Abstract Tracing organic matter sources in a tropical lagoon of the Caribbean Sea
首页> 外文期刊>Continental Shelf Research: A Companion Journal to Deep-Sea Research and Progress in Oceanography >Tracing organic matter sources in a tropical lagoon of the Caribbean Sea
【24h】

Tracing organic matter sources in a tropical lagoon of the Caribbean Sea

机译:在加勒比海的热带泻湖中追踪有机物质来源

获取原文
获取原文并翻译 | 示例
           

摘要

AbstractThe natural protected lagoon of Guanaroca, located between Cienfuegos Bay and the Arimao River, Cuba, has been heavily impacted by human-induced environmental changes over the past century. Sources of organic matter in the Guanaroca lagoon and concentrations of radioisotopes (210Pb,226Ra,137Cs and239,240Pu), as tracers of anthropogenic impacts, were investigated in a 78cm sediment core. Variations in total organic carbon (TOC), total nitrogen (TN), stable isotopic composition (δ13C and δ15N) and ratio of total organic carbon to total nitrogen (C/N) were analysed. On such a basis, environmental changes in the lagoon were revealed. Down core variation patterns of the parameters representing sources of organic matter were predominantly related to the impacts of human activities. Up to the nineteenth century, the principal sources of organic matter to sediments (more than 80%) were a mixing of terrestrial vascular plants (~48%) and freshwater phytoplankton (~8%), with minimal contribution from the marine component (~16%). In the period 1900–1980, due to the strong influence of human activities in the catchment area, the water exchange capacity of the lagoon declined substantially, as indicated by the relatively high proportion of organic matter originated from human activities (58%). Since 1980, as a result of management actions in the protected area, the lagoon has regained gradually its capability to exchange freshwater, showing sources of organic matter similar to the natural conditions recorded previous to 1900,
机译:<![cdata [ 抽象 位于Cienfuegos湾和古巴的阿里莫河之间的古巴拉的自然受保护的泻湖,受到人类诱发的环境变化影响的严重影响过去的世纪。瓜兰科泻湖的有机物源和放射性同位浓度( 210 pb, 226 ra , 137 cs和 239,240 pu),作为人为影响的示踪剂,在a中被研究78cm沉积物核心。总有机碳(TOC),总氮(TN),稳定同位素组合物(δ 13 c和δ n)和总有机碳与总氮气(c / n)的比例。在这种基础上,泻湖的环境变化被揭示。表示有机物质来源的参数的下核变异模式主要与人类活动的影响有关。达到十九世纪,对沉积物的主要来源(超过80%)是陆地血管植物(〜48%)和淡水浮游植物(〜8%)的混合,来自海洋组分的贡献最小(〜 16%)。在1900-1980期间,由于人类活动对集水区的强烈影响,泻湖的水交换能力大幅下降,如源自人类活动的相对高比例的有机物(58%)所表明的。自1980年以来,由于管理领域的管理行动,泻湖已逐步重新恢复其交换淡水的能力,显示出类似于1900年以前记录的自然条件的有机物质来源,

著录项

相似文献

  • 外文文献
  • 中文文献
  • 专利
获取原文

客服邮箱:kefu@zhangqiaokeyan.com

京公网安备:11010802029741号 ICP备案号:京ICP备15016152号-6 六维联合信息科技 (北京) 有限公司©版权所有
  • 客服微信

  • 服务号