Abstract:Marine microbes have a pivotal role in the marine biogeochemical cycle of carbon, because they regulate the turnover of dissolved organic matter (DOM), one of the largest carbon reservoirs on Earth. Microbial communities and DOM are both highly diverse components of the ocean system, yet the role of microbial diversity for carbon processing remains thus far poorly understood. We report here results from an exploration of a mosaic of phytoplankton blooms induced by large-scale natural iron fertilization in the … Show more
“…S3 in the supplemental material). In contrast, in all sampled stations from tropical/subtropical oceans, the Roseobacter communities are overrepresented by the SAG-O19 lineage (each 40 to 60% of all roseobacters) (see Table S3 in the supplemental material), and in samples from the Southern Ocean the lineage DC5-80-3 dominates (ϳ40%) (see Table S3 in the supplemental material), the latter consistent with previous studies based on the analysis of the 16S rRNA gene sequences (49)(50)(51). In several other oceans, the Roseobacter communities appear to be dominated by multiple uncultivated lineages.…”
“…S3 in the supplemental material). In contrast, in all sampled stations from tropical/subtropical oceans, the Roseobacter communities are overrepresented by the SAG-O19 lineage (each 40 to 60% of all roseobacters) (see Table S3 in the supplemental material), and in samples from the Southern Ocean the lineage DC5-80-3 dominates (ϳ40%) (see Table S3 in the supplemental material), the latter consistent with previous studies based on the analysis of the 16S rRNA gene sequences (49)(50)(51). In several other oceans, the Roseobacter communities appear to be dominated by multiple uncultivated lineages.…”
“…However, we found no significant differences in the BCC between the CONTR2 and BB treatment. Shifts in the bacterioplankton composition may be caused by changes in the quality of the DOM (Pinhassi et al 2004, Landa et al 2016, but the quantity of the released DOM may also be important (Sarmento et al 2016). We can make no further conclusions about this topic, based on our data, because we did not characterize the DOM pool in detail.…”
Section: Bacterial Bloom Phasementioning
confidence: 79%
“…Among them, temperature and light are important environmental factors during the development of the spring bloom ) that can also affect bacterial activity and, thus, the bacteria−phytoplankton coupling (Lindh et al 2013, von Scheibner et al 2014, Landa et al 2016. For example, an increase in temperature from the in situ temperature (2.5°C) to 6−8°C boosted bacterial production (BP) and decreased the time lag between PP and secondary production peaks in several experiments (Hoppe et al 2008, von Scheibner et al 2014.…”
“…In aquatic environments, microbial activity and diversity are considered to be closely linked to overall ecosystem function (Finlay et al, 1997), and changes in diversity have been positively associated with organic matter availability and heterotrophic activity (Landa et al, 2016). Our data indicate a minor proportion of OTUs might be replaced during warm periods, and so we need to look into potential loss of functions in surface water microbial communities with temperature increase.…”
Section: Main Drivers Of Temporal Variability Of Microbial Community mentioning
Since microorganisms play a major role in the biogeochemistry of the ocean, understanding structure and dynamics of natural microbial communities is crucial in assessing the impact of environmental changes on marine ecosystems. In order to identify key environmental drivers of microbial community structure in Chilean Patagonian fjords, we analyzed composition of the prokaryotic community over an annual cycle at a single sampling site in Puyuhuapi Fjord. Distinctive communities represented mainly by Actinomycetales, Rhodobacteraceae, Cryomorphaceae, and Flavobacteriaceae were associated with Estuarine Fresh Waters, whereas Cenarchaeaceae and Oceanospirillales were representative of Modified Sub Antarctic Waters present in the fjord. Salinity and oxygen were first-order factors explaining segregation of microbial communities in these contrasting water masses. Positive correlations of members of Flavobacteriaceae, Alteromonadales, and Verrucomicrobiales with diatoms in subsurface waters and of Flavobacteriales (Cryomorphaceae and Flavobacteriaceae), Rhodobacteraceae, and Pelagibacteraceae with dinoflagellates in surface waters suggest that phytoplankton composition could define specific niches for microorganisms in Puyuhuapi fjord waters. A dramatic reduction of richness and individual abundances within Flavobacteriaceae, Rhodobacteraceae, and Cenarchaeaceae families was principally explained by seasonal increase of surface water temperature, with major reduction associated with changes in temperature during winter conditions. Taxa that are sensitive to increased temperature are key components of organic matter and element cycling, and we therefore suggest that potential decrease in diversity associated with rising of surface water temperature could impact current biogeochemical status of Patagonian fjord ecosystems.
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