Aquatic dissolved
organic matter (DOM) is a crucial component of
the global carbon cycle, and the extent to which DOM escapes mineralization
is important for the transport of organic carbon from the continents
to the ocean. DOM persistence strongly depends on its molecular properties,
but little is known about which specific properties cause the continuum
in reactivity among different dissolved molecules. We investigated
how DOM fractions, separated according to their hydrophobicity, differ
in biodegradability across three different inland water systems. We
found a strong negative relationship between hydrophobicity and biodegradability,
consistent for the three systems. The most hydrophilic fraction was
poorly recovered by solid-phase extraction (SPE) (3–28% DOC
recovery) and was thus selectively missed by mass spectrometry analysis
during SPE. The change in DOM composition after incubation was very
low according to SPE–ESI (electrospray ionization)–mass
spectrometry (14% change, while replicates had 11% change), revealing
that this method is sub-optimal to assess DOM biodegradability, regardless
of fraction hydrophobicity. Our results demonstrate that SPE–ESI
mass spectrometry does not detect the most hydrophilic and most biodegradable
species. Hence, they question our current understanding of the relationships
between DOM biodegradability and its molecular composition, which
is built on the use of this method.