Pimenta A R, Oczkowski A, McKinney R, Grear J
Environmental Protection Agency, Atlantic Coastal Environmental Sciences Division, Narragansett, RI 02882, United States of America.
Reg Stud Mar Sci. 2023 Sep;62:1-14. doi: 10.1016/j.rsma.2023.102903.
This study examined geographical and seasonal patterns in carbonate chemistry and will facilitate assessment of acidification conditions and the current state of the seawater carbonate chemistry system in Narragansett Bay. Direct measurements of total alkalinity, dissolved inorganic carbon, dissolved oxygen percent saturation, water temperature, salinity and pressure were performed during monthly sampling cruises carried out over three years. These measurements were used to calculate the following biologically relevant carbonate system parameters: total pH , the partial pressure of carbon dioxide in the gas phase , and the aragonite saturation state . The information provided by carbonate chemistry analysis allowed for the characterization of acidification events which have the potential to disrupt the species composition and ecological functioning of coastal biological communities and threaten commercially important aquatic life. We found very robust relationships between salinity and total alkalinity and between salinity and dissolved inorganic carbon that persisted through all regions, seasons, and depth-layers with mixing of coastal waters with freshwater entering in the upper bay being an important driver on alkalinity and dissolved inorganic carbon distributions. We compared the metabolically linked calculated carbonate system parameters with dissolved oxygen (DO) saturation and found high correlation, with DO percent saturation exhibiting robust correlation with the calculated carbonate system parameters total pH and with partial pressure of carbon dioxide in the gas phase . Using a statistical model to correct for the confounded effects of time and space that are a common challenge in marine survey design, we found that acidification events occurred in the Northern Region of the bay, primarily during the Summer and Fall, and likely due to a combination of microbial respiration and stratification. These acidification events, especially in the Northern Region, have the potential to adversely impact aquatic life.
本研究考察了碳酸盐化学的地理和季节模式,将有助于评估纳拉甘西特湾的酸化状况以及海水碳酸盐化学系统的当前状态。在三年间每月进行的采样航次中,对总碱度、溶解无机碳、溶解氧饱和度百分比、水温、盐度和压力进行了直接测量。这些测量数据用于计算以下与生物相关的碳酸盐系统参数:总pH值、气相中二氧化碳的分压以及文石饱和状态。碳酸盐化学分析提供的信息有助于表征酸化事件,这些事件有可能破坏沿海生物群落的物种组成和生态功能,并威胁到具有商业重要性的水生生物。我们发现盐度与总碱度之间以及盐度与溶解无机碳之间存在非常显著的关系,这种关系在所有区域、季节和深度层都持续存在,上湾中沿海水与淡水的混合是碱度和溶解无机碳分布的一个重要驱动因素。我们将与代谢相关的计算出的碳酸盐系统参数与溶解氧(DO)饱和度进行了比较,发现二者具有高度相关性,DO饱和度百分比与计算出的碳酸盐系统参数总pH值以及气相中二氧化碳的分压呈现出显著相关性。通过使用统计模型来校正时间和空间的混杂效应(这是海洋调查设计中常见的挑战),我们发现该湾北部区域发生了酸化事件,主要发生在夏季和秋季,可能是微生物呼吸和分层共同作用的结果。这些酸化事件,尤其是在北部区域,有可能对水生生物产生不利影响。