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