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In other words, it is a biologically mediated processes which result in the sequestering of carbon in the deep ocean away from the atmosphere and the land. The biological pump is the biological component of the "marine carbon pump" which contains both a physical and biological component. 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href="http://dbpedia.org/resource/Biological_pump">Biological pump</a> </h1> </div> </div> <div class="row"> <div class="col"> <div class="text-muted"> An Entity of Type: <a href="http://www.w3.org/2002/07/owl#Thing">Thing</a>, from Named Graph: <a href="http://dbpedia.org">http://dbpedia.org</a>, within Data Space: <a href="http://dbpedia.org">dbpedia.org</a> </div> </div> </div> <div class="row pt-2"> <div class="col-xs-9 col-sm-10"> The biological pump (or ocean carbon biological pump or marine biological carbon pump) is the ocean's biologically driven sequestration of carbon from the atmosphere and land runoff to the ocean interior and seafloor sediments. In other words, it is a biologically mediated processes which result in the sequestering of carbon in the deep ocean away from the atmosphere and the land. The biological pump is the biological component of the "marine carbon pump" which contains both a physical and biological component. It is the part of the broader oceanic carbon cycle responsible for the cycling of organic matter formed mainly by phytoplankton during photosynthesis (soft-tissue pump), as well as the cycling of calcium carbonate (CaCO3) formed into shells by certain organisms such as plankton and </div> <div class="col-xs-3 col-sm-2"> <a href="#" class="thumbnail"> <img src="http://commons.wikimedia.org/wiki/Special:FilePath/Oceanic_Food_Web.jpg?width=300" alt="thumbnail" class="img-fluid" /> </a> </div> </div> </div> </section>   <section> <div class="container-xl"> <div class="row"> <div class="table-responsive"> <table class="table table-hover table-sm table-light"> <thead> <tr> <th class="col-xs-3 ">Property</th> <th class="col-xs-9 px-3">Value</th> </tr> </thead> <tbody> <tr class="odd"><td class="col-2"><a class="uri" href="http://dbpedia.org/ontology/abstract">dbo:abstract</a> </td><td class="col-10 text-break"><ul> <li style="display:none;">المضخة البيولوجية (بالإنجليزية: Biological pump)‏، هو عزل المحيط الحيوي من الكربون في الغلاف الجوي إلى مياه البحر العميقة والرواسب. وهو هو جزء من دورة الكربون المحيطية المسؤولة عن ركوب المواد العضوية التي تشكلت أساساً من العوالق النباتية أثناء عملية التمثيل الضوئي (مضخة الأنسجة اللينة)، فضلاً عن ركوب كربونات الكالسيوم (CaCO3) التي تشكلت في قذائف من قبل بعض الكائنات الحية مثل العوالق و الرخويات. (ar)</li> <li style="display:none;">Una bomba biològica en bioquímica dels oceans és la suma dels processos biològics de transport de carboni de la zona eufòtica superficial a l'interior de l'oceà. El carboni orgànic que forma la bomba biològica és transportat principalment per les partícules material que s'enfonsen, per exemple organismes morts com les algues o partícules fecals. Tanmateix, part del carboni arriba a les fondàries oceàniques com carboni orgànic dissolt (DOC) per procés físic de transport processes (downwelling). El carboni arriba als fons en dues formes de carbonat de calci (CaCO₃) òrganic i inorgànic. La primera forma es troba en tots els organismes i com inorgànic només en els organismes calcificats com , foraminífers o . En el cas de material orgànic la mineralització o la putrefacció torna el carboni orgànic a diòxid de carboni dissolt. La taxa de dissolució del carbonat de calci depèn de la química el carbonat local. Com aquests processos són generalment més lents que els de síntesi, i pel fet que les partícules s'enfonsen, la bomba biològica transporta material de la superfície als fons del mar. El procés que forma la bomba biològica és difícil de mesurar. Un mètode comú per estimar-lo es basa en la producció primària alimentada pel nitrat i l'amoni. A més de la bomba biològica actua la bomba fisico-química o . (ca)</li> <li>The biological pump (or ocean carbon biological pump or marine biological carbon pump) is the ocean's biologically driven sequestration of carbon from the atmosphere and land runoff to the ocean interior and seafloor sediments. In other words, it is a biologically mediated processes which result in the sequestering of carbon in the deep ocean away from the atmosphere and the land. The biological pump is the biological component of the "marine carbon pump" which contains both a physical and biological component. It is the part of the broader oceanic carbon cycle responsible for the cycling of organic matter formed mainly by phytoplankton during photosynthesis (soft-tissue pump), as well as the cycling of calcium carbonate (CaCO3) formed into shells by certain organisms such as plankton and mollusks (carbonate pump). Budget calculations of the biological carbon pump are based on the ratio between sedimentation (carbon export to the ocean floor) and remineralization (release of carbon to the atmosphere). The biological pump is not so much the result of a single process, but rather the sum of a number of processes each of which can influence biological pumping. Overall, the pump transfers about 11 gigatonnes of carbon every year into the ocean's interior. This takes carbon out of contact with the atmosphere for several thousand years or longer. An ocean without a biological pump would result in atmospheric carbon dioxide levels about 400 ppm higher than the present day. (en)</li> <li style="display:none;">La bomba biológica, también denominada bomba de carbono marino, se refiere a la fijación de carbono proveniente de la atmósfera y de la escorrentía terrestre por el océano. Este mecanismo natural de fijación de carbono es impulsado biológicamente, ya que organismos marinos durante todo su ciclo de vida consumen carbono y lo incorporan a sus tejidos. Al alimentarse, defecar o morir, estos organismos transportan el carbono desde la superficie de los océanos hacia su interior y eventualmente el carbono será depositado en el lecho marino. La bomba biológica es parte del ciclo del carbono oceánico a través del cual la materia orgánica, formada principalmente por el fitoplancton durante la fotosíntesis (bomba de tejido blando), es transportada desde aguas superficiales hacia las profundidades del océano. La bomba biológica también forma parte del ciclo del carbonato de calcio (CaCO3), el cual es utilizado por ciertos organismos como el plancton y los moluscos para formar conchas y caparazones (bomba de carbonato). El cálculo de la eficiencia de la bomba biológica de carbono se basa en la proporción de carbono que es parte de la sedimentación (exportación de carbono) y que forma parte de la remineralización (liberación a la atmósfera). La bomba biológica incluye varios procesos, cada uno de los cuales puede influir en la eficacia del bombeo biológico. En general, cada año la bomba transfiere alrededor de 11 gigatoneladas de carbono al interior del océano. El carbono capturado por los océanos se mantendrá fuera de contacto con la atmósfera durante varios miles de años o incluso más tiempo. Si el océano no contara con una bomba biológica, entonces los niveles de dióxido de carbono atmosférico serían alrededor de 400 ppm más altos que en la actualidad. (es)</li> <li style="display:none;">Dans la biogéochimie des océans, la pompe biologique, qui relève du cycle du carbone océanique, est une série de processus biologiques conduisant à transporter le carbone de la zone photique vers les fonds marins. C'est un élément majeur du cycle du carbone. Grâce à cette pompe, l'océan a ainsi depuis le début de l'ère industrielle pu absorber 41 % du carbone anthropique émis par la consommation des énergies fossiles et la fabrication du ciment. (fr)</li> <li style="display:none;">生物ポンプ（せいぶつぽんぷ）とは、生物海洋学において、海洋表層（有光層）から海洋内部へ生物学的に炭素を輸送する経路を指す。炭素は主に粒子状の状態、例えば生物の遺骸（藻類マットを含む）や動物の糞粒の状態で沈降することで運ばれる。一部の炭素は溶解した有機炭素（DOC）となって、という物理的な運搬過程で海底に運ばれる。深海に沈む炭素には、有機炭素と無機炭素（炭酸カルシウムなど）の両方ある。前者は全ての生物の構成物質であり、後者は（例えばや有孔虫のような）カルシウムの殻を持つ生物の構成物質である。これらの生物源物質の違いを区別する際には、有機炭素の運搬は軟組織ポンプ、無機炭素の運搬は硬組織ポンプと呼ぶ。有機物質の場合、バクテリアの呼吸作用などにより、有機炭素から溶存二酸化炭素となって海水に戻される。炭酸カルシウムの場合は、局所的な炭酸塩の化学過程に依存する。しかしこれらの過程は普通光合成過程よりも遅いので、結果的に生物ポンプは炭素を表層から海洋の深部へ運んでいることになる。　生物ポンプは物理化学的なやと関連付けて考えられている。関連するプロセスとして、という考え方が近年提唱されている。 (ja)</li> <li style="display:none;">Pompa biologiczna - w biogeochemii oceanów stanowi ogół procesów, transportujących węgiel ze strefy eufotycznej do głębi oceanu, w których pośrednią rolę odgrywają organizmy żywe. (pl)</li> <li style="display:none;">Em Oceanografia, o termo bomba biológica se refere ao processo através do qual o carbono liberado por atividades naturais e antropogênicas na atmosfera terrestre é incorporado e armazenado no oceano profundo por meio de processos biológicos (fotossíntese, respiração, alimentação e decomposição e precipitação biogênica de carbonatos). O oceano global armazena aproximadamente 50 vezes mais carbono que a atmosfera. A produção biológica marinha possui um papel muito importante no sequestro de carbono atmosférico, o que por sua vez é um importante mecanismo regulador do clima no planeta. Esse sequestro de carbono na forma de dióxido de carbono (CO2) se deve a atividade da bomba biológica de carbono, fenômeno também conhecido como bombeamento biológico. A bomba biológica de carbono cria um fluxo de matéria orgânica desde a superfície até o interior dos oceanos, que reduz a pressão parcial de dióxido de carbono na superfície e, consequentemente, a quantidade desse gás na atmosfera, permitindo que o mesmo seja absorvido e armazenado nas bacias oceânicas do planeta. (pt)</li> <li style="display:none;">生物传递是以生物或生物行为为动力，将碳元素从大气到海洋内部和海底沉积物的固存。它是的一部分，负责在光合作用（软组织泵）过程中主要由浮游植物形成的有机物质的循环，以及由某些生物（例如浮游生物和软体动物）形成的贝壳中的碳酸钙（CaCO3）的循环（碳酸盐泵）。 (zh)</li> </ul></td></tr><tr class="even"><td class="col-2"><a class="uri" href="http://dbpedia.org/ontology/thumbnail">dbo:thumbnail</a> </td><td class="col-10 text-break"><ul> <li><a class="uri" rel="dbo:thumbnail" resource="http://commons.wikimedia.org/wiki/Special:FilePath/Oceanic_Food_Web.jpg?width=300" href="http://commons.wikimedia.org/wiki/Special:FilePath/Oceanic_Food_Web.jpg?width=300">wiki-commons:Special:FilePath/Oceanic_Food_Web.jpg?width=300</a></li> </ul></td></tr><tr class="odd"><td class="col-2"><a class="uri" href="http://dbpedia.org/ontology/wikiPageID">dbo:wikiPageID</a> </td><td class="col-10 text-break"><ul> <li>240228 (xsd:integer)</li> </ul></td></tr><tr class="even"><td class="col-2"><a class="uri" href="http://dbpedia.org/ontology/wikiPageLength">dbo:wikiPageLength</a> </td><td class="col-10 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Actual mechanisms are likely to include both scenarios. (en)</li> </ul></td></tr><tr class="odd"><td class="col-2"><a class="uri" href="http://dbpedia.org/property/date">dbp:date</a> </td><td class="col-10 text-break"><ul> <li>May 2021 (en)</li> </ul></td></tr><tr class="even"><td class="col-2"><a class="uri" href="http://dbpedia.org/property/direction">dbp:direction</a> </td><td class="col-10 text-break"><ul> <li>horizontal (en)</li> </ul></td></tr><tr class="odd"><td class="col-2"><a class="uri" href="http://dbpedia.org/property/header">dbp:header</a> </td><td class="col-10 text-break"><ul> <li>Phytoplankton (en)</li> <li>Viral shunt (en)</li> </ul></td></tr><tr class="even"><td class="col-2"><a class="uri" href="http://dbpedia.org/property/image">dbp:image</a> </td><td class="col-10 text-break"><ul> <li>Coccolithus pelagicus.jpg (en)</li> <li>Sloppy feeding by zooplankton.jpg (en)</li> <li>Structure of a Myoviridae bacteriophage 2.jpg (en)</li> <li>Triceratium morlandii var. morlandii.jpg (en)</li> <li>Viral shunt.jpg (en)</li> 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http://purl.org/dc/terms/" href="http://dbpedia.org/resource/Category:Chemical_oceanography">dbc:Chemical_oceanography</a></li> <li><a class="uri" rel="dcterms:subject" resource="http://dbpedia.org/resource/Category:Carbon_cycle" prefix="dcterms: http://purl.org/dc/terms/" href="http://dbpedia.org/resource/Category:Carbon_cycle">dbc:Carbon_cycle</a></li> </ul></td></tr><tr class="odd"><td class="col-2"><a class="uri" href="http://purl.org/linguistics/gold/hypernym">gold:hypernym</a> </td><td class="col-10 text-break"><ul> <li><a class="uri" rel="gold:hypernym" resource="http://dbpedia.org/resource/’" prefix="gold: http://purl.org/linguistics/gold/" href="http://dbpedia.org/resource/’">dbr:’</a></li> </ul></td></tr><tr class="even"><td class="col-2"><a class="uri" href="http://www.w3.org/1999/02/22-rdf-syntax-ns#type">rdf:type</a> </td><td class="col-10 text-break"><ul> <li><a class="uri" rel="rdf:type" resource="http://www.w3.org/2002/07/owl#Thing" href="http://www.w3.org/2002/07/owl#Thing">owl:Thing</a></li> </ul></td></tr><tr class="odd"><td class="col-2"><a class="uri" href="http://www.w3.org/2000/01/rdf-schema#comment">rdfs:comment</a> </td><td class="col-10 text-break"><ul> <li style="display:none;">المضخة البيولوجية (بالإنجليزية: Biological pump)‏، هو عزل المحيط الحيوي من الكربون في الغلاف الجوي إلى مياه البحر العميقة والرواسب. وهو هو جزء من دورة الكربون المحيطية المسؤولة عن ركوب المواد العضوية التي تشكلت أساساً من العوالق النباتية أثناء عملية التمثيل الضوئي (مضخة الأنسجة اللينة)، فضلاً عن ركوب كربونات الكالسيوم (CaCO3) التي تشكلت في قذائف من قبل بعض الكائنات الحية مثل العوالق و الرخويات. (ar)</li> <li style="display:none;">Dans la biogéochimie des océans, la pompe biologique, qui relève du cycle du carbone océanique, est une série de processus biologiques conduisant à transporter le carbone de la zone photique vers les fonds marins. C'est un élément majeur du cycle du carbone. Grâce à cette pompe, l'océan a ainsi depuis le début de l'ère industrielle pu absorber 41 % du carbone anthropique émis par la consommation des énergies fossiles et la fabrication du ciment. (fr)</li> <li style="display:none;">生物ポンプ（せいぶつぽんぷ）とは、生物海洋学において、海洋表層（有光層）から海洋内部へ生物学的に炭素を輸送する経路を指す。炭素は主に粒子状の状態、例えば生物の遺骸（藻類マットを含む）や動物の糞粒の状態で沈降することで運ばれる。一部の炭素は溶解した有機炭素（DOC）となって、という物理的な運搬過程で海底に運ばれる。深海に沈む炭素には、有機炭素と無機炭素（炭酸カルシウムなど）の両方ある。前者は全ての生物の構成物質であり、後者は（例えばや有孔虫のような）カルシウムの殻を持つ生物の構成物質である。これらの生物源物質の違いを区別する際には、有機炭素の運搬は軟組織ポンプ、無機炭素の運搬は硬組織ポンプと呼ぶ。有機物質の場合、バクテリアの呼吸作用などにより、有機炭素から溶存二酸化炭素となって海水に戻される。炭酸カルシウムの場合は、局所的な炭酸塩の化学過程に依存する。しかしこれらの過程は普通光合成過程よりも遅いので、結果的に生物ポンプは炭素を表層から海洋の深部へ運んでいることになる。　生物ポンプは物理化学的なやと関連付けて考えられている。関連するプロセスとして、という考え方が近年提唱されている。 (ja)</li> <li style="display:none;">Pompa biologiczna - w biogeochemii oceanów stanowi ogół procesów, transportujących węgiel ze strefy eufotycznej do głębi oceanu, w których pośrednią rolę odgrywają organizmy żywe. (pl)</li> <li style="display:none;">生物传递是以生物或生物行为为动力，将碳元素从大气到海洋内部和海底沉积物的固存。它是的一部分，负责在光合作用（软组织泵）过程中主要由浮游植物形成的有机物质的循环，以及由某些生物（例如浮游生物和软体动物）形成的贝壳中的碳酸钙（CaCO3）的循环（碳酸盐泵）。 (zh)</li> <li style="display:none;">Una bomba biològica en bioquímica dels oceans és la suma dels processos biològics de transport de carboni de la zona eufòtica superficial a l'interior de l'oceà. El carboni orgànic que forma la bomba biològica és transportat principalment per les partícules material que s'enfonsen, per exemple organismes morts com les algues o partícules fecals. Tanmateix, part del carboni arriba a les fondàries oceàniques com carboni orgànic dissolt (DOC) per procés físic de transport processes (downwelling). A més de la bomba biològica actua la bomba fisico-química o . (ca)</li> <li>The biological pump (or ocean carbon biological pump or marine biological carbon pump) is the ocean's biologically driven sequestration of carbon from the atmosphere and land runoff to the ocean interior and seafloor sediments. In other words, it is a biologically mediated processes which result in the sequestering of carbon in the deep ocean away from the atmosphere and the land. The biological pump is the biological component of the "marine carbon pump" which contains both a physical and biological component. It is the part of the broader oceanic carbon cycle responsible for the cycling of organic matter formed mainly by phytoplankton during photosynthesis (soft-tissue pump), as well as the cycling of calcium carbonate (CaCO3) formed into shells by certain organisms such as plankton and (en)</li> <li style="display:none;">La bomba biológica, también denominada bomba de carbono marino, se refiere a la fijación de carbono proveniente de la atmósfera y de la escorrentía terrestre por el océano. Este mecanismo natural de fijación de carbono es impulsado biológicamente, ya que organismos marinos durante todo su ciclo de vida consumen carbono y lo incorporan a sus tejidos. Al alimentarse, defecar o morir, estos organismos transportan el carbono desde la superficie de los océanos hacia su interior y eventualmente el carbono será depositado en el lecho marino. (es)</li> <li style="display:none;">Em Oceanografia, o termo bomba biológica se refere ao processo através do qual o carbono liberado por atividades naturais e antropogênicas na atmosfera terrestre é incorporado e armazenado no oceano profundo por meio de processos biológicos (fotossíntese, respiração, alimentação e decomposição e precipitação biogênica de carbonatos). O oceano global armazena aproximadamente 50 vezes mais carbono que a atmosfera. A produção biológica marinha possui um papel muito importante no sequestro de carbono atmosférico, o que por sua vez é um importante mecanismo regulador do clima no planeta. (pt)</li> </ul></td></tr><tr class="even"><td class="col-2"><a class="uri" href="http://www.w3.org/2000/01/rdf-schema#label">rdfs:label</a> </td><td class="col-10 text-break"><ul> <li style="display:none;">مضخة بيولوجية (ar)</li> <li style="display:none;">Bomba biològica (ca)</li> <li>Biological pump (en)</li> <li style="display:none;">Bomba biológica (es)</li> <li style="display:none;">Pompe biologique (fr)</li> <li style="display:none;">生物ポンプ (ja)</li> <li style="display:none;">Pompa biologiczna (pl)</li> <li style="display:none;">Bomba biológica (pt)</li> <li style="display:none;">生物泵 (zh)</li> </ul></td></tr><tr class="odd"><td class="col-2"><a class="uri" href="http://www.w3.org/2000/01/rdf-schema#seeAlso">rdfs:seeAlso</a> </td><td class="col-10 text-break"><ul> <li><a class="uri" rel="rdfs:seeAlso" resource="http://dbpedia.org/resource/Whale_feces" href="http://dbpedia.org/resource/Whale_feces">dbr:Whale_feces</a></li> <li><a class="uri" rel="rdfs:seeAlso" 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text-break"><ul> <li><a class="uri" rev="foaf:primaryTopic" resource="http://en.wikipedia.org/wiki/Biological_pump" href="http://en.wikipedia.org/wiki/Biological_pump">wikipedia-en:Biological_pump</a></li> </ul></td></tr> </tbody> </table> </div> </div> </div> </section>   <section> <div class="container-xl"> <div class="text-center p-4 bg-light"> <a href="https://virtuoso.openlinksw.com/" title="OpenLink Virtuoso"><img class="powered_by" src="/statics/images/virt_power_no_border.png" alt="Powered by OpenLink Virtuoso"/></a>    <a href="http://linkeddata.org/"><img alt="This material is Open Knowledge" src="/statics/images/LoDLogo.gif"/></a>     <a href="http://dbpedia.org/sparql"><img alt="W3C Semantic Web Technology" src="/statics/images/sw-sparql-blue.png"/></a>     <a href="https://opendefinition.org/"><img alt="This material is Open Knowledge" src="/statics/images/od_80x15_red_green.png"/></a>    <a href="https://validator.w3.org/check?uri=referer"> <img 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