Fluctuating silicate:nitrate ratios and coastal plankton food webs

Marine diatoms require dissolved silicate to form an external shell, and their growth becomes Si-limited when the atomic ratio of silicate to dissolved inorganic nitrogen (Si:DIN) approaches 1:1, also known as the “Redfield ratio.” Fundamental changes in the diatom-to-zooplankton-to-higher trophic level food web should occur when this ratio falls below 1:1 and the proportion of diatoms in the phytoplankton community is reduced. We quantitatively substantiate these predictions by using a variety of data from the Mississippi River continental shelf, a system in which the Si:DIN loading ratio has declined from around 3:1 to 1:1 during this century because of land-use practices in the watershed. We suggest that, on this shelf, when the Si:DIN ratio in the river decreases to less than 1:1, then (i) copepod abundance changes from >75% to <30% of the total mesozooplankton, (ii) zooplankton fecal pellets become a minor component of the in situ primary production consumed, and (iii) bottom-water oxygen consumption rates become less dependent on relatively fast-sinking (diatom-rich) organic matter packaged mostly as zooplankton fecal pellets. This coastal ecosystem appears to be a pelagic food web dynamically poised to be either a food web composed of diatoms and copepods or one with potentially disruptive harmful algal blooms. The system is directed between these two ecosystem states by Mississippi River water quality, which is determined by land-use practices far inland.

Cell cycle regulation and cell type-specific localization of the FtsZ division initiation protein in Caulobacter.

Many genes involved in cell division and DNA replication and their protein products have been identified in bacteria; however, little is known about the cell cycle regulation of the intracellular concentration of these proteins. It has been shown that the level of the tubulin-like GTPase FtsZ is critical for the initiation of cell division in bacteria. We show that the concentration of FtsZ varies dramatically during the cell cycle of Caulobacter crescentus. Caulobacter produce two different cell types at each cell division: (i) a sessile stalked cell that can initiate DNA replication immediately after cell division and (ii) a motile swarmer cell in which DNA replication is blocked. After cell division, only the stalked cell contains FtsZ. FtsZ is synthesized slightly before the swarmer cells differentiate into stalked cells and the intracellular concentration of FtsZ is maximal at the beginning of cell division. Late in the cell cycle, after the completion of chromosome replication, the level of FtsZ decreases dramatically. This decrease is probably mostly due to the degradation of FtsZ in the swarmer compartment of the predivisional cell. Thus, the variation of FtsZ concentration parallels the pattern of DNA synthesis. Constitutive expression of FtsZ leads to defects in stalk biosynthesis suggesting a role for FtsZ in this developmental process in addition to its role in cell division.