Department of Natural Science, Hawai'i Pacific University, Honolulu, Hawai'i, USA.
Daniel K. Inouye Center for Microbial Oceanography-Research and Education, School of Ocean and Earth Science and Technology (SOEST), University of Hawai'i at Mānoa, Honolulu, Hawai'i, USA.
Appl Environ Microbiol. 2022 Mar 22;88(6):e0188421. doi: 10.1128/AEM.01884-21.
To better understand the controls on the opportunistic human pathogen Vibrio vulnificus in warm tropical waters, we conducted a year-long investigation in the Ala Wai Canal, a channelized estuary in Honolulu, HI. The abundance of V. vulnificus, as determined by quantitative PCR (qPCR) of the hemolysin gene (), varied spatially and temporally by nearly 4 orders of magnitude (≤3 to 14,000 mL). Unlike in temperate and subtropical systems, temperatures were persistently warm (19 to 31°C) and explained little of the variability in V. vulnificus abundance. Salinity (1 to 36 ppt) had a significant, but nonlinear, relationship with V. vulnificus abundance with the highest concentrations (>2,500 mL) observed only at salinities from 7 to 22 ppt. V. vulnificus abundances were lower on average during the summer dry season, when waters were warmer but more saline. The highest canal-wide average abundances were observed during a time of modest rainfall, when moderate salinities and elevated concentrations of reduced nitrogen species and silica suggested a groundwater influence. Parallel quantification of the gene suggested that C-type strains, which are responsible for most human infections, comprised 25% of the total V. vulnificus on average, but their relative contribution was greater at higher salinities, suggesting a broader salinity tolerance. Generalized regression models suggested that up to 67% of sample-to-sample variation ( = 202) in log-transformed V. vulnificus abundance was explained using the measured environmental variables, and up to 97% of the monthly variation in canal-wide average concentrations ( = 13) was explained with the best subset of four variables. Our data illustrate that, in the absence of strong seasonal variation in water temperature in the tropics, variation in salinity driven by rainfall becomes a primary controlling variable on V. vulnificus abundance. There is thus a tendency for a rainfall-driven seasonal cycle in V. vulnificus abundance which is inverted from the temperature-driven seasonal cycle at higher latitudes. However, stochasticity in rainfall and its nonlinear, indirect effects on V. vulnificus concentration means that high abundances can occur at any location in the canal at any time of year, making it challenging to predict concentrations of this pathogen at a high temporal or spatial resolution. Much of the variability in canal-wide average concentrations, on the other hand, was explained by a few variables that reflect the magnitude of freshwater input to the system, suggesting that relative risk of exposure to this pathogen could be predicted as an average for the system.
为了更好地了解温暖热带水域中机会性病原体创伤弧菌的控制因素,我们对夏威夷火奴鲁鲁的 Ala Wai 运河进行了为期一年的调查。通过定量 PCR(qPCR)对溶血素基因()的检测,创伤弧菌的丰度在空间和时间上变化了近 4 个数量级(≤3 至 14,000mL)。与温带和亚热带系统不同,温度持续温暖(19 至 31°C),但对创伤弧菌丰度的变化解释不大。盐度(1 至 36 ppt)与创伤弧菌丰度呈显著但非线性关系,最高浓度(>2,500mL)仅在盐度为 7 至 22 ppt 时观察到。在夏季旱季,当水温升高但盐度升高时,平均而言,运河中的创伤弧菌丰度较低。在适度降雨期间,观察到运河内平均丰度最高,此时中等盐度和升高的还原氮物种和硅浓度表明存在地下水影响。平行定量的 基因表明,负责大多数人类感染的 C 型菌株平均占创伤弧菌总数的 25%,但在较高盐度下其相对贡献更大,表明其具有更广泛的盐度耐受性。广义回归模型表明,使用测量的环境变量可以解释多达 67%的样本间变异( = 202),并且可以用最佳的四个变量子集解释高达 97%的运河内平均浓度( = 13)的月变化。我们的数据表明,在热带地区水温没有强烈季节性变化的情况下,降雨驱动的盐度变化成为创伤弧菌丰度的主要控制变量。因此,创伤弧菌丰度会出现一个由降雨驱动的季节性循环,与高纬度地区由温度驱动的季节性循环相反。然而,降雨的随机性及其对创伤弧菌浓度的间接非线性影响意味着,在一年中的任何时间,该病原体的高丰度都可能在运河的任何位置出现,这使得很难在高时间或空间分辨率下预测这种病原体的浓度。另一方面,运河内平均浓度的大部分变化可以用反映系统淡水输入量的几个变量来解释,这表明可以预测该病原体的相对暴露风险作为系统的平均值。