This review originally was going
to be a reply to Tom Gibson’s post on 21.10.2014 but the more I was researching
to back up what I was going to say, the more apparent it was that a full review
of the paper would be more beneficial and perhaps more insightful. Tom and I
had a brief discussion before class yesterday (23.10.2014) which contained what
I had responded with previously (see reply 22.10.2014; 11:46) and that implications
that was stated in the paper was just part of the discussion and they were
highlighting considerations that need to be taken into account when going down
this route of research.
For practical reasons, it is not
surprising that the main focus of marine microbial studies have been focused on
the most abundant phylotypes as they are easier to detect. However, in recent
years, literature has found that the diversity of marine bacteria gone from a
few thousand taxa to 106–109 taxa (the diversity of marine
archaea is said to be 5–10 times less). Studies have suggested that the most
abundant taxa are also the most active and most important in fluxes of
dissolved organic matter, however, abundant species represent only a small
portion of microbial diversity. In 2006, Sogin et al., coined the term ‘rare biosphere’ to explain the analyses of
abundance distribution in diversity. Rare biosphere is one component of
analyses which comprises of a very high number of rare species that contains the
most diversity. In contrast to this, the other component includes the few
species that are very abundant, which is the most studied of the two.
Galand et al., (2009) used pyrosequencing to describe the structure and
composition of the rare biosphere and to test whether it represents
cosmopolitan taxa (biological categories which can be found almost anywhere
around the world) or whether, similar to abundant phylotypes, the rare community
has a biogeography. During the voyages of various Arctic research projects,
samples were collected with a rosette system fitted with PVC bottles and
equipped with a conductivity, temperature and depth (CTD) profiler. Samples
were taken from surface (ACB) and deep water (DAO) masses in five geographical
regions of the Arctic Ocean in the Chukchi Sea, Beaufort Sea, Franklin Bay,
Baffin Bay and Laptev Sea. Shortly after collection, sea water (5-6 L) was filtered
through a 50 µm, 3 µm and 0.2 µm mesh for the DOA samples and a 0.8 µm for the ACB
samples.
The bacterial hypervariable (the
location within nuclear DNA or the D-loop of mitochondrial DNA in which base
pairs of nucleotides repeat (nuclear DNA) or have substitutions (mitochondrial
DNA)) V6 region of the 16S rRNA gene was amplified using a pool of universal
primers. For each read from the sequencer, the primer bases were trimmed from
the beginning and the end, and low-quality sequences were removed. Both
bacteria and archaea communities were investigated to assess the different
levels of diversity within the rare members of the microbial communities. Two
different phylotype definitions to indicate the ecology of the rare biosphere was
used. Reference sequence-based phylotypes were defined as containing all
sequences sharing the same RefHVR_V6 database sequence (or group of sequences from
the VAMPS database; http://vampsarchive.mbl.edu/resources/databases.php) as
their nearest neighbour, a frequently used definition for microbial ecology
studies by pyrosequencing and corresponding to a 94 % identity clustering threshold.
For comparison, a much more stringent definition was used in which sequences
with 100 % identity were grouped as belonging to the same phylotype. Abundant
phylotypes were defined as the phylotypes with a representation > 1 % within
a sample and rare phylotypes were defined as having an abundance < 0.01 %
within a sample.
From the examination of 740,353
16S rRNA gene sequences from 32 bacterial and archaeal communities it was shown
that the rare biosphere did not have a cosmopolitan composition, but rather,
followed patterns similar to those of the most abundant phylotypes. Distinct grouping was apparent with one group
containing all communities from surface waters (ACB) and the other group
containing all deep water mass communities (DAO). On further separation, they
found that distinct grouping corresponded with where the communities were found
in the five geographical regions.
They concluded that the rare
biosphere has a biogeography and that the diversity is most likely subjected to
ecological processes such as selection, speciation, and extinction. In Galand’s
et al., (2009) study, they noted that
distance was much less important than water mass for explaining differences in
community composition (i.e. communities originating from the same water mass
but separated by thousands of kilometres were much more similar to each other
than communities only separated by a few hundred metres but originating from
different water mass).
This reiterates my comment on Tom’s
review that the multidimensional characteristics of the ocean make this field
of research very complicated.
Galand, P.E.,
Casamayor, E.O., Kirchman, D.L., & Lovejoy, C. (2009) 'Ecology of the
rare microbial biosphere of the Arctic Ocean' Proceedings of the National Academy of Sciences 106 (52): 22427-22432.
Sogin, M.L.,
Morrison, H.G., Huber, J.A., Welch, D.M., Huse, S.M., Neal, P.R., Arrieta,
J.M., & Herndl, G.J. (2006) 'Microbial diversity in the deep sea and
the under explored “rare biosphere”' Proceedings
of the National Academy of Sciences 103:
12115-12120.
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