Food for all? Wildfire ash fuels growth of diverse eukaryotic plankton.

In December 2017, one of the largest wildfires in California history, the Thomas Fire, created a large smoke and ash plume that extended over the northeastern Pacific Ocean. Here, we explore the impact of Thomas Fire ash deposition on seawater chemistry and the growth and composition of natural microbial communities. Experiments conducted in coastal California waters during the Thomas Fire revealed that leaching of ash in seawater resulted in significant additions of dissolved nutrients including inorganic nitrogen (nitrate, nitrite and ammonium), silicic acid, metals (iron, nickel, cobalt and copper), organic nitrogen and organic carbon. After exposure to ash leachate at high (0.25 g ash l-1) and low (0.08 g ash l-1) concentrations for 4 days, natural microbial communities had 59-154% higher particulate organic carbon concentrations than communities without ash leachate additions. Additionally, a diverse assemblage of eukaryotic microbes (protists) responded to the ash leachate with taxa from 11 different taxonomic divisions increasing in relative abundance compared with control treatments. Our results suggest that large fire events can be important atmospheric sources of nutrients (particularly nitrogen) to coastal marine systems, where, through leaching of various nutrients, ash may act as a 'food for all' in protist communities.

Ocean fertilization: a potential means of geoengineering?

The oceans sequester carbon from the atmosphere partly as a result of biological productivity. Over much of the ocean surface, this productivity is limited by essential nutrients and we discuss whether it is likely that sequestration can be enhanced by supplying limiting nutrients. Various methods of supply have been suggested and we discuss the efficacy of each and the potential side effects that may develop as a result. Our conclusion is that these methods have the potential to enhance sequestration but that the current level of knowledge from the observations and modelling carried out to date does not provide a sound foundation on which to make clear predictions or recommendations. For ocean fertilization to become a viable option to sequester CO2, we need more extensive and targeted fieldwork and better mathematical models of ocean biogeochemical processes. Models are needed both to interpret field observations and to make reliable predictions about the side effects of large-scale fertilization. They would also be an essential tool with which to verify that sequestration has effectively taken place. There is considerable urgency to address climate change mitigation and this demands that new fieldwork plans are developed rapidly. In contrast to previous experiments, these must focus on the specific objective which is to assess the possibilities of CO2 sequestration through fertilization.

Carbon dioxide-concentrating mechanism and the development of extracellular carbonic anhydrase in the marine picoeukaryote Micromonas pusilla.

A range of marine photosynthetic picoeukaryote phytoplankton species grown in culture were screened for the presence of extracellular carbonic anhydrase (CAext ), a key enzyme in inorganic carbon acquisition under carbon- limiting conditions in some larger marine phytoplankton species. Of the species tested, extracellular carbonic anhydrase was detected only in Micromonas pusilla Butcher. The rapid, light-dependent development of CAext when cells were transferred from carbon-replete to carbon-limiting conditions was regulated by the available free- CO2 concentration and not by total dissolved inorganic carbon. Kinetic studies provided support for a CO2 - concentrating mechanism in that the K0.5 [CO2 ] (i.e. the CO2 concentration required for the half-maximal rate of photosynthesis) was substantially lower than the Km [CO2 ] of Rubisco from related taxa, whilst the intracellular carbon pool was at least seven fold greater than the extracellular DIC concentration, for extracellular DIC values ⩽1.0 mm. It is proposed that when the flux of CO2 into the cell is insufficient to support the photosynthetic rate at an optimum photon irradiance, the development of CAext increases the availability of CO2 at the plasma membrane. This ensures rapid acclimation to environmental change and provides an explanation for the central role of M. pusilla as a carbon sink in oligotrophic environments.

Dissolved inorganic carbon utilization and the development of extracellular carbonic anhydrase by the marine diatom Phaeodactylum tricornutum.

The presence of extracellular carbonic anhydrase (CA) in relation to medium composition was investigated using cultures of the marine diatom Phaeodactylum tricornutum Bohlin. Large-volume cultures, with low initial cell inocula were grown on ASP-2 (no dissolved inorganic carbon (DIC), 550 µM NOa - ), f/2 (2-0 mM DIC, 880µM NO3 - ) and modified f/2 (2.0 mM DIC, 20 µM NO3 - media. Cells growing on ASP-2 showed extracellular CA in the early stages of growth, whereas extracellular CA was not detected until partial depletion of total DIC in the stationary phase for cultures on f/2 or modified f/2. Both HCO3 - and CO2 were important in carbon limitation, extracellular CA being present when the free-CO2 concentration fell below 5 µM, but the HCO3 - concentration needed to be below 1 mM. When carbon-replete cells were transferred to carbon-limited conditions, extracellular CA was recorded within minutes, the process being light-dependent and completely inhibited by 3,3,4-dichlorophenyl-l, 1-dimethylurea (DCMU). The addition of DIC to carbon-limited cells resulted in a rapid decrease in extracellular CA activity. The membrane-impermeable inhibitor of carbonic anhydrase, dextran-bound sulphonamide (DBS) was used to inhibit extracellular CA activity in relation to photosynthetic rate in carbon-replete and carbon-limited cells. At the lowest DIC concentration (O'lOniM), for cells with maximum external CA activity, DBS gave over 80% inhibition of the photosynthetic rate, demonstrating the key role of external CA in maintaining high photosynthetic rate under conditions of carbon limitation. It is proposed that the key factor in the regulation of extracellular CA activity is the total Hux of inorganic carbon (C.) into the cell. This determines the Ci , flux into the chloroplast and when this is inadequate to support the photosynthetic rate attained by a carbon-replete chloroplast at optimum photon flux density, extracellular CA is activated. This mechanism would explain the observed interaction of CO2 and HCO3 - in the regulation of extracellular CA activity.