Benthic-pelagic coupling in the East Siberian Sea from nitrate isotopes
Over the East Siberian Sea and common to the western Arctic Ocean, a subsurface nutrient maximum is reported in the halocline, and generally attributed to both nutrient-rich Pacific inflow and intensive remineralization in shelf bottom waters being advected into the central Arctic basin. We report n...
Main Authors: | , , , , , , , , , |
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Other Authors: | |
Format: | Conference Object |
Language: | French |
Published: |
2017
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Subjects: | |
Online Access: | http://hdl.handle.net/2013/ULB-DIPOT:oai:dipot.ulb.ac.be:2013/299554 |