{"@context":{"@vocab":"https://cir.nii.ac.jp/schema/1.0/","rdfs":"http://www.w3.org/2000/01/rdf-schema#","dc":"http://purl.org/dc/elements/1.1/","dcterms":"http://purl.org/dc/terms/","foaf":"http://xmlns.com/foaf/0.1/","prism":"http://prismstandard.org/namespaces/basic/2.0/","cinii":"http://ci.nii.ac.jp/ns/1.0/","datacite":"https://schema.datacite.org/meta/kernel-4/","ndl":"http://ndl.go.jp/dcndl/terms/","jpcoar":"https://github.com/JPCOAR/schema/blob/master/2.0/"},"@id":"https://cir.nii.ac.jp/crid/1361137044790514944.json","@type":"Article","productIdentifier":[{"identifier":{"@type":"DOI","@value":"10.1029/2007gb003147"}},{"identifier":{"@type":"URI","@value":"https://api.wiley.com/onlinelibrary/tdm/v1/articles/10.1029%2F2007GB003147"}},{"identifier":{"@type":"URI","@value":"https://agupubs.onlinelibrary.wiley.com/doi/pdf/10.1029/2007GB003147"}}],"dc:title":[{"@value":"Simulated 21st century's increase in oceanic suboxia by CO\n                    <sub>2</sub>\n                    ‐enhanced biotic carbon export"}],"description":[{"type":"abstract","notation":[{"@value":"<jats:p>\n                    The primary impacts of anthropogenic CO\n                    <jats:sub>2</jats:sub>\n                    emissions on marine biogeochemical cycles predicted so far include ocean acidification, global warming induced shifts in biogeographical provinces, and a possible negative feedback on atmospheric CO\n                    <jats:sub>2</jats:sub>\n                    levels by CO\n                    <jats:sub>2</jats:sub>\n                    ‐fertilized biological production. Here we report a new potentially significant impact on the oxygen‐minimum zones of the tropical oceans. Using a model of global climate, ocean circulation, and biogeochemical cycling, we extrapolate mesocosm‐derived experimental findings of a\n                    <jats:italic>p</jats:italic>\n                    CO\n                    <jats:sub>2</jats:sub>\n                    ‐sensitive increase in biotic carbon‐to‐nitrogen drawdown to the global ocean. For a simulation run from the onset of the industrial revolution until A.D. 2100 under a “business‐as‐usual” scenario for anthropogenic CO\n                    <jats:sub>2</jats:sub>\n                    emissions, our model predicts a negative feedback on atmospheric CO\n                    <jats:sub>2</jats:sub>\n                    levels, which amounts to 34 Gt C by the end of this century. While this represents a small alteration of the anthropogenic perturbation of the carbon cycle, the model results reveal a dramatic 50% increase in the suboxic water volume by the end of this century in response to the respiration of excess organic carbon formed at higher CO\n                    <jats:sub>2</jats:sub>\n                    levels. This is a significant expansion of the marine “dead zones” with severe implications not only for all higher life forms but also for oxygen‐sensitive nutrient recycling and, hence, for oceanic nutrient inventories.\n                  </jats:p>"}]}],"creator":[{"@id":"https://cir.nii.ac.jp/crid/1381137044790514944","@type":"Researcher","foaf:name":[{"@value":"Andreas Oschlies"}],"jpcoar:affiliationName":[{"@value":"IFM‐GEOMAR, Leibniz‐Institut für Meereswissenschaften  Kiel Germany"}]},{"@id":"https://cir.nii.ac.jp/crid/1381137044790514947","@type":"Researcher","foaf:name":[{"@value":"Kai G. Schulz"}],"jpcoar:affiliationName":[{"@value":"IFM‐GEOMAR, Leibniz‐Institut für Meereswissenschaften  Kiel Germany"}]},{"@id":"https://cir.nii.ac.jp/crid/1381137044790514945","@type":"Researcher","foaf:name":[{"@value":"Ulf Riebesell"}],"jpcoar:affiliationName":[{"@value":"IFM‐GEOMAR, Leibniz‐Institut für Meereswissenschaften  Kiel Germany"}]},{"@id":"https://cir.nii.ac.jp/crid/1381137044790514946","@type":"Researcher","foaf:name":[{"@value":"Andreas Schmittner"}],"jpcoar:affiliationName":[{"@value":"College of Oceanic and Atmospheric Sciences Oregon State University  Corvallis Oregon USA"}]}],"publication":{"publicationIdentifier":[{"@type":"PISSN","@value":"08866236"},{"@type":"EISSN","@value":"19449224"}],"prism:publicationName":[{"@value":"Global Biogeochemical Cycles"}],"dc:publisher":[{"@value":"American Geophysical Union (AGU)"}],"prism:publicationDate":"2008-11-11","prism:volume":"22","prism:number":"4","prism:startingPage":"GB4008"},"reviewed":"false","dc:rights":["http://onlinelibrary.wiley.com/termsAndConditions#vor"],"url":[{"@id":"https://api.wiley.com/onlinelibrary/tdm/v1/articles/10.1029%2F2007GB003147"},{"@id":"https://agupubs.onlinelibrary.wiley.com/doi/pdf/10.1029/2007GB003147"}],"createdAt":"2008-11-10","modifiedAt":"2023-10-12","relatedProduct":[{"@id":"https://cir.nii.ac.jp/crid/1050025031476583168","@type":"Article","resourceType":"学術雑誌論文(journal article)","relationType":["isReferencedBy"],"jpcoar:relatedTitle":[{"@language":"en","@value":"Long-term response of oceanic carbon uptake to global warming via physical and biological pumps"}]},{"@id":"https://cir.nii.ac.jp/crid/1360002214348882816","@type":"Article","resourceType":"学術雑誌論文(journal article)","relationType":["isReferencedBy"],"jpcoar:relatedTitle":[{"@value":"Multidecadal trends of oxygen and their controlling factors in the western North Pacific"}]},{"@id":"https://cir.nii.ac.jp/crid/1360017282242772864","@type":"Article","resourceType":"学術雑誌論文(journal article)","relationType":["isReferencedBy"],"jpcoar:relatedTitle":[{"@value":"CANOPS-GRB v1.0: a new Earth system model for simulating the evolution of ocean–atmosphere chemistry over geologic timescales"}]},{"@id":"https://cir.nii.ac.jp/crid/1360283689327994112","@type":"Article","resourceType":"学術雑誌論文(journal article)","relationType":["isReferencedBy"],"jpcoar:relatedTitle":[{"@value":"Upper ocean O<sub>2</sub> trends: 1958–2015"}]},{"@id":"https://cir.nii.ac.jp/crid/1360290617823191680","@type":"Article","resourceType":"学術雑誌論文(journal article)","relationType":["isReferencedBy"],"jpcoar:relatedTitle":[{"@value":"What drove the evolutionary trend of planktic foraminifers during the Cretaceous: Oceanic Anoxic Events (OAEs) directly affected it?"}]},{"@id":"https://cir.nii.ac.jp/crid/1360565164302986368","@type":"Article","resourceType":"学術雑誌論文(journal article)","relationType":["isReferencedBy"],"jpcoar:relatedTitle":[{"@value":"Global deep ocean oxygenation by enhanced ventilation in the Southern Ocean under long‐term global warming"}]},{"@id":"https://cir.nii.ac.jp/crid/1360567182223473792","@type":"Article","resourceType":"学術雑誌論文(journal article)","relationType":["isReferencedBy"],"jpcoar:relatedTitle":[{"@value":"Impacts of elevated CO2 on organic carbon dynamics in nutrient depleted Okhotsk Sea surface waters"}]},{"@id":"https://cir.nii.ac.jp/crid/1360567183246260608","@type":"Article","resourceType":"学術雑誌論文(journal article)","relationType":["isReferencedBy"],"jpcoar:relatedTitle":[{"@value":"Effect of Euxinic Conditions on Planktic Foraminifers: Culture Experiments and Implications for Past and Future Environments"}]},{"@id":"https://cir.nii.ac.jp/crid/1360588379382339584","@type":"Article","resourceType":"学術雑誌論文(journal article)","relationType":["isReferencedBy"],"jpcoar:relatedTitle":[{"@value":"Measuring deoxygenation effects on marine predators: A new animal‐attached archival tag recording in situ dissolved oxygen, temperature, fine‐scale movements and behaviour"}]},{"@id":"https://cir.nii.ac.jp/crid/2050025942136465280","@type":"Article","resourceType":"学術雑誌論文(journal article)","relationType":["isReferencedBy"],"jpcoar:relatedTitle":[{"@value":"Perspective on the response of marine calcifiers to global warming and ocean acidification : behavior of corals and foraminifera in a high CO2 world “hot house”"}]}],"dataSourceIdentifier":[{"@type":"CROSSREF","@value":"10.1029/2007gb003147"},{"@type":"CROSSREF","@value":"10.1002/2014gb005065_references_DOI_SPTzD1qAgD0i4ch0skAygGgbk6p"},{"@type":"CROSSREF","@value":"10.5194/gmd-15-7593-2022_references_DOI_SPTzD1qAgD0i4ch0skAygGgbk6p"},{"@type":"CROSSREF","@value":"10.1002/2017gl073613_references_DOI_SPTzD1qAgD0i4ch0skAygGgbk6p"},{"@type":"CROSSREF","@value":"10.5194/bg-15-4163-2018_references_DOI_SPTzD1qAgD0i4ch0skAygGgbk6p"},{"@type":"CROSSREF","@value":"10.1016/j.marmicro.2020.101924_references_DOI_SPTzD1qAgD0i4ch0skAygGgbk6p"},{"@type":"CROSSREF","@value":"10.1002/2015gb005181_references_DOI_SPTzD1qAgD0i4ch0skAygGgbk6p"},{"@type":"CROSSREF","@value":"10.1029/2018pa003539_references_DOI_SPTzD1qAgD0i4ch0skAygGgbk6p"},{"@type":"CROSSREF","@value":"10.1016/j.jembe.2010.09.001_references_DOI_SPTzD1qAgD0i4ch0skAygGgbk6p"},{"@type":"CROSSREF","@value":"10.1111/2041-210x.14360_references_DOI_JS8wm7yKSX14Yle3GaZpBJlYhTJ"},{"@type":"CROSSREF","@value":"10.1186/s40645-018-0239-9_references_DOI_SPTzD1qAgD0i4ch0skAygGgbk6p"}]}