Kage Azusa, Asato Eriko, Chiba Yoko, Wada Yuuko, Katsu-Kimura Yumiko, Kubota Ayami, Sawai Satoe, Niihori Maki, Baba Shoji A, Mogami Yoshihiro
Graduate School of Humanities and Sciences, Ochanomizu University, Otsuka, Tokyo 112-8610, Japan.
Zoolog Sci. 2011 Mar;28(3):206-14. doi: 10.2108/zsj.28.206.
Bioconvection emerges in a dense suspension of swimming protists as a consequence of their negative-gravitactic upward migration and later settling as a blob of density greater than that of water. Thus, gravity is an important parameter governing bioconvective pattern formation. However, inconsistencies are found in previous studies dealing with the response of bioconvection patterns to increased gravity acceleration (hypergravity); the wave number of the patterns has been reported to decrease during the hypergravity phases of parabolic aircraft flight, while it increases in centrifugal hypergravity. In this paper, we reassess the responses of bioconvection to altered gravity during parabolic flight on the basis of vertical and horizontal observations of the patterns formed by Tetrahymena thermophila and Chlamydomonas reinhardtii. Spatiotemporal analyses of the horizontal patterns revealed an increase in the pattern wave number in both pre- and post-parabola hypergravity. Vertical pattern analysis was generally in line with the horizontal pattern analysis, and further revealed that hypergravity-induced changes preceded at the top layer of the suspensions while microgravity-induced changes appeared to occur from the bottom part of the settling blobs. The responses to altered gravity were rather different between the two sample species: T. thermophila tended to drastically modify its bioconvection patterns in response to changes in gravity level, while the patterns of C. reinhardtii responded to a much lesser extent. This difference can be attributed to the distinct physical and physiological properties of the individual organisms, suggesting a significant contribution of the gyrotactic property to the swimming behavior of some protists.
生物对流出现在游动原生生物的密集悬浮液中,这是它们负重力向上迁移以及随后以密度大于水的液滴形式沉降的结果。因此,重力是控制生物对流模式形成的一个重要参数。然而,在之前关于生物对流模式对重力加速度增加(超重力)响应的研究中发现了不一致之处;据报道,在抛物线飞机飞行的超重力阶段,模式的波数会减小,而在离心超重力中则会增加。在本文中,我们基于对嗜热四膜虫和莱茵衣藻形成的模式进行的垂直和水平观测,重新评估抛物线飞行过程中生物对流对重力变化的响应。对水平模式的时空分析表明,在抛物线前后的超重力阶段,模式波数均增加。垂直模式分析总体上与水平模式分析一致,并且进一步表明,超重力引起的变化先在悬浮液的顶层出现,而微重力引起的变化似乎从沉降液滴的底部开始。两种样本物种对重力变化的响应差异相当大:嗜热四膜虫倾向于根据重力水平的变化大幅改变其生物对流模式,而莱茵衣藻的模式响应程度要小得多。这种差异可归因于个体生物体独特的物理和生理特性,这表明趋旋性对某些原生生物的游动行为有重大贡献。