Ericson, D; Morgenstein, M; Grinnell, R (1956): Annotated record of the detailed examination of Mn deposits from VEMA 10 Expedition stations [dataset]. PANGAEA, https://doi.org/10.1594/PANGAEA.861920, Supplement to: Ericson, D et al. (1956): Vema Cruise 10 - Preliminary Megascopic Descriptions of Split Cores. Lamont Geological Observatory, Columbia University, New York, unpublished, 145 pp
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Published: 1956 (exact date unknown) • DOI registered: 2016-07-21
Abstract:
The cores and dredges described in this report were taken during the VEMA 10 Expedition from June until September 1956 by the Lamont Geological Observatory, Columbia University from the R/V Vema. A total of 95 cores were recovered and are available at Lamont-Doherty Earth Observatory for sampling and study.
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
Project(s):
Coverage:
Median Latitude: 34.433400 * Median Longitude: -4.985100 * South-bound Latitude: 22.967000 * West-bound Longitude: -68.050000 * North-bound Latitude: 41.533000 * East-bound Longitude: 27.067000
Date/Time Start: 1956-06-30T00:00:00 * Date/Time End: 1956-09-26T00:00:00
Minimum DEPTH, sediment/rock: 0.150 m * Maximum DEPTH, sediment/rock: 9.270 m
Event(s):
V10-1 * Latitude: 35.683000 * Longitude: -3.983000 * Date/Time: 1956-06-30T00:00:00 * Elevation: -1412.0 m * Recovery: 8.3 m * Campaign: V10 * Basis: Vema * Method/Device: Piston corer (PC)
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1989 NOAA-NCEI compiled the NOAA-MMS Marine Minerals Geochemical Database from journal articles, technical reports and unpublished sources from other institutions.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):
| # | Name | Short Name | Unit | Principal Investigator | Method/Device | Comment |
|---|---|---|---|---|---|---|
| 1 | Event label | Event | Ericson, D | |||
| 2 | Date/Time of event | Date/Time | Ericson, D | |||
| 3 | Latitude of event | Latitude | Ericson, D | |||
| 4 | Longitude of event | Longitude | Ericson, D | |||
| 5 | Elevation of event | Elevation | m | Ericson, D | ||
| 6 | Sample ID | Sample ID | Ericson, D | |||
| 7 | DEPTH, sediment/rock | Depth sed | m | Ericson, D | Geocode | |
| 8 | Depth, top/min | Depth top | m | Ericson, D | ||
| 9 | Depth, bottom/max | Depth bot | m | Ericson, D | ||
| 10 | Position | Position | Ericson, D | |||
| 11 | Deposit type | Deposit type | Ericson, D | |||
| 12 | Quantity of deposit | Quantity | Ericson, D | |||
| 13 | Size | Size | Ericson, D | |||
| 14 | Substrate type | Substrate | Ericson, D | |||
| 15 | Sediment type | Sediment | Ericson, D | |||
| 16 | Comment | Comment | Ericson, D | |||
| 17 | Description | Description | Ericson, D |
License:
Creative Commons Attribution 3.0 Unported (CC-BY-3.0)
Size:
254 data points
Data
| 1 Event | 2 Date/Time | 3 Latitude | 4 Longitude | 5 Elevation [m] | 6 Sample ID | 7 Depth sed [m] | 8 Depth top [m] | 9 Depth bot [m] | 10 Position | 11 Deposit type | 12 Quantity | 13 Size | 14 Substrate | 15 Sediment | 16 Comment | 17 Description |
|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|
| V10-1 | 1956-06-30 | 35.6830 | -3.9830 | -1412 | V10-1-1 | 0.700 | 0.70 | 0.70 | In sediment | Mn rich layer | 1 | Clay | Light, faintly brownish-gray, smooth clay with a little black speckling | At 70 cm. appears to be manganese oxide on fracture surface. | ||
| V10-6 | 1956-07-04 | 41.5330 | 9.7670 | -844 | V10-6-1 | 0.305 | 0.27 | 0.34 | In sediment | Mn fragment | Several | Clay | Clay, pale yellowish-orange (10YR8/1), compact, calcareous, foraminiferal, slightly sandy and silty | Dark specks of manganese oxide concentrated from 27-34 cm. | ||
| V10-11 | 1956-07-08 | 41.0500 | 12.7000 | -198 | V10-11-1 | 0.850 | 0.00 | 1.70 | In sediment | Mn micronodule | Several | Sand | Foraminiferal sand, yellowish-gray (5Y7/2), graded and moderately sorted. The carbonate content is approximately 70-75% | The mineral content is approximately 10%, consisting mainly of manganese micronodules and small fragments associated with biotite. | ||
| V10-19 | 1956-07-13 | 39.5170 | 14.8170 | -154 | V10-19-1 | 0.260 | 0.20 | 0.32 | In sediment | Mn rich layer | 1 | Clay | Clay, white (N9) | A layer of light gray (N7) manganese rich clay at 20-32 cm | ||
| V10-20 | 1956-07-13 | 39.5000 | 14.8330 | -263 | V10-20-1 | 0.150 | 0.00 | 0.30 | In sediment | Mn micronodule | Several | Clay | Clay, yellowish-gray (5Y8/1), dry and intact. Carbonate content about 20%. | The sand fraction is composed of subangular quartz, manganese micronodules. | ||
| V10-20 | 1956-07-13 | 39.5000 | 14.8330 | -263 | V10-20-2 | 0.775 | 0.30 | 1.25 | In sediment | Mn micronodule | Few | Clay | Lutaceous coquina, yellowish-gray (5Y8/1) with dusky yellow (5Y6/4) clay | Carbonate fraction about 85% with coral fragments. There are scattered manganese nodules. | ||
| V10-21 | 1956-07-13 | 39.3170 | 14.4170 | -1309 | V10-21-1 | 1.895 | 1.79 | 2.00 | In sediment | Mn rich layer | 1 | Clay | Clay, yellowish-gray (5Y8/1), dry and compact | A high concentration of manganese occurs from 179-200 cm. | ||
| V10-32 | 1956-07-24 | 38.1000 | 22.8830 | -794 | V10-32-1 | 0.600 | 0.00 | 1.20 | In sediment | Mn micronodule | Several | Clay | Calcareous clay, yellowish-gray (5Y8/L), consists almost entirely of carbonate | More than 62 micron fraction comprises approximately 5% of sediment and consists of approximately 50% carbonate fragments. Manganese micronodules present. | ||
| V10-42 | 1956-07-31 | 37.6670 | 23.7670 | -225 | V10-42-1 | 3.285 | 0.40 | 6.17 | In sediment | Mn fragment | Many | Clay | Silty foraminiferal clay, yellowish-gray (5Y8/1). The carbonate content is about 60% | Specks and patches of manganese abound throughout. | ||
| V10-42 | 1956-07-31 | 37.6670 | 23.7670 | -225 | V10-42-2 | 6.920 | 6.40 | 7.44 | In sediment | Mn staining | Several | Foraminifera | Clay | Foraminiferal silty clay, yellowish-gray (5Y8/1) | Manganese patches and occasional burrow mottling present. | |
| V10-50 | 1956-08-04 | 35.9500 | 27.0670 | -2547 | V10-50-1 | 0.160 | 0.12 | 0.20 | In sediment | Mn micronodule | Several | Clay | Clay, very pale orange (10YR7/2). The carbonate content is about 60-70%. | Microlaminations of silt mixed with silt size foraminifera and manganese appear at 12-20 cm. | ||
| V10-50 | 1956-08-04 | 35.9500 | 27.0670 | -2547 | V10-50-2 | 5.235 | 4.99 | 5.48 | In sediment | Mn staining | Several | Foraminifera | Sand | Volcanic deposit, yellowish-gray (5Y8/1), sorted and slightly graded | Coarse grained rhyolitic glass shards are mixed with coarse grained foraminifera tests (20%). Manganese and volcanics increase with depth. | |
| V10-65 | 1956-08-17 | 34.6170 | 23.4170 | -2695 | V10-65-1 | 2.130 | 2.11 | 2.15 | In sediment | Mn rich layer | 1 | Ash | Black layer. Very sharply defined base. Manganese oxide | This layer is largely volcanic ash, judging from washed sample. Black due to manganese oxide. | ||
| V10-72 | 1956-08-28 | 39.6170 | 11.9000 | -3480 | V10-72-1 | 4.735 | 4.67 | 4.80 | In sediment | Mn micronodule | Many | Sand | Laminated sand, yellowish-gray (5Y7/2) | Darker laminations consisting of manganese micronodules associated with clay occur at intercalations. | ||
| V10-72 | 1956-08-28 | 39.6170 | 11.9000 | -3480 | V10-72-2 | 6.300 | 6.30 | 6.30 | In sediment | Mn rich layer | 1 | Clay | Foraminiferal clay, very pale orange (10YR8/2) | Dark manganese clayly laminae occur at 630 cm. | ||
| V10-77 | 1956-08-31 | 36.5170 | 0.4330 | -2111 | V10-77-1 | 2.365 | 0.77 | 3.96 | In sediment | Mn micronodule | Many | Clay | Laminated foraminiferal clay. The overall color is very pale orange (10YR8/2). Carbonate content is about 65-70% and foraminifera content approximately 25%. | The laminae do not exceed 2 mm. in thickness and consist of medium grained clastic sand composed of rounded quartz-feldspar grains, manganese micronodules. | ||
| V10-78 | 1956-09-02 | 35.9500 | -4.2500 | -1305 | V10-78-1 | 3.600 | 0.00 | 7.20 | In sediment | Mn micronodule | Few | Clay | Clay, very light gray 0(N7), dry and compact. The carbonate content is approximately 25-30% | Occasional manganese micronodules were observed and small patches of manganese oxide are scattered throughout. | ||
| V10-80 | 1956-09-05 | 31.3830 | -11.6200 | -2550 | V10-80-1 | 0.270 | 0.00 | 0.54 | In sediment | Mn micronodule | Many | Ooze | Clayly foraminiferal ooze, pale red (10YR6/2), compact, slightly burrow mottled | Silt is make up chiefly of manganese micronodules and amounts to 10% | ||
| V10-82 | 1956-09-09 | 26.2330 | -18.0700 | -3775 | V10-82-1 | 9.270 | 9.10 | 9.44 | In sediment | Mn rich layer | 1 | Ooze | Silty foraminiferal ooze, color when dry, white (N9) to pinkish-gray (5YR8/1). Consists of approximately 50% calcareous, silty lutite, and approximately 50% tests of planktonic foraminifera | Contains extensive iron oxide staining and large black patches of manganese oxide. | ||
| V10-83 | 1956-09-10 | 25.2170 | -21.3800 | -4530 | V10-83-1 | 0.995 | 0.00 | 1.99 | In sediment | Mn micronodule | Several | Clay | Foraminiferal clay, very pale orange (10YR8/2), burrowed. The carbonate content is about 80%; foraminifera content about 35-45% | Manganese micronodules are scattered throughout | ||
| V10-83 | 1956-09-10 | 25.2170 | -21.3800 | -4530 | V10-83-2 | 3.220 | 1.99 | 4.45 | In sediment | Mn micronodule | Several | Clay | Calcareous clay, white (N9), burrowed. The carbonate content is greater than 90%; the foraminifera content does not seem to exceed 15% | Manganese micronodules and small manganese patches scattered throughout | ||
| V10-88 | 1956-09-16 | 22.9670 | -38.2000 | -4971 | V10-88-1 | 0.910 | 0.60 | 1.22 | In sediment | Mn micronodule | Few | Ooze | Calcareous foraminiferal ooze, pinkish-gray (5YR8/1), carbonate content approximately 80%. Sand fraction makes up approximately 50% of sediment and consists of planktonic foraminifera tests | Silt-size manganese oxide nodules disseminated throughout | ||
| V10-88 | 1956-09-16 | 22.9670 | -38.2000 | -4971 | V10-88-2 | 0.910 | 0.60 | 1.22 | In sediment | Mn coating | Foraminifera | Ooze | Calcareous foraminiferal ooze, pinkish-gray (5YR8/1), carbonate content approximately 80%. Sand fraction makes up approximately 50% of sediment and consists of planktonic foraminifera tests | Manganese oxide also occurs as foraminifera coatings and fillings. | ||
| V10-88 | 1956-09-16 | 22.9670 | -38.2000 | -4971 | V10-88-3 | 3.610 | 1.22 | 6.00 | Buried | Mn nodule | Many | 0.1 cm | Clay | Red clay, manganiferous clay, pale brown (5YR5/2), containing no detectable carbonate | Coarse fraction consists of silt to medium sand-size manganese oxide nodules and makes up approximately 1% of sediment. | |
| V10-95 | 1956-09-21 | 26.5170 | -51.7800 | -5376 | V10-95-1 | 5.200 | 0.00 | 10.40 | In sediment | Mn micronodule | Many | Clay | Clay, moderate brown (5YR3/4), manganiferous | Greater than 62 micron fraction makes up less than 1% of sediment and consists of manganese micronodules and rare, small grains of calcite. | ||
| V10-97 | 1956-09-23 | 29.6830 | -58.3700 | -5894 | V10-97-1 | 1.600 | 0.00 | 3.20 | In sediment | Mn micronodule | Several | Clay | Clay, moderate yellowish-brown (10YR5/4), and dark yellowish-brown (10YR4/2). Secondary oxidized clay is dark yellowish-orange (10YR6/6) | Manganese stains and micronodules scattered throughout. | ||
| V10-97 | 1956-09-23 | 29.6830 | -58.3700 | -5894 | V10-97-2 | 3.350 | 3.20 | 3.50 | In sediment | Mn micronodule | Many | Clay | Clay, grayish-orange (10YR7/4), with some mottled yellowish-brown (10YR5/4) clay. Mineral fraction is composed of about 1-2% fine grained subangular to angular quartz | There is a high concentration of manganese micronodules | ||
| V10-99 | 1956-09-26 | 31.6500 | -68.0500 | -5446 | V10-99-1 | 2.450 | 0.00 | 4.90 | In sediment | Mn micronodule | Several | Clay, dark yellowish-brown (10YR4/2), with secondary stains of dark yellowish-grange (10YR6/6) | Manganese micronodules scattered throughout. |
