Porosity of the Northeast Greenland (NEG) shelf sediments from POLARSTERN cruise PS109
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| Title: | Porosity of the Northeast Greenland (NEG) shelf sediments from POLARSTERN cruise PS109 |
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| Authors: | Braeckman, Ulrike |
| Publisher Information: | PANGAEA |
| Publication Year: | 2024 |
| Collection: | PANGAEA - Data Publisher for Earth & Environmental Science (AWI Bremerhaven / MARUM Bremen) |
| Subject Terms: | Arctic Shelf, ARK-XXXI/4, Calculated according to Dalsgaard et al. (2000), Comment, Date/Time of event, Depth, bottom/max, sediment/rock, top/min, Elevation of event, Event label, FRAM, FRontiers in Arctic marine Monitoring, Latitude of event, Longitude of event, Method/Device of event, Multicorer with television, Polarstern, Porosity, PS109, PS109_105-1, PS109_115-3, PS109_125-3, PS109_129-1, PS109_139-4, PS109_154-2, PS109_19-4, PS109_36-3, PS109_45-3, PS109_61-1 |
| Subject Geographic: | MEDIAN LATITUDE: 78.774547 * MEDIAN LONGITUDE: -14.939610 * SOUTH-BOUND LATITUDE: 76.486370 * WEST-BOUND LONGITUDE: -19.321920 * NORTH-BOUND LATITUDE: 80.312990 * EAST-BOUND LONGITUDE: -7.109350 * DATE/TIME START: 2017-09-17T15:16:00 * DATE/TIME END: 2017-10-07T03:28:00 * MINIMUM DEPTH, sediment/rock: 0.0025 m * MAXIMUM DEPTH, sediment/rock: 0.1900 m |
| Description: | Samples for sediment porosity on the Northeast Greenland shelf have been collected with R/V Polarstern during PS109 between September and October 2017 using a camera-equipped multiple corer (TV-MUC; core area 0.007 m²). Upon arrival on deck, the upper 5 cm of three MUC cores were sliced into 1 cm intervals, using a cut-off syringe in order to get a depth resolution of the sediment porosity, and then stored in 5 ml cut-off syringes that were wrapped in aluminium foil. In the laboratory, the samples were sliced into 1 cm intervals. After measuring their wet mass, the sediment samples were dried at 60°C. The sediment porosity was calculated by the difference between the wet and dry mass after Dalsgaard et al., 2000. |
| Document Type: | dataset |
| File Description: | text/tab-separated-values, 1898 data points |
| Language: | English |
| Relation: | Bodur, Yasemin V; Renaud, Paul E; Lins, Lidia; Da Costa Monteiro, Luana; Ambrose, William G Jr; Felden, Janine; Krumpen, Thomas; Wenzhöfer, Frank; Włodarska-Kowalczuk, Maria; Braeckman, Ulrike (2024): Weakened pelagic-benthic coupling on an Arctic outflow shelf (Northeast Greenland) suggested by benthic ecosystem changes. Elementa - Science of the Anthropocene, 12(1), 00005, https://doi.org/10.1525/elementa.2023.00005; Dalsgaard, Tage; Nielsen, Lars Peter; Brotas, Vanda; Viaroli, Pierluigi; Underwood, Graham J; Nedwell, David B; Sundbäck, Kristina; Rysgaard, Søren; Miles, A; Bartoli, Marco; Dong, L F; Thornton, Daniel C O; Ottosen, Lars D M; Risgaard-Petersen, Nils (2000): Protocol Handbook for NICE-Nitrogen Cycling in Estuaries: A Project under the EU Research Programme. Marine Science and Technology (MAST III); https://doi.pangaea.de/10.1594/PANGAEA.959550; https://doi.org/10.1594/PANGAEA.959550 |
| DOI: | 10.1594/PANGAEA.959550 |
| Availability: | https://doi.pangaea.de/10.1594/PANGAEA.959550 https://doi.org/10.1594/PANGAEA.959550 |
| Rights: | CC-BY-4.0: Creative Commons Attribution 4.0 International ; Access constraints: unrestricted ; info:eu-repo/semantics/openAccess |
| Accession Number: | edsbas.4607B666 |
| Database: | BASE |
| Abstract: | Samples for sediment porosity on the Northeast Greenland shelf have been collected with R/V Polarstern during PS109 between September and October 2017 using a camera-equipped multiple corer (TV-MUC; core area 0.007 m²). Upon arrival on deck, the upper 5 cm of three MUC cores were sliced into 1 cm intervals, using a cut-off syringe in order to get a depth resolution of the sediment porosity, and then stored in 5 ml cut-off syringes that were wrapped in aluminium foil. In the laboratory, the samples were sliced into 1 cm intervals. After measuring their wet mass, the sediment samples were dried at 60°C. The sediment porosity was calculated by the difference between the wet and dry mass after Dalsgaard et al., 2000. |
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| DOI: | 10.1594/PANGAEA.959550 |
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