Dellwig, O. | Search bioRxiv

bioRxiv2024

Extraordinary physiology of polyphosphate-accumulating Beggiatoa mats suggests a key role for phosphate buffering in marine sediments

Filamentous sulfide-oxidizing Beggiatoa spp. are widespread in marine coastal environments and can achieve significant biomass because of their substantial size. Their ability to store phosphates in the polymerized form of polyphosphates makes them potentially key players in altering the phosphorus (P) cycle at the sediment-water interface. This study examined phosphate uptake and polyphosphate formation in a P starved culture of the Beggiatoa sp. 35Flor strain. Remarkably, even after severe P starvation over five generations, the survival of the cultures was 46%, demonstrating considerable plasticity to different levels of phosphate availability. Under these P-depleted conditions, 23% of filaments still contained polyphosphates, underscoring its critical role in their metabolism. Upon reintroduction of phosphate to starved cultures, an extremely rapid phosphate uptake was observed within the first 10 minutes, with rates reaching up to 298 mmol P g-1 protein d-1, which is significantly higher than values previously described in the literature for similar-sized organisms. The high phosphate uptake capacity of Beggiatoa spp., estimated at 0.6 - 6 mmol m-2 d-1 for typical densities of filaments in coastal sediments, suggests that these bacteria may play an important role in buffering the phosphate flux in these environments. Thereby, they reduce primary production and subsequent oxygen consumption by other organisms, creating a negative feedback loop that helps maintain ecosystem stability. ImportanceSulfide-oxidizing bacteria of the genus Beggiatoa occur ubiquitously in marine coastal sediments and have a large potential to influence phosphate fluxes at the sediment-water interface owing to their ability to accumulate polyphosphate and their large size. However, the extent to which these bacteria can contribute to phosphorus (P) sequestration or release remains poorly assessed. The importance of this study lies in demonstrating the unusual flexibility in adaptation of the Beggiatoa sp. 35Flor strain to varying P availability, including extreme P starvation, and its capacity to rapidly uptake and store available phosphate in the form of polyphosphate. When considered at a global scale, these physiological traits could lead to P retention in shallow coastal waters, which, in turn, profoundly impacts ecological stability and ecosystem functioning.

microbiology↗

bioRxiv2024

Decoding the Baltic Sea's Past and Present: A simple Molecular Index for Ecosystem Assessment

Marginal sea ecosystems, such as the Baltic Sea, are severely affected by anthropogenic pressures, such as climate warming, pollution, and eutrophication, which increased in the course of the past century. Biodiversity monitoring data and assessment of environmental status in such systems have typically been carried out only for the past few decades, if at all, and knowledge on pre-impact stability and good ecological status is limited. An extension of monitoring time series can potentially be achieved through analyses of paleoecological records, e.g. for phytoplankton, which form the base of the food web and are highly susceptible to environmental changes. Within the phytoplankton community, dinoflagellates and diatoms play a significant role as primary producers, and their relative dominance in the spring bloom, calculated as Dia/Dino index, is used as an indicator for the environmental status of the Baltic Sea. To extend time series on the dominance patterns and include non-fossilized dinoflagellates, we here establish a simple droplet digital PCR (ddPCR) reaction on ancient DNA from sediment cores that decodes phytoplankton dynamics. We focus on two common spring bloom species, the diatom Skeletonema marinoi and the dinoflagellate Apocalathium malmogiense, for which we evaluate a DNA based dominance index. It performs very well in comparison to DNA metabarcoding and modern monitoring and can elucidate past species dominance across the past century in three basins of the Baltic and across millennia in two of these basins. For the past century, we see a dominance shift already starting before the mid-20th century in two of the Baltic Sea basins, thus substantially predating current monitoring programs. Shifts are only partly coeval among the cores and the index shows different degrees of stability. This pattern is confirmed across millennia, where a long-term stable relationship between the diatom and the dinoflagellate is observed in the Eastern Gotland Basin, while data from the Gulf of Finland bear testimony to a much more unstable relationship. This confirms that good ecological status based on the dominance pattern of diatoms and dinoflagellates must be established locally and exemplifies how sediment core DNA can be employed to extend monitoring data.

ecology↗