Ice Flora (Bottom Type): A Mechanism of Primary Production in Polar Seas and the Growth of Diatoms in Sea Ice

A yellowish-brown layer at the bottom of summer sea ice, upturned by an icebreaker, off the coast at Point Barrow, Alaska, extended up to 30 cm from the bottom. It consisted of large diatom colonies which were found to have been formed in brine included in fissures between vertically oriented ice cr...

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Bibliographic Details
Published in:ARCTIC
Main Authors: Meguro, Hiroshi, Ito, Kuniyuki, Fukushima, Hiroshi
Format: Article in Journal/Newspaper
Language:English
Published: The Arctic Institute of North America 1967
Subjects:
Online Access:https://journalhosting.ucalgary.ca/index.php/arctic/article/view/66338