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Titlebook: Coastal-Offshore Ecosystem Interactions; Proceedings of a Sym Bengt-Owe Jansson Conference proceedings 1988 Springer-Verlag Berlin Heidelbe

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书目名称Coastal-Offshore Ecosystem Interactions
副标题Proceedings of a Sym
编辑Bengt-Owe Jansson
视频videohttp://file.papertrans.cn/229/228766/228766.mp4
丛书名称Coastal and Estuarine Studies
图书封面Titlebook: Coastal-Offshore Ecosystem Interactions; Proceedings of a Sym Bengt-Owe Jansson Conference proceedings 1988 Springer-Verlag Berlin Heidelbe
描述stable isotope ratios act as naturally-occurring tracers for organic matter, making possible, under certain conditions, the quantification of coastal-offshore exchanges. In general, organic matter has isotope ratios characteristic of its origin (e. g. plants with different modes of photosynthesis and different growth conditions, anthropogenic compounds). These ratios are maintained as the organic matter moves through the biosphere and geosphere. A mixture of organic matter from two sources has isotope ratios intermediate between those of the two sources, in proportion to the fraction of material from each source. Isotope ratios are one of the few methods which can trace organic matter as it moves through natural ecosystems. Ratios can be measured on both the total organic matter and on particular chemical fractions or compounds. When used on organisms, isotope ratios provide information of organic matter actually assimilated into body tissues, not just material ingested. As with all tools, this method has certain limitations which must be borne in mind when interpreting its results. Firstly, specific environmental conditions must be met. This generally means an ecosystem with a lim
出版日期Conference proceedings 1988
关键词Coast; Mangrove; Ocean; ecosystem; energy; environment; lake
版次1
doihttps://doi.org/10.1007/978-3-642-52452-3
isbn_softcover978-3-540-19051-6
isbn_ebook978-3-642-52452-3Series ISSN 0724-5890
issn_series 0724-5890
copyrightSpringer-Verlag Berlin Heidelberg 1988
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978-3-540-19051-6Springer-Verlag Berlin Heidelberg 1988
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Nonlinear and Adaptive Lifting,and the offshore shelf zone. The mixing processes are conditioned by topography and earth rotation. Mixing of inland and ocean waters is accomplished partly in inshore basins (lagoons or estuaries), partly around inlets and partly offshore on the coastal shelf. Depending on the type of coastal syste
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Nonlinear and Adaptive Lifting,, or a combination of these. In my opinion, the density front that often exists between coastal and offshore waters is as good a dividing line as one could wish, especially for areas with a deep, narrow shelf. Large gradients of temperature, salt, biomass and current velocity occur at these fronts.
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Second Handbook of Academic Integritynd natural terrigenous organic matter in the marine environment. In many circumstances, they provide the only way of deter mining the origins of this material. However, the method has definite limitations which must be taken into account. In particular, one must always measure the possible sources o
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Reference work 2024Latest edition, in addition to knowing the rate of carbon fixation and respiration within the ecosystem, it is equally important to know how the ecosystem interacts with its adjacent ecosystems. Is it autotrophic and subsidizing adjacent regions or is it heterotrophic and dependent on allochthonous organic inputs
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Teaching English as a Third Languageties have received considerable botanical investigation because of their unique taxonomy and ovivipary (Tomlinson, 1986), and the diverse fauna that inhabit these coastal areas (Macnae, 1968;Chapman, 1976). However, the ecology of mangroves is poorly understood, particularly the significance of thes
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