Ruiz Marcela, López-Portillo Jorge
Rev Biol Trop. 2014 Dec;62(4):1309-30.
La Mancha lagoon is connected to the Gulf of Mexico through an estuarine ephemeral inlet, a sand bar, which opens during the rainy season and closes during the late fall and the winter storm season. As the lagoon fills up with the permanent stream flow into its Southern part, the water level increases and the sand bar opens up, releasing huge volumes of water into the ocean and leaving the previously flooded intertidal zone exposed to drying. In this study, we described the spatial and temporal variations of structure and composition of the community living on the surface of red mangrove prop roots, related to the hydrodynamic of the estuarine inlet. Four red mangrove prop roots were collected every three months, over an annual period, at ten sampling stations. Water temperature, salinity, dissolved oxygen, water depth and transparency were also measured at each sampling event. To describe the identity, abundance, biomass, and specific richness of epibiont coverage on the prop roots, measurements were taken at 10 cm intervals (herein called "horizons"). A total of 59,632 specimens and a total biomass of 172 g/cm2 were registered, and a maximum of eleven horizons presented at least one" species of epibionts. Two species of polychaetes, 12 of mollusks and 14 of crustaceans were identified, with Mytilopsis leucophaeata as the most abundant, Ficopomatus miamiensis as the most common and Crassostrea rhizophorae with the highest contribution in biomass. Sampling effort was assessed using species accumulation curves, resulting that the efficiency was, in general, greater than 90% of the richness predicted by asymptotic models. The hydrodynamics of the estuarine inlet had a great influence on the environmental conditions of the lagoon and on the spatial and temporal variation of the epibiont community: (a) when the inlet is open, there is a North-South gradient in environmental parameters (b) when the inlet is closed and the water level increases, the epibionts especially the pioneer species F. miamiensis, occupied the highest horizons of prop roots, and (c) the abundance, biomass and richness of epibionts increased towards the deeper and less saline Southern part of the lagoon, as well as on permanently submerged horizons, and during the seasonal closure of the inlet. Variations in depth are determined by the hydrodynamic behavior of the estuarine-inlet, suggesting that these factors are major biodiversity drivers of the epibiont community at La Mancha.
拉曼查泻湖通过一条河口季节性进水口与墨西哥湾相连,该进水口是一个沙洲,在雨季开放,在深秋和冬季风暴季节关闭。随着泻湖南部有永久性水流注入,水位上升,沙洲打开,大量湖水排入海洋,使先前被淹没的潮间带暴露在阳光下风干。在本研究中,我们描述了与河口进水口水动力相关的红树支柱根表面生物群落结构和组成的时空变化。在一年时间里,每隔三个月在十个采样站采集四根红树支柱根。每次采样时还测量水温、盐度、溶解氧、水深和透明度。为了描述支柱根上附生生物覆盖的种类、丰度、生物量和物种丰富度,每隔10厘米(以下称为“层位”)进行测量。共记录了59632个标本,总生物量为172克/平方厘米,最多有11个层位至少出现一种附生生物。鉴定出两种多毛类动物、12种软体动物和14种甲壳类动物,其中白带肌蛤最为丰富,迈阿密盘管虫最为常见,红树蚶的生物量贡献最高。使用物种积累曲线评估采样效率,结果表明总体效率大于渐近模型预测丰富度的90%。河口进水口的水动力对泻湖的环境条件以及附生生物群落的时空变化有很大影响:(a)当进水口开放时,环境参数存在南北梯度;(b)当进水口关闭且水位上升时,附生生物尤其是先锋物种迈阿密盘管虫占据支柱根的最高层位;(c)附生生物的丰度、生物量和丰富度在泻湖较深且盐度较低的南部区域以及永久淹没的层位,以及进水口季节性关闭期间增加。深度变化由河口进水口的水动力行为决定,这表明这些因素是拉曼查附生生物群落主要的生物多样性驱动因素。