expressed as the partial pressure of CO2 in pascals; for atmospheric conditions, 1μmol/mol = 1 ppm ≈ 0.1 Pa. For modeling of photosynthesis, the more important variable is the CO2 compensation point in the absence of mitochondrial respiration, also known as the CO2 photocompensation point (Γ*), the biochemical CO2 compensation point of Rubisco. It may be measured by whole-leaf isotopic gas exchange, or be estimated in the Laisk method using an intermediate "appearant" value of C* with correction. C* approximates Γ* in the absence of carbon refixation, i.e. carbon fixation from photorespiration products. In plants, both values are lower than their counterparts. In C2 plants that operate by refixation, only C* is significantly lower. As it is not yet common to routinely change the concentration of air, the concentration points are largely theoretical derived from modeling and extrapolation, though they do hold up well in these applications. Both Γ and Γ* are linearly related to the partial pressure of oxygen (p(O2)) due to the side reaction of Rubisco. Γ is also related to temperature due to the temperature-dependence of respiration rates. It is also related to irradiation, as light is required to produce RuBP (ribulose-1,5-bisphosphate), the electron acceptor for Rubisco. At normal irradiation, there would almost always be enough RuBP; but at lwo irradiation, lack of RuBP decreases the photosynthetic activity and therefore affects Γ. The marine environment Respiration occurs by both plants and animals throughout the water column, resulting in the destruction, or usage, of organic matter, but photosynthesis can only take place via photosynthetic algae in the presence of light, nutrients and CO2. In well-mixed water columns plankton are evenly distributed, but a net production only occurs above the compensation depth. Below the compensation depth there is a net loss of organic matter. The total population of photosynthetic organisms cannot increase if the loss exceeds the net production. The compensation depth between photosynthesis and respiration of phytoplankton in the ocean must be dependent on some factors: the illumination at the surface, the transparency of the water, the biological character of the plankton present, and the temperature. The compensation point was found nearer to the surface as you move closer to the coast. It is also lower in the winter seasons in the Baltic Sea according to a study that examined the compensation point of multiple photosynthetic species. The blue portion of the visible spectrum, between 455 and 495