Potential bioavailability of organic matter from atmospheric particles to marine heterotrophic bacteria

• Main Authors: K. Djaoudi, F. Van Wambeke, A. Barani, N. Bhairy, S. Chevaillier, K. Desboeufs, S. Nunige, M. Labiadh, T. Henry des Tureaux, D. Lefèvre, A. Nouara, C. Panagiotopoulos, M. Tedetti, E. Pulido-Villena
• Format: Article
• Language: English
• Published: Copernicus Publications 2020-12-01
• Series: Biogeosciences
• Online Access: https://bg.copernicus.org/articles/17/6271/2020/bg-17-6271-2020.pdf
• ISSN: 1726-4170; 1726-4189

<p>The surface ocean receives important amounts of organic carbon from atmospheric deposition. The degree of bioavailability of this source of organic carbon will determine its impact on the marine carbon cycle. In this study, the potential availability of dissolved organic carbon (DOC) leached from both desert dust and anthropogenic aerosols to marine heterotrophic bacteria was investigated. The experimental design was based on 16 d incubations, in the dark, of a marine bacterial inoculum into artificial seawater amended with water-soluble Saharan dust (D treatment) and anthropogenic (A treatment) aerosols, so that the initial DOC concentration was similar between treatments. Glucose-amended (G) and non-amended (control) treatments were run in parallel. Over the incubation period, an increase in bacterial abundance (BA) and bacterial production (BP) was observed first in the G treatment, followed then by the D and finally A treatments, with bacterial growth rates significantly higher in the G and D treatments than the A treatment. Following this growth, maxima of BP reached were similar in the D (879 <span class="inline-formula">±</span> 64 ng C L<span class="inline-formula">⁻¹</span> h<span class="inline-formula">⁻¹</span>; <span class="inline-formula"><i>n</i>=3</span>) and G (648 <span class="inline-formula">±</span> 156 ng C L<span class="inline-formula">⁻¹</span> h<span class="inline-formula">⁻¹</span>; <span class="inline-formula"><i>n</i>=3</span>) treatments and were significantly higher than in the A treatment (124 ng C L<span class="inline-formula">⁻¹</span> h<span class="inline-formula">⁻¹</span>; <span class="inline-formula"><i>n</i>=2</span>). The DOC consumed over the incubation period was similar in the A (9 <span class="inline-formula">µ</span>M; <span class="inline-formula"><i>n</i>=2</span>) and D (9 <span class="inline-formula">±</span> 2 <span class="inline-formula">µ</span>M; <span class="inline-formula"><i>n</i>=3</span>) treatments and was significantly lower than in the G treatment (22 <span class="inline-formula">±</span> 3 <span class="inline-formula">µ</span>M; <span class="inline-formula"><i>n</i>=3</span>). Nevertheless, the bacterial growth efficiency (BGE) in the D treatment (14.2 <span class="inline-formula">±</span> 5.5 %; <span class="inline-formula"><i>n</i>=3</span>) compared well with the G treatment (7.6 <span class="inline-formula">±</span> 2 %; <span class="inline-formula"><i>n</i>=3</span>), suggesting that the metabolic use of the labile DOC fraction in both conditions was energetically equivalent. In contrast, the BGE in the A treatment was lower (1.7 %; <span class="inline-formula"><i>n</i>=2</span>), suggesting that most of the used labile DOC was catabolized. The results obtained in this study highlight the potential of aerosol organic matter to sustain the metabolism of marine heterotrophs and stress the need to include this external source of organic carbon in biogeochemical models for a better constraining of the carbon budget.</p>