Shipboard Scientific Party (1957): Annotated record of the detailed examination of Mn deposits from VEMA 12 Expedition stations [dataset]. PANGAEA, https://doi.org/10.1594/PANGAEA.862080, Supplement to: Lamont-Doherty Earth Observatory (1957): Vema Cruise 12 - Preliminary Megascopic Descriptions of Split Cores. Lamont Geological Observatory, Columbia University, New York, unpublished, 87 pp
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Abstract:
The cores and dredges described in this report were taken during the VEMA 12 Expedition from December 1956 until August 1957 by the Lamont Geological Observatory, Columbia University from the R/V Vema. A total of 119 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: 0.861212 * Median Longitude: -50.608091 * South-bound Latitude: -41.230000 * West-bound Longitude: -79.330000 * North-bound Latitude: 34.633000 * East-bound Longitude: 10.667000
Date/Time Start: 1956-12-16T00:00:00 * Date/Time End: 1957-08-15T00:00:00
Minimum DEPTH, sediment/rock: 0.020 m * Maximum DEPTH, sediment/rock: 8.670 m
Event(s):
V12-1 * Latitude: 34.633000 * Longitude: -66.600000 * Date/Time: 1956-12-16T00:00:00 * Elevation: -5207.0 m * Recovery: 12.25 m * Campaign: V12 * 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1989 NOAA-NCEI compiled the NOAA-MMS Marine Minerals Geochemical Database from journal articles, technical reports and unpublished sources from other institutions.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 | Lamont-Doherty Earth Observatory | |||
2 | Date/Time of event | Date/Time | Lamont-Doherty Earth Observatory | |||
3 | Latitude of event | Latitude | Lamont-Doherty Earth Observatory | |||
4 | Longitude of event | Longitude | Lamont-Doherty Earth Observatory | |||
5 | Elevation of event | Elevation | m | Lamont-Doherty Earth Observatory | ||
6 | Sample ID | Sample ID | Lamont-Doherty Earth Observatory | |||
7 | DEPTH, sediment/rock | Depth sed | m | Lamont-Doherty Earth Observatory | Geocode | |
8 | Depth, top/min | Depth top | m | Lamont-Doherty Earth Observatory | ||
9 | Depth, bottom/max | Depth bot | m | Lamont-Doherty Earth Observatory | ||
10 | Position | Position | Lamont-Doherty Earth Observatory | |||
11 | Deposit type | Deposit type | Lamont-Doherty Earth Observatory | |||
12 | Quantity of deposit | Quantity | Lamont-Doherty Earth Observatory | |||
13 | Size | Size | Lamont-Doherty Earth Observatory | |||
14 | Substrate type | Substrate | Lamont-Doherty Earth Observatory | |||
15 | Sediment type | Sediment | Lamont-Doherty Earth Observatory | |||
16 | Comment | Comment | Lamont-Doherty Earth Observatory | |||
17 | Description | Description | Lamont-Doherty Earth Observatory |
License:
Creative Commons Attribution 3.0 Unported (CC-BY-3.0)
Size:
377 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 |
---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|
V12-101 | 1957-07-14 | 10.6830 | -65.8300 | -479 | V12-101-1 | 4.500 | 0.00 | 9.00 | In sediment | Mn micronodule | Several | Clay | Olive, poorly sorted, silty clay containing about 10-15% carbonate | Manganese micronodules, micaceous flakes, and glassy non-volcanic materials are evident. | ||
V12-103 | 1957-07-14 | 10.6500 | -65.7200 | -1232 | V12-103-1 | 0.880 | 0.88 | 0.88 | In sediment | Mn micronodule | Many | Clay | Dark olive soft clay is comprised of about 15-20% carbonate | A thin microlamina of light grey silt, comprised mainly of quartz, with foraminifera and manganese micronodules, at 88 cm. | ||
V12-104 | 1957-07-14 | 10.8670 | -65.7500 | -472 | V12-104-1 | 1.860 | 0.00 | 3.72 | In sediment | Mn micronodule | Several | Clay | Dark olive unsorted silty foraminiferal clay is comprised of about 60% carbonate | Micronodules and specks of manganese appear throughout. | ||
V12-107 | 1957-07-15 | 11.3330 | -66.6300 | -1079 | V12-107-1 | 4.455 | 0.00 | 8.91 | In sediment | Mn speck | Many | Clay | Medium to dark olive gray poorly sorted clay | Specks and small patches of manganese are abundant throughout | ||
V12-108 | 1957-07-16 | 11.4000 | -67.8800 | -1717 | V12-108-1 | 1.300 | 0.00 | 2.60 | In sediment | Mn micronodule | Several | Clay | Tan unsorted foraminiferal clay is comprised of 50-60% carbonate | Manganese is scattered throughout in micronodules and small patches. | ||
V12-109 | 1957-07-16 | 11.8000 | -68.5500 | -1701 | V12-109-1 | 4.705 | 0.85 | 8.56 | In sediment | Mn micronodule | Many | Clay | Tan, poorly sorted, foraminiferal clay. Burrows filled with darker colored clay are abundant | Micronodules and patches of manganese become more abundant with depth. | ||
V12-111 | 1957-07-21 | 11.4670 | -75.0700 | -1853 | V12-111-1 | 2.285 | 0.00 | 4.57 | In sediment | Mn micronodule | Several | Clay | Olive gray silty clay | Silt particles, scattered throughout, comprise 15-20% of the total sediment and consist of micaceous flakes, manganese micronodules and quartzfeldspathic materials. | ||
V12-114 | 1957-07-23 | 12.1500 | -75.0700 | -3601 | V12-114-1 | 0.030 | 0.00 | 0.06 | In sediment | Mn micronodule | Several | Clay | Light brown, unsorted, silty clay | Comprised of 25-30% siltsized particles of angular quartz, micaceous flakes and manganese micronodules. | ||
V12-115 | 1957-07-23 | 12.3670 | -75.2200 | -3691 | V12-115-1 | 0.200 | 0.00 | 0.40 | In sediment | Mn micronodule | Few | Clay | Tannish-brown, unsorted, sandy, foraminiferal clay | Manganese micronodules are present. | ||
V12-116 | 1957-07-25 | 11.2330 | -74.3000 | -357 | V12-116-1 | 7.925 | 6.10 | 9.75 | In sediment | Mn micronodule | Several | Clay | Dark greenish-gray clay containing continuous contorted laminae of manganese | Manganese micronodules comprise about 10% of the core | ||
V12-117 | 1957-07-25 | 11.2170 | -74.7700 | -284 | V12-117-1 | 0.520 | 0.00 | 1.04 | In sediment | Mn micronodule | Several | Clay/volcanic ash | Tannish-gray, poorly sorted clay containing small discontinuous lighter laminations throughout. Overlain by a 1 cm dark irregular lamina of volcanic ash | Manganese micronodule and some micaceous flakes occur | ||
V12-120 | 1957-07-27 | 14.3500 | -74.9000 | -4118 | V12-120-1 | 0.250 | 0.00 | 0.50 | In sediment | Mn micronodule | Many | Clay | Light brown foraminiferal silty clay becoming darker with depth | Manganese micronodules are common | ||
V12-120 | 1957-07-27 | 14.3500 | -74.9000 | -4118 | V12-120-2 | 1.975 | 1.58 | 2.37 | In sediment | Mn micronodule | Several | Clay | Brown, unsorted, sandy foraminiferal clay similar to the 10-50 cm. Layer | Manganese micronodules are mixed with the sediment. | ||
V12-121 | 1957-07-28 | 15.3000 | -74.3200 | -4177 | V12-121-1 | 0.750 | 0.00 | 1.50 | In sediment | Mn micronodule | Several | Clay | Tan foraminiferal clay, abundantly burrowed, composed of 50% carbonate. Light gray burrows containing fine volcanic silt occur at 110 cm | Manganese micronodules are scattered throughout. | ||
V12-1 | 1956-12-16 | 34.6330 | -66.6000 | -5207 | V12-1-1 | 4.850 | 0.00 | 9.70 | In sediment | Mn micronodule | Few | Clay | Grayish-brown silty clay | Manganese micronodules are present. | ||
V12-1 | 1956-12-16 | 34.6330 | -66.6000 | -5207 | V12-1-2 | 3.300 | 3.30 | 3.30 | Buried | Mn staining | 1 | 2.5 cm | Rock | Clay | Grayish-brown silty clay | A rock 2 1/2 cm. in diameter occurs at 330 cm |
V12-14 | 1957-01-24 | -23.0300 | -29.0500 | -5110 | V12-14-1 | 4.625 | 0.15 | 9.10 | Buried | Mn staining | Several | Consolidated volcanic ash | Clay | Variegated brown clay | Porous, friable lumps of altered volcanic ash, containing inclusions, of manganese oxide and occasional pyroxene crystals occur throughout. | |
V12-19 | 1957-01-29 | -29.8700 | -36.8000 | -2321 | V12-19-1 | 1.505 | 1.46 | 1.55 | Buried | Mn staining | Several | Volcanic detritus | Clay | Black to dark rusty brown, dry firm conglomeratic clay | Weathered volcanic detritus with manganese iron oxide is found especially near the top. At contact a distinct manganese oxide layer (about 7 cm. thick) marks a real unconformity with above very light tan foraminiferal clay. | |
V12-20 | 1957-01-30 | -31.1500 | -39.4700 | -4667 | V12-20-1 | 0.020 | 0.00 | 0.04 | Buried | Mn coating | 1 | 0.5 cm diam. | Fossil sponge | Clay | Soft dark gray clay contains patches of concentrated siliceous sponge spicules | Siliceous sponge fossil approximately 50 mm in diameter is coated with manganese dioxide. |
V12-20 | 1957-01-30 | -31.1500 | -39.4700 | -4667 | V12-20-2 | 0.720 | 0.63 | 0.81 | In sediment | Mn rich layer | 1 | Clay | Dark bown-black solid layer of manganese dioxide getting patchier near bottom. | |||
V12-22 | 1957-02-01 | -33.7200 | -45.2800 | -4155 | V12-22-1 | 1.420 | 0.00 | 2.84 | In sediment | Mn micronodule | Several | Clay | Dark gray clay | Contains 5-10% manganese micronodules | ||
V12-52 | 1957-04-09 | -39.6000 | -32.8700 | -5015 | V12-52-1 | 0.600 | 0.60 | 0.60 | Buried | Mn nodule | 1 | Clay | Variegated brownish-gray and brown clay. Texture is generally slick | Manganese oxide nodule occurs at 60 cm. | ||
V12-52 | 1957-04-09 | -39.6000 | -32.8700 | -5015 | V12-52-2 | 1.230 | 1.03 | 1.43 | In sediment | Mn micronodule | Many | Clay | Tan clay, very smooth, homogeneous | Very fine manganese oxide micronodules are highly abundant | ||
V12-54 | 1957-04-15 | -41.2300 | -6.1170 | -4082 | V12-54-1 | 8.670 | 8.38 | 8.96 | In sediment | Mn micronodule | Few | Clay/sand | Laminae of white to grayish calcareous clay, which comprise from 40-100% of the sediment, are mixed with laminae of foraminiferal sand | Manganese micronodules are rare | ||
V12-56 | 1957-04-20 | -36.5000 | 8.1000 | -3222 | V12-56-1 | 0.300 | 0.30 | 0.30 | Buried | Mn crust | 1 | Large | Pebbel; mudstone | Clay | Tan to light reddish-brown clay | At 30 cm. a large angular pebble with earthy texture and manganese dioxide crust appears to be a reddish-brown shale or mudstone. |
V12-65 | 1957-05-07 | -22.9800 | 8.1000 | -4118 | V12-65-1 | 6.850 | 6.80 | 6.90 | Buried | Mn crust | 1 | Consolidated sediment | Clay | Very light cream-colored calcareous clay. Some burrows and black specks appear | Contact is very is harp, dips to about 45°, and has a thin coating of manganese oxide. This layer is Neogene in age. | |
V12-72 | 1957-05-20 | -5.6330 | 10.6670 | -2107 | V12-72-1 | 2.450 | 0.00 | 4.90 | In sediment | Mn nodule | Few | Clay | Dark brown silty clay becoming fine-grained sandy clay with depth | The silt and sand particles comprise about 20% of the sediment. They consist primarily of rounded grains of feldspar and pyroxene. Manganese micronodules occur as the minor constituent. | ||
V12-73 | 1957-05-21 | -5.9000 | 9.8830 | -3054 | V12-73-1 | 0.885 | 0.85 | 0.92 | In sediment | Mn rich layer | 1 | Clay | Dark brown clay | |||
V12-80 | 1957-06-01 | 1.7500 | -16.0500 | -4918 | V12-80-1 | 0.765 | 0.33 | 1.20 | In sediment | Mn micronodule | Several | Clay | Bluish-gray unsorted sandy foraminiferal clay becomes darker with depth | Foraminifera, comprising 25-35% of the total sediment, are mixed with manganese micronodules, which constitute 5-7%. | ||
V12-85 | 1957-06-11 | -4.1170 | -29.1200 | -5046 | V12-85-1 | 4.960 | 2.30 | 7.62 | In sediment | Mn speck | Many | Clay | Dark brown smooth clay | Manganese oxide speckling is very abundant. Burrowing occurs throughout. | ||
V12-93 | 1957-07-12 | 12.7670 | -63.1700 | -1463 | V12-93-1 | 0.575 | 0.00 | 1.15 | In sediment | Mn micronodule | Several | Clay | Brownish-green silty unsorted clay | Containing about l5-20% manganese micronodules. | ||
V12-93 | 1957-07-12 | 12.7670 | -63.1700 | -1463 | V12-93-2 | 1.425 | 1.15 | 1.70 | In sediment | Mn micronodule | Several | Sand | Tannish-brown fine to medium grained moderately sorted foraminiferal sand | Containing about 5-10% manganese micronodules | ||
V12-96 | 1957-07-13 | 10.4500 | -64.6800 | -1263 | V12-96-1 | 1.125 | 0.60 | 1.65 | In sediment | Mn micronodule | Several | Clay | Grayish-olive soft poorly sorted clay with about 2% gypsum crystals. Contorted horizontal laminations of grayer clay occur | Manganese micronodules are present throughout. | ||
V12-97 | 1957-07-13 | 10.5830 | -65.0700 | -869 | V12-97-1 | 2.315 | 0.00 | 4.63 | In sediment | Mn micronodule | Several | Clay | Variegated brown clay | Manganese micronodules are scattered throughout. | ||
V12-97 | 1957-07-13 | 10.5830 | -65.0700 | -869 | V12-97-2 | 6.365 | 5.38 | 7.35 | In sediment | Mn micronodule | Several | Clay | Tannish-brown clay | Comprised of about 3-5% carbonate and 3-7% manganese micronodules. | ||
V12-98 | 1957-07-13 | 10.7830 | -65.1200 | -736 | V12-98-1 | 6.200 | 4.06 | 8.34 | In sediment | Mn micronodule | Few | Clay | Medium to light green porous finely laminated silty clay is comprised of about 60% clay and about 40% silt | A few manganese micronodules occur in the darker laminae. | ||
V12-99 | 1957-07-13 | 10.7000 | -65.2000 | -1020 | V12-99-1 | 1.500 | 0.00 | 3.00 | In sediment | Mn micronodule | Many | Clay | Dark green silty unsorted clay with thin horizontal laminae of coarse foraminiferal sand are scattered throughout the layer | Containing abundant manganese, micronodules throughout. | ||
V12-99 | 1957-07-13 | 10.7000 | -65.2000 | -1020 | V12-99-2 | 1.500 | 0.00 | 3.00 | In sediment | Mn filling | Several | Foraminifera test | Clay | Dark green silty unsorted clay with thin horizontal laminae of coarse foraminiferal sand are scattered throughout the layer | Some foraminifera tests are filled with manganese micronodules. | |
V12-99 | 1957-07-13 | 10.7000 | -65.2000 | -1020 | V12-99-3 | 8.200 | 6.60 | 9.80 | In sediment | Mn micronodule | Several | Clay | Pale green clay contains 15-25% fine foraminifera tests | Micronodules and specks of manganese are evident. | ||
V12-127 | 1957-08-15 | 27.9670 | -78.8800 | -816 | V12-127-1 | 0.400 | 0.00 | 0.80 | In sediment | Mn micronodule | Few | Sand | Tan, medium-coarse grained, moderately sorted, pteropod sand containing about 30-40% medium-grained foraminifera tests | Manganese micronodules occur occasionally. | ||
V12-128 | 1957-08-15 | 27.7000 | -79.3300 | -566 | V12-128-1 | 0.400 | 0.00 | 0.80 | In sediment | Mn speck | Few | Sand | Foraminiferal sand, very pale orange, poorly sorted | Manganese fragments also occur throughout layer as a minor constituent. |