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  "code": "7b.b.p",
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  "code": "7b.b.p",
            
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  "contributor": "NIOZ Royal Netherlands Institute for Sea Research",
            
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  "creators": 
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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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004-05-13T22:00:00.000Z\",\"type\":\"collected\",\"information\":\"Leg 
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004-05-13T22:00:00.000Z\",\"type\":\"collected\",\"information\":\"Leg 
            
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period 1\"}]",
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period 1\"}]",
            
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  "deposit_date": "2019-07-19",
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  "deposit_date": "2019-07-19",
            
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  "depositor": "Wim Pool",
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  "depositor": "Wim Pool",
            
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  "distribution_date": "2019-07-19",
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  "distribution_date": "2019-07-19",
            
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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": "2019-07-19",
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  "funding_references": 
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  "funding_references": 
            
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"[{\"name\":\"EU\",\"awardnumber\":\"\",\"awardtitle\":\"Canyons 
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"[{\"name\":\"EU\",\"awardnumber\":\"\",\"awardtitle\":\"Canyons 
            
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2004\"}]",
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2004\"}]",
            
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  "geographic_coverage": "[{\"place\":\"Mediterranean and Atlantic 
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  "geographic_coverage": "[{\"place\":\"Mediterranean and Atlantic 
            
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Iberian 
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Iberian 
            
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\"\",\"longitude_1\":\"\",\"latitude_2\":\"\",\"longitude_2\":\"\"}]",
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\"\",\"longitude_1\":\"\",\"latitude_2\":\"\",\"longitude_2\":\"\"}]",
            
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  "metadata_modified": "2024-10-22T13:46:33.633194",
            
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  "name": "7bbp",
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  "name": "7bbp",
            
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  "notes": "Shelf morphology and local hydrodynamical conditions may 
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  "notes": "Shelf morphology and local hydrodynamical conditions may 
            
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significantly influence the partitioning of material (terrestrial or 
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significantly influence the partitioning of material (terrestrial or 
            
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in situ production) between shelf sediments (0-200 m) and the deeper 
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in situ production) between shelf sediments (0-200 m) and the deeper 
            
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ocean margin sediments (200-2000 m). Submarine canyons are typical 
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ocean margin sediments (200-2000 m). Submarine canyons are typical 
            
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morphological features of the rather narrow Iberian shelf. They have 
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morphological features of the rather narrow Iberian shelf. They have 
            
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been shown to trap and transport material from the shelf to the abyss. 
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been shown to trap and transport material from the shelf to the abyss. 
            
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During the OMEX cruise in 1999 the relative contribution of canyons in 
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During the OMEX cruise in 1999 the relative contribution of canyons in 
            
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off-shelf transport was studied by comparing sediment carbon budgets 
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off-shelf transport was studied by comparing sediment carbon budgets 
            
n
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for the Nazar?? Canyon and for ???normal??? shelf-slope-abyssal 
n
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for the Nazar\u00e9 Canyon and for \u2018normal\u2019 
            
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transects. In this study, three different canyon-shelf systems were 
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shelf-slope-abyssal transects. In this study, three different 
            
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compared, Setubal and Nazar?? Canyons on the Iberian Margin and Cap de 
45
canyon-shelf systems were compared, Setubal and Nazar\u00e9 Canyons on 
            
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Cr??us Canyon in the Gulf of Lyon.",
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the Iberian Margin and Cap de Cr\u00e9us Canyon in the Gulf of Lyon.",
            
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      "display_name": "Shelf - deep sea exchange",
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  "title": "Nutrient pore water profiles in Portuguese marine 
            
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canyons",
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canyons",
            
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