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Zweifel, S. T.

Publications and source records attributed to Zweifel, S. T..

3 recordsLinked to original sources

GUARDIANS OF THE CELL: COCCOSPHERE PREVENTS OPPORTUNISTIC BACTERIA ATTACK IN HEAVY CALCIFYING COCCOLITHOPHORE

Coccolithophores are responsible for 40-60% of marine calcium carbonate production. This occurs through the biomineralization of extracellular calcium carbonate plates that encase the cell in a structure called the coccosphere. Despite its central role in ocean biogeochemistry, the function of coccolithophore calcification remains unresolved. One hypothesis is that the coccosphere acts as a physical shield, deterring predators and microbes. While its protective role has been investigated against grazers and viruses, its function in bacterial defense remains untested. Here, we investigate the interaction between heavily calcified Coccolithus braarudii and the bacterial pathogen Phaeobacter inhibens, known for its lethal Jekyll and Hyde relationship with the bloom-forming Gephyrocapsa huxleyi. We find that in C. braarudii, no P. inhibens pathogenicity is observed--unless the algae are decalcified. Upon decalcification, the relationship with P. inhibens becomes pathogenic, leading to algal cell death. Mortality of decalcified cells is specific to interactions with P. inhibens and is attachment-mediated: no toxicity is observed when cells are exposed to P. inhibens supernatant or to growth-inhibiting concentrations of indole-3-acetic acid-- identified in the P. inhibens-G. huxleyi system. Attachment requirement is further supported by scanning electron microscopy, which reveals extensive bacterial colonization on decalcified but not on calcified C. braarudii with P. inhibens. These findings provide the first experimental evidence that the coccosphere acts as a physical barrier against bacterial attack, underscoring its defensive role in coccolithophores.

microbiology↗

Risk-reward trade-off in motility endurance generates dichotomy in search strategies among copiotrophic marine bacteria

Coptiotrophic marine bacteria contribute significantly to carbon storage in the ocean by remineralizing organic carbon present in nutrient-rich hotspots amidst oligotrophic waters. Motility is both highly beneficial and costly in such environments, presenting copiotrophs with a risk-reward trade-off in search behavior. Here we studied the motility endurance of 26 marine isolates using video microscopy and cell tracking over two days of carbon starvation. We found that this cost-benefit trade-off results in a distinct dichotomy among marine bacteria: risk-averse copiotrophs ceased motility within hours ( limostatic), whereas risk-prone copiotrophs converted 10% of their biomass per day into energy to retain motility for the two days of observation ( limokinetic). We identified a genomic component of this dichotomy, sufficiently robust to predict the response of additional species with 83% accuracy and the prevalence of both strategies in the ocean. This dichotomy can facilitate the incorporation of the bacterial contribution in ocean carbon cycle models.

microbiology↗

Bacteria induce an amoeboid phase in coccolithophores that persists after bloom collapse

Coccolithophores, who contribute approximately 1-10% of phytoplankton biomass, are crucial players in the oceans biogeochemical cycles. Significant contributions come from bloom-forming species including Gephyrocapsa huxleyi (formerly Emiliania huxleyi), which has served as a model system for investigating algal-bacterial and agal-viral interactions as well as algal fitness responses to environmental changes. Coccolithophores follow a biphasic lifecycle, existing as motile haploid and non-motile diploid phases. Here we characterize a third, amoeboid phase, using a combination of light, electron and phase amplitude modulation (PAM) microscopy. Using time-resolved imaging we captured the rapid morphological transition from a spherical haploid to an elongated motile amoeboid cell. Cell tracking revealed slower and more directional swimming compared to haploid cells. Amoeboid metamorphosis was triggered by exposure to bacteria, including strains isolated from G. huxleyi blooms and known G. huxleyi pathogens, but not by a range of classical phytoplankton stressors, including viral infection and oxidative stress. Further, the sub-population of haploids which switched to the amoeboid phase persisted past the rapid crash of the haploid population. This amoeboid phase was only observed in the primary bloom-forming coccolithophore species G. huxleyi and Geopharycapsa oceanica in stationary phase when exposed to high bacterial concentrations, typical of late-stage algal bloom events. Photophysiology of amoeboid cells was confirmed to be unaltered via PAM microscopy, indicating these cells are metabolically active. These findings highlight a previously uncharacterized morphotype in this important phytoplankton species and suggest that the amoeboid phase could be a bacteria-resistant morphotype following algal bloom collapse.

microbiology↗