9 research outputs found

    A Conceptual Framework for Understanding the Biogeochemistry of Dry Riverbeds Through the Lens of Soil Science

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    Intermittent rivers and ephemeral streams (IRES) encompass fluvial ecosystems that eventually stop flowing and run dry at some point in space and time. During the dry phase, channels of IRES consist mainly of dry riverbeds (DRBs), prevalent yet widely unexplored ecotones between dry and wet phases that can strongly influence the biogeochemistry of fluvial networks. DRBs are often overlooked because they do not strictly belong to either domain of soil or freshwater science. Due to this dual character of DRBs, we suggest that concepts and knowledge from soil science can be used to expand the understanding of IRES biogeochemistry. Based on this idea, we propose that DRBs can be conceptually understood as early stage soils exhibiting many similarities with soils through two main forces: i) time since last sediment transport event, and ii) the development status of stabilizing structures (e.g. soil crusts and/or vascular plants). Our analysis suggests that while DRBs and soils may differ in master physical attributes (e.g. soil horizons vs fluvial sedimentary facies), they become rapidly comparable in terms of microbial communities and biogeochemical processes. We further propose that drivers of DRBs biogeochemistry are similar to those of soils and, hence, concepts and methods used in soil science are transferable to DRBs research. Finally, our paper presents future research directions to advance the knowledge of DRBs and to understand their role in the biogeochemistry of intermittent fluvial networks

    At the edge of aquatic systems: intermittent streambed microbial communities’ responses to hydrological alterations

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    Hydrological drought is a process of natural desiccation mainly due to large shortage of rainfall events. Reduced precipitations and prolonged droughts are spreading worldwide and threaten the integrity of aquatic ecosystems. Most Mediterranean streams have an intermittent flow which may become more variable and with larger duration of their no-flow periods under climate change. The enlargement of the dry period can importantly influence the ecosystem functioning, altering the microbiota inhabiting the streambed sediment as well as the processes they carry out (e.g. nutrients cycling). Consequently, hydrological alterations can reduce, limit or change microbial community functions, structure and composition, and therefore compromise the overall aquatic ecosystem functioning. The main objectives of this thesis are to study the responses of bacteria archaea and fungi inhabiting sediment to prolonged dry phase events and to wet episodes, spacing from punctual rains to rewetting eventsLa sequía hidrológica es un proceso de desecación natural debido principalmente a la gran escasez de eventos de lluvia. Las precipitaciones reducidas y las sequías prolongadas se están extendiendo por todo el mundo y amenazan la integridad de los ecosistemas acuáticos. La mayoría de las corrientes mediterráneas tienen un flujo intermitente que puede volverse más variable y con una mayor duración de sus períodos sin flujo bajo el cambio climático. La ampliación del período seco puede influir de manera importante en el funcionamiento del ecosistema, alterando la microbiota que habita en el sedimento fluvial, así como los procesos que llevan a cabo (por ejemplo, el ciclo de nutrientes). En consecuencia, las alteraciones hidrológicas pueden reducir, limitar o cambiar las funciones, la estructura y la composición de la comunidad microbiana y, por lo tanto, comprometer el funcionamiento general del ecosistema acuático. Los objetivos principales de esta tesis son estudiar las respuestas de bacterias, arqueas y hongos que habitan en sedimentos a eventos prolongados de fase seca y episodios húmedos, espaciando desde lluvias puntuales hasta eventos de rehumectaciónPrograma de Doctorat en Ciència i Tecnologia de l'Aigu

    Drying Shapes Aquatic Fungal Community Assembly by Reducing Functional Diversity

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    Aquatic fungi are highly diverse organisms that play a critical role in global biogeochemical cycles. Yet it remains unclear which assembly processes determine their co-occurrence and assembly patterns over gradients of drying intensity, which is a common stressor in fluvial networks. Although aquatic fungi possess drying-specific adaptations, little is known about how functional similarity influences co-occurrence probability and which functional traits are sorted by drying. Using field data from 15 streams, we investigated how co-occurrence patterns and assembly processes responded to drying intensity. To do so, we determined fungal co-occurrence patterns, functional traits that best explain species co-occurrence likelihood, and community assembly mechanisms explaining changes in functional diversity over the drying gradient. Our results identified 24 species pairs with positive co-occurrence probabilities and 16 species pairs with negative associations. The co-occurrence probability was correlated with species differences in conidia shape and fungal endophytic capacity. Functional diversity reduction over the drying gradient is generally associated with non-random abiotic filtering. However, the assembly processes changed over the drying gradient, with random assembly prevailing at low drying intensity and abiotic filtering gaining more importance as drying intensifies. Collectively, our results can help anticipate the impacts of global change on fungal communities and ecosystem functioning.Thisworkwas funded byMCIN/AEI/10.13039/501100011033 through the project RIVSTRESS (PID2020-115708RB-C21). R.A.-R. held a post-doctoral grant “Margarita Salas” from the Spanish Ministry of Universities and the Next Generation EU-Recovery, Transformation and Resilience Plan. P.H. held a post-doctoral grant “Margarita Salas” from the Spanish Ministry of Universities and the Next Generation EU-Recovery, Transformation and Resilience Plan and a ‘Juan de la Cierva– Formación’ contract (Spanish Ministry of Science and Innovation, FJC2020-045923-I). C.G.-C. was supported by a Junior Leader Fellowship contract (LCF/BQ/PR22/11920005) funded by “la Caixa” Foundation (ID 100010434).Peer reviewe

    Towards an improved understanding of biogeochemical processes across surface-groundwater interactions in intermittent rivers and ephemeral streams

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    Este artículo contiene 17 páginas, 7 figuras, 1 tabla.Surface-groundwater interactions in intermittent rivers and ephemeral streams (IRES), waterways which do not flow year-round, are spatially and temporally dynamic because of alternations between flowing, non-flowing and dry hydrological states. Interactions between surface and groundwater often create mixing zones with distinct redox gradients, potentially driving high rates of carbon and nutrient cycling. Yet a complete understanding of how underlying biogeochemical processes across surface-groundwater flowpaths in IRES differ among various hydrological states remains elusive. Here, we present a conceptual framework relating spatial and temporal hydrological variability in surface water-groundwater interactions to biogeochemical processing hotspots in IRES. We combine a review of theIRES biogeochemistry literature with concepts of IRES hydrogeomorphology to: (i) outline common distinctions among hydrological states in IRES; (ii) use these distinctions, together with considerations of carbon, nitrogen, and phosphorus cycles within IRES, to predict the relative potential for biogeochemical processing across different reach-scale processing zones (flowing water, fragmented pools, hyporheic zones, groundwater, and emerged sediments); and (iii) explore the potential spatial and temporal variability of carbon and nutrient biogeochemical processing across entire IRES networks. Our approach estimates the greatest reach-scale potential for biogeochemical processing when IRES reaches are fragmented into isolated surface water pools, and highlights the potential of relatively understudied processing zones, such as emerged sediments. Furthermore, biogeochemical processing in fluvial networks dominated by IRES is likely more temporally than spatially variable. We conclude that biogeochemical research in IRES would benefit from focusing on interactions between different nutrient cycles, surface-groundwater interactions in non-flowing states, and consideration of fluvial network architecture. Our conceptual framework outlines opportunities to advance studies and expand understanding of biogeochemistry in IRES.This study is based upon work from COST Action CA15113 (SMIRES, Science and Management of Intermittent Rivers and Ephemeral Streams, www.smires.eu), supported by COST (European Cooperation in Science and Technology). A.S. was supported by the InterNet Project (Eawag Discretionary Funds, Ernst Gohner ¨ Foundation and Gelbert Foundation), S.A. was supported by the Israel Science Foundation (grant 682/17). G. W. was supported by Klima- and Energiefonds within the ACRP program (PURIFY - KR17AC0K13643). S.B. was supported by the Spanish Government through “Ramon ´ y Cajal” fellow (RYC-2017-22643). HP.G. was supported by the Leibniz Foundation via the IGB household. O.S. was supported by the German Research Foundation (DFG grant SU 405/10- 1). A.W. was additionally supported by Klima- and Energiefonds within the ACRP program (PURIFY - KR17AC0K13643). V.P. is partially funded by the Environmental Protection Agency (Ireland) (EPA). U.R. was supported by a grant from the German Research Foundation (RI 2093/2- 1). S.O. was partially supported by the German Research Foundation (DFG grant SU 405/10-1). O.T. was partially supported by the National Strategic Reference Framework (NSRF). D.vS. was supported by a “Serra Húnter” Fellow. M.I.A. was supported by the “Juan de Cierva” postdoctoral program funded by the Spanish Ministry of Science, Innovation and Universities (Ref: IJC2018-036969-I).Peer reviewe

    Impacts of diffuse urban stressors on stream benthic communities and ecosystem functioning: A review

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    Catchment urbanisation results in urban streams being exposed to a multitude of stressors. Notably, stressors originating from diffuse sources have received less attention than stressors originating from point sources. Here, advances related to diffuse urban stressors and their consequences for stream benthic communities are summarised by reviewing 92 articles. Based on the search criteria, the number of articles dealing with diffuse urban stressors in streams has been increasing, and most of them focused on North America, Europe, and China. Land use was the most common measure used to characterize diffuse stressor sources in urban streams (70.7 % of the articles characterised land use), and chemical stressors (inorganic nutrients, xenobiotics, metals, and water properties, including pH and conductivity) were more frequently reported than physical or biological stressors. A total of 53.3 % of the articles addressed the impact of urban stressors on macroinvertebrates, while 35.9 % focused on bacteria, 9.8 % on fungi, and 8.7 % on algae. Regarding ecosystem functions, almost half of the articles (43.5 %) addressed changes in community dynamics, 40.3 % addressed organic matter decomposition, and 33.9 % addressed nutrient cycling. When comparing urban and non-urban streams, the reviewed studies suggest that urbanisation negatively impacts the diversity of benthic organisms, leading to shifts in community composition. These changes imply functional degradation of streams. The results of the present review summarise the knowledge gained to date and identify its main gaps to help improve our understanding of urban streams.This study has received funding from the Iberian Association of Limnology (AIL) through the project URBIFUN (Urbanization effects on the relationship between microbial biodiversity and ecosystem functioning), awarded to Míriam Colls and Ferran Romero. Authors thank as well the Basque Government (Consolidated Research Group IT951-16) and the MERLIN project 101036337 – H2020-LC-GD-2020/H2020-LC-GD-2020-3.info:eu-repo/semantics/publishedVersio
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