Members of the marine Roseobacter lineage have been characterized as ecological generalists, suggesting that there will be challenges in assigning well-delineated ecological roles and biogeochemical functions to the taxon. To address this issue, genome sequences of 32 Roseobacter isolates were analyzed for patterns in genome characteristics, gene inventory, and individual gene/ pathway distribution using three predictive frameworks: phylogenetic relatedness, lifestyle strategy and environmental origin of the isolate. For the first framework, a phylogeny containing five deeply branching clades was obtained from a concatenation of 70 conserved single-copy genes. Somewhat surprisingly, phylogenetic tree topology was not the best model for organizing genome characteristics or distribution patterns of individual genes/pathways, although it provided some predictive power. The lifestyle framework, established by grouping isolates according to evidence for heterotrophy, photoheterotrophy or autotrophy, explained more of the gene repertoire in this lineage. The environment framework had a weak predictive power for the overall genome content of each strain, but explained the distribution of several individual genes/pathways, including those related to phosphorus acquisition, chemotaxis and aromatic compound degradation. Unassembled sequences in the Global Ocean Sampling metagenomic data independently verified this global-scale geographical signal in some Roseobacter genes. The primary findings emerging from this comparative genome analysis are that members of the lineage cannot be easily collapsed into just a few ecologically differentiated clusters (that is, there are almost as many clusters as isolates); the strongest framework for predicting genome content is trophic strategy, but no single framework gives robust predictions; and previously unknown homologs to genes for H 2 oxidation, proteorhodopsin-based phototrophy, xanthorhodpsin-based phototrophy, and CO 2 fixation by Form IC ribulose-1,5-bisphosphate carboxylase/oxygenase (RuBisCO) expand the possible mechanisms for energy and carbon acquisition in this remarkably versatile bacterial lineage.

Bacterioplankton of the marine Roseobacter clade have genomes that reflect a dynamic environment and diverse interactions with marine plankton. Comparative genome sequence analysis of three cultured representatives suggests that cellular requirements for nitrogen are largely provided by regenerated ammonium and organic compounds (polyamines, allophanate, and urea), while typical sources of carbon include amino acids, glyoxylate, and aromatic metabolites. An unexpectedly large number of genes are predicted to encode proteins involved in the production, degradation, and efflux of toxins and metabolites. A mechanism likely involved in cell-to-cell DNA or protein transfer was also discovered: vir-related genes encoding a type IV secretion system typical of bacterial pathogens. These suggest a potential for interacting with neighboring cells and impacting the routing of organic matter into the microbial loop. Genes shared among the three roseobacters and also common in nine draft Roseobacter genomes include those for carbon monoxide oxidation, dimethylsulfoniopropionate demethylation, and aromatic compound degradation. Genes shared with other cultured marine bacteria include those for utilizing sodium gradients, transport and metabolism of sulfate, and osmoregulation.In surface waters of the open ocean, 1 in 10 bacterial cells is a member of the Roseobacter group (17). In coastal waters, the number of Roseobacter cells increases to 1 in 5 (11, 19). Despite their obvious ecological success, however, roseobacters do not fit the stereotype of a small, metabolically conservative, "oligotrophic" bacterium (8, 18). Instead, they are large (0.08 m 3 ) (38), easily cultured (19), and respond readily to increased substrate availability (7). Analysis of the first Roseobacter genome sequence, that of Silicibacter pomeroyi, revealed a fairly large genome (4.5 Mb) housing abundant and diverse transporters, complex regulatory systems, and multiple pathways for acquiring carbon and energy in seawater. Roseobacters thus appear to be quite versatile from metabolic and ecological standpoints (43), with an assortment of strategies for obtaining carbon and nutrients and, directly or indirectly, affecting the biogeochemical status of seawater.The availability of two additional closed genome sequences of cultured roseobacters provides the opportunity for an ecologically based analysis of the genetic capabilities of this bacterial taxon. The three organisms are assumed to have different niches in the surface ocean based on the conditions of their isolation: S. pomeroyi is a free-living heterotrophic bacterioplankter obtained from coastal seawater (43), congener Silicibacter sp. strain TM1040 (96% 16S rRNA sequence identity to S. pomeroyi [ Fig. 1]) is an associate of the marine dinoflagellate Pfiesteria piscicida (1, 40), and Jannaschia sp. strain CCS1 (with 94% 16S rRNA sequence identity to the two Silicibacter species) represents a recently discovered class of marine aerobic bacteriochlorophyll a-based phototrophs (4). Our comparative an...

Seeded calcite growth experiments were conducted at fixed pH (10.2) and two degrees of supersaturation (X = 5, 16), while varying the Ca 2+ to CO 3 2À solution ratio over several orders of magnitude. The calcite growth rate and the incorporation of Sr in the growing crystals strongly depended on the solution stoichiometry. At a constant degree of supersaturation, the growth rate was highest when the solution concentration ratio, r = [Ca 2+ ]/[CO 3 2À ], equaled one, and decreased symmetrically with increasing or decreasing values of r. This behavior is consistent with the kink growth rate theory for non-Kossel crystals, assuming that the frequency factors for attachment to kink sites are the same for the cation and anion. Measured Sr partition coefficients, D Sr , ranged from 0.02 to 0.12, and correlated positively with the calcite growth rate.

Models test our understanding of processes and can reach beyond the spatial and temporal scales of measurements. Multi-component Reactive Transport Models (RTMs), initially developed more than three decades ago, have been used extensively to explore the interactions of geothermal, hydrologic, geochemical, and geobiological processes in subsurface systems. Driven by extensive data sets now available from intensive measurements efforts, there is a pressing need to couple RTMs with other community models to explore non-linear interactions among the atmosphere, hydrosphere, biosphere, and geosphere. Here we briefly review the history of RTM development, summarize the current state of RTM approaches, and identify new research directions, opportunities, and infrastructure needs to broaden the use of RTMs. In particular, we envision the expanded use of RTMs in advancing process understanding in the Critical Zone, the veneer of the Earth that extends from the top of vegetation to the bottom of groundwater. We argue that, although parsimonious models are essential at larger scales, process-based models are the only way to explore the highly nonlinear coupling that characterizes natural systems. We present seven testable hypotheses that emphasize the unique capabilities of process-based RTMs for (1) elucidating chemical weathering and its physical and biogeochemical drivers; (2) understanding the interactions among roots, microorganisms , carbon, water, and minerals in the rhizosphere; (3) assessing the effects of heterogeneity across spatial and temporal scales; and (4) integrating the vast quantity of novel data, including-omics‖ data (genomics, transcriptomics, proteomics, metabolomics), elemental concentration and speciation data, and isotope data into our understanding of complex earth systems. With strong support from data-driven sciences, we are now in an exciting era where integration of RTM framework into other community models will facilitate process understanding across disciplines and across scales.

Iron oxides are important structural and biogeochemical components of soils that can be strongly altered by redox-driven processes. This study examined the influence of temporal oxygen variations on Fe speciation in soils from the Luquillo Critical Zone Observatory (Puerto Rico). We incubated soils under cycles of oxic-anoxic conditions (τ:τ = 1:6) at three frequencies with and without phosphate addition. Fe(II) production, P availability, and Fe mineral composition were monitored using batch analytical and spectroscopic techniques. The rate of soil Fe(II) production increased from ∼3 to >45 mmol Fe(II) kg d over the experiment with a concomitant increase of an Fe(II) concentration plateau within each anoxic period. The apparent maximum in Fe(II) produced is similar in all treatments, but was hastened by P-amendment. Numerical modeling suggests the Fe(II) dynamics can be explained by the formation of a rapidly reducible Fe(III) phases derived from the progressive dissolution and re-oxidation of native Fe(III) oxides accompanied by minor increases in Fe reducer populations. The shift in Fe(III) reactivity is evident from Fe-reducibility assays using Shewanella sp., however was undetectable by chemical extractions, Mössbauer or X-ray Absorption spectroscopies. More broadly, our findings suggest Fe reduction rates are strongly coupled to redox dynamics of the recent past, and that frequent shifts in redox conditions can prime a soil for rapid Fe-reduction.

Many microalgae induce an extracellular carbonic anhydrase (eCA), associated with the cell surface, at low carbon dioxide (CO 2 ) concentrations. This enzyme is thought to aid inorganic carbon uptake by generating CO 2 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. In contrast to previous methods, eCA activity is treated as a surface process, allowing the effects of eCA on cell boundary-layer chemistry to be assessed. Using this approach, we measured eCA activity in two marine diatoms (Thalassiosira pseudonana and Thalassiosira weissflogii), characterized the kinetics of this enzyme, and studied its regulation as a function of culture pH and CO 2 concentration. In support of a role for eCA in CO 2 supply, eCA activity specifically responded to low CO 2 rather than to changes in pH or HCO 3 2 , and the rates of eCA activity are nearly optimal for maintaining cell surface CO 2 concentrations near those in the bulk solution. Although the CO 2 gradients abolished by eCA are small (less than 0.5 mM concentration difference between bulk and cell surface), CO 2 uptake in these diatoms is a passive process driven by small concentration gradients. Analysis of the effects of short-term and long-term eCA inhibition on photosynthesis and growth indicates that eCA provides a small energetic benefit by reducing the surface-to-bulk CO 2 gradient. Alternative roles for eCA in CO 2 recovery as HCO 3 2 and surface pH regulation were investigated, but eCA was found to have minimal effects on these processes.To overcome the inefficiencies of Rubisco, many phytoplankton operate a CO 2 -concentrating mechanism (CCM) that increases Rubisco's rate of carbon fixation and reduces oxygen fixation by increasing the concentration of CO 2 around the enzyme. CCMs typically consist of inorganic carbon (C i ) pumps, carbonic anhydrases (CAs) to equilibrate HCO 3 2 and CO 2 , and a compartment to confine Rubisco, such as the pyrenoid or carboxysome, minimizing the volume in which CO 2 is elevated (Badger et al., 1998;Kaplan and Reinhold, 1999;Giordano et al., 2005). Intracellular carbonic anhydrases (iCAs) play multiple roles in CCMs, including the conversion of accumulated HCO 3 2 to CO 2 around Rubisco and the prevention of CO 2 leakage (Badger, 2003). Some organisms also have an extracellular carbonic anhydrase (eCA) associated with the cell wall, plasma membrane, or periplasmic space. The role of eCA has been enigmatic, although it is clearly related to the CCM. In Chlamydomonas reinhardtii, where eCA has been most thoroughly studied, the major eCA (Cah1) is up-regulated at low CO 2 , and its regulatory network includes a transcription factor that induces the expression of other CCM genes as well (Yoshioka et al., 2004;Ohnishi et al., 2010). In other organisms, eCA activity generally increases, in some cases dramatically, at low CO 2 , supporting its association with the CCM, but the...

No abstract

Abstract. There is ample evidence that tube-dwelling invertebrates such as chironomids significantly alter multiple important ecosystem functions, particularly in shallow lakes. Chironomids pump large water volumes, and associated suspended and dissolved substances, through the sediment and thereby compete with pelagic filter feeders for particulate organic matter. This can exert a high grazing pressure on phytoplankton, microorganisms, and perhaps small zooplankton and thus strengthen benthic-pelagic coupling. Furthermore, intermittent pumping by tube-dwelling invertebrates oxygenates sediments and creates a dynamic, three-dimensional mosaic of redox conditions. This shapes microbial community composition and spatial distribution, and alters microbe-mediated biogeochemical functions, which often depend on redox potential. As a result, extended hotspots of element cycling occur at the oxic-anoxic interfaces, controlling the fate of organic matter and nutrients as well as fluxes of nutrients between sediments and water. Surprisingly, the mechanisms and magnitude of interactions mediated by these organisms are still poorly understood. To provide a synthesis of the importance of tube-dwelling invertebrates, we review existing research and integrate previously disregarded functional traits into an ecosystem model. Based on existing research and our models, we conclude that tube-dwelling invertebrates play a central role in controlling water column nutrient pools, and hence water quality and trophic state. Furthermore, these tiny ecosystem engineers can influence the thresholds that determine shifts between alternate clear and turbid states of shallow lakes. The large effects stand in contrast to the conventional limnological paradigm emphasizing predominantly pelagic food webs. Given the vast number of shallow lakes worldwide, benthic invertebrates are likely to be relevant drivers of biogeochemical processes at regional and global scales, thereby mediating feedback mechanisms linked to climate change.