ALBERT

All Library Books, journals and Electronic Records Telegrafenberg

X
feed icon rss

Your email was sent successfully. Check your inbox.

An error occurred while sending the email. Please try again.

Proceed reservation?

Export
Filter
  • 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)
  • PANGAEA  (2)
  • American Association for the Advancement of Science (AAAS)
  • American Chemical Society (ACS)
  • 1970-1974  (2)
Collection
Keywords
Publisher
  • PANGAEA  (2)
  • American Association for the Advancement of Science (AAAS)
  • American Chemical Society (ACS)
Years
  • 1970-1974  (2)
Year
  • 1
    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
  • 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
Close ⊗
This website uses cookies and the analysis tool Matomo. More information can be found here...