Gout, with a section on ocular disease in the gouty

by Llewellyn J. Llewellyn

Now, as we hope to show later, whatever be the proximate cause of gout it is at any rate not uric acid. The fact, too, that higher degrees of lithæmia are to be met with in conditions, not even remotely connected with gout, renders it impossible to accept the view that the excess of urates in the blood is responsible for all the varied symptoms accredited by Murchison and his followers to lithæmia. For the same reason, it is difficult to uphold the hypothesis that “the tendency to lithæmia in early life may be an early expression of the ‘gouty’ diathesis.”

In short, excess of uric acid in the blood or lithæmia is not pathognomonic of gout, much less of “potential” gout. But further discussion of this assumed relationship of lithæmia to gout may well be postponed until, in the light of recent blood analyses, we come to consider more narrowly the contention at one time widely held, that lithæmia is an irregular manifestation of gout.

If we are compelled to adopt a more judicial attitude in regard to lithæmia, what of the similar assumptions as to the relationship of lithuria or lithiasis to gout? Now lithuria, like lithæmia, was and probably still is by some held to be an inherited “gouty” proclivity. Sufferers in youth from lithiasis were deemed likely to develop gout in later years. Not only was lithiasis observed to precede but also to be a concomitant or sequel to gout. Nevertheless, although uric acid, gravel and calculi, sometimes arise in those of “gouty” diathesis, these instances are but isolated, so rare indeed as to entitle them to be regarded as mere coincidences. Moreover, when we recall the fact that the formation of calculi takes place in the urinary passages, i.e., outside the economy, it renders even more improbable the hypothesis that the two morbid phenomena are diverse expressions of the “gouty” diathesis.

As a matter of fact, the large bulk of “gouty” subjects are immune from gravel. Conversely, only a negligible percentage of the victims of gravel develop gout. The geographical distribution of the two disorders is wholly distinct one from the other. The Indian native is a martyr to stone, but notably exempt from gout. Coming nearer home, we find stone relatively common in Scotland, but gout rare. Plowright’s researches, too, revealed no correspondence between the incidence of gout and the prevalence of stone in the several counties of England. In some counties in which the mortality from gout was high that from stone was low, and Norfolk, the one most prolific of stone in England, enjoys comparative immunity from gout.

Reverting now to Latham’s views as to the hepatic origin of gout, we find them very similar to those formulated by Murchison. He held that the defective transmutation of glycocine into urea was responsible for the occurrence of uric acid in the urine. These chemical irregularities were attributed by him to functional disturbance or partial suspension of the normal hepatic metabolism. This, again, was referred back by him to some obscure change in the central system, viz., that part of the medulla oblongata from which the vagus takes origin.

Hyperpyræmia

Excess of carbonaceous materials in the blood was considered by Hare to be an essential, though by no means the sole factor in the genesis of gout. This same “hyperpyræmia,” as he terms it, was also, he believed, responsible for migraine, asthma, epilepsy, and other paroxysmal neuroses. For the alternation of attacks of acute articular gout with paroxysms of migraine, asthma, and epilepsy, seemed to him to indicate a kindred origin. The same inference, also, he deemed might be drawn from the well-ascertained fact that the temporary or even permanent cessation of long standing asthma, migraine, and epilepsy, might exactly coincide with the onset of acute gout.

These alternations and substitutions seem to suggest that the preceding alterations in metabolism are similar in nature, finding expression indifferently in gout, asthma, epilepsy, etc. Carbon foods, he considered, are much more likely to accumulate in the blood than the nitrogenous. Ingestion of the latter is swiftly reflected in increased elimination of nitrogenous excreta. On the other hand, following the intake of carbonaceous foodstuffs, no such rapid and proportionate increase in the excretion of carbonic acid ensues. In other words, the capacity of the organism to deal with or katabolise in response to the absorption of excess of carbon foods, is strictly limited. Muscular exercise and exposure to cold, factors which but slightly influence protein katabolism, are largely responsible for adequate carbon katabolism. Accordingly, given deficient exercise, excess of carbonaceous food and a warm temperature, an accumulation of the carbon content of the blood is favoured.

Hare considered that present day habits of warm clothing, warm rooms combined with excessive intake of starch and sugar, are precisely the favourable conditions for producing a state of hyperpyræmia. Increased fat formation would of course tend to diminish such a tendency to carbon accumulation, but this capacity in many subjects is conspicuously lacking, and may already have attained its limit.