Anchor Ice Formation in McMurdo Sound, Antarctica, and Its Biological Effects

Aggregations of ice platelets accumulate below the annual sea ice (subice platelet layer) and on the bottom (anchor ice) to depths of 33 meters. Observations of ice platelets adhering to submerged lines support the conclusion that 33 meters is the lower limit for ice formation in the water column in...

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Bibliographic Details
Published in:Science
Main Authors: Dayton, Paul K., Robilliard, Gordon A., DeVries, Arthur L.
Format: Article in Journal/Newspaper
Language:English
Published: American Association for the Advancement of Science (AAAS) 1969
Subjects:
McMurdo Sound
Antarc*
Antarctica
Sea ice
Online Access:http://dx.doi.org/10.1126/science.163.3864.273
https://www.science.org/doi/pdf/10.1126/science.163.3864.273
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Summary:Aggregations of ice platelets accumulate below the annual sea ice (subice platelet layer) and on the bottom (anchor ice) to depths of 33 meters. Observations of ice platelets adhering to submerged lines support the conclusion that 33 meters is the lower limit for ice formation in the water column in this area. The rising anchor ice lifts epibenthic fauna and has a pronounced effect on the distribution of the epibenthic organisms.

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