Detrital Organic Fluxes Through Pelagic Ecosystems
Detrital Organic Fluxes Through Pelagic Ecosystems
复制标题
通过远洋生态系统的碎屑有机通量
DOI：
--
复制
发表时间：
1984
期刊：
影响因子：
--
通讯作者：
M. Angel
中科院分区：
文献类型：
--
作者：
M. Angel
Menzel（1974）写道：“特别缺乏的是关于有机物质进入深海和在深海中的输入率、利用率和分解率的信息，以及这些过程对海水化学性质的影响程度。在这里，我们特别关注的生态效应和整个水体中碎屑有机物的通量。随着对海洋中层水群落垂直结构的了解不断增加，人们逐渐认识到碎屑物雨在为深海层和深海底栖群落提供燃料方面的重要性（例如Vinogradov，1968年; Angel和Baker，1982年）。
Menzel (1974) wrote ‘particularly lacking is information on the rates of input, utilisation and decomposition of organic matter to and in the deep sea, and the extent to which these processes influence the chemistry of seawater.’ Here we are particularly concerned with the ecological effects and fluxes of detrital organic matter throughout the water column. The steady increase of knowledge of the vertical structure of oceanic midwater communities has gradually increased awareness of the importance of the rain of detrital material in fuelling the bathypelagic and deep benthic communities (e.g. Vinogradov, 1968; Angel and Baker, 1982).