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Nybelin, Orvar (1951): Annotated record of the detailed examination of Mn deposits from the Swedish Deep Sea Expedition [dataset]. PANGAEA, https://doi.org/10.1594/PANGAEA.858485, Supplement to: Nybelin, O (1951): Introduction and Station List. In: Pettersson, H. (Ed.), Jerlov, N. and Kullenberg, B. Reports of the Swedish Deep Sea Expedition, Volume II. Swedish Natural Science Research Council Stockholm 23 - Sweden, 1-28

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Abstract:
The cores and dredges described in this report were taken during the Swedish Deep Sea Expedition from July 1947 until October 1948 aboard the S/S Albatross (Boström). A total of 370 cores and trawls during this World circumnavigation.
Related to:
Arrhenius, Gustaf (1951): Sediment cores from the East Pacific. In: Pettersson, H. (Ed.), Jerlov, N. and Kullenberg, B. Reports of the Swedish Deep Sea Expedition, Volume V. Swedish Natural Science Research Council Stockholm 23 - Sweden, 93-186
Olausson, Eric (1951): Description of the Sediment Cores from the Central and Western Pacific with Adjacent Indonesian Region. In: Pettersson, H. (Ed.), Jerlov, N. and Kullenberg, B. Reports of the Swedish Deep Sea Expedition, Volume VI. Swedish Natural Science Research Council Stockholm 23 - Sweden, 161-195
Source:
Grant, John Bruce; Moore, Carla J; Alameddin, George; Chen, Kuiying; Barton, Mark (1992): The NOAA and MMS Marine Minerals Geochemical Database. National Geophysical Data Center, NOAA, https://doi.org/10.7289/V52Z13FT
Further details:
Warnken, Robin R; Virden, William T; Moore, Carla J (1992): The NOAA and MMS Marine Minerals Bibliography. National Geophysical Data Center, NOAA, https://doi.org/10.7289/V53X84KN
Coverage:
Median Latitude: 8.692762 * Median Longitude: -129.071012 * South-bound Latitude: -13.416700 * West-bound Longitude: -178.950000 * North-bound Latitude: 28.416700 * East-bound Longitude: -60.816700
Date/Time Start: 1947-09-16T14:18:00 * Date/Time End: 1948-08-24T09:15:00
Minimum DEPTH, sediment/rock: 0.00 m * Maximum DEPTH, sediment/rock: 6.91 m
Event(s):
SDSE_065 (core_43)  * Latitude: 6.350000 * Longitude: -103.700000 * Date/Time Start: 1947-09-16T14:18:00 * Date/Time End: 1947-09-16T18:18:00 * Elevation: -3470.0 m * Recovery: 930 cm * Location: North Pacific Ocean * Campaign: SwedishDeepSeaExpedition (NODC-0418) * Basis: Albatross IV (1963) * Method/Device: Core (CORE)
SDSE_066 (core_44)  * Latitude: 6.916700 * Longitude: -104.766700 * Date/Time Start: 1947-09-17T09:53:00 * Date/Time End: 1947-09-17T12:44:00 * Elevation: -3565.0 m * Recovery: 967 cm * Location: North Pacific Ocean * Campaign: SwedishDeepSeaExpedition (NODC-0418) * Basis: Albatross IV (1963) * Method/Device: Core (CORE)
SDSE_068 (core_45)  * Latitude: 7.666700 * Longitude: -106.350000 * Date/Time Start: 1947-09-18T08:50:00 * Date/Time End: 1947-09-18T14:50:00 * Elevation: -3725.0 m * Recovery: 975 cm * Location: North Pacific Ocean * Campaign: SwedishDeepSeaExpedition (NODC-0418) * Basis: Albatross IV (1963) * Method/Device: Core (CORE)
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 labelEventNybelin, Orvar
Date/Time of eventDate/TimeNybelin, Orvar
Latitude of eventLatitudeNybelin, Orvar
Longitude of eventLongitudeNybelin, Orvar
Elevation of eventElevationmNybelin, Orvar
Method/Device of eventMethod/DeviceNybelin, Orvar
Sample IDSample IDNybelin, Orvar
DEPTH, sediment/rockDepth sedmNybelin, OrvarGeocode
Depth, top/minDepth topmNybelin, Orvar
10 Depth, bottom/maxDepth botmNybelin, Orvar
11 PositionPositionNybelin, OrvarVisual description
12 Deposit typeDeposit typeNybelin, Orvar
13 Quantity of depositQuantityNybelin, Orvar
14 SizeSizeNybelin, Orvar
15 Substrate typeSubstrateNybelin, Orvar
16 Sediment typeSedimentNybelin, Orvar
17 CommentCommentNybelin, Orvar
18 DescriptionDescriptionNybelin, Orvar
Size:
276 data points

Data

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


Event

Date/Time

Latitude

Longitude

Elevation [m]

Method/Device

Sample ID

Depth sed [m]

Depth top [m]
10 
Depth bot [m]
11 
Position
12 
Deposit type
13 
Quantity
14 
Size
15 
Substrate
16 
Sediment
17 
Comment
18 
Description
SDSE_073 1947-09-2211.4167-113.8000-4090CoreSDSE_073-SW48-10.000.000.00SurfaceMn nodule11.0 cmClayish oozeGreyish yellow to dark brown siliceous clay overlying a rapidly deposited basal bedA large conchoidal manganese nodule was found growing at the surface. Analysed in Mero, 1965
SDSE_0731947-09-2211.4167-113.8000-4090CoreSDSE_073-SW48-22.692.692.69In sedimentMn nodule10.03 cmClayish oozeGreyish yellow to dark brown siliceous clay overlying a rapidly deposited basal bedAnother nodule, a few millimeters in size, was found at 269 cm. There is no change in the colour of the sediment around the nodules.
SDSE_0731947-09-2211.4167-113.8000-4090CoreSDSE_073-SW48-36.476.006.95In sedimentMn micronoduleManyClayish oozeGreyish yellow to dark brown siliceous clay overlying a rapidly deposited basal bedOn the whole the deposit is very rich in manganese micronodules. Exceptionally high concentrations (> 1 000 micronodules/g) are found in the deposit overlying the basal beds rich in weathering glass.
SDSE_065 1947-09-166.3500-103.7000-3470CoreSDSE_065-13.323.083.56In sedimentMn micronoduleManyOozeGlobigerina and globorotalia chalk oozesSmall manganese nodules ( 0,1 cm) occur frequently
SDSE_066 1947-09-176.9167-104.7667-3565CoreSDSE_066-14.830.009.67In sedimentMn micronoduleFewOozeGlobigerina and globorotalia chalk ooze alterning with globigerina marl oozeVolcanic glass, palagonite and manganese micronodules occur sporadically.
SDSE_068 1947-09-187.6667-106.3500-3725CoreSDSE_068-10.250.000.50In sedimentMn micronoduleManyClayish oozeGlobigerina chalk ooze, and globigerina and globorotalia marl ooze alternating with clayGlass and palagonite are scarce. Manganese micronodules are comparatively frequent (max. 42/g) in the top half meter bed.
SDSE_069 1947-09-198.3667-108.0000-3800CoreSDSE_069-10.250.000.50In sedimentMn micronoduleManyClayish oozeGlobigerina chalk ooze, and globigerina and globorotalia marl ooze alternating with clayManganese micronodules are most frequent in the upper beds (max. 70/g)
SDSE_070 1947-09-209.2333-109.6500-3567CoreSDSE_070-15.504.486.53In sedimentMn micronoduleManyOozeChalk ooze with a few marl ooze layersGlass, palagonite and manganese micronodules are found in most of the sampIes; the nodules being sometimes abundant (448 cm and 653 cm).
SDSE_0701947-09-209.2333-109.6500-3567CoreSDSE_070-20.420.420.42BuriedMn nodule1SmallOozeChalk ooze with a few marl ooze layersSmall nodule was found at 42 cm
SDSE_0701947-09-209.2333-109.6500-3567CoreSDSE_070-32.112.112.11BuriedMn nodule12.0 cmCore; weathered volcanic glassOozeChalk ooze with a few marl ooze layersA big rounded nodule, 2 cm in diameter, was found suspended in the sediment at 211 cm. The nucleus consisted of a piece of weathered glass
SDSE_0701947-09-209.2333-109.6500-3567CoreSDSE_070-44.214.214.21BuriedMn nodule1SmallOozeChalk ooze with a few marl ooze layersSmall nodule was found at 421 cm
SDSE_076 1947-09-2413.3333-117.9667-4248CoreSDSE_076-10.000.000.00SurfaceMn nodule11.0 cmClayBrown, stratified clayA conchoidal manganese nodule approx. 1 cm in diameter was found at the surface of the deposit. The lower side was irregular and the upper smooth and rounded surface was protruding into the water.
SDSE_0761947-09-2413.3333-117.9667-4248CoreSDSE_076-20.120.000.25In sedimentMn micronoduleSeveralClayBrown, stratified clayManganese micronodules are most frequent in the upper part of the core.
SDSE_078 1947-09-2615.6667-123.3500-4300CoreSDSE_078-16.625.008.25In sedimentMn micronoduleManyClayLight, greyish yellow clay, partly coloured dark by manganese and iron compounds.Comparatively large quantities of manganese micronodules ( > 20/g) are found in the beds P2, P4, and P6 and their frequencies are fairly weIl correlated with the concentration of phosphorus.
SDSE_079 1947-09-2716.5833-124.8000-4230CoreSDSE_079-SW52-10.030.000.06BuriedMn crust1Hardened sediment, palagoniteClayFossil-bearing, greyish brown clay rich in glass and palagoniteThe crusts are formed by rounded nodules rich in clay, glass and palagonite and loosely or strongly cemented together.
SDSE_0791947-09-2716.5833-124.8000-4230CoreSDSE_079-SW52-20.290.270.32BuriedMn crust1Hardened sediment, palagoniteClayFossil-bearing, greyish brown clay rich in glass and palagoniteThe crusts are formed by rounded nodules rich in clay, glass and palagonite and loosely or strongly cemented together. The lower crust is more cemented
SDSE_0791947-09-2716.5833-124.8000-4230CoreSDSE_079-SW52-30.000.000.00SurfaceMn coatingSeveral0.01 cmGrain; palagoniteClayFossil-bearing, greyish brown clay rich in glass and palagoniteIn the intermediate part of the intercalated clay , an increased amount of manganese micronodules are presesnt of which a great number contain palagonite grains as a nucleus.
SDSE_081 1947-09-2915.5667-127.1833-4730CoreSDSE_081-10.450.000.90In sedimentMn micronoduleSeveralOozeChalk and marl ooze bedThe upper chalk and marl ooze bed is comparatively rich in manganese micronodules
SDSE_086 1947-10-029.8333-128.2167-4629CoreSDSE_086-10.080.070.09In sedimentMn micronoduleManyCalcareous oozeThe calcareous basal layer has a somewhat light er colour than the overlying bed.The present top of the truncated sequence is strongly encrusted by manganese micronodules, indicating a considerable time of nondeposition.
SDSE_087 1947-10-038.4167-128.8000-4607CoreSDSE_087-12.852.802.90In sedimentMn micronoduleManyMarlForaminiferal marl and calcareous clayHigh concentrations of manganese micronodules occur in the marl bed.
SDSE_102 1947-11-06-13.4167-149.5000-4625Gravity corerSDSE_102-11.660.003.31In sedimentMn micronoduleSeveralRed clayFerruginous red clayFerruginous red clay with many small crystals of phillipsite, and with manganese nodules.
SDSE_104 1947-11-08-11.2500-150.5000-4900CoreSDSE_104-11.700.003.40In sedimentMn micronoduleSeveralRed clayFerruginous red clayFerruginous red clay with many small crystals of phillipsite, and with manganese nodules.
SDSE_105-2 1947-11-10-7.6333-152.8833-5015CoreSDSE_105-2-11.320.002.65In sedimentMn micronoduleSeveralRed clayFerruginous red clayFerruginous red clay with manganese nodules, sponge spicules and fish teeth.
SDSE_114-2 1947-11-173.7500-149.7333-5155CoreSDSE_114-2-1In sedimentMn micronoduleSeveralOozeChalk ooze, rich in radiolarian tests
SDSE_125-2 1947-12-1616.3167-162.9500-5650CoreSDSE_125-2-1In sedimentMn micronoduleSeveralLargeRed clayRed clay with large manganese concretions and numerous phillipsite crystals.
SDSE_127-2 1947-12-1714.4667-164.9833-5460CoreSDSE_127-2-SW81-10.000.000.00SurfaceMn crust1Red clayRed clay with manganese concretions and phillipsite crystals. Corer tumbled, manganese crust.
SDSE_128 1947-12-1812.2667-166.8000-5080CoreSDSE_128-SW82-10.000.000.00SurfaceMn crust1HardgroundCorer not released; manganese crust.
SDSE_136-2 1947-12-242.3833-173.8333-5560CoreSDSE_136-2-10.320.320.32BuriedMn nodule1OozeRadiolarian ooze with some diatom frustulesMn nodule found by Kröll at 32 cm (Kröll, 1953)
SDSE_139-2 1947-12-27-2.8000-178.9500-5465CoreSDSE_139-2-16.916.707.12BuriedMn noduleSeveralCore; pumiceRed clayFerruginous red clayFerruginous red clay with skeletons of siliceous organisms, especially radiolaria but also some diatoms.
SDSE_373-2 1948-08-2328.4167-61.1000-5500Trawl netSDSE_373-SW270-10.000.000.00SurfaceMn noduleMany2.0-3.0 cmRed clayRed clay. Poor in calcium carbonateMasses of manganese nodules and stones as well as a number of sharks' teeth etc.. In the large bag some few concretions and pebbles and a quantity of clay.