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  • PANGAEA
  • 1990-1994  (1,459)
  • 1992  (1,459)
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  • 1990-1994  (1,459)
Year
  • 1
    Publication Date: 2016-01-14
    Repository Name: EPIC Alfred Wegener Institut
    Type: PANGAEA Documentation , notRev
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  • 2
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    PANGAEA
    In:  EPIC3WOCE., Bremerhaven, PANGAEA
    Publication Date: 2019-07-17
    Repository Name: EPIC Alfred Wegener Institut
    Type: PANGAEA Documentation , notRev
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  • 3
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    PANGAEA
    In:  EPIC3WOCE., Bremerhaven, PANGAEA
    Publication Date: 2019-07-17
    Repository Name: EPIC Alfred Wegener Institut
    Type: PANGAEA Documentation , notRev
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  • 4
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    PANGAEA
    In:  EPIC3WOCE., Bremerhaven, PANGAEA
    Publication Date: 2019-07-17
    Repository Name: EPIC Alfred Wegener Institut
    Type: PANGAEA Documentation , notRev
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  • 5
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    PANGAEA
    In:  EPIC3WOCE., Bremerhaven, PANGAEA
    Publication Date: 2019-07-17
    Repository Name: EPIC Alfred Wegener Institut
    Type: PANGAEA Documentation , notRev
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  • 6
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    PANGAEA
    In:  EPIC3Geographical Research Institute, Hungarian Academy of SCiences, Budapest, Gustav Fischer Verlag, Stuttgart Jena New York., Bremerhaven, PANGAEA
    Publication Date: 2019-07-17
    Repository Name: EPIC Alfred Wegener Institut
    Type: PANGAEA Documentation , notRev
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  • 7
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    PANGAEA
    In:  EPIC3WOCE., Bremerhaven, PANGAEA
    Publication Date: 2019-07-17
    Repository Name: EPIC Alfred Wegener Institut
    Type: PANGAEA Documentation , notRev
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  • 8
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    PANGAEA
    In:  EPIC3WOCE., Bremerhaven, PANGAEA
    Publication Date: 2019-07-17
    Repository Name: EPIC Alfred Wegener Institut
    Type: PANGAEA Documentation , notRev
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  • 9
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    PANGAEA
    In:  EPIC3WOCE., Bremerhaven, PANGAEA
    Publication Date: 2019-07-17
    Repository Name: EPIC Alfred Wegener Institut
    Type: PANGAEA Documentation , notRev
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  • 10
    Publication Date: 2019-07-17
    Repository Name: EPIC Alfred Wegener Institut
    Type: PANGAEA Documentation , notRev
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  • 11
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    PANGAEA
    In:  EPIC3WOCE., Bremerhaven, PANGAEA
    Publication Date: 2019-07-17
    Repository Name: EPIC Alfred Wegener Institut
    Type: PANGAEA Documentation , notRev
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  • 12
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    PANGAEA
    In:  EPIC3WOCE., Bremerhaven, PANGAEA
    Publication Date: 2019-07-17
    Repository Name: EPIC Alfred Wegener Institut
    Type: PANGAEA Documentation , notRev
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  • 13
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    PANGAEA
    In:  EPIC3WOCE., Bremerhaven, PANGAEA
    Publication Date: 2019-07-17
    Repository Name: EPIC Alfred Wegener Institut
    Type: PANGAEA Documentation , notRev
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  • 14
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    PANGAEA
    In:  EPIC3ODP - Instructions for contributors, Bremerhaven, PANGAEA, 1 p.
    Publication Date: 2019-07-17
    Repository Name: EPIC Alfred Wegener Institut
    Type: PANGAEA Documentation , notRev
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  • 15
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    PANGAEA
    In:  EPIC3Universidad Nacional Agraria La Molina., Bremerhaven, PANGAEA
    Publication Date: 2019-07-17
    Repository Name: EPIC Alfred Wegener Institut
    Type: PANGAEA Documentation , notRev
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  • 16
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    PANGAEA
    In:  EPIC3Alfred Wegener Institute for Polar and Marine Research, Bremerhaven., Bremerhaven, PANGAEA
    Publication Date: 2018-08-10
    Repository Name: EPIC Alfred Wegener Institut
    Type: PANGAEA Documentation , notRev
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  • 17
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    PANGAEA
    In:  EPIC3Alfred Wegener Institute, Bremerhaven, Bremerhaven, PANGAEA, 4 p.
    Publication Date: 2019-07-16
    Repository Name: EPIC Alfred Wegener Institut
    Type: PANGAEA Documentation , notRev
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  • 18
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    In:  Supplement to: Wei, Wuchang (1992): Updated nannofossil stratigraphy of the CIROS-1 core from McMurdo Sound (Ross Sea). In: Wise, SW; Schlich, R; et al. (eds.), Proceedings of the Ocean Drilling Program, Scientific Results, College Station, TX (Ocean Drilling Program), 120, 1105-1117, https://doi.org/10.2973/odp.proc.sr.120.197.1992
    Publication Date: 2023-07-10
    Description: Semiquantitative data of calcareous nannofossil species abundance were collected for 31 samples from 380.00 to 696.61 m below sea floor (mbsf) in the CIROS-1 core from the western McMurdo Sound (Ross Sea). This core has provided the most complete record of Paleogene glacial history of Antarctica. Only half of the samples yielded calcareous nannofossils and species diversity is generally low. However, several samples contain diverse assemblages and nannofossil zonal markers. Isthmolithus recurvus was found between 406.57 and 681.16 mbsf. This species has an age range of ~35-39 Ma in the mid to high latitudes, as calibrated previously by magnetostratigraphy at a number of DSDP/ODP sites. The interval from 406.57 to 681.16 mbsf can be assigned to the late Eocene-earliest Oligocene (~35-39 Ma), and the sample at 391.85 mbsf, which still contains Reticulofenestra hillae and Reticulofenestra umbilica but does not contain I. recurvus, is identified as early Oligocene age (~33-34 Ma). This represents an age refinement of the previous nannofossil biostratigraphy, where the interval from 385.77 to 690.40 mbsf was dated as middle Eocene-early Oligocene. Comparison of the nannofossil assemblages in the CIROS-1 core with those in a similar glaciomarine sequence recovered in Prydz Bay (East Antarctica) and those at deep-sea ODP Sites 738 and 744, where lowermost Oligocene ice-rafted debris (IRD) were found, suggests that the nannofossils in the CIROS-1 core samples examined are in situ. The semiquantitative nannofossil data also suggest that Isthmolithus recurvus and Reticulofenestra davies¸ are most tolerant of cold waters within the late Eocene-early Oligocene nannofloras.
    Keywords: Braarudosphaera bigelowii; Butter Point; Chiasmolithus altus; Chiasmolithus cf. oamaruensis; Chiasmolithus oamaruensis; Chiasmolithus sp.; CIROS; CIROS-1; Coccolithus pelagicus; Cyclicargolithus floridanus; DEPTH, sediment/rock; DRILL; Drilling/drill rig; Epoch; Isthmolithus recurvus; Lithostromation simplex; Nannofossil abundance; Nannofossils preservation; Nannofossil zone; Reticulofenestra bisecta; Reticulofenestra daviesii; Reticulofenestra hillae; Reticulofenestra umbilicus; Sampling/drilling ice; Sphenolithus moriformis; Zygrhablithus bijugatus
    Type: Dataset
    Format: text/tab-separated-values, 850 data points
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  • 19
    Publication Date: 2023-07-10
    Keywords: Chiasmolithus expansus; Chiasmolithus grandis; Chiasmolithus solitus; Coccolithus formosus; Coccolithus pelagicus; DEPTH, sediment/rock; Discoaster barbadiensis; Discoaster lodoensis; Discoaster saipanensis; Discoaster spp.; Discoaster sublodoensis; ELT24; ELT24.008-PC; Eltanin; Isthmolithus recurvus; Markalius inversus; Nannofossil abundance; Nannofossils preservation; Neococcolithes dubius; PC; Piston corer; Reticulofenestra daviesii; Reticulofenestra samodurovii; Sphenolithus moriformis
    Type: Dataset
    Format: text/tab-separated-values, 36 data points
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  • 20
    Publication Date: 2023-07-10
    Keywords: 20-198A; Adercotryma sp.; Ammodiscus cretaceus; Bolivinopsis parvissimus; Counting 〉63 µm fraction; Deep Sea Drilling Project; DRILL; Drilling/drill rig; Dry mass; DSDP; DSDP/ODP/IODP sample designation; Foraminifera, benthic agglutinated; Glomar Challenger; Glomospira charoides; Glomospira gordialis; Glomospira irregularis; Glomospira serpens; Haplophragmoides biumbilicalis; Haplophragmoides ex gr. H. herbichi; Haplophragmoides ex gr. H. perexplicatus-constrictus; Haplophragmoides fraudulentus; Haplophragmoides incredibilis; Haplophragmoides multicamerus; Hormosina crassa; Hormosina ovulum; Hyperammina spp.; Kalamopsis grzybowskii; Leg20; North Pacific/BASIN; Number of species; Paratrochamminoides corpulentus; Paratrochamminoides dubius; Paratrochamminoides intricatus; Paratrochamminoides semipellucidus; Paratrochamminoides sp.; Plectorecurvoides parvus; Praecystammina globigerinaeformis; Recurvoides sp.; Rhizammina sp.; Sample code/label; Subreophax scalaris; Trochamminoides ex. gr. H. proteus; Trochamminoides olszewskii; Volume
    Type: Dataset
    Format: text/tab-separated-values, 840 data points
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  • 21
    Publication Date: 2023-07-10
    Keywords: 371; 373; 375; 376; 377; 378; 381; 383; 386; 388; Acridine Orange Direct Counting (AODC); Atlantic Ocean; Bacteria, biomass as carbon; Bacteria per unit wet sediment; BC; Box corer; Calculated; Colony forming unit; Date/Time of event; Depth, bottom/max; DEPTH, sediment/rock; Depth, top/min; Elevation of event; Event label; GEOTROPEX 83, NOAMP I; Giant box corer; GIK16421-2; GIK16422-2; GIK16424-1; GIK16425-1; GIK16426-3; GIK16427-1; GIK16430-2; GIK16432-1; GIK16435-1; GIK16437-3; GKG; Gravity corer (Kiel type); Latitude of event; Longitude of event; M65; Mesophiles per unit wet sediment; Meteor (1964); Optional event label; Psychrophiles per unit wet sediment; SL; Succinate per unit wet sediment; Temperature, in rock/sediment; van Veen Grab; VGRAB; Yeast extract per unit wet sediment
    Type: Dataset
    Format: text/tab-separated-values, 161 data points
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  • 22
    Publication Date: 2023-07-10
    Keywords: Chiasmolithus expansus; Chiasmolithus grandis; Coccolithus formosus; Coccolithus pelagicus; DEPTH, sediment/rock; Discoaster barbadiensis; Discoaster spp.; ELT24; ELT24.009-PC; Eltanin; Nannofossil abundance; Nannofossils preservation; PC; Piston corer; Reticulofenestra samodurovii; Sphenolithus moriformis; Tribrachiatus orthostylus
    Type: Dataset
    Format: text/tab-separated-values, 33 data points
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  • 23
    Publication Date: 2023-07-10
    Keywords: 20-196; Adercotryma sp.; Ammodiscus tenuissimus; Bolivinopsis parvissimus; Buzasina pacifica; Counting 〉63 µm fraction; Deep Sea Drilling Project; Dendrophrya excelsa; DRILL; Drilling/drill rig; Dry mass; DSDP; DSDP/ODP/IODP sample designation; Foraminifera, benthic agglutinated; Foraminifera, benthic agglutinated indeterminata; Glomar Challenger; Glomospira charoides; Glomospira gordialis; Glomospira irregularis; Haplophragmoides biumbilicalis; Haplophragmoides ex gr. H. perexplicatus-constrictus; Haplophragmoides fraudulentus; Haplophragmoides krasheninnikovi; Haplophragmoides molestus; Hormosina crassa; Hormosina ovulum; Hyperammina sp.; Leg20; North Pacific/ABYSSAL FLOOR; Number of species; Paratrochamminoides corpulentus; Paratrochamminoides dubius; Paratrochamminoides intricatus; Paratrochamminoides semipellucidus; Paratrochamminoides sp.; Plectorecurvoides parvus; Plectorecurvoides rotundus; Praecystammina globigerinaeformis; Pseudobolivina munda; Rhizammina sp.; Sample code/label; Subreophax scalaris; Volume
    Type: Dataset
    Format: text/tab-separated-values, 442 data points
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  • 24
    Publication Date: 2023-07-24
    Keywords: 48-401; AGE; Cibicidoides spp., δ13C; Cibicidoides spp., δ18O; Deep Sea Drilling Project; DEPTH, sediment/rock; DRILL; Drilling/drill rig; DSDP; DSDP/ODP/IODP sample designation; Glomar Challenger; Leg48; Mass spectrometer Finnigan MAT 251; North Atlantic/TERRACE; Sample code/label
    Type: Dataset
    Format: text/tab-separated-values, 164 data points
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  • 25
    Publication Date: 2023-07-24
    Keywords: 81-555; AGE; Cibicidoides spp., δ13C; Cibicidoides spp., δ18O; Deep Sea Drilling Project; DEPTH, sediment/rock; DRILL; Drilling/drill rig; DSDP; DSDP/ODP/IODP sample designation; Glomar Challenger; Leg81; Mass spectrometer Finnigan MAT 251; North Atlantic/PLATEAU; Sample code/label
    Type: Dataset
    Format: text/tab-separated-values, 180 data points
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  • 26
    Publication Date: 2023-08-28
    Description: On a previous R/V Polarstern cruise ANT-VIII/5 (1989/90), a deep-sea area in the central Weddell Sea was investigated along geophysical and bathymetrical transects. As a result, a seamount-like structure, the informally named "Polarstern Seamount", was detected. This seamount was one of the sampling areas during the ANT-IX/3 leg. Attempts were made to retrieve glaciomarine and hemipelagic sediments, which in this area were expected not to be so strongly affected by bottom currents as are the sediments in the deeper surroundings seas. The seafloor on top of the Polarstern Searnount revealed to be densely covered with Mn encrusted dropstones, as observed by the underwater video-recording obtained from a camera installed at the multi box corer (MG), as well as in the retrieved sediments.
    Keywords: Agulhas Basin; ANT-IX/3; ANT-IX/4; AWI_Paleo; Comment; Deposit type; DEPTH, sediment/rock; Description; Elevation of event; Event label; Gravity corer (Kiel type); Identification; KL; Latitude of event; Longitude of event; Maud Rise; NOAA and MMS Marine Minerals Geochemical Database; NOAA-MMS; Paleoenvironmental Reconstructions from Marine Sediments @ AWI; Piston corer (BGR type); Polarstern; Polarstern Kuppe; Position; PS18; PS18/145; PS18/147; PS18/225; PS18/238; PS2003-2; PS2005-1; PS2070-1; PS2082-1; Quantity of deposit; Sediment type; Size; SL; Substrate type; Visual description
    Type: Dataset
    Format: text/tab-separated-values, 50 data points
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  • 27
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    PANGAEA
    In:  Supplement to: Usui, Akira; Nishimura, Akira (1992): Submersible observations of hydrothermal manganese deposits on the Kaikata Seamount, Izu-Ogasawara (Bonin) Arc. Marine Geology, 106(3-4), 203-216, https://doi.org/10.1016/0025-3227(92)90130-A
    Publication Date: 2023-08-28
    Description: During Dive 408 of Shinkai 2000 on the flank of the Kaikata Seamount located on the volcanic front of the Izu-Ogasawara (Bonin) Arc, possibly recent hydrothermal manganese deposits were observed on sandy volcanic sediments at water depths of between 800 and 1200 m. The deposits cover almost the entire surface sediment across the manganese belt on the northwestern flank on the seamount on a scale of kilometers. The occurrence of the deposits, seafloor morphology and temperature of the sediments, together with previous shipboard results, lead to a possible model for the formation of the manganese deposits: A low-temperature hydrothermal solution ascends through fractures or faults in the volcanic substrate into permeable volcanic sands and precipitates manganate minerals which cement several centimeters of surface sand as hardpan. More intense and probably intermittent discharge of hydrothermal solution follows and forms many typical ridge-like vents and mounds on the seafloor. Subsequently, pure dense manganate layers developed beneath the semi-consolidated volcanic sandstone and act as a cap to the ascending fluids. The proposed mechanism may be the dominant type of low-temperature hydrothermal mineralization in submarine island-arc volcanoes and rifts. Similar hydrothermal manganese deopsits most probably occur in other active areas of the modern seafloors and in inactive island arcs.
    Keywords: Date/Time of event; Deposit type; DEPTH, sediment/rock; Description; DV408/St_1; DV408/St_2; DV408/St_3; DV408/St_4; Elevation of event; Event label; Kaikata Seamount, Pacific Ocean; Latitude of event; Longitude of event; Na8906; Natsushima; NOAA and MMS Marine Minerals Geochemical Database; NOAA-MMS; Position; Quantity of deposit; S2000; Sample ID; Sediment type; Shinkai2000_408-S1; Shinkai2000_408-S2; Shinkai2000_408-S3; Shinkai2000_408-S4; Shinkai2000_DV408; Size; Submersible Shinkai 2000; Substrate type; Uniform resource locator/link to image
    Type: Dataset
    Format: text/tab-separated-values, 32 data points
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  • 28
    Publication Date: 2023-08-26
    Keywords: Activity; Activity, standard deviation; Arctowski_Meteo; Arctowski-Station; Henryk Arctowski Polish Ant. Station; King George Island, Antarctic Peninsula; Long-term meteorological data; Material; Sample, optional label/labor no; STAT; Station; δ13C
    Type: Dataset
    Format: text/tab-separated-values, 25 data points
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  • 29
    Publication Date: 2023-07-24
    Keywords: 40-360; AGE; Cibicidoides spp., δ13C; Cibicidoides spp., δ18O; Deep Sea Drilling Project; DEPTH, sediment/rock; DRILL; Drilling/drill rig; DSDP; DSDP/ODP/IODP sample designation; Glomar Challenger; Leg40; Mass spectrometer Finnigan MAT 251; Sample code/label; South Atlantic
    Type: Dataset
    Format: text/tab-separated-values, 117 data points
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  • 30
    Publication Date: 2023-07-24
    Keywords: 81-553; AGE; Cibicidoides spp., δ13C; Cibicidoides spp., δ18O; Deep Sea Drilling Project; DEPTH, sediment/rock; DRILL; Drilling/drill rig; DSDP; DSDP/ODP/IODP sample designation; Glomar Challenger; Leg81; Mass spectrometer Finnigan MAT 251; North Atlantic/PLATEAU; Sample code/label
    Type: Dataset
    Format: text/tab-separated-values, 264 data points
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  • 31
    Publication Date: 2023-07-24
    Keywords: 82-563; AGE; Cibicidoides spp., δ13C; Cibicidoides spp., δ18O; Deep Sea Drilling Project; DEPTH, sediment/rock; DRILL; Drilling/drill rig; DSDP; DSDP/ODP/IODP sample designation; Glomar Challenger; Leg82; Mass spectrometer Finnigan MAT 251; North Atlantic/RIDGE; Sample code/label
    Type: Dataset
    Format: text/tab-separated-values, 297 data points
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  • 32
    Publication Date: 2023-07-24
    Keywords: 94-608; AGE; Cibicidoides spp., δ13C; Cibicidoides spp., δ18O; Deep Sea Drilling Project; DEPTH, sediment/rock; DRILL; Drilling/drill rig; DSDP; DSDP/ODP/IODP sample designation; Glomar Challenger; Leg94; Mass spectrometer Finnigan MAT 251; North Atlantic/FLANK; Sample code/label
    Type: Dataset
    Format: text/tab-separated-values, 240 data points
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  • 33
    Publication Date: 2023-07-24
    Keywords: 94-607; Age model; Age model, paleomag, Berggren et al (1985); Cibicidoides spp., δ13C; Cibicidoides spp., δ18O; Deep Sea Drilling Project; DEPTH, sediment/rock; DRILL; Drilling/drill rig; DSDP; Glomar Challenger; Leg94; Mass spectrometer Finnigan MAT 251; North Atlantic/FLANK
    Type: Dataset
    Format: text/tab-separated-values, 777 data points
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  • 34
    Publication Date: 2023-07-10
    Keywords: 91-596; Antimony; Arsenic; Barium; Caesium; Chromium; Cobalt; Deep Sea Drilling Project; DEPTH, sediment/rock; DRILL; Drilling/drill rig; DSDP; DSDP/ODP/IODP sample designation; Element analysis, neutron activation (NAA); Glomar Challenger; Iridium; Iron; Leg91; Rubidium; Sample code/label; South Pacific; Tantalum; Thorium
    Type: Dataset
    Format: text/tab-separated-values, 1632 data points
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  • 35
    Publication Date: 2023-07-10
    Keywords: 94-607; Age, comment; Age model; Age model, paleomag, Berggren et al (1985); Deep Sea Drilling Project; Depth, bottom/max; Depth, composite; Depth, composite bottom; Depth, composite top; DEPTH, sediment/rock; Depth, top/min; DRILL; Drilling/drill rig; DSDP; Glomar Challenger; Leg94; North Atlantic/FLANK
    Type: Dataset
    Format: text/tab-separated-values, 42 data points
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  • 36
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    In:  Supplement to: Aldridge, John N; Bergman, Magda J N; Bolam, T; Craeymeersch, Johan A; Degraer, Steven; Duineveld, Gerard C A; Eggleton, J D; Goethals, P; Hillewaert, H; Irion, G; Kershaw, P J; Kröncke, Ingrid; Lavaleye, Marc; Mason, Claire; Rachor, Eike; Rees, H L; Reiss, Henning; Rumohr, Heye; Schratzberger, M; Smith, R; Vanden Berghe, E; van Hoey, G; Vincx, Magda; Willems, W (2007): Structure and dynamics of the North Sea benthos. Ices Cooperative Research Report-Rapport des Recherches Collectives, 288, 265 pp, hdl:10013/epic.34479.d001
    Publication Date: 2023-08-05
    Description: In 1986 participants of the Benthos Ecology Working Group of ICES conducted a synoptic mapping of the infauna of the southern and central North Sea. Together with a mapping of the infauna of the northern North Sea by Eleftheriou and Basford (1989, doi:10.1017/S0025315400049158) this provides the database for the description of the benthic infauna of the whole North Sea in this paper. Division of the infauna into assemblages by TWINSPAN analysis separated northern assemblages from southern assemblages along the 70 m depth contour. Assemblages were further separated by the 30, 50 m and 100 m depth contour as well as by the sediment type. In addition to widely distributed species, cold water species do not occur further south than the northern edge of the Dogger Bank, which corresponds to the 50 m depth contour. Warm water species were not found north of the 100 m depth contour. Some species occur on all types of sediment but most are restricted to a special sediment and therefore these species are limited in their distribution. The factors structuring species distributions and assemblages seem to be temperature, the influence of different water masses, e.g. Atlantic water, the type of sediment and the food supply to the benthos.
    Keywords: ICES 100; ICES 110; ICES 118; ICES 125; ICES 126; ICES 127; ICES 128; ICES 129; ICES 130; ICES 131; ICES 137; ICES 138; ICES 139; ICES 140; ICES 141; ICES 147; ICES 148; ICES 149; ICES 150; ICES 151; ICES 152; ICES 158; ICES 159; ICES 160; ICES 161; ICES 162; ICES 163; ICES 168; ICES 169; ICES 170; ICES 171; ICES 172; ICES 173; ICES 55; ICES 63; ICES 72; ICES 81; ICES 90; MarGIS_DANS_Label: ICES8586BSe_8; North Sea; van Veen Grab; VGRAB; VH1486; VH1486_055; VH1486_063; VH1486_072; VH1486_081; VH1486_090; VH1486_100; VH1486_110; VH1486_118; VH1486_125; VH1486_126; VH1486_127; VH1486_128; VH1486_129; VH1486_130; VH1486_131; VH1486_137; VH1486_138; VH1486_139; VH1486_140; VH1486_141; VH1486_147; VH1486_148; VH1486_149; VH1486_150; VH1486_151; VH1486_152; VH1486_158; VH1486_159; VH1486_160; VH1486_161; VH1486_162; VH1486_163; VH1486_168; VH1486_169; VH1486_170; VH1486_171; VH1486_172; VH1486_173; Victor Hensen; xxxVH1486_091; xxxVH1486_101; xxxVH1486_111; xxxVH1486_124; xxxVH1486_165; xxxVH1486_175; xxxVH1486_177; xxxVH1486_179; xxxVH1486_181; xxxVH1486_184; xxxVH1486_186; xxxVH1486_189; xxxVH1486_192; xxxVH1486_194; xxxVH1486_196; xxxVH1486_199; xxxVH1486_201; xxxVH1486_202; xxxVH1486_205; xxxVH1486_208; xxxVH1486_209; xxxVH1486_210; xxxVH1486_212; xxxVH1486_215; xxxVH1486_217; xxxVH1486_220; xxxVH1486_221; xxxVH1486_222; xxxVH1486_223; xxxVH1486_226; xxxVH1486_227; xxxVH1486_230; xxxVH1486_233; xxxVH1486_234; xxxVH1486_235
    Type: Dataset
    Format: application/zip, 2 datasets
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  • 37
    Publication Date: 2023-07-24
    Keywords: 81-552A; Age model; Age model, paleomag, Berggren et al (1985); Cibicidoides spp., δ13C; Cibicidoides spp., δ18O; Deep Sea Drilling Project; DEPTH, sediment/rock; DRILL; Drilling/drill rig; DSDP; Glomar Challenger; Isotope ratio mass spectrometry; Leg81; North Atlantic/PLATEAU
    Type: Dataset
    Format: text/tab-separated-values, 408 data points
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  • 38
    Publication Date: 2023-07-24
    Keywords: 94-610A; Age model; Age model, paleomag, Berggren et al (1985); Cibicidoides spp., δ13C; Cibicidoides spp., δ18O; Deep Sea Drilling Project; DEPTH, sediment/rock; DRILL; Drilling/drill rig; DSDP; Glomar Challenger; Leg94; Mass spectrometer Finnigan MAT 251; North Atlantic/RIDGE
    Type: Dataset
    Format: text/tab-separated-values, 1011 data points
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  • 39
    facet.materialart.
    Unknown
    PANGAEA
    In:  Supplement to: Klee, Susanne; Baumann, Albrecht; Thiedig, Friedhelm (1992): 9. Age relations of the high grade metamorphic rocks in the Terra Nova Bay Area, North Victoria Land, Antarctica: a preliminary report. Polarforschung, 60(2), 101-106, hdl:10013/epic.29659.d001
    Publication Date: 2023-07-11
    Description: Samples of high grade metamorphic basement rocks of Wilson Terrane cropping out in the Deep Freeze Range and on Kay Island were collected during GANOVEX VI to study their isotopic evolution. The age and origin of granulite facies gneisses and of their migmatite host rocks are especially of interest for the interpretation of the geological and tectonic development of North Victoria Land. Another important research aspect is the influence of the polyphase metamorphic evolution on the isotopic systems of whole rocks and minerals like zircon, garnet, orthopyroxene, amphibole and feldspar.
    Keywords: 500 m NE of Gondwana Station; Age, 206Pb/207Pb Lead-Lead; Age, 235U/207Pb Uranium-Lead; Age, 238U/206Pb Uranium-Lead; Age, dated; ANT102; ANT104; Comment; DEPTH, sediment/rock; Event label; Geological sample; GEOS; Lead; Lead-206; Lead-206/Uranium-238 ratio; Lead-207/Lead-206 ratio; Lead-207/Uranium-235 ratio; Lead-208/Lead-206 ratio; Sample code/label; Sample mass; Size fraction; Uranium; Wilson Terrain, North Victoria Land, Antarctica
    Type: Dataset
    Format: text/tab-separated-values, 192 data points
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  • 40
    Publication Date: 2023-11-01
    Keywords: Atlantic Ocean; Bacterial strains, alteromonas; Bacterial strains, bacillus; Bacterial strains, gram-positiv cocci; Bacterial strains, pseudomonas; Bacterial strains, unidentified gram-negative; Bacterial strains, unidentified gram-positive; Bacterial strains, vibrio; CT; Depth, bathymetric, maximum; Depth, bathymetric, minimum; Depth, bottom/max; DEPTH, sediment/rock; Depth, top/min; GEOTROPEX 83, NOAMP I; Incubation of surface soil/sediment, ex-situ; LATITUDE; LONGITUDE; M65; M65-track; Meteor (1964); Number of isolates; Sample code/label; Temperature, in rock/sediment, maximum; Temperature, in rock/sediment, minimum; Underway cruise track measurements
    Type: Dataset
    Format: text/tab-separated-values, 198 data points
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  • 41
    facet.materialart.
    Unknown
    PANGAEA
    In:  Supplement to: Willkomm, Horst; Bölter, Manfred; Kappen, Ludger (1992): Age estimation of Antarctic Macrolichens by radiocarbon measurements. Polarforschung, 61(2/3), 103-112, hdl:10013/epic.29685.d001
    Publication Date: 2023-08-26
    Description: By the nuclear bomb tests during the 1950s and early 1960s, the radiocarbon content of the atmospheric CO, on the Southern Hemisphere rose within a few years from 98 to 162% of the standard recent value and then dropped to 122% (at the end of 1984). This rapid fluctuation was used to determine the lifetime of five species of lichens collected in the beginning of 1985 in the maritime Antarctic. Under the assumption that Lichens assimilate each year carbon at the same rate and that carbon once fixed at least in main branches never will be exchanged later on. The age of mature thalli of Caioplaco regalis, Ramalino tetebrata and Ustiea antarctica was determined to 32 years, while U, aurantiaco-atra and Himantormia lugubris gave an age of ca. 38 years and ca. 60 years, respectively.
    Keywords: Arctowski_Meteo; Arctowski-Station; Henryk Arctowski Polish Ant. Station; King George Island, Antarctic Peninsula; Long-term meteorological data; STAT; Station
    Type: Dataset
    Format: application/zip, 2 datasets
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  • 42
    Publication Date: 2023-08-26
    Keywords: Activity; Activity, standard deviation; Arctowski_Meteo; Arctowski-Station; Henryk Arctowski Polish Ant. Station; King George Island, Antarctic Peninsula; Long-term meteorological data; Sample, optional label/labor no; Species; STAT; Station; δ13C
    Type: Dataset
    Format: text/tab-separated-values, 20 data points
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  • 43
    facet.materialart.
    Unknown
    PANGAEA
    In:  Supplement to: de Lange, Gert J; van Os, B; Poorter, R (1992): Geochemical composition and inferred accretion rates of sediments and managanese nodules from a submarine hill in the Madeira Abyssal Plain, eastern North Atlantic. Marine Geology, 109(1-2), 171-194, https://doi.org/10.1016/0025-3227(92)90227-9
    Publication Date: 2023-08-28
    Description: The porewater and sediment composition of two boxcores and of a small gravity core, taken on a manganese-nodule-covered hill and in the Madeira Abyssal Plain proper respectively, are compared. The pore-water study of the two boxcores indicates that oxic conditions prevail in both cores. In addition, it indicates that no detectable fluxes of Mn or Fe occur from the porewater to the ocean bottom water. Variations in the geochemical composition of the sediments can be explained by fluctuations in the amount of carbonate, which acts as a diluting agent. A clear carbonate minimum is observed at 20-22 cm depth in the two cores. This minimum is likely to be associated with the last glacial period (10-20 kyr B.P.). This association is supported by the sediment accumulation rate of 15 mm/kyr as found by extrapolation from the rate for pelagic sediments in the Madeira Abyssal Plain. The bulk composition of the manganese nodules recovered from the submarine hill is chemically almost identical to the average composition of Atlantic nodules. The trace metal and Rare Earth Elements composition indicate a hydrogenous origin for the manganese nodules of this study. On the basis of the chemical composition, and that of nodules relative to that of the adjacent sediments, an average nodule accretian rate of 2.8-3.3 mm/myr has been calculated. Although the analyses of the entire ferromanganese nodules that have been studied seem to indicate a homogenous composition, internal structures of the nodules reveal great inhomogeneity, both visually and chemically. These fluctuations may be related to variations in the fluxes of Mn and Fe, which in turn could be climate-related.
    Keywords: NOAA and MMS Marine Minerals Geochemical Database; NOAA-MMS
    Type: Dataset
    Format: application/zip, 2 datasets
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  • 44
    facet.materialart.
    Unknown
    PANGAEA
    In:  Supplement to: Cornwell, Jeffrey C; Kipphut, G W (1992): Biogeochemistry of manganese- and iron-rich sediments in Toolik Lake, Alaska. Hydrobiologia, 240(1-3), 45-59, https://doi.org/10.1007/BF00013451
    Publication Date: 2023-08-28
    Description: The sediments within Toolik Lake in arctic Alaska are characterized by extremely low rates of organic matter sedimentation and unusually high concentrations of iron and manganese. Pore water and solid phase measurements of iron, manganese, trace metals, carbon, nitrogen, phosphorus, and sulfur are consistent with the hypothesis that the reduction of organic matter by iron and manganese is the most important biogeochemical reaction within the sediment. Very low rates of dissolved oxygen consumption by the sediments result in an oxidizing environment at the sediment-water interface. This results in high retention of upwardly-diffusing iron and manganese and the formation of metal-enriched sediment. Phosphate in sediment pore waters is strongly adsorbed by the metal-enriched phases. Consequently, fluxes of phosphorus from the sediments to overlying waters are very small and contribute to the oligotrophic nature of the Toolik Lake aquatic system. Toolik Lake contains an unusual type of lacustrine sediment, and in many ways the sediments are similar to those found in oligotrophic oceanic environments.
    Keywords: Aluminium; Atomic absorption spectrometry (AAS); Barium; Biogenic silica; Calcium; Carbon, organic, total; Carbon in carbonate; Chromium; Cobalt; Colorimetric; Copper; Core; CORE; Depth, bathymetric; Depth, bottom/max; DEPTH, sediment/rock; Depth, top/min; Description; Element analyser CHN; Event label; Gas chromatography; Iron; Latitude of event; Longitude of event; Magnesium; Manganese; Nickel; Nitrogen, total; NOAA and MMS Marine Minerals Geochemical Database; NOAA-MMS; Phosphorus; Potassium; TCK-A; TCK-B; TCK-C; TCK-D; TCK-E; TCK-F; TCK-G; TCK-H; TCK-I; TCK-J; TCK-K; TCK-L; Toolik Lake, Alaska; Zinc
    Type: Dataset
    Format: text/tab-separated-values, 243 data points
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  • 45
    Publication Date: 2023-08-28
    Keywords: 86B12; 86B26; APNAP1; Atlantic Ocean; BC; Box corer; Deposit type; Depth, bottom/max; DEPTH, sediment/rock; Depth, top/min; Description; Elevation of event; Event label; Latitude of event; Longitude of event; Method/Device of event; NOAA and MMS Marine Minerals Geochemical Database; NOAA-MMS; Position; Quantity of deposit; Sample ID; Sediment type; Size; T86-B12; T86-B26; Tyro
    Type: Dataset
    Format: text/tab-separated-values, 34 data points
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  • 46
    Publication Date: 2023-08-28
    Keywords: 86B12; Aluminium; APNAP1; Arsenic; Atlantic Ocean; Barium; BC; Box corer; Cadmium; Calcium; Cerium; Chromium; Cobalt; Copper; DEPTH, sediment/rock; Description; Europium; Hafnium; Inductively coupled plasma - mass spectrometry (ICP-MS); Iron; Lanthanum; Lead; Lutetium; Magnesium; Manganese; Molybdenum; Neodymium; Nickel; NOAA and MMS Marine Minerals Geochemical Database; NOAA-MMS; Phosphorus; Potassium; Samarium; Sample ID; Sodium; Strontium; Sulfur, total; T86-B12; Terbium; Thorium; Titanium; Tyro; Vanadium; Ytterbium; Yttrium; Zinc; Zirconium
    Type: Dataset
    Format: text/tab-separated-values, 36 data points
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  • 47
    Publication Date: 2023-08-28
    Keywords: Comment; Deposit type; Description; Event label; HALCSR-A; HALCSR-B; HAM; Hammer; Identification; Mina el Frances, Costa Rica; NOAA and MMS Marine Minerals Geochemical Database; NOAA-MMS; Punta Conchal, Costa Rica; Quantity of deposit; Sediment type; Size
    Type: Dataset
    Format: text/tab-separated-values, 14 data points
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  • 48
    facet.materialart.
    Unknown
    PANGAEA
    In:  Supplement to: Halbach, Peter; Gursky, H J; Gursky, M M; Schmidt-Effing, R; Maresch, W V (1992): Composition and formation of fossil manganese nodules in Jurassic to Cretaceous radiolarites from the Nicoya Ophiolite Complex (NW Costa Rica). Mineralium Deposita, 27(2), 153-160, https://doi.org/10.1007/BF00197101
    Publication Date: 2023-08-28
    Description: Horizons of several types of Upper Jurassic to Lower Cretaceous manganese nodules occur locally in sequences of radiolarian cherts within the Nicoya Ophiolite Complex (NW Costa Rica). Field studies, X-ray diffraction analysis, petrographic, chemical and experimental studies give evidence of a sedimentary, early diagenetic origin of the nodules, in contrast to earlier suggestions. Smooth, discoidal, compact and very dense nodules with diameters of some mm to 9 cm dominate. They are characterized by braunite, hollandite, pyrolusite and quartz as well as 39-61% Mn, 0.9-1.6% Fe, 5-26% SiO2, 1.3-1.9% Al2O3, 1.5-3.0% Ba, 460-5400 ppm Cu, 85-340 ppm Ni and 40-130 ppm Co, among others. It is suggested that the original mineralogy (todorokite?) was altered during thermometamorphic (braunite) and hydrothermal (hollandite. pyrolusite) events. Petrographic similarities between the fossil nodules and modern deep-sea nodules are striking. Using standard hydrothermal techniques in an experimental study it is shown that under special conditions, braunite can be produced from modern nodule material.
    Keywords: NOAA and MMS Marine Minerals Geochemical Database; NOAA-MMS
    Type: Dataset
    Format: application/zip, 2 datasets
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  • 49
    Publication Date: 2023-08-28
    Description: The cores and dredges described at this site were taken on the REDSED cruise from 2 to 22 September 1992 by the Muséum National d'Histoire Naturelle from the R/V Marion Dufresne. A total of 60 cores and dredges were recovered and are available at MNHN for sampling and study.
    Keywords: Deposit type; Depth, bottom/max; DEPTH, sediment/rock; Depth, top/min; Description; Feature; Marion Dufresne (1972); MD73; MD73-48; MD-GS921037; NOAA and MMS Marine Minerals Geochemical Database; NOAA-MMS; PC; Piston corer; Position; Redsed; Sample code/label; Sediment type; Visual description
    Type: Dataset
    Format: text/tab-separated-values, 8 data points
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  • 50
    Publication Date: 2023-07-24
    Keywords: 90-588_Site; Allomorphina pacifica; Anomalinoides globulosus; Anomalinoides sp.; Anomalinoides spp.; Astrononion spp.; Bolivina cf. anastomosa; Bolivina decussata; Bolivina minuta; Bolivina robusta; Bolivina seminuda; Bolivina sp.; Bolivina spp.; Bolivinopsis sp.; Bulimina rostrata; Bulimina spp.; Bulimina striata; Cassidella bradyi; Cassidulina carinata; Cassidulina sp.; Cassidulina spp.; Cibicidoides bradyi; Cibicidoides cf. opacus; Cibicidoides kullenbergi; Cibicidoides lobatulus; Cibicidoides mundulus; Cibicidoides pseudoungerianus; Cibicidoides sp.; Cibicidoides spp.; Cibicidoides wuellerstorfi; COMPCORE; Composite Core; Counting 〉63 µm fraction; Deep Sea Drilling Project; Dentalina spp.; Discorbinella bertheloti; Discorbis spp.; DSDP; DSDP/ODP/IODP sample designation; Eggerella spp.; Ehrenbergina hystrix; Ehrenbergina trigona; Epistominella exigua; Epistominella rotunda; Epistominella rugosa; Epistominella sp.; Epistominella umbonifera; Epoch; Fissurina spp.; Foraminifera, benthic; Foraminifera, benthic indeterminata; Gaudryina sp.; Gavelinella sp.; Gavelinopsis lobatulus; Globocassidulina ornata; Globocassidulina subglobosa; Glomar Challenger; Gyroidina acuta; Gyroidina broeckhiana; Gyroidina cf. quinqueloba; Gyroidina lamarckiana; Gyroidina neosoldanii; Gyroidina sp.; Gyroidina spp.; Hanzawaia spp.; Heronallenia spp.; Karreriella bradyi; Lagena spp.; Laticarinina altocamerata; Laticarinina pauperata; Leg90; Lenticulina spp.; Martinottiella spp.; Melonis barleeanus; Melonis cf. nicobarensis; Melonis spp.; Nodosaria spp.; Nonionella spp.; Oolina spp.; Ophthalmidium pusillum; Oridorsalis sp.; Oridorsalis umbonatus; Osangularia culter; Parafissurina spp.; Pleurostomella spp.; Pullenia bulloides; Pullenia osloensis; Pullenia quinqueloba; Pullenia sp.; Pullenia spp.; Pyrgo murrhina; Pyrgo spp.; Pyrulina spp.; Quinqueloculina spp.; Rectuvigerina sp.; Sample code/label; Seabrookia earlandi; Sigmoilina edwardsi; Sigmoilopsis schlumbergeri; Siphonaperta sp.; Siphonina australis; Siphotextularia rolshauseni; Siphotextularia spp.; South Pacific/Tasman Sea/CONT RISE; Sphaeroidina bulloides; Spiroloculina sp.; Stainforthia complanata; Stilostomella spp.; Textularia lythostrata; Textularia spp.; Trifarina sp.; Triloculina tricarinata; Uvigerina hispida; Uvigerina peregrina; Uvigerina proboscidea; Uvigerina spp.; Uvigerina vadescens; Vaginulina spp.; Valvulineria sp.; Virgulopsis sp.
    Type: Dataset
    Format: text/tab-separated-values, 5382 data points
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  • 51
    Publication Date: 2023-08-05
    Keywords: Abra alba; Abra nitida; Abra prismatica; Acanthocardia echinata; Acidostoma obesum; Acidostoma sarsi; Acrenhydrosoma perplexum; Acrocnida brachiata; Acteon tornatilis; Ameira brevipes; Ameira parvula; Ameira pusilla; Ameira sp.; Ameiropsis brevicornis; Ameiropsis mixta; Ampelisca brevicornis; Ampelisca diadema; Ampelisca macrocephala; Ampelisca spinipes; Ampelisca tenuicornis; Ampelisca typica; Ampharete; Ampharete baltica; Ampharete falcata; Ampharete finmarchica; Amphicteis gunneri; Amphictene auricoma; Amphitrite cirrata; Amphiura chiajei; Amphiura filiformis; Anaitides; Anaitides groenlandica; Anaitides longipes; Anaitides mucosa; Anaitides rosea; Anobothrus gracilis; Antalis entalis; Anthozoa; Antinoella sarsi; Aonides paucibranchiata; Aoridae; Apherusa ovalipes; Aphrodita aculeata; Arctica islandica; Arenocaris bifida; Arenosetella germanica; Arenosetella sp.; Aricidea catherinae; Aricidea cerrutii; Aricidea simonae; Armina loveni; Ascidiacea; Asellopsis intermedia; Astarte sulcata; Bathyporeia elegans; Bathyporeia tenuipes; Brachyura; Brada villosa; Bradya scotti; Bradya typica; Brissopsis lyrifera; Bulbamphiascus imus; Bulbamphiascus sp.; Byblis gaimardi; Callianassa subterranea; Campylaspis glabra; Campylaspis rubicunda; Canuella perplexa; Capitellidae; Chaetoderma nitidulum; Chaetoparia nilssoni; Chaetopterus variopedatus; Chaetozone setosa; Chamelea gallina; Cheirocratus intermedius; Cirratulus cirratus; Cletodes limicola; Cletodes longicaudatus; Cletodes pusillus; Cletodes sp.; Cletodes tenuipes; Cletodidae sp.; Cnidaria; Cochlodesma praetenue; Colus gracilis; Copepoda; Corbula gibba; Corophium crassicorne; Corystes cassivelaunus; Counting; Curveulima macrophthalmica; Cylichna cylindracea; Dactylopusia tisboides; Danielssenia typica; Date/Time of event; DEPTH, sediment/rock; Diastylis boecki; Diastylis bradyi; Diastylis laevis; Diastylis lucifera; Diastylis rathkei; Diplocirrus glaucus; Ditrupa arietina; Dosinia exoleta; Dyopedos monacanthus; Echinocardium cordatum; Echinocardium flavescens; Echinocyamus pusillus; Echiurus echiurus; Eclysippe vanelli; Ectinosoma melaniceps; Ectinosoma normani; Ectinosoma sp.; Ectinosoma tenuipes; Enhydrosoma buchholtzi; Enhydrosoma sp.; Enipo kinbergi; Enteropneusta; Epitonium trevelyanum; Ericthonius difformis; Eriopisa elongata; Eteone flava; Eteone foliosa; Eteone longa; Euclymene; Euclymene droebachiensis; Eudorella emarginata; Eudorella truncatula; Eudorellopsis deformis; Eulima bilineata; Eumida sanguinea; Eusyllis blomstrandi; Euterpina acutifrons; Evansula pygmaea; Event label; Exogone hebes; Exogone verugera; Fabulina fabula; Facelina bostoniensis; Gammaropsis nitida; Gari fervensis; Gastrotricha; Gattyana cirrosa; Glycera; Glycera alba; Glycera celtica; Glycera lapidum; Glycera rouxi; Glycera tridactyla; Glycinde nordmanni; Goniada maculata; Goniada norvegica; Halectinosoma gothiceps; Halectinosoma herdmani; Halectinosoma propinquum; Halectinosoma sarsi; Halectinosoma sp.; Haloschizopera bulbifera; Haloschizopera pygmaea; Haploops tubicola; Harmothoe; Harmothoe antilopes; Harmothoe castanea; Harmothoe glabra; Harmothoe impar; Harmothoe lunulata; Harmothoe mcintoshi; Harpinia antennaria; Harpinia crenulata; Hastigerella sp.; Hemilamprops rosea; Heteroclymene robusta; Heterolaophonte sp.; Heterolaophonte stroemi; Hippomedon denticulatus; Holothurioidea; Hyala vitrea; Hyalinoecia tubicola; Hyas coarctatus; Hydroides norvegica; Hydrozoa; ICES 100; ICES 109; ICES 110; ICES 118; ICES 119; ICES 120; ICES 125; ICES 126; ICES 127; ICES 128; ICES 129; ICES 130; ICES 131; ICES 137; ICES 138; ICES 139; ICES 140; ICES 141; ICES 142; ICES 143; ICES 147; ICES 148; ICES 149; ICES 150; ICES 151; ICES 152; ICES 153; ICES 158; ICES 159; ICES 160; ICES 161; ICES 162; ICES 163; ICES 168; ICES 169; ICES 170; ICES 171; ICES 172; ICES 173; ICES 55; ICES 63; ICES 72; ICES 81; ICES 90; ICES 99; Idyanthe pusilla; Idyella exigua; Idyella major; Idyella pallidula; Idyellopsis typica; Interleptomesochra eulittoralis; Interleptomesochra tenuicornis; Iphimedia obesa; Isopoda; Kinorhyncha; Lagis koreni; Langerhansia cornuta; Lanice conchilega; Laonice cirrata; Laophonte cornuta; Laophonte inornata; Laophonte longicaudata; Latitude of event; Leptastacus laticaudatus; Leptastacus sp.; Leucothoe lilljeborgi; Levinsenia gracilis; Liocarcinus holsatus; Longipedia coronata; Longipedia helgolandica; Longipedia scotti; Longitude of event; Lucinoma borealis; Lumbrineris; Lumbrineris fragilis; Lumbrineris hibernica; Lumbrineris latreilli; Lumbrineris tetraura; Lunatia montagui; Lunatia poliana; Lysilla loveni; Mactra stultorum; Magelona; Magelona alleni; Maldane sarsi; Maldanidae; MarGIS_DANS_Label: ICES8586BSe_8; Megamphopus cornutus; Microphthalmus; Minuspio cirrifera; Molgula; Montacuta substriata; Mya truncata; Myriochele; Mysella bidentata; Nebalia bipes; Nematoda; Nemertea; Neomenia carinata; Nephtys; Nephtys caeca; Nephtys hombergii; Nephtys incisa; Nephtys longosetosa; Nereimyra punctata; Nereiphylla; Nereis zonata; Nicomache; Nicomache lumbricalis; North Sea; Nothria conchylega; Notomastus latericeus; Nucula nitidosa; Nuculoma tenuis; Nyctiphanes couchi; Ophelia borealis; Ophelina acuminata; Ophiodromus flexuosus; Ophiura affinis; Ophiura albida; Ophiura ophiura; Orbinia sertulata; Ostracoda; Owenia fusiformis; Paphia rhomboides; Paralaophonte congenera; Paraleptastacus espinulatus; Paraleptastacus holsaticus; Paraleptastacus spinicauda; Paramphiascoides vararensis; Paramphiascopsis longirostris; Paramphinome jeffreysii; Paramphitrite tetrabranchia; Paranannopus sp.; Parapleustes bicuspis; Parvicardium minimum; Phaxas pellucidus; Philine quadrata; Philine scabra; Philomedes globosus; Pholoe; Phoronis; Photis longicaudata; Photis reinhardi; Phoxocephalus holbolli; Phtisica marina; Pisione remota; Poecilochaetus serpens; Polychaeta; Polydora caulleryi; Polydora ciliata; Polynoidae; Polyphysia crassa; Pontocrates; Pontocrates longimanus; Praxillella affinis; Praxillura longissima; Priapulida; Prionospio malmgreni; Proameira hiddensoensis; Proameira sp.; Protomedeia fasciata; Psammotopa phyllosetosa; Pseudameira crassicornis; Pseudameira perplexa; Pseudameira sp.; Pseudamphiascopsis herdmani; Pseudobradya pulchella; Pseudobradya sp.; Pseudocuma simile; Pseudolaophonte spinosa; Pseudomesochra longifurcata; Pseudomesochra sp.; Pseudonychocamptus proximus; Pseudopolydora cf. pauchibranchiata; Pseudopolydora pulchra; Pseudosarsameira exilis; Pseudotachidius coronatus; Rhodine gracilior; Sabellidae; Sample code/label; Samytha sexcirrata; Sarsameira parva; Sarsameira sp.; Saxicavella jeffreysi; Scalibregma inflatum; Scolelepis bonnieri; Scolelepis tridentata; Scoloplos armiger; Scopelocheirus hopei; Sicameira leptoderma; Siphonoecetes striatus; Sipunculida indeterminata; Spatangus purpureus; Sphaerodorum flavum; Spiochaetopterus typicus; Spio filicornis; Spio mecznikowianus; Spiophanes bombyx; Spiophanes kroeyeri; Spisula subtruncata; Stenhelia aemula; Stenhelia gibba; Stenhelia sp.; Stenothoe monoculoides; Sthenelais limicola; Streblosoma bairdi; Stylicletodes longicaudatus; Synelmis klatti; Tachidiella minuta; Tachidiella sp.; Tachidiopsis cyclopoides; Tanaidacea; Tardigrada; Tellimya ferruginosa; Terebellides stroemii; Tharyx; Thelepus cincinnatus; Thracia phaseolina; Thyasira; Thyasira ferruginea; Timoclea ovata; Tiron spiniferum; Tisbe sp.; Tmetonyx cicada; Travisia forbesii; Trichobranchus roseus; Tridonta montagui; Tritonia hombergii; Tryphosites longipes; Turbellaria; Turbonilla crenata; Turritella communis; Typhlamphiascus confusus; Typhlamphiascus gracilis; Unciola planipes; Urothoe elegans; van Veen Grab; VGRAB; VH1486; VH1486_055; VH1486_063; VH1486_072; VH1486_081; VH1486_090; VH1486_099; VH1486_100; VH1486_109; VH1486_110; VH1486_118; VH1486_119; VH1486_120; VH1486_125; VH1486_126; VH1486_127; VH1486_128; VH1486_129; VH1486_130; VH1486_131; VH1486_137; VH1486_138; VH1486_139; VH1486_140; VH1486_141; VH1486_142;
    Type: Dataset
    Format: text/tab-separated-values, 27432 data points
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  • 52
    Publication Date: 2023-07-10
    Keywords: Chiasmolithus eograndis; Chiasmolithus expansus; Chiasmolithus grandis; Chiasmolithus solitus; Coccolithus formosus; Coccolithus pelagicus; DEPTH, sediment/rock; Discoaster barbadiensis; Discoaster kuepperi; Discoaster lodoensis; Discoaster saipanensis; Discoaster spp.; Discoaster sublodoensis; ELT13; ELT13.004-PC; Eltanin; Helicosphaera sp.; Markalius inversus; Nannofossil abundance; Nannofossils preservation; Neococcolithes dubius; PC; Piston corer; Reticulofenestra samodurovii; Sphenolithus moriformis; Toweius magnicrassus; Tribrachiatus orthostylus
    Type: Dataset
    Format: text/tab-separated-values, 105 data points
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  • 53
    Publication Date: 2023-07-10
    Keywords: Chiasmolithus expansus; Chiasmolithus grandis; Chiasmolithus solitus; Coccolithus formosus; Coccolithus pelagicus; DEPTH, sediment/rock; Discoaster spp.; ELT24; ELT24.010-PC; Eltanin; Nannofossil abundance; Nannofossils preservation; Neococcolithes dubius; PC; Piston corer; Reticulofenestra bisecta; Reticulofenestra samodurovii; Reticulofenestra umbilicus; Sphenolithus moriformis; Sphenolithus sp.
    Type: Dataset
    Format: text/tab-separated-values, 56 data points
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  • 54
    Publication Date: 2023-07-10
    Keywords: 27-261; Assipetra infracretacea; Axopodorhabdus cylindratus; Axopodorhabdus dietzmannii; Biscutum dubium; Biscutum ellipticum; Biscutum erismatum; Calcisphere sp.; Conusphaera mexicana minor; Cretarhabdus conicus; Crucibiscutum salebrosum; Cruciellipsis cuvillieri; Cyclagelosphaera argoensis; Cyclagelosphaera margerelii; Deep Sea Drilling Project; Diazomatolithus lehmanii; DRILL; Drilling/drill rig; DSDP; DSDP/ODP/IODP sample designation; Ethmorhabdus gallicus; Ethmorhabdus hauterivianus; Glomar Challenger; Grantarhabdus coronadventis; Haqius circumradiatus; Haquis ellipticus; Heliolithus rotundus; Indian Ocean//PLAIN; Leg27; Manivitella pemmatoidea; Microstaurus chiastus; Microstaurus quadratus; Nannofossils preservation; Pickelhaube furtiva; Podorhabdid; Retecapsa angustiforata; Retecapsa crenulata; Retecapsa surirella; Retecapsid; Rhagodiscus nebulosus; Rotelapillus laffittei; Sample code/label; Speetonia colligata; Stephanolithion bigotii; Tegumentum striatum; Tubodiscus verenae; Vagalapilla matalosa; Vagalapilla sp.; Vagalapilla stradneri; Watznaueria barnesae; Watznaueria biporta; Watznaueria britannica; Watznaueria fossacincta; Watznaueria manivitae; Watznaueria sp.; Zeugrhabdotus cooperi; Zeugrhabdotus embergeri; Zeugrhabdotus erectus; Zeugrhabdotus sp.
    Type: Dataset
    Format: text/tab-separated-values, 3976 data points
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  • 55
    facet.materialart.
    Unknown
    PANGAEA
    In:  Supplement to: Gartner, Stefan (1992): Miocene nannofossil chronology in the North Atlantic, DSDP Site 608. Marine Micropaleontology, 18(4), 307-331, https://doi.org/10.1016/0377-8398(92)90045-L
    Publication Date: 2023-07-10
    Description: DSDP North Atlantic Site 608 yielded an excellent Miocene pelagic section which affords a further opportunity for elucidating the chronology of the calcareous nannofossil succession in the framework of magnetostratigraphic control. Most of the conventional (zonal) markers have been documented for this site and some of the earlier results are confirmed and refined. In addition several unconventional and less known markers have been added. The first two are the highest (last) occurrence of Sphenolithus delphix and Sphenolithus capricornutus at 23.6 Ma, which is immediately above the Oligocene-Miocene boundary as identified by the last occurrence of Reticulofenestra bisecta at 23.7 Ma. The next unconventional datum is the highest (last) occurrence of Ilselithina fusa at 22.8 Ma, which is also the highest (last) occurrence of Helicosphaera recta. Calcidiscus tropicus' lowest (first) occurrence is at 19.5 Ma, which is also the lowest occurrence of Sphenolithus belemnos, and Calcidiscus leptoporus' lowest (first) occurrence coincides with that of Sphenolithus heteromorphus at 18.5 Ma. Sphenolithus dissimilis' highest (last) occurrence is at 18.2 Ma and the Calcidiscus premacintyrei lowest (first) and highest (last) occurrences are, respectively, at 17.7 and 11.7 Ma. Discoaster braarudii occurs from 11.6 to 11.3 Ma and its highest (last) occurrence corresponds to that of Cyclicargolithus floridanus. Minylitha convallis occurs from 9.0 to 6.9 Ma. Within the range of Minylitha, at 8.0 Ma, a major shift occurs in reticulofenestrid placoliths from dominantly large (Reticulofenestra pseudoumbilicus) and medium size (Reticulofenestra minutula) species below to significant numbers of very small species (Dictyococcites productus and Gephyrocapsa) above. This is interpreted to be a major, though perhaps seasonal, change of productivity of the North Atlantic at Site 608. A new genus and species Cryptococcolithus takayamae, is described and a variety, Reticulofenestra pseudoumbilicus var. amplus is identified.
    Keywords: 94-608; Amaurolithus delicatus; Amaurolithus ninae; Amaurolithus primus; Calcidiscus leptoporus; Calcidiscus macintyrei; Calcidiscus premacintyrei; Calcidiscus tropicus; Catinaster calyculus; Catinaster sp.; Coccolithus miopelagicus; Coccolithus pelagicus; Coccolithus pliopelagicus; Coccolithus streckeri; Coronocyclus nitescens; Cribrocentrum latipons; Cryptococcolithus takayamae; Cyclicargolithus floridanus; Cyclolithella cricota; Cyclolithella protoannula; Cyclolithella rotula; Deep Sea Drilling Project; Dictyococcites abisectus; Dictyococcites bisectus; Discoaster asymmetricus; Discoaster bellus; Discoaster berggrenii; Discoaster bollii; Discoaster braarudii; Discoaster brouweri; Discoaster calculosus; Discoaster deflandrei; Discoaster druggii; Discoaster exilis; Discoaster hamatus; Discoaster kugleri; Discoaster loeblichii; Discoaster neohamatus; Discoaster neorectus; Discoaster obtusus; Discoaster pentaradiatus; Discoaster prepentaradiatus; Discoaster quinqueramus; Discoaster surculus; Discoaster variabilis; Discolithina sp.; DRILL; Drilling/drill rig; DSDP; DSDP/ODP/IODP sample designation; Glomar Challenger; Helicosphaera ampliaperta; Helicosphaera carteri; Helicosphaera granulata; Helicosphaera intermedia; Helicosphaera parallela; Helicosphaera perch-nielseniae; Helicosphaera recta; Helicosphaera sellii; Helicosphaera sp.; Helicosphaera truempyi; Ilselithina fusa; Leg94; Minylitha convallis; North Atlantic/FLANK; ORDINAL NUMBER; Reticulofenestra minuta; Reticulofenestra minutula; Reticulofenestra producta; Reticulofenestra pseudoumbilicus; Reticulofenestra pseudoumbilicus var. am; Sample code/label; Scyphosphaera amphora; Scyphosphaera pulcherrima; Sphenolithus abies; Sphenolithus belemnos; Sphenolithus capricornutus; Sphenolithus ciperoensis; Sphenolithus conicus; Sphenolithus delphix; Sphenolithus dissimilis; Sphenolithus heteromorphus; Sphenolithus moriformis; Triquetrorhabdulus carinatus; Triquetrorhabdulus milowii; Triquetrorhabdulus rugosus; Zygrhablithus bijugatus
    Type: Dataset
    Format: text/tab-separated-values, 17143 data points
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  • 56
    Publication Date: 2023-07-10
    Keywords: 79-4; Age, 14C milieu/reservoir corrected (-440 yr); Age, comment; Age, dated; Age, dated material; Age, dated standard deviation; Core; CORE; Depth, composite; DEPTH, sediment/rock; Event label; Håkon Mosby; HM79; HM79-4; HM79-6.2; Norwegian Sea; PC; Piston corer; Quaternary Environment of the Eurasian North; QUEEN
    Type: Dataset
    Format: text/tab-separated-values, 46 data points
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  • 57
    Publication Date: 2023-07-10
    Keywords: 86-580; Actinocyclus curvatulus; Actinocyclus ehrenbergii; Actinocyclus ellipticus; Actinoptychus spp.; AGE; Asteromphalus spp.; Azpeitia nodulifera; Azpeitia tabularis; Chaetoceros spores; Coscinodiscus marginatus; Coscinodiscus oculus-iridis; Coscinodiscus radiatus; Deep Sea Drilling Project; DEPTH, sediment/rock; Diatoms, other; DRILL; Drilling/drill rig; DSDP; DSDP/ODP/IODP sample designation; Glomar Challenger; Hemidiscus cuneiformis; Leg86; Neodenticula kamtschatica; Neodenticula koizumii; Nitzschia fossilis; Nitzschia jouseae; Nitzschia reinholdii; Nitzschia spp.; North Pacific; Paralia sulcata; Rhizosolenia barboi; Rhizosolenia spp.; Rossiella tatsunokuchiensis; Sample code/label; Stellaria spp.; Stephanopyxis spp.; Thalassionema nitzschioides; Thalassiosira antiqua; Thalassiosira convexa; Thalassiosira eccentrica; Thalassiosira jacksonii; Thalassiosira latimarginata; Thalassiosira leptopus; Thalassiosira nidulus; Thalassiosira oestrupii; Thalassiosira spp.; Thalassiothrix longissima
    Type: Dataset
    Format: text/tab-separated-values, 1554 data points
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  • 58
    Publication Date: 2023-12-07
    Keywords: 47-398D; Counting 〉63 µm fraction; Deep Sea Drilling Project; DRILL; Drilling/drill rig; DSDP; DSDP/ODP/IODP sample designation; Glomar Challenger; Leg47; North Atlantic/SEAMOUNT; Number of species; Sample code/label
    Type: Dataset
    Format: text/tab-separated-values, 58 data points
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  • 59
    facet.materialart.
    Unknown
    PANGAEA
    In:  Supplement to: Polyakova, Elena I; Pavlidis, Yury A; Levin, A A (1992): Factors governing diatom fossil distributions in the surface layer of bottom sediments on the Barents Sea shelf. Oceanology, 32(1), 112-119
    Publication Date: 2023-12-06
    Description: The surface layer of bottom sediments on the Barents Sea shelf has an irregular but generally very low abundance of diatoms. Tests of species belonging to present-day diatom flora were absent in nearly half of samples; their abundance was only a few shells per gram of dry sediment in 30% of the samples, it was up to 100 shells per gram in 9% of the samples, and was in thousands of shells per gram in only 13% of the samples. The lowest abundances of diatom shells were found in sediments of the eastern and northeastern parts of the sea owing to unfavorable sedimentation conditions and deficiency of dissolved silica in water. But distribution of diatom species on the surface of bottom sediments is strictly consistent with their present-day ranges. About 30% of the samples contained re-deposited Cretaceous and Paleogene diatoms indicating that bottom sediments have largely formed by scouring and re-deposition of underlying material.
    Keywords: Archive of Ocean Data; ARCOD; Area/locality; Barents Sea; Depth, bottom/max; DEPTH, sediment/rock; Depth, top/min; Elevation of event; Event label; GC; Grab; GRAB; Grain size, sieving; Grain size, sieving/settling tube; Grain size analysis after Petelin (1967, Nauka, Moscow); Gravity corer; Latitude of event; Longitude of event; Professor Shtokman; PS-1268; PS-1301; PS-1303; PS-16; Size fraction 〈 0.001 mm, clay; Size fraction 〉 1 mm, gravel; Size fraction 0.005-0.001 mm; Size fraction 0.010-0.005 mm; Size fraction 0.050-0.010 mm; Size fraction 0.100-0.050 mm; Size fraction 0.250-0.100 mm; Size fraction 0.500-0.250 mm, 1.0-2.0 phi, medium sand; Size fraction 1.000-0.500 mm, 0.0-1.0 phi, coarse sand
    Type: Dataset
    Format: text/tab-separated-values, 36 data points
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  • 60
    Publication Date: 2023-11-25
    Keywords: DEPTH, sediment/rock; ERDC; ERDC-093P; Globigerinoides sacculifer, δ13C; Globigerinoides sacculifer, δ18O; Isotope ratio mass spectrometry; PC; Piston corer; Thomas Washington
    Type: Dataset
    Format: text/tab-separated-values, 382 data points
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  • 61
    Publication Date: 2023-11-25
    Keywords: Age model; Age model, SPECMAP chronology, Imbrie et al. (1984); DEPTH, sediment/rock; PC; Piston corer; RC17; RC17-177; Robert Conrad
    Type: Dataset
    Format: text/tab-separated-values, 33 data points
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  • 62
    facet.materialart.
    Unknown
    PANGAEA
    In:  Supplement to: Shackleton, Nicholas J; Le, Jianning; Mix, Alan C; Hall, Michael A (1992): Carbon istotope records from Pacific surface waters and atmospheric carbon dioxide. Quaternary Science Reviews, 11(4), 387-400, https://doi.org/10.1016/0277-3791(92)90021-Y
    Publication Date: 2023-11-25
    Description: We have stacked planktonic carbon isotope data from three cores in the western equatorial Pacific in order to generate a new reconstruction of atmospheric carbon dioxide over the past 450,000 years. Our new reconstruction resembles that of Shackleton et al. (1983) based on data from East Pacific core V19-30, which successfully predicted features that were subsequently verified by Barnola et al. (1987) in the record from the Vostock ice core. In addition the new data confirm the discovery of Shackleton and Pisias (1985) that changes in atmospheric CO2 lead changes in ice volume and hence probably contributed to the glacial-interglacial cycles. Our new reconstruction avoids some of the deficiencies of the previous reconstruction: in particular the planktonic species (Neogloboquadrina dutertrei), on which the earlier reconstruction depends, does not calcify in truly nutrient-free surface water as the model assumes, whereas our new reconstruction uses Globigerinoides sacculifer which is expected to be more reliable. In addition, the surface waters in the west Pacific are closer to the nutrient-free ideal on which the model (Broecker, 1982) depends. On the other hand, the amplitude of the new reconstruction is significantly smaller than the amplitude observed by Barnola et al. (1987). It is not clear whether this smaller range is a better estimate of the amplitude of the 'biological pump' effect, or whether the true amplitude is reduced by bioturbation in the west Pacific cores that we studied.
    Keywords: ERDC; ERDC-093P; PC; Piston corer; RC17; RC17-177; Robert Conrad; Thomas Washington; V24; V24-109; Vema
    Type: Dataset
    Format: application/zip, 6 datasets
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  • 63
    Publication Date: 2023-11-25
    Keywords: DEPTH, sediment/rock; Globigerinoides sacculifer, δ13C; Globigerinoides sacculifer, δ18O; Isotope ratio mass spectrometry; PC; Piston corer; V24; V24-109; Vema
    Type: Dataset
    Format: text/tab-separated-values, 426 data points
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  • 64
    Publication Date: 2023-11-25
    Keywords: Age model; Age model, SPECMAP chronology, Imbrie et al. (1984); DEPTH, sediment/rock; PC; Piston corer; V24; V24-109; Vema
    Type: Dataset
    Format: text/tab-separated-values, 29 data points
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  • 65
    Publication Date: 2023-11-25
    Keywords: Age model; Age model, SPECMAP chronology, Imbrie et al. (1984); DEPTH, sediment/rock; ERDC; ERDC-093P; PC; Piston corer; Thomas Washington
    Type: Dataset
    Format: text/tab-separated-values, 35 data points
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  • 66
    Publication Date: 2023-11-25
    Keywords: DEPTH, sediment/rock; Globigerinoides sacculifer, δ13C; Globigerinoides sacculifer, δ18O; Isotope ratio mass spectrometry; PC; Piston corer; RC17; RC17-177; Robert Conrad
    Type: Dataset
    Format: text/tab-separated-values, 884 data points
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  • 67
    facet.materialart.
    Unknown
    PANGAEA
    In:  Supplement to: Brummer, Geert-Jan A; van Eijden, AJM (1992): "Blue-ocean" paleoproductivity estimates from pelagic carbonate mass accumulation rates. Marine Micropaleontology, 19(1-2), 99-117, https://doi.org/10.1016/0377-8398(92)90023-D
    Publication Date: 2024-01-09
    Description: More than 95% of the carbon lost from the "blue-ocean" reservoir to the sedimentary sink appears to be transferred as skeletal CaCO3, produced in the surface waters. This skeletal CaCO3 carries a productivity signal which is much better preserved in the underlying pelagic carbonate sediments than that of the refractory organic carbon accompanying it. Here, we develop a new method to quantify this signal in terms of organic carbon paleoproductivity, using the sedimentary mass accumulation rates of pelagic carbonate. These are converted into carbonate transit-paleofluxes, which are then translated into the corresponding transit-fluxes of organic carbon, via the carbonate to organic carbon ratios reported from deep-moored sediment trap experiments in modern blue-ocean environments. Paleoproductivity can then be estimated quantitatively by using published algorithms describing the relationship between the export production of particulate organic carbon at depth and primary productivity in the euphotic zone. Although our approach seems rather straightforward, it contains several pitfalls, the effects of which are highlighted by an example comprising three Paleocene/Oligocene to Recent pelagic carbonate sequences drilled during ODP Leg 121 in the eastern Indian Ocean. Although some extreme values are likely due to errors, such as poorly constrained datum levels and dissolution peaks, the results for the Quaternary and Neogene correlate well from site to site and are within the productivity range of present-day low to medium latitude open oceans. Our method may provide an opportunity to actually quantify blue-ocean primary productivity in sedimentary carbonate environments, but requires validation by other, more established ones.
    Keywords: 121-756; 121-757; 121-758; COMPCORE; Composite Core; Indian Ocean; Joides Resolution; Leg121; Ocean Drilling Program; ODP; South Indian Ridge, South Indian Ocean
    Type: Dataset
    Format: application/zip, 3 datasets
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  • 68
    facet.materialart.
    Unknown
    PANGAEA
    In:  Supplement to: Raymo, Maureen E; Hodell, David A; Jansen, Eystein (1992): Response of deep ocean circulation to initiation of Northern Hemisphere glaciation (3-2 MA). Paleoceanography, 7(5), 645-672, https://doi.org/10.1029/92PA01609
    Publication Date: 2024-01-09
    Description: Carbon isotopic records from benthic foraminifera are used to map patterns of deep ocean circulation between 3 and 2 million years ago, the interval when significant northern hemisphere glaciation began. The delta18O and delta13C data from four Atlantic sites (552, 607, 610, and 704) and one Pacific site (677) show that global cooling over this interval was associated with increased suppression of North Atlantic Deep Water (NADW) formation. However, the relative strength of NADW production was always greater than is observed during late Pleistocene glaciations when extreme decreases in NADW are observed in the deep North Atlantic. Our data indicate that an increase in the equator-to-pole temperature gradient associated with the onset of northern hemisphere glaciation did not intensify deepwater production in the North Atlantic but rather the opposite occurred. This is not unexpected as it is the "warm high-salinity" characteristic, rather than the "low temperature", of thermocline waters that is critical to the deepwater formation process in this region today.
    Keywords: 111-677A; 114-704A; 81-552A; 94-607; 94-610A; Deep Sea Drilling Project; DRILL; Drilling/drill rig; DSDP; Glomar Challenger; Joides Resolution; Leg111; Leg114; Leg81; Leg94; North Atlantic/FLANK; North Atlantic/PLATEAU; North Atlantic/RIDGE; North Pacific Ocean; Ocean Drilling Program; ODP; South Atlantic Ocean
    Type: Dataset
    Format: application/zip, 10 datasets
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  • 69
    facet.materialart.
    Unknown
    PANGAEA
    In:  Supplement to: Ehrmann, Werner; Mackensen, Andreas (1992): Sedimentological evidence for the formation of an East Antarctic ice sheet in Eocene/Oligocene time. Palaeogeography, Palaeoclimatology, Palaeoecology, 93(1-2), 85-112, https://doi.org/10.1016/0031-0182(92)90185-8
    Publication Date: 2024-01-09
    Description: Middle Eocene to late Oligocene sediments recovered at Ocean Drilling Program Sites 689 and 690 on Maud Rise in the southernmost Atlantic Ocean and at Sites 738 and 744 on Kerguelen Plateau in the southernmost Indian Ocean were analysed in order to study the depositional environment and the palaeoclimate. Special emphasis was placed on the reconstruction of the formation of a cryosphere on the Antarctic continent. The investigations include quantifications of carbonate and opal contents, grain size analyses and studies of clay mineral assemblages. The sedimentary sequence at all sites under investigation is highly pelagic, with nannofossil oozes and chalks dominant. The first indication of probable glacierization at sea level is in the form of isolated gravel and terrigenous sand grains, which indicate ice-rafting from middle Eocene time at c. 45.5 Ma. This is supported by enhanced concentrations of detrital chlorite and reworked kaolinite. Probably, some glaciers reached the sea, while most of the continent remained under the influence of a humid and warm to temperate climate. The growth of the inland ice resulted in enhanced physical weathering and in increased contents of detrital chlorite and kaolinite from about 40 Ma. A strengthening of the glacial conditions and the onset of continental East Antarctic glaciation is recorded in early Oligocene sediments with an age of 36 Ma. All major sediment parameters document this event. The clay mineralogy changed between c. 36.3 Ma and c. 35.5 Ma from smectite-dominated assemblages to illite- and chlorite-dominated assemblages, the latter being indicative of physical weathering under cooler climates. Large quantities of ice-rafted gravel and sand accumulated on the Kerguelen Plateau between 36.0 Ma and 35.8 Ma. At the same time, an increase in opal content occurred as well as a decrease in carbonate. The sediment parameters imply that the East Antarctic continent was more or less totally buried beneath the ice during Oligocene time. The ice sheet, however, probably did not have a polar but a temperate character, as indicated by the occurrence of Nothofagus and relatively warm surface water temperatures prohibiting the long-distance transport of debris by icebergs.
    Keywords: 119-738B; 119-738C; 119-744A; DRILL; Drilling/drill rig; Indian Ocean; Joides Resolution; Leg119; Ocean Drilling Program; ODP
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    Format: application/zip, 10 datasets
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  • 70
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    In:  Supplement to: Li, Qianyu; Radford, Sally S; Banner, Fred T (1992): Distribution of microperforate tenuitellid planktonic foraminifers in holes 747A and 749B; Kerguelen Plateau. In: Wise, SW; Schlich, R; et al. (eds.), Proceedings of the Ocean Drilling Program, Scientific Results, College Station, TX (Ocean Drilling Program), 120, 569-594, https://doi.org/10.2973/odp.proc.sr.120.171.1992
    Publication Date: 2024-01-09
    Description: Late Eocene to Pleistocene planktonic foraminifers from Leg 120 Holes 747A and 749B on the Kerguelen Plateau were quantitatively analyzed. Microperforate tenuitellid forms dominate the Oligocene to middle Miocene, and 17 species (including the new species Tenuitella jamesi and Tenuitellinata selleyi) are recorded. A lineage zonation of tenuitellid foraminifers is proposed as an alternative scheme for refinement of the Oligocene-Miocene biostratigraphy in high latitudes. Progressive or abrupt alterations in morphological characters within this lineage, producing different morphotypes or species, coincided with prolonged or sudden changes in paleoclimate. These microperforate planktonic foraminifers thus appear to have potential as indicators of cold-water masses and temperature fluctuations in post-Eocene oceans.
    Keywords: 120-747A; 120-749B; DRILL; Drilling/drill rig; Joides Resolution; Leg120; Ocean Drilling Program; ODP; South Indian Ridge, South Indian Ocean
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  • 71
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    In:  Supplement to: Berggren, William A (1992): Neogene planktonic foraminifer magnetostratigraphy of the southern Kerguelen Plateau (Sites 747, 748, 751). In: Wise, SW; Schlich, R; et al. (eds.), Proceedings of the Ocean Drilling Program, Scientific Results, College Station, TX (Ocean Drilling Program), 120, 631-647, https://doi.org/10.2973/odp.proc.sr.120.153.1992
    Publication Date: 2024-01-09
    Description: With the exception of a brief (2 m.y.) late Miocene-early Pliocene hiatus, an essentially complete Neogene record was recovered on the Kerguelen Plateau in a calcareous biofacies. The stratigraphic distribution of about 30 taxa of Neogene planktonic foraminifers recovered at Sites 747, 748,and 751 (Central and Southern Kerguelen plateaus; approximately 54°-58°S) is recorded. Faunas are characterized by low diversity and high dominance and exhibit a gradual decline in species numbers (reflecting a concomitant increase in biosiliceous forms, particularly diatoms) from about 10 in the early Miocene to 5-8 in the middle Miocene, 3-4 in the late Miocene, to essentially a lone (Neogloboquadrina pachyderma) form in the Pliocene-Pleistocene. A provisional sevenfold biostratigraphic zonation has been formulated that, together with the recovery of a representative Neogene magnetostratigraphic record, may ultimately lead to a correlation with low-latitude magnetobiostratigraphies. The initial appearance of Neogloboquadrina pachyderma is associated with magnetic polarity Chron (MPC) 4 (~7 Ma) and MPC 4A (〉8 Ma) at Sites 747 and 751, respectively.
    Keywords: 120-747A; 120-748B; 120-751A; DRILL; Drilling/drill rig; Joides Resolution; Leg120; Ocean Drilling Program; ODP; South Indian Ridge, South Indian Ocean
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    Format: application/zip, 9 datasets
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  • 72
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    In:  Supplement to: Bralower, Timothy J; Siesser, William G (1992): Cretaceous calcareous nannofossil biostratigraphy of sites 761, 762, and 763, xmouth and Wombat Plateaus, Northwest Australia. In: von Rad, U; Haq, BU; et al. (eds.), Proceedings of the Ocean Drilling Program, Scientific Results, College Station, TX (Ocean Drilling Program), 122, 529-556, https://doi.org/10.2973/odp.proc.sr.122.169.1992
    Publication Date: 2024-01-09
    Description: Three sites drilled during Leg 122, Site 761 on the Wombat Plateau and Sites 762 and 763 on the Exmouth Plateau, provide a composite Cretaceous section ranging in age from Berriasian to Maestrichtian. Together, these sites contain an apparently complete, expanded Aptian-Maestrichtian record. Consistently occurring and moderately well-preserved nannofossil assemblages allow reasonably high biostratigraphic resolution. Our data indicate that traditional middle and Upper Cretaceous nannofossil biozonations are not entirely applicable in this region. In this investigation, we compare in detail the relative ranges of key Cretaceous nannofossil markers in the eastern Indian Ocean and in sections from Europe and North Africa. We have determined which previously used events are applicable, and which additional markers have biostratigraphic utility in this region. Significant differences in Campanian-Maestrichtian assemblages exist between the more northern Site 761 and Sites 762 and 763. Such differences are surprising, considering that these sites are only separated by 3° of latitude. We interpret them as marking a strong thermal gradient over the Exmouth Plateau region. Other results include the recovery of an expanded Albian-Cenomanian sequence containing a mixture of Austral and Tethyan floras, which will enable correlation of biozonations established for these two realms; the recovery of two condensed but apparently complete Cenomanian-Turonian boundary sections; correlation of Upper Cretaceous calcareous nannofossil biostratigraphy with magneto- and foraminifer stratigraphy; and correlation of portions of the Barrow Group equivalents to the Berriasian and Valanginian stages.
    Keywords: 122-761B; 122-762C; 122-763B; DRILL; Drilling/drill rig; Joides Resolution; Leg122; Ocean Drilling Program; ODP; South Indian Ridge, South Indian Ocean
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    Format: application/zip, 6 datasets
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  • 73
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    In:  Supplement to: Siesser, William G; Bralower, Timothy J (1992): Cenozoic calcareous nannofossil biostratigraphy on the Exmouth Plateau, Eastern Indian Ocean. In: von Rad, U; Haq, BU; et al. (eds.), Proceedings of the Ocean Drilling Program, Scientific Results, College Station, TX (Ocean Drilling Program), 122, 601-631, https://doi.org/10.2973/odp.proc.sr.122.162.1992
    Publication Date: 2024-01-09
    Description: Six sites (759-764) were drilled on the Exmouth Plateau during Ocean Drilling Program Leg 122. Nannofossilrich Cenozoic sediments were recovered at all six sites, reflecting the open-ocean conditions that prevailed over the Exmouth Plateau during the Cenozoic. Calcareous nannofossils are abundant, diverse (250 different species identified), and generally well preserved throughout the composite lower Paleocene to Quaternary section. The diversity and preservation of nannofossils permits a high degree of stratigraphic resolution at each site. Site 762 on the central part of the Exmouth Plateau contains an almost unbroken Cenozoic record (only Miocene Zones NN3, NN8, and NN10 are missing). This site may prove to be a useful Cenozoic biostratigraphic and biomagnetochronologic reference section for the eastern Indian Ocean.
    Keywords: 122-760A; 122-761B; 122-762B; 122-762C; 122-763A; DRILL; Drilling/drill rig; Joides Resolution; Leg122; Ocean Drilling Program; ODP; South Indian Ridge, South Indian Ocean
    Type: Dataset
    Format: application/zip, 15 datasets
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  • 74
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    In:  Supplement to: Helby, R; McMinn, Andrew (1992): A preliminary report of early Cretaceous dinocyst floras from Site 765, Argo Abyssal Plain, Northwest Australia. In: Gradstein, FM; Ludden, JN; et al. (eds.), Proceedings of the Ocean Drilling Program, Scientific Results, College Station, TX (Ocean Drilling Program), 123, 407-420, https://doi.org/10.2973/odp.proc.sr.123.121.1992
    Publication Date: 2024-01-09
    Description: Results of a preliminary study of Early Cretaceous dinocyst assemblages from Site 765 on the Argo Abyssal Plain, off northwestern Australia, are presented. The palynological sequence is interpreted in terms of Australian zones and is, in descending order, the late Aptian Diconodinium davidii Zone (Cores 123-765C-33R to -39R), the middle to early Aptian Odontochitina operculata Zone (Cores 123-765C-40R to -49R), the Barremian Muderongia australis Zone (Cores 123-765C-50R to -54R), and the Berriasian lower Batioladinium reticulatum Zone (Core 123-765C-59R). The dating of the sequence as late Aptian to Berriasian on the basis of dinocysts is supported, in part, by data concerning associated foraminiferal, radiolarian, and calcareous nannofossil suites.
    Keywords: 123-765C; DRILL; Drilling/drill rig; Joides Resolution; Leg123; Ocean Drilling Program; ODP; South Indian Ridge, South Indian Ocean
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  • 75
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    In:  Supplement to: Milner, G J (1992): Middle Eocene to early Oligocene foraminifers from the Izu-Bonin Forearc, Hole 786A. In: Fryer, P; Pearce, JA; Stokking, LB; et al. (eds.), Proceedings of the Ocean Drilling Program, Scientific Results, College Station, TX (Ocean Drilling Program), 125, 71-90, https://doi.org/10.2973/odp.proc.sr.125.143.1992
    Publication Date: 2024-01-09
    Description: Drilling at Site 786, located in the center of the Izu-Bonin forearc basin, penetrated an apparently continuous section of middle Eocene/lower Oligocene volcaniclastic breccias and nannofossil oozes. Planktonic foraminiferal faunas underwent a gradual transition from relatively high-diversity middle Eocene through late Eocene tropical or warm-water assemblages to a cooler-water, less diverse assemblage during the early Oligocene. In the cosmopolitan benthic foraminiferal faunas, the major transition occurred during the early late Eocene. Middle Eocene benthic assemblages resembling the bathyal 'Lenticulina' fauna (characterized by Osangularia mexicana, Cibicidoides eocaenus, and several buliminid species) changed to an upper Eocene abyssal 'Globocassidulina subglobosa' fauna (characterized by Cibicidoides praemundulus, Globocassidulina subglobosa, Gyroidinoides girardanus, Oridorsalis umbonatus, and Siphonodosaria aculeata). Even though no large, abrupt faunal changes appear to have been associated with the assumed Eocene/Oligocene boundary, benthic species turnover continued through the late Eocene and into the early Oligocene. This resulted in a slightly lower diversity early Oligocene fauna dominated by three species: Laevidentalina sp., Bulimina jarvisi, and Gyroidinoides girardanus. The progression from a middle Eocene bathyal 'Lenticulina' fauna, rather than an abyssal 'Nuttallides truempyi' fauna, to an abyssal 'Globocassidulina subglobosa' fauna during the early late Eocene, suggests that a bathymetric deepening occurred at Site 786. Increased water depths may have resulted from tectonic subsidence.
    Keywords: 125-786A; DRILL; Drilling/drill rig; Joides Resolution; Leg125; North Pacific Ocean; Ocean Drilling Program; ODP
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  • 76
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    In:  Supplement to: Brenner, Wolfram W (1992): Dinoflagellate cyst stratigraphy of the lower Cretaceous sequence at sites 762 and 763, Exmouth Plateau, Northwest Australia. In: von Rad, U; Haq, BU; et al. (eds.), Proceedings of the Ocean Drilling Program, Scientific Results, College Station, TX (Ocean Drilling Program), 122, 511-528, https://doi.org/10.2973/odp.proc.sr.122.158.1992
    Publication Date: 2024-01-09
    Description: Cores from Leg 122, Sites 762 and 763, were sampled at intervals of one sample per 1.5-m section in the Lower Cretaceous sequences. More than 400 samples were studied, most of which contained dinoflagellate cysts, spores, pollen, and various types of palynoclasts. From the entire palynomorph assemblage mainly dinoflagellate cysts were studied to give a stratigraphic outline for the Lower Cretaceous. Stratigraphic units were interpreted in terms of zones in use for the Jurassic and Cretaceous of Australia. At both sites a condensed Valanginian to Aptian sequence and an expanded middle to late Berriasian sequence containing a rich microplankton assemblage were recovered. Sites 762 and 763 can be correlated with each other and with the wells Eendracht-1 and Vinck-1.
    Keywords: 122-762C; 122-763B; 122-763C; DRILL; Drilling/drill rig; Joides Resolution; Leg122; Ocean Drilling Program; ODP; South Indian Ridge, South Indian Ocean
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    Format: application/zip, 3 datasets
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  • 77
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    In:  Supplement to: Dépêche, Francoise; Crasquin-Soleau, Sylvie (1992): Triassic marine ostracodes of the Australain Margin (Holes 759B, 760B, 761C, and 764B). In: von Rad, U; Haq, BU; et al. (eds.), Proceedings of the Ocean Drilling Program, Scientific Results, College Station, TX (Ocean Drilling Program), 122, 453-462, https://doi.org/10.2973/odp.proc.sr.122.177.1992
    Publication Date: 2024-01-09
    Description: Sixty-five species of benthic ostracodes have been discovered in the Triassic sediments of Ocean Drilling Program Leg 122, drilled on the northwestern margin of Australia. Known species were found in the samples studied from the upper Norian-Rhaetian at Holes 759B and 760B and from the Rhaetian at Holes 761C, 764A, and 764B. A large part of material of the recovered ostracodes belong to taxa that are related to ostracodes described in the Tethyan province. Seven species are known from northwestern Europe and five from Iran. Ogmoconcha and Rhombocythere, which are stratigraphically important genera in northern Europe, extend into the Tethyan province. Species of Ogmoconcha are present in Holes 760B, 764A, and 764B. The highly ornate baidiids of the Alpine Tethyan province are dominant in Hole 761C. The affinities with the fauna of Iran noted by Kristan-Tollmann are corroborated by the presence of the genera Mostlerella, Hiatobairdia, and other bairdiids.
    Keywords: 122-759B; 122-760B; 122-761C; 122-764A; DRILL; Drilling/drill rig; Joides Resolution; Leg122; Ocean Drilling Program; ODP; South Indian Ridge, South Indian Ocean
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  • 78
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    In:  Supplement to: Bralower, Timothy J (1992): Stable isotopic, assemblage, and paleoenvironmental investigations of juvenil-ocean sediments recovered on Leg 122, Wombat Plateau, Northwest Australia. In: von Rad, U; Haq, BU; et al. (eds.), Proceedings of the Ocean Drilling Program, Scientific Results, College Station, TX (Ocean Drilling Program), 122, 569-585, https://doi.org/10.2973/odp.proc.sr.122.155.1992
    Publication Date: 2024-01-09
    Description: A sedimentary sequence documenting the early history of the proto-Indian Ocean was drilled at Site 761 on the Wombat Plateau, northwest Australia. Directly above the post-rift unconformity, two lithologic units were recovered which reflect deposition in incipient oceanic environments. The lower unit, composed of sandstone, contains abundant belemnites and a few lenses composed of low-diversity coccolith assemblages. The second unit, composed of chalk, contains abundant calcispheres, thoracospheres, low-diversity coccolith assemblages, and a few radiolarians. Belemnites and organisms that produced calcispheres and thoracospheres are thought to be opportunistic. Their abundance, and the absence of a normal marine fauna and flora, reflects an unstable early ocean environment. Stable oxygen and carbon isotopic data for the two units fall into almost separate fields. Heavy delta18O values for the belemnites indicate that they have not been affected by recrystallization. Instead, these isotopic values are thought to indicate either the deep, cool habitat of the belemnites or strong vital effects. A bulk chalk delta18O value from the belemnite sand is 3 to 4 parts per mil lighter than the belemnite delta18O values, possibly because it is largely composed of coccoliths which inhabited warmer surface waters. Light delta13C values for bulk calcisphere-bearing nannofossil chalk samples are thought to be a direct result of upwelling or of vital effects. Heavy delta18O values for the chalk unit are interpreted as resulting from upwelling of cool waters. Assemblage and isotopic data are consistent with this incipient ocean basin being highly productive, either as a result of upwelling or runoff of nutrient-rich waters from nearby land areas. However, it is not possible to rule out the control of vital effects on the isotopic signature of any of the fossil groups.
    Keywords: 122-761C; DRILL; Drilling/drill rig; Joides Resolution; Leg122; Ocean Drilling Program; ODP; South Indian Ridge, South Indian Ocean
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  • 79
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    In:  Supplement to: Damotte, Renée (1992): Data report: Cretaceous ostracodes from holes 761B and 764A (Wombat Plateau) and holes 762C, 763B, and 763C (Exmouth Plateau). In: von Rad, U; Haq, BU; et al. (eds.), Proceedings of the Ocean Drilling Program, Scientific Results, College Station, TX (Ocean Drilling Program), 122, 819-834, https://doi.org/10.2973/odp.proc.sr.122.175.1992
    Publication Date: 2024-01-09
    Description: The Cretaceous ostracodes species recognized on Leg 122 represent elements of South Gondwanan faunistic province. In Lower and middle Cretaceous cores, ostracodes species present were originally described from South Africa and in cores from Deep Sea Drilling Project Leg 36 (Falkland Plateau): Arculicythere tumida, Bythocypris? cf. nodosa, 'Bythocypris' cf. strogylae, Collosaboris? stanleyensis, Cytherella bensoni, Majungaella nematis, Robsoniella cf. falklandensis and Pirileberis aff. mkuzensis. In Upper Cretaceous levels, the Australian species Apateloschizocythere geniculata, Bairdia austracretacea, Cytherella cf. atypica, Cytherella cf. jonesi, Cytherelloidea cf. carnarvonensis, Cytherelloidea cf. colemani, Karsteneis aspericava, and Trachyleberis anteplana were found.
    Keywords: 122-761B; 122-762C; 122-763B; 122-763C; DRILL; Drilling/drill rig; Joides Resolution; Leg122; Ocean Drilling Program; ODP; South Indian Ridge, South Indian Ocean
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  • 80
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    In:  Supplement to: Zachariasse, Willem-Jan (1992): Neogene planktonic foraminifers from sites 761 and 762 off Northwest Australia. In: von Rad, U; Haq, BU; et al. (eds.), Proceedings of the Ocean Drilling Program, Scientific Results, College Station, TX (Ocean Drilling Program), 122, 665-675, https://doi.org/10.2973/odp.proc.sr.122.190.1992
    Publication Date: 2024-01-09
    Description: Diverse, warm-water planktonic foraminiferal faunas prevailed on the Wombat and Exmouth plateaus during the Neogene, in spite of the northward drift of Australia across 10° to 15° latitude since the early Miocene. Invasions of cool-water species occurred during periods of global cooling in the late middle Miocene, late Miocene, and Pleistocene, and reflect periods of increased northward transport of cool surface water, probably via the West Australian Current. The sedimentary record of the Neogene on Wombat and Exmouth Plateau is interrupted by two hiatuses (lower Miocene, Zone N5, and upper middle to upper Miocene, Zones N15-N17), and one redeposited section of upper Miocene to uppermost Pliocene sediments. Mechanical erosion or nondeposition by increased deep-water flow or tilting and uplift of Wombat and Exmouth plateaus, resulting in sediment shedding, are the most likely explanations for these Miocene hiatuses, but which of these processes were actually operative on the Wombat and Exmouth plateaus is uncertain. The redeposited section of upper Miocene to uppermost Pliocene sediments in Hole 761B, however, certainly reflects a latest Pliocene period of uplift and tilting of the Wombat Plateau. An important finding was the occurrence of Zone N15-correlative sediments in Hole 762B without any representative of Neogloboquadrina. Similar findings in Java and Jamaica indicate that the earliest spreading of Neogloboquadrina acostaensis in the tropical region resulted from migration. The evolution of this species, therefore, must have taken place in higher latitudes. I suggest that Neogloboquadrina acostaensis evolved from Neogloboquadrina atlantica in the North Atlantic within Zone NN9, but how and where in the region this speciation took place is still uncertain
    Keywords: 122-761B; 122-762B; DRILL; Drilling/drill rig; Joides Resolution; Leg122; Ocean Drilling Program; ODP; South Indian Ridge, South Indian Ocean
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  • 81
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    In:  Supplement to: Mutterlose, Jörg (1992): Lower Cretaceous nannofossil biostratigraphy off northwestern Australia (Leg 123). In: Gradstein, FM; Ludden, JN; et al. (eds.), Proceedings of the Ocean Drilling Program, Scientific Results, College Station, TX (Ocean Drilling Program), 123, 343-368, https://doi.org/10.2973/odp.proc.sr.123.124.1992
    Publication Date: 2024-01-09
    Description: Moderately to sparsely nannofossiliferous Neocomian siliciclastics and rich Aptian-Albian nannofossil chalks were cored at two Leg 123 sites on the abyssal plains off northwestern Australia. At Site 765, the basal 70 m of cored section yields questionable Tithonian and Berriasian to early Hauterivian assemblages of moderate diversity containing Cruelellipsis cuvillieri, Tegumentum striatum, Speetonia colligata, and Crucibiscutum salebrosum. The overlying Hauterivianlower Aptian is represented by 140 m of sediments barren of nannofossils. Above this, the remaining 80 m of the Lower Cretaceous section has been assigned to the Rhagodiscus angustus Zone (late Aptian-early Albian in age) and the Prediscosphaera columnata Zone (middle-late Albian in age). Common species include Rhagodiscus angustus, Prediscosphaera columnata, Eprolithus floralis, Eprolithus sp., Chiastozygus litterarius, Rucinolithus irregularis, and Flabellites biforaminis. At Site 766, the Neocomian, represented by 200 m of sediment, yields C. cuvillieri, T. striatum, S. colligata, and C. salebrosum. Within the overlying Aptian-Albian sequence of 80 m, the Rhagodiscus angustus, and P. columnata zones were recognized. The paleobiogeographic patterns and implications are discussed, with special emphasis paid to the bipolar high-latitude distribution pattern of C. salebrosum in the Valanginian-Hauterivian. Biostratigraphically important species are discussed and their occurrence in the Indian Ocean is compared with one from the Tethys and Boreal realms. Two new species, Serbiscutum gaultensis and Eprolithus bettenstaedtii, are described.
    Keywords: 123-765C; 123-766A; DRILL; Drilling/drill rig; Joides Resolution; Leg123; Ocean Drilling Program; ODP; South Indian Ridge, South Indian Ocean
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  • 82
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    In:  Supplement to: Baumgartner, Peter O (1992): Lower Cretaceous radiolarian biostratigraphy and biogeography off northwestern Australia (ODP sites 765 and 766 and DSDP Site 261), Argo Abyssal Plain and lower Exmouth Plateau. In: Gradstein, FM; Ludden, JN; et al. (eds.), Proceedings of the Ocean Drilling Program, Scientific Results, College Station, TX (Ocean Drilling Program), 123, 299-342, https://doi.org/10.2973/odp.proc.sr.123.127.1992
    Publication Date: 2024-01-09
    Description: During Leg 123, abundant and well-preserved Neocomian radiolarians were recovered at Site 765 (Argo Abyssal Plain) and Site 766 (lower Exmouth Plateau). The assemblages are characterized by a scarcity or absence of Tethyan taxa. The Berriasian-early Aptian radiolarian record recovered at Site 765 is unique in its density of well-preserved samples and in its faunal contents. Remarkable contrasts exist between radiolarian assemblages extracted from claystones of Site 765 and reexamined DSDP Site 261, and faunas recovered from radiolarian sand layers of Site 765. Clay faunas are unusual in their low diversity of apparently ecologically tolerant species, whereas sand faunas are dominated by non-Tethyan species that have never been reported before. Comparisons with Sites 766 and 261, as well as sedimentological observations, lead to the conclusion that this faunal contrast results from a difference in provenance, rather than from hydraulic sorting. Biostratigraphic dating proved difficult principally because of the paucity or even absence of (Tethyan) species used in published zonations. In addition, published zonations are contradictory and do not reflect total ranges of species. Radiolarian assemblages recovered from claystones at Sites 765 and 261 in the Argo Basin reflect restricted oceanic conditions for the latest Jurassic to Barremian time period. Neither the sedimentary facies nor the faunal associations bear any resemblance to sediment and radiolarian facies observed in typical Tethyan sequences. I conclude that the Argo Basin was paleoceanographically separated from Tethys during the Late Jurassic and part of the Early Cretaceous by its position at a higher paleolatitude and by enclosing landmasses, i.e., northeastern India and the Shillong Block, which were adjacent to the northwestern Australian margin before the opening. Assemblages recovered from radiolarian sand layers are dominated by non-Tethyan species that are interpreted as circumantarctic. Their sudden appearance in the late Berriasian/early Valanginian pre-dates the oceanization of the Indo-Australian break-up (Ml 1, late Valanginian) by about 5 m.y., but coincides with a sharp increase in margin-derived pelagic turbidites. The Indo-Australian rift zone and its adjacent margins probably were submerged deeply enough to allow an intermittent "spillover" of circumantarctic cold water into the Argo Basin, creating increased bottom current activity. Circumantarctic cold-water radiolarians transported into the Argo Basin upwelled along the margin and died en masse. Concomitant winnowing by bottom currents led to their accumulation in distinct radiolarite layers. High rates of faunal change and the sharp increase of bottom current activity are thought to be synchronous with the two pronounced late Berriasian-early Valanginian lowstands in sea level. Hypothetically, both phenomena might have been caused by a glaciation on the Antarctic-Australian continent, which was for the first time isolated from the rest of Gondwana by oceanic seaways as a result of Jurassic and Early Cretaceous seafloor spreading. The absence of typical Tethyan radiolarian species during the late Valanginian to late Hauterivian period is interpreted as reflecting a time of strong influx of circumantarctic cold water following oceanization (Mil) and rapid spreading between southeast India and western Australia. The reappearance and gradual increase in abundance and diversity of Tethyan forms along with the still dominant circumantarctic species are thought to result from overall more equitable climatic conditions during the Barremian and early Aptian and may have resulted from the establishment of an oceanic connection with the Tethys Ocean during the early Aptian.
    Keywords: 123-765C; 123-766A; DRILL; Drilling/drill rig; Joides Resolution; Leg123; Ocean Drilling Program; ODP; South Indian Ridge, South Indian Ocean
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  • 83
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    In:  Supplement to: Wang, Yu-Jing; Yang, Qun (1992): Neogene and Quaternary radiolarians from Leg 125. In: Fryer, P; Pearce, JA; Stokking, LB; et al. (eds.), Proceedings of the Ocean Drilling Program, Scientific Results, College Station, TX (Ocean Drilling Program), 125, 95-112, https://doi.org/10.2973/odp.proc.sr.125.174.1992
    Publication Date: 2024-01-09
    Description: Radiolarians were recovered from three of the five holes investigated during Leg 125. Relative abundances are estimated at Holes 782A and 784A, where preservation is poor to good. Rare, poorly preserved radiolarians are present in Hole 786A. Seven radiolarian zones are recognized in the latest early- middle Miocene to early Pleistocene of Holes 782A and 784A. These zones are approximately correlated to the zones of Sanfilippo and others published in 1985.
    Keywords: 125-782A; 125-784A; 125-786A; DRILL; Drilling/drill rig; Joides Resolution; Leg125; North Pacific Ocean; Ocean Drilling Program; ODP
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    Format: application/zip, 3 datasets
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  • 84
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    In:  Supplement to: Aitchison, Jonathan C (1992): Radiolarians from sediments of the Izu-Bonin Region, Leg 126. In: Taylor, B; Fujioka, K.; et al. (eds.), Proceedings of the Ocean Drilling Program, Scientific Results, College Station, TX (Ocean Drilling Program), 126, 321-330, https://doi.org/10.2973/odp.proc.sr.126.140.1992
    Publication Date: 2024-01-09
    Description: Radiolarians occur at five Leg 126 sites. Well-preserved radiolarians were recovered from Miocene and Pliocene through Holocene sections. The results of this study may help to fill the informational gap on Quaternary radiolarian distribution at mid-latitudes in the western Pacific. Radiolarian preservation is discontinuous, and, although present in Oligocene sections, specimens are poorly preserved.
    Keywords: 126-787B; 126-790A; 126-790B; 126-790C; 126-791A; 126-791B; 126-792A; 126-792B; 126-792C; 126-792D; 126-792E; 126-793A; 126-793B; DRILL; Drilling/drill rig; Joides Resolution; Leg126; North Pacific Ocean; Ocean Drilling Program; ODP; Philippine Sea
    Type: Dataset
    Format: application/zip, 13 datasets
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  • 85
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    In:  Supplement to: Ehrendorfer, Thomas; Aubry, Marie-Pierre (1992): Calcareous nannoplankton changes across the Cretaceous/Paleocene boundary in the southern Indian Ocean. In: Wise, SW; Schlich, R; et al. (eds.), Proceedings of the Ocean Drilling Program, Scientific Results, College Station, TX (Ocean Drilling Program), 120, 451-470, https://doi.org/10.2973/odp.proc.sr.120.148.1992
    Publication Date: 2024-01-09
    Description: Changes in the composition of calcareous nannoplankton across the Cretaceous/Paleocene boundary at southern high-latitude Ocean Drilling Program Hole 750A are documented in this semiquantitative study. These changes are compared with changes described from other localities at high- and low-latitudes. This study provides additional data toward a detailed documentation of the paleontologic changes that occurred in the late Maestrichtian and the early Paleocene, despite limitations to the interpretation caused by coring gaps, drilling disturbance, and the presence of an unconformity at the boundary at this site.
    Keywords: 120-750A; DRILL; Drilling/drill rig; Joides Resolution; Leg120; Ocean Drilling Program; ODP; South Indian Ridge, South Indian Ocean
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  • 86
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    In:  Supplement to: Hovan, Steven A; Rea, David K (1992): The Cenozoic record of continental mineral deposition on Broken and Ninetyeast Ridges, Indian Ocean: Southern African aridity and sediment delivery from the Himalayas. Paleoceanography, 7(6), 833-860, https://doi.org/10.1029/92PA02176
    Publication Date: 2024-01-09
    Description: The mineral component of pelagic sediments recovered from the Indian Ocean provides both a history of eolian deposition related to climatic changes in southern Africa and a record of terrigenous input related to sediment delivery from the Himalayas. A composite Cenozoic dust flux record from four sites in the central Indian Ocean is used to define the evolution of the Kalahari and Namib desert source regions. The overall record of dust input is one of very low flux for much of the Cenozoic indicating a long history of climate stability and regional hyperaridity. The most significant reduction in dust flux occurred near the Paleocene/Eocene boundary and is interpreted as a shift from semiarid climates during the Paleocene to more arid conditions in the early Eocene. Further aridification is recorded as stepwise reductions in the input of dust material which occur from about 35 to 40 Ma, 27 to 32 Ma, and 13 to 15 Ma and correlate to significant enrichments in benthic foraminifer delta18O values. The mineral flux in sediments from the northern Indian Ocean, site 758, records changes in the terrigenous input apparently related to the erosion of the Himalayas and indicates a rapid late Cenozoic uplift history. Three major pulses of increased terrigeneous sediment flux are inferred from the depositional record. The initial increase began at about 9.5 Ma and continued for roughly 1.0 million years. A second pulse with approximately the same magnitude occurred from about 7.0 to 5.6 Ma. The largest pulse of enhanced terrigenous influx occurred during the Pliocene from about 3.9 to 2.0 Ma when average flux values were severalfold greater than at any other time in the Cenozoic.
    Keywords: 121-756A; 121-757A; 121-758A; 22-215; Deep Sea Drilling Project; DRILL; Drilling/drill rig; DSDP; Glomar Challenger; Indian Ocean; Indian Ocean//BASIN; Joides Resolution; Leg121; Leg22; Ocean Drilling Program; ODP; South Indian Ridge, South Indian Ocean
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    Format: application/zip, 6 datasets
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  • 87
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    In:  Supplement to: Bitschene, Peter Rene; Mehl, Klaus Wilhelm; Schmincke, Hans-Ulrich (1992): Composition and origin of marine ash layers and epiclastic rocks from the Kerguelen Plateau, southern Indian Ocean (Legs 119 and 120). In: Wise, SW; Schlich, R; et al. (eds.), Proceedings of the Ocean Drilling Program, Scientific Results, College Station, TX (Ocean Drilling Program), 120, 135-149, https://doi.org/10.2973/odp.proc.sr.120.132.1992
    Publication Date: 2024-01-09
    Description: Epiclastic volcanogenic rocks recovered from the Kerguelen Plateau during Ocean Drilling Program Legs 119 and 120 comprise (pre-)Cenomanian(?) claystones (52 m thick, Site 750); a Turonian(?) basaltic pebble conglomerate (1.2 m thick, Site 748; Danian mass flows (45 m thick, Site 747); and volcanogenic debris flows of Quaternary age at Site 736 (clastic apron of Kerguelen Island). Pyroclastic rocks comprise numerous Oligocene to Quaternary marine ash layers. The epiclastic sediments with transitional mid-ocean-ridge basalt (T-MORB) origin indicate weathering (Site 750) and erosion (Site 747) of Early Cretaceous T-MORB from a then-emergent Kerguelen Plateau, connected to Late Cretaceous tectonic events. The basal pebble conglomerate of Site 748 has an oceanic-island basalt (OIB) composition and denotes erosion and reworking of seamount to oceanic-island-type volcanic sources. The vitric- to crystal-rich marine ash layers are a few centimeters thick, have rather uniform grain sizes around 60 ± 40 µm, and are a result of Plinian eruptions. Crystal-poor silicic vitric ashes may also represent co-ignimbrite ashes. The ash layers have bimodal, basaltic, and silicic compositions with a few intermediate shards. The basaltic ashes are evolved high-titanium T-MORB; a few grains in a silicic pumice lapilli layer have a low-titanium basaltic composition. The silicic ashes comprise trachytic and rhyolitic glass shards belonging to a high-K series, except for a few low-K glasses admixed to a basaltic ash layer. Feldspar and clinopyroxene compositions fit the glass chemistry: high-Ti tholeiite-basaltic glasses have Plagioclase of An40-80 and pigeonite to augite clinopyroxene compositions. Silicic ashes have K-rich anorthoclase and minor Plagioclase around An20 and ferriaugitic to hedenbergitic clinopyroxene compositions. The line of magmatic evolution for the glass shards is not compatible with simple two-end member (high-Ti T-MORB and high-K rhyolite) mixing, but favors successive Ca-Mg-Fe pyroxene, Ti magnetite, and apatite fractionation, and K-rich alkali feldspar fractionation in trachytic magmas to yield rhyolitic compositions. Plagioclase fractionation occurs throughout. This qualitative model is in basic accordance with the observed mineral assemblage. However, as the time span for explosive volcanism spans 〉30 m.y., this basic model cannot comply with fractional crystallization in a single magma reservoir. The ash layers resulted from highly explosive eruptions on Kerguelen and, with less probability, Heard islands since the Oligocene. The explosive history starts with widespread Oligocene basaltic ash layers that indicate sea-level or subaerial volcanism on the Northern Kerguelen Plateau. After a hiatus of 24 m.y.(?), explosive magmatic activity was vigorously renewed in the late Miocene with more silicic eruptions. A peak in explosive activity is inferred for the Pliocene-Pleistocene. The composition and evolution of Kerguelen Plateau ash layers resemble those from other hotspot-induced, oceanic-island realms such as Iceland and Jan Mayen in the North Atlantic, and the Canary Islands archipelago in the Central Atlantic.
    Keywords: 119-736A; 119-736C; 119-737A; 119-737B; 119-738C; 119-745B; 120-747A; 120-747C; 120-748C; 120-750B; DRILL; Drilling/drill rig; Indian Ocean; Joides Resolution; Leg119; Leg120; Ocean Drilling Program; ODP; South Indian Ridge, South Indian Ocean
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  • 88
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    In:  Supplement to: Mao, Shaozhi; Mohr, Barbara A R (1992): Late Cretaceous dinoflagellate cysts (?Santonian-Maestrichtian) from the southern Indian Ocean (Hole 748C). In: Wise, SW; Schlich, R; et al. (eds.), Proceedings of the Ocean Drilling Program, Scientific Results, College Station, TX (Ocean Drilling Program), 120, 307-341, https://doi.org/10.2973/odp.proc.sr.120.190.1992
    Publication Date: 2024-01-09
    Description: At Ocean Drilling Program Hole 748C in the Southern Indian Ocean, a total of 171 Late Cretaceous dinoflagellate taxa were encountered in 38 productive samples from Cores 120-748C-27R through 120-748C-62R (407-740 mbsf). Four provisional dinoflagellate assemblage zones and five subzones were recognized based on the character of the dinoflagellate flora and the first/last occurrences of some key species. Isabelidinium korojonense and Nelsoniella aceras occur in Zone A together with Oligosphaeridium pulcherrimum and Trithyrodinium suspect urn. Zone B was delineated by the total range of Odontochitina cribropoda. Zone C was separated from Zone B by the presence of Satyrodinium haumuriense, and Zone D is dominated by new taxa. The dinocyst assemblages bear a strong affinity to Australian assemblages. Paleoenvironmental interpretations based mainly on dinocysts suggest that during the ?Santonian-Campanian to the Maestrichtian this portion of the Kerguelen Plateau was a shallow submerged plateau, similar to nearshore to offshore to upper slope environments with water depths of tens to hundreds of meters, but isolated from the major continents of the Southern Hemisphere. Starting perhaps in the late Cenomanian (Mohr and Gee, 1992, doi:10.2973/odp.proc.sr.120.196.1992), the Late Cretaceous transgression over the plateau reached its maximum during the late Campanian. The plateau may have been exposed above sea level and subjected to weathering during the latest Maestrichtian. The studied dinocyst assemblages characterized by species of Amphidiadema, Nelsoniella, Satyrodinium, and Xenikoon together with abundant Chatangiella (the large-size species) and Isabelidinium suggest that a South Indian Province (tentatively named the Helby suite) may have existed during the Campanian-Maestrichtian in comparison with the other four provinces of Lentin and Williams. One new genus, three new species, and two new subspecies of dinocysts are described.
    Keywords: 120-748C; DRILL; Drilling/drill rig; Joides Resolution; Leg120; Ocean Drilling Program; ODP; South Indian Ridge, South Indian Ocean
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  • 89
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    In:  Supplement to: Beaufort, Luc; Aubry, Marie-Pierre (1992): Paleoceanographic implications of a 17-m.y.-long record of high-latitude Miocene calcareous nannoplankton fluctuations. In: Wise, SW; Schlich, R; et al. (eds.), Proceedings of the Ocean Drilling Program, Scientific Results, College Station, TX (Ocean Drilling Program), 120, 539-549, https://doi.org/10.2973/odp.proc.sr.120.147.1992
    Publication Date: 2024-01-09
    Description: A record based on counts of the relative abundance of the dominant calcareous nannofossil taxa Coccolithus pelagicus and Reticulofenestra spp. in sediments recovered from Ocean Drilling Program Hole 747A (Kerguelen Plateau, Southern Indian Ocean) is established in this paper. This record (17 m.y. long) virtually spans the entire Miocene. Broad, steplike variations in the abundance of C. pelagicus range between 0% and 96%. Based on these variations, five stratigraphic units characterized by high abundance in C. pelagicus are delineated. We suggest that these variations are caused by water-mass movements (such as the north/south shifting of a front). This pronounced signal is compared with paleoceanographic events revealed by isotopic (d18O and d13C) studies. The five defined units are tentatively correlated to well-known global isotopic events. In particular, Units A and D correlate respectively with the Oligocene/Miocene boundary glaciation and the middle Miocene cooling event. Time-series analysis indicates the presence of the three main periodic components of the eccentricity of the Earth's orbit. A 200-k.y. cycle is also present. The stratigraphic and paleoceanographic significance of this record is discussed.
    Keywords: 120-747A; DRILL; Drilling/drill rig; Joides Resolution; Leg120; Ocean Drilling Program; ODP; South Indian Ridge, South Indian Ocean
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  • 90
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    In:  Supplement to: Morche, Wolfgang; Hubberten, Hans-Wolfgang; Mackensen, Andreas; Keller, Jörg (1992): Geochemistry of Cenozoic ash layers from the Kerguelen Plateau (Leg 120): a first step toward a tephrostratigraphy of the Southern Indian Ocean. In: Wise, SW; Schlich, R; et al. (eds.), Proceedings of the Ocean Drilling Program, Scientific Results, College Station, TX (Ocean Drilling Program), 120, 151-160, https://doi.org/10.2973/odp.proc.sr.120.163.1992
    Publication Date: 2024-01-09
    Description: Geochemical investigations were conducted on 10 discrete ash layers and 22 samples of dispersed ash accumulations from Sites 747, 749, and 751 of Ocean Drilling Program (ODP) Leg 120 to the Kerguelen Plateau in the southern Indian Ocean. The chemical data obtained from some 400 single-grain glass analyses allow the characterization of two rock series. The first consists of transitional to alkali basalts; the second, mainly of trachytes with subordinated rhyolites, all reflecting the characteristic magmatological evolution of the Kerguelen Plateau as a hotspot-related volcanism. Chemical correlation with possible source areas indicates that the ashes were most probably erupted from the Kerguelen Islands. The investigated ash layers clearly reflect the Oligocene to Quaternary changes in the composition of the volcanic material recorded from the Kerguelen Islands. In addition to the Kerguelen Islands, Heard Island, Crozet Island, and other sources may have contributed to deposition of the tephras. Pleistocene tephras of "exotic" calc-alkaline composition are most probably derived from enhanced magmatic activity during that time span at the South Sandwich island arc. When using data obtained from tephras of the ODP Leg 119 Kerguelen sites, several eruptive periods can be correlated through the composition of the deposited ashes. Some of them are widely distributed over the Kerguelen Plateau and are seen as a first step toward a southern Indian Ocean tephrostratigraphy.
    Keywords: 120-747A; 120-747B; 120-749B; 120-751A; DRILL; Drilling/drill rig; Joides Resolution; Leg120; Ocean Drilling Program; ODP; South Indian Ridge, South Indian Ocean
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  • 91
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    In:  Supplement to: Patience, R L; Baxby, M; Bartle, K D; Perry, DL; Rees, A W G; Rowland, Steve J (1992): The functionality of organic nitrogen in some recent sediments from the Peru upwelling region. Organic Geochemistry, 18(2), 161-169, https://doi.org/10.1016/0146-6380(92)90126-I
    Publication Date: 2024-01-09
    Description: Nitrogen in fossil fuels is present in pyrrolic- and pyridinic-functional groups. In contrast, organic nitrogen in living organisms is overwhelmingly found in amino acids in proteins and peptides. Petroleum is the result of the maturation of the organic remains of organisms, so what causes the change in nitrogen functionality between organisms and oil, and when does it occur? Using X-ray photoelectron spectroscopy (XPS) supported by elemental analysis, biochemical analysis, and pyrolysis-gas chromatography with atomic emission detection (py43C-AED) for nitrogen, surface sediments from the Peru upwelling region were shown to contain at least four different organic nitrogen-containing functional groups: amino, pyrrole, pyridine and (tentatively) quaternary nitrogen. The percent in amino groups is at most 40-45%, and possibly as little as 10-15%. Heterocyclic nitrogen (pyrroles and pyridines) makes up a greater proportion of the total than amino N, with pyrroles more abundant than pyridines. With increasing burial depth, the percentage of total N present as amino nitrogen declines to low levels, whilst the proportion present as (tentatively) quaternary nitrogen increases. Pyrroles are always more abundant than pyridines. These semi-quantitative data suggest that the pyrrolic and pyridinic structures, found in petroleums and coals, are present at a very shallow burial depths in the Peru upwelling sediments.
    Keywords: 112-679D; 112-680B; DRILL; Drilling/drill rig; Joides Resolution; Leg112; Ocean Drilling Program; ODP; South Pacific Ocean
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  • 92
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    In:  Supplement to: Erba, Elisabetta; Covington, James M (1992): Calcareous nannofossil biostratigraphy of Mesozoic sediments recovered from the western Pacific, Leg 129. In: Larson, RL; Lancelot, Y; et al. (eds.), Proceedings of the Ocean Drilling Program, Scientific Results, College Station, TX (Ocean Drilling Program), 129, 179-187, https://doi.org/10.2973/odp.proc.sr.129.118.1992
    Publication Date: 2024-01-09
    Description: Calcareous nannofossils were studied from Jurassic and Cretaceous sediments drilled in the western Pacific during Ocean Drilling Program Leg 129. Mesozoic sediments at Sites 800, 801, and 802 are dominated by volcaniclastic turbidites, claystones, porcellanites, and radiolarites. Pelagic limestones are limited to the middle Cretaceous, and a few calcareous claystones were recovered in the Upper Jurassic section at Site 801. We documented the distribution of nannofossils, their total abundance, preservation, and relative species abundance based on semiquantitative and qualitative studies. Preservation of the calcareous nannofloras is poor to moderate, and the total abundance fluctuates from rare to very abundant. Marker species proposed for the middle and Late Cretaceous were recognized, allowing the application of standard nannofossil biozonations. At Site 800 calcareous nannofloras are abundant and moderately preserved in the Aptian-Cenomanian, and nannofossil biostratigraphy constitutes the basic stratigraphic framework for this interval. Radiolarians are the most abundant and persistent group throughout the sequence drilled at Site 801. Long intervals are barren of nannofloras and assemblages are usually characterized by low abundance and poor preservation. Nannofossil biostratigraphy was applied to the upper Aptian-Cenomanian interval and a few marker species were recognized for the late Tithonian. At Site 802 Cretaceous biostratigraphy is mainly based on calcareous nannofossil biozones corroborated by radiolarian and palynomorph events in the late Aptian-Coniacian age interval. A hiatus was indicated between the Santonian and the late Campanian, and another is suspected in the interval between the Cenomanian and the Coniacian.
    Keywords: 129-800A; 129-801A; 129-801B; 129-802A; DRILL; Drilling/drill rig; Joides Resolution; Leg129; North Pacific Ocean; Ocean Drilling Program; ODP
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    Format: application/zip, 3 datasets
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  • 93
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    In:  Supplement to: Ogg, Gabi (1992): Early Cretaceous palynomorphs of the western Pacific Ocean. In: Larson, RL; Lancelot, Y; et al. (eds.), Proceedings of the Ocean Drilling Program, Scientific Results, College Station, TX (Ocean Drilling Program), 129, 221-228, https://doi.org/10.2973/odp.proc.sr.129.122.1992
    Publication Date: 2024-01-09
    Description: Lower Cretaceous and Jurassic sediments from Ocean Drilling Program Leg 129 (Sites 800, 801, and 802) and Deep Sea Drilling Project Sites 167, 195, 196, and 463 were analyzed for palynomorphs. In contrast to Atlantic occurrences, all Cretaceous pelagic sediments at these sites in the Pacific are barren of preserved palynomorphs. This absence of palynomorphs appears to be independent of facies, sedimentation rate, paleodepth, and paleolatitude. Except for one sample, the dinocyst-bearing sediments also contain spores and pollen grains. The only palynomorphs observed were in redeposited material having sources near former emergent seamounts. Among the dinoflagellate cysts at Site 802, Dingodinium cerviculum, Odontochitina operculata, Canninginopsis colliveri, and Oligosphaeridium complex are the most important species. Based on the presence of these species and their known biostratigraphic ranges, this basal interval of Site 802 is considered to be Aptian/earliest Albian in age. The lack of dinocysts within the Pacific pelagic sediments may be the result of ubiquitous oxygenated bottom waters throughout the Cretaceous or may indicate that open-marine dinoflagellate populations in this ocean did not produce cysts.
    Keywords: 129-802A; DRILL; Drilling/drill rig; Joides Resolution; Leg129; North Pacific Ocean; Ocean Drilling Program; ODP
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  • 94
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    In:  Supplement to: Johnson, Lynn E (1992): Mafic clasts in serpentinite seamounts: petrology and geochemistry of a diverse crustal suite from the outer Mariana Forearc. In: Fryer, P; Pearce, JA; Stokking, LB; et al. (eds.), Proceedings of the Ocean Drilling Program, Scientific Results, College Station, TX (Ocean Drilling Program), 125, 401-413, https://doi.org/10.2973/odp.proc.sr.125.130.1992
    Publication Date: 2024-01-09
    Description: Clasts of metamorphosed mafic igneous rock of diverse composition were recovered in two drill sites on a serpentine mud volcano in the outer Mariana forearc during Ocean Drilling Program Leg 125. These clasts are xenolithic fragments that have been entrained in the rising serpentine mud, and make up less that 9% of the total rock recovered at Sites 778 and 779. Most samples are metabasalt or metadiabase, although one clast of possible boninite and one cumulate gabbro were recovered. On the basis of trace element signatures, samples are interpreted to represent both arc-derived and mid-ocean ridge-derived compositions. Rocks with extremely low TiO2 (〈0.3 wt%) and Zr (〈30 ppm) are similar to boninite series rocks. Samples with low TiO2 (〈0.9 wt%) and Zr (〈50 ppm) and extreme potassium enrichment (K2O/Na2O 〉3.9) may represent island arc rocks similar to shoshonites. However, the K2O/Na2O ratios are much higher than those reported for shoshonites from modem or ancient arcs and may be the result of metamorphism. Samples with moderate TiO2 (1.4 to 1.5 wt%) and Zr (72 to 85 ppm) are similar to rocks from mid-ocean ridges. A few samples have TiO2 and Zr intermediate between island arc and mid-ocean ridge basalt-like rocks. Two samples have high iron (Fe2O3* = 〉12.8 to 18.5 wt%) (Fe2O3* = total iron calculated as Fe2O3) and TiO2 (〉2.3 wt%) and resemble FeTi basalt recovered from mid-ocean ridges. Metamorphism in most samples ranges from low-temperature zeolite, typical of ocean floor weathering, to prehnite-pumpellyite facies and perhaps lower greenschist. Blue amphibole and lawsonite minerals are present in several samples. One diabase clast (Sample 9) exhibits Ca enrichment, similar to rodingite metamorphism, typical of mafic blocks in serpentinized masses. The presence of both low-grade (clays and zeolites) and higher grade (lawsonite) metamorphism indicates retrograde processes in these clasts. These clasts are fragments of the forearc crust and possibly of the subducting plate that have been entrained in the rising serpentine and may represent the deepest mafic rocks ever recovered from the Mariana forearc. The variable compositions and degree of metamorphism of these clasts requires at least two tectonic origins. The recovery of clasts with mid-ocean ridge and arc chemical affinities in a single drill hole requires these clasts to have been "mixed" on a small scale either (1) in the forearc crustal sequence, or (2) after inclusion in the rising serpentine mud. The source of the MORB-like samples and an explanation for the presence of both MORB-like and arc-like rocks in close proximity is critical to any model of the evolution of the Mariana forearc. The source of the MORB-like samples likely will be one (or more) of the following: (1) accretion of Pacific plate lithosphere, (2) remnants of original forearc crust (trapped plate), (3) volcanism in the supra-subduction zone (arc or forearc) environment, or (4) derivation from the subducting slab by faulting along the dÈcollement.
    Keywords: 125-778A; 125-779A; 125-783A; 125-784A; DRILL; Drilling/drill rig; Joides Resolution; Leg125; North Pacific Ocean; Ocean Drilling Program; ODP
    Type: Dataset
    Format: application/zip, 3 datasets
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  • 95
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    In:  Supplement to: Ishii, Teruaki; Robinson, Paul T; Maekawa, Hirokazu; Fiske, Richard (1992): Petrological studies of peridotites from diapiric serpentinite seamounts in the Izu-Ogasawara-Mariana Forearc, Leg 125. In: Fryer, P; Pearce, JA; Stokking, LB; et al. (eds.), Proceedings of the Ocean Drilling Program, Scientific Results, College Station, TX (Ocean Drilling Program), 125, 445-485, https://doi.org/10.2973/odp.proc.sr.125.129.1992
    Publication Date: 2024-01-09
    Description: Refractory spinel peridotites were drilled during Leg 125 from two diapiric serpentinite seamounts: Conical Seamount in the Mariana forearc (Sites 778-780) and Torishima Forearc Seamount (Sites 783-784) in the Izu-Ogasawara forearc. Harzburgite is the predominant rock type in the recovered samples, with subordinate dunite; no lherzolite was found. The harzburgite is diopside-free to sparsely diopside-bearing, with modal percentages of diopside that range from 0% to 2%. Spinels in the harzburgites are chrome-rich (Cr/[Cr + Al] = 0.38-0.83; Fe3+/[Fe3+ + Cr + Al] = 0.01-0.07). Olivine and orthopyroxene are magnesian (Mg# = 0.92). Discrete diopsides reveal extreme depletion of light rare earth elements. Primary hornblende is rare. The bulk major-element chemistry shows low average values of TiO2 (trace), Al2O3 (0.55%) and CaO (0.60%), but high Mg# (0.90). These rocks are more depleted than the abyssal peridotites from the mid-oceanic ridge. They are interpreted as residues of extensive partial melting (= 30%), of which the last episode was in the mantle wedge, probably associated with the generation of incipient island-arc magma, including boninite and/or arc-tholeiite. These depleted peridotites probably represent the residues of melting within mantle diapirs that developed within the mantle wedge.
    Keywords: 125-778A; 125-779A; 125-780C; 125-780D; 125-783A; 125-784A; DRILL; Drilling/drill rig; Joides Resolution; Leg125; North Pacific Ocean; Ocean Drilling Program; ODP
    Type: Dataset
    Format: application/zip, 10 datasets
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  • 96
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    PANGAEA
    In:  Supplement to: Ling, Hsin Yi (1992): Late Neogene silicoflagellates and ebridians from Leg 128, Sea of Japan. In: Pisciotto, KA; Ingle, JCJr.; von Breymann, MT; Barron, J; et al. (eds.), Proceedings of the Ocean Drilling Program, Scientific Results, College Station, TX (Ocean Drilling Program), 127/128(1), 237-248, https://doi.org/10.2973/odp.proc.sr.127128-1.126.1992
    Publication Date: 2024-01-09
    Description: Datum levels and biostratigraphy, including a new zonation of late Neogene silicoflagellates and ebridians, are presented, based on analysis of submarine sediments collected from Sites 798 and 799, Sea of Japan, during the Leg 128 cruise.
    Keywords: 128-798A; 128-798B; 128-798C; 128-799A; DRILL; Drilling/drill rig; Japan Sea; Joides Resolution; Leg128; Ocean Drilling Program; ODP
    Type: Dataset
    Format: application/zip, 4 datasets
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  • 97
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    In:  Supplement to: Ali, Jason Richard; Haston, Roger B; Stokking, Laura B (1992): Magnetostratigraphy of Sites 782, 783, 784, and 786, Izu-Bonin Outer Forearc, western Pacific. In: Fryer, P; Pearce, JA; Stokking, LB; et al. (eds.), Proceedings of the Ocean Drilling Program, Scientific Results, College Station, TX (Ocean Drilling Program), 125, 547-560, https://doi.org/10.2973/odp.proc.sr.125.155.1992
    Publication Date: 2024-01-09
    Description: During Leg 125, scientists drilled Sites 782, 783, 784, and 786 across a transect of the Izu-Bonin forearc near 31°N. Magnetostratigraphy for whole-core and discrete specimens has been integrated with biostratigraphic data and correlated to the geomagnetic polarity time scale. These correlations are good back to the middle Miocene at Sites 783, 784, and 786 and to the late Oligocene at Site 782, but become more tentative in older sediments because of poor recovery and complex magnetizations.
    Keywords: 125-782A; 125-783A; 125-784A; 125-786A; DRILL; Drilling/drill rig; Joides Resolution; Leg125; North Pacific Ocean; Ocean Drilling Program; ODP
    Type: Dataset
    Format: application/zip, 2 datasets
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  • 98
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    PANGAEA
    In:  Supplement to: Stokking, Laura B; Merrill, Dean L; Haston, Roger B; Ali, Jason Richard; Saboda, Kristine L (1992): Rock magnetic studies of serpentinite seamounts in the Mariana and Izu-Bonin regions. In: Fryer, P; Pearce, JA; Stokking, LB; et al. (eds.), Proceedings of the Ocean Drilling Program, Scientific Results, College Station, TX (Ocean Drilling Program), 125, 561-579, https://doi.org/10.2973/odp.proc.sr.125.158.1992
    Publication Date: 2024-01-09
    Description: During Leg 125, scientists drilled two serpentinite seamounts: Conical Seamount in the Mariana forearc and Torishima Forearc Seamount in the Izu-Bonin forearc. Grain densities of the serpentinized peridotites range from 2.44 to 3.02 g/cm**3. The NRM intensity of the serpentinized peridotites ranges from 0.01 to 0.59 A/m and that of serpentine sediments ranges from 0.01 to 0.43 A/m. Volume susceptibilities of serpentinized peridotites range from 0.05 * 10**-3 SI to 9.78 * 10**-3 SI and from 0.12 * 10**-3 to 4.34 * 10**-3 SI in the sediments. Koenigsberger ratios, a measure of the relative contributions of remanent vs. induced magnetization to the magnetic anomaly, vary from 0.09 to 80.93 in the serpentinites and from 0.06 to 4.74 in the sediments. The AF demagnetization behavior of the serpentinized peridotites shows that a single component of remanence (probably a chemical remanence carried by secondary magnetite) can be isolated in many samples that have a median destructive field less than 9.5 mT. Multiple remanence components are observed in other samples. Serpentine sediments exhibit similar behavior. Comparison of the AF demagnetization of saturation isothermal remanence and NRM suggests that the serpentinized peridotites contain both single-domain and multidomain magnetite particles. The variability of the magnetic properties of serpentinized peridotites reflects the complexity of magnetization acquired during serpentinization. Serpentinized peridotites may contribute to magnetic anomalies in forearc regions.
    Keywords: 125-778A; 125-779A; 125-780C; 125-784A; DRILL; Drilling/drill rig; Joides Resolution; Leg125; North Pacific Ocean; Ocean Drilling Program; ODP
    Type: Dataset
    Format: application/zip, 2 datasets
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  • 99
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    PANGAEA
    In:  Supplement to: Stabell, Bjorg; Ali, Jason Richard; Ciampo, Giuliano; Milner, G J; Wang, Yu-Jing; Xu, Yulin (1992): Biostratigraphic summary, Leg 125. In: Fryer, P; Pearce, JA; Stokking, LB; et al. (eds.), Proceedings of the Ocean Drilling Program, Scientific Results, College Station, TX (Ocean Drilling Program), 125, 615-622, https://doi.org/10.2973/odp.proc.sr.125.169.1992
    Publication Date: 2024-01-09
    Description: Samples from 15 holes at nine sites in the Izu-Bonin-Mariana region were examined for calcareous nannofossils, foraminifers, diatoms, and radiolarians. The ages of the containing sediments range from middle Eocene to Holocene. Biostratigraphic indicators date the sediments flanking Conical Seamount in the Mariana forearc as Pleistocene, whereas sediments flanking a seamount at Site 784 in the Izu-Bonin forearc were dated as middle Miocene. Sediments in the Izu-Bonin forearc are as old as the middle Eocene. Useful magnetostratigraphic results range from Holocene to mid-Miocene. Nannofossils provided the most useful biostratigraphic framework, but were supplemented with satisfactory agreement by data from foraminifers, radiolarians, and diatoms. Evidence from the biostratigraphic framework shows the likely presence of a sedimentary hiatus in the early Miocene. The presence of a single short hiatus in the early Oligocene and two in the late Miocene and early Pliocene is suggested, but supporting evidence other than nannofossil data is sparse. Evidence from approximate age-depth plots shows that sediment accumulation varies from hole to hole. The fastest rates of sediment accumulation were found to be in the late Miocene to Holocene whereas the slowest rates are present in the middle Eocene to Oligocene. The increased sedimentation rates in the late Miocene to Holocene resulted from an increase in volcanogenic sediment content from an uncertain source.
    Keywords: 125-782A; 125-784A; 125-786A; DRILL; Drilling/drill rig; Joides Resolution; Leg125; North Pacific Ocean; Ocean Drilling Program; ODP
    Type: Dataset
    Format: application/zip, 3 datasets
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  • 100
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    In:  Supplement to: Koizumi, Itaru (1992): Diatom biostratigraphy of the Japan Sea: Leg 127. In: Pisciotto, KA; Ingle, JCJr.; von Breymann, MT; Barron, J; et al. (eds.), Proceedings of the Ocean Drilling Program, Scientific Results, College Station, TX (Ocean Drilling Program), 127/128(1), 249-289, https://doi.org/10.2973/odp.proc.sr.127128-1.127.1992
    Publication Date: 2024-01-09
    Description: A series of excellent upper Miocene through Quaternary diatomaceous sequences recovered at four sites during Leg 127 was examined for diatoms. The diagenetic transition from opal-A to opal-CT is a diachronic horizon from the uppermost part of the Denticulopsis katayamae Zone (8.5 Ma) at Hole 797B to the uppermost part of the Neodenticula kamtschatica Zone (5.73 Ma) at Hole 795A. The diatom zonation of Koizumi (1985) best divides the upper Miocene to Quaternary sequences above the opal-A/opal-CT boundary and also is useful to date carbonate concretions including diatoms below the boundary. Forty diatom datum levels were evaluated biostratigraphically based on the sediment accumulation rate curve, and several isochronous datum levels are newly proposed for the Japan Sea area. A warm-water current did not penetrated into the Japan Sea through the Tsushima strait during the late Miocene and Pliocene time, because subtropical warm-water diatoms are essentially not present in such sediment samples. The occurrences of diatom are cyclic throughout the Quaternary sediments and are affected by eustatic sea level changes.
    Keywords: 127-794A; 127-795A; 127-796A; 127-797B; DRILL; Drilling/drill rig; Japan Sea; Joides Resolution; Leg127; Ocean Drilling Program; ODP
    Type: Dataset
    Format: application/zip, 6 datasets
    Location Call Number Expected Availability
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