Ice algal bloom development on the surface of the Greenland Ice Sheet

It is fundamental to understand the development of Zygnematophycean (Streptophyte) micro-algal blooms within Greenland Ice Sheet (GrIS) supraglacial environments, given their potential to significantly impact both physical (melt) and chemical (carbon and nutrient cycling) surface characteristics. Here, we report on a space-for-time assessment of a GrIS ice algal bloom, achieved by sampling an ∼85 km transect spanning the south-western GrIS bare ice zone during the 2016 ablation season. Cell abundances ranged from 0 to 1.6 × 104 cells ml-1, with algal biomass demonstrated to increase in surface ice with time since snow line retreat (R2 = 0.73, P < 0.05). A suite of light harvesting and photo-protective pigments were quantified across transects (chlorophylls, carotenoids and phenols) and shown to increase in concert with algal biomass. Ice algal communities drove net autotrophy of surface ice, with maximal rates of net production averaging 0.52 ± 0.04 mg C l-1 d-1, and a total accumulation of 1.306 Gg C (15.82 ± 8.14 kg C km-2) predicted for the 2016 ablation season across an 8.24 × 104 km2 region of the GrIS. By advancing our understanding of ice algal bloom development, this study marks an important step toward projecting bloom occurrence and impacts into the future.

Microspatial variability in community structure and photophysiology of calcified macroalgal microbiomes revealed by coupling of hyperspectral and high-resolution fluorescence imaging

Calcifying coralline macroalgae provide biogenic habitats colonised by epiphytic microalgae that contribute significantly to community productivity. Georeferenced hyperspectral and high-resolution fluorescence imaging were coupled to microspatially mapped community composition and relative biomass of macroalgal host and epiphyte microalgal groups, and their weighted contributions to productivity within host fronds of Corallina officinalis on upper and lower zones of a rocky shore were determined. Lower shore epiphytes were dominated by filamentous diatoms (Bacillariophyta), confined to the apex of the frond structure, which were low light acclimated but retained a high capacity for photoprotective down regulation and contributed up to 51% of total community productivity. Upper shore epiphytes were dominated by green algae (Chlorophyta) and single-celled diatoms (principally Cocconeis spp.), which were high light acclimated but present at far lower relative biomass and contributed negligibly to productivity. The host, C. officinalis was the main primary producer. Variation in light environment resulting from differences in shore height and shading within the host macroalga, likely play a large role in determining patterns in epiphyte community structure, biomass and productivity observed. Additionally, microspatial gradients in photophysiological parameters along the host macroalga likely resulted from age-dependent variation in pigments as well as the gradient in light environment.

Functional group diversity increases with modularity in complex food webs

Biodiversity increases the ability of ecosystems to provide multiple functions. Most studies report a positive relationship between species richness and the number of ecosystem functions. However, it is not known whether the number of functional groups is related to the structure of the underlying species interaction network. Here we present food web data from 115 salt marsh islands and show that network structure is associated with the number of functional groups present. Functional group diversity is heterogeneously distributed across spatial scales, with some islands hosting more functional groups than others. Functional groups form modules within the community so that food webs with more modular architectures have more functional group diversity. Further, in communities with different interaction types, modularity can be seen as the multifunctional equivalent of trophic complementarity. Collectively, these findings reveal spatial heterogeneity in the number of functional groups that emerges from patterns in the structure of the food web.

The influence of functional group diversity on food web structure is less well known than that of biodiversity. Analysing species interactions in a network of salt marsh islands, Montoya et al. show that functional group diversity is higher in more modular networks and varies spatially across the archipelago.

Measuring nanoscale forces with living probes

Optical trapping techniques have been used to investigate fundamental biological processes ranging from the identification of the processive mechanisms of kinesin and myosin to understanding the mechanics of DNA. To date, these investigations have relied almost exclusively on the use of isotropic probes based on colloidal microspheres. However, there are many potential advantages in utilizing more complex probe morphologies: use of multiple trapping points enables control of the interaction volume; increasing the distance between the optical trap and the sample minimizes photodamage in sensitive biological materials; and geometric anisotropy introduces the potential for asymmetric surface chemistry and multifunctional probes. Here we demonstrate that living cells of the freshwater diatom Nitzschia subacicularis Hustedt can be exploited as advanced probes for holographic optical tweezing applications. We characterize the optical and material properties associated with the high shape anisotropy of the silica frustule, examine the trapping behavior of the living algal cells, and demonstrate how the diatoms can be calibrated for use as force sensors and as force probes in the presence of rat B-cell hybridoma (11B11) cells.

Interrelationships between Rates of Microbial Production, Exopolymer Production, Microbial Biomass, and Sediment Stability in Biofilms of Intertidal Sediments

The upper few millimeters of intertidal sediment supports a varied biomass of microbial consortia and microphytobenthos. Many of these organisms release extracellular polymers into the surrounding sediment matrix that can result in sediment cohesion and the increased stability of the sediment. The relationship between the heterotrophic and autotrophic components of these biofilms is not well understood. A combination of mesocosm and field investigations were used to investigate the relationship between microbial production rate (algae and bacteria), the extracellular carbohydrates, biomass, and stability in conjunction with a variety of environmental factors. An inverse relationship was found between rates of algal production and sediment stability both in the field and in laboratory mesocosms, though the relationship was significant only in the field (P < 0.001). Stability of sediments increased with increasing bacterial production rate (P < 0.001). Positive correlations were found between sediment stability and a range of other variables, including algal biomass (P < 0.001), colloidal-S EPS (P < 0.001), colloidal-S carbohydrate (P < 0.01), colloidal-S EDTA (P < 0.01), and sediment water content (P < 0.001). Using the data acquired, a preliminary model was developed to predict changes in sediment stability. Chlorophyll a, water content, and colloidal-S EPS were found to be the most important predictors of stability in intact cores incubated under laboratory conditions. Differences observed in patterns of the surface (0-2 mm) distribution of colloidal-S carbohydrate and chlorophyll a when expressed on a dry weight or areal basis were attributed to effects of dewatering and concomitant changes in wet bulk density. The polymeric carbohydrate (colloidal-S EPS) component of the biofilms was not found to be a constant fraction of the colloidal-S carbohydrate extract, varying from 16 to 58%, and the percentage of polymer decreased logarithmically as chlorophyll a concentrations increased and the biofilms matured (P < 0.001). Changes in the relationships between these variables over the period of biofilm development and maturation highlight the difficulties in their use to predict sediment stability. Exopolymer concentrations were more closely correlated with algal biomass than with bacterial numbers. Rates of algal carbon fixation were considerably greater than those for bacteria, suggesting that the algae have a much greater potential for exopolymer production. It is suggested that the microphytobenthos secretions make a more important contribution to sediment stability.