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...

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Bibliographic Details
Published in:Marine Biology
Main Authors: Kemp, K.M., Fraser, Keiron P.P., Collins, Martin Anthony, Priede, I.G.
Format: Article in Journal/Newspaper
Language:unknown
Published: Springer 2008
Subjects:
Online Access:http://nora.nerc.ac.uk/id/eprint/11544/