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Titlebook: Deep-Sea Food Chains and the Global Carbon Cycle; Gilbert T. Rowe,Vita Pariente Book 1992 Springer Science+Business Media Dordrecht 1992 O

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發(fā)表于 2025-3-21 17:13:56 | 只看該作者 |倒序?yàn)g覽 |閱讀模式
書目名稱Deep-Sea Food Chains and the Global Carbon Cycle
編輯Gilbert T. Rowe,Vita Pariente
視頻videohttp://file.papertrans.cn/265/264687/264687.mp4
叢書名稱Nato Science Series C:
圖書封面Titlebook: Deep-Sea Food Chains and the Global Carbon Cycle;  Gilbert T. Rowe,Vita Pariente Book 1992 Springer Science+Business Media Dordrecht 1992 O
描述Carbon dioxide and other `greenhouse‘ gases are increasing inthe atmosphere due to the burning of fossil fuels, the destruction ofrain forests, etc., leading to predictions of a gradual global warmingwhich will perturb the global biosphere. An important process whichcounters this trend toward potential climate change is the removal ofcarbon dioxide from the surface ocean by photosynthesis. This processpackages carbon in phytoplankton which enter the food chain or sinkinto the deep sea. Their ultimate fate is a `rain‘ of organic debrisout of the surface-mixed layer of the ocean. On a global scale, themechanisms and overall rate of this process are poorly known. .The authors of the 25 papers in this volume present theirstate-of-the-art approaches to quantifying the mechanisms by which the`rain‘ of biogenic debris nourishes deep ocean life. .Prominent deep sea ecologists, geochemists and modelers addressrelationships between data and models of carbon fluxes and food chainsin the deep ocean. An attempt is made to estimate the fate of carbonin the deep sea on a global scale by summing up the utilization oforganic matter among all the populations of the abyssal biosphere.Comparisons are
出版日期Book 1992
關(guān)鍵詞Ocean; biosphere; forest; phytoplankton; plankton; synthesis
版次1
doihttps://doi.org/10.1007/978-94-011-2452-2
isbn_softcover978-94-010-5082-1
isbn_ebook978-94-011-2452-2Series ISSN 1389-2185
issn_series 1389-2185
copyrightSpringer Science+Business Media Dordrecht 1992
The information of publication is updating

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The Role of Deep-Sea Zooplankton in Carbon Cycles,(Santa Catalina Basin in the California Borderland, Volcano 7 seamount in the Eastern Tropical Pacific). Differences in copepod gut contents between the 1300 m sites in the two geographic locations included less algal material in the Santa Catalina Basin animals and the presence of abundant bacteria
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Possible Roles for Xenophyophores in Deep-Sea Carbon Cycling,icrobial enhancement require verification before their importance can be considered. Evidence that xenophyophores enhance deposition of fine particles comes from flow visualization, excess .Th profiles, and photographic observations. Reticulate and folded tests are believed to act like small, passiv
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Production/Biomass Ratios, Size Frequencies and Biomass Spectra in Deep-Sea Demersal Fishes, fishes gives values similar to those derived previously by other means. Patterns in the frequency distribution of sizes attained by individual species at various depths can be related to probable feeding modes, and these are supported by information on diets. The biomass spectrum for the continenta
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Effects of Spatial and Temporal Scale on the Relationship of Surface Pigment Biomass to Community S, Gastropoda, Cumacea and Bivalvia). Surface pigment biomass directly above the benthic sampling stations was averaged monthly and seasonally over a three-year period at three spatial scales corresponding to square areas of 1, 9 and 121 pixels (0.83, 7.43 and 99.83 km. respectively). Benthic biomass
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Benthic Food Web Flows in the Santa Monica Basin Estimated Using Inverse Methodology,ed material poor in nitrogen while the grazers consumed material rich in nitrogen. Although bacteria consumed more carbon than did the grazers, the bacteria released equal amount of ammonia. Small protozoan microfauna consumed and mineralized most of the material available to the grazer populations.
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