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  • Data  (243)
  • 1980-1984  (243)
  • 1925-1929
  • 1982  (119)
  • 1980  (124)
Collection
Keywords
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Years
  • 1980-1984  (243)
  • 1925-1929
Year
  • 1
    Publication Date: 2023-02-08
    Description: Abstract
    Description: The Institute of Seismology, University of Helsinki (ISUH) was founded in 1961 as a response to the growing public concern for environmental hazards caused by nuclear weapon testing. Since then ISUH has been responsible for seismic monitoring in Finland. The current mandate covers government regulator duties in seismic hazard mitigation and nuclear test ban treaty verification, observatory activities and operation of the Finnish National Seismic Network (FNSN) as well as research and teaching of seismology at the University of Helsinki.The first seismograph station of Finland was installed at the premises of the Department of Physics, University of Helsinki in 1924. However, the mechanical Mainka seismographs had low magnification and thus the recordings were of little practical value for the study of local seismicity. The first short-period seismographs were set up between 1956 and 1963. The next significant upgrade of FNSN occurred during the late 1970’s when digital tripartite arrays in southern and central Finland became fully operational, allowing for systematic use of instrumental detection, location and magnitude determination methods. By the end of the 1990’s, the entire network was operating using digital telemetric or dial-up methods. The FNSN has expanded significantly during the 21st Century. It comprises now 36 permanent stations. Most of the stations have Streckeisen STS-2, Nanometrics Trillium (Compact/P/PA/QA) or Guralp CMG-3T broad band sensors. Some Teledyne-Geotech S13/GS13 short period sensors are also in use. Data acquisition systems are a combination of Earth Data PS6-24 digitizers and PC with Seiscomp/Seedlink software or Nanometrics Centaurs. The stations are connected to the ISUH with Seedlink via Internet and provide continuous waveform data at 40 Hz (array) or 100-250 Hz sampling frequency. Further information about instrumentation can be found at the Institute’s web site (www.seismo.helsinki.fi). Waveform data are available from the GEOFON data centre, under network code HE, and arefully open.
    Keywords: geophysics ; seismology ; seismic noise ; earthquakes ; induced ; seismic hazard ; broad band ; velocity ; acceleration ; displacement ; Monitoring system ; Seismological stations ; In Situ/Laboratory Instruments 〉 Magnetic/Motion Sensors 〉 Seismometers ; In Situ Land-based Platforms 〉 GEOPHYSICAL STATIONS/NETWORKS
    Type: Dataset , Seismic Network
    Format: ~300G
    Format: .mseed
    Format: XML
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  • 2
    Publication Date: 2023-05-12
    Description: Abstract
    Description: Sodankylä geophysical observatory (SGO) has operated in Sodankylä in northern Finland since 1913. SGO was originally founded by the Finnish Academy of Science and Letters. Now it takes care of national and international duties studying the space and geoenvironment as an independent research organisation in the University of Oulu. SGO performs long-term measurements, builds instruments, innovates and maintains domestic and international measurements, and performs research from these measurements. The seismic observations at SGO started in Sodankylä 1956. In 2005-2006 SGO seismic stations were updated to broadband instrumentation and connected to GEOFON data center. Today, the number of seismic stations has increased to 9. The stations have Streckeisen STS-2 or Nanometrics Trillium PA/PH broadband sensors. 3 of the stations are so called Posthole stations located in borehole 7-20 m below surface. The rest of the stations are located on the surface or in a more traditional type of vault. Data acquisition systems are either Earth Data PS6-24 digitisers and PC with Seiscomp or Nanometrics Centaurs. The continuous wave form data is collected at 100 Hz sampling frequency. The VH, LH and BH channel data is available from GEOFON data center and the 100Hz HH data from SGO by request. Further information about instrumentation can be found at the Institute’s web site (https://www.sgo.fi/). Waveform data are available from the GEOFON data centre, under network code FN, and arefully open.
    Keywords: geophysics ; seismology ; seismic noise ; earthquakes ; induced ; seismic hazard ; broad band ; velocity ; acceleration ; displacement ; Broadband seismic waveforms ; Seismic monitoring ; EARTH SCIENCE 〉 SOLID EARTH 〉 TECTONICS 〉 EARTHQUAKES ; In Situ/Laboratory Instruments 〉 Magnetic/Motion Sensors 〉 Seismometers ; In Situ Land-based Platforms 〉 GEOPHYSICAL STATIONS/NETWORKS ; In Situ Land-based Platforms 〉 GEOPHYSICAL STATIONS/NETWORKS 〉 SEISMOLOGICAL STATIONS
    Type: Dataset , Seismic Network
    Format: ~300G
    Format: .mseed
    Format: XML
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  • 3
    Publication Date: 2023-07-09
    Keywords: A150/180; A180-73; CH70-K11; CH7X; Cibicidoides kullenbergi, δ13C; Cibicidoides kullenbergi, δ18O; Cibicidoides sp., δ13C; Cibicidoides sp., δ18O; Cibicidoides wuellerstorfi, δ13C; Cibicidoides wuellerstorfi, δ18O; CLIMAP; Climate: Long-Range Investigation, Mapping, and Prediction; Coccoliths, δ18O; D117; DEPTH, sediment/rock; East Atlantic; Elevation of event; ELT49; ELT49.018-PC; Eltanin; Event label; Favocassidulina favus, δ13C; Favocassidulina favus, δ18O; Foraminifera, benthic; Foraminifera, planktic indeterminata; GC; GIK12392-1; Globigerina bulloides, δ13C; Globigerina bulloides, δ18O; Globigerina quinqueloba, δ13C; Globigerina quinqueloba, δ18O; Globigerinoides ruber pink, δ13C; Globigerinoides ruber pink, δ18O; Globigerinoides sacculifer, δ13C; Globigerinoides sacculifer, δ18O; Globocassidulina subglobosa, δ13C; Globocassidulina subglobosa, δ18O; Globoquadrina conglomerata, δ18O; Globorotalia inflata, δ13C; Globorotalia inflata, δ18O; Globorotalia truncatulinoides, δ13C; Globorotalia truncatulinoides, δ18O; Gravity corer; Gyroidina sp., δ13C; Gyroidina sp., δ18O; Hoeglundina elegans, δ13C; Hoeglundina elegans, δ18O; Indian Ocean; Jean Charcot; K708-001; KAL; Kasten corer; Latitude of event; Longitude of event; M12392-1; M25; Marion Dufresne (1972); MD00; MD73025-2; Melonis pompilioides, δ13C; Melonis pompilioides, δ18O; Melonis sp., δ13C; Melonis sp., δ18O; Meteor (1964); Neogloboquadrina dutertrei, δ18O; Neogloboquadrina pachyderma sinistral, δ13C; Neogloboquadrina pachyderma sinistral, δ18O; Nonion sp., δ13C; Nonion sp., δ18O; Oridorsalis sp., δ13C; Oridorsalis sp., δ18O; Oridorsalis tener, δ13C; Oridorsalis tener, δ18O; OSIRIS I; PC; Piston corer; Pulleniatina obliquiloculata, δ18O; Pyrgo murrhina, δ13C; Pyrgo murrhina, δ18O; Pyrgo sp., δ13C; Pyrgo sp., δ18O; RC08; RC08-145; RC08-39; RC10; RC10-65; RC11; RC1112; RC11-120; RC11-210; RC11-230; RC11-86; RC12; RC12-294; RC12-339; RC13; RC13-205; RC13-228; RC13-229; RC15; RC15-61; RC17; RC17-69; RC17-98; Robert Conrad; TR126-23; TR126-29; Uvigerina sp., δ13C; Uvigerina sp., δ18O; V12; V12-122; V18; V18-68; V19; V19-29; V19-53; V21; V21-146; V22; V22-108; V22-174; V22-182; V22-196; V22-38; V23; V23-82; V25; V25-59; V27; V27-20; V27-86; V28; V28-127; V28-14; V28-238; V28-304; V28-345; V28-56; V29; V29-179; V29-29; V30; V30-97; V32; V32-126; V32-128; V34; V34-88; Vema; Y71-06; Y71-06-12; Y7211; Y7211-1; Yaquina; δ18O, adjusted/corrected
    Type: Dataset
    Format: text/tab-separated-values, 5924 data points
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  • 4
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    PANGAEA
    In:  Deutscher Wetterdienst/Seewetteramt, Offenbach/Hamburg
    Publication Date: 2023-07-10
    Keywords: Characteristic of barometric tendency; Cloud base height; CT; DATE/TIME; Dew/frost point; Direction of first swell waves; Height of first swell waves; Height of waves; High cloud; Horizontal visibility; Humidity, relative; Indicator for inclusion or ommission of precipitation data; Indicator for source and units of wind speed; LATITUDE; LONGITUDE; Low/middle cloud amount; Low cloud; M60; M60-track; Mean ships course; Mean ships speed; Meteor (1964); Middle cloud; Past weather1; Past weather2; Periode of first swell waves; Present weather; Pressure, atmospheric; Quality control indicator for (a); Quality control indicator for (clouds); Quality control indicator for (dd); Quality control indicator for (Ds); Quality control indicator for (ff); Quality control indicator for (h); Quality control indicator for (HwHw); Quality control indicator for (iR,RRR,tR); Quality control indicator for (ppp); Quality control indicator for (PPPP); Quality control indicator for (PwPw); Quality control indicator for (swell); Quality control indicator for (tbtbtb); Quality control indicator for (TdTdTd); Quality control indicator for (TTT); Quality control indicator for (TwTwTw); Quality control indicator for (Vs); Quality control indicator for (VV); Quality control indicator for (weather); SUBTROPEX 82; Temperature, air; Temperature, air, wet bulb; Temperature, water; Total cloud amount; Underway cruise track measurements; Wave period; Wind direction; Wind speed
    Type: Dataset
    Format: text/tab-separated-values, 20406 data points
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  • 5
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    PANGAEA
    In:  Supplement to: Murray, David W; Schrader, Hans-Jürgen (1982): The size distribution of the centric diatom Coscinodiscus nodulifer, Site 480, Guaymas Basin Slope, Gulf of California. In: Curray, JR; Moore, DG; et al. (eds.), Initial Reports of the Deep Sea Drilling Project (U.S. Govt. Printing Office), 64, 1239-1244, https://doi.org/10.2973/dsdp.proc.64.163.1982
    Publication Date: 2023-07-10
    Description: Analysis of individual laminae in Recent sediments from the slopes of the Guaymas Basin indicates an increased abundance of the larger sizes (〉60 µm) of Coscinodiscus nodulifer when upwelling conditions persist over the depositional site and an increase of the smaller sizes (〈60 µm) when nonupwelling conditions exist. The size distributions of C. nodulifer in 10-cm composite samples from Hole 480 show a greater abundance of the large sizes (〉60 µm) associated with well-laminated sections and more of the smaller sizes (〈60 µm) in samples from the homogeneous sections. We have tentatively correlated the pronounced homogeneous zones with late Pleistocene glacial periods. These results indicate a persistence of nonupwelling conditions over Hole 480 during glacial periods (homogeneous zones) and a predominance of upwelling conditions during interglacial periods (laminated zones). Other evidence from diatom and silicoflagellate floral analysis seems to support these preliminary conclusions.
    Keywords: 64-480; Coscinodiscus nodulifer; Deep Sea Drilling Project; Description; DRILL; Drilling/drill rig; DSDP; DSDP/ODP/IODP sample designation; Glomar Challenger; Leg64; North Pacific/Gulf of California/BASIN; Sample code/label; Smear slide analysis
    Type: Dataset
    Format: text/tab-separated-values, 96 data points
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  • 6
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    PANGAEA
    In:  Deutscher Wetterdienst/Seewetteramt, Offenbach/Hamburg
    Publication Date: 2023-07-10
    Keywords: Characteristic of barometric tendency; Cloud base height; CT; DATE/TIME; Dew/frost point; Direction of first swell waves; Height of first swell waves; Height of waves; High cloud; Horizontal visibility; Humidity, relative; Indicator for inclusion or ommission of precipitation data; Indicator for source and units of wind speed; LATITUDE; LONGITUDE; Low/middle cloud amount; Low cloud; M63; M63-track; Mean ships course; Mean ships speed; Meteor (1964); Middle cloud; Past weather1; Past weather2; Periode of first swell waves; Present weather; Pressure, atmospheric; Quality control indicator for (a); Quality control indicator for (clouds); Quality control indicator for (dd); Quality control indicator for (Ds); Quality control indicator for (ff); Quality control indicator for (h); Quality control indicator for (HwHw); Quality control indicator for (iR,RRR,tR); Quality control indicator for (ppp); Quality control indicator for (PPPP); Quality control indicator for (PwPw); Quality control indicator for (swell); Quality control indicator for (tbtbtb); Quality control indicator for (TdTdTd); Quality control indicator for (TTT); Quality control indicator for (TwTwTw); Quality control indicator for (Vs); Quality control indicator for (VV); Quality control indicator for (weather); Temperature, air; Temperature, air, wet bulb; Temperature, water; Total cloud amount; Underway cruise track measurements; Wave period; Wind direction; Wind speed
    Type: Dataset
    Format: text/tab-separated-values, 6595 data points
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  • 7
    Publication Date: 2023-07-09
    Keywords: Aplanochytrium sp.; Bottle, Nansen; Counting; DEPTH, water; Dermocystidium sp.; Fungi; Labyrinthuloides sp.; M13; M13_066-1; Meteor (1964); NAS; Number of species; off West Africa; Sample code/label; Schizochytrium aggregatum; Schizochytrium sp.; Thraustochytrium aggregatum; Thraustochytrium multirudimentale; Thraustochytrium sp.; Ulkenia minuta
    Type: Dataset
    Format: text/tab-separated-values, 102 data points
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  • 8
    Publication Date: 2023-07-09
    Keywords: Aplanochytrium sp.; Auftrieb 75; Auftrieb77; BCR; Box corer (Reineck); Counting; Depth, bottom/max; DEPTH, sediment/rock; Depth, top/min; Dermocystidium sp.; East Atlantic; Elevation of event; Event label; Fungi; Grab (Shipek); KAL; Kasten corer; Labyrinthuloides sp.; Latitude of event; Longitude of event; M13; M13_058-2; M13_061-2; M13_062-2; M13_063-2; M13_064-2; M13_065-2; M13_067-2; M13_068-2; M13_070-2; M13_071-2; M13_074-2; M13_076-2; M36; M36_094-2; M36_095-4; M36_096-3; M36_097-3; M36_098-3; M36_099-3; M36_100-4; M36_101-1; M36_102-1; M36_103-1; M36_104-3; M36_105-4; M36_106-1; M36_110-1; M36_124-1; M36_125-1; M36_127-3; M36_128-2; M36_128-3; M36_129-1; M36_129-2; M36_130-1; M36_130-3; M36_131-1; M36_131-2; M44; M44_127-2; M44_127-6; M44_128-4; M44_129-3; M44_129-7; M44_132-1; M44_132-3; M44_133-2; M44_133-4; M44_134-1; M44_134-3; M44_135-1; M44_135-4; M44_193-2; M44_196-2; M44_199-3; M44_199-6; M44_200-1; M44_217-1; M44_235-2; M44_235-3; M44_236-3; M44_236-4; M44_239-2; M44_239-3; M44_242-1; M44_242-3; M44_243-1; M44_244-3; Meteor (1964); Number of species; off Northwest Africa; off West Africa; Sample code/label; Schizochytrium aggregatum; Schizochytrium sp.; SHIPEK; Thraustochytrium aggregatum; Thraustochytrium kinnei; Thraustochytrium motivum; Thraustochytrium multirudimentale; Thraustochytrium pachydermum; Thraustochytrium sp.; Thraustochytrium striatum; Ulkenia minuta; Ulkenia visurgensis; van Veen Grab; VGRAB
    Type: Dataset
    Format: text/tab-separated-values, 1659 data points
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  • 9
    Publication Date: 2023-07-09
    Keywords: Aplanochytrium sp.; Auftrieb 75; Auftrieb77; BCR; Bottle, Nansen; Box corer (Reineck); Counting; DEPTH, water; Dermocystidium sp.; East Atlantic; Event label; FS; Fungi; Labyrinthuloides sp.; Latitude of event; Longitude of event; M13; M13_058-1; M13_059-1; M13_060-1; M13_061-1; M13_062-1; M13_063-1; M13_064-1; M13_065-1; M13_067-1; M13_068-1; M13_069-1; M13_070-1; M13_071-1; M13_074-1; M13_076-1; M36; M36_094_3; M36_095-5; M36_096-7; M36_097-2; M36_098-4; M36_099-2; M36_100-3; M36_103-2; M36_104-4; M36_105-5; M36_108-1; M36_110-2; M36_116-1; M36_124-3; M36_125-5; M36_128-1; M36_129-3; M36_130-2; M36_131-3; M44; M44_127-1; M44_128-5; M44_129-6; M44_131-4; M44_132-7; M44_134-8; M44_135-7; M44_191-3; M44_192-5; M44_193-6; M44_194-2; M44_195-2; M44_196-5; M44_197-1; M44_199-5; M44_200-2; M44_207-2; M44_208-2; M44_209-2; M44_210-2; M44_234-1; M44_235-6; M44_236-2; M44_239-3; M44_240-1; M44_241-1; M44_242-6; Meteor (1964); NAS; Number of species; off Northwest Africa; off West Africa; Photo sledge BGR; Salinity; Sample code/label; Schizochytrium aggregatum; Schizochytrium sp.; Temperature, water; Thraustochytrium aggregatum; Thraustochytrium motivum; Thraustochytrium multirudimentale; Thraustochytrium roseum; Thraustochytrium sp.; Ulkenia minuta; Ulkenia visurgensis; Water sample; WS
    Type: Dataset
    Format: text/tab-separated-values, 1478 data points
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  • 10
    Publication Date: 2023-07-09
    Keywords: Aplanochytrium sp.; Auftrieb 75; Auftrieb77; BCR; Box corer (Reineck); Counting; DEPTH, water; Dermocystidium sp.; East Atlantic; Event label; Fungi; Labyrinthuloides sp.; Latitude of event; Longitude of event; M36; M36_095-4; M36_096-3; M36_097-3; M36_098-3; M36_099-3; M36_100-4; M36_104-3; M36_106-1; M36_110-1; M36_124-1; M36_127-3; M36_128-2; M36_128-3; M36_129-1; M36_129-2; M36_130-1; M36_130-3; M36_131-1; M36_131-2; M44; M44_129-3; M44_132-3; M44_133-2; M44_134-1; M44_134-3; M44_135-1; M44_193-2; M44_199-3; M44_235-2; M44_236-4; M44_239-2; Meteor (1964); Number of species; off Northwest Africa; Sample code/label; Sample volume; Schizochytrium sp.; Thraustochytrium aggregatum; Thraustochytrium motivum; Thraustochytrium multirudimentale; Thraustochytrium pachydermum; Thraustochytrium sp.; Thraustochytrium striatum; Ulkenia minuta; Ulkenia visurgensis; van Veen Grab; VGRAB
    Type: Dataset
    Format: text/tab-separated-values, 671 data points
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  • 11
    Publication Date: 2023-07-09
    Keywords: Aplanochytrium sp.; BC; BCR; Box corer; Box corer (Reineck); Cape Blanc/Meteor Bank/Portugal; Counting; Depth, bottom/max; DEPTH, sediment/rock; Depth, top/min; Dermocystidium sp.; Elevation of event; Event label; FBG; Fungi; Labyrinthuloides sp.; Latitude of event; Longitude of event; M19; M19_193-2; M19_197-2; M19_201-2; M19_202-2; M19_209a-2; M19_210a-2; M19_213-2; M19_215-2; M19_216-2; M19_217-2; M19_218-2; M19_219-2; M19_223-2; M19_229-2; M19_232-2; M19_234-2; M19_236-2; M19_238-2; M19_239-2; M19_241-2; M19_243-2; M19_245-2; M19_246-2; M19_250-2; M19_251-2; M19_252-2; M19_257-2; M19_270-2; M19_271-2; M19_272-2; M19_273-2; M19_274-2; M19_275-2; M19_276-2; M19_277-2; M19_278-2; M19_279-2; M19_282-2; M19_283-2; M19_284-2; M19_285-2; M19_286-2; M19_291-2; M19_292-2; M19_294-2; M19_296-2; M19_298-2; M19_299-2; M19_304-2; Meteor (1964); Number of species; Photo grab; Rossbreiten-Expedition 1970; Sample code/label; Schizochytrium aggregatum; Schizochytrium sp.; Thraustochytrium aggregatum; Thraustochytrium kinnei; Thraustochytrium motivum; Thraustochytrium multirudimentale; Thraustochytrium pachydermum; Thraustochytrium sp.; Thraustochytrium striatum; Ulkenia minuta; Ulkenia sp.; Ulkenia visurgensis; van Veen Grab; VGRAB
    Type: Dataset
    Format: text/tab-separated-values, 1378 data points
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  • 12
    Publication Date: 2023-07-09
    Keywords: 20; Counting; DEPTH, water; Dermocystidium sp.; Fungi; Labyrinthula sp.; Labyrinthuloides sp.; North Sea; Number of species; Salinity; Sample code/label; Schizochytrium aggregatum; Schizochytrium sp.; Temperature, water; Thraustochytrium aggregatum; Thraustochytrium aureum; Thraustochytrium multirudimentale; Thraustochytrium pachydermum; Thraustochytrium sp.; Ulkenia minuta; Ulkenia visurgensis; VH_06_76_482-1; VH0676; Victor Hensen; Water sample; WS
    Type: Dataset
    Format: text/tab-separated-values, 96 data points
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  • 13
    Publication Date: 2023-07-09
    Keywords: 23; Counting; DEPTH, water; Dermocystidium sp.; Fungi; Labyrinthula sp.; Labyrinthuloides sp.; North Sea; Number of species; Salinity; Sample code/label; Schizochytrium aggregatum; Schizochytrium sp.; Temperature, water; Thraustochytrium aggregatum; Thraustochytrium aureum; Thraustochytrium multirudimentale; Thraustochytrium pachydermum; Thraustochytrium sp.; Ulkenia minuta; Ulkenia visurgensis; VH_06_76_479-1; VH0676; Victor Hensen; Water sample; WS
    Type: Dataset
    Format: text/tab-separated-values, 96 data points
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  • 14
    Publication Date: 2023-07-09
    Keywords: 14; CO2BaseSleipner; Counting; DEPTH, water; Dermocystidium sp.; Fungi; Labyrinthula sp.; Labyrinthuloides sp.; North Sea; Number of species; Salinity; Sample code/label; Schizochytrium aggregatum; Schizochytrium sp.; Temperature, water; Thraustochytrium aggregatum; Thraustochytrium aureum; Thraustochytrium multirudimentale; Thraustochytrium pachydermum; Thraustochytrium sp.; Ulkenia minuta; Ulkenia visurgensis; VH_06_76_488-1; VH0676; Victor Hensen; Water sample; WS
    Type: Dataset
    Format: text/tab-separated-values, 96 data points
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  • 15
    Publication Date: 2023-07-09
    Keywords: Cibicides wuellerstorfi, δ18O; DEPTH, sediment/rock; Foraminifera, benthic δ18O; Globigerina pachyderma, δ18O; Mass spectrometer VG Micromass 602; Oridorsalis tener, δ18O; PC; Piston corer; V27; V27-86; Vema
    Type: Dataset
    Format: text/tab-separated-values, 130 data points
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  • 16
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    PANGAEA
    Publication Date: 2023-07-09
    Keywords: 55-433; 55-433A; Abundance; Actinocyclus curvatulus; Actinocyclus divisus; Actinocyclus ehrenbergii; Actinocyclus ehrenbergii var. tenella; Actinocyclus ellipticus; Actinocyclus ellipticus elongatus; Actinocyclus ellipticus forma lanceolata; Actinocyclus ingens; Actinocyclus ochotensis; Actinocyclus oculatus; Actinocyclus tsugaruensis; Actinoptychus undulatus; Asterolampra acutiloba; Asterolampra grevillei; Asterolampra marylandica; Asteromphalus darwinii; Asteromphalus flabellatus; Asteromphalus hookeri; Asteromphalus hungaricus; Asteromphalus robustus; Cocconeis costata; Coscinodiscus curvatulus; Coscinodiscus endoi; Coscinodiscus lewisianus; Coscinodiscus marginatus; Coscinodiscus nodulifer; Coscinodiscus oculus-iridis; Coscinodiscus stellaris; Coscinodiscus symbolophorus; Coscinodiscus tabularis; Cosmiodiscus insignis; Counting, diatoms; Deep Sea Drilling Project; Denticula hyalina; Denticula kamtschatica; Denticula lauta; Denticula punctata; Denticula seminae; Denticula seminae fossilis; Depth, bottom/max; DEPTH, sediment/rock; Depth, top/min; Diatom preservation; Diatom zone; Diploneis bombus; DRILL; Drilling/drill rig; DSDP; DSDP/ODP/IODP sample designation; Epoch; Event label; Glomar Challenger; Hemidiscus cuneiformis; Leg55; Mediaria splendida; Nitzschia cf. oceanica; Nitzschia fossilis; Nitzschia jouseae; Nitzschia marina; Nitzschia miocenica; Nitzschia reinholdii; Nitzschia rolandii; Nitzschia suikoensis; North Pacific/SEAMOUNT; Planktoniella sol; Pseudoeunotia doliolus; Rhabdonema japonicum; Rhizosolenia barboi; Rhizosolenia bergonii; Rhizosolenia curvirostris; Rhizosolenia hebetata forma hiemalis; Rhizosolenia sp.; Rhizosolenia styliformis; Rouxia californica; Rouxia naviculoides; Rouxia yabei; Sample code/label; Stephanopyxis turris; Synedra jouseana; Thalassionema nitzschioides; Thalassiosira aff. borealis; Thalassiosira antiqua; Thalassiosira borealis; Thalassiosira convexa; Thalassiosira decipiens; Thalassiosira eccentrica; Thalassiosira eccentrica var. fasiculatus; Thalassiosira eccentrica var. jouseae; Thalassiosira eccentrica var. leasareolatus; Thalassiosira gravida; Thalassiosira gravida fossilis; Thalassiosira hyalina; Thalassiosira jacksonii; Thalassiosira leptopus; Thalassiosira lineata; Thalassiosira miocenica; Thalassiosira oestrupii; Thalassiosira opposita; Thalassiosira plicata; Thalassiosira praeconvexa; Thalassiothrix longissima
    Type: Dataset
    Format: text/tab-separated-values, 4226 data points
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  • 17
    facet.materialart.
    Unknown
    PANGAEA
    In:  Supplement to: Keigwin, Lloyd D (1982): Stable isotope stratigraphy and paleoceanography of Sites 502 and 503. In: Prell, WL; Gardner, JV; et al. (eds.), Initial Reports of the Deep Sea Drilling Project (U.S. Govt. Printing Office), 68, 445-453, https://doi.org/10.2973/dsdp.proc.68.119.1982
    Publication Date: 2023-07-09
    Description: Analyses of stable isotopes of monospecific planktonic foraminifers (G. quadrilobatus group) and monogeneric benthic foraminifers (Cibicidoides spp.) from late Neogene Atlantic Site 502 and Pacific Site 503 were conducted in order to determine the paleoceanographic changes resulting from the late Neogene uplift of the Panama Isthmus and from climatic cooling. In general, results at each site are similar to those from previous studies for the late Miocene and late Pliocene time interval, documenting the late Miocene (6 Ma) shift in carbon isotopes and the inferred growth of permanent Northern Hemisphere continental ice sheets beginning about 3.2 Ma. Comparison of Atlantic-Pacific planktonic-benthic isotope data for four stratigraphic intervals (~6-8, ~5-6, ~3-5, and ~2-3 Ma) suggests that increasing isolation of Atlantic and Pacific low-latitude waters may be related to the emergence of the Panama Isthmus. The contrast between Atlantic and Pacific benthic foraminiferal d13C increased in two steps from 0.60 per mil to 1 per mil (the modern contrast) at about 6 Ma and 3 Ma. The first increase (0.15 per mil) may represent the end of previously limited deep-water communication between the Atlantic and Pacific at the present location of Panama. The second increase (0.25 per mil) may be due to increased production of North Atlantic Deep Water. This probably reflects the development of modern deep-sea circulation. The d18O of planktonic foraminifers begins to increase in Atlantic Site 502 at 4.2 Ma and may reflect the increasing salinity of the North Atlantic Ocean arising from diminishing surface-water exchange across Panama. This increase is clearly shown by contrasting the d18O of Atlantic and Pacific planktonic foraminifers, as well as the d18O of planktonic and benthic foraminifers at Site 502. This inferred increase in surface-water salinity begins at the time of increasing provinciality of Atlantic and Pacific planktonic foraminifers.
    Keywords: 68-502A; 68-502B; 68-502C; 68-503A; 68-503B; Caribbean Sea/RIDGE; Cibicidoides kullenbergi, δ13C; Cibicidoides kullenbergi, δ18O; Cibicidoides wuellerstorfi, δ13C; Cibicidoides wuellerstorfi, δ18O; Deep Sea Drilling Project; DEPTH, sediment/rock; DRILL; Drilling/drill rig; DSDP; DSDP/ODP/IODP sample designation; Elevation of event; Event label; Globigerinoides quadrilobatus, δ13C; Globigerinoides quadrilobatus, δ18O; Glomar Challenger; Latitude of event; Leg68; Longitude of event; North Pacific/FLANK; Oridorsalis tener, δ13C; Oridorsalis tener, δ18O; Sample code/label; see reference(s)
    Type: Dataset
    Format: text/tab-separated-values, 699 data points
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  • 18
    Publication Date: 2023-07-09
    Keywords: 10; 11; 12; 13; 14; 15; 16; 17; 18; 19; 20; 21; 22; 23; 24; 25; 26; 27; 28; 29; 30; 31; 32; 7; 8; 9; Aplanochytrium sp.; CO2BaseSleipner; Counting; Date/Time of event; DEPTH, water; Dermocystidium sp.; Event label; Fungi; Hyalochlorella; Labyrinthuloides sp.; Latitude of event; Limfjorden; Longitude of event; North Sea; Number of species; Oder Estuary; Salinity; Sample code/label; Schizochytrium aggregatum; Schizochytrium sp.; Temperature, water; Thraustochytrium aggregatum; Thraustochytrium kinnei; Thraustochytrium multirudimentale; Thraustochytrium pachydermum; Thraustochytrium roseum; Thraustochytrium sp.; Thraustochytrium striatum; Ulkenia minuta; Ulkenia visurgensis; VH_03_76_244-1; VH_03_76_245-1; VH_03_76_246-1; VH_03_76_247-1; VH_03_76_251-1; VH_03_76_252-1; VH_03_76_253-1; VH_03_76_254-1; VH_03_76_255-1; VH_03_76_256-1; VH_03_76_257-1; VH_03_76_258-1; VH_03_76_259-1; VH_03_76_260-1; VH_03_76_261-1; VH_03_76_262-1; VH_03_76_263-1; VH_03_76_264-1; VH_03_76_265-1; VH_03_76_266-1; VH_03_76_267-1; VH_03_76_268-1; VH_03_76_269-1; VH_03_76_270-1; VH_03_76_271-1; VH_03_76_272-1; VH_03_76_273-1; VH_03_76_274-1; VH_06_76_447-1; VH_06_76_448-1; VH_06_76_452-1; VH_06_76_453-1; VH_06_76_473-1; VH_06_76_474-1; VH_06_76_475-1; VH_06_76_476-1; VH_06_76_477-1; VH_06_76_478-1; VH_06_76_479-1; VH_06_76_480-1; VH_06_76_481-1; VH_06_76_482-1; VH_06_76_483-1; VH_06_76_484-1; VH_06_76_485-1; VH_06_76_486-1; VH_06_76_487-1; VH_06_76_488-1; VH_06_76_489-1; VH_06_76_490-1; VH_06_76_491-1; VH_06_76_492-1; VH_09_76_831-1; VH_09_76_832-1; VH_09_76_834-1; VH_09_76_835-1; VH_09_76_837-1; VH_09_76_838-1; VH_09_76_839-1; VH_09_76_840-1; VH_09_76_841-1; VH_09_76_842-1; VH_09_76_843-1; VH_09_76_844-1; VH_09_76_845-1; VH_09_76_846-1; VH_09_76_847-1; VH_09_76_848-1; VH_09_76_849-1; VH_09_76_850-1; VH_09_76_851-1; VH_09_76_852-1; VH_09_76_853-1; VH_09_76_854-1; VH_09_76_855-1; VH_09_76_856-1; VH_09_76_858-1; VH_10_75_376-1; VH_10_75_377-1; VH_10_75_378-1; VH_10_75_379-1; VH_10_75_380-1; VH_10_75_381-1; VH_10_75_382-1; VH_10_75_383-1; VH_10_75_384-1; VH_10_75_385-1; VH_10_75_386-1; VH_10_75_387-1; VH_10_75_388-1; VH_10_75_389-1; VH_10_75_390-1; VH_10_75_391-1; VH_10_75_392-1; VH_10_75_393-1; VH_10_75_394-1; VH_10_75_395-1; VH_10_75_396-1; VH_10_75_397-1; VH_10_75_398-1; VH_10_75_399-1; VH_10_75_400-1; VH_12_75_521-1; VH_12_75_522-1; VH_12_75_523-1; VH_12_75_524-1; VH_12_75_525-1; VH_12_75_526-1; VH_12_75_527-1; VH_12_75_528-1; VH_12_75_529-1; VH_12_75_530-1; VH_12_75_531-1; VH_12_75_532-1; VH0376; VH0676; VH0976; VH1075; VH1275; Victor Hensen; Water sample; WS
    Type: Dataset
    Format: text/tab-separated-values, 3178 data points
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  • 19
    Publication Date: 2023-07-09
    Keywords: 17; CO2BaseSleipner; Counting; DEPTH, water; Dermocystidium sp.; Fungi; Labyrinthula sp.; Labyrinthuloides sp.; North Sea; Number of species; Salinity; Sample code/label; Schizochytrium aggregatum; Schizochytrium sp.; Temperature, water; Thraustochytrium aggregatum; Thraustochytrium aureum; Thraustochytrium multirudimentale; Thraustochytrium pachydermum; Thraustochytrium sp.; Ulkenia minuta; Ulkenia visurgensis; VH_06_76_485-1; VH0676; Victor Hensen; Water sample; WS
    Type: Dataset
    Format: text/tab-separated-values, 96 data points
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  • 20
    Publication Date: 2023-07-09
    Keywords: 10; 11; 12; 13; 14; 15; 16; 17; 18; 19; 20; 21; 22; 23; 24; 25; 26; 27; 28; 29; 30; 31; 32; 7; 8; 9; Aplanochytrium sp.; CO2BaseSleipner; Counting; Date/Time of event; DEPTH, sediment/rock; Dermocystidium sp.; Elevation of event; Event label; Fungi; Labyrinthuloides sp.; Latitude of event; Longitude of event; North Sea; Number of species; Sample code/label; Schizochytrium sp.; Thraustochytrium aggregatum; Thraustochytrium kinnei; Thraustochytrium multirudimentale; Thraustochytrium pachydermum; Thraustochytrium sp.; Ulkenia minuta; Ulkenia visurgensis; van Veen Grab; VGRAB; VH_03_76_244-2; VH_03_76_245-2; VH_03_76_246-2; VH_03_76_247-2; VH_03_76_251-2; VH_03_76_252-2; VH_03_76_253-2; VH_03_76_254-2; VH_03_76_255-2; VH_03_76_256-2; VH_03_76_257-2; VH_03_76_258-2; VH_03_76_259-2; VH_03_76_260-2; VH_03_76_261-2; VH_03_76_262-2; VH_03_76_263-2; VH_03_76_264-2; VH_03_76_265-2; VH_03_76_266-2; VH_03_76_268-2; VH_03_76_269-2; VH_03_76_270-2; VH_03_76_271-2; VH_03_76_272-2; VH_03_76_273-2; VH_03_76_274-2; VH_06_76_447-2; VH_06_76_448-2; VH_06_76_449-2; VH_06_76_452-2; VH_06_76_453-2; VH_06_76_473-2; VH_06_76_474-2; VH_06_76_475-2; VH_06_76_476-2; VH_06_76_477-2; VH_06_76_478-2; VH_06_76_479-2; VH_06_76_480-2; VH_06_76_481-2; VH_06_76_482-2; VH_06_76_483-2; VH_06_76_484-2; VH_06_76_485-2; VH_06_76_486-2; VH_06_76_487-2; VH_06_76_488-2; VH_06_76_489-2; VH_06_76_490-2; VH_06_76_491-2; VH_06_76_492-2; VH_09_76_831-2; VH_09_76_832-2; VH_09_76_834-2; VH_09_76_835-2; VH_09_76_837-2; VH_09_76_838-2; VH_09_76_839-2; VH_09_76_840-2; VH_09_76_841-2; VH_09_76_842-2; VH_09_76_843-2; VH_09_76_844-2; VH_09_76_845-2; VH_09_76_846-2; VH_09_76_847-2; VH_09_76_848-2; VH_09_76_849-2; VH_09_76_850-2; VH_09_76_851-2; VH_09_76_852-2; VH_09_76_853-2; VH_09_76_854-2; VH_09_76_855-2; VH_09_76_856-2; VH_09_76_858-2; VH_10_75_376-2; VH_10_75_377-2; VH_10_75_378-2; VH_10_75_380-2; VH_10_75_381-2; VH_10_75_382-2; VH_10_75_383-2; VH_10_75_384-2; VH_10_75_385-2; VH_10_75_386-2; VH_10_75_387-2; VH_10_75_388-2; VH_10_75_389-2; VH_10_75_390-2; VH_10_75_391-2; VH_10_75_392-2; VH_10_75_393-2; VH_10_75_394-2; VH_10_75_395-2; VH_10_75_396-2; VH_10_75_397-2; VH_10_75_399-2; VH_10_75_400-2; VH_12_75_521-2; VH_12_75_522-2; VH_12_75_523-2; VH_12_75_524-2; VH_12_75_525-2; VH_12_75_526-2; VH_12_75_527-2; VH_12_75_528-2; VH_12_75_529-2; VH_12_75_530-2; VH_12_75_531-2; VH_12_75_532-2; VH0376; VH0676; VH0976; VH1075; VH1275; Victor Hensen
    Type: Dataset
    Format: text/tab-separated-values, 2373 data points
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  • 21
    facet.materialart.
    Unknown
    PANGAEA
    In:  Supplement to: Murdmaa, Ivar O; Avdeiko, G P (1980): Volcaniclastic constituents in the Leg 55 sediments. In: Jackson, ED; Koisumi, I; et al., (eds.), Initial Reports of the Deep Sea Drilling Project (U.S. Govt. Printing Office), 55, 503-505, https://doi.org/10.2973/dsdp.proc.55.119.1980
    Publication Date: 2023-07-07
    Description: This chapter was previously intended to trace volcanic episodes through the Neogene and Pleistocene geological history recorded in the sedimentary sections drilled on the Emperor seamounts. Drilling disturbance, poor core recovery, and incomplete stratigraphic sections recovered from the seamounts have frustrated that plan, however. Moreover, the Leg 55 sedimentologists found in their smear-slide studies that transported island-arc tephra is scarce in the sediments, if present at all. So we have restricted our objective to description of the volcaniclastic admixture in sediments, as determined by mineralogical and geochemical data. We studied geochemistry of bulk samples (see Murdmaa et al., 1980), coarse-fraction mineralogy, and additional smear slides. The results obtained, however, do not tell much more about the volcaniclastic matter than did shipboard core descriptions.
    Keywords: 55-430; 55-432; 55-433A; 55-433B; Apatite; Barite; Carbonates; Clinopyroxene; Deep Sea Drilling Project; DRILL; Drilling/drill rig; DSDP; DSDP/ODP/IODP sample designation; Elevation of event; Epidote; Event label; Feldspar; Garnet; Glomar Challenger; Heavy minerals; Hornblende; Iron oxide; Latitude of event; Leg55; Light minerals; Longitude of event; North Pacific/SEAMOUNT; North Pacific/SEDIMENT POND; North Pacific/TERRACE; Opal, biogenic silica; Opaque minerals; Orthopyroxene; Plagioclase; Pyrite, FeS2; Quartz; Sample code/label; Smear slide analysis; Sphene; Volcanic glass; Zeolite; Zircon
    Type: Dataset
    Format: text/tab-separated-values, 286 data points
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  • 22
    Publication Date: 2023-07-07
    Keywords: 57-439; Biotite; Calcite; Chert; Clinopyroxene; Deep Sea Drilling Project; DRILL; Drilling/drill rig; DSDP; DSDP/ODP/IODP sample designation; Glomar Challenger; Grain size, maximum; Hornblende; Leg57; Limestone; North Pacific/TRENCH; Sample code/label; Sandstone; Smear slide analysis; Volcanic fragments
    Type: Dataset
    Format: text/tab-separated-values, 88 data points
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  • 23
    Publication Date: 2023-07-07
    Keywords: 56-434; 56-434A; 56-434B; 56-435; 56-435A; 56-436; 57-438; 57-438A; 57-439; 57-440; 57-440A; 57-440B; Actinolite; Anatase; Apatite; Barite; Biotite; Carbonates; Chalcedony; Chlorite; Clinopyroxene; Deep Sea Drilling Project; DRILL; Drilling/drill rig; DSDP; DSDP/ODP/IODP sample designation; Elevation of event; Epidote; Event label; Feldspar; Garnet; Glauconite; Glomar Challenger; Heavy minerals; Hornblende; Iron oxide; Latitude of event; Leg56; Leg57; Leucoxene; Longitude of event; Minerals; North Pacific/BASIN; North Pacific/RIDGE; North Pacific/TRENCH; Olivine; Opal, biogenic silica; Opaque minerals; Orthopyroxene; Phosphate; Plagioclase; Pyrite, FeS2; Quartz; Quartz/Feldspar ratio; Ratio; Rhodochrosite (2.84 Å); Rutile; Sample code/label; Sphene; Volcanic glass; Volcanic glass, acidic; X-ray diffraction (XRD); Zeolite; Zircon
    Type: Dataset
    Format: text/tab-separated-values, 2437 data points
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  • 24
    Publication Date: 2023-07-07
    Keywords: 55-432A; Apatite; Clinopyroxene; Deep Sea Drilling Project; DRILL; Drilling/drill rig; DSDP; DSDP/ODP/IODP sample designation; Glomar Challenger; Leg55; North Pacific/TERRACE; Olivine; Opaque minerals; Plagioclase; Sample code/label; Volcanic glass
    Type: Dataset
    Format: text/tab-separated-values, 49 data points
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  • 25
    Publication Date: 2023-07-07
    Keywords: 67-494; 67-494A; 67-495; 67-496; 67-499; Actinolite; Apatite; Barite; Biotite; Clinopyroxene; Counting; Deep Sea Drilling Project; DEPTH, sediment/rock; DRILL; Drilling/drill rig; DSDP; DSDP/ODP/IODP sample designation; Elevation of event; Epidote; Event label; Garnet; Glomar Challenger; Heavy minerals; Hornblende; Latitude of event; Leg67; Longitude of event; North Pacific/TRENCH; Olivine; Orthopyroxene; Sample code/label; Sphene; Spinel; Zircon
    Type: Dataset
    Format: text/tab-separated-values, 705 data points
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  • 26
    Publication Date: 2023-07-07
    Keywords: 66-487; Clinopyroxene; Deep Sea Drilling Project; Description; DRILL; Drilling/drill rig; DSDP; DSDP/ODP/IODP sample designation; Glomar Challenger; Leg66; Matrix; Minerals; North Pacific/TRENCH; Olivine; Plagioclase; Sample code/label; Spinel; Titanomagnetite
    Type: Dataset
    Format: text/tab-separated-values, 110 data points
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  • 27
    Publication Date: 2023-07-10
    Keywords: Aluminium oxide; Archive of Ocean Data; ARCOD; Barium; Boron; Calcium oxide; Carbon dioxide; Chromium; Cobalt; Copper; DM1402-D2; DM17; Dmitry Mendeleev; Dredge; DRG; Fluorine; Hafnium; Iron oxide, Fe2O3; Iron oxide, FeO; Lithium; Magnesium oxide; Manganese oxide; Nickel; Niobium; Philippine Sea; Phosphorus pentoxide; Potassium oxide; Rubidium; Sample code/label; Sample type; Scandium; Silicon dioxide; Sodium oxide; Strontium; Sum; Tantalum; Thorium; Titanium dioxide; Uranium; Vanadium; Water in rock; Yttrium; Zinc; Zirconium
    Type: Dataset
    Format: text/tab-separated-values, 477 data points
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  • 28
    Publication Date: 2023-07-10
    Keywords: 66-487; 67-495; 67-499C; 67-499D; 67-500; 67-500B; Antimony; Barium; Caesium; Cerium; Chromium; Cobalt; Deep Sea Drilling Project; DRILL; Drilling/drill rig; DSDP; DSDP/ODP/IODP sample designation; Element analysis, neutron activation (NAA); Elevation of event; Europium; Event label; Glomar Challenger; Hafnium; Iron; Lanthanum; Latitude of event; Leg66; Leg67; Longitude of event; Manganese; Nickel; Niobium; North Pacific/TRENCH; Rubidium; Sample code/label; Scandium; Strontium; Tantalum; Terbium; Thorium; Titanium; Uranium; Vanadium; X-ray fluorescence (XRF); Yttrium; Zinc; Zirconium
    Type: Dataset
    Format: text/tab-separated-values, 387 data points
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  • 29
    Publication Date: 2023-07-10
    Keywords: 60-453; 60-454A; 60-456; 60-456A; 60-457; 60-458; 60-459B; 60-460; 60-461A; Aluminium oxide; Barium; Calcium; Calcium oxide; Cerium; Chromium; Cobalt; Deep Sea Drilling Project; DRILL; Drilling/drill rig; DSDP; DSDP/ODP/IODP sample designation; Element analysis, neutron activation (NAA); Elevation of event; Europium; Event label; Gallium; Glomar Challenger; Hafnium; Iron oxide, Fe2O3; Iron oxide, FeO; Lanthanum; Latitude of event; Leg60; Location; Longitude of event; Magnesium number; Magnesium oxide; Manganese oxide; Nickel; North Pacific/RIDGE; North Pacific/SEDIMENT POND; North Pacific/TRENCH; Phosphorus pentoxide; Potassium oxide; Rubidium; Sample code/label; Sample ID; Scandium; Silicon dioxide; Sodium oxide; Strontium; Tantalum; Terbium; Thorium; Titanium dioxide; Total; Uranium; X-ray fluorescence (XRF); Yttrium; Zinc; Zirconium
    Type: Dataset
    Format: text/tab-separated-values, 551 data points
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  • 30
    Publication Date: 2023-07-10
    Keywords: 60-453; Aluminium (IV); Aluminium (VI); Aluminium oxide; Calcium; Calcium oxide; Calculated based on oxygen number; Deep Sea Drilling Project; DRILL; Drilling/drill rig; DSDP; DSDP/ODP/IODP sample designation; Glomar Challenger; Iron 2+ and 3+; Iron oxide, FeO; Leg60; Lithology/composition/facies; Magnesium; Magnesium oxide; Manganese; Manganese oxide; Minerals; North Pacific/SEDIMENT POND; Number of oxygens; Potassium; Potassium oxide; Sample code/label; Silicon; Silicon dioxide; Sodium; Sodium oxide; Titanium; Titanium dioxide; Total; X-ray fluorescence (XRF)
    Type: Dataset
    Format: text/tab-separated-values, 167 data points
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  • 31
    Publication Date: 2023-07-10
    Keywords: 60-459B; Albite; Aluminium; Aluminium oxide; Anorthite; Calcium; Calcium oxide; Calculated based on oxygen number; CIPW Norm; Deep Sea Drilling Project; DRILL; Drilling/drill rig; DSDP; DSDP/ODP/IODP sample designation; Electron microprobe (EMP); Enstatite; Ferrosilite; Glomar Challenger; Iron 2+ and 3+; Iron oxide, FeO; Leg60; Magnesium; Magnesium oxide; Manganese; Manganese oxide; Mineral name; North Pacific/SEDIMENT POND; Number of oxygens; Orthoclase; Potassium; Potassium oxide; Sample code/label; Silicon; Silicon dioxide; Sodium; Sodium oxide; Titanium; Titanium dioxide; Total; Wollastonite
    Type: Dataset
    Format: text/tab-separated-values, 127 data points
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  • 32
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    Unknown
    PANGAEA
    Publication Date: 2023-07-10
    Keywords: 55-431; 55-431A; Abundance; Actinocyclus curvatulus; Coscinodiscus marginatus; Coscinodiscus nodulifer; Coscinodiscus tabularis; Counting, diatoms; Deep Sea Drilling Project; Denticula seminae; Depth, bottom/max; DEPTH, sediment/rock; Depth, top/min; Diatom preservation; Diatoms; Diatom zone; DRILL; Drilling/drill rig; DSDP; DSDP/ODP/IODP sample designation; Epoch; Event label; Glomar Challenger; Leg55; North Pacific/TERRACE; Pseudoeunotia doliolus; Sample code/label; Thalassionema nitzschioides; Thalassiosira leptopus; Thalassiosira lineata; Thalassiosira oestrupii; Thalassiothrix longissima
    Type: Dataset
    Format: text/tab-separated-values, 95 data points
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  • 33
    Publication Date: 2023-07-10
    Keywords: 55-433C; Cerium; Cerium, standard deviation; Chromium; Chromium, standard deviation; Cobalt; Cobalt, standard deviation; Comment; Deep Sea Drilling Project; DRILL; Drilling/drill rig; DSDP; DSDP/ODP/IODP sample designation; Europium; Europium, standard deviation; Glomar Challenger; Hafnium; Hafnium, standard deviation; Holmium; Holmium, standard deviation; Instrumental neutron activation analysis (INAA); Lanthanum; Lanthanum, standard deviation; Leg55; Lutetium; Lutetium, standard deviation; Neodymium; Neodymium, standard deviation; North Pacific/SEAMOUNT; Samarium; Samarium, standard deviation; Sample code/label; Scandium; Scandium, standard deviation; Tantalum; Tantalum, standard deviation; Terbium; Terbium, standard deviation; Thorium; Thorium, standard deviation; Unit; Ytterbium; Ytterbium, standard deviation
    Type: Dataset
    Format: text/tab-separated-values, 335 data points
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  • 34
    Publication Date: 2023-07-10
    Keywords: 55-430A; 55-432A; 55-433A; 55-433B; 55-433C; Aluminium; Aluminium oxide; Calculated based on oxygen number; Chromium; Chromium(III) oxide; Deep Sea Drilling Project; Description; DRILL; Drilling/drill rig; DSDP; DSDP/ODP/IODP sample designation; Electron microprobe (EMP); Elevation of event; Event label; Glomar Challenger; Identification; Iron 2+; Iron 3+; Iron oxide, Fe2O3; Iron oxide, FeO; Latitude of event; Leg55; Longitude of event; Magnesium; Magnesium oxide; Magnetite; Manganese; Manganese oxide; North Pacific/SEAMOUNT; North Pacific/SEDIMENT POND; North Pacific/TERRACE; Number of oxygens; Rock type; Sample code/label; Titanium; Titanium dioxide; Total; Ulvöspinel; Unit
    Type: Dataset
    Format: text/tab-separated-values, 552 data points
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  • 35
    Publication Date: 2023-07-10
    Keywords: Aluminium oxide; Archive of Ocean Data; ARCOD; Barium; Boron; Calcium oxide; Carbon dioxide; Chromium; Cobalt; Comment; Copper; DM1403-D; DM1431-D; DM17; Dmitry Mendeleev; Dredge; DRG; Elevation of event; Elevation of event 2; Event label; Fluorine; Hafnium; Iron oxide, Fe2O3; Iron oxide, FeO; Latitude of event; Latitude of event 2; Lithium; Longitude of event; Longitude of event 2; Magnesium oxide; Manganese oxide; Nickel; Niobium; Philippine Sea; Phosphorus pentoxide; Potassium oxide; Rubidium; Sample code/label; Sample type; Scandium; Silicon dioxide; Sodium oxide; Strontium; Sum; Tantalum; Thorium; Titanium dioxide; Uranium; Vanadium; Water in rock; Yttrium; Zinc; Zirconium
    Type: Dataset
    Format: text/tab-separated-values, 205 data points
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  • 36
    Publication Date: 2023-07-10
    Keywords: Aluminium oxide; Archive of Ocean Data; ARCOD; Barium; Boron; Calcium oxide; Carbon dioxide; Chromium; Cobalt; Copper; DM1404-D; DM17; Dmitry Mendeleev; Dredge; DRG; Fluorine; Hafnium; Iron oxide, Fe2O3; Iron oxide, FeO; Lithium; Loss on ignition; Magnesium oxide; Manganese oxide; Nickel; Niobium; Philippine Sea; Phosphorus pentoxide; Potassium oxide; Rubidium; Sample code/label; Sample type; Scandium; Silicon dioxide; Sodium oxide; Strontium; Sum; Tantalum; Thorium; Titanium dioxide; Uranium; Vanadium; Water in rock; Yttrium; Zinc; Zirconium
    Type: Dataset
    Format: text/tab-separated-values, 485 data points
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  • 37
    Publication Date: 2023-07-10
    Keywords: Aluminium oxide; Archive of Ocean Data; ARCOD; Barium; Boron; Calcium oxide; Carbon dioxide; Chromium; Cobalt; Copper; DM1398-D; DM17; Dmitry Mendeleev; Dredge; DRG; Fluorine; Hafnium; Iron oxide, Fe2O3; Iron oxide, FeO; Lithium; Loss on ignition; Magnesium oxide; Manganese oxide; Nickel; Niobium; Philippine Sea; Phosphorus pentoxide; Potassium oxide; Rubidium; Sample code/label; Sample type; Scandium; Silicon dioxide; Sodium oxide; Strontium; Sum; Tantalum; Thorium; Titanium dioxide; Uranium; Vanadium; Water in rock; Yttrium; Zinc; Zirconium
    Type: Dataset
    Format: text/tab-separated-values, 257 data points
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  • 38
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    PANGAEA
    In:  P.P. Shirshov Institute of Oceanology, Russian Academy of Sciences, Moscow
    Publication Date: 2023-07-10
    Keywords: 42-379A; 42-380; 42-380A; 42-381; Achnanthes brevipes; Actinocyclus divisus; Actinocyclus ehrenbergii; Actinocyclus normannii; Actinocyclus ochotensis; Actinoptychus undulatus; Amphiprora gigantea; Amphora variabilis; Black Sea; Chaetoceros danicus; Chaetoceros peruvianus; Coscinodiscus hungaricus; Coscinodiscus stockesianus; Cyclotella caspia; Cyclotella corona; Cyclotella kutzingiana; Cyclotella praekutzingiana; Cyclotella proshkinae; Cyclotella servant-vildary; Cyclotella servant-vildary elegans; Deep Sea Drilling Project; Depth, bottom/max; DEPTH, sediment/rock; Depth, top/min; DRILL; Drilling/drill rig; DSDP; DSDP/ODP/IODP sample designation; Elevation of event; Epoch; Event label; Glomar Challenger; Gyrosigma acuminatum; Hemiaulus hauckii; Latitude of event; Leg42; Lithologic unit/sequence; Longitude of event; Melosira bellicosa; Melosira elegans; Melosira hibschii; Melosira papilio; Melosira praegranulata; Melosira praeislandica; Microscopy; Period; Rhaphoneis maeotica; Rhizosolenia alata; Rhizosolenia bezrukovii; Rhizosolenia calcar-avis; Rhizosolenia setigera; Sample code/label; Stephanodiscus astraea; Stephanodiscus carconensis; Stephanodiscus dubius; Stephanodiscus hantzschii; Stephanodiscus marginatus; Stephanodiscus pontica; Stephanodiscus prohantzschii; Surirella striatula; Thalassionema nitzschioides; Thalassiosira maeotica; Thalassiosira makarovae; Thalassiosira oestrupii; Thalassiosira subsalina
    Type: Dataset
    Format: text/tab-separated-values, 1566 data points
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  • 39
    Publication Date: 2023-07-10
    Keywords: 60-456A; Aluminium; Aluminium oxide; Calcium; Calcium oxide; Calculated based on oxygen number; Chromium; Chromium(III) oxide; Deep Sea Drilling Project; DRILL; Drilling/drill rig; DSDP; DSDP/ODP/IODP sample designation; Electron microprobe (EMP); Glomar Challenger; Iron 2+ and 3+; Iron oxide, FeO; Leg60; Lithology/composition/facies; Magnesium; Magnesium oxide; Manganese; Manganese oxide; Nickel oxide; North Pacific/SEDIMENT POND; Number of oxygens; Potassium; Potassium oxide; Sample code/label; Silicon; Silicon dioxide; Sodium; Sodium oxide; Sum; Titanium; Titanium dioxide; Total
    Type: Dataset
    Format: text/tab-separated-values, 126 data points
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  • 40
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    Unknown
    PANGAEA
    Publication Date: 2023-07-10
    Keywords: 55-430; 55-430A; Abundance; Asteromphalus robustus; Coscinodiscus marginatus; Counting, diatoms; Deep Sea Drilling Project; Depth, bottom/max; DEPTH, sediment/rock; Depth, top/min; Diatom preservation; Diatoms; Diatom zone; DRILL; Drilling/drill rig; DSDP; DSDP/ODP/IODP sample designation; Epoch; Event label; Glomar Challenger; Leg55; North Pacific/SEDIMENT POND; Pseudoeunotia doliolus; Sample code/label; Thalassionema nitzschioides; Thalassiosira eccentrica; Thalassiosira oestrupii; Thalassiosira tabularis; Thalassiothrix longissima
    Type: Dataset
    Format: text/tab-separated-values, 96 data points
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  • 41
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    PANGAEA
    Publication Date: 2023-07-10
    Keywords: 55-432; Abundance; Actinocyclus curvatulus; Actinoptychus undulatus; Coscinodiscus marginatus; Coscinodiscus nodulifer; Coscinodiscus radiatus; Coscinodiscus stellaris; Coscinodiscus tabularis; Counting, diatoms; Cyclotella striata; Deep Sea Drilling Project; Denticula seminae; Depth, bottom/max; DEPTH, sediment/rock; Depth, top/min; Diatom preservation; Diatoms; Diatom zone; DRILL; Drilling/drill rig; DSDP; DSDP/ODP/IODP sample designation; Epoch; Glomar Challenger; Hemidiscus cuneiformis; Leg55; Nitzschia kolaczeckii; Nitzschia marina; Nitzschia sicula; North Pacific/TERRACE; Pseudoeunotia doliolus; Rhizosolenia barboi; Rhizosolenia hebetata forma hiemalis; Roperia tesselata; Sample code/label; Thalassionema nitzschioides; Thalassiosira eccentrica; Thalassiosira eccentrica var. fasiculatus; Thalassiosira lineata; Thalassiosira oestrupii; Thalassiosira pacifica; Thalassiothrix longissima
    Type: Dataset
    Format: text/tab-separated-values, 132 data points
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  • 42
    Publication Date: 2023-07-07
    Keywords: Apatite; Archive of Ocean Data; ARCOD; Black ore; Chrome-spinellid; Clinopyroxene; Corundum; Counting, Stereo Microscope; Depth, bottom/max; DEPTH, sediment/rock; Depth, top/min; DM1397-1; DM1397-2; DM1397-4; DM1398-2; DM1398-3b; DM1399-2; DM1401; DM1402-1; DM1403; DM1405; DM1412-1; DM1412-2; DM1416; DM1424; DM1428; DM1429; DM1430; DM1431; DM1437; DM17; Dmitry Mendeleev; Elevation of event; Epidote; Event label; Garnet; GC; Grab; GRAB; Gravity corer; Hornblende; Latitude of event; Longitude of event; Nonidentified, altered, heavy; Olivine; Orthopyroxene; Oxides/hydroxides; Philippine Sea; Pyrite, FeS2; Sphene; Tremolite/Actinolite; Zircon
    Type: Dataset
    Format: text/tab-separated-values, 342 data points
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  • 43
    Publication Date: 2023-07-07
    Keywords: 58-445; Augite; Calcite; Chert; Clinopyroxene; Comment; Deep Sea Drilling Project; DEPTH, sediment/rock; DRILL; Drilling/drill rig; DSDP; DSDP/ODP/IODP sample designation; Foraminifera; Fragments; Glomar Challenger; Leg58; Limestone; Minerals; North Pacific/BASIN; Olivine; Plagioclase; Rock fragments; Sample code/label; Smectite; Volcanic glass; X-ray diffraction (XRD)
    Type: Dataset
    Format: text/tab-separated-values, 411 data points
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  • 44
    Publication Date: 2023-07-07
    Keywords: -; 64-477; 64-478; 64-481A; Anorthite; Clinopyroxene; Comment; Deep Sea Drilling Project; DRILL; Drilling/drill rig; DSDP; DSDP/ODP/IODP sample designation; Elevation of event; Event label; Forsterite; Glomar Challenger; Latitude of event; Leg64; Liquid fraction; Longitude of event; North Pacific/Gulf of California/BASIN; North Pacific/Gulf of California/CHANNEL; Number; Olivine; Plagioclase; Sample code/label; Sample code/label 2; Spinel
    Type: Dataset
    Format: text/tab-separated-values, 276 data points
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  • 45
    Publication Date: 2023-07-07
    Description: Heavy and light minerals were examined in 29 samples from Sites 494, 498, 499, 500, and 495 on the Deep Sea Drilling Project Leg 67 Middle America Trench transect; these sites represent lower slope, trench, and oceanic crust environments off Guatemala. All samples are Quaternary except those from Hole 494A (Pliocene) and Hole 498A (Miocene). Heavy-mineral assemblages of the Quaternary sediments are characterized by an immature pyroxene-amphibole suite with small quantities of olivine and epidote. The Miocene sediments yielded an assemblage dominated by epidote and pyroxene but lacking olivine; the absence of olivine is attributed to selective removal of the most unstable components by intrastratal solution. Light-mineral assemblages of all samples are predominantly characterized by volcanic glass and plagioclase feldspar. The feldspar compositions are compatible with andesitic source rocks and frequently exhibit oscillatory zoning. The heavy- and light-mineral associations of these sediments suggest a proximal volcanic source, most probably the Neogene highland volcanic province of Guatemala. Sand-sized components from Site 495 are mainly biogenic skeletons and volcanic glass and, in one instance (Section 495-5-3), euhedral crystals of gypsum.
    Keywords: 67-494; 67-494A; 67-498A; 67-499; 67-500; Amphibole; Apatite; Clinopyroxene; Deep Sea Drilling Project; DRILL; Drilling/drill rig; DSDP; DSDP/ODP/IODP sample designation; Electron microprobe (EMP); Elevation of event; Epidote; Epoch; Event label; Glomar Challenger; Heavy mineral grains; Latitude of event; Leg67; Longitude of event; North Pacific/TRENCH; Olivine; Orthopyroxene; Rutile; Sample code/label; Sphene
    Type: Dataset
    Format: text/tab-separated-values, 425 data points
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  • 46
    Publication Date: 2023-07-07
    Keywords: -; 64-474A; 64-475B; Anorthite; Clinopyroxene; Comment; Deep Sea Drilling Project; DRILL; Drilling/drill rig; DSDP; DSDP/ODP/IODP sample designation; Event label; Forsterite; Glomar Challenger; Leg64; Liquid fraction; North Pacific/Gulf of California/BASIN; North Pacific/Gulf of California/SLOPE; Number; Olivine; Plagioclase; Sample code/label; Sample code/label 2; Spinel
    Type: Dataset
    Format: text/tab-separated-values, 220 data points
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  • 47
    Publication Date: 2023-07-07
    Keywords: 25-248; Carbonates; Chlorophaeite; Clinopyroxene; Deep Sea Drilling Project; DRILL; Drilling/drill rig; DSDP; DSDP/ODP/IODP sample designation; Glomar Challenger; Indian Ocean//BASIN; Leg25; Olivine; Opaque minerals; Plagioclase; Sample code/label; Total
    Type: Dataset
    Format: text/tab-separated-values, 67 data points
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  • 48
    Publication Date: 2023-07-07
    Keywords: 58-443; 58-445; 58-446A; Clinopyroxene; Comment; Comment 2 (continued); Deep Sea Drilling Project; DRILL; Drilling/drill rig; DSDP; DSDP/ODP/IODP sample designation; Elevation of event; Event label; Glasses; Glomar Challenger; Ilmenite; Latitude of event; Leg58; Longitude of event; North Pacific/BASIN; North Pacific/Philippine Sea/BASIN; Olivine; Plagioclase; Rock type; Sample code/label; Texture; Titanomagnetite
    Type: Dataset
    Format: text/tab-separated-values, 114 data points
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  • 49
    Publication Date: 2023-07-07
    Keywords: 55-433C; Alteration; Clinopyroxene; Deep Sea Drilling Project; DRILL; Drilling/drill rig; DSDP; DSDP/ODP/IODP sample designation; Elements; Glomar Challenger; Leg55; Magnesium number; North Pacific/SEAMOUNT; Olivine; Plagioclase; Sample code/label; Texture; Unit; Water in rock
    Type: Dataset
    Format: text/tab-separated-values, 250 data points
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  • 50
    Publication Date: 2023-07-07
    Keywords: 54-421; 54-422; 54-424; 54-424B; 54-425; 54-427; 54-428; 54-428A; 54-429A; Alteration; Clinopyroxene; Deep Sea Drilling Project; DRILL; Drilling/drill rig; DSDP; DSDP/ODP/IODP sample designation; Elevation of event; Event label; Glomar Challenger; Latitude of event; Leg54; Longitude of event; Mesostasis; North Pacific/CONT RISE; North Pacific/MOUND; North Pacific/RIDGE; North Pacific/SEDIMENT POND; North Pacific/TROUGH; Olivine; Opaque minerals; Phyllosilicate; Piece; Plagioclase; Sample code/label; see reference(s); Vesicle; Volcanic glass
    Type: Dataset
    Format: text/tab-separated-values, 196 data points
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  • 51
    Publication Date: 2023-07-07
    Keywords: 57-439; Biogenic particles; Biotite; Carbonates; Clinopyroxene; Deep Sea Drilling Project; DRILL; Drilling/drill rig; DSDP; DSDP/ODP/IODP sample designation; Epidote; Feldspar; Garnet; Glauconite; Glomar Challenger; Heavy minerals; Hornblende; Leg57; Lithic grains; Minerals; North Pacific/TRENCH; Opaque minerals; Orthopyroxene; Quartz; Sample code/label; Sand; Silt; Size fraction 〈 0.002 mm, clay; Smear slide analysis; Volcanic glass; Zircon
    Type: Dataset
    Format: text/tab-separated-values, 880 data points
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  • 52
    Publication Date: 2023-07-07
    Keywords: 55-430A; 55-432A; 55-433A; 55-433B; 55-433C; Alteration; Clinopyroxene; Deep Sea Drilling Project; DRILL; Drilling/drill rig; DSDP; DSDP/ODP/IODP sample designation; Elevation of event; Event label; Glomar Challenger; Latitude of event; Leg55; Longitude of event; Magnesium number; Mass spectrometry; North Pacific/SEAMOUNT; North Pacific/SEDIMENT POND; North Pacific/TERRACE; Olivine; Plagioclase; Rock type; Sample code/label; Texture; Unit
    Type: Dataset
    Format: text/tab-separated-values, 359 data points
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  • 53
    Publication Date: 2023-07-11
    Keywords: 56-436; Aluminium oxide; Calcium oxide; Deep Sea Drilling Project; DRILL; Drilling/drill rig; DSDP; DSDP/ODP/IODP sample designation; Glomar Challenger; Iron oxide, Fe2O3; Iron oxide, FeO; Leg56; Loss on ignition; Magnesium oxide; Manganese oxide; North Pacific/RIDGE; Potassium oxide; Sample code/label; Silicon dioxide; Size fraction; Sodium oxide; Titanium dioxide; Total; Wet chemistry
    Type: Dataset
    Format: text/tab-separated-values, 84 data points
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  • 54
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    PANGAEA
    In:  Supplement to: Kastner, Miriam (1982): Evidence for two distinct hydrothermal systems in the Guaymas Basin. In: Curray, JR; Moore, DG; et al. (eds.), Initial Reports of the Deep Sea Drilling Project (U.S. Govt. Printing Office), 64, 1143-1157, https://doi.org/10.2973/dsdp.proc.64.154.1982
    Publication Date: 2023-08-04
    Description: Mineralogical and oxygen isotopic analyses of samples from Deep Sea Drilling Project Sites 477, 481, and 477 in the Guaymas Basin indicate the existence of two distinct hydrothermal systems. In the first, at Sites 481 and 478, hot dolerite sills intruded into highly porous hemipelagic siliceous mudstones that were moderately rich in organic matter, thermally altered the adjacent sediments, and expelled hydrothermal pore fluids. The second, at Site 477 and active at present, is most probably caused by a recent igneous intrusion forming a magma chamber at shallow depth. In the first hydrothermal system, the main thermal reactions above and below the sills are dissolution of opal-A and formation of quartz, either directly or through opal-CT; formation of smectite; formation of analcime only above the sills; dissolution and recrystallization of calcite and occasional formation of dolomite or protodolomite. The d18O values of the hydrothermally altered sediments range from 9.9 to 12.2 per mil (SMOW). The d18O values of recrystallized calcites above the first sill complex, Site 481, indicate temperatures of 140° to 170°C. No fluid recharge is required in this system. The thickness of the sill complexes and the sequence and depth of intrusion into the sediment column determine the thickness of the alteration zones, which ranges from 2 or 3 to approximately 50 meters. Generally, the hydrothermally altered zone is thicker above than below the sill. In the second type, the sediments are extensively recrystallized. The characteristic greenschist-facies mineral assemblage of quartz-albite-chlorite-epidote predominates. Considerable amounts of pyrite, pyrrhotite, and sphene are also present. The lowest d18O value of the greenschist facies rocks is 6.6 per mil, and the highest d18O value of the associated pore fluids is +1.38 per mil (SMOW). The paragenesis and the oxygen isotopes of individual phases indicate alteration temperatures of 300 ± 50°C. On the basis of the oxygen isotopes of the solids and associated fluids, it is concluded that recharge of fluids is required. The water/rock ratio in wt.% is moderate, approximately 2/1 to 3/1 - higher than the calculated water/rock ratio of the hydrothermal system at the East Pacific Rise, 21 °N.
    Keywords: 64-477; 64-477A; 64-478; 64-481; 64-481A; Deep Sea Drilling Project; DRILL; Drilling/drill rig; DSDP; Glomar Challenger; Leg64; North Pacific/Gulf of California/BASIN; North Pacific/Gulf of California/CHANNEL
    Type: Dataset
    Format: application/zip, 9 datasets
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  • 55
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    PANGAEA
    Publication Date: 2023-08-04
    Keywords: -; 64-477; 64-477A; Analcime; Calcite; Clinoptilolite; Comment; Deep Sea Drilling Project; DEPTH, sediment/rock; Dolomite; DRILL; Drilling/drill rig; DSDP; DSDP/ODP/IODP sample designation; Event label; Glomar Challenger; Gypsum; Illite; Kalifeldspar; Leg64; Minerals; North Pacific/Gulf of California/BASIN; Opal-A; Plagioclase; Pyrite; Quartz; Sample code/label; Smectite; X-ray diffraction (XRD)
    Type: Dataset
    Format: text/tab-separated-values, 560 data points
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  • 56
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    PANGAEA
    In:  Supplement to: Barrett, T J; Friedrichsen, Hans (1982): Elemental and isotopic compositions of some metalliferous and pelagic sediments from the Galapagos mounds area, DSDP Leg 70. Chemical Geology, 36(3-4), 275-298, https://doi.org/10.1016/0009-2541(82)90052-3
    Publication Date: 2023-08-28
    Description: Nontronite, the main metalliferous phase of the Galapagos mounds, occurs at a subsurface depth of ~2–20 m; Mn-oxide material is limited to the upper 2 m of these mounds. The nontronite forms intervals of up to a few metres thickness, consisting essentially of 100% nontronite granules, which alternate with intervals of normal pelagic sediment. The metalliferous phases represent essentially authigenic precipitates, apparently formed in the presence of upwelling basement-derived hydrothermal solutions which dissolved pre-existent pelagic sediment. Electron microprobe analyses of nontronite granules from different core samples indicate that: (1) there is little difference in major-element composition between nontronitic material from varying locations within the mounds; and (2) adjacent granules from a given sample have very similar compositions and are internally homogeneous. This indicates that the granules are composed of a single mineral of essentially constant composition, consistent with relatively uniform conditions of solution Eh and composition during nontronite formation. The Pb-isotopic composition of the nontronite and Mn-oxide sediments indicates that they were formed from solutions which contained variable proportions of basaltic Pb, introduced into pore waters by basement-derived solutions, and of normal-seawater Pb. However, the Sr-isotopic composition of these sediments is essentially indistinguishable from the value for modern seawater. On the basis of 18O/16O ratios, formation temperatures of ~20–30°C have been estimated for the nontronites. By comparison, temperatures of up to 11.5°C at 9 m depth have been directly measured within the mounds and heat flow data suggest present basement-sediment interface temperatures of 15–25°C.
    Keywords: 70-506; 70-506B; 70-506C; 70-506G; 70-507B; 70-507D; 70-507F; 70-508B; 70-509B; 70-510; Deep Sea Drilling Project; DRILL; Drilling/drill rig; DSDP; Glomar Challenger; Leg70; NOAA and MMS Marine Minerals Geochemical Database; NOAA-MMS; North Pacific; North Pacific/MOUND
    Type: Dataset
    Format: application/zip, 7 datasets
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  • 57
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    PANGAEA
    In:  Supplement to: Lonsdale, Peter; Burns, Virginia Mee; Fisk, Mary B (1980): Nodules of Hydrothermal Birnessite in the Caldera of a Young Seamount on JSTOR. The Journal of Geology, 88(5), 611-618, http://www.jstor.org/stable/30066087
    Publication Date: 2023-08-28
    Description: Manganese nodules made of radiating rods of well crystallized birnessite were sampled at 8 degree 481.2'N, 103 degree 53.8W, 1875 m below sea level by a dredge that also collected hyaloclastite and basaltic talus. The nodule field is on the floor of a caldera within a young tholeiitic seamount and was discovered and photographed during a deep-two survey. It is interpreted as a brecciated hydrothermal deposit, crystallized from an amorphous manganese oxide precipitate that formed when seawater-based hydrothermal fluids mixed with oxidized seawater. The nodules and surrounding igneous rocks have subsequently been encrusted with hydrogenous ferromanganese oxides.
    Keywords: DEEPSONDE; DPSN02-D3; DPSN02-D4; DPSN02-D5; Dredge; DRG; East Pacific Ocean; Indomed_leg_1; INMD-1D; Melville; NOAA and MMS Marine Minerals Geochemical Database; NOAA-MMS; Pacific Ocean; SIQR-4D; SIQUEIROS; Thomas Washington
    Type: Dataset
    Format: application/zip, 2 datasets
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  • 58
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    PANGAEA
    In:  Supplement to: Krishnaswami, Seth; Mangini, Augusto; Thomas, J H; Sharma, P; Cochran, J Kirk; Turekian, Karl K; Parker, P D (1982): 10Be and Th isotopes in manganese nodules and adjacent sediments: Nodule growth histories and nuclide behavior. Earth and Planetary Science Letters, 59(2), 217-234, https://doi.org/10.1016/0012-821X(82)90127-3
    Publication Date: 2023-08-28
    Description: The usefulness of cosmogenic beryllium-10 (half life = 2.5 Ma) for studying the rates of accumulation of ferromanganese nodules is reported based on its measured depth distribution in the top 20 mm of these deposits. Accumulation rates have been obtained in the range of 1 to 4 mm/Ma, which are in good agreement with rates determined using the 230Th method on the same nodules. The use of 10Be offers promise in extending the dating to the outer few cm of the nodules. This contrasts with conventional methods using 230Th and 231Pa isotopes which, due to their comparatively short half lives, are limited to a few mm at the surface of the nodules. Detailed studies of 10Be in the manganese deposits coupled with other trace element analyses should prove valuable in understanding the processes of formation of these deposits and the chronology of events recorded by them.
    Keywords: ARRH-TF; BC; Box corer; DOMES-A47-16; Dredge; DRG; Indian Ocean; NOAA and MMS Marine Minerals Geochemical Database; NOAA-MMS; Oceanographer; Pacific Ocean; RP8OC75; RP8OC75-47-16; Vit 5186; Vityaz (ex-Mars); Vityaz-35; VITYAZ5186
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    Format: application/zip, 2 datasets
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  • 59
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    In:  Supplement to: Humphris, Susan E; Thompson, Robert N; Marriner, Giselle F (1980): The mineralogy and geochemistry of basalt weathering, holes 417A and 418A. In: Donnelly, T.; Francheteau, J.; Bryan, W.; Robinson, P.; Flower, M.; Salisbury, M.; et al., Initial Reports of the Deep Sea Drilling Project, U.S. Government Printing Office, LI, LII, LIII, 1201-1217, https://doi.org/10.2973/dsdp.proc.515253.147.1980
    Publication Date: 2023-08-28
    Description: The successful drilling on Legs 51, 52, and 53 created a rare opportunity to investigate the long-term effects of seawater-rock interactions on the mineralogy and chemistry of basalts erupted on the sea floor. The purpose of this paper is to describe the weathering of the basalts in terms of the changes in their mineralogy and chemistry, and to compare the weathering observed in Hole 418A with that in the upper parts of Hole 417A.
    Keywords: 51-417A; Deep Sea Drilling Project; DRILL; Drilling/drill rig; DSDP; Glomar Challenger; Leg51; NOAA and MMS Marine Minerals Geochemical Database; NOAA-MMS; North Atlantic/CONT RISE
    Type: Dataset
    Format: application/zip, 2 datasets
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  • 60
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    In:  Supplement to: Hekinian, Roger; Rosendahl, Bruce R; Natland, James H (1980): Ocean Crust Geothermal Processes: A Perspective from the Vantage of Leg 54 Drilling. In: Rosendahl, B.R.; Hekinian, R.; et al., Initial Reports of the Deep Sea Drilling Project, U.S. Government Printing Office, VIV, 267-294, https://doi.org/10.2973/dsdp.proc.54.115.1980
    Publication Date: 2023-08-28
    Description: Two distinct sedimentary facies produced by sea-floor hydrothermal activity were cored during Deep Sea Drilling Project Leg 54. The first is equivalent to the typical basal iron- and manganese-rich, clayey mud recovered at many DSDP sites. It was sampled as a dispersed component throughout the cores taken in small sediment ponds in several sites within 120 km of the East Pacific Rise at 9°N. We infer that this component was originally deposited as iron hydroxides dispersed from high-temperature vents over the axial magma chamber of the East Pacific Rise. In the sediments, the iron hydroxides have reacted diagenetically with siliceous microfossil tests and detrital clays to form K- and Fe-rich clays with variable SiO2/Fe2O3 and Fe2O3/Al2O3, ratios.
    Keywords: 54-419; 54-420; 54-421; 54-424; 54-424A; 54-424B; 54-424C; 54-425; 54-427; 54-428; 54-428A; Deep Sea Drilling Project; DRILL; Drilling/drill rig; DSDP; Glomar Challenger; Leg54; NOAA and MMS Marine Minerals Geochemical Database; NOAA-MMS; North Pacific/CONT RISE; North Pacific/MOUND; North Pacific/RIDGE; North Pacific/SEDIMENT POND; North Pacific/TROUGH
    Type: Dataset
    Format: application/zip, 2 datasets
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  • 61
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    In:  Supplement to: Coleman, Max L; Fleet, Andy; Donson, Paul (1982): Preliminary studies of manganese-rich carbonate nodules from Leg 68, Site 503, eastern Equatorial Pacific. In: Prell, WL; Gardner, JV; et al. (eds.), Initial Reports of the Deep Sea Drilling Project (U.S. Govt. Printing Office), 68, 481-489, https://doi.org/10.2973/dsdp.proc.68.123.1982
    Publication Date: 2023-08-28
    Description: Nodules occur in the siliceous calcareous ooze and siliceous marl at Site 503 in the eastern equatorial Pacific. They are present below a depth of about 11 meters throughout the green-colored reduced part of the section down to 228 meters, although they are most abundant between 30 and 85 meters. They are cylindrical or barrel-shaped, up to 70 mm long, and usually have an axial channel through them or are hollow. They appear to have formed around and/or within burrows. XRD studies and microprobe analyses show that they are homogeneous and consist of calcian rhododrosite and minor calcite; Mn is present to the extent of about 30%. Isotopic analyses of the carbonate give carbon values which range from -1.2 per mil to -3.8 per mil, and oxygen isotope compositions vary from +4.0 per mil to +6.0 per mil. These values are different from those for marine-derived carbonates as exemplified by the soft sediment filling of a burrow: d13C, -0.26 per mil; d18O, +1.05 per mil. The carbon isotope data indicate that carbonate derived (possibly indirectly) from seawater was mixed with some produced by organic diagenesis to form the nodules. The d18O values suggest that although they formed near the sediment surface, some modification or the introduction of additional diagenetic carbonate occurred during burial.
    Keywords: 68-503A; 68-503B; Deep Sea Drilling Project; DRILL; Drilling/drill rig; DSDP; Glomar Challenger; Leg68; NOAA and MMS Marine Minerals Geochemical Database; NOAA-MMS; North Pacific/FLANK
    Type: Dataset
    Format: application/zip, 2 datasets
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  • 62
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    In:  Supplement to: MNHN (1980): ANTIPROD II Cruise - MD21, R/V Marion Dufresne, Core list. Muséum National d'Histoire Naturelle, Paris, unpublished, https://geocores.mnhn.fr/index.php?catid=7&blogid=1
    Publication Date: 2023-08-28
    Description: The cores and dredges described at this site were taken on the ANTIPROD II cruise from 21 February to 9 April 1980 by the Muséum National d'Histoire Naturelle from the R/V Marion Dufresne. A total of 10 cores were recovered and are available at MNHN for sampling and study.
    Keywords: ANTIPROD2; Comment; Date/Time of event; Deposit type; Depth, bottom/max; DEPTH, sediment/rock; Depth, top/min; Description; Device type; Elevation of event; Event label; Indian Ocean; Latitude of event; Longitude of event; Marion Dufresne (1972); MD 21-11-GS; MD 21-19-GS; MD-GS800306; MD-GS800309; NOAA and MMS Marine Minerals Geochemical Database; NOAA-MMS; PC; Piston corer; Position; Quantity of deposit; Sample ID; Sediment type; Size
    Type: Dataset
    Format: text/tab-separated-values, 121 data points
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  • 63
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    In:  Supplement to: Morris, R J (1982): RRS Discovery Cruise 128, 2 May - 26 May 1982. Geochemical and biological studies in the Guinea Basin. Institute of Oceanographic Sciences Cruise Report, Wormley, UK, 134, 26 pp pp, https://eprints.soton.ac.uk/id/eprint/14155
    Publication Date: 2023-08-28
    Description: The cores and dredges described in this report were taken on Cruise 128 of the R.R.S. "Discovery" in May 1982 by the National Institute of Oceanography, Wormley, United Kingdom. A total of 12 cores were recovered and are available through the British Oceanographic Data Centre for sampling and study.
    Keywords: Atlantic Ocean; BC; Box corer; D10516; Date/Time of event; Deposit type; DEPTH, sediment/rock; Description; Elevation of event; Latitude of event; Longitude of event; NOAA and MMS Marine Minerals Geochemical Database; NOAA-MMS; Position; Quantity of deposit; Sample ID; Sediment type; Size; Substrate type
    Type: Dataset
    Format: text/tab-separated-values, 8 data points
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  • 64
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    In:  Supplement to: Hoffert, Michel (1980): Les "argiles rouges des grands fonds" dans le Pacifique centre-est: authigenèse, transport, diagenèse (PhD Dissertation). Université Louis Pasteur, Strasbourg, France, 231 pp
    Publication Date: 2023-08-28
    Description: The text studies the deep-sea red clays in the East-Central Pacific ocean (Tahiti-Touamotou Archipelago), their authigenic formation, transport and diagenetic character in particular through their composition in REE.
    Keywords: Aluminium; Boron; Calcium; Chromium; Cobalt; Date/Time of event; Deposit type; DEPTH, sediment/rock; Elevation of event; Gallium; Iron; Latitude of event; Lead; Le Noroit; Longitude of event; Magnesium; Manganese; Molybdenum; NIXO; NOAA and MMS Marine Minerals Geochemical Database; NOAA-MMS; Pacific Ocean; PC; Piston corer; Potassium; Quantum emission spectrography; Sample ID; Scandium; Sediment type; Shape; Silicon; Sodium; Strontium; Titanium; TKS16; TRANSPAC; TRSPC1-KS16; Vanadium; Zinc
    Type: Dataset
    Format: text/tab-separated-values, 23 data points
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  • 65
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    In:  Supplement to: Piepgras, Donald J; Wasserburg, Gerald J (1980): Neodymium isotopic variations in seawater. Earth and Planetary Science Letters, 50(1), 128-138, https://doi.org/10.1016/0012-821X(80)90124-7
    Publication Date: 2023-08-28
    Description: New data for the direct measurement of the isotopic composition of neodymium in Atlantic Ocean seawater are compared with previous measurements of Pacific Ocean seawater and ferromanganese sediments from major ocean basins. Data for Atlantic seawater are in excellent agreement with Nd isotopic measurements made on Atlantic ferromanganese sediments and are distinctly different from the observed compositions of Pacific samples. These results clearly demonstrate the existence of distinctive differences in the isotopic composition of Nd in the waters of the major ocean basins and are characteristic of the ocean basin sampled. The average eNd(0) values for the major oceans as determined by data from seawater and ferromanganese sediments are as follows: Atlantic Ocean, eNd(0) = -12 ± 2; Indian Ocean, eNd(0) = -8 ± 2; Pacific Ocean, eNd(0) = -3 ± 2. These values are considerably less than eNd(0) value sources with oceanic mantle affinities indicating that the REE in the oceans are dominated by continental sources. The difference in the absolute abundance of 143Nd between the Pacific and Atlantic Oceans corresponds to ab. 10**6 atoms 143Nd per gram of seawater. The correspondence between the 143Nd/144Nd in seawater and in the associated sediments suggests the possible application of this approach to paleo-oceanography. Distinctive differences in eNd(0) values are observed in the Atlantic Ocean between deep-ocean water associated with North Atlantic Deep Water and near-surface water. This suggests that North Atlantic Deep Water may be relatively well mixed with respect to Nd isotopic composition whereas near-surface water may be quite heterogeneous, reflecting different sources for surface waters relative to deep water. This suggests that it may be possible to distinguish the sources of water masses within an ocean basin on the basis of Nd isotopic composition. The Nd isotopic variations in seawater are used to relate the residence time of Nd and mixing rates between the oceans.
    Keywords: Calculated; Deposit type; DEPTH, sediment/rock; Description; DISTANCE; Distance, maximum; Distance, minimum; Dredge; DRG; Identification; L-10-76-HW; L1076HW-9A; Neodymium-143/Neodymium-144 ratio; Neodymium-143/Neodymium-144 ratio, standard deviation; NOAA and MMS Marine Minerals Geochemical Database; NOAA-MMS; Pacific Ocean; Sample code/label; Samuel P. Lee; ε-Neodymium; ε-Neodymium, standard deviation
    Type: Dataset
    Format: text/tab-separated-values, 20 data points
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  • 66
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    In:  Supplement to: Pawson, D L (1982): Deep-sea echinoderms in the Tongue of the Ocean, Bahama Islands: a survey, using the research submersible Alvin. Australian Museum Memoir, 16, 129-145, https://doi.org/10.3853/j.0067-1967.16.1982.362
    Publication Date: 2023-08-28
    Description: Deep-sea echinoderms of the Tongue of the Ocean, Bahama Islands, have been studied, using trawled collections made by the University of Miami together with observations from the deep submersible Alvin. Transect runs in the submersible permitted studies of population densities and behaviour of approximately 38 species of larger invertebrates, of which 27 were echinoderms. Several echinoderm species show a patchy distribution pattern which is apparently not related to available food resources. Some species are exclusively herbivores, feeding on fragments of turtle grass, Thalassia testudinata and sargassum weed, Sargassum spp. Feeding habits of some Tongue of the Ocean echinoderms are compared with those of the same species from further north, where supplies of plant material are not nearly so abundant.
    Keywords: ALV703; ALV-703; Alvin; Comment; Deposit type; DEPTH, sediment/rock; Description; File name; Grab; GRAB; Identification; NOAA and MMS Marine Minerals Geochemical Database; NOAA-MMS; Position; Quantity of deposit; Sediment type; Substrate type; Tongue of the Ocean; Uniform resource locator/link to image; Visual description
    Type: Dataset
    Format: text/tab-separated-values, 10 data points
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  • 67
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    In:  Supplement to: Donnelly, Thomas W; Francheteau, Jean; Bryan, Wilfred B; Robinson, Paul T; Flower, Martin F J; Salisbury, Matthew H (1980): Initial Reports of the Deep Sea Drilling Project. Deep Sea Drilling Project, U.S. Government Printing Office, LI, LII, LIII, 1597 pp, https://doi.org/10.2973/dsdp.proc.515253.1980
    Publication Date: 2023-08-28
    Description: The JOIDES Paleoenvironment Panel had noted that the Neogene section had only been spot-cored on previous legs in the Western Atlantic (Legs 1, 2, 4, 11, and 43). The Panel accordingly requested that the complete section be recovered on Legs 51 through 53 in order to examine the transition from siliceous, Pacific-type Eocene sedimentation to non-siliceous sedimentation resulting from the gradual emergence of the Central American isthmus. It was also detremined to examine in detail the thick Cretaceous-Tertiary section overlying the basement.
    Keywords: 51-417A; 51-417D; 52-418A; 53-418B; Comment; Deep Sea Drilling Project; Deposit type; DEPTH, sediment/rock; Description; DRILL; Drilling/drill rig; DSDP; Event label; Glomar Challenger; Identification; Leg51; Leg52; Leg53; NOAA and MMS Marine Minerals Geochemical Database; NOAA-MMS; North Atlantic/CONT RISE; Position; Quantity of deposit; Sample code/label; Sediment type; Substrate type; Visual description
    Type: Dataset
    Format: text/tab-separated-values, 208 data points
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  • 68
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    In:  Supplement to: Schrader, Ed L; Furbish, William J; Mattey, David P; May, J A (1980): Geochemistry and Carbonate Petrology of Selected Sediment Samples from Deep Sea Drilling Project Leg 54, Eastern Pacific. In: Rosendahl, B.R.; Hekinian, R.; et al., Initial Reports of the Deep Sea Drilling Project, U.S. Government Printing Office, LIV, 319-328, https://doi.org/10.2973/dsdp.proc.54.110.1980
    Publication Date: 2023-08-28
    Description: Thirty selected samples of pelagic and hydrothermal sediments retrieved on DSDP Leg 54 were chemically analyzed for major and minor oxide concentrations. Additionally, 11 samples of lithified carbonate sediments were petrologically studied. The pelagic sediments, which are described as foraminiferal biomicrite, were found to be generally higher in Fe and Zn, similar in Co content, and lower in Cu content, than the average Pacific pelagic sediments. Mineralogically, these samples are composed principally of calcite with minor amounts of quartz and clays. Hydrothermal sediments from Site 424 are divisible into three classes: (1) silica-rich, iron-poor smectites; (2) silica-poor, iron-rich mixtures of smectites and oxides; and (3) silica-poor, iron-rich materials, comprising mainly amorphous manganese oxides. Thus, two chemically distinct hydrothermal phases are recognizable: Class 1, iron-rich smectites, and Class 3, Mn-rich oxides and oxyhydroxides. Dolomite and pyrite were identified in X-ray diffraction studies of samples from Site 427.
    Keywords: 54-419; 54-420; 54-424; 54-424A; 54-427; Atomic absorption spectrometry (AAS); Cobalt; Copper; Deep Sea Drilling Project; Deposit type; DEPTH, sediment/rock; DRILL; Drilling/drill rig; DSDP; Event label; Glomar Challenger; Identification; Iron; Leg54; Manganese; Molybdenum; NOAA and MMS Marine Minerals Geochemical Database; NOAA-MMS; North Pacific/MOUND; North Pacific/SEDIMENT POND; North Pacific/TROUGH; Sediment type; X-ray fluorescence (XRF); Zinc
    Type: Dataset
    Format: text/tab-separated-values, 99 data points
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  • 69
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    In:  Supplement to: Lonsdale, Peter; Spiess, Fred N (1980): Deep-Tow Observations at the East Pacific Rise, 8°45'N, and Some Interpretations. In: Rosendahl, B.R.; Hekinian, R.; et al., Initial Reports of the Deep Sea Drilling Project, U.S. Government Printing Office, LIV, 43-62, https://doi.org/10.2973/dsdp.proc.54.104.1980
    Publication Date: 2023-08-28
    Description: A near-bottom survey of a 24-km length of the East Pacific Rise (EPR) crest near the Leg 54 drill sites has established that the axial ridge is a 12- to 15-km-wide lava plateau, bounded by steep 300-meter-high slopes that in places are large outward-facing fault scarps. The plateau is bisected asymmetrically by a 1- to 2-km-wide crestal rift zone, with summit grabens, pillow walls, and axial peaks, which is the locus of dike injection and fissure eruption. About 900 sets of bottom photos of this rift zone and adjacent parts of the plateau show that the upper oceanic crust is composed of several different types of pillow and sheet lava. Sheet lava is more abundant at this rise crest than on slow-spreading ridges or on some other fastspreading rises. Beyond 2 km from the axis, most of the plateau has a patchy veneer of sediment, and its surface is increasingly broken by extensional faults and fissures. At the plateau's margins, secondary volcanism builds subcircular peaks and partly buries the fault scarps formed on the plateau and at its boundaries. Another deep-tow survey of a patch of young abyssal hills 20 to 30 km east of the spreading axis mapped a highly lineated terrain of inactive horsts and grabens. They were created by extension on inward- and outwardfacing normal faults, in a zone 12 to 20 km from the axis. Sediments sampled on the rise crest and flanks are mixtures of calcareous ooze and metalliferous precipitates, and they have been redistributed by southerly currents with average velocities of 9 cm/s.
    Keywords: Deposit type; DEPTH, sediment/rock; Description; East Pacific Ocean; Event label; File name; Identification; Indomed_leg_1; INMD-3-2C; INMD-3-7C; INMD-4-1C; INMD-4-3C; Melville; NOAA and MMS Marine Minerals Geochemical Database; NOAA-MMS; Photo/Video; Position; PV; Quantity of deposit; Sediment type; Size; Uniform resource locator/link to image; Visual description
    Type: Dataset
    Format: text/tab-separated-values, 35 data points
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  • 70
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    In:  Supplement to: Lonsdale, Peter; Bischoff, James L; Burns, Virginia Mee; Kastner, Miriam; Sweeney, Colm (1980): A high-temperature hydrothermal deposit on the seabed at a gulf of California spreading center. Earth and Planetary Science Letters, 49(1), 8-20, https://doi.org/10.1016/0012-821X(80)90144-2
    Publication Date: 2023-08-28
    Description: A submersible dive on a turbidite-covered spreading axis in Guaymas Basin photographed and sampled extensive terraces and ledges of talc. The rock contains siliceous microfossils, smectite, and euhedral pyrrhotite as well as rather pure iron-rich talc. Sulfur and oxygen isotopes indicate precipitation around a hydrothermal vent, at about 280°C.
    Keywords: CDRILL; Core drilling; Deposit type; DEPTH, sediment/rock; Description; Dive 308; DSV477; DSV477-308-1; DSV477-308-3; DSV-4 Seacliff; Event label; File name; Guaymas Basin, Gulf of California; Identification; NOAA and MMS Marine Minerals Geochemical Database; NOAA-MMS; Photo/Video; Position; PV; Quantity of deposit; Sediment type; Substrate type; Uniform resource locator/link to image; Visual description
    Type: Dataset
    Format: text/tab-separated-values, 18 data points
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  • 71
    Publication Date: 2023-08-28
    Description: Leg 55 was conceived as part of the decade-long experiment to test the kinematic hot-spot hypothesis and several of its more imporant corollaries for the origin of the Hawaiian-Emperor chain. Also of particular importance was the question of whether the Hawaiian hot spot has remained fixed in the mantle. The specific primary objectives of Leg 55, were to determine (1) whether the known increase in the age of the volcanoes on the Hawaiian chain with distance from Kilauea continues northward along the Emperor Seamounts; (2) whether the lavas of the Emperor volcanoes are of the same chemical composition and were erupted in the same sequence as those of Hawaiian volcanoes; (3) the latitude of formation of Suiko Seamount as a test of hot-spot fixity; and (4) whether the Emperor Seamounts were once islands and, if so, to determine their post-volcanic and subsidence history.
    Keywords: 55-430; 55-431; 55-431A; 55-432; Comment; Deep Sea Drilling Project; Deposit type; DEPTH, sediment/rock; Description; DRILL; Drilling/drill rig; DSDP; Event label; File name; Glomar Challenger; Identification; Leg55; NOAA and MMS Marine Minerals Geochemical Database; NOAA-MMS; North Pacific/SEDIMENT POND; North Pacific/TERRACE; Position; Quantity of deposit; Sample code/label; Sediment type; Size; Substrate type; Uniform resource locator/link to image; Visual description
    Type: Dataset
    Format: text/tab-separated-values, 196 data points
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  • 72
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    In:  Supplement to: Mullins, Henry T; Keller, G H; Kofoed, John; Lambert, D N; Stubblefield, W L; Warme, J E (1982): Geology of Great Abaco Submarine Canyon (Blake Plateau): Observations from the research submersible “Alvin”. Marine Geology, 48(3-4), 239-257, https://doi.org/10.1016/0025-3227(82)90099-8
    Publication Date: 2023-08-28
    Description: Scientists from the Woods Hole Oceanographic Institution, the U.S. Navy, the State University of New York at Albany, Wesleyan University, Nine dives in the research submersible ?Alvin? were made into Great Abaco Submarine Canyon to depths ranging from 1850 to 3666 m. Our observations indicate that the walls of this canyon are distinctly terraced, consisting of nearly vertical to overhanging rock cliffs and intervening, less steep sediment-covered slopes. The wall rock consists mostly of massive, shallow-water limestones and dolostones of Cretaceous age, coated on exposed surfaces with manganese oxides. These rocks are heavily jointed/fractured and thus very blocky to angular in appearance, with sponges and other sessile organisms commonly attached. Talus slopes and sedimentary breccia deposits containing angular boulders are present at the base of these steep escarpments. Short-term bottom current measurements in the axis of the eastern part of the canyon indicate that currents are relatively weak, reaching velocities of only 10 cm/sec. This relatively placid setting is further corroborated by the abundance of turtle grass (Thalassia) found along the canyon axis. However, abundant subdued, symmetrical ripple marks and large scour depressions at the base of boulders, indicate that high-energy events sporadically impact the canyon axis. Contemporary erosional activity along the axis of the western (headward) part of the canyon appears to be more significant, as evidenced by asymmetrical ripple marks, sand waves and bioerosion. Great Abaco Canyon has evolved with time via a variety of processes, including: (1) faulting: (2) subsidence; (3) defacement; and (4) erosional down-cutting. The location, orientation and initiation of this canyon appear to be structurally controlled by the Great Abaco Fracture Zone during pre-Santonian time. Regional subsidence during the Mesozoic allowed the walls of Great Abaco Canyon to build vertically by accretion of shallow-water limestones, whereas joint-controlled defacement has widened the canyon while maintaining steep walls. Erosional down-cutting in the canyon axis by carbonate sediment gravity flows also appears to have been important episodically, particularly during the Miocene and Pleistocene.
    Keywords: ALV570; ALV570-1C; ALV570-2C; ALV756; ALV756-1D; Alvin; Blake Plateau, Atlantic Ocean; Deposit type; DEPTH, sediment/rock; Description; Event label; File name; Grab; GRAB; Identification; NOAA and MMS Marine Minerals Geochemical Database; NOAA-MMS; Photo/Video; Position; PV; Quantity of deposit; Sediment type; Substrate type; Uniform resource locator/link to image; Visual description
    Type: Dataset
    Format: text/tab-separated-values, 25 data points
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  • 73
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    In:  Supplement to: Bonatti, Enrico; Lawrence, James R; Hamlyn, P R; Breger, Dee (1980): Aragonite from deep sea ultramafic rocks. Geochimica et Cosmochimica Acta, 44(8), 1207-1214, https://doi.org/10.1016/0016-7037(80)90074-5
    Publication Date: 2023-08-28
    Description: Aragonite mineralization was observed in serpentinized peridotites from the Romanche and Vema Fracture Zones in the Atlantic and the Owen Fracture Zone in the Indian Ocean, either in veins or as radial aggregates in cavities within the serpentinites. Evidence of incipient dissolution of the aragonite crystals was observed in one case. The aragonites tend to have lower Mg content (〈 0.03%) and higher Sr content (〉 0.95%) relative to other marine aragonites. Their 18O16O, 13C12C and 87Sr86Sr isotopic ratios suggest the aragonite was deposited at ocean floor temperatures from solutions derived from sea water circulating in fissures and fractures within the ultramafic rocks. The 18O16O ratios of the serpentines indicate serpentinization occurred at higher temperatures, probably deeper in the crust. Low-T reactions between circulating seawater and Mg-silicates (primarily serpentine and pyroxenes) caused high pH and enrichment of Mg and Ca in the solution, conditions favoring carbonate precipitation. Aragonite was formed rather than calcite presumably because the high Mg2+ concentration in the solution inhibited calcite precipitation. The high Sr content of the aragonites is probably related, at least in part, to their low temperature of formation. Opaque mineral grains containing over 8% NiO and over 40% MnO were observed concentrated along the margins of some of the aragonite veins, suggesting that Ni is one of the elements mobilized during reactions between ultramafic rocks and circulating seawater.
    Keywords: Aluminium oxide; Calcium oxide; Deposit type; DEPTH, sediment/rock; Description; Dredge; DRG; Electron microprobe (EMP); G-7309; G-7309-81; Gerda; Identification; Iron oxide, FeO; Magnesium oxide; Manganese oxide; Nickel oxide; NOAA and MMS Marine Minerals Geochemical Database; NOAA-MMS; Potassium oxide; Romanche Fracture Zone, Atlantic Ocean; Sample code/label; Silicon dioxide; Sodium oxide; Substrate type
    Type: Dataset
    Format: text/tab-separated-values, 14 data points
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  • 74
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    In:  Supplement to: deVries Klein, George; Kobayashi, Kazuo; White, Stan (1980): Initial Reports of the Deep Sea Drilling Project. U.S. Government Printing Office, LVIII, 1013 pp, https://doi.org/10.2973/dsdp.proc.58.1980
    Publication Date: 2023-08-28
    Description: The JOIDES Active Margin Panel for Leg 58 decided that the drilling would occur in the north Philippine Sea, namely, the Shikoku Basin, the Daito Ridge and Basin province. The Shikoku Basin sites were selected to solve several problems concerning back-arc basins formed by ocean-floor spreading. The main objectives were: (1) to determine the age of the oldest sediment, so as to calibrate magnetic-anomaly ages and to provide a test for various spreading models suggested for the basin; (2) to investigate the mineralogy, petrology, and chemistry of basalt samples recovered by drilling, and to compare there basalts with those of midocean ridges, so as to understand the nature and source of magmatic materials in these basins; (3) to determine the distribution of sediment types in time, and to relate that distribution to the tectonic history of the basin.
    Keywords: 58-442A; 58-442B; 58-443; 58-444; 58-445; 58-446; 58-446A; Comment; Deep Sea Drilling Project; Deposit type; DEPTH, sediment/rock; Description; DRILL; Drilling/drill rig; DSDP; Event label; Glomar Challenger; Identification; Leg58; NOAA and MMS Marine Minerals Geochemical Database; NOAA-MMS; North Pacific/BASIN; North Pacific/Philippine Sea/BASIN; Position; Quantity of deposit; Sample code/label; Sediment type; Size; Substrate type; Visual description
    Type: Dataset
    Format: text/tab-separated-values, 301 data points
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  • 75
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    PANGAEA
    In:  Supplement to: Wories, Henk; Whelan, Jean K; Thompson, Peter R; Sakai, Toyusaburo; Robinson, Paul T; Pisciotto, Kenneth A; Murdmaa, Ivar O; Müller, German; Kurnosov, Victor B; Harper, Howard E; Bruns, T; Adelseck, C; Langseth, Marcus G; Okada, Hakuyu (1980): Initial Reports of the Deep Sea Drilling Project. U. S. Government Printing Office, LVI, 436 pp, https://doi.org/10.2973/dsdp.proc.5657.1980
    Publication Date: 2023-08-28
    Description: The Japan Trench area was identified a favorable place for studying convergent margins during the initial deliberations of the IPOD Active Margins Panel. The Leg 56-57 DSDP drill sampling along the Japan Trench transect has indicated that material tectonically accreted during the present convergent episode is limited to a surprisingly small zone. The limits seem well established by the seaward extent of crust with continental thickness and lithologies and by the age and thickness of a terrigenous slope apron covering the presumed but probably unsampled accreted oceanic material.
    Keywords: 56-434B; 56-436; Comment; Deep Sea Drilling Project; Deposit type; DEPTH, sediment/rock; Description; DRILL; Drilling/drill rig; DSDP; Event label; File name; Glomar Challenger; Identification; Leg56; NOAA and MMS Marine Minerals Geochemical Database; NOAA-MMS; North Pacific/RIDGE; North Pacific/TRENCH; Position; Quantity of deposit; Sample code/label; Sediment type; Substrate type; Uniform resource locator/link to image; Visual description
    Type: Dataset
    Format: text/tab-separated-values, 77 data points
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  • 76
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    PANGAEA
    In:  Supplement to: Dalrymple, G Brent; Garcia, M O (1980): Age and Chemistry of Volcanic Rocks Dredged from JingƄ Seamount, Emperor Seamount Chain. In: Jackson, E.D.; Koisumi, I.; et al., Initial Reports of the Deep Sea Drilling Project, U.S. Government Printing Office, LV, 685-693, https://doi.org/10.2973/dsdp.proc.55.130.1980
    Publication Date: 2023-08-28
    Description: 40Ar/39Ar incremental heating experiments on three samples dredged from Jingu Seamount indicate that Jingu is 55.4 ± 0.9 m.y. old — older than the Hawaiian-Emperor bend and younger than the two dated Emperor Seamounts to the north. Major-oxide chemistry and petrography show that the samples are similar to hawaiites and mugearites from the Hawaiian Islands. By analogy with Hawaiian alkalic volcanic rocks, groundmass plagioclase compositions (An40-47) indicate that the three Jingu samples are probably mugearites. These results suggest that Jingu is a Hawaiian-type volcano and that the Emperor volcanoes become progressively older from south to north, as predicted by the hot-spot hypothesis.
    Keywords: Deep Sea Drilling Project; Deposit type; DEPTH, sediment/rock; Description; Dredge; DRG; DSDP; Identification; Kana Keoki; KK760806; KK760806-01,KK760806-02,KK76; KK760806-2 STA24 RD10; KK760806-RD10; NOAA and MMS Marine Minerals Geochemical Database; NOAA-MMS; Pacific Ocean; Position; Quantity of deposit; Sediment type; Size; Substrate type; Visual description
    Type: Dataset
    Format: text/tab-separated-values, 8 data points
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  • 77
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    PANGAEA
    In:  Supplement to: Sharaskin, Anatoly; Packham, G H; Natland, James H; Nakamura, K; Meijer, Arend; Kling, Stanley; Horai, Ki-Iti; Francis, T J G; Ellis, C Howard; Bleil, Ulrich; Blanchet, R; Hussong, Donald M; Uyeda, Seiya (1982): Initial Reports of the Deep Sea Drilling Project. Initial Reports of the Deep Sea Drilling Project, U.S. Government Printing Office, LX, 929 pp, https://doi.org/10.2973/dsdp.proc.60.1982
    Publication Date: 2023-08-28
    Description: Two consecutive drilling legs (Legs 59 and 60) were assigned to drill an east-west transect of sites along latitude 18°N, from the Mariana Basin of the Pacific Ocean to the oldest inactive island arcs and back-arc spreading basins of the Philippine Sea. The western (older, inactive) half of this transect (Philippine Sea, Palau-Kyushu Ridge, Parece Vela Basin, and the West Mariana Ridge-Sites 447-451) was drilled during Leg 59. The objective of Leg 60 was to sample the tectonically active eastern portion of the transect in a closely spaced series of holes across the presently opening back-arc basin (Mariana Trough, Site Survey Target SP-4: Sites 453-456), the Mariana arc itself (Site Survey Target SP-3b: Site 457), the Mariana fore-arc region (Site Survey Target SP-3, Sites 458 and 459), and deep within the Mariana Trench (Site Survey Target SP-2: Sites 460 and 461). In addition, one site (Site Survey Target SP-1: Site 452) was drilled on the Pacific plate seaward of the trench to obtain a reference section of sediments and oceanic crust being delivered to the trench.
    Keywords: 60-452; 60-452A; 60-453; 60-454; 60-454A; 60-456; 60-456A; 60-458; 60-459B; 60-460; 60-460A; 60-461; 60-461A; Comment; Deep Sea Drilling Project; Deposit type; DEPTH, sediment/rock; Description; DRILL; Drilling/drill rig; DSDP; Event label; Glomar Challenger; Identification; Leg60; NOAA and MMS Marine Minerals Geochemical Database; NOAA-MMS; North Pacific/BASIN; North Pacific/SEDIMENT POND; North Pacific/TRENCH; Position; Quantity of deposit; Sample code/label; Sediment type; Size; Substrate type; Visual description
    Type: Dataset
    Format: text/tab-separated-values, 555 data points
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  • 78
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    PANGAEA
    In:  Supplement to: Juteau, Thierry; Eissen, Jean-Philippe; Francheteau, Jean; Needham, David; Choukroune, P; Rangin, Claude; Séguret, Marie J M; Ballard, R D; Fox, P J; Normark, William R; Carranza, A; Cordoba, D; Guerrero, J (1980): Homogeneous basalts from the East Pacific Rise at 21° N: seady state magma reservoirs at moderately fast spreading centers. Oceanologica Acta, 3(4), 487-503, https://archimer.ifremer.fr/doc/00323/43430/
    Publication Date: 2023-08-28
    Description: Forty basaltic rocks collected by submersible during the Cyamex expedition (1978) on the East PacifIc Rise at 21°N, a moderately fast spreading segment (6 cm/year opening rate) of the mid-ocean ridge, consist of angular pillow fragments and glass buds, sheet-flow slabs and samples of columnar pillars standing in collapsed fossillava pools. Most of the rocks are from the crestal are a of the Rise. The collection shows a striking petrographic homogeneity wh en compared with the range of basalts found on other segments of midocean ridges: olivine-phyric, or highly plagioclase-phyric rocks, so common in the slowspreading Famous are a in the Atlantic, are absent. All samples are typical lowpotassium oceanic tholeiites with a limited fractionation trend. Pillow-lavas, thin and thick sheet-flows cannot be distinguished by their major element compositions, as in the Galapagos rift which has the same spreading rate as the EPR at 21°N. Further, ferrobasalts have been described from the Galapagos rift, but do not appear in the Cyamex rocks. In the Cyamex area, olivine and plagioclase are the main silicate phases, and clinopyroxene is absent. In the pillows and sheet-flow samples, four generations of olivine and plagioclase crystals are distinguished. Samples from the fossillava pools are aphyric. The corresponding magma batches are presumed to have migrated rapidly through the magma chamber, and to have been extruded in large volumes, possibly during episodes ofhigh instantaneous opening rate. Fe-Ni and Fe-Cu-rich sulphide phases are common in an lava types as massive globules scatterred through the glass, or as microglobules decorating the walls of empty vesicles. Palagonite and Fe-Mn oxide thicknesses across the strike of the Rise indicate relative ages compatible with successive extrusions at the Rise axis.
    Keywords: CY-78-07-12D; CY-78-10-17D; CY-78-10-18D; CY-78-11-26D; CY-78-12-35D; CY-78-13-42D; CY-78-13-43D; CY-78-13-44D; CY-78-15-55D; CY-78-15-56D; CY-78-16-57D; CY-78-16-58D; CY-78-17-60D; CY-78-17-61D; CY-78-18-63D; CY-78-18-65D; CY-78-18-66D; CY-78-19-69D; CY-78-20-76D; CYAMEX; Cyana (Submersible); Deposit type; DEPTH, sediment/rock; Description; East Pacific Rise; Elevation of event; Event label; Identification; Latitude of event; Longitude of event; NOAA and MMS Marine Minerals Geochemical Database; NOAA-MMS; Percentage; Position; ROBA; Robotic arm; Sediment type; Substrate type; Visual description
    Type: Dataset
    Format: text/tab-separated-values, 108 data points
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  • 79
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    PANGAEA
    In:  Supplement to: Vacquier, Victor; Simoneit, Bernd R T; Schrader, Hans-Jürgen; Saunders, Andrew D; Rueda-Gaxiola, Jaime; Niemitz, Jeffrey W; Molina-Cruz, Adolfo; Matoba, Y; Lyle, Mitchell W; Kelts, Kerry; Kastner, Miriam; Guerrero-Garcia, Jose; Gieskes, Joris M; Fornari, Daniel J; Einsele, Gerhard; Aubry, Marie-Pierre; Aguayo, J Eduardo; Curray, Joseph R; Moore, David G (1982): Initial Reports of the Deep Sea Drilling Project. U.S. Government Printing Office, LXIV, 507 pp + 1303 pp, https://doi.org/10.2973/dsdp.proc.64.1982
    Publication Date: 2023-08-28
    Description: The origin and evolution of passive continental margins are of great scientific interest and economic importance. During DSDP Leg 64 the Glomar Challenger drilled at eight sites (474-481) in the Gulf of California region. The Gulf of California presented a singular example of tectonics and sedimentation in a very young ocean, being formed by translation and oblique rifting. The sedimentation of the region is hemipelagic, rapid, and largely dominated by siliceous microfossils.Sites 474, 475, and 476 form a transect from oceanic crust to continental crust at the southern tip of Baja California in order to define passive-margin subsidence during the early post-rifting phase. Sites 477, 478, and 481 investigate of the nature of young ocean crust in the Guaymas Basin, where high accumulation rates are common and variable high heat flow indicates active rifting and hydrothermal activity. Sites 479 and 480, are situated on the Guaymas Basin Slope above the proto-Gulf sequences. Interest focused on the paleoceanography of laminated, homogeneous diatom-rich, anoxic sediments within the zone of low oxygen.
    Keywords: 64-474; 64-474A; 64-475; 64-479; 64-480; 64-481A; Comment; Deep Sea Drilling Project; Deposit type; DEPTH, sediment/rock; Description; DRILL; Drilling/drill rig; DSDP; Event label; Glomar Challenger; Identification; Leg64; NOAA and MMS Marine Minerals Geochemical Database; NOAA-MMS; North Pacific/Gulf of California/BASIN; North Pacific/Gulf of California/SLOPE; Position; Quantity of deposit; Sample code/label; Sediment type; Substrate type; Visual description
    Type: Dataset
    Format: text/tab-separated-values, 150 data points
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  • 80
    Publication Date: 2023-08-28
    Description: Leg 66 was part of two broader investigations of subduction complexes and convergent margin geology, one led by the Active Margin Panel (AMP) of the International Phase of Ocean Drilling (IPOD) to drill selected convergent margins to elucidate structure and evolution and the other, led by the University of Texas Marine Science Instituted (UTMSI) Galveston Geophysical Laboratory (GGL) to investigate the tectonics of the Middle America Trench from the Cocos Fracture Zone to the Riviera Fracture Zone. In this context, the specific objective at Site 487 was the coring of pelagic and hemipelagic sediment section and underlying oceanic basement. It is the farthest offshore site off the Cocos Fracture Zone.
    Keywords: 66-487; Comment; Deep Sea Drilling Project; Deposit type; DEPTH, sediment/rock; Description; DRILL; Drilling/drill rig; DSDP; Glomar Challenger; Identification; Leg66; NOAA and MMS Marine Minerals Geochemical Database; NOAA-MMS; North Pacific/TRENCH; Position; Quantity of deposit; Sample code/label; Sediment type; Visual description
    Type: Dataset
    Format: text/tab-separated-values, 24 data points
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  • 81
    Publication Date: 2023-08-28
    Description: The Oaxaca transect, located off southern Mexico and drilled during Leg 66, sampled a truncated margin and subduction complex. In contrast, the Guatemala transect was selected because accretion was thought to have continued in this area during most of the Tertiary. Site surveys conducted by the University of Texas Marine Science Institute provided multichannel seismic records, among which profile GUA-13 was chosen as the location for Leg 67 drill holes. Selection of this transect arises in part from the fact that it includes a portion of the San José Canyon, thus layers of hemipelagic drape may have been stripped away by erosion, allowing quicker access to deep horizons. By studying the continental margin off Guatemala it was hoped to strengthen the tie between offshore and onshore geology, to describe the stratigraphic sequence from the continental slope to the subducting oceanic plate beneath, to recover in ash layers a record of Central American volcanism.
    Keywords: 67-495; 67-496; 67-497; 67-499; 67-499B; 67-499C; 67-500; Comment; Deep Sea Drilling Project; Deposit type; DEPTH, sediment/rock; Description; DRILL; Drilling/drill rig; DSDP; Event label; Glomar Challenger; Identification; Leg67; NOAA and MMS Marine Minerals Geochemical Database; NOAA-MMS; North Pacific/SLOPE; North Pacific/TRENCH; Position; Quantity of deposit; Sample code/label; Sediment type; Substrate type; Visual description
    Type: Dataset
    Format: text/tab-separated-values, 116 data points
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  • 82
    Publication Date: 2023-08-28
    Description: The general objectives of this cruise were to use the newly developed HPC to recover two undisturbed, continuous records of the late Neogene and Quaternary, one from the western Caribbean and the other from the eastern equatorial Pacific, and to test the coring capabilities of the HPC. At site 502 in the Caribbean an hemipelagic facies with accumulation rates of about 3 cm/k.y near site 154 were a coarse-grained volcanogenic turbidite sequence had been recovered at a depth equivalent to a strong seismic reflector. Site 503 was located as close as possible to previously rotary-drilled Site 83 in the eastern equatorial Pacific.
    Keywords: 68-502; 68-502A; 68-502B; 68-503; 68-503A; 68-503B; Caribbean Sea/RIDGE; Comment; Deep Sea Drilling Project; Deposit type; DEPTH, sediment/rock; Description; DRILL; Drilling/drill rig; DSDP; Event label; File name; Glomar Challenger; Identification; Leg68; NOAA and MMS Marine Minerals Geochemical Database; NOAA-MMS; North Pacific/FLANK; Position; Quantity of deposit; Sample code/label; Sediment type; Size; Substrate type; Uniform resource locator/link to image; Visual description
    Type: Dataset
    Format: text/tab-separated-values, 224 data points
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  • 83
    Publication Date: 2023-08-28
    Description: The recovery of hydrothermal sediments at depth beneath the mounds of hydrothermal origin during a brief period of drilling on Deep Sea Drilling Project (DSDP) Leg 54 provided some evidence suggesting that hydrothermal material may be pervasive over a relatively large region inclusive of the mounds but also incorporating adjacent seafloor presently covered by pelagic sediments. As a result of the incomplete recovery of sediments at some sites and the poor recovery of basement rocks during Leg 54, it was suggested that a more carefully planned program be designed to drill a broader range of sites in the Galapagos mounds field. The major objectives of the first part of Leg 70 were to collect data and sediment representative of the hydrothermal mounds and ridges located about 20 km south of the Galapagos spreading axis.
    Keywords: 70-506; 70-506B; 70-506C; 70-507C; 70-507D; 70-507F; 70-509; 70-509B; Comment; Deep Sea Drilling Project; Deposit type; DEPTH, sediment/rock; Description; DRILL; Drilling/drill rig; DSDP; Elevation of event; Event label; File name; Glomar Challenger; Identification; Latitude of event; Leg70; Longitude of event; NOAA and MMS Marine Minerals Geochemical Database; NOAA-MMS; North Pacific/MOUND; Position; Quantity of deposit; Sample code/label; Sediment type; Size; Substrate type; Uniform resource locator/link to image; Visual description
    Type: Dataset
    Format: text/tab-separated-values, 428 data points
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  • 84
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    PANGAEA
    In:  Supplement to: Curray, Joseph R; Moore, David G; Kelts, Kerry; Einsele, Gerhard (1982): Tectonics and Geological History of the Passive Continental Margin at the Tip of Baja California. In: Curray, J.R.; Moore, D.G.; et al., Initial Reports of the Deep Sea Drilling Project, U.S. Government Printing Office, LXIV, 1089-1136, https://doi.org/10.2973/dsdp.proc.64.150.1982
    Publication Date: 2023-08-28
    Description: he three-site Leg 64 Deep Sea Drilling transect at the tip of the Peninsula of Baja California straddled the transition from continental to oceanic crust. The outer site, 474, penetrated mainly mud turbidites and bottomed in "middle" Pliocene oceanic crust about 3 m.y. old. Two sites on the lower continental slope penetrated hemipelagic muddy sediments, a thin section of low-oxygen, phosphoritic, and glauconitic sediments, and a metamorphic cobble conglomerate; one of the sites, 476, bottomed in deeply weathered granite. The oldest marine sediments at this site are early Pliocene, about 4.5 m.y. old. Depth indicators in these holes suggest that all sites were in almost 1000 meters of water by the time oceanic crust was first generated and sea-floor spreading began. Block faulting, subsidence, and deposition of marine sediments on continental crust had preceded the start of sea-floor spreading. Close examination of lineated magnetic anomalies demonstrates that the transition from continental to oceanic crust in this region is diachronous, as early as 4.9 m.y. in some places, but as young as 3.2 m.y. along the line of the transect. We propose a geological history scenario which involves termination of subduction along the western margin of Baja California at 12.5 Ma, a period of transform motion between the Pacific and North American plates along the Tosco Abreojos Transform Fault zone along the west side of Baja California, and a jump of the Pacific-North American plate edge to the alignment of the Gulf at 5.5 Ma. Between 5.5 Ma and about 3.2 Ma, separation of the blocks occurred locally by sea-floor spreading, but elsewhere by "diffuse extension", largely involving listric normal faulting and thinning of the continental crust, accompanied by subsidence and marine inundation. Thus, the plate edge system in the mouth and southern part of the Gulf evolved as early as 5.5 Ma, but the transition from rifting to drifting was diachronous, starting only 3.2 Ma along the line of the transect.
    Keywords: Argo; BAC-17; BAC-44; BAC-58; BAC-59; BAC-61; BACANYON; Deposit type; DEPTH, sediment/rock; Description; Dredge; DRG; Elevation of event; Event label; GUAY-1D; GUAY-2D; GUAY-5D; GUAYAMAS; Identification; Latitude of event; Longitude of event; NOAA and MMS Marine Minerals Geochemical Database; NOAA-MMS; Pacific Ocean; Position; Quantity of deposit; Sediment type; Size; Substrate type; Thomas Washington; Visual description
    Type: Dataset
    Format: text/tab-separated-values, 55 data points
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  • 85
    Publication Date: 2023-08-28
    Description: A detailed geophysical and geological survey of the Mariana Trough, an actively extensional back-arc basin, was conducted in 1976 and 1977 to provide data for selection of drilling sites for DSDP Leg 60. These surveys revealed large-scale bathymetric trends, sediment distribution, crustal seismic veolocity structure, and earthquake activity that suggest the basin is opening around an axial spreading center tectonically similar to the slowly spreading Mid-Atlantic Ridge. There are, however, significant differences in the character of the trough, such as poorly defined magnetic anomalies, extreme bathymetric relief, and the frequent occurrence of low-magnitude earthquakes but absence of larger seismic events. Seafloor spreading in the Mariana Trough may be characteristic of the initial opening stages of any oceanic rift system, whether or not it is in a back-arc setting.
    Keywords: Comment; Deposit type; Depth, bottom/max; DEPTH, sediment/rock; Depth, top/min; Description; Dredge, rock; DRG_R; Event label; Identification; Kana Keoki; KK77; KK770317; KK770317-4 M01; KK770317-4 M05; KK770317-4 M06; KK770317-4 M08; KK770317-4 M09; KK770317-4 M10; KK770317-4 M11; KK770317-4-RD01; KK770317-4-RD05; KK770317-4-RD06; KK770317-4-RD08; KK770317-4-RD09; KK770317-4-RD10; KK770317-4-RD11; KK770317-PC04; KK770317-PC14; KK770317-PC18; KK770317-RD19; KK770317-RD20; KK770317-RD21; KK770317-RD22; KK770317-RD23; KK770317 STA48; KK770317 STA50; KK770317 STA56; KK770317 STA57; KK770317 STA58; NOAA and MMS Marine Minerals Geochemical Database; NOAA-MMS; Pacific Oean; PC; PC18; PCOD14; PCOD 4; Piston corer; Position; Quantity of deposit; Sediment type; Size; Substrate type; Uniform resource locator/link to image; Visual description
    Type: Dataset
    Format: text/tab-separated-values, 237 data points
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  • 86
    Publication Date: 2023-08-28
    Description: Cores, submarine photography and dredges described in this report were taken during the R/V Melville Cruise Vulcan-1 in September 1980 by the School of Oceanography, Oregon State University. This cruise was part of the International Decade of Ocean Exploration (IDOE) Manganese Nodule Program (MANOP). It surveyed MANOP Sites H and M in the Pacific Ocean.
    Keywords: BC; Box corer; Comment; Deposit type; Depth, bottom/max; DEPTH, sediment/rock; Depth, top/min; Description; Elevation of event; Event label; GC; Gravity corer; Identification; Latitude of event; Longitude of event; MANOP Site H, Pacific Ocean; MANOP Site M, Pacific Ocean; Melville; Method/Device of event; NOAA and MMS Marine Minerals Geochemical Database; NOAA-MMS; Position; Quantity of deposit; Sediment type; Size; Visual description; VLCN-1; VLCN-1-26GC; VLCN-1-34GC; VLCN-1-36GC; VLCN-1-37BC; VLCN-1-38GC; VLCN-1-40BX; VLCN-1-47GC; VLCN-1-48BC; VLCN-1-49GC; VLCN-1-50BC; VLCN-1-52BX; VLCN-1-54GC; VLCN-1-55BX; VLCN-1-60GC; VLCN-1-62BX; VLCN-1-63GC; VLCN-1-64GC; VLCN-1-66BX; VLCN-1-68BX; VLCN-1-69BC; VLCN-1-70GC; VULCAN Leg 1
    Type: Dataset
    Format: text/tab-separated-values, 307 data points
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  • 87
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    In:  Supplement to: Sorem, Ronald K; Fewkes, Ronald H (1980): Distribution of Todorokite and Birnessite in manganese nodules from the "Horn Region", Eastern Pacific Ocean. in: Varentsov, I. M., Grasselly, G. (Eds.), Geology and Geochemistry of Manganese, E. Schweizerbart'sche Verlagsbuchhandlung, Stuttgart, Germany, 1, 201-229, https://store.pangaea.de/Projects/NOAA-MMS/Sorem_1980.pdf
    Publication Date: 2023-08-28
    Description: The oxide portion of marine manganese nodules deserves intensive study because it probably reflects directly the conditions under which nodules form in the Bea. A better understanding of the nature of the oxides in nodules should therefore throw new light on basic problems of nodule origin.
    Keywords: BC; Box corer; Comment; Date/Time of event; Deposit type; DEPTH, sediment/rock; Description; Dredge; DRG; Elevation of event; Event label; FFGR; Free-fall grab; KEN72-SP9; Latitude of event; Longitude of event; Mn-74-01-001-FFG-001; Mn-74-01-002-FFG-004; Mn-74-01-003-FFG-007; Mn-74-01-005-B2; Mn-74-01-005-FFG-015; Mn-74-01-006-FFG-017; Mn-74-01-006-FFG-018; Mn-74-01-006-FFG-019; Mn-74-01-006-FFG-020; Mn-74-01-006-FFG-021; Mn-74-01-006-FFG-022; Mn-74-01-006-FFG-023; Mn-74-01-006-FFG-024; Mn-74-01-006-FFG-025; Mn-74-01-006-FFG-026; Mn-74-01-007-FFG-028; Mn-74-01-007-FFG-029; Mn-74-01-007-FFG-030; Mn-74-01-009-FFG-036; Mn-74-01-010-FFG-037; Mn-74-01-010-FFG-038; Mn-74-01-010-FFG-040; Mn-74-01-010-FFG-043; Mn-74-01 IODE; Mn-74-02-13A-FFG-002; Mn-74-02-13A-FFG-003; Mn-74-02-13A-FFG-004; Mn-74-02-13B-FFG-005; Mn-74-02-13B-FFG-007; Mn-74-02-13B-FFG-008; Mn-74-02-13C-FFG-009; Mn-74-02-13C-FFG-010; Mn-74-02-13C-FFG-011; Mn-74-02-13C-FFG-012; Mn-74-02-15-FFG-021; Mn-74-02-15-FFG-023; Mn-74-02-15-FFG-025; Mn-74-02 IDOE DOMES; Moana Wave; MW7401; MW7401-01G01; MW7401-02G04; MW7401-03G07; MW7401-05B02; MW7401-05G15; MW7401-06G17; MW7401-06G18; MW7401-06G19; MW7401-06G20; MW7401-06G21; MW7401-06G22; MW7401-06G23; MW7401-06G24; MW7401-06G25; MW7401-06G26; MW7401-07G28; MW7401-07G29; MW7401-07G30; MW7401-09G36; MW7401-10G37; MW7401-10G38; MW7401-10G40; MW7401-10G43; MW7402; MW7402-13G02; MW7402-13G03; MW7402-13G04; MW7402-13G05; MW7402-13G07; MW7402-13G08; MW7402-13G09; MW7402-13G10; MW7402-13G11; MW7402-13G12; MW7402-15G21; MW7402-15G23; MW7402-15G25; NOAA and MMS Marine Minerals Geochemical Database; NOAA-MMS; Pacific Ocean; Position; Sample code/label; Sample ID; Size; Substrate type; Uniform resource locator/link to image
    Type: Dataset
    Format: text/tab-separated-values, 597 data points
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  • 88
    Publication Date: 2023-08-28
    Description: Methods of estimating manganese nodule grade and concentration were investigated using bottom photographs from a well-explored east-central Pacific manganese nodule deposit.
    Keywords: Automated image processing; Coverage; DATE/TIME; Deposit type; DEPTH, sediment/rock; Description; DOMES Site C, Pacific Ocean; ELEVATION; LATITUDE; LONGITUDE; NOAA and MMS Marine Minerals Geochemical Database; NOAA-MMS; Nodules, mass abundance; Oceanographer; Photo/Video; PV; RP8OC76; RP-8-OC-76; RP8OC76-3-1C; Sample ID; Statistical inference
    Type: Dataset
    Format: text/tab-separated-values, 1230 data points
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  • 89
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    PANGAEA
    In:  Supplement to: Cochran, J Kirk; Krishnaswami, Seth (1980): Radium, thorium, uranium, and 210 Pb in deep-sea sediments and sediment pore waters from the North Equatorial Pacific. American Journal of Science, 280(9), 849-889, https://doi.org/10.2475/ajs.280.9.849
    Publication Date: 2023-08-28
    Description: Determination of radium, thorium, uranium isotopes, and 210Pb in sediments and sediment pore waters from North Equatorial Pacific deep-sea clay-silicous oozes shows that the radium and uranium isotopes are mobile in the pore water. The concentration-depth profiles of radium can be understood in terms of a diagenetic model which takes into account mixing of sediment particles by bioturbation, molecular diffusion in the pore water, adsorption onto particle surfaces, as well as radioactive production and decay. The 234U/238U activity ratios in several samples are higher than the seawater value, indicating some enrichment of 234U in the pore water. However, the absolute concentrations of 238U and 234U are 25% lower than those in seawater, suggesting that the sediments form a sink for uranium isotopes. 210Pb is present in the pore water at concentrations approx. 20% that of 226Ra. The origin of 210Pb in the pore water is uncertain and could be due either to its in situ mobilization in the sediments or subsequent production in the laboratory from the decay of 222Rn. 230Th is present in measurable concentrations in the pore waters, but its distribution does not show any systematic trend with depth or other parameters. The most likely source of 230/Th appears to be minute amounts of sediment particles collected in the pore waters during the squeezing operation.
    Keywords: BC; Box corer; Date/Time of event; DEPTH, sediment/rock; DISTANCE; Distance, maximum; Distance, minimum; DOMES-A47-16; DOMES Site B, Pacific Ocean; DOMES Site C, Pacific Ocean; Elevation of event; Event label; Latitude of event; Lead-210; Lead-210, standard deviation; Lead-210 excess; Lead-210 excess, standard deviation; Longitude of event; NOAA and MMS Marine Minerals Geochemical Database; NOAA-MMS; Oceanographer; Pacific Ocean; Radium-226; Radium-226, standard deviation; RP8OC75; RP-8-OC-75; RP8OC7503; RP8OC75-47-16; RP8OC75-52-39; RP8OC75-57-58; Sample ID; Sample type; Thorium-228/Thorium-232 activity ratio; Thorium-228/Thorium-232 activity ratio, standard deviation; Thorium-230; Thorium-230, standard deviation; Thorium-230/Thorium-227 activity ratio; Thorium-230/Thorium-227 activity ratio, standard deviation; Thorium-230/Thorium-232 activity ratio; Thorium-230/Thorium-232 activity ratio, standard deviation; Thorium-232; Thorium-232, standard deviation; Uranium-234/Uranium-238 activity ratio; Uranium-234/Uranium-238 activity ratio, standard deviation; Uranium-238; Uranium-238, standard deviation
    Type: Dataset
    Format: text/tab-separated-values, 462 data points
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  • 90
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    Unknown
    PANGAEA
    In:  Supplement to: Kadko, David; Burckle, Lloyd H (1980): Manganese nodule growth rates determined by fossil diatom dating. Nature, 287(5784), 725-726, https://doi.org/10.1038/287725a0
    Publication Date: 2023-08-28
    Description: We report here that a manganese nodule from the Central Pacific manganese nodule province has been dated by fossil diatoms found in mud scraped from near the nodule's centre. The nodule was taken at DOMES Site B from Core B55-56 at 11°50.3'N and 137°28.2'W in a water depth of 4,892 m. It was resting on the sediment surface, with about 1.5 cm of the nodule bottom (of a total nodule height of 4.2 cm) buried in the mud. The top surface of the nodule was covered with a smooth manganese coating, but the bottom had a very rough, crusty texture. It was found that recent mud had leaked in through cracks in the nodule bottom, but that there were no pre-Pleistocene diatoms in this material. The date obtained was compared with the growth rate determined by the 230Th excess method and found to be in reasonable agreement. This study adds to the work of Harada1,2 on the biostratigraphy (mainly coccoliths) of manganese nodules.
    Keywords: Alpha counting; BC; Box corer; Deposit type; DEPTH, sediment/rock; Description; DISTANCE; DOMES Site B, Pacific Ocean; Identification; NOAA and MMS Marine Minerals Geochemical Database; NOAA-MMS; Oceanographer; RP-8-OC-75; RP8OC7503; RP8OC75-55-56; Thorium-230 excess; Thorium-230 excess, standard deviation
    Type: Dataset
    Format: text/tab-separated-values, 33 data points
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  • 91
    Publication Date: 2023-08-28
    Keywords: 51-417A; Comment; Deep Sea Drilling Project; Deposit type; DEPTH, sediment/rock; Description; DRILL; Drilling/drill rig; DSDP; Glomar Challenger; Identification; Leg51; NOAA and MMS Marine Minerals Geochemical Database; NOAA-MMS; North Atlantic/CONT RISE; Position; Quantity of deposit; Sample code/label; Sediment type; Substrate type; Visual description
    Type: Dataset
    Format: text/tab-separated-values, 24 data points
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  • 92
    Publication Date: 2023-08-28
    Keywords: Age, comment; Aluminium oxide; Atomic emission spectroscopy (AES); Barium; Beal Traversier, Hautes-Alpes, France; Bois Durat, Hautes-Alpes, France; BRB-B; BRB-BD; BRB-BT; BRB-C; BRB-CBO; BRB-CBR; BRB-CC; BRB-CF; BRB-COU; BRB-CQ; BRB-CR; BRB-CV; BRB-E; BRB-Ey; BRB-FS; BRB-GB; BRB-GE; BRB-L; BRB-LAU; BRB-LBL; BRB-M; BRB-MMA; BRB-MN; BRB-MO; BRB-MS; BRB-O; BRB-OB; BRB-P; BRB-PEY; BRB-Pl; BRB-RA; BRB-RAS; BRB-RCV; BRB-RG; BRB-RSR; BRB-RSRW; BRB-SA; BRB-SCN; BRB-SOU; BRB-STC; BRB-TN; BRB-VAL; BRB-VC; Calcium oxide; Carbon dioxide; Cariiere de la Lame, Hautes-Alpes, France; Chromium; Clot de la Cime, Hautes-Alpes, France; Clot des Fonds, Hautes-Alpes, France; Cobalt; Col de la Pisse, Hautes-Alpes, France; Col du Lauzon, Hautes-Alpes, France; Colonel Bonnet, Hautes-Alpes, France; Combe Bremond, Hautes-Alpes, France; Condamine, Hautes-Alpes, France; Copper; Coste Rousse, Hautes-Alpes, France; Couloir du Queyrellin, Hautes-Alpes, France; Crete de la Plate, Hautes-Alpes, France; Crete des Couniets, Hautes-Alpes, France; Crete de Vars, Hautes-Alpes, France; Deposit type; DEPTH, sediment/rock; Elevation of event; Event label; Eychauda, Hautes-Alpes, France; Eygliers, Hautes-Alpes, France; Fluorine; Font Sancte, Hautes-Alpes, France; Fort de l'Olive, Hautes-Alpes, France; HAM; Hammer; Identification; Iron oxide, Fe2O3; Lac Blanc, Hautes-Alpes, France; Lac de l'Ascencion, Hautes-Alpes, France; Lac du Vallonnet, Hautes-Alpes, France; Latitude of event; La Vachette, Hautes-Alpes, France; Lead; Longitude of event; Loss on ignition; Magnesium oxide; Manganese oxide; Montbrison Nord, Hautes-Alpes, France; Montbrison Sud, Hautes-Alpes, France; Monte Maniglia, Hautes-Alpes, France; Mouliere, Hautes-Alpes, France; Nickel; NOAA and MMS Marine Minerals Geochemical Database; NOAA-MMS; Ombilic, Hautes-Alpes, France; Peyron, Hautes-Alpes, France; Phosphorus pentoxide; Pic Balart, Hautes-Alpes, France; Pointe de Rasis, Hautes-Alpes, France; Potassium oxide; Ratier, Hautes-Alpes, France; Replat des Genisses, Hautes-Alpes, France; Roche Chevalire, Hautes-Alpes, France; Roche Gauthier, Hautes-Alpes, France; Rocher du Roux, Hautes-Alpes, France; Rocher du Roux Ouest, Hautes-Alpes, France; Sablier, Hautes-Alpes, France; Sample code/label; Serre Chevalier, Hautes-Alpes, France; Silicon dioxide; Sodium oxide; Souliers, Hautes-Alpes, France; St Crepin, Hautes-Alpes, France; Strontium; Sulfur, total; Tete Noire, Hautes-Alpes, France; Titanium dioxide; Torrent du Grand Bois, Hautes Alpes; Vanadium; Wet chemistry; Yttrium; Zinc
    Type: Dataset
    Format: text/tab-separated-values, 2863 data points
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  • 93
    Publication Date: 2023-09-01
    Keywords: AGE; AII60-13APC; DEPTH, sediment/rock; Mass spectrometer VG Micromass 602; PC; Piston corer; Planulina wuellerstorfi, δ13C; Planulina wuellerstorfi, δ18O; Vema Channel
    Type: Dataset
    Format: text/tab-separated-values, 36 data points
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  • 94
    Publication Date: 2023-09-01
    Keywords: AGE; CHN115-70PC; DEPTH, sediment/rock; Mass spectrometer VG Micromass 602; PC; Piston corer; Planulina wuellerstorfi, δ13C; Planulina wuellerstorfi, δ18O; Vema Channel
    Type: Dataset
    Format: text/tab-separated-values, 40 data points
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  • 95
    Publication Date: 2023-09-01
    Keywords: AGE; CHN115-88PC; DEPTH, sediment/rock; Mass spectrometer VG Micromass 602; PC; Piston corer; Planulina wuellerstorfi, δ13C; Planulina wuellerstorfi, δ18O; Vema Channel
    Type: Dataset
    Format: text/tab-separated-values, 60 data points
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  • 96
    Publication Date: 2023-09-01
    Keywords: AGE; CHN115-91PC; DEPTH, sediment/rock; Mass spectrometer VG Micromass 602; PC; Piston corer; Planulina wuellerstorfi, δ13C; Planulina wuellerstorfi, δ18O; Vema Channel
    Type: Dataset
    Format: text/tab-separated-values, 30 data points
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  • 97
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    Unknown
    PANGAEA
    In:  Supplement to: Maury, R C; Bougault, Henri; Joron, Jean Louis; Girard, D; Treuil, M; Azéma, Jacques; Aubouin, Jean (1982): Volcanic rocks from Leg 67 Sites: mineralogy and geochemistry. In: Abouin, J; von Huene, R; et al. (eds.), Initial Reports of the Deep Sea Drilling Project (U.S. Govt. Printing Office), LXVII, 557-576, https://doi.org/10.2973/dsdp.proc.67.123.1982
    Publication Date: 2023-08-28
    Description: Mineralogical (microprobe) and geochemical (X-ray fluorescence, neutron activation analyses) data are given for 18 samples of volcanic rocks from the Guatemala Trench area (Deep Sea Drilling Project Leg 67). Typical fresh oceanic tholeiites occur in the trench itself (Hole 500) and in its immediate vicinity on the Cocos Plate (Site 495). Several samples (often reworked) of "spilitic" oceanic tholeiites are also described from the Trench: their mineralogy (greenschist facies association - actinolite + plagioclase + chlorite) and geochemistry (alteration, sometimes linked to manganese and zinc mineralization) are shown to result from high-temperature (300°-475°C) hydrothermal sea water-basalt interactions. The samples studied are depleted in light rare-earth elements (LREE), with the exception of the slightly LREE-enriched basalts from Hole 500. The occurrence of such different oceanic tholeiites in the same area is problematic. Volcanic rocks from the Guatemala continental slope (Hole 494A) are described as greenschist facies metabasites (actinolite + epidote + chlorite + plagioclase + calcite + quartz), mineralogically different from the spilites exposed on the Costa Rica coastal range (Nicoya Peninsula). Their primary magmatic affinity is uncertain: clinopyroxene and plagioclase compositions, together with titanium and other hygromagmaphile element contents, support an "active margin" affinity. The LREE-depleted patterns encountered in the present case, however, are not frequently found in orogenic samples but are typical of many oceanic tholeiites.
    Keywords: 66-487; 67-494; 67-494A; 67-495; 67-499B; 67-499C; 67-499D; 67-500; 67-500B; Deep Sea Drilling Project; DRILL; Drilling/drill rig; DSDP; Glomar Challenger; Leg66; Leg67; North Pacific/TRENCH
    Type: Dataset
    Format: application/zip, 13 datasets
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  • 98
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    Unknown
    PANGAEA
    In:  Supplement to: Frakes, Lawrence A (1982): Metal chemistry of manganese nodules from the Cape Leeuwin field, southeast Indian Ocean. Marine Geology, 47(1-2), M1-M10, https://doi.org/10.1016/0025-3227(82)90014-7
    Publication Date: 2023-08-28
    Description: Manganese nodules from 36 stations in the Cape Leeuwin field were analyzed for Mn, Fe, Ni, Cu and Co and the results were combined with earlier work to demonstrate quantitative and geographic variations. Nodules in this field are moderately enriched in Ni, moderately depleted in Cu, and contain intermediate values of Co. The sum of Ni + Cu vs. Mn/Fe plots along a hyperbolic regression line derived from nodules of the southeastern Pacific, suggesting that this relationship has general applicability. Regional variations in nodule grade (Ni + Cu + Co) assist in defining pathways of Antarctic Bottom Water between the Southeast Indian Ridge and the Wharton basin.
    Keywords: NOAA and MMS Marine Minerals Geochemical Database; NOAA-MMS
    Type: Dataset
    Format: application/zip, 4 datasets
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  • 99
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    Unknown
    PANGAEA
    In:  Supplement to: USGS Woods Hole Coastal and Marine Science Center (1982): GYRE 82-11 Expedition, Sample Log, R/V Gyre. hdl:10013/epic.46138.d014, 49 pp, http://cotuit.er.usgs.gov/Data/1982-034-FA/NL/001/04/82034sm1.pdf
    Publication Date: 2023-08-28
    Description: The purpose of the expedition was to test new techniques to determine thickness, distribution and quality of mineral deposits on the Blake Plateau with special reference to manganese nodules and manganese-phosphate pavements.
    Keywords: 82034 G-11-82-SE; Blake Plateau, Atlantic Ocean; C11-Sta20 - Patio Block; C6-Sta3; C9-Sta14; D10-Sta18 - Patio Block; D11-Sta19 - Patio Block; D12-Sta23; D14-Sta24; D15-Sta25 - Southwest Blake Plateau Triple Junctio; D16-Sta26 - South Blake Plateau; D17-Sta27; D1-Sta2A; D2-Sta6; D3-Sta7; D4-Sta7; D5-Sta8; D8-Sta15; D9-Sta17; Date/Time of event; Deposit type; DEPTH, sediment/rock; Description; Dredge, rock; DRG_R; Elevation of event; Event label; File name; GC; Gravity corer; Gyre; GYRE82-11; GYRE82-11-C06; GYRE82-11-C09; GYRE82-11-C11; GYRE82-11-D01; GYRE82-11-D02; GYRE82-11-D03; GYRE82-11-D04; GYRE82-11-D05; GYRE82-11-D08; GYRE82-11-D09; GYRE82-11-D10; GYRE82-11-D11; GYRE82-11-D12; GYRE82-11-D14; GYRE82-11-D15; GYRE82-11-D16; GYRE82-11-D17; Latitude of event; Longitude of event; Method/Device of event; NOAA and MMS Marine Minerals Geochemical Database; NOAA-MMS; PC; Piston corer; Position; Quantity of deposit; Sample ID; Sediment type; Size; Substrate type; Uniform resource locator/link to image
    Type: Dataset
    Format: text/tab-separated-values, 191 data points
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  • 100
    facet.materialart.
    Unknown
    PANGAEA
    In:  Supplement to: Commeau, J A; Manheim, Frank T (1982): Testing the variation of Fe-Mn concentration as a function of preparation treatment for phosphate-manganese nodules from the Blake Plateau. (Expedition GYRE 82-11), Cruise Note. USGS Woods Hole Coastal and Marine Science Center
    Publication Date: 2023-08-28
    Description: Sample preparation technique is critical for valid chemical analyses. A main source of error comes from the fact that the great specific surface area of crusts or nodules enhances their tendency to retain or attract hygroscopic moisture. Variable treatment of this moisture can in extreme cases lead to analytical value differences as great as 40-50 %. In order to quantify these influences, samples of ferromanganese oxide-phosphorite pavement from the Blake Plateau have been subjected to various drying techniques before analysis using X-ray fluorescence.
    Keywords: 82034 G-11-82-SE; Blake Plateau, Atlantic Ocean; C6-Sta3; C9-Sta14; Calcium; D10-Sta18 - Patio Block; D11-Sta19 - Patio Block; D12-Sta23; D14-Sta24; D15-Sta25 - Southwest Blake Plateau Triple Junctio; D16-Sta26 - South Blake Plateau; D17-Sta27; D1-Sta2A; D2-Sta6; D3-Sta7; D4-Sta7; D5-Sta8; D8-Sta15; D9-Sta17; Date/Time of event; Description; Dredge, rock; DRG_R; Elevation of event; Event label; GC; Gravity corer; Gyre; GYRE82-11; GYRE82-11-C06; GYRE82-11-C09; GYRE82-11-D01; GYRE82-11-D02; GYRE82-11-D03; GYRE82-11-D04; GYRE82-11-D05; GYRE82-11-D08; GYRE82-11-D09; GYRE82-11-D10; GYRE82-11-D11; GYRE82-11-D12; GYRE82-11-D14; GYRE82-11-D15; GYRE82-11-D16; GYRE82-11-D17; Heated at 500°C for one hour; Ignited at 1000°C for one hour; Iron; Latitude of event; Longitude of event; Loss on drying; Loss on ignition; Manganese; NOAA and MMS Marine Minerals Geochemical Database; NOAA-MMS; Oven-dry, heated at 110°C overnight; Sample ID; X-ray fluorescence (XRF)
    Type: Dataset
    Format: text/tab-separated-values, 128 data points
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