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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)
  • 14-135; 14-136; 14-137; 14-141; Comment; Deep Sea Drilling Project; Deposit type; DEPTH, sediment/rock; Description; DRILL; Drilling/drill rig; DSDP; Event label; Glomar Challenger; Identification; Leg14; NOAA and MMS Marine Minerals Geochemical Database; NOAA-MMS; North Atlantic/DIAPIR; North Atlantic/HILL; North Atlantic/PLAIN; Position; Quantity of deposit; Sample code/label; Sediment type; Size; Substrate 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
    (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
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    DATA PANGAEA
  • 2
    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
  • 3
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    Unknown
    Annotated record of the detailed examination of Mn deposits from DSDP Leg 14 (Sites 14-135, 14-136, 14-137, 14-141) (1972)
    PANGAEA
    In:  Supplement to: Berger, Wolfgang H; von Rad, Ulrich (1972): Cretaceous and Cenozoic Sediments from the Atlantic Ocean. In: Hayes, D.E.; Pimm, A.C.; et al., Initial Reports of the Deep Sea Drilling Project, Initial Reports of the Deep Sea Drilling Project, U.S. Government Printing Office, XIV, 787-954, https://doi.org/10.2973/dsdp.proc.14.126.1972
    Details
    Publication Date: 2023-08-28
    Description: Leg 14 of the Deep Sea Drilling Project completed 9 holes; 7 were located off NW Africa, 1 in Ceara Abyssal Plain, and 1 on Demerara Rise. Quaternary and Pliocene sediments consist of nanno chalk oozes and brown clay. The facies boundary (CCD) is near 5000 meters. Sedimentation rates are between 10 and 30 meters/million years (m/My) for chalk ooze and 2 to 4 m/My for pelagic clay. Redeposition off the Amazon produces terrigenous and bioclastic turbidite sequences with rates increasing, on the average, from 50 to 150 m/My. Small manganese nodules (coarse sand and small pebbles) are common in sediments associated with hiatuses at Sites 135 (Eocene-Miocene, Core SW1), 136 (Late Cretaceous- Miocene, Cores 3 to 6), and to a lesser extent at 141 (Middle Miocene-Pliocene, Core 7). Additional occurrences were noted in the pelagic clays at Site 137 (Late Cretaceous to Miocene). At 135-8 (Cenomanian) micro-nodules occur within a mixture of siltstone fragments, compressed planktonic foraminifera, fish debris, as well as chert pebbles and other redeposited components. Manganese concretions are generally younger than Turonian and are restricted to the predominantly oxidized part of the sequences, that is, where sediments are mostly red, brown, or yellow-colored.
    Keywords: 14-135; 14-136; 14-137; 14-141; Comment; Deep Sea Drilling Project; Deposit type; DEPTH, sediment/rock; Description; DRILL; Drilling/drill rig; DSDP; Event label; Glomar Challenger; Identification; Leg14; NOAA and MMS Marine Minerals Geochemical Database; NOAA-MMS; North Atlantic/DIAPIR; North Atlantic/HILL; North Atlantic/PLAIN; Position; Quantity of deposit; Sample code/label; Sediment type; Size; Substrate type; Visual description
    Type: Dataset
    Format: text/tab-separated-values, 72 data points
    Location Call Number Expected Availability
    BibTip Others were also interested in ...
    DATA PANGAEA
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