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  "code": "7b.b.s",
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  "code": "7b.b.s",
            
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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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  "creators": 
            
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rstname\":\"Sabine\",\"lastname\":\"Haalboom\",\"affiliation\":\"Royal 
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rstname\":\"Sabine\",\"lastname\":\"Haalboom\",\"affiliation\":\"Royal 
            
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Netherlands Institute for Sea 
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Netherlands Institute for Sea 
            
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correspondingauthor\":true},{\"firstname\":\"Henko\",\"lastname\":\"de 
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correspondingauthor\":true},{\"firstname\":\"Henko\",\"lastname\":\"de 
            
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Stigter\",\"affiliation\":\"Royal Netherlands Institute for Sea 
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Stigter\",\"affiliation\":\"Royal Netherlands Institute for Sea 
            
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:\"\",\"contactemailaddress\":\"\",\"iscorrespondingauthor\":false}]",
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  "dataset_persistent_id": "DOI:10.25850/nioz/7b.b.s",
            
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  "dates": 
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  "dates": 
            
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-04-23T22:00:00.000Z\",\"type\":\"collected\",\"information\":\"\"}]",
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-04-23T22:00:00.000Z\",\"type\":\"collected\",\"information\":\"\"}]",
            
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  "deposit_date": "2019-11-26",
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  "deposit_date": "2019-11-26",
            
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  "depositor": "Sabine Haalboom",
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  "depositor": "Sabine Haalboom",
            
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  "distribution_date": "2019-11-26",
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  "distribution_date": "2019-11-26",
            
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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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  "funding_references": 
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  "funding_references": 
            
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[{\"name\":\"NWO\",\"awardnumber\":\"13273\",\"awardtitle\":\"TREASURE 
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[{\"name\":\"NWO\",\"awardnumber\":\"13273\",\"awardtitle\":\"TREASURE 
            
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(Towards Responsible ExtrAction of SUbmarine REsources\"}]",
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(Towards Responsible ExtrAction of SUbmarine REsources\"}]",
            
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  "geographic_coverage": "[{\"place\":\"Rainbow hydrothermal vent 
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  "geographic_coverage": "[{\"place\":\"Rainbow hydrothermal vent 
            
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.7,\"longitude_1\":36.4,\"latitude_2\":-34.05,\"longitude_2\":36.1}]",
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  "name": "7bbs",
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  "name": "7bbs",
            
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  "notes": "Hydrothermal vent fields found at mid-ocean ridges emit 
35
  "notes": "Hydrothermal vent fields found at mid-ocean ridges emit 
            
36
hydrothermal fluids which disperse as neutrally buoyant plumes. From 
36
hydrothermal fluids which disperse as neutrally buoyant plumes. From 
            
37
these fluids seafloor massive sulfides (SMS) deposits are formed which 
37
these fluids seafloor massive sulfides (SMS) deposits are formed which 
            
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are being explored as possible new mining sites for (trace) metals and 
38
are being explored as possible new mining sites for (trace) metals and 
            
39
rare earth elements (REE). It has been suggested that during mining 
39
rare earth elements (REE). It has been suggested that during mining 
            
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activities large amounts of suspended matter will appear in the water 
40
activities large amounts of suspended matter will appear in the water 
            
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column due to excavation processes, and due to discharge of mining 
41
column due to excavation processes, and due to discharge of mining 
            
42
waste from the surface vessel.  Understanding how hydrothermal plumes 
42
waste from the surface vessel.  Understanding how hydrothermal plumes 
            
43
can be characterised by means of geochemistry and microbiology as they 
43
can be characterised by means of geochemistry and microbiology as they 
            
44
spread away from their source and how they affect their surrounding 
44
spread away from their source and how they affect their surrounding 
            
45
environment may help in characterising the behaviour of the dilute 
45
environment may help in characterising the behaviour of the dilute 
            
46
distal part of chemically enriched mining plumes.\nThis study on the 
46
distal part of chemically enriched mining plumes.\nThis study on the 
            
47
extensive Rainbow hydrothermal plume, observed up to 25 km downstream 
47
extensive Rainbow hydrothermal plume, observed up to 25 km downstream 
            
48
from the vent site, enabled us to investigate how microbial 
48
from the vent site, enabled us to investigate how microbial 
            
49
communities and (trace) metal composition change in a natural plume 
49
communities and (trace) metal composition change in a natural plume 
            
50
with distance. The (trace) metal and REE content of suspended 
50
with distance. The (trace) metal and REE content of suspended 
            
51
particulate matter (SPM) was determined using HR-ICP mass spectrometry 
51
particulate matter (SPM) was determined using HR-ICP mass spectrometry 
            
52
and the microbial communities of the neutrally buoyant plume, above 
52
and the microbial communities of the neutrally buoyant plume, above 
            
53
plume-, below plume-, and near-bottom water and sediment were 
53
plume-, below plume-, and near-bottom water and sediment were 
            
54
characterised by using 16S rRNA amplicon sequencing methods. Both 
54
characterised by using 16S rRNA amplicon sequencing methods. Both 
            
55
vertically in the water column and horizontally along the neutrally 
55
vertically in the water column and horizontally along the neutrally 
            
56
buoyant plume, geochemical and biological changes were evident as the 
56
buoyant plume, geochemical and biological changes were evident as the 
            
57
neutrally buoyant plume stood out by its enrichments in (trace) metals 
57
neutrally buoyant plume stood out by its enrichments in (trace) metals 
            
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and REEs as e.g. Fe, Cu, V, Mn and REE were enriched by factors of up 
58
and REEs as e.g. Fe, Cu, V, Mn and REE were enriched by factors of up 
            
59
to ~80, ~90, ~52, ~2.5 and ~40 respectively, compared to above plume 
59
to ~80, ~90, ~52, ~2.5 and ~40 respectively, compared to above plume 
            
60
water samples taken at 1000 m water depth. The concentrations of these 
60
water samples taken at 1000 m water depth. The concentrations of these 
            
61
elements changed as the plume aged shown by the decrease of element/Fe 
61
elements changed as the plume aged shown by the decrease of element/Fe 
            
62
molar ratios of chalcophile elements (Cu, Co, Zn), indicative of rapid 
62
molar ratios of chalcophile elements (Cu, Co, Zn), indicative of rapid 
            
63
removal from the hydrothermal plume or removal from the solid phase. 
63
removal from the hydrothermal plume or removal from the solid phase. 
            
64
Conversely, increasing REE/Fe molar ratios imply uptake of REE from 
64
Conversely, increasing REE/Fe molar ratios imply uptake of REE from 
            
65
the ambient seawater onto Fe-oxyhydroxides. This was also reflected in 
65
the ambient seawater onto Fe-oxyhydroxides. This was also reflected in 
            
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the background pelagic system as Epsilonproteobacteria started to 
66
the background pelagic system as Epsilonproteobacteria started to 
            
67
dominate and univariate microbial biodiversity declined with distance 
67
dominate and univariate microbial biodiversity declined with distance 
            
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away from the Rainbow hydrothermal vent field. The Rainbow 
68
away from the Rainbow hydrothermal vent field. The Rainbow 
            
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hydrothermal plume provides a geochemically enriched natural 
69
hydrothermal plume provides a geochemically enriched natural 
            
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environment, which is a heterogeneous, dynamic habitat that is 
70
environment, which is a heterogeneous, dynamic habitat that is 
            
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conducive to ecological changes in a short time span. This study of a 
71
conducive to ecological changes in a short time span. This study of a 
            
72
hydrothermal plume provides a baseline study to characterize the 
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hydrothermal plume provides a baseline study to characterize the 
            
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natural plume before the interference of deep-sea mining.",
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