The annual cycle of certain calanoid species in West Greenland.

The West Greenland coast is a typical fjord region with a considerable development of local deepwater basins. The majority of the West Greenland fjords are of the typcial bottom configuration, with a well-developed threshold at the mouth, which normally rises to within 100 or 200 m of the surface. S...

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Bibliographic Details
Main Author: Maclellan, Delphine C.
Other Authors: Dunbar, M. (Supervisor)
Format: Thesis
Language:English
Published: McGill University 1964
Subjects:
Marine Sciences
Calanoida
Copepoda > Greenland
Ameralik
Arctic
Greenland
Ameralik fjord
Online Access:http://digitool.Library.McGill.CA:80/R/?func=dbin-jump-full&object_id=116561
Description
Summary:The West Greenland coast is a typical fjord region with a considerable development of local deepwater basins. The majority of the West Greenland fjords are of the typcial bottom configuration, with a well-developed threshold at the mouth, which normally rises to within 100 or 200 m of the surface. Such a fjord has been named an "Arctic" type fjord by Stephensen (1916), because the bottom water is arctic in character, having a negative temperature and low salinity. Ameralik fjord (Latitude 64o 3' N., Longitude 52o 30' W.) (map) is in this category. [.]

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