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Report
  • Language: en
  • Pages: 2492

Report

  • Type: Book
  • -
  • Published: 1953
  • -
  • Publisher: Unknown

None

Annual Report
  • Language: en
  • Pages: 80

Annual Report

  • Type: Book
  • -
  • Published: 1986
  • -
  • Publisher: Unknown

None

Oversight of Marine Fisheries Management
  • Language: en
  • Pages: 672
Catalog of Copyright Entries. Third Series
  • Language: en
  • Pages: 1830
Development of Fishes of the Mid-Atlantic Bight: Hardy, J. D. Anguillidae through Syngnathidae
  • Language: en
  • Pages: 476

Development of Fishes of the Mid-Atlantic Bight: Hardy, J. D. Anguillidae through Syngnathidae

  • Type: Book
  • -
  • Published: 1978
  • -
  • Publisher: Unknown

None

Development of Fishes of the Mid-Atlantic Bight
  • Language: en
  • Pages: 476

Development of Fishes of the Mid-Atlantic Bight

  • Type: Book
  • -
  • Published: 1978
  • -
  • Publisher: Unknown

None

Whales, Dolphins, and Porpoises
  • Language: en
  • Pages: 754

Whales, Dolphins, and Porpoises

None

Annual Report for Fiscal Year ...
  • Language: en
  • Pages: 404

Annual Report for Fiscal Year ...

  • Type: Book
  • -
  • Published: 1963
  • -
  • Publisher: Unknown

None

International Symposium on Biological Sound Scattering in the Ocean, Airlie House, 1970
  • Language: en
  • Pages: 652

International Symposium on Biological Sound Scattering in the Ocean, Airlie House, 1970

  • Type: Book
  • -
  • Published: 1971
  • -
  • Publisher: Unknown

None

Late Neogene Chronostratigraphy, Biostratigraphy, Biochronology and Paleoclimatology
  • Language: en
  • Pages: 834

Late Neogene Chronostratigraphy, Biostratigraphy, Biochronology and Paleoclimatology

  • Type: Book
  • -
  • Published: 1973
  • -
  • Publisher: Unknown

The integration of modern paleomagnetic, radiometric, and biostratigraphic studies has provided an accurate geochronological framework for the past 10 million years--the Late Neogene. Marine zones based on calcareous and siliceous planktonic organisms are recognized from the sub-Arctic region to the sub-Antarctic and their correlation to the paleomagnetic time scale is now feasible in some detail for the past 5 my. Likewise, the relationship of geochemically calibrated mammalian biochronology to the marine succession has been greatly improved. Within this framework of time it is possible to delineate the history of major features in Late Neogene paleontology, climatology, and oceanography. (Author).