In:
Journal of Geophysical Research: Oceans, American Geophysical Union (AGU), Vol. 122, No. 6 ( 2017-06), p. 4539-4553
Abstract:
POC and opal fluxes to NW Atlantic margin deep waters are mainly controlled by biological production in surface waters CaCO 3 and lithogenic material predominantly derive from lateral transport of resuspended sediment Resuspended sediment accounts for ca. 63% of the total particle flux at 3000 m
Type of Medium:
Online Resource
ISSN:
2169-9275
,
2169-9291
DOI:
10.1002/2016JC012549
Language:
English
Publisher:
American Geophysical Union (AGU)
Publication Date:
2017
detail.hit.zdb_id:
2016804-4
detail.hit.zdb_id:
161667-5
detail.hit.zdb_id:
3094219-6
SSG:
16,13
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