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Seagrass sediments reveal the long-term deterioration of an estuarine ecosystem

机译:海草沉积物揭示了河口生态系统的长期恶化

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The study of a Posidonia australis sediment archive has provided a record of ecosystem dynamics and processes over the last 600years in Oyster Harbour (SW Australia). Ecosystem shifts are a widespread phenomenon in coastal areas, and this study identifies baseline conditions and the time-course of ecological change (cycles, trends, resilience and thresholds of ecosystem change) under environmental stress in seagrass-dominated ecosystem. The shifts in the concentrations of chemical elements, carbonates, sediments 0.125mm and stable carbon isotope signatures (C-13) of the organic matter were detected between 1850s and 1920s, whereas the shift detected in P concentration occurred several decades later (1960s). The first degradation phase (1850s-1950s) follows the onset of European settlement in Australia and was characterized by a strong increase in sediment accumulation rates and fine-grained particles, driven primarily by enhanced run-off due to land clearance and agriculture in the catchment. About 80% of total seagrass area at Oyster Harbour was lost during the second phase of environmental degradation (1960s until present). The sharp increase in P concentration and the increasing contribution of algae and terrestrial inputs into the sedimentary organic matter pool around 1960s provides compelling evidence of the documented eutrophication of the estuary and the subsequent loss of seagrass meadows. The results presented demonstrate the power of seagrass sedimentary archives to reconstruct the trajectories of anthropogenic pressures on estuarine ecosystem and the associated regime shifts, which can be used to improve the capacity of scientists and environmental managers to understand, predict and better manage ecological change in these ecosystems.
机译:对澳大利亚波西多尼亚沉积物档案的研究提供了过去600年牡蛎港(澳大利亚澳大利亚西南部)生态系统动力学和过程的记录。在沿海地区,生态系统变化是一种普遍现象,这项研究确定了在以海草为主的生态系统环境压力下的基线条件和生态变化的时程(周期,趋势,复原力和生态系统变化的阈值)。在1850到1920年代之间发现了有机物的化学元素,碳酸盐,沉积物<0.125mm和稳定的碳同位素特征(C-13)浓度的变化,而P浓度的变化发生在几十年后(1960年代)。 。第一个退化阶段(1850年代至1950年代)是在欧洲开始在澳大利亚定居之后发生的,其特点是沉积物积聚速率和细粒颗粒显着增加,这主要是由于集水区和集水区农业带来的径流增加所致。在环境退化的第二阶段(1960年代至今),牡蛎港的海草总面积损失了大约80%。磷浓度的急剧增加以及藻类和陆地投入物对沉积有机质库的贡献不断增加,为有记录的河口富营养化以及随后的海草草甸损失提供了令人信服的证据。提出的结果表明,海草沉积档案库能够重建人为对河口生态系统的压力轨迹和相关的政权转移,可用于提高科学家和环境管理者了解,预测和更好地管理这些环境变化的能力。生态系统。

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