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渤海湾湾口表层沉积物中的核心细菌群落结构及其对环境因子的响应 期刊论文
微生物学通报, 2018, 卷号: 45, 期号: 09, 页码: 1940-1955
作者:  刘鹏远;  陈庆彩;  胡晓珂
Adobe PDF(3381Kb)  |  收藏  |  浏览/下载：286/83  |  提交时间：2020/07/08
渤海湾  沉积物  微生物群落  16S rRNA基因多样性  
河口三角洲湿地健康生态圈构建:理论与方法 期刊论文
应用生态学报, 2018, 卷号: 29, 期号: 8, 页码: 2787-2796
作者:  韩广轩;  牛振国;  栾兆擎;  王光美;  张俪文;  管博
浏览  |  Adobe PDF(708Kb)  |  收藏  |  浏览/下载：520/226  |  提交时间：2020/07/08
河口三角洲  栖息地破碎化  生态圈  连通性  生境异质性  食物网  生态功能  
液质联用技术在测定浮游植物色素与粒级分类中的应用 期刊论文
海洋通报, 2018, 卷号: 37, 期号: 02, 页码: 158-164
作者:  张晶晶;  刘东艳;  孙慧慧;  王晓峰
收藏  |  浏览/下载：182/0  |  提交时间：2020/07/07
黄海  Chl a  浮游植物特征色素  粒级结构  UHPLC-MS/MS  
黄河三角洲自然湿地景观连接度动态变化及其驱动因素分析 期刊论文
生态环境学报, 2018, 卷号: 27, 期号: 01, 页码: 71-78
作者:  吴晶晶;  栗云召;  于良巨;  高猛;  吴晓青;  毕晓丽
浏览  |  Adobe PDF(1942Kb)  |  收藏  |  浏览/下载：535/243  |  提交时间：2020/07/08
景观连接度  自然湿地  驱动因素  黄河三角洲  
烟台夹河口外柱状沉积物还原性无机硫、活性铁的变化特征及其相互关系 期刊论文
海洋科学, 2018, 卷号: 42, 期号: 8, 页码: 90-97
作者:  姜明;  赵国强;  李兆冉;  盛彦清
浏览  |  Adobe PDF(1528Kb)  |  收藏  |  浏览/下载：525/230  |  提交时间：2020/07/08
还原性无机硫  活性铁  深层柱状沉积物  硫化度  矿化度  Reduced inorganic sulfur  Reactive iron  Deep core sediments  Degree of pyritization  Degree of sulfidity  The distribution characteristics and coupling mechanism of reduced inorganic sulfur (RIS)and reactive iron in marine core sediments are closely related to the evolution of environment quality.In this study,an improved cold diffusion method and hydrochloric acid extraction method were applied to the acid-volatile sulfur (AVS),pyrite sulfur (CRS),elemental sulfur (ES),and reactive iron [Fe (Ⅱ)and Fe (III)] analyses.The distribution characteristics and coupling mechanism of S and Fe were investigated based on a core sediment 4 meters deep collected in the northern sea area of the mouth of Jiahe River,Yantai.The results showed that the RIS in sediments was dominated by CRS,followed by AVS and ES.The content of AVS presented a narrow range with depth,whereas the CRS and ES were higher at the top and bottom layers than the middle layer  reactive iron was dominated by Fe (II),which increased with depth,while Fe (Ⅲ)gradually decreased with depth.Most of the Fe (III)was reduced to the disssolved Fe(II),which was combined with the soluble H_2S of the sulfate-reducing bacteria to produce CRS and ES in the deep layer,resulting in their accumulation at the bottom of core sediments.Furthermore,this study showed that reactive iron was not a limiting factor for the accumulation of RIS with lower degree of pyritization and degree of sulfidity.