Abstract

AbstractHumic‐like substances (HULIS) are present in every environmental reservoir, including the ocean and the atmosphere. Ocean‐derived HULIS can be transferred to the atmosphere in the form of sea spray aerosols (SSA). Little information exists on the factors controlling this transfer process or how HULIS alter SSA physicochemical properties, cloud‐forming ability, and atmospheric reactions. Here, using excitation‐emission matrix spectroscopy and isolated ocean‐atmosphere systems, we investigated how ocean biology affects HULIS sea‐to‐air transfer during multiple phytoplankton bloom experiments. We posit that bacterial enzymatic activity on phytoplankton‐derived organic matter control HULIS size, production, and chemical composition. We found that changes in fluorescence indices and shifts in the HULIS fluorescence emission spectra reveal changes in HULIS chemical composition induced by bacteria. High bacterial enzymatic activity on the proteinaceous, lipid, and phosphorus‐rich organic pools enhanced HULIS production and its transfer to SSA. Seawater HULIS consistently accumulated across all experiments. The majority of HULIS was smaller than 0.2 μm or 50 kDa. Our results suggest that enzymatic‐processing bacteria transform the composition of HULIS in seawater, degrading dissolved organic matter into diverse chemical structures that are more efficiently transferred to the atmosphere in SSA.

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