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1. Perennial grass bioenergy cropping systems: Impacts on soil fauna and implications for soil carbon accrual

   https://doi.org/10.1111/gcbb.12903  

   Zahorec, Allison; Reid, Matthew L.; Tiemann, Lisa K.; Landis, Douglas A. (October 2021, GCB Bioenergy)

   ABSTRACT Perennial grass energy crop production is necessary for the successful and sustainable expansion of bioenergy in North America. Numerous environmental advantages are associated with perennial grass cropping systems, including their potential to promote soil carbon accrual. Despite growing research interest in the abiotic and biotic factors driving soil carbon cycling within perennial grass cropping systems, soil fauna remain a critical yet largely unexplored component of these ecosystems. By regulating microbial activity and organic matter decomposition dynamics, soil fauna influence soil carbon stability with potentially significant implications for soil carbon accrual. We begin by reviewing the diverse, predominantly indirect effects of soil fauna on soil carbon dynamics in the context of perennial grass cropping systems. Since the impacts of perennial grass energy crop production on soil fauna will mediate their potential contributions to soil carbon accrual, we then discuss how perennial grass energy crop traits, diversity, and management influence soil fauna community structure and activity. We assert that continued research into the interactions of soil fauna, microbes, and organic matter will be important for advancing our understanding of soil carbon dynamics in perennial grass cropping systems. Furthermore, explicit consideration of soil faunal effects on soil carbon can improve our ability to predict changes in soil carbon following perennial grass cropping system establishment. We conclude by addressing the major knowledge gaps that should be prioritized to better understand and model the complex connections between perennial grass bioenergy systems, soil fauna, and carbon accrual. 

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2. Modeling seasonal vegetation phenology from hydroclimatic drivers for contrasting plant functional groups within drylands of the Southwestern USA

   https://doi.org/10.1088/2752-664X/acb9a0  

   Warter, Maria Magdalena; Singer, Michael Bliss; Cuthbert, Mark O; Roberts, Dar; Caylor, Kelly K; Sabathier, Romy; Stella, John (March 2023, Environmental Research: Ecology)

   Abstract In dryland ecosystems, vegetation within different plant functional groups exhibits distinct seasonal phenologies that are affected by the prevailing hydroclimatic forcing. The seasonal variability of precipitation, atmospheric evaporative demand, and streamflow influences root-zone water availability to plants in water-limited environments. Increasing interannual variations in climate forcing of the local water balance and uncertainty regarding climate change projections have raised the potential for phenological shifts and changes to vegetation dynamics. This poses significant risks to plant functional types across large areas, especially in drylands and within riparian ecosystems. Due to the complex interactions between climate, water availability, and seasonal plant water use, the timing and amplitude of phenological responses to specific hydroclimate forcing cannot be determined a priori , thus limiting efforts to dynamically predict vegetation greenness under future climate change. Here, we analyze two decades (1994–2021) of remote sensing data (soil adjusted vegetation index (SAVI)) as well as contemporaneous hydroclimate data (precipitation, potential evapotranspiration, depth to groundwater, and air temperature), to identify and quantify the key hydroclimatic controls on the timing and amplitude of seasonal greenness. We focus on key phenological events across four different plant functional groups occupying distinct locations and rooting depths in dryland SE Arizona: semi-arid grasses and shrubs, xeric riparian terrace and hydric riparian floodplain trees. We find that key phenological events such as spring and summer greenness peaks in grass and shrubs are strongly driven by contributions from antecedent spring and monsoonal precipitation, respectively. Meanwhile seasonal canopy greenness in floodplain and terrace vegetation showed strong response to groundwater depth as well as antecedent available precipitation (aaP = P − PET) throughout reaches of perennial and intermediate streamflow permanence. The timings of spring green-up and autumn senescence were driven by seasonal changes in air temperature for all plant functional groups. Based on these findings, we develop and test a simple, empirical phenology model, that predicts the timing and amplitude of greenness based on hydroclimate forcing. We demonstrate the feasibility of the model by exploring simple, plausible climate change scenarios, which may inform our understanding of phenological shifts in dryland plant communities and may ultimately improve our predictive capability of investigating and predicting climate-phenology interactions in the future. 

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3. Shrub encroachment of coastal ecosystems depends on dune elevation

   https://doi.org/10.1007/s11258-024-01453-2  

   Woods, Natasha N; Zinnert, Julie C (August 2024, Plant Ecology)

   Woody plant encroachment is infuenced by interactions between the physical environment and vegetation, which create heterogenous microenvironments some of which favor shrub recruitment through mitigation of the abiotic environment. Encroachment of native shrub, Morella cerifera into grasslands on Hog Island, Virginia has been attributed to warmer winter temperature; however, recruitment of seedlings in grasslands may be impacted by multiple factors at the level of the microhabitat. Our study focuses on a critical gap in understanding factors specifcally infuencing M. cerifera seedling recruitment and survival. By experimentally planting M. cerifera seedlings at varying dune elevations and grass densities, we tested hypotheses that dune elevation infuences the microclimate, soil characteristics and vegetation cover and that grass cover/density is related to shrub establishment. We tested these hypotheses through gathering data from temperature data loggers, conducting soil water content and chloride analyses, and determining percent cover of grasses relative to dune elevation. Results indicate that dune elevation was positively related to moderated temperatures with reduced temperature extremes and vegetation cover/composition that led to favorable locations for M. cerifera establishment and growth. Where dune elevation is>2 m, we document an upper limit of grass cover on natural seedling establishment, suggesting a switch from facilitative to competitive efects with grass density. Overall, our work demonstrates interactions between dune elevation and medium grass density has a facilitative infuence on M. cerifera establishment and can be used for future predictions of shrub growth with rising sea-levels. 

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4. Microbial Communities in the Changing Vegetation of the Chihuahuan Desert

   Embury, Emily L (February 2024, ProQuest)

   The encroachment of woody shrubs into grasslands is a phenomenon that has been occurring in the Chihuahuan Desert since the 1800s. Research shows that extensive livestock grazing and increased drought levels have acted as the main drivers of the grassland-to-shrubland transition. Very few studies have considered the impacts of such vegetation changes on microbial communities. Microbes play important ecosystem roles in nutrient cycling and carbon sequestration but also have the potential to act as pathogens. As the role of microbes in ecosystems is so important, it is crucial to understand the potential impacts of shrub encroachment on microbes and vice versa. Additionally, dryland microbes in general are understudied and as drylands cover over 40% of Earth’s land, understanding these microbes is of great ecological importance. The goal of this study was to assess microbial communities in shrub encroached systems in the Chihuahuan Desert to improve understanding of the ecological impacts of encroachment and increase general knowledge of dryland microbes. To conduct this study, soil samples were collected from sites dominated by black grama grass (Bouteloua eriopoda), sites dominated by honey mesquite shrubs (Prosopis glandulosa), and transition sites with both black grama and mesquite. DNA from soil samples was sequenced for bacteria (16S) and fungi (ITS2). Soil sampling was conducted through five sampling periods across a 10-month range to assess any potential seasonal variation in the microbial communities. In addition to DNA sequencing, microbial biomass and other environmental variables were collected. Statistical analyses were conducted to assess potential differences in microbial communities between vegetation types and seasons. Analyses included assessments of alpha and beta diversity, co-occurrence networks, and differential abundance analyses. Results show that there are significant changes in the microbial communities across vegetation types and seasons. Unique fungal and bacterial communities were identified in association with the different vegetation types, demonstrating that differences in vegetation influence microbial communities. Additionally, findings show that microbial communities are strongly impacted by seasons, showing decreases in biomass and changes to community composition in warm summer months compared to cooler months. Additionally, results show higher proportions of fungal pathogens in grass sites compared to other sites. Overall, this study demonstrates that microbial communities are influenced by shrub encroachment. As dryland microbial communities are often understudied, these findings can provide valuable insight into the ecology of dryland microbes and shrub-encroached systems. 

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5. A sequence of multiyear wet and dry periods provides opportunities for grass recovery and state change reversals

   https://doi.org/10.1002/ecm.1590  

   Peters, Debra P. C.; Savoy, Heather M. (September 2023, Ecological Monographs)

   Abstract Multiyear periods (≥4 years) of extreme rainfall are increasing in frequency as climate continues to change, yet there is little understanding of how rainfall amount and heterogeneity in biophysical properties affect state changes in a sequence of wet and dry periods. Our objective was to examine the importance of rainfall periods, their legacies, and vegetation and soil properties to either the persistence of woody plants or a shift toward perennial grass dominance and a state reversal. We examined a 28‐year record of rainfall consisting of a sequence of multiyear periods (average, dry, wet, dry, average) for four ecosystem types in the Jornada Basin. We analyzed relationships between above ground net primary production (ANPP) and rainfall for three plant functional groups that characterize alternative states (perennial grasses, other herbaceous plants, dominant shrubs). A multimodel comparison was used to determine the relative importance of rainfall, soil, and vegetation properties. For perennial grasses, the greatest mean ANPP in mesquite‐ and tarbush‐dominated shrublands occurred in the wet period and in the dry period following the wet period in grasslands. Legacy effects in grasslands were asymmetric, where the lowest production was found in a dry period following an average period, and the greatest production occurred in a dry period following a wet period. For other herbaceous plants, in contrast, the greatest ANPP occurred in the wet period. Mesquite was the only dominant shrub species with a significant positive response in the wet period. Rainfall amount was a poor predictor of ANPP for each functional group when data from all periods were combined. Initial herbaceous biomass at the plant scale, patch‐scale biomass, and soil texture at the landscape scale improved the predictive relationships of ANPP compared with rainfall alone. Under future climate, perennial grass production is expected to benefit the most from wet periods compared with other functional groups with continued high grass production in subsequent dry periods that can shift (desertified) shrublands toward grasslands. The continued dominance by shrubs will depend on the effects that rainfall has on perennial grasses and the sequence of high‐ and low‐rainfall periods rather than the direct effects of rainfall on shrub production. 

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