Changes
On October 22, 2024, 9:40:45 AM UTC,
-
Changed the version of Patterns of (trace) metals and microorganisms in the Rainbow hydrothermal vent plume at the Mid-Atlantic Ridge to 3 (previously 2)
| f | 1 | { | f | 1 | { |
| 2 | "author": null, | 2 | "author": null, | ||
| 3 | "author_email": null, | 3 | "author_email": null, | ||
| 4 | "code": "7b.b.s", | 4 | "code": "7b.b.s", | ||
| 5 | "contributor": "NIOZ Royal Netherlands Institute for Sea Research", | 5 | "contributor": "NIOZ Royal Netherlands Institute for Sea Research", | ||
| 6 | "creator_user_id": "949caa75-d2e8-4e3a-98ad-f2ef85832c20", | 6 | "creator_user_id": "949caa75-d2e8-4e3a-98ad-f2ef85832c20", | ||
| 7 | "creators": | 7 | "creators": | ||
| 8 | rstname\":\"Sabine\",\"lastname\":\"Haalboom\",\"affiliation\":\"Royal | 8 | rstname\":\"Sabine\",\"lastname\":\"Haalboom\",\"affiliation\":\"Royal | ||
| 9 | Netherlands Institute for Sea | 9 | Netherlands Institute for Sea | ||
| 10 | correspondingauthor\":true},{\"firstname\":\"Henko\",\"lastname\":\"de | 10 | correspondingauthor\":true},{\"firstname\":\"Henko\",\"lastname\":\"de | ||
| 11 | Stigter\",\"affiliation\":\"Royal Netherlands Institute for Sea | 11 | Stigter\",\"affiliation\":\"Royal Netherlands Institute for Sea | ||
| 12 | :\"\",\"contactemailaddress\":\"\",\"iscorrespondingauthor\":false}]", | 12 | :\"\",\"contactemailaddress\":\"\",\"iscorrespondingauthor\":false}]", | ||
| 13 | "dataset_persistent_id": "DOI:10.33591/nioz/7b.b.s", | 13 | "dataset_persistent_id": "DOI:10.33591/nioz/7b.b.s", | ||
| 14 | "dates": | 14 | "dates": | ||
| 15 | -04-23T22:00:00.000Z\",\"type\":\"collected\",\"information\":\"\"}]", | 15 | -04-23T22:00:00.000Z\",\"type\":\"collected\",\"information\":\"\"}]", | ||
| 16 | "deposit_date": "2019-11-26", | 16 | "deposit_date": "2019-11-26", | ||
| 17 | "depositor": "Sabine Haalboom", | 17 | "depositor": "Sabine Haalboom", | ||
| 18 | "distribution_date": "2019-11-26", | 18 | "distribution_date": "2019-11-26", | ||
| 19 | "distributor": "Research Data Management(NIOZ Royal Netherlands | 19 | "distributor": "Research Data Management(NIOZ Royal Netherlands | ||
| 20 | Institute for Sea Research)", | 20 | Institute for Sea Research)", | ||
| 21 | "doi_date_published": "2019-11-26", | 21 | "doi_date_published": "2019-11-26", | ||
| 22 | "funding_references": | 22 | "funding_references": | ||
| 23 | [{\"name\":\"NWO\",\"awardnumber\":\"13273\",\"awardtitle\":\"TREASURE | 23 | [{\"name\":\"NWO\",\"awardnumber\":\"13273\",\"awardtitle\":\"TREASURE | ||
| 24 | (Towards Responsible ExtrAction of SUbmarine REsources\"}]", | 24 | (Towards Responsible ExtrAction of SUbmarine REsources\"}]", | ||
| 25 | "geographic_coverage": "[{\"place\":\"Rainbow hydrothermal vent | 25 | "geographic_coverage": "[{\"place\":\"Rainbow hydrothermal vent | ||
| 26 | .7,\"longitude_1\":36.4,\"latitude_2\":-34.05,\"longitude_2\":36.1}]", | 26 | .7,\"longitude_1\":36.4,\"latitude_2\":-34.05,\"longitude_2\":36.1}]", | ||
| 27 | "groups": [], | 27 | "groups": [], | ||
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| 33 | "metadata_created": "2024-10-22T09:40:41.854089", | 33 | "metadata_created": "2024-10-22T09:40:41.854089", | ||
| n | 34 | "metadata_modified": "2024-10-22T09:40:44.164620", | n | 34 | "metadata_modified": "2024-10-22T09:40:44.878702", |
| 35 | "name": "7bbs", | 35 | "name": "7bbs", | ||
| 36 | "notes": "Hydrothermal vent fields found at mid-ocean ridges emit | 36 | "notes": "Hydrothermal vent fields found at mid-ocean ridges emit | ||
| 37 | hydrothermal fluids which disperse as neutrally buoyant plumes. From | 37 | hydrothermal fluids which disperse as neutrally buoyant plumes. From | ||
| 38 | these fluids seafloor massive sulfides (SMS) deposits are formed which | 38 | these fluids seafloor massive sulfides (SMS) deposits are formed which | ||
| 39 | are being explored as possible new mining sites for (trace) metals and | 39 | are being explored as possible new mining sites for (trace) metals and | ||
| 40 | rare earth elements (REE). It has been suggested that during mining | 40 | rare earth elements (REE). It has been suggested that during mining | ||
| 41 | activities large amounts of suspended matter will appear in the water | 41 | activities large amounts of suspended matter will appear in the water | ||
| 42 | column due to excavation processes, and due to discharge of mining | 42 | column due to excavation processes, and due to discharge of mining | ||
| 43 | waste from the surface vessel. Understanding how hydrothermal plumes | 43 | waste from the surface vessel. Understanding how hydrothermal plumes | ||
| 44 | can be characterised by means of geochemistry and microbiology as they | 44 | can be characterised by means of geochemistry and microbiology as they | ||
| 45 | spread away from their source and how they affect their surrounding | 45 | spread away from their source and how they affect their surrounding | ||
| 46 | environment may help in characterising the behaviour of the dilute | 46 | environment may help in characterising the behaviour of the dilute | ||
| 47 | distal part of chemically enriched mining plumes.\nThis study on the | 47 | distal part of chemically enriched mining plumes.\nThis study on the | ||
| 48 | extensive Rainbow hydrothermal plume, observed up to 25 km downstream | 48 | extensive Rainbow hydrothermal plume, observed up to 25 km downstream | ||
| 49 | from the vent site, enabled us to investigate how microbial | 49 | from the vent site, enabled us to investigate how microbial | ||
| 50 | communities and (trace) metal composition change in a natural plume | 50 | communities and (trace) metal composition change in a natural plume | ||
| 51 | with distance. The (trace) metal and REE content of suspended | 51 | with distance. The (trace) metal and REE content of suspended | ||
| 52 | particulate matter (SPM) was determined using HR-ICP mass spectrometry | 52 | particulate matter (SPM) was determined using HR-ICP mass spectrometry | ||
| 53 | and the microbial communities of the neutrally buoyant plume, above | 53 | and the microbial communities of the neutrally buoyant plume, above | ||
| 54 | plume-, below plume-, and near-bottom water and sediment were | 54 | plume-, below plume-, and near-bottom water and sediment were | ||
| 55 | characterised by using 16S rRNA amplicon sequencing methods. Both | 55 | characterised by using 16S rRNA amplicon sequencing methods. Both | ||
| 56 | vertically in the water column and horizontally along the neutrally | 56 | vertically in the water column and horizontally along the neutrally | ||
| 57 | buoyant plume, geochemical and biological changes were evident as the | 57 | buoyant plume, geochemical and biological changes were evident as the | ||
| 58 | neutrally buoyant plume stood out by its enrichments in (trace) metals | 58 | neutrally buoyant plume stood out by its enrichments in (trace) metals | ||
| 59 | and REEs as e.g. Fe, Cu, V, Mn and REE were enriched by factors of up | 59 | and REEs as e.g. Fe, Cu, V, Mn and REE were enriched by factors of up | ||
| 60 | to ~80, ~90, ~52, ~2.5 and ~40 respectively, compared to above plume | 60 | to ~80, ~90, ~52, ~2.5 and ~40 respectively, compared to above plume | ||
| 61 | water samples taken at 1000 m water depth. The concentrations of these | 61 | water samples taken at 1000 m water depth. The concentrations of these | ||
| 62 | elements changed as the plume aged shown by the decrease of element/Fe | 62 | elements changed as the plume aged shown by the decrease of element/Fe | ||
| 63 | molar ratios of chalcophile elements (Cu, Co, Zn), indicative of rapid | 63 | molar ratios of chalcophile elements (Cu, Co, Zn), indicative of rapid | ||
| 64 | removal from the hydrothermal plume or removal from the solid phase. | 64 | removal from the hydrothermal plume or removal from the solid phase. | ||
| 65 | Conversely, increasing REE/Fe molar ratios imply uptake of REE from | 65 | Conversely, increasing REE/Fe molar ratios imply uptake of REE from | ||
| 66 | the ambient seawater onto Fe-oxyhydroxides. This was also reflected in | 66 | the ambient seawater onto Fe-oxyhydroxides. This was also reflected in | ||
| 67 | the background pelagic system as Epsilonproteobacteria started to | 67 | the background pelagic system as Epsilonproteobacteria started to | ||
| 68 | dominate and univariate microbial biodiversity declined with distance | 68 | dominate and univariate microbial biodiversity declined with distance | ||
| 69 | away from the Rainbow hydrothermal vent field. The Rainbow | 69 | away from the Rainbow hydrothermal vent field. The Rainbow | ||
| 70 | hydrothermal plume provides a geochemically enriched natural | 70 | hydrothermal plume provides a geochemically enriched natural | ||
| 71 | environment, which is a heterogeneous, dynamic habitat that is | 71 | environment, which is a heterogeneous, dynamic habitat that is | ||
| 72 | conducive to ecological changes in a short time span. This study of a | 72 | conducive to ecological changes in a short time span. This study of a | ||
| 73 | hydrothermal plume provides a baseline study to characterize the | 73 | hydrothermal plume provides a baseline study to characterize the | ||
| 74 | natural plume before the interference of deep-sea mining.", | 74 | natural plume before the interference of deep-sea mining.", | ||
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| 192 | "subject": "Earth and Environmental Sciences", | 192 | "subject": "Earth and Environmental Sciences", | ||
| 193 | "tags": [ | 193 | "tags": [ | ||
| 194 | { | 194 | { | ||
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| 202 | "title": "Patterns of (trace) metals and microorganisms in the | 202 | "title": "Patterns of (trace) metals and microorganisms in the | ||
| 203 | Rainbow hydrothermal vent plume at the Mid-Atlantic Ridge", | 203 | Rainbow hydrothermal vent plume at the Mid-Atlantic Ridge", | ||
| 204 | "type": "dataset", | 204 | "type": "dataset", | ||
| 205 | "url": "https://dataportal.nioz.nl/doi/10.33591/nioz/7b.b.s", | 205 | "url": "https://dataportal.nioz.nl/doi/10.33591/nioz/7b.b.s", | ||
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