Abstract

Seaweed farming is widely perceived as one of the most environmentally benign types of aquaculture activity. In the past 10 yr, global seaweed production has doubled and reached 31.8 million t. Farmed seaweed also has important functions in local ecosystems. We focus on the production, bioavailability, and bacterial degradation rates of dissolved organic carbon (DOC) from cultured kelp Saccharina japonica. Semi in situ incubations in 2 growing seasons were conducted to estimate DOC production, and laboratory incubations were used to determine bioavailability and decay rates of DOC from cultured kelp. Results showed that DOC production was 6.2-7.0 mg C (g dry wt)-1 d-1 in the growing seasons, and the proportion of DOC in net primary production was 23.7-39.1%. The decomposition rate of DOC was 4 ± 1% d-1 and 9 ± 1% d-1 in January and April, respectively. About 37.8% remained as refractory DOC after 150 d incubation. It was calculated that the total DOC from kelp in Sanggou Bay was approximately 11.3 times of that from phytoplankton for the whole bay (144 km2). Our results suggest that more than half of the bioavailable DOC will be exported out of the bay to potentially support the wider food chain through bacterial uptake. Cultured kelp is therefore an important source of DOC in the embayment, contributes to the coastal DOC pool and provides a potential pathway for carbon dioxide sequestration.

Highlights

  • Marine dissolved organic carbon (DOC) represents one of the largest and most exchangeable organic carbon pools on Earth and plays an important role in marine biogeochemical cycles

  • 69.4−91.2% and 34.0−76.1% will be exported out of the bay, respectively, entering the Yellow Sea, where no kelp is cultured and phytoplankton is the main primary producer. Both the absolute release rate of DOC and the proportion of DOC in net primary production (NPP) are important in evaluating the function of macroalgae in biological cycling of carbon (Krause-Jensen & Duarte 2016)

  • We conducted the study in a semi-in situ system using entire kelp individuals and extended the study time through day and night to accurately quantify NPP and DOC production

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Summary

Introduction

Marine dissolved organic carbon (DOC) represents one of the largest and most exchangeable organic carbon pools on Earth and plays an important role in marine biogeochemical cycles. The released DOC contributes to the coastal DOC pool. Macroalgal DOC contribution can reach 20% of the total DOC concentrations (Wada et al 2007, Wada & Hama 2013). It has been shown that about 53.7% of released DOC is mineralized in 30 d decomposition experiments (Wada et al 2008), and that DOC from kelp is more refractory than DOC from phytoplankton, which can be removed by bacteria in days to weeks (Kirchman et al 1991, Chen & Wangersky 1996, Hama et al 2004, Davis & Benner 2007), because bioavailability of DOC varies depending on DOC chemical composition (Benner & Opsahl 2001, Wada et al 2007) and production of refractory components (Cottrell & Kirchman 2000, Lønborg et al 2009). In a particular coastal ecosystem, the DOC fate (utilization versus export) and its function in the local system will depend on the balance between the half-life of DOC and the water residence time (Lønborg & Álvarez-Salgado 2012)

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