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1. Nitrate addition stimulates microbial decomposition of organic matter in salt marsh sediments

   https://doi.org/10.1111/gcb.14726  

   Bulseco, Ashley N.; Giblin, Anne E.; Tucker, Jane; Murphy, Anna E.; Sanderman, Jonathan; Hiller‐Bittrolff, Kenly; Bowen, Jennifer L. (July 2019, Global Change Biology)

   Abstract Salt marshes sequester carbon at rates more than an order of magnitude greater than their terrestrial counterparts, helping to mitigate climate change. As nitrogen loading to coastal waters continues, primarily in the form of nitrate, it is unclear what effect it will have on carbon storage capacity of these highly productive systems. This uncertainty is largely driven by the dual role nitrate can play in biological processes, where it can serve as a nutrient‐stimulating primary production or a thermodynamically favorable electron acceptor fueling heterotrophic metabolism. Here, we used a controlled flow‐through reactor experiment to test the role of nitrate as an electron acceptor, and its effect on organic matter decomposition and the associated microbial community in salt marsh sediments. Organic matter decomposition significantly increased in response to nitrate, even at sediment depths typically considered resistant to decomposition. The use of isotope tracers suggests that this pattern was largely driven by stimulated denitrification. Nitrate addition also significantly altered the microbial community and decreased alpha diversity, selecting for taxa belonging to groups known to reduce nitrate and oxidize more complex forms of organic matter. Fourier Transform‐Infrared Spectroscopy further supported these results, suggesting that nitrate facilitated decomposition of complex organic matter compounds into more bioavailable forms. Taken together, these results suggest the existence of organic matter pools that only become accessible with nitrate and would otherwise remain stabilized in the sediment. The existence of such pools could have important implications for carbon storage, since greater decomposition rates as N loading increases may result in less overall burial of organic‐rich sediment. Given the extent of nitrogen loading along our coastlines, it is imperative that we better understand the resilience of salt marsh systems to nutrient enrichment, especially if we hope to rely on salt marshes, and other blue carbon systems, for long‐term carbon storage. 

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2. Metagenomics coupled with biogeochemical rates measurements provide evidence that nitrate addition stimulates respiration in salt marsh sediments

   https://doi.org/10.1002/lno.11326  

   Bulseco, Ashley N.; Vineis, Joseph H.; Murphy, Anna E.; Spivak, Amanda C.; Giblin, Anne E.; Tucker, Jane; Bowen, Jennifer L. (October 2019, Limnology and Oceanography)

   Abstract High‐throughput sequencing has enabled robust shotgun metagenomic sequencing that informs our understanding of the genetic basis of important biogeochemical processes. Slower to develop, however, are the application of these tools in a controlled experimental framework that pushes the field beyond exploratory analysis toward hypothesis‐driven research. We performed flow‐through reactor experiments to examine how salt marsh sediments from varying depths respond to nitrate addition and linked biogeochemical processes to this underlying genetic foundation. Understanding the mechanistic basis of carbon and nitrogen cycling in salt marsh sediments is critical for predicting how important ecosystem services provided by marshes, including carbon storage and nutrient removal, will respond to global change. Prior to the addition of nitrate, we used metagenomics to examine the functional potential of the sediment microbial community that occurred along a depth gradient, where organic matter reactivity changes due to decomposition. Metagenomic data indicated that genes encoding enzymes involved in respiration, including denitrification, were higher in shallow sediments, and genes indicative of resource limitation were greatest at depth. After 92 d of nitrate enrichment, we measured cumulative increases in dissolved inorganic carbon production, denitrification, and dissimilatory nitrate reduction to ammonium; these rates correlated strongly with genes that encode essential enzymes in these important pathways. Our results highlight the importance of controlled experiments in linking biogeochemical rates to underlying genetic pathways. Furthermore, they indicate the importance of nitrate as an electron acceptor in fueling microbial respiration, which has consequences for carbon and nitrogen cycling and fate in coastal marine systems. 

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3. Interactions and Community Structure of Fungi and Prokaryotes in Salt and Brackish Marsh Ecosystems

   https://doi.org/10.1002/edn3.70199  

   Thompson, Madeleine_A; Peng, Xuefeng (October 2025, Environmental DNA)

   ABSTRACT Microbial communities play a fundamental role in biogeochemical cycling within salt and brackish marsh ecosystems, yet fungal‐prokaryotic interactions in these environments remain poorly understood. This study employed metabarcoding of the 16S and 28S rRNA genes to investigate prokaryotic and fungal communities across four locations in sediments and surface waters of the North Inlet salt marsh and Winyah Bay brackish marsh (South Carolina, USA) over four time points from 2020 to 2021. Co‐occurrence network analyses were used to identify potential microbial interactions and their ecological implications. Distinct fungal and prokaryotic communities were observed between the two marsh types. From the 16S prokaryotic primer set, Proteobacteria, Bacteroidota, and Cyanobacteriota dominated both marshes. Early diverging fungi and Actinomycetota (bacteria) were prevalent in the brackish marsh, whereas salt marsh communities were primarily composed of Dikarya fungi (Ascomycota and Basidiomycota) and Desulfobacteria. Network analyses revealed contrasting interactions between surface water and sediment. In brackish marsh sediments, fungi and prokaryotes exhibited nearly exclusively negative connections, suggesting strong resource competition. In contrast, Dikarya fungi in brackish marsh surface water displayed numerous positive connections with bacteria, suggesting potential cross‐feeding interactions. In the salt marsh, fungi and prokaryotes exhibited potential cooperative and competitive/antagonistic interactions. Ascomycota were positively connected with Desulfobacteria, suggesting a role in complex organic matter degradation. Conversely, negative connections between Chytridiomycota (early diverging fungi) and Cyanobacteriota (bacteria) implied parasitic interactions. These findings highlight the dynamic nature of fungal‐prokaryotic interactions in coastal ecosystems. By analyzing potential microbial relationships in salt and brackish marshes, this study provides new insights into the ecological roles of fungi in estuarine environments, particularly their contributions to nutrient cycling and organic matter decomposition. Understanding these interactions is crucial for generating hypotheses and predicting microbial responses to environmental changes—such as shifts in salinity and nutrient availability—and their potential impacts on marsh ecosystem functioning. 

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4. Peat Decomposition and Erosion Contribute to Pond Deepening in a Temperate Salt Marsh

   https://doi.org/10.1029/2022JG007063  

   Luk, Sheron; Eagle, Meagan J.; Mariotti, Giulio; Gosselin, Kelsey; Sanderman, Jonathan; Spivak, Amanda C. (February 2023, Journal of Geophysical Research: Biogeosciences)

   Abstract Salt marsh ponds expand and deepen over time, potentially reducing ecosystem carbon storage and resilience. The water filled volumes of ponds represent missing carbon due to prevented soil accumulation and removal by erosion and decomposition. Removal mechanisms have different implications as eroded carbon can be redistributed while decomposition results in loss. We constrained ponding effects on carbon dynamics in a New England marsh and determined whether expansion and deepening impact nearby soils by conducting geochemical characterizations of cores from three ponds and surrounding high marshes and models of wind‐driven erosion. Radioisotope profiles demonstrate that ponds are not depositional environments and that contemporaneous marsh accretion represents prevented accumulation accounting for 32%–42% of the missing carbon. Erosion accounted for 0%–38% and was bracketed using radioisotope inventories and wind‐driven resuspension models. Decomposition, calculated by difference, removes 22%–68%, and when normalized over pond lifespans, produces rates that agree with previous metabolism measurements. Pond surface soils contain new contributions from submerged primary producers and evidence of microbial alteration of underlying peat, as higher levels of detrital biomarkers and thermal stability indices, compared to the marsh. Below pond surface horizons, soil properties and organic matter composition were similar to the marsh, indicating that ponding effects are shallow. Soil bulk density, elemental content, and accretion rates were similar between marsh sites but different from ponds, suggesting that lateral effects are spatially confined. Consequently, ponds negatively impact ecosystem carbon storage but at current densities are not causing pervasive degradation of marshes in this system. 

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5. Lake Sediment Methane Responses to Organic Matter are Related to Microbial Community Composition in Experimental Microcosms

   https://doi.org/10.3389/fenvs.2022.834829  

   Bertolet, Brittni L.; Koepfli, Cristian; Jones, Stuart E. (March 2022, Frontiers in Environmental Science)

   Lake sediment microbial communities mediate carbon diagenesis. However, microbial community composition is variable across lakes, and it is still uncertain how variation in community composition influences sediment responses to environmental change. Sediment methane (CH 4 ) production has been shown to be substantially elevated by increased lake primary productivity and organic matter supply. However, the magnitude of the response of CH 4 production varies across lakes, and recent studies suggest a role for the microbial community in mediating this response. Here, we conducted sediment incubation experiments across 22 lakes to determine whether variation in sediment microbial community composition is related to the response of sediment CH 4 production to increases in organic matter. We sampled the 22 lakes across a gradient of pH in order to investigate lakes with variable sediment microbial communities. We manipulated the incubations with additions of dried algal biomass and show that variation in the response of CH 4 production to changes in organic matter supply is significantly correlated with metrics of sediment microbial community composition. Specifically, the diversity and richness of the non-methanogen community was most predictive of sediment CH 4 responses to organic matter additions. Additionally, neither metrics of microbial abundance nor preexisting organic matter availability explained meaningful variation in the response. Thus, our results provide experimental support that differences in sediment microbial communities influences CH 4 production responses to changes in organic matter availability. 

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