长期干燥粪便样本的寄生虫学研究。

R. Samuels
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Anthropo logically, the intestinal animal parasites infect ing the group can give a measure of various habits that pertain to hygiene, living conditions, and foods. Biologically, it is of interest to know both the antiquity and earlier geographic distri bution of a group of organisms and to determine if there have been any changes. All the fecal specimens were, of course, in a dry state. The fact that they have remained recognizable suggests that they dried rapidly; otherwise they would have disintegrated in a short time. Fast drying would also have been favorable for the preservation of certain para sites and their products before autolysis and microorganisms could destroy them. Particu larly, it was expected that portions of intestinal worms, if present, might have survived in recog nizable form. Nematodes (roundworms) possess a cuticle which is highly resistant to biological and chemical activity, and this would still be recognizable even if the soft tissues had decom posed. This is true of all stages, egg to adult, and for different organisms any of the stages may appear in feces. Platyhelminths (flat worms) have fewer structures which would last as well, but there is some possibility of remains. The probability of finding recognizable remnants of protozoan parasites seemed much more re mote. Recognizable traces of trophozoites in the unprotected, motile forms would be most un likely; the cysts, although encased in a wall, 1 This is Contribution No. 29 of the Wetherill Mesa Archeological Project. would not be much more resistant to such severe treatment. The pressure and distortion of drying would probably have rendered such small objects unrecognizable. Severe drying of the specimens to the parch mentlike or stony objects found was thus a mixed blessing. In diagnostic laboratory prac tice, dried material is not considered suitable for analysis and is rejected. Since it was im possible to find material of better quality, it was necessary to find a method, or methods, suited to these special circumstances. Any technique to be used would have to rehydrate without severe chemical damage. Crushing the material, as a preliminary step, was also inadvisable, since large objects, such as worms, might easily be broken into unrecognizable fragments. Materials and Methods The fecal specimens were excavated by proj ect personnel at a number of sites, primarily at Long House and Mug House. Identification of the material as being of human origin was made by Olaus Murie and Douglas Osborne. On an empirical basis, denaturing of protein and precipitation of salts in drying, were the chief problems in reclaiming the material for study. Basic solutions with cation-sequestering properties were tried at various concentrations and temperatures. Glycerol and other penetrat ing and wetting agents, such as detergents, were also used initially. The final procedure evolved was quite simple. A large fragment of the speci men, 1 to 5 cm. in diameter, was detached with as little crushing as possible, weighed, and placed in a beaker. For each gram of feces, 20 ml. of rehydrating solution were added, and the beaker was then placed in the refrigerator for 24 to 72 hours. The beaker was swirled gently several times a day to aid penetration and dissolution of the specimen. The solution most used has been 2% (w/v) sodium hydroxide plus .5% (w/v) ethylenedinitrilo tetraacetic acid disodium salt (disodium EDTA). About 20 specimens were studied in detail with this technique. When the specimen had softened and mixed, a preliminary search for larger specimens was made with a hand lens; none was found. 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Recognizable traces of trophozoites in the unprotected, motile forms would be most un likely; the cysts, although encased in a wall, 1 This is Contribution No. 29 of the Wetherill Mesa Archeological Project. would not be much more resistant to such severe treatment. The pressure and distortion of drying would probably have rendered such small objects unrecognizable. Severe drying of the specimens to the parch mentlike or stony objects found was thus a mixed blessing. In diagnostic laboratory prac tice, dried material is not considered suitable for analysis and is rejected. Since it was im possible to find material of better quality, it was necessary to find a method, or methods, suited to these special circumstances. Any technique to be used would have to rehydrate without severe chemical damage. Crushing the material, as a preliminary step, was also inadvisable, since large objects, such as worms, might easily be broken into unrecognizable fragments. 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引用次数: 41

摘要

用碱性螯合液(冷)复水干燥的古人类粪便标本。是否发现了一种人类动物寄生虫的确凿证据?蛭状肠虫的卵。一个标本中有横纹肌样线虫,许多标本中有螨虫,可能在粪便沉积后逃逸。如果线虫是一种玉米寄生虫,如果数量足够大,它们可能会造成作物损失。不同地层标本中螨虫的镇静作用可能为Mesa Verde地区螨虫的进化提供证据。在L Wetherill M sa悬崖民居的遗迹中,有一些人类粪便标本。由于在人类粪便中发现了许多人类寄生虫的证据,因此对这些遗骸进行研究的可能价值立即显现出来。从人类学的逻辑上讲,感染人群的肠道动物寄生虫可以衡量与卫生、生活条件和食物有关的各种习惯。在生物学上,了解一组生物的古代和早期地理分布,并确定是否有任何变化,是很有意义的。当然,所有的粪便标本都处于干燥状态。它们仍然可以辨认的事实表明,它们干得很快;否则它们会在短时间内解体。快速干燥也有利于某些对位及其产物在自溶和微生物破坏它们之前的保存。特别是,人们预计肠道蠕虫的一部分,如果存在的话,可能以可识别的形式存活下来。线虫(蛔虫)具有高度抵抗生物和化学活动的角质层,即使软组织已经腐烂,它仍然可以识别。从卵到成虫的所有阶段都是如此,对于不同的生物体,任何阶段都可能出现在粪便中。白嘴虫(扁平蠕虫)的结构也更少,可以保存下来,但也有可能保留下来。找到可识别的原生动物寄生虫残留物的可能性似乎要小得多。在未受保护的、可运动的形态中发现滋养体的可识别痕迹是最不可能的;这是Wetherill Mesa考古项目的第29号贡献品。对这种严酷的治疗不会有更强的抵抗力。干燥的压力和变形可能会使这些小物体变得无法辨认。因此,对于发现的干燥的或石质的物体来说,标本的严重干燥是一件好坏参半的事情。在诊断实验室实践中,干燥的材料被认为不适合分析而被拒绝。由于不可能找到质量更好的材料,因此有必要找到一种或几种适合这些特殊情况的方法。使用的任何技术都必须在不造成严重化学损害的情况下进行补水。作为第一步,粉碎材料也是不可取的,因为像蠕虫这样的大物体很容易被打碎成无法辨认的碎片。材料和方法粪便标本由项目人员在许多地点挖掘,主要是在Long House和Mug House。奥劳斯·穆里和道格拉斯·奥斯本鉴定出这些材料是人类的。在经验基础上,蛋白质的变性和干燥过程中盐的沉淀是回收研究的主要问题。在不同浓度和温度下,对具有阳离子隔离特性的碱性溶液进行了试验。甘油和其他渗透和润湿剂,如洗涤剂,最初也被使用。最后的步骤很简单。标本的大碎片,1至5厘米。直径,分离与尽可能少的挤压,称重,并放置在一个烧杯。每克粪便加入20毫升复水化液,将烧杯放入冰箱冷藏24 ~ 72小时。烧杯每天轻轻旋转几次,以帮助试样的渗透和溶解。最常用的溶液是2% (w/v)氢氧化钠加0.5% (w/v)乙二腈四乙酸二钠(EDTA二钠)。用这种方法对20个标本进行了详细的研究。当标本软化并混合后,用手透镜对较大的标本进行初步搜索;没有找到。然后将沉积物样本移液到
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Parasitological study of long-dried fecal samples.
To rehydrate dried, ancient human fecal specimens an alkaline chelating solution (cold) was used. Identi fiable evidence of one animal parasite of man was found ? the eggs of Enterobius vermicularis. Rhabditoid nema todes in one specimen and mites in many probably in vaded the feces after deposition. If the nematodes were a maize parasite, they might have caused crop loss, if present in large enough numbers. The sedation of mites in specimens from different strata may provide evidence concerning their evolution in the Mesa Verde area. AMONG the remains of occupation at the L Wetherill M sa cliff dwellings were a num ber of human fecal specimens. Since evidences of many human parasites are found in man's feces, the possible value of a study of these re mains was immediately apparent. Anthropo logically, the intestinal animal parasites infect ing the group can give a measure of various habits that pertain to hygiene, living conditions, and foods. Biologically, it is of interest to know both the antiquity and earlier geographic distri bution of a group of organisms and to determine if there have been any changes. All the fecal specimens were, of course, in a dry state. The fact that they have remained recognizable suggests that they dried rapidly; otherwise they would have disintegrated in a short time. Fast drying would also have been favorable for the preservation of certain para sites and their products before autolysis and microorganisms could destroy them. Particu larly, it was expected that portions of intestinal worms, if present, might have survived in recog nizable form. Nematodes (roundworms) possess a cuticle which is highly resistant to biological and chemical activity, and this would still be recognizable even if the soft tissues had decom posed. This is true of all stages, egg to adult, and for different organisms any of the stages may appear in feces. Platyhelminths (flat worms) have fewer structures which would last as well, but there is some possibility of remains. The probability of finding recognizable remnants of protozoan parasites seemed much more re mote. Recognizable traces of trophozoites in the unprotected, motile forms would be most un likely; the cysts, although encased in a wall, 1 This is Contribution No. 29 of the Wetherill Mesa Archeological Project. would not be much more resistant to such severe treatment. The pressure and distortion of drying would probably have rendered such small objects unrecognizable. Severe drying of the specimens to the parch mentlike or stony objects found was thus a mixed blessing. In diagnostic laboratory prac tice, dried material is not considered suitable for analysis and is rejected. Since it was im possible to find material of better quality, it was necessary to find a method, or methods, suited to these special circumstances. Any technique to be used would have to rehydrate without severe chemical damage. Crushing the material, as a preliminary step, was also inadvisable, since large objects, such as worms, might easily be broken into unrecognizable fragments. Materials and Methods The fecal specimens were excavated by proj ect personnel at a number of sites, primarily at Long House and Mug House. Identification of the material as being of human origin was made by Olaus Murie and Douglas Osborne. On an empirical basis, denaturing of protein and precipitation of salts in drying, were the chief problems in reclaiming the material for study. Basic solutions with cation-sequestering properties were tried at various concentrations and temperatures. Glycerol and other penetrat ing and wetting agents, such as detergents, were also used initially. The final procedure evolved was quite simple. A large fragment of the speci men, 1 to 5 cm. in diameter, was detached with as little crushing as possible, weighed, and placed in a beaker. For each gram of feces, 20 ml. of rehydrating solution were added, and the beaker was then placed in the refrigerator for 24 to 72 hours. The beaker was swirled gently several times a day to aid penetration and dissolution of the specimen. The solution most used has been 2% (w/v) sodium hydroxide plus .5% (w/v) ethylenedinitrilo tetraacetic acid disodium salt (disodium EDTA). About 20 specimens were studied in detail with this technique. When the specimen had softened and mixed, a preliminary search for larger specimens was made with a hand lens; none was found. A sample of the sediment was then pipetted to a
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