The following are the main features which have been noticed during 1923 with regard to malaria in the Kirkuk Division of Northern Mesopotamia in dealing with indigenous natives. Treatment and preventive measures are not touched upon. There were two malaria seasons, the main one in the summer and a lesser one in the late autumn. The summer malaria season lasted roughly from the beginning of June to the middle of August. It was caused by the malignant tertian, and to a less extent by the benign tertian, parasite. The autumn malaria season occurred in late October and November, being most marked in the first half of the latter month. It was due to the malignant tertian parasite. Malaria in 1923 showed certain features which were the outcome of malaria in the preceding summer, when it was prevalent in epidemic form. The chief feature was the marked prevalence and predominance of residual quartan malaria, which existed during the first five months of the year until the starting of the malaria season. It is judged that normally quartan malaria is a comparatively common infection, and that a fuller explanation of the marked quartan predominance referred to is that it was due to residual infections from an epidemic year occurring in an area where quartan is peculiarly common. Quartan malaria was not confined to any one part of the division but was equally prevalent everywhere. Malignant tertian was the main cause of the summer and autumn malaria seasons. Infections started somewhat later than the benign form (roughly fifteen days) and rapidly disappeared with the passing of the malaria season. Crescent infections were comparatively not common. The main clinical manifestation was a quotidian fever of no great severity. Pernicious forms were absent. Benign tertian was the earliest infection to appear in any number with the opening of the malaria season. This parasite seemed to depart markedly from its usual rôle as a cause of relapses, its behaviour as regards disappearance of infection at the end of the malaria season closely resembling that of malignant tertian. There was no evidence that benign tertian was a factor in the autumn malaria season. Quartan malaria. Presumably its season of infectivity coincided with the summer malaria season. This, however, could not be proved, fresh cases being obscured by the mass of already existing quartan malaria. Triple infections were comparatively common, especially in the early months. Double infections not common. Quartan malaria, as met with, has quite sustained its reputation as the cause of an extremely chronic infection. Nomadic Arabs on the whole suffer very little from malaria. Its occurrence can be explained by their habits. During both the summer and autumn malaria season they are in fixed camping grounds, and according to the malarious nature of these grounds so will malaria among them vary. Malaria was most seen in small sections which camped alongside the fringe of villages on the edge of the desert, to the west of Kirkuk and Taza Khurmatu. The Quaraghan — Kifri — Tuz — Tauk — Taza — Kirkuk — Alton Keupri road serves as a rough line of division of malarial endemicity. On the east, or hilly side, malaria is hyperendemic and shows very high spleen rates. The area to the west or desert side shows medium spleen rates, passing to low or nil the further one goes into the desert. Malaria in the Kirkuk Division seems to be associated with— A higher degree of splenic enlargement than that usually recorded. Very high spleen rates among the children and often a comparatively high spleen rate in adults. A surprisingly low parasite rate in children and adults considering the high spleen rate. The theory is advanced that (a) is due to the prevalence of quartan malaria. It is possible that this fact also contributes to (b) and (c). Each malaria season was preceded by a marked increase of mosquito breeding, including Anopheles. A feature of the main malaria season was the fact that it lasted throughout the hottest and dryest month of the year, when the 8 a.m. mean temperature was about 90°F. and the mean relative humidity was below 30 per cent. Humidity, within limits, appeared to be a factor of comparatively little importance in influencing malarial prevalence.
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