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Greenhouse gas cycling by the plastisphere: The sleeper issue of plastic pollution

Chemosphere 2019 58 citations ? Citation count from OpenAlex, updated daily. May differ slightly from the publisher's own count. Score: 35 ? 0–100 AI score estimating relevance to the microplastics field. Papers below 30 are filtered from public browse.
Marcela Cornejo, Verónica Molina, Javiera Pavez, Nelson Silva

Summary

The microbial community living on ocean microplastics (the plastisphere) appears to contribute to cycling of greenhouse gases CO2 and N2O in the South Pacific Ocean. This finding suggests that the plastisphere may play a previously unrecognized role in ocean biogeochemistry with implications for climate change.

Study Type Environmental

Plastic is an allochthonous material to marine ecosystems but is rapidly colonized by marine microbial communities, with an as yet unclear contribution to biogeochemical cycles. In this study, we investigated the influence of an active microbial community grown on microplastic particles (the plastisphere) on CO and NO recycling and its potential role in greenhouse gas inventories and air-sea exchange. Microplastics were collected during two cruises (Cimar 21 and FIP Montes Submarinos) from the surface layer (5 m depth) from several contrasting trophic regions of the South Pacific Ocean, i.e., from a transition zone off the eutrophic coastal upwelling of Chile, to a mesotrophic transition area of oceanic seamounts and, finally, to an oligotrophic zone in the South Pacific Subtropical Gyre. . Experiments were carried out onboard to evaluate CO and NO production/consumption by the plastisphere. The active microbial community and its specific quantification were determined for Cimar 21 using iTag 16 S rRNA. The experiments showed that the plastisphere generally contributed to CO and NO production/consumption, with rates ranging from -20.5 (consumption) to +4.5 (production) μmol/m/d. The seamounts and the transition zone presented the highest production/consumption rates. The experiments performed in the two seamount stations showed that production and consumption of CO were related to the environmental nutrient concentration. Both stations presented NO consumption that was associated with the high nitrogen deficit of the subantarctic water mass. The transition zone presented CO and NO production in a plastisphere dominated by heterotrophic communities. The plastisphere in oligotrophic waters was diverse and active. The experiments, however, presented low or no production of greenhouse gases. Our results show a contribution of CO and NO to the global gas surface inventories and air-sea exchange is lower than 1% of the global sources. These results highlight different critical impacts of plastic pollution on the environment that have, until now, not been considered.

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