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Pimm, Anthony C (1974): Annotated record of the detailed examination of Mn deposits from DSDP Leg 22 (Sites 212, 213, 215, 216, 217, 217A) [dataset]. PANGAEA, https://doi.org/10.1594/PANGAEA.869093, Supplement to: Pimm, AC (1974): Sedimentology and History of the Northeastern Indian Ocean from Late Cretaceous to Recent. In: von der Borch, C.C.; Sclater, J.G.; et al., Initial Reports of the Deep Sea Drilling Project, Initial Reports of the Deep Sea Drilling Project, U.S. Government Printing Office, XXII, 717-803, https://doi.org/10.2973/dsdp.proc.22.139.1974

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Abstract:
Eight sites were drilled on Leg 22 in the northeastern Indian Ocean. Three sites (214, 216, 217) on Ninetyeast Ridge penetrated a thick sequence of mostly Tertiary calcareous oozes passing down into shallow-water sediments with volcanogenic material in Sites 214 and 216. The age of the basal sequence increases northwards from Paleocene (214) through Maastrichtian (216) to Campanian (217). A nonmarine sequence of volcanoclastics and lignite overlies basalt at 214. Drilling terminated in a dolomite chert sequence at 217 before bsalt was encountered. Two sites (213, 215), in deep water on either side of Ninetyeast Ridge, showed calcareous ooze of Paleocene to early Eocene age overlying basalt passing up into brown clay and finally siliceous ooze of late Miocene and younger age. A major hiatus centered in the Oligocene occurs at both these sites. One site (212), drilled in the deepest part of the Wharton Basin, penetrated a brown clay sequence interbedded with several thick calcareous units, each of a very short time duration. Evidence from sedimentary structures and calcareous microfossils.
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: -3.034650 * Median Longitude: 91.878467 * South-bound Latitude: -19.189000 * West-bound Longitude: 86.791700 * North-bound Latitude: 8.926200 * East-bound Longitude: 99.297300
Date/Time Start: 1972-01-27T00:00:00 * Date/Time End: 1972-02-24T00:00:00
Minimum DEPTH, sediment/rock: 5.09 m * Maximum DEPTH, sediment/rock: 508.52 m
Event(s):
22-212  * Latitude: -19.189000 * Longitude: 99.297300 * Date/Time: 1972-01-27T00:00:00 * Elevation: -6233.0 m * Penetration: 521 m * Recovery: 171.2 m * Location: Indian Ocean//BASIN * Campaign: Leg22 * Basis: Glomar Challenger * Method/Device: Drilling/drill rig (DRILL) * Comment: 38 cores; 355 m cored; 0 m drilled; 48.2 % recovery
22-213  * Latitude: -10.211800 * Longitude: 93.896200 * Date/Time: 1972-02-04T00:00:00 * Elevation: -5601.0 m * Penetration: 163 m * Recovery: 143.6 m * Location: Indian Ocean//BASIN * Campaign: Leg22 * Basis: Glomar Challenger * Method/Device: Drilling/drill rig (DRILL) * Comment: 18 cores; 163 m cored; 0 m drilled; 88.1 % recovery
22-215  * Latitude: -8.121700 * Longitude: 86.791700 * Date/Time: 1972-02-13T00:00:00 * Elevation: -5309.0 m * Penetration: 175 m * Recovery: 116 m * Location: Indian Ocean//BASIN * Campaign: Leg22 * Basis: Glomar Challenger * Method/Device: Drilling/drill rig (DRILL) * Comment: 20 cores; 175 m cored; 0 m drilled; 66.3 % recovery
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 labelEvent
IdentificationID
Sample code/labelSample label
DEPTH, sediment/rockDepth sedmGeocode
PositionPositionVisual description
Deposit typeDeposit type
Quantity of depositQuantity
SizeSize
Substrate typeSubstrate
10 Sediment typeSediment
11 CommentComment
12 DescriptionDescription
Size:
122 data points

Data

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Event

ID

Sample label

Depth sed [m]

Position

Deposit type

Quantity

Size

Substrate
10 
Sediment
11 
Comment
12 
Description
22-212 22-212-10-1,25-122-212-10-1,25164.75In sedimentMn micronoduleManyClayIron oxide rich clay (Middle Miocene)25% Mn micronodules. ( Site 212, Core 10, Cored interval 164.5-174.0 m, page 50 )
22-21222-212-16-1,80-122-212-16-1,80298.30In sedimentMn micronoduleManyClayZeolite-bearing iron-oxide-rich claystone (Eocene)30% Mn micronodules. ( Site 212, Core 16, Cored interval 297.5-307.0 m, page 53 )
22-21222-212-29-0,16-122-212-29-0,16421.16In sedimentMn micronoduleSeveralClayClay-bearing to essentially pure (>95% nannofossils) nannofossil chalk (Upper cretaceous)Volcanic glass and manganese micronodules comprise a significant admixture to the nannofossils. ( Site 212, Core 29, Cored interval 421-430.5 m, page 58 )
22-21222-212-38-2,52-122-212-38-2,52508.52In sedimentMn micronoduleSeveralClayIron rich claystone 15% Mn nodules15% Mn micronodules. ( Site 212, Core 38, Cored interval 506.5-516.0 m, page 62 )
22-213 22-213-1-4,39-122-213-1-4,395.09In sedimentMn micronoduleSeveralClayManganese clay with radiolarian rich diatom ooze (Quaternary)14% Mn micronodules. ( Site 213, Core 1, Cored interval 0-9 m, page 93 )
22-21322-213-2-2,60-122-213-2-2,6011.10In sedimentMn micronoduleSeveralAshVolcanic ash clay manganese bearing radiolarian rich diatom ooze (Quaternary)10% Mn micronodules. ( Site 213, Core 2, Cored interval 9-18.5 m, page 93 )
22-21322-213-12-61,115-122-213-12-61,115112.65In sedimentMn micronoduleSeveralClayManganese iron oxide mineral rich clay10% Mn micronodules. ( Site 213, Core 12, Cored interval 9-18.5 m, page 98 )
22-21322-213-16-41,145-122-213-16-41,145147.95In sedimentMn micronoduleManyClayClay rich iron oxide (Upper Paleocene)80% Mn micronodules. ( Site 213, Core 16, Cored interval 142-151.5 m, page 100 )
22-21322-213-17-2,0-122-213-17-2,0152.00BuriedMn coatingSeveralRock; basaltBasaltA succession of at least 11 basaltic flowsEach flow is a pillow-lava with chilled margins, 80% Mn micronodules. ( Site 213, Core 17, Cored interval 151.5-159.5 m, page 101 )
22-215 22-215-9-1,48-122-215-9-1,4874.48In sedimentMn micronoduleSeveralClayZeolite Mn-Fe rich clay (Lower Eocene)10% Mn micronodule. ( Site 215, Core 9, Cored interval 74-83.5 m, page 204 )
22-21522-215-17-11,100-122-215-17-11,100151.00In sedimentMn micronoduleSeveralClayIron oxide rich clay, nanno ooze (Paleocene)12% Mn micronodule. ( Site 215, Core 17, Cored interval 150-155.5 m, page 208 )
22-216 22-216-20-1,90-122-216-20-1,90301.90In sedimentMn micronoduleSeveralChalkNanno chalk white (N9), also light olive gray 5Y6/1 and grayish orange pink (5YR7/2)(Paleocene)Mn micronodules and specks. ( Site 216, Core 20, Cored interval 301-310.5 m, page 227 )
22-21622-216-21-11,120-122-216-21-11,120311.70In sedimentMn micronoduleSeveralChalkPink white ooze chert with white chalk (Paleocene)Mn micronodules in gray laminae. ( Site 216, Core 21, Cored interval 310.5-320 m, page 227 )
22-217 22-217-14-1,10-122-217-14-1,10392.60In sedimentMn micronoduleSeveralUp to 0.5 cmChalkForam bearing nanno chalk (Middle Paleocene)With some Mn micronodules (<5 mm). ( Site 217, Core 14, Cored interval 392.5-402 m, page 282 )
22-217A 22-217A-2-3,80-122-217A-2-3,8013.30In sedimentMn micronoduleSeveralClayForam bearing clay, rich in nanno ooze (Quaternary)Some darker layers with specs of black Mn. ( Site 217A, Core 2, Cored interval 9.5-19 m, page 293 )