The substantial release of microplastics (MPs) into the marine environment is now deeply integrated into Earth's carbon cycle. However, the mechanisms by which warming regulates the release of MP-leached dissolved organic matter (MP-DOM) in seawater media remain highly uncertain. This work considers four typical MPs that enter the ocean (polyethylene, PE; polypropylene, PP; polyethylene terephthalate, PET; and polyvinyl chloride, PVC) over 1-week experiments under UV light and dark conditions at a narrow temperature interval of 5 °C between10-35 °C. The results indicate that different MPs have variable photoleaching rates of dissolved organic carbon (MP-DOC, 0.06 ± 0.01-0.61 ± 0.07 mg-C/g-MP/week) and fluorescent DOM (MP-FDOM). An unexpected inconsistency emerged in the photoleaching of MP-DOC and MP-FDOM, with dominant MP-DOC release for PE, PP and PVC, while PET showed substantial release of both. The humification index and biological index pair is a useful indicator to distinguish MP-DOM versus natural DOM. The Q10 values, which reflect the temperature sensitivity of MP-DOC photoleaching, ranged from 1.62 (PVC) to 1.93 (PET) indicating an exponential increase in MP-DOC leaching rates with rising temperature. These findings highlight the need for incorporating ocean warming into predicting the effects of plastic pollution on the marine carbon cycle.
Keywords: Dissolved organic carbon; Microplastic degradation; Ocean warming; Temperature sensitivity; UV irradiation.
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