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Titlebook: An Introduction to Coastal Ecology; Patrick J. S. Boaden,Raymond Seed Book 1985 Chapman & Hall 1985 adaptation.chemistry.coral reef.echino

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發(fā)表于 2025-3-21 18:55:43 | 只看該作者 |倒序?yàn)g覽 |閱讀模式
期刊全稱An Introduction to Coastal Ecology
影響因子2023Patrick J. S. Boaden,Raymond Seed
視頻videohttp://file.papertrans.cn/156/155174/155174.mp4
學(xué)科分類Tertiary Level Biology
圖書封面Titlebook: An Introduction to Coastal Ecology;  Patrick J. S. Boaden,Raymond Seed Book 1985 Chapman & Hall 1985 adaptation.chemistry.coral reef.echino
影響因子Studies of marine ecology have traditionally been approached through lectures and field courses devoted mainly to intertidal and inshore habitats, and it is surprising in these days of increased awareness of man‘s environmental impact that so little attention has been given to integrated approaches involving the whole coastal zone and including the terrestrial part, which is man‘s major habitat. The coastal zone has been the subject of extensive investigation, not only because of its biological diversity and accessibility, but also because of its economic and aesthetic importance to man. This book is written with the intention of providing a concise but readable account of coastal ecology for advanced undergraduates and immediate postgraduates. We have adopted a habitat-organismal ap- proach because we believe that a knowledge of biota and major features of their environment is the best key to an understanding of both larger-scale processes, such as energy flow and nutrient cycling, and smaller-scale but equally fundamental processes, such as behavioural and physiological ecology. Examples have been selected from polar, temperate and tropical regions of the world. The breadth of th
Pindex Book 1985
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Life in Sediments,hich are thus protected from extreme salinity fluctuations. Sediments also provide some insulation from temperature change (Figure 4.1) providing that the organisms can avoid the immediate surface. The specific heat of damp sand is usually 0.1–0.3 of that of water. The granulometric composition of s
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itats, and it is surprising in these days of increased awareness of man‘s environmental impact that so little attention has been given to integrated approaches involving the whole coastal zone and including the terrestrial part, which is man‘s major habitat. The coastal zone has been the subject of
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https://doi.org/10.1007/978-3-642-91379-27). Many open coasts are continuously exposed to oceanic swell and extreme wave action, whilst deeply indented coastlines may be perpetually calm. Salinity, temperature and turbidity are also subject to wide variations.
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Life on Rocky Coasts,7). Many open coasts are continuously exposed to oceanic swell and extreme wave action, whilst deeply indented coastlines may be perpetually calm. Salinity, temperature and turbidity are also subject to wide variations.
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https://doi.org/10.1007/978-3-642-91379-2nd many of the important commercial fisheries are located in these inshore waters. The . (= epipelagic) zone is that part of the pelagic realm which is well illuminated. Its lower boundary varies according to the clarity of the water but, is usually around 100–200 m. It grades into the . zone which is permanently dark below about 1000 m.
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Wie es in einer Werkstatt aussieht,imited to particular areas. The need also arises because some of man’s activities prejudice the continuing use of resources. Many of these detrimental activities differ from overfishing because they result from additions to, rather than removals from, the environment. Damaging added-substances are usually called ..
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