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  • ALBAT-62; Archive of Ocean Data; ARCOD; Central Basin, Pacific Ocean; Elevation of event; Event label; GC; Gravity corer; Indian Ocean; Latitude of event; Longitude of event; Pacific Ocean; Thomas G. Thompson (1964); TT028; TT028-14; TT028-17; TT028-19; TT028-22; TT028-23; TT028-24; V24-58; V24-59; V24-60; V24-62; VITYAZ; Vityaz (ex-Mars); Vityaz-31; Vityaz-34; VITYAZ3802-GC; VITYAZ4599-GC; Vityaz-48; VITYAZ5071-GC; VITYAZ5082-GC; VITYAZ5098-GC; VITYAZ5100-GC; VITYAZ6277-3-GC; VITYAZ6337-GC; Zone boundary, lower; Zone boundary, upper  (2)
  • 13-126; Comment; Deep Sea Drilling Project; Deposit type; DEPTH, sediment/rock; Description; DRILL; Drilling/drill rig; DSDP; Glomar Challenger; Identification; Leg13; Mediterranean Sea/RIDGE; NOAA and MMS Marine Minerals Geochemical Database; NOAA-MMS; Position; Quantity of deposit; Sample code/label; Sediment type; Visual description  (1)
  • PANGAEA  (3)
  • American Association for the Advancement of Science (AAAS)
  • American Chemical Society (ACS)
  • 1970-1974  (3)
Collection
Keywords
Publisher
  • PANGAEA  (3)
  • American Association for the Advancement of Science (AAAS)
  • American Chemical Society (ACS)
Years
  • 1970-1974  (3)
Year
  • 1
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    Unknown
    Annotated record of the detailed examination of Mn deposits from DSDP Site 126, Leg 13 (Core 126-2) (1973)
    PANGAEA
    In:  Supplement to: Ryan, William B F; Hsü, Kenneth J; Cita, Maria Bianca; Dumitrica, Paulian; Llort, Jennifer; Maync, Wolf; Nesteroff, Wladimir D; Pautot, Guy; Stradner, Herbert; Wezel, Forese C (1973): Site 126. In: Ryan, W.B.F.; Hsu, K.J.; et al., Initial Reports of the Deep Sea Drilling Project, Initial Reports of the Deep Sea Drilling Project, U.S. Government Printing Office, XIII, 219-241, https://doi.org/10.2973/dsdp.proc.13.108.1973
    Details
    Publication Date: 2023-08-28
    Description: The single "raison d'être" for selecting Site 126 was to explore the pre-evaporite history of the eastern Mediterranean and hopefully to establish the paleoenvironment which preceded the Late Miocene salinity crisis. The selcetd site is in a deep cleft in the Mediterranean Ridge in the central Ionian Sea, a cleft that cuts more than 250 meters below the level of Horizon M and at the same time is floored by flat-lying sediments. A secondary objective of the cleft site-selection was to ascertain what kind of sediment makes up the horizontal fill and hopefully to determine some details of the history and mechanics of the depression-filling process.
    Keywords: 13-126; Comment; Deep Sea Drilling Project; Deposit type; DEPTH, sediment/rock; Description; DRILL; Drilling/drill rig; DSDP; Glomar Challenger; Identification; Leg13; Mediterranean Sea/RIDGE; NOAA and MMS Marine Minerals Geochemical Database; NOAA-MMS; Position; Quantity of deposit; Sample code/label; Sediment type; Visual description
    Type: Dataset
    Format: text/tab-separated-values, 8 data points
    Location Call Number Expected Availability
    BibTip Others were also interested in ...
    DATA PANGAEA
  • 2
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    Unknown
    (Table 1) Positions of the Mesocena elliptica zone in sediment cores from the Pacific and Indian Oceans (1973)
    PANGAEA
    In:  P.P. Shirshov Institute of Oceanology, Russian Academy of Sciences, Moscow | Supplement to: Zhuse, Anastasiya P; Mukhina, Valentina V (1973): The Mesocena elliptica Ehr. zone in the Pleistocene sediments of the Pacific Ocean. Oceanology, 13, 386-394
    Details
    Publication Date: 2023-09-15
    Description: The Mesocena elliptica Ehr. zone in deep-sea sediments of the Pacific Ocean is characterized by a short vertical range at the base of the Pleistocene section. Depending on sedimentation rate this zone lies at various depths below the ocean bottom. M. elliptica is unknown in recent oceanic plankton. In fossil state known species indicate that sediments containing them are of Oligocene-Miocene age. New data obtained in early 1960's show that within a short interval, evidently in Early Pleistocene, M. elliptica was abundant in plankton, primarily in tropical regions. Correlation of paleomagnetic data with results of diatom analysis shows that the Mesocena elliptica zone always lies above the Pliocene-Pleistocene boundary, and that maximum contents of M. elliptica coincide with the Jaramillo event (0.85-0.95 million years ago).
    Keywords: ALBAT-62; Archive of Ocean Data; ARCOD; Central Basin, Pacific Ocean; Elevation of event; Event label; GC; Gravity corer; Indian Ocean; Latitude of event; Longitude of event; Pacific Ocean; Thomas G. Thompson (1964); TT028; TT028-14; TT028-17; TT028-19; TT028-22; TT028-23; TT028-24; V24-58; V24-59; V24-60; V24-62; VITYAZ; Vityaz (ex-Mars); Vityaz-31; Vityaz-34; VITYAZ3802-GC; VITYAZ4599-GC; Vityaz-48; VITYAZ5071-GC; VITYAZ5082-GC; VITYAZ5098-GC; VITYAZ5100-GC; VITYAZ6277-3-GC; VITYAZ6337-GC; Zone boundary, lower; Zone boundary, upper
    Type: Dataset
    Format: text/tab-separated-values, 38 data points
    Location Call Number Expected Availability
    BibTip Others were also interested in ...
    DATA PANGAEA
  • 3
    facet.materialart.
    Unknown
    (Table 1) Positions of the Mesocena elliptica zone in sediment cores from the Pacific and Indian Oceans (1973)
    PANGAEA
    In:  P.P. Shirshov Institute of Oceanology, Russian Academy of Sciences, Moscow | Supplement to: Zhuse, Anastasiya P; Mukhina, Valentina V (1973): The Mesocena elliptica Ehr. zone in the Pleistocene sediments of the Pacific Ocean. Oceanology, 13, 386-394
    Details
    Publication Date: 2023-09-15
    Description: The Mesocena elliptica Ehr. zone in deep-sea sediments of the Pacific Ocean is characterized by a short vertical range at the base of the Pleistocene section. Depending on sedimentation rate this zone lies at various depths below the ocean bottom. M. elliptica is unknown in recent oceanic plankton. In fossil state known species indicate that sediments containing them are of Oligocene-Miocene age. New data obtained in early 1960's show that within a short interval, evidently in Early Pleistocene, M. elliptica was abundant in plankton, primarily in tropical regions. Correlation of paleomagnetic data with results of diatom analysis shows that the Mesocena elliptica zone always lies above the Pliocene-Pleistocene boundary, and that maximum contents of M. elliptica coincide with the Jaramillo event (0.85-0.95 million years ago).
    Keywords: ALBAT-62; Archive of Ocean Data; ARCOD; Central Basin, Pacific Ocean; Elevation of event; Event label; GC; Gravity corer; Indian Ocean; Latitude of event; Longitude of event; Pacific Ocean; Thomas G. Thompson (1964); TT028; TT028-14; TT028-17; TT028-19; TT028-22; TT028-23; TT028-24; V24-58; V24-59; V24-60; V24-62; VITYAZ; Vityaz (ex-Mars); Vityaz-31; Vityaz-34; VITYAZ3802-GC; VITYAZ4599-GC; Vityaz-48; VITYAZ5071-GC; VITYAZ5082-GC; VITYAZ5098-GC; VITYAZ5100-GC; VITYAZ6277-3-GC; VITYAZ6337-GC; Zone boundary, lower; Zone boundary, upper
    Type: Dataset
    Format: text/tab-separated-values, 38 data points
    Location Call Number Expected Availability
    BibTip Others were also interested in ...
    DATA PANGAEA
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