Database of diazotrophs in global ocean: abundances, biomass and nitrogen fixation rates

[EN] Marine N2 fixing microorganisms, termed diazotrophs, are a key functional group in marine pelagic ecosystems. The biological fixation of dinitrogen (N2) to bioavailable nitrogen provides an important new source of nitrogen for pelagic marine ecosystems 5 and influences primary productivity and organic matter export to the deep ocean. As one of a series of efforts to collect biomass and rates specific to different phytoplankton functional groups, we have constructed a database on diazotrophic organisms in the global pelagic upper ocean by compiling about 12 000 direct field measurements of cyanobacterial diazotroph abundances (based on microscopic cell counts or qPCR 10 assays targeting the nifH genes) and N2 fixation rates. Biomass conversion factors are estimated based on cell sizes to convert  abundance data to diazotrophic biomass. The database is limited spatially, lacking large regions of the ocean especially in the Indian Ocean. The data are approximately log-normal distributed, and large variances exist in most sub-databases with non-zero values differing 5 to 8 orders of magnitude. 15 Lower mean N2 fixation rate was found in the North Atlantic Ocean than the Pacific Ocean. Reporting the geometric mean and the range of one geometric standard error below and above the geometric mean, the pelagic N2 fixation rate in the global ocean is estimated to be 62 (53–73) TgNyr−1 and the pelagic diazotrophic biomass in the global ocean is estimated to be 4.7 (2.3–9.6) TgC from cell counts and to 89 (40–20 200) TgC from nifH-based abundances. Uncertainties related to biomass conversion factors can change the estimate of geometric mean pelagic diazotrophic biomass in the global ocean by about ±70 %. This evolving database can be used to study spatial and temporal distributions and variations of marine N2 fixation, to validate geochemical estimates and to parameterize and validate biogeochemical models. The database is 25 stored in PANGAEA (http://doi.pangaea.de/10.1594/PANGAEA.774851).

Axenic cell culture of the seagrass Cymodocea nodosa from cotyledonary tissue

[EN] Plant Tissue Culture, also called “micropropagation”, is the propagation of plants from different tissues (or explants) in a shorter time than conventional propagation, making use of the ability that many plant cells have to regenerate a whole plant (totipotency).There are two alternative mechanisms by which an explant can regenerate an entire plant, namely organogenesis and somatic embryogenesis. Since the last decades, the number of higher terrestrial plants species from which these techniques have been successfully applied has continually increased. However, few attempts have been carried out in marine plants. Previous seagrasses authors have focused their studies on i) vegetative propagation of rhizome fragments as explants in Ruppia maritima, Halophila engelmannii, Cymodocea nodosa and Posidonia oceanica; ii) culture of meristems in Heterozostera tasmanica, C. nodosa or P. oceanica; and iii) culture of germinated seeds on aseptic conditions, in Thalassia testudinum, H. ovalis, P. coriacea, P. oceanica, and H. decipiens. All these studies determine the most adequate culture medium for each species (seawater, nutrients, vitamins, carbon sources, etc...), often supplemented with different plant growth regulators and the necessary conditions for the culture maintenance, such as light and temperature. On the other hand, several studies have previously established protocols for cell or protoplast isolation in the species Zostera marina, Z. muelleri, P. oceanica, and C. nodosa, using shoots collected from natural meadows as original vegetal source, but further cell growth was never accomplished. Due to the absence of somatic embryogenesis or organogenetic studies in seagrasses we wonder: IS THE SUCCESSFUL APPLICATION OF TISSUE CULTURE TECHNIQUES POSSIBLE IN SEAGRASSES?