潮汐周期和一天中的时间控制着西印度洋沿海栖息地的pH值:坦桑尼亚的Mnazi和Chwaka海湾的例子

Rushingisha George, B.R. Lugendo
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引用次数: 1

摘要

海洋酸化是由于从大气中吸收二氧化碳(CO2)而导致的pH值逐渐下降和海水碳酸盐化学变化,这是一个日益严重的威胁海洋物种的危机。在西印度洋沿海水域,与物种自然栖息地有关的pH值数据仍然很少,这限制了开展操作性研究以更好地了解海洋酸化对海洋物种的影响的能力。本研究以坦桑尼亚为例,调查了WIO红树林、海草和珊瑚礁生境的潮汐和昼夜pH值变化。海岸带生境的平均pH以海草最高(8.49±0.29),珊瑚礁次之(8.33±0.06),红树林最低(8.20±0.17)。海草生境在大潮低潮时白天pH值最高(9.06),红树林生境在大潮高潮时白天pH值最高(8.45),珊瑚礁生境在低潮时白天pH值最高(8.47)。海草生境pH值范围最大(1.03),其次是红树林(0.54),珊瑚礁生境pH值范围最小(0.23)。白天pH值最高的水在涨潮时被输送到附近的红树林生境,在退潮时被输送到珊瑚礁生境,导致春季涨潮和退潮时红树林和珊瑚礁生境的平均pH值分别最高。海草生境pH值与温度(r=0.80)、溶解氧(r=0.84)、盐度(r=0.72)呈正相关,红树林生境pH值与溶解氧呈正相关(r=0.59)。本研究提供了有关WIO沿海栖息地pH值随时间和空间波动的现场证据,来自海草栖息地的水能够在白天提高附近红树林和珊瑚礁栖息地水的pH值,从而可能有助于减轻海洋酸化对这些栖息地的影响。
本文章由计算机程序翻译,如有差异,请以英文原文为准。
Tidal cycle and time of day control pH levels in coastal habitats of the western Indian Ocean: the case of Mnazi and Chwaka Bays in Tanzania
Ocean acidification, a progressive decrease in the pH and change in the carbonate chemistry of seawater caused by the uptake of carbon dioxide (CO2) from the atmosphere, is a growing crisis that threatens marine species. pH data relevant to a species’ natural habitat in the coastal waters of the western Indian Ocean (WIO) is still sparse, limiting the capacity to undertake manipulative studies to better understand the impacts of ocean acidification on marine species. This study investigated tidal and day-night pH variations in mangrove, seagrass, and coral reef habitats of the WIO by using Tanzania as a case study. The mean pH of the studied coastal habitats was highest in seagrass (8.49 ± 0.29), followed by coral reef (8.33 ± 0.06), and lowest in mangrove (8.20 ± 0.17). Seagrass habitats had the highest pH (9.06) during the day at low spring tides, mangrove habitats had the highest pH (8.45) during the day at high spring tides, and coral reef habitats had the highest pH (8.47) during the day at low tides. Seagrass habitats had the widest pH range (1.03), followed by mangrove habitats (0.54), while coral reef habitats had the narrowest range (0.23). The water with the highest pH during the day was transported to nearby mangrove habitats during incoming tides and to coral reef habitats during outgoing tides, resulting in the highest mean pH in mangrove and coral reef habitats during spring high and low tides, respectively. pH within the seagrass habitats correlated strongly and positively with changes in temperature (r=0.80), dissolved oxygen (r=0.84), and salinity (r=0.72), while pH in mangrove habitats correlated moderately and positively with dissolved oxygen (r=0.59). This study provides in-situ evidence on the pH fluctuations in the WIO’s coastal habitats over time and space, with water from seagrass habitats capable of raising the pH of water in nearby mangrove and coral reef habitats during the day, thereby potentially helping in the mitigation of the effects of ocean acidification on these habitats.
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