Laboratorio de Produccion Primaria CINVESTAV-IPN, Unidad Mérida., Carr. Antigua a Progreso km. 6, C.P. 97310 Mérida, Yucatán, México.
Water Res. 2010 Dec;44(20):5949-64. doi: 10.1016/j.watres.2010.07.046. Epub 2010 Jul 23.
Terrestrial and oceanic influences like groundwater discharges and/or oceanic upwelling define the hydrochemical and biological characteristics of near-shore regions. In karst environments, such as the Yucatan Peninsula (SE Mexico), the balance between these two influences on spatial and temporal scales is poorly understood. This study focused on near-shore waters within 200 m offshore along the Yucatan coast. The trophic status and hydrochemical zones of the study area were determined as a function of physical and nutrient data collected from 2005 to 2006. The main terrestrial influence was groundwater discharge, while the most important marine influence was related to seasonal changes in water turbulence. Spatial differences (p < 0.05) were observed among salinity, light extinction coefficient (k), NO(3)(-), NH(4)(+), and Chl-a. Seasonal differences were observed for all variables except for k. During the dry season, terrestrial influences are the dominant factor on near-shore hydrochemistry. The region around Dzilam exhibited the maximum influence of groundwater discharge estimated by salinity dissolution (δ). During the rainy and "nortes" seasons, there is a balance between oceanic and terrestrial influences. The trophic status measured using the TRIX index, indicated that near-shore waters were mainly oligo-mesotrophic; with a meso-eutrophic status in areas with documented anthropogenic impacts. Four hydrological zones were identified by a Canonical Variate Analysis (CVA) using salinity, NO(2)(-), k and NH(4)(+) as the main discriminating variables. Zones I and II showed almost pristine conditions, with well-balanced terrestrial-oceanic influences. In Zone III, terrestrial influences such as groundwater discharges and inland pollution suggesting human impacts were dominant respect to the effects of oceanic influences like upwelling and sediment resuspension caused by winds and oceanic currents. Zone IV received enhanced groundwater and associated nutrients. Anthropogenic activities have led to ecosystem degradation but the speed at which this occurs depends on local and regional characteristics. Therefore, this study has defined those characteristics so as to enact better management policies.
陆地和海洋的影响,如地下水排放和/或海洋上升流,决定了近岸地区的水化学和生物特征。在岩溶环境中,例如尤卡坦半岛(墨西哥东南部),这两种影响在时空尺度上的平衡关系还不太清楚。本研究集中在尤卡坦海岸 200 米以内的近岸水域。根据 2005 年至 2006 年收集的物理和营养数据,确定了研究区域的营养状态和水化学带。主要的陆地影响是地下水排放,而最重要的海洋影响与水动力的季节性变化有关。在盐度、消光系数(k)、硝酸盐(NO3-)、氨(NH4+)和叶绿素 a 等方面观察到空间差异(p<0.05)。除 k 外,所有变量均观察到季节性差异。在旱季,陆地影响是近岸水化学的主要因素。Dzilam 周围地区显示出由盐度溶解(δ)估计的最大地下水排放影响。在雨季和“北风”季节,海洋和陆地影响之间存在平衡。使用 TRIX 指数测量的营养状态表明,近岸水域主要是寡营养-中营养;在有记录的人为影响的地区为中营养-富营养状态。通过使用盐度、NO2-、k 和 NH4+作为主要判别变量的典范变量分析(CVA),确定了四个水文学区。区 I 和 II 显示出几乎原始的条件,陆地-海洋影响平衡良好。在区 III 中,地下水排放和内陆污染等陆地影响占主导地位,表明人类活动的影响大于上升流和海洋流引起的风引起的海洋影响。区 IV 接收了增强的地下水和相关养分。人为活动导致了生态系统的退化,但发生的速度取决于当地和区域的特征。因此,本研究定义了这些特征,以便制定更好的管理政策。