The requirement for external carbonic anhydrase in diatoms is influenced by the supply and demand for dissolved inorganic carbon.

Photosynthesis by marine diatoms contributes significantly to the global carbon cycle. Due to the low concentration of CO in seawater, many diatoms use extracellular carbonic anhydrase (eCA) to enhance the supply of CO to the cell surface. While much research has investigated how the requirement for eCA is influenced by changes in CO availability, little is known about how eCA contributes to CO supply following changes in the demand for carbon.

Widespread use of proton-pumping rhodopsin in Antarctic phytoplankton.

Photosynthetic carbon (C) fixation by phytoplankton in the Southern Ocean (SO) plays a critical role in regulating air-sea exchange of carbon dioxide and thus global climate. In the SO, photosynthesis (PS) is often constrained by low iron, low temperatures, and low but highly variable light intensities. Recently, proton-pumping rhodopsins (PPRs) were identified in marine phytoplankton, providing an alternate iron-free, light-driven source of cellular energy.

C NMR metabolomics: J-resolved STOCSY meets INADEQUATE.

Robust annotation of metabolites is a challenging task in metabolomics. Among available applications, C NMR experiment INADEQUATE determines direct C-C connectivity unambiguously, offering indispensable information on molecular structure. Despite its great utility, it is not always practical to collect INADEQUATE data on every sample in a large metabolomics study because of its relatively long experiment time.

The BBSome restricts entry of tagged carbonic anhydrase 6 into the cis-flagellum of Chlamydomonas reinhardtii.

The two flagella of Chlamydomonas reinhardtii are of the same size and structure but display functional differences, which are critical for flagellar steering movements. However, biochemical differences between the two flagella have not been identified. Here, we show that fluorescence protein-tagged carbonic anhydrase 6 (CAH6-mNG) preferentially localizes to the trans-flagellum, which is organized by the older of the two flagella-bearing basal bodies.

Molecular composition and biodegradation of loggerhead sponge Spheciospongia vesparium exhalent dissolved organic matter.

Sponges are critical components of marine reefs due to their high filtering capacity, wide abundance, and alteration of biogeochemical cycling. Here, we characterized dissolved organic matter (DOM) composition in the sponge holobiont exhalent seawater of a loggerhead sponge (Spheciospongia vesparium) and in ambient seawater in Florida Bay (USA), as well as the microbial responses to each DOM pool through dark incubations. The sponge holobiont removed 6% of the seawater dissolved organic carbon (DOC), utilizing compounds that were low in carbon and oxygen, yet high in nitrogen content relative to the ambient seawater.

Influence of Temperature and CO On Plasma-membrane Permeability to CO and HCO in the Marine Haptophytes Emiliania huxleyi and Calcidiscus leptoporus (Prymnesiophyceae).

Membrane permeabilities to CO and HCO constrain the function of CO concentrating mechanisms that algae use to supply inorganic carbon for photosynthesis. In diatoms and green algae, plasma membranes are moderately to highly permeable to CO but effectively impermeable to HCO . Here, CO and HCO membrane permeabilities were measured using an O-exchange technique on two species of haptophyte algae, Emiliania huxleyi and Calcidiscus leptoporus, which showed that the plasma membranes of these species are also highly permeable to CO (0.

Automated classification of three-dimensional reconstructions of coral reefs using convolutional neural networks.

Coral reefs are biologically diverse and structurally complex ecosystems, which have been severally affected by human actions. Consequently, there is a need for rapid ecological assessment of coral reefs, but current approaches require time consuming manual analysis, either during a dive survey or on images collected during a survey. Reef structural complexity is essential for ecological function but is challenging to measure and often relegated to simple metrics such as rugosity.

Reduced nitrogenase efficiency dominates response of the globally important nitrogen fixer Trichodesmium to ocean acidification.

The response of the prominent marine dinitrogen (N)-fixing cyanobacteria Trichodesmium to ocean acidification (OA) is critical to understanding future oceanic biogeochemical cycles. Recent studies have reported conflicting findings on the effect of OA on growth and N fixation of Trichodesmium. Here, we quantitatively analyzed experimental data on how Trichodesmium reallocated intracellular iron and energy among key cellular processes in response to OA, and integrated the findings to construct an optimality-based cellular model.

Pervasive iron limitation at subsurface chlorophyll maxima of the California Current.

Subsurface chlorophyll maximum layers (SCMLs) are nearly ubiquitous in stratified water columns and exist at horizontal scales ranging from the submesoscale to the extent of oligotrophic gyres. These layers of heightened chlorophyll and/or phytoplankton concentrations are generally thought to be a consequence of a balance between light energy from above and a limiting nutrient flux from below, typically nitrate (NO). Here we present multiple lines of evidence demonstrating that iron (Fe) limits or with light colimits phytoplankton communities in SCMLs along a primary productivity gradient from coastal to oligotrophic offshore waters in the southern California Current ecosystem.

Plasma Membrane-Type Aquaporins from Marine Diatoms Function as CO/NH Channels and Provide Photoprotection.

Aquaporins (AQPs) are ubiquitous water channels that facilitate the transport of many small molecules and may play multiple vital roles in aquatic environments. In particular, mechanisms to maintain transmembrane fluxes of important small molecules have yet to be studied in marine photoautotrophic organisms. Here, we report the occurrence of multiple AQPs with differential cellular localizations in marine diatoms, an important group of oceanic primary producers.

Dynamic changes in carbonate chemistry in the microenvironment around single marine phytoplankton cells.

Photosynthesis by marine diatoms plays a major role in the global carbon cycle, although the precise mechanisms of dissolved inorganic carbon (DIC) uptake remain unclear. A lack of direct measurements of carbonate chemistry at the cell surface has led to uncertainty over the underlying membrane transport processes and the role of external carbonic anhydrase (eCA). Here we identify rapid and substantial photosynthesis-driven increases in pH and [CO] primarily due to the activity of eCA at the cell surface of the large diatom Odontella sinensis using direct simultaneous microelectrode measurements of pH and CO along with modelling of cell surface inorganic carbonate chemistry.

Mechanisms of carbon dioxide acquisition and CO sensing in marine diatoms: a gateway to carbon metabolism.

Diatoms are one of the most successful marine eukaryotic algal groups, responsible for up to 20% of the annual global CO fixation. The evolution of a CO-concentrating mechanism (CCM) allowed diatoms to overcome a number of serious constraints on photosynthesis in the marine environment, particularly low [CO] in seawater relative to concentrations required by the CO fixing enzyme, ribulose-1,5-bisphosphate carboxylase/oxygenase (RubisCO), which is partly due to the slow diffusion rate of CO in water and a limited CO formation rate from [Formula: see text] in seawater. Diatoms use two alternative strategies to take up dissolved inorganic carbon (DIC) from the environment: one primarily relies on the direct uptake of [Formula: see text] through plasma-membrane type solute carrier (SLC) 4 family [Formula: see text] transporters and the other is more reliant on passive diffusion of CO formed by an external carbonic anhydrase (CA).

The potential for co-evolution of CO2-concentrating mechanisms and Rubisco in diatoms.

Diatoms are a diverse group of unicellular algae that contribute significantly to global photosynthetic carbon fixation and export in the modern ocean, and are an important source of microfossils for paleoclimate reconstructions. Because of their importance in the environment, diatoms have been a focus of study on the physiology and ecophysiology of carbon fixation, in particular their CO2-concentrating mechanisms (CCMs) and Rubisco characteristics. While carbon fixation in diatoms is not as well understood as in certain model aquatic photoautotrophs, a greater number of species have been examined in diatoms.

The diversity of CO2-concentrating mechanisms in marine diatoms as inferred from their genetic content.

Marine diatoms are one of the most ecologically significant primary producers in the ocean. Most diatoms use a CO2-concentrating mechanism (CCM) to overcome the scarcity of CO2 in the ocean and limitations of the carbon-fixing enzyme Rubisco. However, the CCMs in model diatoms differ substantially in their genetic make-up and structural organization.

The physiology and genetics of CO2 concentrating mechanisms in model diatoms.

Diatoms, a diverse and ecologically-important group of unicellular algae, use a CO2 concentrating mechanism to enhance the performance of RubisCO and overcome the limited availability of CO2 in their habitats. The recent development of genetic manipulation techniques for the model diatoms Phaeodactylum tricornutum and Thalassiosira pseudonana and the sequencing of their genomes have enabled the rapid identification of genes involved in their CO2 concentrating mechanisms (CCMs). These include numerous carbonic anhydrases (CAs), which are localized to distinct subcellular compartments in the two diatom species, and putative bicarbonate transporters, one of which has been functionally characterized.

Microelectrode characterization of coral daytime interior pH and carbonate chemistry.

Reliably predicting how coral calcification may respond to ocean acidification and warming depends on our understanding of coral calcification mechanisms. However, the concentration and speciation of dissolved inorganic carbon (DIC) inside corals remain unclear, as only pH has been measured while a necessary second parameter to constrain carbonate chemistry has been missing. Here we report the first carbonate ion concentration ([CO3(2-)]) measurements together with pH inside corals during the light period.

Size scaling of extracellular carbonic anhydrase activity in centric marine diatoms.

Many microalgae have a surface-associated extracellular carbonic anhydrase (eCA) that converts HCO3 (-) to CO2 for uptake and subsequent photosynthetic fixation. We investigated eCA activity and assessed its importance for photosynthetic CO2 supply in six centric diatom species spanning nearly the full range of cell sizes for centric diatoms (equivalent spherical radius 3-67 μm). Since larger cells are more susceptible to diffusion limitation, we hypothesized that eCA activity would increase with cell size as would its importance for CO2 supply.

Marine diatom proteorhodopsins and their potential role in coping with low iron availability.

Proteorhodopsins (PR) are retinal-binding membrane proteins that function as light-driven proton pumps to generate energy for metabolism and growth. Recently PR-like genes have been identified in some marine eukaryotic protists, including diatoms, dinoflagellates, haptophytes and cryptophytes. These rhodopsins are homologous to green-light-absorbing, ATP-generating PRs present within bacteria.

Internal carbonic anhydrase activity in the tissue of scleractinian corals is sufficient to support proposed roles in photosynthesis and calcification.

Reef-building corals import inorganic carbon (Ci) to build their calcium carbonate skeletons and to support photosynthesis by the symbiotic algae that reside in their tissue. The internal pathways that deliver Ci for both photosynthesis and calcification are known to involve the enzyme carbonic anhydrase (CA), which interconverts CO2 and HCO3 (-). We have developed a method for absolute quantification of internal CA (iCA) activity in coral tissue based on the rate of (18)O-removal from labeled Ci.

The minimal CO2-concentrating mechanism of Prochlorococcus spp. MED4 is effective and efficient.

As an oligotrophic specialist, Prochlorococcus spp. has streamlined its genome and metabolism including the CO2-concentrating mechanism (CCM), which serves to elevate the CO2 concentration around Rubisco. The genomes of Prochlorococcus spp.

Low temperature reduces the energetic requirement for the CO2 concentrating mechanism in diatoms.

The goal of this study is to investigate the CO2 concentrating mechanism (CCM) of the dominant phytoplankton species during the growing season at Palmer station in the Western Antarctic Peninsula. Key CCM parameters (cellular half-saturation constants for CO2 fixation, carbonic anhydrase activity, CO2 /HCO3 (-) uptake, δ(13) Corg ) in natural phytoplankton assemblages were determined. Those results, together with additional measurements on CO2 membrane permeability from Fragilariopsis cylindrus laboratory cultures, were used to develop a numerical model of the CCM of cold water diatoms.

Localization of putative carbonic anhydrases in the marine diatom, Thalassiosira pseudonana.

Thirteen putative carbonic anhydrase (CA) genes have been identified in the marine multipolar centric diatom, Thalassiosira pseudonana, and two of these CAs have been localized previously. The first, an alpha CA (TpαCA1), was localized in the chloroplast stroma; the second, a zeta-type CA (TpζCA1), was localized to the periplasmic space. In the present study, cloning and localization of the remaining CAs were carried out.

A chloroplast pump model for the CO2 concentrating mechanism in the diatom Phaeodactylum tricornutum.

Prior analysis of inorganic carbon (Ci) fluxes in the diatom Phaeodactylum tricornutum has indicated that transport of Ci into the chloroplast from the cytoplasm is the major Ci flux in the cell and the primary driving force for the CO2 concentrating mechanism (CCM). This flux drives the accumulation of Ci in the chloroplast stroma and generates a CO2 deficit in the cytoplasm, inducing CO2 influx into the cell. Here, the "chloroplast pump" model of the CCM in P.

Quantification of extracellular carbonic anhydrase activity in two marine diatoms and investigation of its role.

Many microalgae induce an extracellular carbonic anhydrase (eCA), associated with the cell surface, at low carbon dioxide (CO2) concentrations. This enzyme is thought to aid inorganic carbon uptake by generating CO2 at the cell surface, but alternative roles have been proposed. We developed a new approach to quantify eCA activity in which a reaction-diffusion model is fit to data on (18)O removal from inorganic carbon.

Sizing up metatranscriptomics.

A typical marine bacterial cell in coastal seawater contains only ∼200 molecules of mRNA, each of which lasts only a few minutes before being degraded. Such a surprisingly small and dynamic cellular mRNA reservoir has important implications for understanding the bacterium's responses to environmental signals, as well as for our ability to measure those responses. In this perspective, we review the available data on transcript dynamics in environmental bacteria, and then consider the consequences of a small and transient mRNA inventory for functional metagenomic studies of microbial communities.