{CO_2} + \mathrm{H_2O} \xrightarrow{\text{light}} \text{“CH}_2\text{O”} + \mathrm{O_2}
$$

where “CH$_2$O” represents the average composition of carbohydrate.

Key redox agent:

The energy for these uphill transformations comes from absorbed light; chemically, this energy is first captured in excited electronic states and then stored in proton gradients, ATP, and reduced cofactors.

Ecological and Biogeochemical Significance

While this course focuses on molecular structures and reactions, it is important to note the broader consequences of photosynthetic autotrophic assimilation:

Photosynthesis thus links the organic chemistry of living systems to the composition of the atmosphere, hydrosphere, and lithosphere.

Summary

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