Ocean Sampling Day was initiated by the EU-funded Micro B3 (Marine Microbial Biodiversity, Bioinformatics, Biotechnology) project to obtain a snapsho

Despite considerable research on the linkages between dissolved organic matter (DOM) and bacteria, it is not yet clear how the abundance of the main aquatic clades relates to DOM composition in natural aquatic systems. We evaluated this relation using PARAFAC modeling of excitation–emission fluorescence spectroscopy and spectroscopic indexes to characterize DOM composition, and fluorescence in situ hybridization, to quantify the major bacterial groups in a subtropical lagoon. The DOM exhibited marked temporal variations in concentration, molecular weight, aromaticity, color, degree of humification, and freshness, and proportion of the three different fluorescent components identified. All major bacterial clades (Alphaproteobacteria, Betaproteobacteria, Gammaproteobacteria, and Cytophaga‐Flavobacteria) were significantly linked to DOM concentration and/or composition, being those crucial factors for modeling their abundance in situ. The combination and significance of the factors was specific for each bacterial group, strongly indicating that they behave as coherent and distinctive units. Cytophaga‐Flavobacteria and Betaproteobacteria were the groups which correlated with more DOM properties. Alphaproteobacteria and Gammaproteobacteria abundances were significantly explained by low or high dissolved organic carbon concentrations, respectively. The significant relationships between DOM properties and the main bacterial groups delineated a profile of each group regarding DOM preferences/dislikes, in agreement with evidence derived from genome analysis to single‐cell substrate uptake. These results highlight the specificities of the main bacterial clades, providing support for a functional classification of the bacterioplankton regarding DOM processing at the level of bacterial classes.

Measurements of dissolved organic carbon (DOC), nitrogen (DON), and phosphorus (DOP) concentrations are used to characterize the dissolved organic matter (DOM) pool and are important components of biogeochemical cycling in the coastal ocean. Here, we present the first edition of a global database (CoastDOM v1; available at https://doi.org/10.1594/PANGAEA.964012, Lønborg et al., 2023) compiling previously published and unpublished measurements of DOC, DON, and DOP in coastal waters. These data are complemented by hydrographic data such as temperature and salinity and, to the extent possible, other biogeochemical variables (e.g. chlorophyll a, inorganic nutrients) and the inorganic carbon system (e.g. dissolved inorganic carbon and total alkalinity). Overall, CoastDOM v1 includes observations of concentrations from all continents. However, most data were collected in the Northern Hemisphere, with a clear gap in DOM measurements from the Southern Hemisphere. The data included were collected from 1978 to 2022 and consist of 62 338 data points for DOC, 20 356 for DON, and 13 533 for DOP. The number of measurements decreases progressively in the sequence DOC > DON > DOP, reflecting both differences in the maturity of the analytical methods and the greater focus on carbon cycling by the aquatic science community. The global database shows that the average DOC concentration in coastal waters (average ± standard deviation (SD): 182±314 µmol C L⁻¹; median: 103 µmol C L⁻¹) is 13-fold higher than the average coastal DON concentration (13.6±30.4 µmol N L⁻¹; median: 8.0 µmol N L⁻¹), which is itself 39-fold higher than the average coastal DOP concentration (0.34±1.11 µmol P L⁻¹; median: 0.18 µmol P L⁻¹). This dataset will be useful for identifying global spatial and temporal patterns in DOM and will help facilitate the reuse of DOC, DON, and DOP data in studies aimed at better characterizing local biogeochemical processes; closing nutrient budgets; estimating carbon, nitrogen, and phosphorous pools; and establishing a baseline for modelling future changes in coastal waters.

The role of ecophysiological traits in the success and expansion of the toxic cyanobacterium Cylindrospermopsis raciborskii is still under debate. One key factor appears to be the high physiological flexibility of this organism when obtaining limiting resources. Recent studies have found that filamentous bloom-forming cyanobacteria are able to optimize their growth by adjusting phosphate uptake during fluctuating nutrient conditions. We investigated the growth response of two phosphate-deficient C. raciborskii isolates (MVCC19 from Uruguay and CCMP1973 from USA) to short-term fluctuations in phosphate supply. These isolates were exposed to five phosphate concentrations which were provided in two supply modes: a single pulse (SingleP) versus the same amount divided in 10 pulses (TenP), with one pulse applied every 6 min. Morphological traits and changes in chlorophyll a and phycocyanin fluorescence were also evaluated. Growth rates of CCMP1973 and MVCC19 almost doubled and tripled, respectively, when exposed to multiple rather than single phosphate additions. Different growth rates were observed with the same total added resource, thus contradicting the classical model of dependence of growth rate on absolute external concentration. Phosphate-deficient C. raciborskii showed a remarkable physiological flexibility in adapting to phosphate availability on a timescale from minutes to hours. The TenP mode provided an extension of phosphate exposure time that allowed the energetic optimization of uptake and growth. The morphological plasticity of the species in response to phosphate supply mode was also shown by differences in trichome length and individual size. Our results are the first evidence of growth optimization of phosphate-deficient C. raciborskii to short-term nutrient fluctuations, revealing its physiological flexibility. This adaptive behaviour may help to explain the invasive success of this diazotrophic cyanobacterium in a wide range of aquatic ecosystems where phosphorus is frequently the limiting resource.