{"@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/1363670318367309440.json","@type":"Article","productIdentifier":[{"identifier":{"@type":"DOI","@value":"10.1038/nature10582"}},{"identifier":{"@type":"URI","@value":"https://www.nature.com/articles/nature10582.pdf"}},{"identifier":{"@type":"URI","@value":"https://www.nature.com/articles/nature10582"}}],"dc:title":[{"@value":"Subsurface water and clay mineral formation during the early history of Mars"}],"creator":[{"@id":"https://cir.nii.ac.jp/crid/1383670318367309444","@type":"Researcher","foaf:name":[{"@value":"Bethany L. Ehlmann"}]},{"@id":"https://cir.nii.ac.jp/crid/1383670318367309445","@type":"Researcher","foaf:name":[{"@value":"John F. Mustard"}]},{"@id":"https://cir.nii.ac.jp/crid/1383670318367309441","@type":"Researcher","foaf:name":[{"@value":"Scott L. Murchie"}]},{"@id":"https://cir.nii.ac.jp/crid/1383670318367309442","@type":"Researcher","foaf:name":[{"@value":"Jean-Pierre Bibring"}]},{"@id":"https://cir.nii.ac.jp/crid/1383670318367309440","@type":"Researcher","foaf:name":[{"@value":"Alain Meunier"}]},{"@id":"https://cir.nii.ac.jp/crid/1383670318367309443","@type":"Researcher","foaf:name":[{"@value":"Abigail A. Fraeman"}]},{"@id":"https://cir.nii.ac.jp/crid/1383670318367309446","@type":"Researcher","foaf:name":[{"@value":"Yves Langevin"}]}],"publication":{"publicationIdentifier":[{"@type":"PISSN","@value":"00280836"},{"@type":"EISSN","@value":"14764687"}],"prism:publicationName":[{"@value":"Nature"}],"dc:publisher":[{"@value":"Springer Science and Business Media LLC"}],"prism:publicationDate":"2011-11-02","prism:volume":"479","prism:number":"7371","prism:startingPage":"53","prism:endingPage":"60"},"reviewed":"false","dc:rights":["https://www.springer.com/tdm","https://www.springer.com/tdm"],"url":[{"@id":"https://www.nature.com/articles/nature10582.pdf"},{"@id":"https://www.nature.com/articles/nature10582"}],"createdAt":"2011-11-01","modifiedAt":"2023-06-10","relatedProduct":[{"@id":"https://cir.nii.ac.jp/crid/1050021218879286528","@type":"Article","resourceType":"学術雑誌論文(journal article)","relationType":["isReferencedBy"],"jpcoar:relatedTitle":[{"@language":"en","@value":"Hydrogen generation from ferrous saponite in reaction with H₂S-containing fluid: relevance to early Martian habitability"},{"@value":"Hydrogen Generation From Ferrous Saponite in Reaction With H<sub>2</sub>S‐Containing Fluid: Relevance to Early Martian Habitability"}]},{"@id":"https://cir.nii.ac.jp/crid/1050307746540945536","@type":"Article","resourceType":"学術雑誌論文(journal article)","relationType":["isReferencedBy"],"jpcoar:relatedTitle":[{"@language":"en","@value":"The Mars system revealed by the Martian Moons eXploration mission"}]},{"@id":"https://cir.nii.ac.jp/crid/1360004231417594496","@type":"Article","resourceType":"学術雑誌論文(journal article)","relationType":["isReferencedBy"],"jpcoar:relatedTitle":[{"@value":"Indicators and Methods to Understand Past Environments from ExoMars Rover Drills"}]},{"@id":"https://cir.nii.ac.jp/crid/1360004232184452736","@type":"Article","resourceType":"学術雑誌論文(journal article)","relationType":["isReferencedBy"],"jpcoar:relatedTitle":[{"@value":"A lower limit of atmospheric pressure on early Mars inferred from nitrogen and argon isotopic compositions"}]},{"@id":"https://cir.nii.ac.jp/crid/1360004233290665856","@type":"Article","resourceType":"学術雑誌論文(journal article)","relationType":["isReferencedBy"],"jpcoar:relatedTitle":[{"@value":"Two‐dimensional numerical studies on the effects of water on Martian mantle evolution induced by magmatism and solid‐state mantle convection"}]},{"@id":"https://cir.nii.ac.jp/crid/1360004235937271936","@type":"Article","resourceType":"学術雑誌論文(journal article)","relationType":["isReferencedBy"],"jpcoar:relatedTitle":[{"@value":"Fe-oxide concretions formed by interacting carbonate and acidic waters on Earth and Mars"}]},{"@id":"https://cir.nii.ac.jp/crid/1360013168723941632","@type":"Article","resourceType":"学術雑誌論文(journal article)","relationType":["isReferencedBy"],"jpcoar:relatedTitle":[{"@value":"Reconstruction of pH, redox condition, and concentrations of major components in ancient liquid water from the Karasburg member, Murray formation, Gale Crater, Mars"}]},{"@id":"https://cir.nii.ac.jp/crid/1360017279855457152","@type":"Article","resourceType":"学術雑誌論文(journal article)","relationType":["isReferencedBy"],"jpcoar:relatedTitle":[{"@value":"The Deep Rocky Biosphere: New Geomicrobiological Insights and Prospects"}]},{"@id":"https://cir.nii.ac.jp/crid/1360017282450945792","@type":"Article","resourceType":"学術雑誌論文(journal article)","relationType":["isReferencedBy"],"jpcoar:relatedTitle":[{"@value":"Effects of rheological stratification and elasticity of lithosphere on subduction initiation"}]},{"@id":"https://cir.nii.ac.jp/crid/1360025429423107200","@type":"Article","resourceType":"学術雑誌論文(journal article)","relationType":["isReferencedBy"],"jpcoar:relatedTitle":[{"@value":"Iron redox states in closed-basin lakes on early Mars: Its sensitivity to water chemistry, hydrology, and atmospheric composition"}]},{"@id":"https://cir.nii.ac.jp/crid/1360285707146395136","@type":"Article","resourceType":"学術雑誌論文(journal article)","relationType":["isReferencedBy"],"jpcoar:relatedTitle":[{"@value":"The Goshogake mud volcano field, Tohoku, northern Japan: An acidic, high-temperature system related to magmatic volcanism"}]},{"@id":"https://cir.nii.ac.jp/crid/1360285714477160832","@type":"Article","resourceType":"学術雑誌論文(journal article)","relationType":["isReferencedBy"],"jpcoar:relatedTitle":[{"@value":"A Hypothesis: Life Initiated from Two Genes, as Deduced from the RNA World Hypothesis and the Characteristics of Life-Like Systems"}]},{"@id":"https://cir.nii.ac.jp/crid/1360290617778816256","@type":"Article","resourceType":"学術雑誌論文(journal article)","relationType":["isReferencedBy"],"jpcoar:relatedTitle":[{"@value":"Thermodynamic Constraints on Smectite and Iron Oxide Formation at Gale Crater, Mars: Insights into Potential Free Energy from Aerobic Fe Oxidation in Lake Water–Groundwater Mixing Zone"}]},{"@id":"https://cir.nii.ac.jp/crid/1360290617843720448","@type":"Article","resourceType":"学術雑誌論文(journal article)","relationType":["isReferencedBy"],"jpcoar:relatedTitle":[{"@value":"Deep microbial proliferation at the basalt interface in 33.5–104 million-year-old oceanic crust"}]},{"@id":"https://cir.nii.ac.jp/crid/1360294643702061312","@type":"Article","resourceType":"学術雑誌論文(journal article)","relationType":["isReferencedBy"],"jpcoar:relatedTitle":[{"@value":"Synthesis of ferrian and ferro-saponites: Implications for the structure of (Fe,Mg)-smectites formed under reduced conditions"}]},{"@id":"https://cir.nii.ac.jp/crid/1360298755603034112","@type":"Article","resourceType":"学術雑誌論文(journal article)","relationType":["isReferencedBy"],"jpcoar:relatedTitle":[{"@value":"Characterization of groundwater chemistry beneath Gale Crater on early Mars by hydrothermal experiments"}]},{"@id":"https://cir.nii.ac.jp/crid/1360565164304355840","@type":"Article","resourceType":"学術雑誌論文(journal article)","relationType":["isReferencedBy"],"jpcoar:relatedTitle":[{"@value":"The sustainability of habitability on terrestrial planets: Insights, questions, and needed measurements from Mars for understanding the evolution of Earth‐like worlds"}]},{"@id":"https://cir.nii.ac.jp/crid/1360565166569290752","@type":"Article","resourceType":"学術雑誌論文(journal article)","relationType":["isReferencedBy"],"jpcoar:relatedTitle":[{"@value":"Nitrogen Isotopic Fractionation in Ammonia during Adsorption on Silicate Surfaces"}]},{"@id":"https://cir.nii.ac.jp/crid/1360567182088812672","@type":"Article","resourceType":"学術雑誌論文(journal article)","relationType":["isReferencedBy"],"jpcoar:relatedTitle":[{"@value":"Meteoritic evidence for a previously unrecognized hydrogen reservoir on Mars"}]},{"@id":"https://cir.nii.ac.jp/crid/1360567185751455616","@type":"Article","resourceType":"学術雑誌論文(journal article)","relationType":["isReferencedBy"],"jpcoar:relatedTitle":[{"@value":"The potential science and engineering value of samples delivered to Earth by Mars sample return"}]},{"@id":"https://cir.nii.ac.jp/crid/1360572092879513216","@type":"Article","resourceType":"学術雑誌論文(journal article)","relationType":["isReferencedBy"],"jpcoar:relatedTitle":[{"@value":"EXAFS Determination of Clay Minerals in Martian Meteorite Allan Hills 84001 and Its Implication for the Noachian Aqueous Environment"}]},{"@id":"https://cir.nii.ac.jp/crid/1360576118678886912","@type":"Article","resourceType":"学術雑誌論文(journal article)","relationType":["isReferencedBy"],"jpcoar:relatedTitle":[{"@value":"Anaerobic Microscopic Analysis of Ferrous Saponite and Its Sensitivity to Oxidation by Earth’s Air: Lessons Learned for Analysis of Returned Samples from Mars and Carbonaceous Asteroids"}]},{"@id":"https://cir.nii.ac.jp/crid/1360580229788217856","@type":"Article","resourceType":"学術雑誌論文(journal article)","relationType":["isReferencedBy"],"jpcoar:relatedTitle":[{"@value":"Recognition and Classification of Martian Chaos Terrains Using Imagery Machine Learning: A Global Distribution of Chaos Linked to Groundwater Circulation, Catastrophic Flooding, and Magmatism on Mars"}]},{"@id":"https://cir.nii.ac.jp/crid/1360584339762429952","@type":"Article","resourceType":"学術雑誌論文(journal article)","relationType":["isReferencedBy"],"jpcoar:relatedTitle":[{"@value":"Identification of carbonate-associated sulfate (CAS) in a Noachian Martian meteorite Allan Hills 84001"}]},{"@id":"https://cir.nii.ac.jp/crid/1360848656916738816","@type":"Article","resourceType":"学術雑誌論文(journal article)","relationType":["isReferencedBy"],"jpcoar:relatedTitle":[{"@value":"Planetary protection on international waters: An onboard protocol for capsule retrieval and biosafety control in sample return mission"}]},{"@id":"https://cir.nii.ac.jp/crid/1360853567796167552","@type":"Article","resourceType":"学術雑誌論文(journal article)","relationType":["isReferencedBy"],"jpcoar:relatedTitle":[{"@value":"A New Constraint on the Physicochemical Condition of Mars Surface during the Amazonian Epoch Based on Chemical Speciation for Secondary Minerals in Martian Nakhlites"}]},{"@id":"https://cir.nii.ac.jp/crid/1360857593703440384","@type":"Article","resourceType":"学術雑誌論文(journal article)","relationType":["isReferencedBy"],"jpcoar:relatedTitle":[{"@value":"Global climate and river transport simulations of early Mars around the Noachian and Hesperian boundary"}]},{"@id":"https://cir.nii.ac.jp/crid/1360857593819027840","@type":"Article","resourceType":"学術雑誌論文(journal article)","relationType":["isReferencedBy"],"jpcoar:relatedTitle":[{"@value":"The Four‐Stage Evolution of Martian Mantle Inferred From Numerical Simulation of the Magmatism‐Mantle Upwelling Feedback"}]},{"@id":"https://cir.nii.ac.jp/crid/1360861707153993088","@type":"Article","resourceType":"学術雑誌論文(journal article)","relationType":["isReferencedBy"],"jpcoar:relatedTitle":[{"@value":"Assessing Diffusion Relaxation of Interlayer Water in Clay Minerals Using a Minimalist Three-Parameter Model"}]},{"@id":"https://cir.nii.ac.jp/crid/1360861707386077184","@type":"Article","resourceType":"学術雑誌論文(journal article)","relationType":["isReferencedBy"],"jpcoar:relatedTitle":[{"@value":"Bleached-spot formation in Fe-oxide-rich rock by inorganic process"}]},{"@id":"https://cir.nii.ac.jp/crid/1360869854368245632","@type":"Article","resourceType":"学術雑誌論文(journal article)","relationType":["isReferencedBy"],"jpcoar:relatedTitle":[{"@value":"Reconstructing the geological and geomorphological history of Morella Crater, Mars"}]},{"@id":"https://cir.nii.ac.jp/crid/1360869856030331776","@type":"Article","resourceType":"学術雑誌論文(journal article)","relationType":["isReferencedBy"],"jpcoar:relatedTitle":[{"@value":"Seismic discontinuity in the Martian crust possibly caused by water-filled cracks"}]},{"@id":"https://cir.nii.ac.jp/crid/1361131415957334912","@type":"Article","resourceType":"学術雑誌論文(journal article)","relationType":["isReferencedBy"],"jpcoar:relatedTitle":[{"@value":"Experimental and Simulation Efforts in the Astrobiological Exploration of Exooceans"}]},{"@id":"https://cir.nii.ac.jp/crid/1361694365910710016","@type":"Article","resourceType":"学術雑誌論文(journal article)","relationType":["isReferencedBy"],"jpcoar:relatedTitle":[{"@value":"Relict Ocean Worlds: Ceres"}]},{"@id":"https://cir.nii.ac.jp/crid/1390001204553908352","@type":"Article","resourceType":"学術雑誌論文(journal article)","relationType":["isReferencedBy"],"jpcoar:relatedTitle":[{"@language":"en","@value":"Combined investigation of H isotopic compositions and U-Pb chronology of young Martian meteorite Larkman Nunatak 06319"}]},{"@id":"https://cir.nii.ac.jp/crid/1390001205321265920","@type":"Article","resourceType":"学術雑誌論文(journal article)","relationType":["isReferencedBy"],"jpcoar:relatedTitle":[{"@language":"en","@value":"LDM (Life Detection Microscope): In Situ Imaging of Living Cells on Surface of Mars"}]},{"@id":"https://cir.nii.ac.jp/crid/1390001206240184576","@type":"Article","resourceType":"学術雑誌論文(journal article)","relationType":["isReferencedBy"],"jpcoar:relatedTitle":[{"@language":"en","@value":"Aqueous environmental history of Mars revealed by mineralogy and geochemistry of outcrop exposures of sedimentary rocks"},{"@language":"ja","@value":"鉱物・化学組成から読み取る火星の環境変動史"},{"@language":"ja-Kana","@value":"コウブツ ・ カガク ソセイ カラ ヨミトル カセイ ノ カンキョウ ヘンドウシ"}]},{"@id":"https://cir.nii.ac.jp/crid/1390295568881188224","@type":"Article","resourceType":"学術雑誌論文(journal article)","relationType":["isReferencedBy"],"jpcoar:relatedTitle":[{"@language":"en","@value":"Occurrence and formational mechanisms of spherical Fe-oxide concretions on Earth and Mars"},{"@language":"ja","@value":"地球と火星に見られる球状鉄コンクリーションの産状と成因"}]},{"@id":"https://cir.nii.ac.jp/crid/1390849931318623232","@type":"Article","relationType":["isReferencedBy"],"jpcoar:relatedTitle":[{"@language":"en","@value":"Mars had the suitable water chemistry for life"},{"@language":"ja","@value":"火星は生命の誕生と生存に適した環境だった"},{"@value":"サイエンスよみもの 火星は生命の誕生と生存に適した環境だった"},{"@language":"ja-Kana","@value":"サイエンス ヨミ モノ カセイ ワ セイメイ ノ タンジョウ ト セイゾン ニ テキシタ カンキョウ ダッタ"}]},{"@id":"https://cir.nii.ac.jp/crid/2050870367067985792","@type":"Article","resourceType":"学術雑誌論文(journal article)","relationType":["isReferencedBy"],"jpcoar:relatedTitle":[{"@value":"Sensitivity of elastic thickness to water in the Martian lithosphere"}]},{"@id":"https://cir.nii.ac.jp/crid/2051151842057867776","@type":"Article","resourceType":"学術雑誌論文(journal article)","relationType":["isReferencedBy"],"jpcoar:relatedTitle":[{"@value":"Analytical protocols for Phobos regolith samples returned by the Martian Moons eXploration (MMX) mission"}]},{"@id":"https://cir.nii.ac.jp/crid/2051996266985512064","@type":"Article","resourceType":"学術雑誌論文(journal article)","relationType":["isReferencedBy"],"jpcoar:relatedTitle":[{"@value":"Strength models of the terrestrial planets and implications for their lithospheric structure and evolution"}]}],"dataSourceIdentifier":[{"@type":"CROSSREF","@value":"10.1038/nature10582"},{"@type":"CROSSREF","@value":"10.1007/s11084-016-9492-3_references_DOI_6gBN3Qqbnu1YVaKiHCzlgOgalAH"},{"@type":"CROSSREF","@value":"10.1029/2012je004054_references_DOI_6gBN3Qqbnu1YVaKiHCzlgOgalAH"},{"@type":"CROSSREF","@value":"10.1126/sciadv.aau0872_references_DOI_6gBN3Qqbnu1YVaKiHCzlgOgalAH"},{"@type":"CROSSREF","@value":"10.1021/acsearthspacechem.6b00006_references_DOI_6gBN3Qqbnu1YVaKiHCzlgOgalAH"},{"@type":"CROSSREF","@value":"10.1016/j.gca.2022.02.005_references_DOI_6gBN3Qqbnu1YVaKiHCzlgOgalAH"},{"@type":"CROSSREF","@value":"10.3389/fmicb.2021.785743_references_DOI_6gBN3Qqbnu1YVaKiHCzlgOgalAH"},{"@type":"CROSSREF","@value":"10.3389/feart.2022.988320_references_DOI_6gBN3Qqbnu1YVaKiHCzlgOgalAH"},{"@type":"CROSSREF","@value":"10.1016/j.gca.2024.07.030_references_DOI_6gBN3Qqbnu1YVaKiHCzlgOgalAH"},{"@type":"CROSSREF","@value":"10.3390/life6030029_references_DOI_6gBN3Qqbnu1YVaKiHCzlgOgalAH"},{"@type":"CROSSREF","@value":"10.1016/j.geomorph.2018.12.035_references_DOI_6gBN3Qqbnu1YVaKiHCzlgOgalAH"},{"@type":"CROSSREF","@value":"10.2322/tastj.16.299_references_DOI_6gBN3Qqbnu1YVaKiHCzlgOgalAH"},{"@type":"CROSSREF","@value":"10.5575/geosoc.2012.0001_references_DOI_6gBN3Qqbnu1YVaKiHCzlgOgalAH"},{"@type":"CROSSREF","@value":"10.3390/min11040341_references_DOI_6gBN3Qqbnu1YVaKiHCzlgOgalAH"},{"@type":"CROSSREF","@value":"10.1038/s42003-020-0860-1_references_DOI_6gBN3Qqbnu1YVaKiHCzlgOgalAH"},{"@type":"CROSSREF","@value":"10.5575/geosoc.2022.0052_references_DOI_6gBN3Qqbnu1YVaKiHCzlgOgalAH"},{"@type":"CROSSREF","@value":"10.1016/j.icarus.2022.115149_references_DOI_6gBN3Qqbnu1YVaKiHCzlgOgalAH"},{"@type":"CROSSREF","@value":"10.1029/2024je008538_references_DOI_6gBN3Qqbnu1YVaKiHCzlgOgalAH"},{"@type":"CROSSREF","@value":"10.1002/2016je005134_references_DOI_6gBN3Qqbnu1YVaKiHCzlgOgalAH"},{"@type":"CROSSREF","@value":"10.1111/maps.13242_references_DOI_6gBN3Qqbnu1YVaKiHCzlgOgalAH"},{"@type":"CROSSREF","@value":"10.2343/geochemj.2.0424_references_DOI_6gBN3Qqbnu1YVaKiHCzlgOgalAH"},{"@type":"CROSSREF","@value":"10.1186/s40645-019-0298-6_references_DOI_6gBN3Qqbnu1YVaKiHCzlgOgalAH"},{"@type":"CROSSREF","@value":"10.1016/j.icarus.2017.08.020_references_DOI_6gBN3Qqbnu1YVaKiHCzlgOgalAH"},{"@type":"CROSSREF","@value":"10.1016/j.asr.2013.12.041_references_DOI_6gBN3Qqbnu1YVaKiHCzlgOgalAH"},{"@type":"CROSSREF","@value":"10.1186/s40645-020-00388-2_references_DOI_6gBN3Qqbnu1YVaKiHCzlgOgalAH"},{"@type":"CROSSREF","@value":"10.3390/min11020176_references_DOI_6gBN3Qqbnu1YVaKiHCzlgOgalAH"},{"@type":"CROSSREF","@value":"10.3390/min11111244_references_DOI_6gBN3Qqbnu1YVaKiHCzlgOgalAH"},{"@type":"CROSSREF","@value":"10.1186/s40623-021-01438-9_references_DOI_6gBN3Qqbnu1YVaKiHCzlgOgalAH"},{"@type":"CROSSREF","@value":"10.1186/s40623-021-01417-0_references_DOI_6gBN3Qqbnu1YVaKiHCzlgOgalAH"},{"@type":"CROSSREF","@value":"10.3390/rs14163883_references_DOI_6gBN3Qqbnu1YVaKiHCzlgOgalAH"},{"@type":"CROSSREF","@value":"10.1016/j.epsl.2023.118345_references_DOI_6gBN3Qqbnu1YVaKiHCzlgOgalAH"},{"@type":"CROSSREF","@value":"10.1016/j.epsl.2014.11.022_references_DOI_6gBN3Qqbnu1YVaKiHCzlgOgalAH"},{"@type":"CROSSREF","@value":"10.3390/min11050514_references_DOI_6gBN3Qqbnu1YVaKiHCzlgOgalAH"},{"@type":"CROSSREF","@value":"10.1016/j.icarus.2021.114618_references_DOI_6gBN3Qqbnu1YVaKiHCzlgOgalAH"},{"@type":"CROSSREF","@value":"10.1029/2021je006997_references_DOI_6gBN3Qqbnu1YVaKiHCzlgOgalAH"},{"@type":"CROSSREF","@value":"10.2138/am-2022-8231_references_DOI_6gBN3Qqbnu1YVaKiHCzlgOgalAH"},{"@type":"CROSSREF","@value":"10.1021/acs.jpcc.1c04322_references_DOI_6gBN3Qqbnu1YVaKiHCzlgOgalAH"},{"@type":"CROSSREF","@value":"10.1016/j.chemgeo.2022.121049_references_DOI_6gBN3Qqbnu1YVaKiHCzlgOgalAH"},{"@type":"CROSSREF","@value":"10.1016/j.geomorph.2025.109740_references_DOI_6gBN3Qqbnu1YVaKiHCzlgOgalAH"},{"@type":"CROSSREF","@value":"10.1130/g52369.1_references_DOI_6gBN3Qqbnu1YVaKiHCzlgOgalAH"},{"@type":"CROSSREF","@value":"10.1007/s11214-020-0635-5_references_DOI_6gBN3Qqbnu1YVaKiHCzlgOgalAH"},{"@type":"CROSSREF","@value":"10.1007/s11214-020-00683-w_references_DOI_6gBN3Qqbnu1YVaKiHCzlgOgalAH"},{"@type":"CROSSREF","@value":"10.3327/jaesjb.62.7_378_references_DOI_6gBN3Qqbnu1YVaKiHCzlgOgalAH"}]}