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  "code": "7b.b.f",
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  "code": "7b.b.f",
            
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  "contributor": "NIOZ Royal Netherlands Institute for Sea Research",
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  "contributor": "NIOZ Royal Netherlands Institute for Sea Research",
            
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  "creators": 
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\"firstname\":\"Eric\",\"lastname\":\"Epping\",\"affiliation\":\"Royal 
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\"firstname\":\"Eric\",\"lastname\":\"Epping\",\"affiliation\":\"Royal 
            
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Netherlands Institute for Sea 
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Netherlands Institute for Sea 
            
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iladdress\":\"eric.epping@nioz.nl\",\"iscorrespondingauthor\":true}]",
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iladdress\":\"eric.epping@nioz.nl\",\"iscorrespondingauthor\":true}]",
            
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  "dates": 
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  "dates": 
            
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  "deposit_date": "2018-09-19",
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  "deposit_date": "2018-09-19",
            
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  "depositor": "Eric Epping",
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  "depositor": "Eric Epping",
            
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  "distribution_date": "2018-09-19",
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  "distribution_date": "2018-09-19",
            
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  "distributor": "Research Data Management(NIOZ Royal Netherlands 
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  "distributor": "Research Data Management(NIOZ Royal Netherlands 
            
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Institute for Sea Research)",
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Institute for Sea Research)",
            
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  "doi_date_published": "2018-09-19",
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  "doi_date_published": "2018-09-19",
            
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  "funding_references": "[{\"name\":\"European Community 
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  "funding_references": "[{\"name\":\"European Community 
            
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ST\",\"awardnumber\":\"MAS3-CT96-0056\",\"awardtitle\":\"OMEX-II\"}]",
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ST\",\"awardnumber\":\"MAS3-CT96-0056\",\"awardtitle\":\"OMEX-II\"}]",
            
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  "geographic_coverage": "[{\"place\":\"Iberian 
            
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  "name": "7bbf",
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  "name": "7bbf",
            
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  "notes": "Comparison of in situ and shipboard techniques to measure 
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  "notes": "Comparison of in situ and shipboard techniques to measure 
            
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oxygen distribution in deep sea sediment reveals non-steady state 
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oxygen distribution in deep sea sediment reveals non-steady state 
            
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behavior when profiles are measured shipboard. This suggest a boosting 
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behavior when profiles are measured shipboard. This suggest a boosting 
            
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of microbial activity in the surface sediment, probably due to the 
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of microbial activity in the surface sediment, probably due to the 
            
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exudation of highly reactive organics by in fauna due to 
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exudation of highly reactive organics by in fauna due to 
            
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decompression.",
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decompression.",
            
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  "subject": "Earth and Environmental Sciences",
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  "title": "Sediment oxygen concentrations in Iberian Margin 
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  "title": "Sediment oxygen concentrations in Iberian Margin 
            
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sediments",
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sediments",
            
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