Abstract
Dark ocean microbial dynamics are fundamental to understand ecosystem metabolism and ocean biogeochemical processes. Yet, the ecological response of deep ocean communities to environmental perturbations remains largely unknown. Temporal and spatial dynamics of the meso- and bathypelagic prokaryotic communities were assessed throughout a 2-year seasonal sampling across the western Mediterranean Sea. A common pattern of prokaryotic communities’ depth stratification was observed across the different regions and throughout the seasons. However, sporadic and drastic alterations of the community composition and diversity occurred either at specific water masses or throughout the aphotic zone and at a basin scale. Environmental changes resulted in a major increase in the abundance of rare or low abundant phylotypes and a profound change of the community composition. Our study evidences the temporal dynamism of dark ocean prokaryotic communities, exhibiting long periods of stability but also drastic changes, with implications in community metabolism and carbon fluxes. Taken together, the results highlight the importance of monitoring the temporal patterns of dark ocean prokaryotic communities.
Highlights
Marine prokaryotes are crucial for the global ocean biogeochemical cycles[1]
Our results show that the dark prokaryotic communities are depth-stratified and temporally dynamic throughout the basin, occasionally exhibiting pronounced changes in community composition, cell abundance and contribution of high nucleic acid (HNA) cells to the prokaryotic community at several spatial scales
By performing a spatio-temporal survey of meso- and bathypelagic prokaryotic communities, we show that dark ocean prokaryotic communities were temporally dynamic, changing severely their structure
Summary
Marine prokaryotes are crucial for the global ocean biogeochemical cycles[1]. The relation between the prokaryotic community composition, metabolic activity and biogeochemical fluxes is critical in ecosystem function and to understand ecosystem response to natural or anthropogenic c hanges[2]. Diverse physical phenomena have been described in the Mediterranean Sea, such as open-sea intense convective mixing, cascading of dense shelf waters and other mesoscale d ynamics[35,36], that can have an effect on deep-sea community composition and activity[20,21]. These hydrographic dynamics can transport surface communities to deeper layers, increase ventilation and sediment resuspension and change the quality and quantity of organic matter pools[37,38,39,40]. The response of dark ocean communities to temporal disturbances and the identification of the members leading the ecosystem response remain largely unknown
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