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夹皮沟矿区金矿床的分布规律和成矿模式 总被引：1，自引：0，他引：1
夹皮沟是我国著名的老金矿区。已探明工业矿床15处,查明金矿点近百个。矿床赋存于太古代高铁镁质的角闪岩中,受北西向构造带控制。矿化集中,呈带状展布。各矿床间距约2000米。含金石英脉出露标高均在450～800米之间。金主要来自太古代海底火山的喷发产物,部分来自陆源风化冲积物。区域变质作用使金活化。海西晚期—燕山早期的重熔岩浆作用是成矿的定位期。近矿围岩蚀变有黄铁矿化和硅化。 相似文献
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Lake Dianchi has undergone accelerated alternations resulting from human activities during the last 50 years, and provides an exceptional example for the study of regime shift in a shallow lake. Focusing on regime shift, we systematically studied and analysed alternations of key components of its ecosystem, including water parameters, phytoplankton and zooplankton biomass, macrophyte composition and fish populations. We found that the shifting course of Lake Dianchi went through three major phases, corresponding to three distinct states: Phase I clean, stable state during the 1950 s; Phase II transitional state during the 1970 s–1980 s; and phase III stable, turbid state since 1993. We analysed all data and samples, identifying the threshold concentrations at which regime shift occurred: total nitrogen(TN) and phosphorus(TP) reaching 1.2 mg/L and 0.13 mg/L, respectively. Results from this study strongly suggest that the increasing input of external nutrients, reclaiming land from the lake and foreign fish invasion were major inducements to the accelerated shift of Lake Dianchi to its turbid, stable state. These findings provide valuable guidelines for potential efforts to reverse this unnatural process in Lake Dianchi. The restoration may need to:(1) thoroughly and accurately identify pollution sources to control and reduce excessive external nutrients flowing into the lake;(2) return reclaimed land to the lake and recover the littoral zone to its natural state to facilitate increased restoration of macrophytes; and(3) strategically adjust fish populations by reducing benthivorous and filter-feeding fish populations that prey on zooplankton, while enlarging zooplankton populations to control phytoplankton biomass. 相似文献
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利用1990—2020年洪湖水环境监测数据和2011—2020年洪湖沉水植物调查数据,探讨洪湖湿地生态环境演化规律,识别稳态转换关键驱动因子并确定其阈值。研究结果表明:1990—2020年以来洪湖水质变化主要总结为5个阶段和3个时期,整体上呈现出不断恶化的趋势;2011—2020年以来洪湖沉水植物Margalef物种丰富度指数、Shannon-Wiener多样性指数、Simpson和Pielou均匀度指数分别降低32%、59%、60%和46%,特别是2016年洪涝灾害后沉水植物出现严重衰退;洪湖生态系统发生稳态转换的关键时期是2002和2011年,总磷是洪湖湿地生态系统稳态转换的关键驱动因子;清水态向浊水态转换的总磷阈值为0.092 mg/L,浊水态向清水态转化的阈值为0.051 mg/L。本研究可为洪湖入湖污染负荷削减量估算提供参考,为洪湖湿地生态修复的营养盐优先控制策略提供指导。 相似文献
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为了解丹江口库区浮游生物群落的多样性,本研究于2020年7月在丹江口库区丹库、汉库和入库支流等区域共计9个样点采集水体样品,抽滤并提取总DNA样本后,基于18S和16S分子标记进行单分子实时测序,分别探究真核和原核浮游生物群落的多样性及其群落特征.结果表明：（1）真核浮游生物群落的主要优势类群包括节肢动物、链型植物、绿藻门、硅藻门等;本研究在种水平上鉴定出库区分布广泛且相对丰度较大的物种,包括弯曲隐藻、对蛋白核隐藻和空球藻等,它们与库区化学需氧量密切相关;库区化学需氧量是影响真核浮游生物群落格局的重要环境因子.（2）原核浮游生物群落的主要优势类群为变形菌门;原核生物中相对丰度较大的不动杆菌Acinetobacter是污水污染的指示菌群;群落中起重要作用的Limnohabitans与水体的富营养化密切相关;尽管库区蓝藻相对丰度较低,但与蓝藻关系密切的CL500-29_marine_group和hgcI_clade两类细菌在浮游生物群落中也起着重要作用;原核生物群落中的各类物种均指示丹江口水库的水生态健康存在一定风险,需要加强监测以预防生态环境的恶化.（3）丹江口水库不同区域的浮游生物群落异质性较大,tb-RDA分析显示丹江口的浮游生物群落可以分为丹库型、汉库型和入库支流型,其组间差异要大于组内差异.综上所述,丹江口水库的浮游生物群落具有明显的空间异质性,整个库区的群落结构与水体富营养化、水体有机污染和污水污染等方面相关,需要加强对丹江口库区的水生态监测. 相似文献
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