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多细胞趋磁原核生物的游动极性在使用磁体的分离过程中可能会发生变化:游动极性与磁矩强度之间关系的证据。

The swimming polarity of multicellular magnetotactic prokaryotes can change during an isolation process employing magnets: evidence of a relation between swimming polarity and magnetic moment intensity.

作者信息

de Melo Roger Duarte, Acosta-Avalos Daniel

机构信息

Centro Brasileiro de Pesquisas Fisicas, Rua Xavier Sigaud 150, Urca, Rio de Janeiro, RJ, CEP 22290-180, Brazil.

出版信息

Eur Biophys J. 2017 Sep;46(6):533-539. doi: 10.1007/s00249-017-1199-5. Epub 2017 Feb 4.

DOI:10.1007/s00249-017-1199-5
PMID:28161748
Abstract

Magnetotactic microorganisms are characterized by swimming in the direction of an applied magnetic field. In nature, two types of swimming polarity have been observed: north-seeking microorganisms that swim in the same direction as the magnetic field, and south-seeking microorganisms that swim in the opposite direction. The present work studies the reversal in the swimming polarity of the multicellular magnetotactic prokaryote Candidatus Magnetoglobus multicellularis following an isolation process using high magnetic fields from magnets. The proportion of north- and south-seeking organisms was counted as a function of the magnetic field intensity used during the isolation of the organisms from sediment. It was observed that the proportion of north-seeking organisms increased when the magnetic field was increased. The magnetic moment for north- and south-seeking populations was estimated using the U-turn method. The average magnetic moment was higher for north- than south-seeking organisms. The results suggest that the reversal of swimming polarity must occur during the isolation process in the presence of high magnetic fields and magnetic field gradients. It is shown for the first time that the swimming polarity reversal depends on the magnetic moment intensity of multicellular magnetotactic prokaryotes, and new studies must be undertaken to understand the role of magnetic moment polarity and oxygen gradients in determination of swimming polarity.

摘要

趋磁微生物的特点是沿外加磁场方向游动。在自然界中,已观察到两种游动极性类型:向北游动的微生物,其游动方向与磁场方向相同;向南游动的微生物,其游动方向与磁场方向相反。本研究探讨了多细胞趋磁原核生物球形趋磁球菌(Candidatus Magnetoglobus multicellularis)在使用磁体产生的强磁场进行分离过程后游动极性的反转。向北和向南游动的生物体比例作为从沉积物中分离生物体时所用磁场强度的函数进行计数。观察到随着磁场增强,向北游动的生物体比例增加。使用掉头法估算向北和向南游动群体的磁矩。向北游动的生物体的平均磁矩高于向南游动的生物体。结果表明,游动极性的反转必定发生在存在强磁场和磁场梯度的分离过程中。首次表明,游动极性反转取决于多细胞趋磁原核生物的磁矩强度,必须开展新的研究以了解磁矩极性和氧梯度在确定游动极性中的作用。

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引用本文的文献

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3
U-turn trajectories of magnetotactic cocci allow the study of the correlation between their magnetic moment, volume and velocity.

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