浮游生物的弹道:海洋原生生物的各向异性游泳行为

Rudi Schuech, Susanne Menden-Deuer
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引用次数: 35

摘要

包括单细胞原生生物在内的许多浮游生物物种的Diel垂直迁移(DVMs)在野外得到了很好的记录,并构成了许多浮游生物运输和生态学大尺度数值模型的核心组成部分。然而,描述单个原生生物运动行为的稀疏定量数据经常表明,运动只表现出几秒或数百微米量级的短期相关性,类似于更大尺度上的扩散运输——这与DVM不相容,DVM需要弹道(直线)运动。我们询问了一套广泛的三维原生动物运动轨迹,以努力确定空间和时间相关尺度。尽管运动的水平分量是扩散的,但在观察期间(长达120秒和6.1毫米),在没有重力以外的任何环境线索的情况下,几乎所有物种的垂直分量都保持高度相关(即非随机)。在之前的一些研究中,由于使用限制性容器、维度集总、各向同性分析和/或观察偏差,这些持续的运动模式可能被掩盖了,这些偏差是用固定摄像机观察自由游动的生物所固有的,我们在本研究中对此进行了解释。根据12小时的外推,保守估计原生生物在这里观察到的垂直移动范围为3-10米,而扩散的水平运动最多可导致大约10厘米的移动。因此,这些对系统发育多样性游泳原生生物的扩展观察,加上对数据各向异性的定量分析,说明了DVM的小规模机制基础。
本文章由计算机程序翻译,如有差异,请以英文原文为准。

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Going ballistic in the plankton: Anisotropic swimming behavior of marine protists

Diel vertical migrations (DVMs) of many plankton species, including single-celled protists, are well documented in the field and form a core component of many large-scale numerical models of plankton transport and ecology. However, the sparse quantitative data available describing motility behaviors of individual protists have frequently indicated that motility exhibits only short-term correlation on the order of a few seconds or hundreds of micrometers, resembling diffusive transport at larger scales—a result incompatible with DVM, which requires ballistic (straight-line) motion. We interrogated an extensive set of three-dimensional protistan movement trajectories in an effort to identify spatial and temporal correlation scales. Whereas the horizontal components of movement were diffusive, the vertical component remained highly correlated (i.e., nonrandom) for nearly all species for the duration of observation (up to 120 s and 6.1 mm) and in the absence of any environmental cues besides gravity. These persistent motility patterns may have been obscured in some previous studies due to the use of restrictive containers, dimensionally lumped, isotropic analyses, and/or an observation bias, inherent to observing free-swimming organisms with stationary cameras, which we accounted for in this study. Extrapolated over a 12-h period, conservative estimates of vertical travel ranges for the protists observed here would be 3–10 m, while diffusive horizontal motion would result in about 10 cm of travel at most. Hence, these extended observations of phylogenetically diverse swimming protists, coupled with a quantitative analysis that accounts for anisotropy in the data, illustrate the small-scale mechanistic underpinnings of DVM.

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