Seasonal variation in the white muscle biochemical composition of deep-sea macrourids in the North-east Atlantic
The foremost temporal signal to the deep benthos, where temperature and light conditions are relatively constant, is a seasonal pulse of organic carbon sinking from the photic layer. In the Porcupine Seabight region of the NE Atlantic this flux begins during late spring and early summer, although th...
Published in: | Marine Biology |
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Main Authors: | , , , |
Format: | Article in Journal/Newspaper |
Language: | unknown |
Published: |
Springer
2008
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Subjects: | |
Online Access: | http://nora.nerc.ac.uk/id/eprint/11544/ |