The Sea Surface Microlayer (SML) represents the uppermost
tens of microns of the air-sea interface. Previous studies have shown this
layer to be distinct in terms of microbial and physiochemical composition relative
to the underlying subsurface waters. As an air-sea boundary, a proper
understanding of the SML’s chemistry and microbial ecology is necessary to appreciate
globally-important geochemical processes such as air-sea greenhouse gas
exchange and the production of marine aerosols. An influencing factor in such
processes is the presence of biogenic surfactants. When present, surfactants
alter the surface tension of the water in which they are dissolved, in turn
influencing wave formation and the biophysics of the air-sea interface. The
microbiology of marine surfactant cycling in the SML is poorly understood, as
most assays are culture-dependent. Therefore, Kurata and colleagues (2016) set
out to further our understanding of this phenomenon.
The authors focussed their attention on sampling ‘slicks’
(pronounced areas of concentrated surfactants) and non-slick areas of the SML
off the Floridian coast. Field sampling was coordinated with satellites
equipped with synthetic aperture radar (SAR) technology capable of visualising
slicks from space, and the 16S rRNA signature of bacterioneuston communities
from such slicks was 454 sequenced. After controlling for contamination from
control filters, the study found the greatest abundance of
surfactant-associated Bacteria in the
subsurface waters directly below the slick SML – showing high abundance of the
surfactant-producing genera Pseudomonas and
Bacillus. This presence of these
groups below the slick SML, as opposed to within it, drove the authors to
hypothesise an updated model of slick formation. They propose that bacterial
surfactant production occurs primarily in organic-rich subsurface waters and
surfactants are subsequently transported to the SML by physical processes such
as convection and bubble scavenging.
Overall, this paper provides a successful case study in using
a novel fusion of satellite imaging and high-throughput sequencing to sample
surfactant-associated SML Bacteria.
While the authors humbly accept the limitations of their study and outline the
work as a proof-of-concept, I believe the extrapolations of their findings
beyond a case study is unwarranted. The premise of the study (using molecular
data to overcome the limitations of culture-dependant identification of
surfactant-associated Bacteria) falls
down by functionally categorising bacteria
genera into surfactant-associated roles which were initially categorised
using culture-dependent methods. The 16S rRNA signature of the slick SML was
classified by the authors as 97.9% ‘not associated with surfactants’, which I
find hard to believe. I propose the more likely explanation is that
surfactant-associated roles in these genera have not yet been classified in
culture and may play a major role in surfactant production/degradation. This
makes the foundation of the slick-formation model proposed by the authors
unstable, therefore I would need further evidence to accept this proposal
outright.
This hybrid methodology shows promise, and I would be keen
to see the molecular biology of surfactant cycling further developed by using
metatranscriptomics to identify genes expressed in these processes in cultured
species to apply to environmental samples. It would also be exciting to see
this methodology applied to the surfactant-associated eukaryotes, which may
play a key predation role in slick-associated microbial food webs. Despite its
limitations, this paper proposes an intriguing new method for studying microbial
surfactant cycling and provides an important basis for further research into a
geochemically important phenomenon.
Reviewed Paper: Kurata, N., Vella, K., Hamilton, B., Shivji,
M., Soloviev, A., Matt, S., ... & Perrie, W. (2016). Surfactant-associated
bacteria in the near-surface layer of the ocean. Scientific reports, 6. https://www.ncbi.nlm.nih.gov/pmc/articles/PMC4709576/
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