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Temporal Pattern and Profile of a Coastal‐Deep Sea Conveyor at a Marginal Deep Oligotrophic Sea
1 Introduction Margins are recognized as a significant source of organic carbon to the deep ocean, contributing over 50% of the particulate organic carbon (POC) in deep ocean sediments, with predominance of terrestrial POC (Berner, 1992; Buesseler et al., 2010; Danovaro et al., 1999; Hedges & Keil, 1995; Lamborg et al., 2008; Shen et al., 2020; Wheatcroft et al., 2010).
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