Dikou Angela, van Woesik Robert
Department of Environment, University of the Aegean, Xenia Bld., University Hill, Mytilene 81100, Lesvos Isl., Greece.
Mar Pollut Bull. 2006 Jan;52(1):7-21. doi: 10.1016/j.marpolbul.2005.07.021. Epub 2005 Nov 15.
Six reef sites were chosen along the west coasts of Singapore's southern islands, to: (1) quantitatively assess and compare coral community composition and structure, and recruitment rates, (2) assess the relationship between the aforementioned patterns and the environmental conditions, and (3) provide insights on potential processes that incorporate history at these study sites. Chronic exposure to high sediment load was the most obvious form of anthropogenic stress. Recruitment rates on ceramic tiles were low (1.4+/-1.0-20+/-14.7 recruits m(-2)year(-1)) but decreased towards the main island of Singapore as did hard coral cover and coral density. Coral fauna consisted of genera generally found in deeper waters (e.g., fungiids, foliose Oxypora, Leptoseris, and Echinopora) or those well adapted to turbid waters (e.g., Porites, Pectinia, Leptastrea, Montipora). Light extinction coefficient (K) and % live coral cover (%LCC) showed a strong and inverse curvilinear relationship (%LCC=13.60 *K(-3.40)). Similarly, the rate of sediment deposition (DFSPM) (Recruitment rate, RR=1.51-0.17 *DFSPM) and water clarity (RR=3.56-2.92 *K) exhibited strong and inverse relationships with recruitment rates. Although measured levels of the down-ward flux of suspended particulate matter and suspended solids were well within "normal" levels recorded in the literature, it was the proportion of benthic space, generic coral composition, and site history that offered compelling evidence of chronic exposure to increased sediment load. Clearly a reduction in both water clarity and live-coral cover has taken place since monitoring efforts began in the early 1970s, in fact coral cover has more than halved at all sites examined since the 1980s and benthic space was predominantly occupied by dead corals covered with sediment and filamentous algae.
在新加坡南部岛屿的西海岸选择了六个珊瑚礁地点,目的是:(1)定量评估和比较珊瑚群落的组成、结构及补充率;(2)评估上述模式与环境条件之间的关系;(3)深入了解这些研究地点纳入历史的潜在过程。长期暴露于高沉积物负荷是最明显的人为压力形式。瓷砖上的补充率较低(1.4±1.0 - 20±14.7个补充个体/平方米·年),但随着靠近新加坡主岛,其补充率、硬珊瑚覆盖率和珊瑚密度均呈下降趋势。珊瑚动物群包括通常在较深水域发现的属(如石芝珊瑚、叶状刺孔珊瑚、薄星珊瑚和刺星珊瑚)或那些适应浑浊水域的属(如鹿角珊瑚、梳状珊瑚、瘦长星珊瑚、蔷薇珊瑚)。光消光系数(K)和活珊瑚覆盖率(%LCC)呈现出强烈的反曲线关系(%LCC = 13.60×K^(-3.40))。同样,沉积物沉积速率(DFSPM)(补充率,RR = 1.51 - 0.17×DFSPM)和水体透明度(RR = 3.56 - 2.92×K)与补充率呈现出强烈的反比关系。尽管测量的悬浮颗粒物和悬浮固体向下通量水平完全在文献记录的“正常”水平范围内,但底栖空间比例、珊瑚属组成和地点历史为长期暴露于增加的沉积物负荷提供了有力证据。自20世纪70年代初开始监测以来,水体透明度和活珊瑚覆盖率明显下降,事实上,自20世纪80年代以来,所有检查地点的珊瑚覆盖率均减少了一半以上,底栖空间主要被覆盖着沉积物和丝状藻类的死珊瑚占据。