Remineralization of particulate organic carbon in an ocean oxygen minimum zone.

4a ), which, although marginally significant, is an order of magnitude lower than our mean rate for both fractions (see Supplementary Table 1 ) and an order of magnitude greater than that determined with an ultrasensitive STOX sensor for raw, unadulterated, or non-concentrated, seawater of up to 0.085 μmol l −1 h −1 (ref. 65 ).

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