Peatland wildfires contribute significantly to the atmospheric
release of light-absorbing organic carbon, often referred to as brown
carbon. In this study, we examine the presence of nitrogen-containing
organic compounds (NOCs) within marine aerosols across the Western
Pacific Ocean, which are influenced by peatland fires from Southeast
Asia. Employing ultrahigh-resolution Fourier transform ion cyclotron
resonance mass spectrometry (FT-ICR MS) in electrospray ionization
(ESI) positive mode, we discovered that NOCs are predominantly composed
of reduced nitrogenous bases, including CHN+ and CHON+ groups. Notably,
the count of NOC formulas experiences a marked increase within plumes
from peatland wildfires compared to those found in typical marine
air masses. These NOCs, often identified as N-heterocyclic alkaloids,
serve as potential light-absorbing chromophores. Furthermore, many
NOCs demonstrate pyrolytic stability, engage in a variety of substitution
reactions, and display enhanced hydrophilic properties, attributed
to chemical processes such as methoxylation, hydroxylation, methylation,
and hydrogenation that occur during emission and subsequent atmospheric
aging. During the daytime atmospheric transport, aging of aromatic
N-heterocyclic compounds, particularly in aliphatic amines prone to
oxidation and reactions with amine, was observed. The findings underscore
the critical role of peatland wildfires in augmenting nitrogen-containing
organics in marine aerosols, underscoring the need for in-depth research
into their effects on marine ecosystems and regional climatic conditions.