Divalent cation distribution in dinoflagellate chromosomes imaged by high-resolution ion probe mass spectrometry.

From a variety of analytical electron microscopy experiments, the chromosomes of dinoflagellates are known to contain sizeable amounts of cations, the latter thought to contribute to the neutralization of the negative charge carried by the phosphate groups in the DNA backbone. From previous Ca and Mg chelation experiments, it is also known that these cations are necessary for the compaction and preservation of the chromosome architecture. Similar conclusions have been recently presented by our group concerning mammalian mitotic chromosomes, in studies based on secondary ion mass spectrometry (SIMS) carried out with the University of Chicago high-resolution scanning ion microprobe (UC-SIM).

Chronic acidosis-induced alteration in bone bicarbonate and phosphate.

Chronic metabolic acidosis increases urinary calcium excretion without altering intestinal calcium absorption, suggesting that bone mineral is the source of the additional urinary calcium. In vivo and in vitro studies have shown that metabolic acidosis causes a loss of mineral calcium while buffering the additional hydrogen ions. Previously, we studied changes in femoral, midcortical ion concentrations after 7 days of in vivo metabolic acidosis induced by oral ammonium chloride.

Acute acidosis-induced alteration in bone bicarbonate and phosphate.

During an acute fall in systemic pH due to a decrease in the concentration of serum bicarbonate ([HCO(3)(-)]), metabolic acidosis, there is an influx of hydrogen ions into the mineral phase of bone, buffering the decrement in pH. When bone is cultured in medium modeling acute metabolic acidosis, the influx of hydrogen ions is coupled to an efflux of sodium and potassium and a depletion of mineral carbonate. These ionic fluxes would be expected to neutralize some of the excess hydrogen ions and restore the pH toward normal.