The evolutionary hypothesis of benign paroxysmal positional vertigo

Human otoliths, primarily formed from salts of calcium and carbonate, are different from bones of the skeleton, which are composed of calcium phosphate. The echinoderms, which share the earliest common ancestor with us, began to protect the body by making an endoskeleton out of calcium and carbon dioxide dissolved in the sea. In subsequent vertebrates, aerobic respiration supported strong muscle activity, but an occasional shortage of oxygen led to low pH due to the accumulation of lactate produced by anaerobic respiration, increasing the risk of melting bones composed of calcium carbonate. So, all vertebrates used calcium phosphate to increase bone strength, having a stronger ionic bonding than calcium carbonate. But otoliths, which are in the inner ear and thereby not connected to muscles, still use calcium carbonate. Benign paroxysmal positional vertigo (BPPV) is a disorder in which otoliths detached from the utricle enter the semicircular canals and cause a sense of rotation. Otoliths, the calcium carbonate ear bones retaining a long evolutionary history, can be easily broken at low pH. During sleep, shallow breathing produces mild respiratory acidosis and low pH in the blood. Since otoliths are corroded at low pH during nighttime, BPPV occurs frequently in the morning. In addition, diabetes mellitus or gout often decreases pH in the blood and increases the occurrence of BPPV.