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石膏样小孢子菌在胱氨酸上生长时形成硫酸盐、亚硫酸盐和S-磺基半胱氨酸。

Formation of sulphate, sulphite and S-sulphocysteine by the fungus Microsporum gypseum during growth on cystine.

作者信息

Kunert J

出版信息

Folia Microbiol (Praha). 1975;20(2):142-51. doi: 10.1007/BF02876771.

Abstract

The dermatophyte Microsporum gypseum was cultivated in media containing 0.5% cystine in suspension, and 0.05% peptone or 1% glucose and 0.05% peptone. During growth on cystine the excess sulphur was oxidized and excreted into the medium not only in the form of sulphate but also in the form of sulphite. Sulphite was produced especially during first phases of growth, where its quantity was higher than that of sulphate and its maximum concentration exceeded 1 mg/ml. S-sulphocysteine, detected chromatographically and determined quantitatively, originated in large quantities by the reaction of sulphite with cystine in the medium. Both sulphite and S-sulphocysteine were further oxidized to sulphate. After exhaustion of cystine 90-93% of the sulphur present was converted to sulphate in the cultivation medium.

摘要

皮肤癣菌石膏样小孢子菌在含有0.5%胱氨酸的悬浮培养基中培养,以及在含有0.05%蛋白胨或1%葡萄糖和0.05%蛋白胨的培养基中培养。在胱氨酸上生长期间,过量的硫被氧化并以硫酸盐和亚硫酸盐的形式排泄到培养基中。亚硫酸盐尤其在生长的第一阶段产生,其数量高于硫酸盐,其最大浓度超过1mg/ml。通过色谱检测并定量测定的S-磺基半胱氨酸大量源自培养基中亚硫酸盐与胱氨酸的反应。亚硫酸盐和S-磺基半胱氨酸都进一步氧化为硫酸盐。胱氨酸耗尽后,培养基中90-93%的硫转化为硫酸盐。

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