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Mero, John L (1965): (Table XXX, pages 182-221) Chemical analyses of manganese nodules and crusts from the Pacific Ocean [dataset]. PANGAEA, https://doi.org/10.1594/PANGAEA.864077, In supplement to: Mero, JL (1965): The Mineral Resources of the Sea. Elsevier Oceanography Series, 1, 312 pp, https://www.sciencedirect.com/bookseries/elsevier-oceanography-series/vol/1/suppl/C

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Coverage:
Median Latitude: 0.511183 * Median Longitude: -152.094130 * South-bound Latitude: -64.183000 * West-bound Longitude: 138.683333 * North-bound Latitude: 40.483000 * East-bound Longitude: -83.116667
Date/Time Start: 1875-11-11T00:00:00 * Date/Time End: 1962-06-15T00:00:00
Minimum DEPTH, sediment/rock: 0.00 m * Maximum DEPTH, sediment/rock: 0.49 m
Event(s):
CHA-256 (256) * Latitude: 30.333333 * Longitude: -154.933333 * Elevation: -5395.0 m * Location: Eastern Central Pacific Ocean * Campaign: Challenger1872 * Basis: H.M.S. Challenger (1872) * Method/Device: Dredge (DRG)
CHA-297 * Latitude: -37.483333 * Longitude: -83.116667 * Date/Time: 1875-11-11T00:00:00 * Elevation: -2915.0 m * Campaign: Challenger1872 * Basis: H.M.S. Challenger (1872) * Method/Device: Grab (GRAB)
CHUB-X (CHUB02BD-010G) * Latitude: 11.633000 * Longitude: -103.800000 * Date/Time: 1954-12-08T00:00:00 * Elevation: -3438.0 m * Recovery: 52 cm * Location: Pacific Ocean * Campaign: CHUBASCO (CHUB01BD) * Basis: Spencer F. Baird * Method/Device: Core (CORE) * Comment: PI: R. L. Fisher
Comment:
The H2O is determined by air-drying the nodule samples at 200°C for two hours. The loss on ignition (LOI) is then measured after a one hour heating at 1100°C. In reducing the analyses to a detrital mineral free basis, SiO2, Al2O3, H2O, and CaCO3 in amounts greater than 5%, were considered as detrital minerals.
From 1983 until 1989 NOAA-NCEI compiled the NOAA-MMS Marine Minerals Geochemical Database from journal articles, technical reports and unpublished sources from other institutions. At the time it was the most extended data compilation on ferromanganese deposits world wide. Initially published in a proprietary format incompatible with present day standards it was jointly decided by AWI and NOAA to transcribe this legacy data into PANGAEA. This transfer is augmented by a careful checking of the original sources when available and the encoding of ancillary information (sample description, method of analysis...) not present in the NOAA-MMS database.
Parameter(s):
#NameShort NameUnitPrincipal InvestigatorMethod/DeviceComment
1Event labelEventMero, John L
2Date/Time of eventDate/TimeMero, John L
3Latitude of eventLatitudeMero, John L
4Longitude of eventLongitudeMero, John L
5Elevation of eventElevationmMero, John L
6Sample IDSample IDMero, John L
7Sample code/labelSample labelMero, John L
8DEPTH, sediment/rockDepth sedmMero, John LGeocode
9Aluminium oxideAl2O3%Mero, John LX-ray fluorescence (XRF)
10Silicon dioxideSiO2%Mero, John LX-ray fluorescence (XRF)
11PotassiumK%Mero, John LX-ray fluorescence (XRF)
12CalciumCa%Mero, John LX-ray fluorescence (XRF)
13TitaniumTi%Mero, John LX-ray fluorescence (XRF)
14ManganeseMn%Mero, John LX-ray fluorescence (XRF)
15IronFe%Mero, John LX-ray fluorescence (XRF)
16CobaltCo%Mero, John LX-ray fluorescence (XRF)
17NickelNi%Mero, John LX-ray fluorescence (XRF)
18CopperCu%Mero, John LX-ray fluorescence (XRF)
19ZincZn%Mero, John LX-ray fluorescence (XRF)
20StrontiumSr%Mero, John LX-ray fluorescence (XRF)
21MolybdenumMo%Mero, John LX-ray fluorescence (XRF)
22BariumBa%Mero, John LX-ray fluorescence (XRF)
23LeadPb%Mero, John LX-ray fluorescence (XRF)
24Water in rockH2O%Mero, John LWet chemistry
25Loss on ignitionLOI%Mero, John L
26Deposit typeDeposit typeMero, John L
27SizeSizeMero, John L
28Specific gravitySpecific gravityMero, John L
29Sediment typeSedimentMero, John L
30DescriptionDescriptionMero, John L
31Page(s)Page(s)Mero, John L
Size:
1130 data points

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