Protists
interact in several ways with bacterial and archaeal populations which has the effect
of substantially shaping the structure of these communities within the marine
environment.
Protists
graze using a mode of nutrition called phagotrophy. This method of grazing can
affect the activity, quantity and physiological state of the prey organisms,
these factors can lead to protists exhibiting prey preferences. An assemblage of
protists feeding in this manner may graze on anything from 25% to >100% of
the daily production of prokaryote plankton.
A study carried
out by Pachiadaki et al (2014) looks at the grazing activities of phagotrophic
protists in the Eastern Mediterranean Sea at depths ranging from 40m down to
3540m at the redoxcline in the Urania basin. The Authors of this paper carried
out the first in situ incubation of samples and due to the fact that the sample
was being suspended at depths of 40 - 3540m for periods of time extending from
4 – 16h they were not able to carry out replicates of the full experiment and
only managed to replicate the counts of the organisms in each treatment. Two
variations of the experiment were carried out. Both experiments used fluorescently
labelled prokaryotes (FLPs) to track the grazing impact of the protistan
communities. The experiments differed in the length of incubation. The shorter
incubation experiments were used to trace the ingested FLPs; the longer
incubation times were used to estimate the rate of disappearance of the FLPs.
The study
found that both prokaryotic and Protistan abundance fell between the euphotic
zone and mesopelagic zone. The difference came when the abundance of prokaryotic
cells stabilised the deeper the sampling went into the mesopelagic layer whereas
the protistan abundance continued to fall with depth. The samples at the
greatest depths of 3000m and 3540m showed an increase in not only prokaryotic
and protistan abundance but also showed elevated rates of daily prokaryotic
turnover. This was especially noticeable at the Urania interface where the
turnover rate was greater than that measured in the photic zone at 40m. The
increased abundance of both prokaryotic and protistan cells was in conflict
with previous counts but this unusual increase in abundance was put down to a resent
eruption of a mud volcano in the vicinity of the test area.
This study
provided a good insight to the microbial assemblages at varying depths and the effects
of protistan grazing on the prokaryotic communities present. It also proved
that in situ incubation and sampling of cultures is possible although the
technology does need some improvement to be able to replicate the whole
experiment to increase the reliability of future experiments.