Jump to content

PSII/PSI quantification

From OceanWiki

Template:BreadcrumbsPrimaryProduction


Photosystem stoichiometry (PSII/PSI)
Approach: immunodetection or targeted mass spectrometry of PSII/PSI proteins
Context: in situ, incubation, lab
Spatial scale: point sample
Temporal scale: minutes to hours
Units: mol protein per cell; mol protein L-1; protein mass fraction
Community captured: bulk to group-specific
Co-measurements: Single Turnover Chlorophyll Fluorescence; 14C or 13C fixation; total protein

Method Overview

The reaction center proteins of photosystem II (D1, encoded by psbA) and photosystem I (PsaA/PsaB) are quantified by immunodetection (Western blotting using global antibodies) or targeted proteomics by mass spectrometry. The PSII:PSI stoichiometry reflects light-acclimation state: high-light-acclimated cells typically have lower PSII:PSI ratios than low-light-acclimated cells. Community-level photosystem stoichiometry can be linked to variable fluorescence measurements (Fv/Fm, σPSII) to constrain PSII electron transport rates and, ultimately, carbon fixation[1].

Scale of measurement

Each filtered sample provides a point measurement. Protein turnover is slower than mRNA, so photosystem protein concentrations integrate the physiological state over hours to days. Diurnal patterns in PSII:PSI ratios have been observed in some taxa.

Data generated

Absolute or relative concentrations of D1, PsaA, and PsaB proteins per cell or per unit volume. The PSII:PSI ratio is used to characterize light-acclimation state. When combined with carbon fixation data, the protein-specific rate of carbon fixation can be derived.

Units & currency

Units are mol protein per cell, mg protein L-1, or protein mass fraction. The currency is protein (carbon fixation is derived).

Sample size

Typical samples are ~1 L in volume.

Repositories & databases

Limitations

Peptide standards and antibodies may not capture the full diversity of D1, PsaA, and PsaB variants across the community. Post-translational modifications affect antibody recognition and activity. Total protein per liter is difficult to measure accurately in dilute open-ocean waters. Models linking photosystem stoichiometry to carbon fixation rates are still being developed and validated.

Example Applications & Protocols

Classic examples

  • Campbell et al. (2003) Analysing photosynthetic complexes in uncharacterized species or mixed microalgal communities using global antibodies [1]

Recent applications

  • Macey et al. (2014) Photosynthetic protein stoichiometry and photophysiology in the high latitude North Atlantic [2]

Common calculations/conversions

  • ETRPSII per unit volume = [PSII] × kPSII; where kPSII (s-1) is the PSII-specific photochemical rate derived from σPSII and irradiance.

References

  1. 1.0 1.1 Campbell, D. A., Cockshutt, A. M., & Porankiewicz-Asplund, J. (2003). Analysing photosynthetic complexes in uncharacterized species or mixed microalgal communities using global antibodies. Physiologia Plantarum, 119(3), 322–327. https://doi.org/10.1034/j.1399-3054.2003.00175.x
  2. Macey, A. I., Ryan-Keogh, T., Richier, S., Moore, C. M., & Bibby, T. S. (2014). Photosynthetic protein stoichiometry and photophysiology in the high latitude North Atlantic. Limnology and Oceanography, 59(6), 1853–1864. https://doi.org/10.4319/lo.2014.59.6.1853