Department of Ocean Science, The Hong Kong University of Science and Technology, Hong Kong.
College of the Environment & Ecology, Xiamen University, Xiamen 361102, China.
Sci Total Environ. 2023 Jul 15;882:163568. doi: 10.1016/j.scitotenv.2023.163568. Epub 2023 Apr 20.
Hypoxia and ocean warming are two mounting global environmental threats influencing marine ecosystems. However, the interactive effects of rising temperature and depleted dissolved oxygen (DO) on marine protists remains unknown. Here, we conducted a series of laboratory experiments on four protozoa with distinct cell sizes to investigate the combined effects of temperature (19, 22, 25, 28, and 31 °C) and oxygen availability (hypoxia, 2 mg DO L and normoxia, 7 mg DO L) on their physiological performances (i.e., growth, ingestion, and respiration rates). The hypoxia-induced inhibition in three physiological rates increased with the biovolume of the protists. As the larger surface area to volume (SA/V) quotients of smaller protists facilitate higher capabilities of oxygen absorption and utilization, the smaller protists suffered less inhibitions induced by hypoxia. Moreover, the hypoxia-induced inhibition in physiological rates was exacerbated by increasing temperature, which can be verified by the reductions in the temperature sensitivities (represented by the activation energy, E). These results suggest that hypoxia could lead to a shift of protistan community with enhanced domination of small protists, and warming could exacerbate such a trend. We further examined our laboratory results in the Pearl River Estuary, where extensive bottom hypoxia often occurs in summer. We found the mean protist biovolume in hypoxic waters was significantly lower than that at normal stations. Also, the mean protist biovolume decreased with declining DO concentration and rising temperature, indicating the interactive effect of temperature and oxygen availability. Collectively, we suggest that hypoxia could cause a higher proportion of small-sized cells in the marine protistan community, and the projected ocean warming could intensify the tendency, which could undermine the capacity of oceanic carbon sequestration.
缺氧和海洋变暖是影响海洋生态系统的两个日益严重的全球环境威胁。然而,关于温度升高和溶解氧(DO)耗尽对海洋原生动物的相互作用影响仍不清楚。在这里,我们对四种具有不同细胞大小的原生动物进行了一系列实验室实验,以研究温度(19、22、25、28 和 31°C)和氧气供应(缺氧,2 mg DO L 和正常氧,7 mg DO L)对其生理性能(即生长、摄食和呼吸速率)的综合影响。缺氧引起的三种生理速率的抑制作用随原生动物的生物体积增加而增加。由于较小原生动物的较大表面积与体积(SA/V)比率有利于更高的氧气吸收和利用能力,因此较小的原生动物受到缺氧的抑制作用较小。此外,生理速率的缺氧诱导抑制作用随温度升高而加剧,这可以通过生理速率的温度敏感性(以活化能 E 表示)的降低来验证。这些结果表明,缺氧可能导致原生动物群落发生变化,小型原生动物的主导地位增强,而变暖可能会加剧这种趋势。我们进一步在珠江口检验了我们的实验室结果,那里夏季经常出现广泛的底层缺氧。我们发现缺氧水域的原生动物平均生物体积明显低于正常站位。此外,原生动物的平均生物体积随 DO 浓度的降低和温度的升高而降低,表明温度和氧气供应的相互作用。总的来说,我们认为缺氧可能导致海洋原生动物群落中出现更高比例的小型细胞,而预计的海洋变暖可能会加剧这种趋势,从而破坏海洋碳固存的能力。