以色列Kinneret湖生态系统的湖泊变化:起源及其意义

M. Gophen
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引用次数: 4

摘要

Kinneret湖(以色列)生态系统经历了湖泊学变化。这种变化趋势始于20世纪90年代中期。与以前已知的生态系统稳定的长期结构的偏离包括浮游植物群落结构、营养动态、浮游动物密度、水温升高、水位下降和渔业管理等。本研究旨在通过关注生态系统的三个主要部分来确定生态系统的稳定性:总溶解固体(TSS),浮游生物(植物和动物园)和碎屑(TSS减去浮游生物)。这表明,尽管记录了生物和非生物参数的显著临时变化,尽管存在正常的季节波动,但主要隔室的结构关系并未改变。研究的目的是分析修改趋势的过程启动。以往的研究和报告主要集中在对修改后的参数进行描述性评价。预期的结果是对修改过程进行全面评价。因此,结果预测可能是管理者改进管理设计的工具。
本文章由计算机程序翻译,如有差异,请以英文原文为准。
Limnological Changes in the Lake Kinneret (Israel) Ecosystem: The Beginning and Its Significance
The Lake Kinneret (Israel) ecosystem has undergone limnological changes. The trend of changes started in the mid 1990’s. The deviation from the previously known as stable long-term structure of the ecosystem included, among others, phytoplankton community structure, nutrient dynamics, zooplankton densities, water temperature increase, water level decline, and fishery management. This study is aimed at identifying ecosystem stability by focusing on three major compartments of the ecosystem: Total Dissolved Solids (TSS), Plankton (Phyto and Zoo), and Detritus (TSS minus plankton). It is suggested that although significant temporary changes of biotic and abiotic parameters were recorded and despite the existence of the normal seasonal fluctuations, the major compartments’ structural relations were not modified. The objective of the study is to analyze the process initiation of the modification trend. Previous studies and reports were focused on descriptive evaluation of the modified parameters. The expected outcome is a comprehensive evaluation of the modification process. Consequently, resulted prediction might be a tool for managers to improve management design.
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