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Givati, S.

Publications and source records attributed to Givati, S..

2 recordsLinked to original sources

Dynamics of cell death due to N and P starvation across intra-clade diversity in Prochlorococcus

Nutrient starvation and subsequent mortality are processes that can shape ecosystem dynamics and influence global biogeochemical cycles yet are poorly understood. Here, we examined the dynamics of culture decline in 15 strains of Prochlorococcus, globally abundant marine cyanobacteria, under nitrogen (N) and phosphate (P) starvation. We then ask whether mortality patterns can be related to the evolutionary history of each strain, the geographic location and environmental conditions where it was isolated from, or the copy number of specific acquisition genes. We observed diverse decline patterns across starvation conditions and strains, identifying three differential features: maximum culture fluorescence, the number of fluorescence peaks during the decline stage, and the decline rate. Based on these features, each strain was categorized as being more sensitive to either nitrogen starvation or phosphorus/co-starvation. High light (HL) strains are more sensitive to N starvation, whereas other facets of the strains evolutionary or ecological origin were not correlated with mortality features. Surprisingly, the number of genes known to be involved in either N or P acquisition in each genome was not correlated with starvation sensitivity. Rather, genes involved in DNA damage repair were associated with N sensitivity to starvation, especially in HL strains, whereas genes related to protein quality control were more abundant in LL strains and associated with P/co starvation sensitivity. These findings reveal a previously unrecognized diversity in the dynamics of starvation and mortality across closely related Prochlorococcus strains, potentially driven by differences in the responses to DNA and protein damage.

microbiology↗

Seasonal dynamics of phytoplankton and bacterioplankton at the ultra-oligotrophic southeastern Mediterranean Sea

The Eastern Mediterranean Sea (EMS) is a poorly studied ultra-oligotrophic marine environment, dominated by small-size phyto- and bacterioplankton. Here, we describe the dynamics of a single annual cycle (2018-19) of phyto- and bacterioplankton (abundances, pigments and productivity) in relation to the physical and chemical conditions in the photic water column at an offshore EMS site (Station THEMO-2, [~]1,500m depth, 50km offshore). We show that phytoplankton biomass (as chlorophyll a), primary and bacterial productivity differed between the mixed winter (January-April) and the thermally stratified (May-December) periods. Prochlorococcus and Synechococcus numerically dominated the picophytoplankton populations, with each clade revealing different temporal and depth changes indicative to them, while pico-eukaryotes (primarily haptophytes) were less abundant, yet likely contributed significant biomass. Estimated primary productivity ([~]32 gC m-2 y-1) was lower compared with other well-studied oligotrophic locations, including the north Atlantic and Pacific (BATS and HOT observatories), the western Mediterranean (DYFAMED observatory) and the Red Sea, and was on-par with the ultra-oligotrophic South Pacific Gyre. In contrast, integrated bacterial production ([~]11 gC m-2 y-1) was similar to other oligotrophic locations. Phytoplankton seasonal dynamics were similar to those at BATS and the Red Sea, suggesting an observable effect of winter mixing in this ultra-oligotrophic location. These results highlight the ultra-oligotrophic conditions in the EMS and provide, for the first time in this region, a full-year baseline and context to ocean observatories in the region. HighlightsO_LIBacterioplankton dynamics were assessed monthly in the Eastern Mediterranean Sea C_LIO_LISmall-sized picophytoplankton numerically dominated the phytoplankton community C_LIO_LISeasonal phytoplankton dynamics are similar to BATS and Red Sea, but not to HOT C_LIO_LIAnnual primary productivity is among the lowest in the worlds oceans C_LIO_LIBacterial to primary production ratio is higher than most oligotrophic seas C_LI

microbiology↗