Mass flux, major components and the Lead 210 concentration of sediment collected using a Bottom Boundary (BOBO) lander at the Gardar Drift in the North Atlantic
To monitor particle fluxes and near bottom hydrographic variability a modified version of the benthic Bottom Boundary (BOBO) lander was deployed at 57 29.09 N, 27 54.53 W on the Gardar Drift at a water depth of 2630 m. The lander was fitted with three extended Technicap PPS 4/3 sediment traps, each...
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Format: | Dataset |
Language: | English |
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PANGAEA
2022
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Online Access: | https://doi.pangaea.de/10.1594/PANGAEA.947855 https://doi.org/10.1594/PANGAEA.947855 |
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ftpangaea:oai:pangaea.de:doi:10.1594/PANGAEA.947855 |
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openpolar |
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Open Polar |
collection |
PANGAEA - Data Publisher for Earth & Environmental Science |
op_collection_id |
ftpangaea |
language |
English |
topic |
Alpha spectrometry Benthic bottom boundary lander BOBO lander Calcium carbonate Calculated Carbon organic total Carlo Erba Flash 1112 elemental analyser contourite Date/time end Date/time start Gardar_Drift Lead-210 standard deviation Lithogenic material Mass flux Nitrogen Opal biogenic silica Sample code/label sediment trap Sequential leaching technique Split Technicap PPS4/3 Total mass flux per day |
spellingShingle |
Alpha spectrometry Benthic bottom boundary lander BOBO lander Calcium carbonate Calculated Carbon organic total Carlo Erba Flash 1112 elemental analyser contourite Date/time end Date/time start Gardar_Drift Lead-210 standard deviation Lithogenic material Mass flux Nitrogen Opal biogenic silica Sample code/label sediment trap Sequential leaching technique Split Technicap PPS4/3 Total mass flux per day Jonkers, Lukas Mass flux, major components and the Lead 210 concentration of sediment collected using a Bottom Boundary (BOBO) lander at the Gardar Drift in the North Atlantic |
topic_facet |
Alpha spectrometry Benthic bottom boundary lander BOBO lander Calcium carbonate Calculated Carbon organic total Carlo Erba Flash 1112 elemental analyser contourite Date/time end Date/time start Gardar_Drift Lead-210 standard deviation Lithogenic material Mass flux Nitrogen Opal biogenic silica Sample code/label sediment trap Sequential leaching technique Split Technicap PPS4/3 Total mass flux per day |
description |
To monitor particle fluxes and near bottom hydrographic variability a modified version of the benthic Bottom Boundary (BOBO) lander was deployed at 57 29.09 N, 27 54.53 W on the Gardar Drift at a water depth of 2630 m. The lander was fitted with three extended Technicap PPS 4/3 sediment traps, each with a baffled collecting area of 0.05 m2 positioned at 4 metres above the seafloor. Trap bottles were filled with ambient seawater and poisoned with a pH-buffered HgCl2 solution and rotated every 11 days. To test the performance of each sediment trap, two traps were programmed to collect material synchronously for three intervals during the deployment. Fluxes were intercepted successfully from 2007-09-19 through 2008-08-03. Full details about the deployment can be found in Jonkers et al., 2010 (doi:10.1016/j.dsr.2010.05.005). Pitch and roll of the lander were recorded and displayed very little variation (1.8370.031 and 0.3370.041, respectively); trapping efficiency was thus uncompromised by the movement of the lander. Upon recovery the pH of the supernatant was measured and found to range from 8.5 to 8.8, indicating minimum sample degradation. The samples were stored at 4 degC. Before sample processing in the laboratory the supernatant was sampled for dissolved Si analysis to correct for the dissolution of the particulate biogenic silica (doi:10.1016/j.margeo.2005.11.001; doi:10.1016/S0967-0645(97)00018-0). Swimmers larger than 1 mm were removed prior to splitting of the samples for further analysis. Carbon and nitrogen were separately analysed on weighed aliquots of the bulk material before and after removal of the carbonate-carbon (doi:10.1016/S0967-0637(02)00030-4) using a Carlo Erba Instruments Flash 1112 elemental analyzer. Biogenic silica (BSi) was determined by continuous alkaline leaching that accounts for contributions by co-leaching of Al-silicates (doi:10.1023/A:1020318610178). The lithogenic content was calculated according to doi:10.1016/S0924-7963(02)00189-6. Samples were analysed for 210Pb activity ... |
format |
Dataset |
author |
Jonkers, Lukas |
author_facet |
Jonkers, Lukas |
author_sort |
Jonkers, Lukas |
title |
Mass flux, major components and the Lead 210 concentration of sediment collected using a Bottom Boundary (BOBO) lander at the Gardar Drift in the North Atlantic |
title_short |
Mass flux, major components and the Lead 210 concentration of sediment collected using a Bottom Boundary (BOBO) lander at the Gardar Drift in the North Atlantic |
title_full |
Mass flux, major components and the Lead 210 concentration of sediment collected using a Bottom Boundary (BOBO) lander at the Gardar Drift in the North Atlantic |
title_fullStr |
Mass flux, major components and the Lead 210 concentration of sediment collected using a Bottom Boundary (BOBO) lander at the Gardar Drift in the North Atlantic |
title_full_unstemmed |
Mass flux, major components and the Lead 210 concentration of sediment collected using a Bottom Boundary (BOBO) lander at the Gardar Drift in the North Atlantic |
title_sort |
mass flux, major components and the lead 210 concentration of sediment collected using a bottom boundary (bobo) lander at the gardar drift in the north atlantic |
publisher |
PANGAEA |
publishDate |
2022 |
url |
https://doi.pangaea.de/10.1594/PANGAEA.947855 https://doi.org/10.1594/PANGAEA.947855 |
op_coverage |
LATITUDE: 57.485833 * LONGITUDE: -27.914722 |
long_lat |
ENVELOPE(-27.914722,-27.914722,57.485833,57.485833) |
genre |
North Atlantic |
genre_facet |
North Atlantic |
op_relation |
Jonkers, Lukas (2022): Current speed and acoustic backscatter data measured with a Bottom Boundary (BOBO) lander at the Gardar Drift in the North Atlantic. PANGAEA, https://doi.org/10.1594/PANGAEA.947849 Jonkers, Lukas (2022): Salinity, temperature and optical backscatter data measured with a Bottom Boundary (BOBO) lander at the Gardar Drift in the North Atlantic. PANGAEA, https://doi.org/10.1594/PANGAEA.947853 Jonkers, Lukas; Mienis, Furu; Boer, Wim; Hall, Ian R; Brummer, Geert-Jan A (2010): Intra-annual variability of extremely rapid sedimentation onto Gardar Drift in the northern North Atlantic. Deep Sea Research Part I: Oceanographic Research Papers, 57(8), 1027-1038, https://doi.org/10.1016/j.dsr.2010.05.005 https://doi.pangaea.de/10.1594/PANGAEA.947855 https://doi.org/10.1594/PANGAEA.947855 |
op_rights |
CC-BY-4.0: Creative Commons Attribution 4.0 International Access constraints: unrestricted info:eu-repo/semantics/openAccess |
op_rightsnorm |
CC-BY |
op_doi |
https://doi.org/10.1594/PANGAEA.947855 https://doi.org/10.1594/PANGAEA.947849 https://doi.org/10.1594/PANGAEA.947853 https://doi.org/10.1016/j.dsr.2010.05.005 |
_version_ |
1766137013794242560 |
spelling |
ftpangaea:oai:pangaea.de:doi:10.1594/PANGAEA.947855 2023-05-15T17:37:13+02:00 Mass flux, major components and the Lead 210 concentration of sediment collected using a Bottom Boundary (BOBO) lander at the Gardar Drift in the North Atlantic Jonkers, Lukas LATITUDE: 57.485833 * LONGITUDE: -27.914722 2022-09-02 text/tab-separated-values, 416 data points https://doi.pangaea.de/10.1594/PANGAEA.947855 https://doi.org/10.1594/PANGAEA.947855 en eng PANGAEA Jonkers, Lukas (2022): Current speed and acoustic backscatter data measured with a Bottom Boundary (BOBO) lander at the Gardar Drift in the North Atlantic. PANGAEA, https://doi.org/10.1594/PANGAEA.947849 Jonkers, Lukas (2022): Salinity, temperature and optical backscatter data measured with a Bottom Boundary (BOBO) lander at the Gardar Drift in the North Atlantic. PANGAEA, https://doi.org/10.1594/PANGAEA.947853 Jonkers, Lukas; Mienis, Furu; Boer, Wim; Hall, Ian R; Brummer, Geert-Jan A (2010): Intra-annual variability of extremely rapid sedimentation onto Gardar Drift in the northern North Atlantic. Deep Sea Research Part I: Oceanographic Research Papers, 57(8), 1027-1038, https://doi.org/10.1016/j.dsr.2010.05.005 https://doi.pangaea.de/10.1594/PANGAEA.947855 https://doi.org/10.1594/PANGAEA.947855 CC-BY-4.0: Creative Commons Attribution 4.0 International Access constraints: unrestricted info:eu-repo/semantics/openAccess CC-BY Alpha spectrometry Benthic bottom boundary lander BOBO lander Calcium carbonate Calculated Carbon organic total Carlo Erba Flash 1112 elemental analyser contourite Date/time end Date/time start Gardar_Drift Lead-210 standard deviation Lithogenic material Mass flux Nitrogen Opal biogenic silica Sample code/label sediment trap Sequential leaching technique Split Technicap PPS4/3 Total mass flux per day Dataset 2022 ftpangaea https://doi.org/10.1594/PANGAEA.947855 https://doi.org/10.1594/PANGAEA.947849 https://doi.org/10.1594/PANGAEA.947853 https://doi.org/10.1016/j.dsr.2010.05.005 2023-01-20T09:16:19Z To monitor particle fluxes and near bottom hydrographic variability a modified version of the benthic Bottom Boundary (BOBO) lander was deployed at 57 29.09 N, 27 54.53 W on the Gardar Drift at a water depth of 2630 m. The lander was fitted with three extended Technicap PPS 4/3 sediment traps, each with a baffled collecting area of 0.05 m2 positioned at 4 metres above the seafloor. Trap bottles were filled with ambient seawater and poisoned with a pH-buffered HgCl2 solution and rotated every 11 days. To test the performance of each sediment trap, two traps were programmed to collect material synchronously for three intervals during the deployment. Fluxes were intercepted successfully from 2007-09-19 through 2008-08-03. Full details about the deployment can be found in Jonkers et al., 2010 (doi:10.1016/j.dsr.2010.05.005). Pitch and roll of the lander were recorded and displayed very little variation (1.8370.031 and 0.3370.041, respectively); trapping efficiency was thus uncompromised by the movement of the lander. Upon recovery the pH of the supernatant was measured and found to range from 8.5 to 8.8, indicating minimum sample degradation. The samples were stored at 4 degC. Before sample processing in the laboratory the supernatant was sampled for dissolved Si analysis to correct for the dissolution of the particulate biogenic silica (doi:10.1016/j.margeo.2005.11.001; doi:10.1016/S0967-0645(97)00018-0). Swimmers larger than 1 mm were removed prior to splitting of the samples for further analysis. Carbon and nitrogen were separately analysed on weighed aliquots of the bulk material before and after removal of the carbonate-carbon (doi:10.1016/S0967-0637(02)00030-4) using a Carlo Erba Instruments Flash 1112 elemental analyzer. Biogenic silica (BSi) was determined by continuous alkaline leaching that accounts for contributions by co-leaching of Al-silicates (doi:10.1023/A:1020318610178). The lithogenic content was calculated according to doi:10.1016/S0924-7963(02)00189-6. Samples were analysed for 210Pb activity ... Dataset North Atlantic PANGAEA - Data Publisher for Earth & Environmental Science ENVELOPE(-27.914722,-27.914722,57.485833,57.485833) |