翻訳と辞書
Words near each other
・ Biomedical Engineering Society
・ Biomedical Equipment Technician
・ Biomedical Imaging and Intervention Journal
・ Biomedical Informatics Research Network
・ Biomedical material
・ Biomedical Materials (journal)
・ Biomedical Microdevices
・ Biomedical model
・ Biomedical Optics Express
・ Biomedical Primate Research Centre
・ Biomedical Research Council
・ Biomedical research in the Middle East
・ Biomedical Research Institute
・ Biomedical sciences
・ Biological psychopathology
Biological pump
・ Biological Radio
・ Biological recording
・ Biological Records Centre
・ Biological Research Centre (Hungarian Academy of Sciences)
・ Biological Research for Nursing
・ Biological resistance
・ Biological resource center
・ Biological Resources Discipline
・ Biological response modifiers
・ Biological robot
・ Biological role of oxygen
・ Biological Sciences Curriculum Study
・ Biological screw joint
・ Biological small-angle scattering


Dictionary Lists
翻訳と辞書 辞書検索 [ 開発暫定版 ]
スポンサード リンク

Biological pump : ウィキペディア英語版
Biological pump

The biological pump, in its simplest form, is the ocean’s biologically driven sequestration of carbon from the atmosphere to the deep sea.〔Sigman DM & GH Haug. 2006. The biological pump in the past. In: Treatise on Geochemistry; vol. 6, (ed.). Pergamon Press, pp. 491-528〕 It is the part of the oceanic carbon cycle responsible for the cycling of organic matter formed by phytoplankton during photosynthesis (soft-tissue pump), as well as the cycling of calcium carbonate (CaCO3) formed by certain plankton and mollusks as a protective coating (carbonate pump).
==Overview==
The biological pump can be divided into three distinct phases,〔De La Rocha CL. 2006. The Biological Pump. In: Treatise on Geochemistry; vol. 6, (ed.). Pergamon Press, pp. 83-111〕 the first of which is the production of fixed carbon by planktonic phototrophs in the euphotic (sunlit) surface region of the ocean. In these surface waters, phytoplankton use carbon dioxide (CO2), nitrogen (N), phosphorus (P), and other trace elements (barium, iron, zinc, etc.) during photosynthesis to make carbohydrates, lipids, and proteins. Some plankton, (e.g. coccolithophores and foraminifera) combine calcium (Ca) and dissolved carbonates (carbonic acid and bicarbonate) to form a calcium carbonate (CaCO3) protective coating.
Once this carbon is fixed into soft or hard tissue, the organisms either stay in the euphotic zone to be recycled as part of the regenerative nutrient cycle or once they die, continue to the second phase of the biological pump and begin to sink to the ocean floor. The sinking particles will often form aggregates as they sink, greatly increasing the sinking rate. It is this aggregation that gives particles a better chance of escaping predation and decomposition in the water column and eventually make it to the sea floor.
The fixed carbon that is either decomposed by bacteria on the way down or once on the sea floor then enters the final phase of the pump and is remineralized to be used again in primary production. The particles that escape these processes entirely are sequestered in the sediment and may remain there for thousands of years. It is this sequestered carbon that is responsible for ultimately lowering atmospheric CO2.

抄文引用元・出典: フリー百科事典『 ウィキペディア(Wikipedia)
ウィキペディアで「Biological pump」の詳細全文を読む



スポンサード リンク
翻訳と辞書 : 翻訳のためのインターネットリソース

Copyright(C) kotoba.ne.jp 1997-2016. All Rights Reserved.