BIODIVERSITY OF THE PELAGIC OCEAN

被引:179
作者
ANGEL, MV
机构
[1] Institute of Oceanographic Sciences Deacon Laboratory, Wormley Godalming, Surrey
关键词
D O I
10.1046/j.1523-1739.1993.740760.x
中图分类号
X176 [生物多样性保护];
学科分类号
090705 ;
摘要
This paper reviews knowledge of biodiversity in open ocean pelagic communities and discusses the possible causal factors for the patterns. The oceanic pelagic ecosystem is by far the largest on Earth and, although locally its assemblages may be as rich as many terrestrial ecosystems, its global diversity (at both a species and an ecosystem level) is low. There are latitudinal trends in pelagic species diversity similar to those in many terrestrial taxa. High species richness in the oceans, however, tends to be associated with regions of low productivity that lack strong seasonality in the production cycle. The richest zones occur at the boundaries between different types of oceanic water where different faunas are mixed together, but the geographical locations of these boundaries are unstable and shift seasonally by hundreds of kilometers. If high diversity is emphasized in the development of protocols for conservation, then not only will the oceans receive low priority in conservation and resource management, but the regions most important in terms of process will also be overlooked. The scales of oceanic systems are so large that the methodologies developed for terrestrial conservation and resource management are inapplicable Biodiversity may be regarded as the principal criterion for developing management strategies, yet the links (if any) between the ecological processes in the ocean that play such an important role in global homeostasis remain poorly characterized. The basis for a predictive understanding of the interaction between diversity and ecological process can be greatly enhanced relatively inexpensively by systematically collating existing data and working up extant collections of material
引用
收藏
页码:760 / 772
页数:13
相关论文
共 71 条
[1]  
Angel M.V., A vertical profile of planktonic ostracods at 42° N, 17° W from depths of 1500–3900 m, Applications of Ostracoda, pp. 549-559, (1983)
[2]  
Angel M.V., 22, pp. 1-46, (1989)
[3]  
Angel M.V., Variations in time and space: Is biogeography relevant to studies of long‐time scale change?, Journal of the Marine Biological Association of the United Kingdom, 71, pp. 191-206, (1991)
[4]  
Angel M.V., Fasham M.J.R, Analysis of the vertical and geographical distribution of the abundant species of planktonic ostracods in the North‐east Atlantic, Journal of the Marine Biological Association of the United Kingdom, 55, pp. 709-737, (1975)
[5]  
Badcock J., Merrett N.R, Midwater fishes in the eastern North Atlantic, Progress in Oceanography, 7, pp. 3-58, (1976)
[6]  
Barron J.A., Baldauf J.G., Tertiary cooling steps and paleoproductivity as reflected by diatoms and biosiliceous sediments, Productivity of the ocean: Present and past, pp. 341-354, (1989)
[7]  
Berger W.H., Smetachek V.S., Ocean productivity and paleoproductivity, pp. 1-34, (1989)
[8]  
Briggs J.C., Marine zoogeography, (1975)
[9]  
Cameron A.N., Endean R., 75, pp. 251-258, (1991)
[10]  
Campbell J.W., Aarup T., New production in the North Atlantic derived from seasonal patterns of surface chlorophyll, Deep-Sea Research, 39, pp. 1669-1694, (1992)