Lacy G H, Swatek F E
Appl Microbiol. 1974 Feb;27(2):379-88. doi: 10.1128/am.27.2.379-388.1974.
Outbreaks of coccidioidomycosis and isolation of Coccidioides immitis have been reported from Amerindian middens. This study was undertaken to determine the most important ecological component(s) for the occurrence of C. immitis at archeological sites. Soils from 10 former Indian villages with no prior history of coccidioidal infection were collected and cultured. The physicochemical properties of the midden soils were compared with nonmidden soils and positive soils. The following theories for the sporadic distribution of the pathogen in the soil of the Lower Sonoran Life Zone were considered: (i) the Larrea tridentata (creosote bush) association, (ii) the preference for saline soils, (iii) isolation near rodent burrows, and (iv) animals as possible agents of dispersal. Results showed that a high percentage of the midden soils contained C. immitis, whereas none of the adjacent, nonmidden soils yielded the fungus. Physicochemical analyses revealed that the dark color and alkaline pH of the midden soils were due to past organic contamination. Repeated isolations were made from soils with low to moderate alkalinity. Alkalinity and sandy texture were consistent features of all soils in this study. However, the lack of any reports of nonsandy infested soils possibly indicates that the sandy texture and alkalinity may be factors in the distribution of this fungus. The organic content, soil parent material, and color were not important in the soil ecology. L. tridentata was not significant in the macroflora at the infested sites surveyed. Samples collected without reference to rodent burrows yielded a high percentage of recoveries. Animals, although not the major natural reservoir, cannot be ignored as possible factors in the ecology of C. immitis.
美洲印第安人的贝丘中曾有球孢子菌病爆发及粗球孢子菌分离的报道。本研究旨在确定考古遗址中粗球孢子菌出现的最重要生态因素。采集了10个以前没有球孢子菌感染病史的印第安村庄的土壤并进行培养。将贝丘土壤的理化性质与非贝丘土壤及阳性土壤进行比较。考虑了以下关于该病原体在下索诺兰生命带土壤中散发分布的理论:(i)三齿拉瑞阿(牧豆树)群落,(ii)对盐渍土的偏好,(iii)在啮齿动物洞穴附近的隔离,以及(iv)动物作为可能的传播媒介。结果显示,贝丘土壤中有很大比例含有粗球孢子菌,而相邻的非贝丘土壤均未分离出该真菌。理化分析表明,贝丘土壤的深色和碱性pH值是过去有机污染所致。从低至中度碱度的土壤中反复分离出该菌。碱度和沙质质地是本研究中所有土壤的一致特征。然而,没有关于非沙质感染土壤的任何报道,这可能表明沙质质地和碱度可能是该真菌分布的因素。有机含量、土壤母质和颜色在土壤生态学中并不重要。在所调查的受感染地点的大型植物区系中,三齿拉瑞阿并不显著。不参照啮齿动物洞穴采集的样本回收率很高。动物虽然不是主要的天然宿主,但作为粗球孢子菌生态学中的可能因素不能被忽视。