Alexander S. Kolker

Impacts of diverted freshwater on dissolved organic matter and microbial communities in Barataria Bay, Louisiana, U.S.A.

Here we present results of an initial assessment of the impacts of a water diversion event on the concentrations and chemical composition of dissolved organic matter (DOM) and bacterioplankton community composition in Barataria Bay, Louisiana U.S.A, an important estuary within the Mississippi River Delta complex. Concentrations and spectral properties of DOM, as reflected by UV/visible absorbance and fluorescence, were strikingly similar at 26 sites sampled along transects near two western and two eastern areas of Barataria Bay in July and September 2010. In September 2010, dissolved organic carbon (DOC) was significantly higher (568.1-1043 μM C, x=755.6+/-117.7 μM C, n=14) than in July 2010 (249.1-577.1 μM C, x=383.7+/-98.31 μM C, n=14); conversely, Abs254 was consistently higher at every site in July (0.105-0.314) than in September (0.080-0.221), averaging 0.24±0.06 in July and 0.15±0.04 in September. Fluorescence data via the fluorescence index (FI450/500) revealed that only 30% (8 of 26) of the July samples had an FI450/500 above 1.36, compared to 96% (25 of 26) for the September samples. This indicates a more terrestrial origin for the July DOM. Bacterioplankton from eastern sites differed in composition from bacterioplankon in western sites in July. These differences appeared to result from reduced salinities caused by the freshwater diversion. Bacterioplankton communities in September differed from those in July, but no spatial structure was observed. Thus, the trends in bacterioplankton and DOM were likely due to changes in water masses (e.g., input of Mississippi River water in July and a return to estuarine waters in September). Discharge of water from the Davis Pond Freshwater Diversion (DPFD) through Barataria Bay may have partially mitigated some adverse effects of the oil spill, inasmuch as DOM is concerned.

Biotic and abiotic controls on sediment aggregation and consolidation: Implications for geochemical fluxes and coastal restoration

This study examined the influence of particle size and organic matter on aggregation and compaction of 3 hydraulically dredged sediments from coastal Louisiana (clay, silt loam, sandy loam) saturated under a range of salinity regimes (1 and 5 PSU, 5 and 10 PSU, and 15 and 25 PSU) for 4 time periods (1, 8, 16, and 26 weeks). Particle sizes were determined using a laser diffraction particle size analyzer, which allowed us to develop high-resolution results indicating changes in aggregate size across a spectrum of experimental conditions. The sediments with greater organic matter content exhibited approximately 60% aggregation, as indicated by fewer aggregates in the clay size fraction, and subsequently more aggregates in the sand size fraction, when organic matter remained in the sediment. Additionally, the sandy sediment compacted more than the organic sediments in the first 16 weeks. These findings suggest that sediments with greater clay and organic matter content behave as larger particles and may undergo particle rearrangement and compaction over longer time scales than sandy sediments with low organic matter. For coastal wetland restoration, models should include the effect of organic matter on particle aggregation to understand sediment dynamics over geologic time.

Brackish Marsh Plant Community Responses to Regional Precipitation and Relative sea-Level Rise

Climate-driven shifts in environmental conditions can transform the structure and function of coastal ecosystems. Here we examine how two back-barrier brackish marshes in Pamlico Sound (North Carolina, USA) responded to changes in precipitation, temperature, and relative sea level and whether local rates of accretion have kept pace with relative sea-level rise. We used the distribution of seeds in sediment cores, coupled with 210Pb-sediment geochronology, to determine patterns of community and ecosystem change over the past century. The chronologies demonstrate that both marshes recently transitioned from communities dominated by Cladium jamaicense, which prefers fresh and brackish settings, to communities dominated by Schoenoplectus americanus, which prefers brackish and saline environments. Multiple regression analysis indicates that community shifts are best explained by relative sea-level rise and regional trends in precipitation. Results also indicate that the marshes are developing an elevation deficit with respect to rising sea level, which likely influenced the conversion from C. jamaicense dominated to S. americanus dominated communities. These findings substantiate a growing body of evidence indicating that climate-driven shifts in environmental conditions are transforming coastal ecosystems and suggest that brackish intertidal marshes may become increasingly threatened by accelerated sea-level rise and associated environmental changes expected to unfold this century.

Vegetation and Shear Strength in a Delta-splay Mouth Bar

The mechanism by which new deltaic wetlands form is a complex suite of biological and physical processes that can modify one another. Understanding these processes and their interactions is imperative to successful coastal restoration. This study investigated the relationship between belowground plant biomass and sediment cohesion. We hypothesized that greater root densities increase shear strength, variably across plant communities, and that these communities are associated with distinct inundation regimes. A significant relationship was found between belowground biomass and surface shear strength when accounting for sediment grain size, water content, and organic matter content. Sites dominated by native graminoids or woody species had significantly higher shear strengths than unvegetated areas. However, sites dominated by Phragmites australis or forbs did not differ significantly in shear strength from the unvegetated sites. Sites dominated by Phragmites australis were also subject to significantly higher inundation rates during the previous water year than any other vegetation type. These results suggest that vegetation community differences lead to differences in shear strength that result in locally differential erosion rates, in turn modifying future geomorphology, hydrology, sedimentation, and vegetation distribution. This feedback implies that certain vegetation communities in wetland restoration projects could not only impart immediate erosion resistance to the substrate, but affect the long-term potential for land creation.

Clonal Vegetation Patterns Mediate Shoreline Erosion

Understanding processes governing coastal erosion is becoming increasingly urgent because highly valued ecosystems like salt marshes are being lost at accelerating rates. Here we examine the role of biotic interactions in mediating marsh shoreline erosion under wind wave forces. We parameterized analytical and cellular automata models with field data to assess how soil heterogeneity among clonal patches of an ecosystem engineer mediates spatiotemporal patterns of marsh shoreline erosion. We found that spatial heterogeneity accelerates erosion, especially when it is organized in patches of intermediate size. Patch size also mediated interannual variability in erosion and strongly controlled shoreline roughness. Our results indicate that shoreline roughness can be diagnostic of internal biological structure and spatiotemporal variability in erosion. Hence, measures of shoreline roughness may inform the timeframe and spatial extent needed to accurately monitor erosion. These findings highlight how the physical response of marsh shorelines to wind wave erosion is a function of landscape ecology.