Biotic Interactions in Benthic Foraminifera
Biotic Interactions in Benthic Foraminifera
复制标题
底栖有孔虫的生物相互作用
DOI：
10.1007/978-1-4757-0740-3_8
复制
发表时间：
1983
影响因子：
1.9
通讯作者：
J. Lipps
中科院分区：
文献类型：
--
作者：
J. Lipps
有孔虫时代有很长的地质记录，可能可以追溯到寒武纪，它们在中生代的大部分时间里都是丰富多样的。现在已经描述了超过40，000种，其中大约4000种生活在今天（Tappan，1971）。它们存在于所有现代海洋群落中，也被发现生活在半咸水和淡水中（Arnal，1958年; Boltovskoy和Lena，1971年; Resig，1974年）。有孔虫在深海、珊瑚礁和许多软底浅水生境中特别多样和丰富（Hessler，1974年; Smith等人，1978; Thiel，1975; Murray，1973; Wefer and Lutze，1976），使它们成为地球上最重要的动物群体之一。然而，人们对它们与其他生物的相互作用知之甚少，尽管关于它们的分布模式已经发表了很多文章。有孔虫在古生物学和古环境解释中的成功应用需要更详细的生态学知识（Lipps，1981）。
Foraminif era have a long geologic record, extending back perhaps to the Cambrian, and they are both abundant and diverse during most of the Phanerozoic. Over 40,000 species now have been described, of which approximately 4000 are living today (Tappan, 1971). They occur in all modern marine communities, and have also been found living in brackish and fresh water (Arnal, 1958; Boltovskoy and Lena, 1971; Resig, 1974). Foraminifera are especially diverse and abundant in deep-sea, coral reef, and many soft-bottom, shallow-water habitats (Hessler, 1974; Smith et al., 1978; Thiel, 1975; Murray, 1973; Wefer and Lutze, 1976), making them one of the most important animal groups on earth. Yet little is known about their interactions with other organisms, although much has been published on their distributional patterns. Successful use of foraminifera in paleobiology and paleoenvironmental interpretations requires more detailed ecologic knowledge (Lipps, 1981).