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Szefer, Piotr; Glasby, Geoffrey P; Kunzendorf, Helmar; Görlich, E A; Latka, K; Ikuta, K; Ali, Arshad (1998): Annotated record of the detailed examination of Mn deposits from the Polish EEZ and the Gulf of Bothnia [dataset]. PANGAEA, https://doi.org/10.1594/PANGAEA.860659, In supplement to: Szefer, P et al. (1998): The distribution of rare earth and other elements and the mineralogy of the iron oxyhydroxide phase in marine ferromanganese concretions from within Slupsk Furrow in the southern Baltic. Applied Geochemistry, 13(3), 305-312, https://doi.org/10.1016/S0883-2927(97)00099-1

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Coverage:
Median Latitude: 55.266842 * Median Longitude: 17.266640 * South-bound Latitude: 55.166850 * West-bound Longitude: 16.533280 * North-bound Latitude: 55.333490 * East-bound Longitude: 18.000020
Date/Time Start: 1987-05-01T10:00:00 * Date/Time End: 1987-05-01T10:00:00
Minimum DEPTH, sediment/rock: m * Maximum DEPTH, sediment/rock: m
Event(s):
SZEF-153  * Latitude: 55.275190 * Longitude: 16.533300 * Date/Time: 1987-05-01T10:00:00 * Elevation: -70.0 m * Location: Baltic Sea * Campaign: Oceana-87 * Basis: Oceana * Method/Device: Dredge (DRG)
SZEF-155  * Latitude: 55.166850 * Longitude: 16.533280 * Date/Time: 1987-05-01T10:00:00 * Elevation: -75.0 m * Location: Baltic Sea * Campaign: Oceana-87 * Basis: Oceana * Method/Device: Dredge (DRG)
SZEF-172  * Latitude: 55.333490 * Longitude: 17.999960 * Date/Time: 1987-05-01T10:00:00 * Elevation: -78.0 m * Location: Baltic Sea * Campaign: Oceana-87 * Basis: Oceana * Method/Device: Dredge (DRG)
Comment:
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1989 NOAA-NCEI compiled the NOAA-MMS Marine Minerals Geochemical Database from journal articles, technical reports and unpublished sources from other institutions.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
Event labelEventSzefer, Piotr
Latitude of eventLatitudeSzefer, Piotr
Longitude of eventLongitudeSzefer, Piotr
Elevation of eventElevationmSzefer, Piotr
Method/Device of eventMethod/DeviceSzefer, Piotr
IdentificationIDSzefer, Piotr
DEPTH, sediment/rockDepth sedmSzefer, PiotrGeocode
PositionPositionSzefer, PiotrVisual description
Deposit typeDeposit typeSzefer, Piotr
10 Quantity of depositQuantitySzefer, Piotr
11 SizeSizeSzefer, Piotr
12 ShapeShapeSzefer, Piotr
13 Substrate typeSubstrateSzefer, Piotr
14 Sediment typeSedimentSzefer, Piotr
15 CommentCommentSzefer, Piotr
16 DescriptionDescriptionSzefer, Piotr
Size:
62 data points

Data

Download dataset as tab-delimited text — use the following character encoding:


Event

Latitude

Longitude

Elevation [m]

Method/Device

ID

Depth sed [m]

Position

Deposit type
10 
Quantity
11 
Size
12 
Shape
13 
Substrate
14 
Sediment
15 
Comment
16 
Description
SZEF-B2 55.291818.0000-92DredgeSZEF-B2-10SurfaceMn nodule401.5x1.5x0.5-3.0x3.0x0.2 cmDiscoidalCore; weathered materialMainly thin discoidal or fragments of discoidal concretions. Some of the discoidal concretions are flat but many have a convex upper surface and concave lower surface. A few have an erratic nucleus usually rather weathered.
SZEF-B255.291818.0000-92DredgeSZEF-B2-20SurfaceMn crust4Up to 4.0x3.0x1.5 cmFragments of ferromanganese crust
SZEF-B255.291818.0000-92DredgeSZEF-B2-30SurfaceMn coating11860.1 cm thickMussel shellCore; glacial erraticMudGrey green sandy mud about 5.0 cm thick overlying dark grey silty clay.Ferromanganese coatings also occurred on the shells of living specimens of the mussel Astarte borealis
SZEF-153 55.275216.5333-70DredgeSZEF-153-10SurfaceMn nodule92.0x2.0x0.5-7.5x5.0x1.2 cmDiscoidal with rimCore; glacial erraticMudMedium brown muddy gravelly sand about 5.0 cm thick overlying dark grey silty clay.Discoidal concretions mostly formed around a glacial erratic nucleus and had developed a slight rim.
SZEF-15355.275216.5333-70DredgeSZEF-153-20SurfaceMn crust21.0-1.5 cm thickMudMedium brown muddy gravelly sand about 5.0 cm thick overlying dark grey silty clay.Fragments of flat ferromanganese crusts
SZEF-155 55.166816.5333-75DredgeSZEF-155-10SurfaceMn nodule62.0x2.0x0.9-7.0x5.0x1.2 cmDiscoidal with rimCore; glacial erraticSandMedium brown muddy gravelly sand about 5.0 cm thick overlying dark grey silty clay.Irregular discoidal concretions with a large fragment of glacial erratic as core (rather large in terms of the total size of the concretions) and had developed a rim.
SZEF-172 55.333518.0000-78DredgeSZEF-172-10SurfaceMn nodule302.3x2.0x1.2-12.0x5.5x1.5Discoidal with rimCore; glacial erraticMudGrey green sandy mud about 5.0 cm thick overlying dark grey silty clay.Irregular discoidal concretions formed on glacial erratic as core (rather large in terms of the total size of the concretions) and with a rim around the biggest cores.