Soil plant atmosphere continuum Soil plant atmosphere continuum The soil-plant-atmosphere continuum (SPAC) is the pathway for water moving from soil through plants to the atmosphere. Continuum in the description highlights the continuous nature of water connection through the pathway. The low water potential of the atmosphere, and relatively higher (i.e. less negative) water potential inside leaves, leads to a diffusion gradient across the stomatal pores of leaves, drawing water out of the leaves as vapour. As water vapour transpires out of the leaf, further water molecules evaporate off the surface of mesophyll cells to replace the lost molecules since water in the air inside
Zero ionic layer studies that use exocytotic SNAREs of yeast as models, a mutation from glutamine to arginine in the zero ionic layer leads to yeast cells that have deficient growth and protein secretion ability. However, a mutation from arginine to glutamine in this layer leads to yeast cells that are functionally wild-type. In the mutation where all four amino acids in the zero ionic layer are glutamine residues, the cells still exhibit normal secretory ability, but defects may become pronounced when there are other mutations. Complementary mutations, where a glutamine to arginine mutation is paired with an arginine to glutamine mutation in