98 results on '"Obrador, B."'
Search Results
2. Microbial carbon processing along a river discontinuum
- Author
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Proia, L., von Schiller, D., Gutierrez, C., Casas-Ruiz, J. P., Gómez-Gener, L., Marcé, R., Obrador, B., Acuña, V., and Sabater, S.
- Published
- 2016
3. Global CO2 emissions from dry inland waters share common drivers across ecosystems
- Author
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Keller, P. S., Catalán, N., von Schiller, D., Grossart, H.-P., Koschorreck, M., Obrador, B., Frassl, M. A., Karakaya, N., Barros, N., Howitt, J. A., Mendoza-Lera, C., Pastor, A., Flaim, G., Aben, R., Riis, T., Arce, M. I., Onandia, G., Paranaíba, J. R., Linkhorst, A., del Campo, R., Amado, A. M., Cauvy-Fraunié, S., Brothers, S., Condon, J., Mendonça, R. F., Reverey, F., Rõõm, E.-I., Datry, T., Roland, F., Laas, A., Obertegger, U., Park, J.-H., Wang, H., Kosten, S., Gómez, R., Feijoó, C., Elosegi, A., Sánchez-Montoya, M. M., Finlayson, C. M., Melita, M., Oliveira Junior, E. S., Muniz, C. C., Gómez-Gener, L., Leigh, C., Zhang, Q., and Marcé, R.
- Published
- 2020
- Full Text
- View/download PDF
4. The drawdown phase of dam decommissioning is a hot moment of gaseous carbon emissions from a temperate reservoir
- Author
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Biología vegetal y ecología, Landaren biologia eta ekologia, Amani, Mabano, Von Schiller Calle, Daniel Gaspar, Suárez, Isabel, Atristain, Miren, Elosegi Irurtia, Arturo, Marcé, Rafael, García-Baquero Moneo, Gonzalo, Obrador, B., Biología vegetal y ecología, Landaren biologia eta ekologia, Amani, Mabano, Von Schiller Calle, Daniel Gaspar, Suárez, Isabel, Atristain, Miren, Elosegi Irurtia, Arturo, Marcé, Rafael, García-Baquero Moneo, Gonzalo, and Obrador, B.
- Abstract
Dam decommissioning (DD) is a viable management option for thousands of ageing dams. Reservoirs are large carbon sinks, and reservoir drawdown results in important carbon dioxide (CO2) and methane (CH4) emissions. We studied the effects of DD on CO2 and CH4 fluxes from impounded water, exposed sediment, and lotic water before, during, and 3-10 months after drawdown of the Enobieta Reservoir, north Iberian Peninsula. During the study period, impounded water covered 0-100%, exposed sediment 0-96%, and lotic water 0-4% of the total reservoir area (0.14 km(2)). Areal CO2 fluxes in exposed sediment (mean [SE]: 295.65 [74.90] mmol m(-2) d(-1)) and lotic water (188.11 [86.09] mmol m(-2) d(-1)) decreased over time but remained higher than in impounded water (-36.65 [83.40] mmol m(-2) d(-1)). Areal CH4 fluxes did not change over time and were noteworthy only in impounded water (1.82 [1.11] mmol m(-2) d(-1)). Total ecosystem carbon (CO2 + CH4) fluxes (kg CO2-eq d(-1)) were higher during and after than before reservoir drawdown because of higher CO2 fluxes from exposed sediment. The reservoir was a net sink of carbon before reservoir drawdown and became an important emitter of carbon during the first 10 months after reservoir drawdown. Future studies should examine mid- and long-term effects of DD on carbon fluxes, identify the drivers of areal CO2 fluxes from exposed sediment, and incorporate DD in the carbon footprint of reservoirs.
- Published
- 2022
5. Chronological reconstruction of metal contamination in the Port of Maó (Minorca, Spain)
- Author
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Garcia-Orellana, J., Cañas, L., Masqué, P., Obrador, B., Olid, C., and Pretus, J.
- Published
- 2011
- Full Text
- View/download PDF
6. Spatio-temporal variability of carbon dioxide and methane emissions from a Mediterranean reservoir
- Author
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Montes-Pérez, J. J., primary, Obrador, B., additional, Conejo-Orosa, T., additional, Rodríguez, V., additional, Marcé, R., additional, Escot, C., additional, Reyes, I., additional, Rodríguez, J. J., additional, and Moreno-Ostos, E., additional
- Published
- 2022
- Full Text
- View/download PDF
7. Carbon dioxide emission from drawdown areas of a Mediterranean reservoir
- Author
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Pozzo-Pirotta, L. J., primary, Montes-Pérez, J. J., additional, Sammartino, S., additional, Marcé, R., additional, Obrador, B., additional, Escot, C., additional, Reyes, I., additional, and Moreno-Ostos, E., additional
- Published
- 2022
- Full Text
- View/download PDF
8. Global carbon budget of reservoirs is overturned by the quantification of drawdown areas
- Author
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Keller, Philipp, Marcé, R., Obrador, B., Koschorreck, Matthias, Keller, Philipp, Marcé, R., Obrador, B., and Koschorreck, Matthias
- Abstract
Reservoir drawdown areas—where sediment is exposed to the atmosphere due to water-level fluctuations—are hotspots for carbon dioxide (CO2) emissions. However, the global extent of drawdown areas is unknown, precluding an accurate assessment of the carbon budget of reservoirs. Here we show, on the basis of satellite observations of 6,794 reservoirs between 1985 and 2015, that 15% of the global reservoir area was dry. Exposure of drawdown areas was most pronounced in reservoirs close to the tropics and shows a complex dependence on climatic (precipitation, temperature) and anthropogenic (water use) drivers. We re-assessed the global carbon emissions from reservoirs by apportioning CO2 and methane emissions to water surfaces and drawdown areas using published areal emission rates. The new estimate assigns 26.2 (15–40) (95% confidence interval) TgCO2-C yr−1 to drawdown areas, and increases current global CO2 emissions from reservoirs by 53% (60.3 (43.2–79.5) TgCO2-C yr−1). Taking into account drawdown areas, the ratio between carbon emissions and carbon burial in sediments is 2.02 (1.04–4.26). This suggests that reservoirs emit more carbon than they bury, challenging the current understanding that reservoirs are net carbon sinks. Thus, consideration of drawdown areas overturns our conception of the role of reservoirs in the carbon cycle.
- Published
- 2021
9. Cross-continental importance of CH4 emissions from dry inland-waters
- Author
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Paranaíba, J.R., Aben, R., Barros, N., Quadra, G., Linkhorst, A., Amado, A.M., Brothers, S., Catalán, N., Condon, J., Finlayson, C.M., Grossart, H.-P., Howitt, J., Oliveira Junior, E.S., Keller, Philipp, Koschorreck, Matthias, Laas, A., Leigh, C., Marcé, R., Mendonça, R., Muniz, C.C., Obrador, B., Onandia, G., Raymundo, D., Reverey, F., Roland, F., Rõõm, E.-I., Sobek, S., von Schiller, D., Wang, H., Kosten, S., Paranaíba, J.R., Aben, R., Barros, N., Quadra, G., Linkhorst, A., Amado, A.M., Brothers, S., Catalán, N., Condon, J., Finlayson, C.M., Grossart, H.-P., Howitt, J., Oliveira Junior, E.S., Keller, Philipp, Koschorreck, Matthias, Laas, A., Leigh, C., Marcé, R., Mendonça, R., Muniz, C.C., Obrador, B., Onandia, G., Raymundo, D., Reverey, F., Roland, F., Rõõm, E.-I., Sobek, S., von Schiller, D., Wang, H., and Kosten, S.
- Abstract
Despite substantial advances in quantifying greenhouse gas (GHG) emissions from dry inland waters, existing estimates mainly consist of carbon dioxide (CO2) emissions. However, methane (CH4) may also be relevant due to its higher Global Warming Potential (GWP). We report CH4 emissions from dry inland water sediments to i) provide a cross-continental estimate of such emissions for different types of aquatic systems (i.e., lakes, ponds, reservoirs, and streams) and climate zones (i.e., tropical, continental, and temperate); and ii) determine the environmental factors that control these emissions. CH4 emissions from dry inland waters were consistently higher than emissions observed in adjacent uphill soils, across climate zones and in all aquatic systems except for streams. However, the CH4 contribution (normalized to CO2 equivalents; CO2-eq) to the total GHG emissions of dry inland waters was similar for all types of aquatic systems and varied from 10 to 21%. Although we discuss multiple controlling factors, dry inland water CH4 emissions were most strongly related to sediment organic matter content and moisture. Summing CO2 and CH4 emissions revealed a cross-continental average emission of 9.6 ± 17.4 g CO2-eq m−2 d−1 from dry inland waters. We argue that increasing droughts likely expand the worldwide surface area of atmosphere-exposed aquatic sediments, thereby increasing global dry inland water CH4 emissions. Hence, CH4 cannot be ignored if we want to fully understand the carbon (C) cycle of dry sediments.
- Published
- 2021
10. Global CO2 emissions from dry inland waters share common drivers across ecosystems
- Author
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Keller, P.S., Catalan, N., Schiller, D., Grossart, H.P., Koschorreck, M., Obrador, B., Frassl, M.A., Karakaya, N., Barros, N., Howitt, J.A., Mendoza-Lera, C., Pastor, A., Flaim, G., Aben, R.C.H., Riis, T., Arce, M.I., Onandia, G., Paranaiba, J.R., Linkhorst, A., Campo, R., Amado, A.M., Cauvy-Fraunie, S., Brothers, S., Condon, J., Mendonca, R.F., Reverey, F., Room, E.I., Datry, T., Roland, F., Laas, A., Obertegger, U., Park, J.H., Wang, H, Kosten, S., Gomez, R., Feijoo, C., Elosegi, A., Sanchez-Montoya, M.M., Finlayson, C.M., Melita, M., Oliveira Junior, E.S., Muniz, C.C., Gomez-Gener, L., Leigh, C., Marce, R., Keller, P.S., Catalan, N., Schiller, D., Grossart, H.P., Koschorreck, M., Obrador, B., Frassl, M.A., Karakaya, N., Barros, N., Howitt, J.A., Mendoza-Lera, C., Pastor, A., Flaim, G., Aben, R.C.H., Riis, T., Arce, M.I., Onandia, G., Paranaiba, J.R., Linkhorst, A., Campo, R., Amado, A.M., Cauvy-Fraunie, S., Brothers, S., Condon, J., Mendonca, R.F., Reverey, F., Room, E.I., Datry, T., Roland, F., Laas, A., Obertegger, U., Park, J.H., Wang, H, Kosten, S., Gomez, R., Feijoo, C., Elosegi, A., Sanchez-Montoya, M.M., Finlayson, C.M., Melita, M., Oliveira Junior, E.S., Muniz, C.C., Gomez-Gener, L., Leigh, C., and Marce, R.
- Abstract
Contains fulltext : 226569.pdf (publisher's version ) (Open Access)
- Published
- 2020
11. Global CO2 emissions from dry inland waters share common drivers across ecosystems
- Author
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Biología vegetal y ecología, Landaren biologia eta ekologia, Keller, P.S., Catalán, N., Von Schiller Calle, Daniel Gaspar, Grossart, Hans Peter, Koschorreck, M., Obrador, B., Frassl, M. A., Karakaya, N., Barros, N., Howitt, J. A., Mendoza Lera, B., Pastor, Ada, Flaim, G., Aben, R., Riis, T., Arce, M. I., Onandia, G., Paranaíba, J. R., Linkhorst, A., Del Campo, Rubén, Amado, A. M., Cauvy Fraunié, S., Brothers, S., Condon, J., Mendonça, R. F., Reverey, F., Rõõm, E. I., Datry, T., Roland, F., Laas, A., Obertegger, U., Park, J. H., Wang, H., Kosten, S., Gómez, R., Feijoó, Claudia, Elosegi Irurtia, Arturo, Sánchez Montoya, María Mar, Finlayson, C. M., Melita, M., Oliveira Junior, E. S., Muniz, C. C.., Gómez Gener, L., Leigh, C., Zhang, Q., Marcé, R., Biología vegetal y ecología, Landaren biologia eta ekologia, Keller, P.S., Catalán, N., Von Schiller Calle, Daniel Gaspar, Grossart, Hans Peter, Koschorreck, M., Obrador, B., Frassl, M. A., Karakaya, N., Barros, N., Howitt, J. A., Mendoza Lera, B., Pastor, Ada, Flaim, G., Aben, R., Riis, T., Arce, M. I., Onandia, G., Paranaíba, J. R., Linkhorst, A., Del Campo, Rubén, Amado, A. M., Cauvy Fraunié, S., Brothers, S., Condon, J., Mendonça, R. F., Reverey, F., Rõõm, E. I., Datry, T., Roland, F., Laas, A., Obertegger, U., Park, J. H., Wang, H., Kosten, S., Gómez, R., Feijoó, Claudia, Elosegi Irurtia, Arturo, Sánchez Montoya, María Mar, Finlayson, C. M., Melita, M., Oliveira Junior, E. S., Muniz, C. C.., Gómez Gener, L., Leigh, C., Zhang, Q., and Marcé, R.
- Abstract
[EN] Many inland waters exhibit complete or partial desiccation, or have vanished due to global change, exposing sediments to the atmosphere. Yet, data on carbon dioxide (CO2) emissions from these sediments are too scarce to upscale emissions for global estimates or to understand their fundamental drivers. Here, we present the results of a global survey covering 196 dry inland waters across diverse ecosystem types and climate zones. We show that their CO2 emissions share fundamental drivers and constitute a substantial fraction of the carbon cycled by inland waters. CO2 emissions were consistent across ecosystem types and climate zones, with local characteristics explaining much of the variability. Accounting for such emissions increases global estimates of carbon emissions from inland waters by 6% (~0.12 Pg C y−1). Our results indicate that emissions from dry inland waters represent a significant and likely increasing component of the inland waters carbon cycle.
- Published
- 2020
12. Global CO2 emissions from dry inland waters share common drivers across ecosystems
- Author
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Keller, P. S. Catalán, N. von Schiller, D. Grossart, H. P. Koschorreck, M. Obrador, B. Frassl, M. A. Karakaya, N. Barros, N. Howitt, J. A. Mendoza-Lera, C. Pastor, A. Flaim, G. Aben, R. Riis, T. Arce, M. I. Onandia, G. Paranaíba, J. R. Linkhorst, A. del Campo, R. Amado, A. M. Cauvy-Fraunié, S. Brothers, S. Condon, J. Mendonça, R. F. Reverey, F. Rõõm, E. I. Datry, T. Roland, F. Laas, A. Obertegger, U. Park, J. H. Wang, H. Kosten, S. Gómez, R. Feijoó, C. Elosegi, A. Sánchez-Montoya, M. M. Finlayson, C. M. Melita, M. Oliveira Junior, E. S. Muniz, C. C. Gómez-Gener, L. Leigh, C. Zhang, Q. Marcé, R. and Keller, P. S. Catalán, N. von Schiller, D. Grossart, H. P. Koschorreck, M. Obrador, B. Frassl, M. A. Karakaya, N. Barros, N. Howitt, J. A. Mendoza-Lera, C. Pastor, A. Flaim, G. Aben, R. Riis, T. Arce, M. I. Onandia, G. Paranaíba, J. R. Linkhorst, A. del Campo, R. Amado, A. M. Cauvy-Fraunié, S. Brothers, S. Condon, J. Mendonça, R. F. Reverey, F. Rõõm, E. I. Datry, T. Roland, F. Laas, A. Obertegger, U. Park, J. H. Wang, H. Kosten, S. Gómez, R. Feijoó, C. Elosegi, A. Sánchez-Montoya, M. M. Finlayson, C. M. Melita, M. Oliveira Junior, E. S. Muniz, C. C. Gómez-Gener, L. Leigh, C. Zhang, Q. Marcé, R.
- Abstract
Many inland waters exhibit complete or partial desiccation, or have vanished due to global change, exposing sediments to the atmosphere. Yet, data on carbon dioxide (CO2) emissions from these sediments are too scarce to upscale emissions for global estimates or to understand their fundamental drivers. Here, we present the results of a global survey covering 196 dry inland waters across diverse ecosystem types and climate zones. We show that their CO2 emissions share fundamental drivers and constitute a substantial fraction of the carbon cycled by inland waters. CO2 emissions were consistent across ecosystem types and climate zones, with local characteristics explaining much of the variability. Accounting for such emissions increases global estimates of carbon emissions from inland waters by 6% (~0.12 Pg C y−1). Our results indicate that emissions from dry inland waters represent a significant and likely increasing component of the inland waters carbon cycle.
- Published
- 2020
- Full Text
- View/download PDF
13. Global CO2 emissions from dry inland waters share common drivers across ecosystems
- Author
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Keller, Philipp, Catalán, N., von Schiller, D., Grossart, H.-P., Koschorreck, Matthias, Obrador, B., Frassl, Marieke, Karakaya, N., Barros, N., Howitt, J.A., Mendoza-Lera, C., Pastor, A., Flaim, G., Aben, R., Riis, T., Arce, M.I., Onandia, G., Paranaíba, J.R., Linkhorst, A., del Campo, R., Amado, A.M., Cauvy-Fraunié, S., Brothers, S., Condon, J., Mendonça, R.F., Reverey, F., Rõõm, E.-I., Datry, T., Roland, F., Laas, A., Obertegger, U., Park, J.-H., Wang, H., Kosten, S., Gómez, R., Feijoó, C., Elosegi, A., Sánchez-Montoya, M.M., Finlayson, C.M., Melita, M., Oliveira Junior, E.S., Muniz, C.C., Gómez-Gener, L., Leigh, C., Zhang, Q., Marcé, R., Keller, Philipp, Catalán, N., von Schiller, D., Grossart, H.-P., Koschorreck, Matthias, Obrador, B., Frassl, Marieke, Karakaya, N., Barros, N., Howitt, J.A., Mendoza-Lera, C., Pastor, A., Flaim, G., Aben, R., Riis, T., Arce, M.I., Onandia, G., Paranaíba, J.R., Linkhorst, A., del Campo, R., Amado, A.M., Cauvy-Fraunié, S., Brothers, S., Condon, J., Mendonça, R.F., Reverey, F., Rõõm, E.-I., Datry, T., Roland, F., Laas, A., Obertegger, U., Park, J.-H., Wang, H., Kosten, S., Gómez, R., Feijoó, C., Elosegi, A., Sánchez-Montoya, M.M., Finlayson, C.M., Melita, M., Oliveira Junior, E.S., Muniz, C.C., Gómez-Gener, L., Leigh, C., Zhang, Q., and Marcé, R.
- Abstract
Many inland waters exhibit complete or partial desiccation, or have vanished due to global change, exposing sediments to the atmosphere. Yet, data on carbon dioxide (CO2) emissions from these sediments are too scarce to upscale emissions for global estimates or to understand their fundamental drivers. Here, we present the results of a global survey covering 196 dry inland waters across diverse ecosystem types and climate zones. We show that their CO2 emissions share fundamental drivers and constitute a substantial fraction of the carbon cycled by inland waters. CO2 emissions were consistent across ecosystem types and climate zones, with local characteristics explaining much of the variability. Accounting for such emissions increases global estimates of carbon emissions from inland waters by 6% (~0.12 Pg C y−1). Our results indicate that emissions from dry inland waters represent a significant and likely increasing component of the inland waters carbon cycle.
- Published
- 2020
14. Sediment Respiration Pulses in Intermittent Rivers and Ephemeral Streams
- Author
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von Schiller, D, Datry, T, Corti, R, Foulquier, A, Tockner, K, Marcé, R, García‐Baquero, G, Odriozola, I, Obrador, B, Elosegi, A, Mendoza‐Lera, C, Gessner, M O, Stubbington, R, Albariño, R, Allen, D C, Altermatt, Florian, Arce, M I, Arnon, S, Banas, D, Banegas‐Medina, A, Beller, E, Blanchette, M L, Blanco‐Libreros, J F, Blessing, J, Boëchat, I G, Boersma, K S, Bogan, M T, Bonada, N, Bond, N R, Brintrup, K, et al, University of Zurich, and von Schiller, D
- Subjects
Environmental Chemistry river ,Atmospheric Science ,Global and Planetary Change ,stream ,2306 Global and Planetary Change ,temporary ,2300 General Environmental Science ,10127 Institute of Evolutionary Biology and Environmental Studies ,intermittent ,2304 Environmental Chemistry ,1902 Atmospheric Science ,570 Life sciences ,biology ,590 Animals (Zoology) ,respiration ,General Environmental Science - Published
- 2019
15. A conceptual framework for understanding the biogeochemistry of dry riverbeds through the lens of soil science
- Author
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Arce, M.I., Mendoza-Lera, C., Almagro, M., Catalán, N., Romaní, A.M., Martí, E., Gómez, R., Bernal, S., Foulquier, A., Mutz, M., Marcé, R., Zoppini, A., Gionchetta, G., Weigelhofer, G., del Campo, R., Robinson, C.T., Gilmer, A., Rulik, M., Obrador, B., Shumilova, O., Zlatanovic, S., Arnon, S., Baldrian, P., Singer, G., Datry, T., Skoulikidis, N., Tietjen, B., and Von Schiller Calle, Daniel Gaspar
- Abstract
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. © 2018 The Authors This paper resulted from discussions conducted as part of working group 3 “Coupled Aquatic-terrestrial Biogeochemistry in IRES” 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). Additional support was provided for MIA by an Alexander von Humboldt Grant (Ref: 1162886 ) and a Juan de la Cierva Grant (Ref: FJCI-2015-26192 ), for CM-L by an Early Career Fellowship from the Graduate Research School (GRS) at BTU Cottbus-Senftenberg and by the French Agency for Biodiversity (ONEMA-AFB, Action 13, Colmatage, échange snappe-rivière et processus biogéochimiques), for MA by the Spanish Government (Ref: DISECO CGL-2014-55-405-R ) and by a Juan de la Cierva Grant (Ref: IJCI-2015-23500 ), for NC by a Juan de la Cierva Grant (Ref: FJCI-2014-23064 ), for SB by Spanish Government (Ref: NICUS CGL-2014-55234-JIN ), for RG by the Science and Technology Agency of Murcia Region (SENECA Foundation, Ref: 19525/PI/14 ), for OS by the SMART joint Doctorate Programme (Science for the MAnagement of Rivers and their Tidal systems, funded by the Erasmus Mundus programme of the European Union ) and for DvS by the Spanish Government (Ref: CGL2016-77487-R ) and Basque Government (Ref: IT951-16 ).
- Published
- 2019
16. Sediment Respiration Pulses in Intermittent Rivers and Ephemeral Streams
- Author
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von Schiller, D., Datry, T., Corti, R., Foulquier, A., Tockner, K., Marce, R., Garcia-Baquero, G., Odriozola, I, Obrador, B., Elosegi, A., Mendoza-Lera, C., Gessner, M. O., Stubbington, R., Albarino, R., Allen, D. C., Altermatt, F., Arce, M. , I, Arnon, S., Banas, D., Banegas-Medina, A., Beller, E., Blanchette, M. L., Blanco-Libreros, J. F., Blessing, J., Boechat, I. G., Boersma, K. S., Bogan, M. T., Bonada, N., Bond, N. R., Brintrup, K., Bruder, A., Burrows, R. M., Cancellario, T., Carlson, S. M., Cauvy-Fraunie, S., Cid, N., Danger, M., de Freitas Terra, B., Dehedin, A., De Girolamo, A. M., del Campo, R., Diaz-Villanueva, V., Duerdoth, C. P., Dyer, F., Faye, E., Febria, C., Figueroa, R., Four, B., Gafny, S., Gomez, R., Gómez-Gener, Lluís, Graca, M. A. S., Guareschi, S., Gucker, B., Hoppeler, F., Hwan, J. L., Kubheka, S., Laini, A., Langhans, S. D., Leigh, C., Little, C. J., Lorenz, S., Marshall, J., Martin, E. J., McIntosh, A., Meyer, E. , I, Milisa, M., Mlambo, M. C., Moleon, M., Morais, M., Negus, P., Niyogi, D., Papatheodoulou, A., Pardo, I, Paril, P., Pesic, V, Piscart, C., Polasek, M., Rodriguez-Lozano, P., Rolls, R. J., Sanchez-Montoya, M. M., Savic, A., Shumilova, O., Steward, A., Taleb, A., Uzan, A., Vander Vorste, R., Waltham, N., Woelfle-Erskine, C., Zak, D., Zarfl, C., Zoppini, A., von Schiller, D., Datry, T., Corti, R., Foulquier, A., Tockner, K., Marce, R., Garcia-Baquero, G., Odriozola, I, Obrador, B., Elosegi, A., Mendoza-Lera, C., Gessner, M. O., Stubbington, R., Albarino, R., Allen, D. C., Altermatt, F., Arce, M. , I, Arnon, S., Banas, D., Banegas-Medina, A., Beller, E., Blanchette, M. L., Blanco-Libreros, J. F., Blessing, J., Boechat, I. G., Boersma, K. S., Bogan, M. T., Bonada, N., Bond, N. R., Brintrup, K., Bruder, A., Burrows, R. M., Cancellario, T., Carlson, S. M., Cauvy-Fraunie, S., Cid, N., Danger, M., de Freitas Terra, B., Dehedin, A., De Girolamo, A. M., del Campo, R., Diaz-Villanueva, V., Duerdoth, C. P., Dyer, F., Faye, E., Febria, C., Figueroa, R., Four, B., Gafny, S., Gomez, R., Gómez-Gener, Lluís, Graca, M. A. S., Guareschi, S., Gucker, B., Hoppeler, F., Hwan, J. L., Kubheka, S., Laini, A., Langhans, S. D., Leigh, C., Little, C. J., Lorenz, S., Marshall, J., Martin, E. J., McIntosh, A., Meyer, E. , I, Milisa, M., Mlambo, M. C., Moleon, M., Morais, M., Negus, P., Niyogi, D., Papatheodoulou, A., Pardo, I, Paril, P., Pesic, V, Piscart, C., Polasek, M., Rodriguez-Lozano, P., Rolls, R. J., Sanchez-Montoya, M. M., Savic, A., Shumilova, O., Steward, A., Taleb, A., Uzan, A., Vander Vorste, R., Waltham, N., Woelfle-Erskine, C., Zak, D., Zarfl, C., and Zoppini, A.
- Abstract
Intermittent rivers and ephemeral streams (IRES) may represent over half the global stream network, but their contribution to respiration and carbon dioxide (CO2) emissions is largely undetermined. In particular, little is known about the variability and drivers of respiration in IRES sediments upon rewetting, which could result in large pulses of CO2. We present a global study examining sediments from 200 dry IRES reaches spanning multiple biomes. Results from standardized assays show that mean respiration increased 32-fold to 66-fold upon sediment rewetting. Structural equation modeling indicates that this response was driven by sediment texture and organic matter quantity and quality, which, in turn, were influenced by climate, land use, and riparian plant cover. Our estimates suggest that respiration pulses resulting from rewetting of IRES sediments could contribute significantly to annual CO2 emissions from the global stream network, with a single respiration pulse potentially increasing emission by 0.2-0.7%. As the spatial and temporal extent of IRES increases globally, our results highlight the importance of recognizing the influence of wetting-drying cycles on respiration and CO2 emissions in stream networks.
- Published
- 2019
- Full Text
- View/download PDF
17. Sediment Respiration Pulses in Intermittent Rivers and Ephemeral Streams
- Author
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Von Schiller Calle, Daniel Gaspar, Datry, T., Corti, R., Foulquier, A., Tockner, K., Marcé, R., García-Baquero, G., Odriozola, I., Obrador, B., Elosegi Irurtia, Arturo, Mendoza-Lera, C., Gessner, M.O., Stubbington, R., Albariño, R., Allen, D.C., Altermatt, F., Arce, M.I., Arnon, S., Banas, D., Banegas-Medina, A., Beller, E., Blanchette, M.L., Blanco-Libreros, J.F., Blessing, J., Boëchat, I.G., Boersma, K.S., Bogan, M.T., Bonada, N., Bond, N.R., Brintrup, K., Bruder, A., Burrows, R.M., Cancellario, T., Carlson, S.M., Cauvy-Fraunié, S., Cid, N., Danger, M., de Freitas Terra, B., Dehedin, A., De Girolamo, A.M., del Campo, R., Díaz-Villanueva, V., Duerdoth, C.P., Dyer, F., Faye, E., Febria, C., Figueroa, R., Four, B., Gafny, S., Gómez, R., Gómez-Gener, L., Graça, M.A.S., Guareschi, S., Gücker, B., Hoppeler, F., Hwan, J.L., Kubheka, S., Laini, A., Langhans, S.D., Leigh, C., Little, C.J., Lorenz, S., Marshall, J., Martín, E.J., McIntosh, A., Meyer, E.I., Milisa, M., Mlambo, M.C., Moleón, M., Morais, M., Negus, P., Niyogi, D., Papatheodoulou, A., Pardo, I., Paril, P., Pesic, V., Piscart, C., Polasek, M., Rodríguez-Lozano, P., Rolls, R.J., Sánchez-Montoya, M.M., Savic, A., Shumilova, O., Steward, A., Taleb, A., Uzan, A., Van der Vorste, R., Waltham, N., Woelfle-Erskine, C., Zak, D., Zarfl, C., Zoppini, A., Von Schiller Calle, Daniel Gaspar, Datry, T., Corti, R., Foulquier, A., Tockner, K., Marcé, R., García-Baquero, G., Odriozola, I., Obrador, B., Elosegi Irurtia, Arturo, Mendoza-Lera, C., Gessner, M.O., Stubbington, R., Albariño, R., Allen, D.C., Altermatt, F., Arce, M.I., Arnon, S., Banas, D., Banegas-Medina, A., Beller, E., Blanchette, M.L., Blanco-Libreros, J.F., Blessing, J., Boëchat, I.G., Boersma, K.S., Bogan, M.T., Bonada, N., Bond, N.R., Brintrup, K., Bruder, A., Burrows, R.M., Cancellario, T., Carlson, S.M., Cauvy-Fraunié, S., Cid, N., Danger, M., de Freitas Terra, B., Dehedin, A., De Girolamo, A.M., del Campo, R., Díaz-Villanueva, V., Duerdoth, C.P., Dyer, F., Faye, E., Febria, C., Figueroa, R., Four, B., Gafny, S., Gómez, R., Gómez-Gener, L., Graça, M.A.S., Guareschi, S., Gücker, B., Hoppeler, F., Hwan, J.L., Kubheka, S., Laini, A., Langhans, S.D., Leigh, C., Little, C.J., Lorenz, S., Marshall, J., Martín, E.J., McIntosh, A., Meyer, E.I., Milisa, M., Mlambo, M.C., Moleón, M., Morais, M., Negus, P., Niyogi, D., Papatheodoulou, A., Pardo, I., Paril, P., Pesic, V., Piscart, C., Polasek, M., Rodríguez-Lozano, P., Rolls, R.J., Sánchez-Montoya, M.M., Savic, A., Shumilova, O., Steward, A., Taleb, A., Uzan, A., Van der Vorste, R., Waltham, N., Woelfle-Erskine, C., Zak, D., Zarfl, C., and Zoppini, A.
- Abstract
Intermittent rivers and ephemeral streams (IRES) may represent over half the global stream network, but their contribution to respiration and carbon dioxide (CO2) emissions is largely undetermined. In particular, little is known about the variability and drivers of respiration in IRES sediments upon rewetting, which could result in large pulses of CO2. We present a global study examining sediments from 200 dry IRES reaches spanning multiple biomes. Results from standardized assays show that mean respiration increased 32-fold to 66-fold upon sediment rewetting. Structural equation modeling indicates that this response was driven by sediment texture and organic matter quantity and quality, which, in turn, were influenced by climate, land use, and riparian plant cover. Our estimates suggest that respiration pulses resulting from rewetting of IRES sediments could contribute significantly to annual CO2 emissions from the global stream network, with a single respiration pulse potentially increasing emission by 0.2 0.7%. As the spatial and temporal extent of IRES increases globally, our results highlight the importance of recognizing the influence of wetting-drying cycles on respiration and CO2 emissions in stream networks. (c)2019. American Geophysical Union. All Rights Reserved.
- Published
- 2019
18. Simulating rewetting events in intermittent rivers and ephemeral streams: A global analysis of leached nutrients and organic matter
- Author
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Shumilova, O., Zak, D., Datry, T., Von Schiller Calle, Daniel Gaspar, Corti, R., Foulquier, A., Obrador, B., Tockner, K., Allan, D.C., Altermatt, F., Arce, M.I., Arnon, S., Banas, D., Banegas-Medina, A., Beller, E., Blanchette, M.L., Blanco-Libreros, J.F., Blessing, J., Boëchat, I.G., Boersma, K., Bogan, M.T., Bonada, N., Bond, N.R., Brintrup, K., Bruder, A., Burrows, R., Cancellario, T., Carlson, S.M., Cauvy-Fraunié, S., Cid, N., Danger, M., de Freitas, Terra, B., Girolamo, A.M.D., del Campo, R., Dyer, F., Elosegi, A., Faye, E., Febria, C., Figueroa, R., Four, B., Gessner, M.O., Gnohossou, P., Cerezo, R.G., Gomez-Gener, L., Graça, M.A.S., Guareschi, S., Gücker, B., Hwan, J.L., Kubheka, S., Langhans, S.D., Leigh, C., Little, C.J., Lorenz, S., Marshall, J., McIntosh, A., Mendoza-Lera, C., Meyer, E.I., Milisa, M., Mlambo, M.C., Moleón, M., Negus, P., Niyogi, D., Papatheodoulou, A., Pardo, I., Paril, P., Pesic, V., Rodriguez-Lozano, P., Rolls, R.J., Sanchez-Montoya, M.M., Savic, A., Steward, A., Stubbington, R., Taleb, A., Vorste, R.V., Waltham, N., Zoppini, A., Zarfl, C., Shumilova, O., Zak, D., Datry, T., Von Schiller Calle, Daniel Gaspar, Corti, R., Foulquier, A., Obrador, B., Tockner, K., Allan, D.C., Altermatt, F., Arce, M.I., Arnon, S., Banas, D., Banegas-Medina, A., Beller, E., Blanchette, M.L., Blanco-Libreros, J.F., Blessing, J., Boëchat, I.G., Boersma, K., Bogan, M.T., Bonada, N., Bond, N.R., Brintrup, K., Bruder, A., Burrows, R., Cancellario, T., Carlson, S.M., Cauvy-Fraunié, S., Cid, N., Danger, M., de Freitas, Terra, B., Girolamo, A.M.D., del Campo, R., Dyer, F., Elosegi, A., Faye, E., Febria, C., Figueroa, R., Four, B., Gessner, M.O., Gnohossou, P., Cerezo, R.G., Gomez-Gener, L., Graça, M.A.S., Guareschi, S., Gücker, B., Hwan, J.L., Kubheka, S., Langhans, S.D., Leigh, C., Little, C.J., Lorenz, S., Marshall, J., McIntosh, A., Mendoza-Lera, C., Meyer, E.I., Milisa, M., Mlambo, M.C., Moleón, M., Negus, P., Niyogi, D., Papatheodoulou, A., Pardo, I., Paril, P., Pesic, V., Rodriguez-Lozano, P., Rolls, R.J., Sanchez-Montoya, M.M., Savic, A., Steward, A., Stubbington, R., Taleb, A., Vorste, R.V., Waltham, N., Zoppini, A., and Zarfl, C.
- Abstract
Climate change and human pressures are changing the global distribution and the extent of intermittent rivers and ephemeral streams (IRES), which comprise half of the global river network area. IRES are characterized by periods of flow cessation, during which channel substrates accumulate and undergo physico-chemical changes (preconditioning), and periods of flow resumption, when these substrates are rewetted and release pulses of dissolved nutrients and organic matter (OM). However, there are no estimates of the amounts and quality of leached substances, nor is there information on the underlying environmental constraints operating at the global scale. We experimentally simulated, under standard laboratory conditions, rewetting of leaves, riverbed sediments, and epilithic biofilms collected during the dry phase across 205 IRES from five major climate zones. We determined the amounts and qualitative characteristics of the leached nutrients and OM, and estimated their areal fluxes from riverbeds. In addition, we evaluated the variance in leachate characteristics in relation to selected environmental variables and substrate characteristics. We found that sediments, due to their large quantities within riverbeds, contribute most to the overall flux of dissolved substances during rewetting events (56% 98%), and that flux rates distinctly differ among climate zones. Dissolved organic carbon, phenolics, and nitrate contributed most to the areal fluxes. The largest amounts of leached substances were found in the continental climate zone, coinciding with the lowest potential bioavailability of the leached OM. The opposite pattern was found in the arid zone. Environmental variables expected to be modified under climate change (i.e. potential evapotranspiration, aridity, dry period duration, land use) were correlated with the amount of leached substances, with the strongest relationship found for sediments. These results show that the role of IRES should be accounted for in g
- Published
- 2019
19. Simulating rewetting events in intermittent rivers and ephemeral streams: A global analysis of leached nutrients and organic matter
- Author
-
Shumilova, O, Zak, D, Datry, T, von Schiller, D, Corti, R, Foulquier, A, Obrador, B, Tockner, K, Allan, DC, Altermatt, F, Isabel Arce, M, Arnon, S, Banas, D, Banegas-Medina, A, Beller, E, Blanchette, ML, Blanco-Libreros, JF, Blessing, J, Boechat, IG, Boersma, K, Bogan, MT, Bonada, N, Bond, NR, Brintrup, K, Bruder, A, Burrows, R, Cancellario, T, Carlson, SM, Cauvy-Fraunie, S, Cid, N, Danger, M, de Freitas Terra, B, De Girolamo, AM, del Campo, R, Dyer, F, Elosegi, A, Faye, E, Febria, C, Figueroa, R, Four, B, Gessner, MO, Gnohossou, P, Cerezo, RG, Gomez-Gener, L, Graca, MAS, Guareschi, S, Guecker, B, Hwan, JL, Kubheka, S, Langhans, SD, Leigh, C, Little, CJ, Lorenz, S, Marshall, J, McIntosh, A, Mendoza-Lera, C, Meyer, EI, Milisa, M, Mlambo, MC, Moleon, M, Negus, P, Niyogi, D, Papatheodoulou, A, Pardo, I, Paril, P, Pesic, V, Rodriguez-Lozano, P, Rolls, RJ, Sanchez-Montoya, MM, Savic, A, Steward, A, Stubbington, R, Taleb, A, Vander Vorste, R, Waltham, N, Zoppini, A, Zarfl, C, Shumilova, O, Zak, D, Datry, T, von Schiller, D, Corti, R, Foulquier, A, Obrador, B, Tockner, K, Allan, DC, Altermatt, F, Isabel Arce, M, Arnon, S, Banas, D, Banegas-Medina, A, Beller, E, Blanchette, ML, Blanco-Libreros, JF, Blessing, J, Boechat, IG, Boersma, K, Bogan, MT, Bonada, N, Bond, NR, Brintrup, K, Bruder, A, Burrows, R, Cancellario, T, Carlson, SM, Cauvy-Fraunie, S, Cid, N, Danger, M, de Freitas Terra, B, De Girolamo, AM, del Campo, R, Dyer, F, Elosegi, A, Faye, E, Febria, C, Figueroa, R, Four, B, Gessner, MO, Gnohossou, P, Cerezo, RG, Gomez-Gener, L, Graca, MAS, Guareschi, S, Guecker, B, Hwan, JL, Kubheka, S, Langhans, SD, Leigh, C, Little, CJ, Lorenz, S, Marshall, J, McIntosh, A, Mendoza-Lera, C, Meyer, EI, Milisa, M, Mlambo, MC, Moleon, M, Negus, P, Niyogi, D, Papatheodoulou, A, Pardo, I, Paril, P, Pesic, V, Rodriguez-Lozano, P, Rolls, RJ, Sanchez-Montoya, MM, Savic, A, Steward, A, Stubbington, R, Taleb, A, Vander Vorste, R, Waltham, N, Zoppini, A, and Zarfl, C
- Abstract
Climate change and human pressures are changing the global distribution and the extent of intermittent rivers and ephemeral streams (IRES), which comprise half of the global river network area. IRES are characterized by periods of flow cessation, during which channel substrates accumulate and undergo physico-chemical changes (preconditioning), and periods of flow resumption, when these substrates are rewetted and release pulses of dissolved nutrients and organic matter (OM). However, there are no estimates of the amounts and quality of leached substances, nor is there information on the underlying environmental constraints operating at the global scale. We experimentally simulated, under standard laboratory conditions, rewetting of leaves, riverbed sediments, and epilithic biofilms collected during the dry phase across 205 IRES from five major climate zones. We determined the amounts and qualitative characteristics of the leached nutrients and OM, and estimated their areal fluxes from riverbeds. In addition, we evaluated the variance in leachate characteristics in relation to selected environmental variables and substrate characteristics. We found that sediments, due to their large quantities within riverbeds, contribute most to the overall flux of dissolved substances during rewetting events (56%–98%), and that flux rates distinctly differ among climate zones. Dissolved organic carbon, phenolics, and nitrate contributed most to the areal fluxes. The largest amounts of leached substances were found in the continental climate zone, coinciding with the lowest potential bioavailability of the leached OM. The opposite pattern was found in the arid zone. Environmental variables expected to be modified under climate change (i.e. potential evapotranspiration, aridity, dry period duration, land use) were correlated with the amount of leached substances, with the strongest relationship found for sediments. These results show that the role of IRES should be accounted for in g
- Published
- 2019
20. Sediment Respiration Pulses in Intermittent Rivers and Ephemeral Streams
- Author
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von Schiller, D; https://orcid.org/0000-0002-9493-3244, Datry, T; https://orcid.org/0000-0003-1390-6736, Corti, R, Foulquier, A, Tockner, K, Marcé, R; https://orcid.org/0000-0002-7416-4652, García‐Baquero, G; https://orcid.org/0000-0001-6550-1584, Odriozola, I; https://orcid.org/0000-0002-5289-7935, Obrador, B; https://orcid.org/0000-0003-4050-0491, Elosegi, A, Mendoza‐Lera, C; https://orcid.org/0000-0002-3222-2498, Gessner, M O, Stubbington, R, Albariño, R, Allen, D C, Altermatt, Florian, Arce, M I, Arnon, S; https://orcid.org/0000-0002-7109-8979, Banas, D, Banegas‐Medina, A, Beller, E, Blanchette, M L, Blanco‐Libreros, J F, Blessing, J, Boëchat, I G; https://orcid.org/0000-0002-9651-6364, Boersma, K S, Bogan, M T, Bonada, N, Bond, N R; https://orcid.org/0000-0003-4294-6008, Brintrup, K, et al, von Schiller, D; https://orcid.org/0000-0002-9493-3244, Datry, T; https://orcid.org/0000-0003-1390-6736, Corti, R, Foulquier, A, Tockner, K, Marcé, R; https://orcid.org/0000-0002-7416-4652, García‐Baquero, G; https://orcid.org/0000-0001-6550-1584, Odriozola, I; https://orcid.org/0000-0002-5289-7935, Obrador, B; https://orcid.org/0000-0003-4050-0491, Elosegi, A, Mendoza‐Lera, C; https://orcid.org/0000-0002-3222-2498, Gessner, M O, Stubbington, R, Albariño, R, Allen, D C, Altermatt, Florian, Arce, M I, Arnon, S; https://orcid.org/0000-0002-7109-8979, Banas, D, Banegas‐Medina, A, Beller, E, Blanchette, M L, Blanco‐Libreros, J F, Blessing, J, Boëchat, I G; https://orcid.org/0000-0002-9651-6364, Boersma, K S, Bogan, M T, Bonada, N, Bond, N R; https://orcid.org/0000-0003-4294-6008, Brintrup, K, and et al
- Abstract
Intermittent rivers and ephemeral streams (IRES) may represent over half the global stream network, but their contribution to respiration and carbon dioxide (CO2) emissions is largely undetermined. In particular, little is known about the variability and drivers of respiration in IRES sediments upon rewetting, which could result in large pulses of CO2. We present a global study examining sediments from 200 dry IRES reaches spanning multiple biomes. Results from standardized assays show that mean respiration increased 32‐fold to 66‐fold upon sediment rewetting. Structural equation modeling indicates that this response was driven by sediment texture and organic matter quantity and quality, which, in turn, were influenced by climate, land use, and riparian plant cover. Our estimates suggest that respiration pulses resulting from rewetting of IRES sediments could contribute significantly to annual CO2 emissions from the global stream network, with a single respiration pulse potentially increasing emission by 0.2–0.7%. As the spatial and temporal extent of IRES increases globally, our results highlight the importance of recognizing the influence of wetting‐drying cycles on respiration and CO2 emissions in stream networks.
- Published
- 2019
21. Sediment Respiration Pulses in Intermittent Rivers and Ephemeral Streams
- Author
-
von Schiller, D., primary, Datry, T., additional, Corti, R., additional, Foulquier, A., additional, Tockner, K., additional, Marcé, R., additional, García‐Baquero, G., additional, Odriozola, I., additional, Obrador, B., additional, Elosegi, A., additional, Mendoza‐Lera, C., additional, Gessner, M. O., additional, Stubbington, R., additional, Albariño, R., additional, Allen, D. C., additional, Altermatt, F., additional, Arce, M. I., additional, Arnon, S., additional, Banas, D., additional, Banegas‐Medina, A., additional, Beller, E., additional, Blanchette, M. L., additional, Blanco‐Libreros, J. F., additional, Blessing, J., additional, Boëchat, I. G., additional, Boersma, K. S., additional, Bogan, M. T., additional, Bonada, N., additional, Bond, N. R., additional, Brintrup, K., additional, Bruder, A., additional, Burrows, R. M., additional, Cancellario, T., additional, Carlson, S. M., additional, Cauvy‐Fraunié, S., additional, Cid, N., additional, Danger, M., additional, de Freitas Terra, B., additional, Dehedin, A., additional, De Girolamo, A. M., additional, del Campo, R., additional, Díaz‐Villanueva, V., additional, Duerdoth, C. P., additional, Dyer, F., additional, Faye, E., additional, Febria, C., additional, Figueroa, R., additional, Four, B., additional, Gafny, S., additional, Gómez, R., additional, Gómez‐Gener, L., additional, Graça, M. A. S., additional, Guareschi, S., additional, Gücker, B., additional, Hoppeler, F., additional, Hwan, J. L., additional, Kubheka, S., additional, Laini, A., additional, Langhans, S. D., additional, Leigh, C., additional, Little, C. J., additional, Lorenz, S., additional, Marshall, J., additional, Martín, E. J., additional, McIntosh, A., additional, Meyer, E. I., additional, Miliša, M., additional, Mlambo, M. C., additional, Moleón, M., additional, Morais, M., additional, Negus, P., additional, Niyogi, D., additional, Papatheodoulou, A., additional, Pardo, I., additional, Pařil, P., additional, Pešić, V., additional, Piscart, C., additional, Polášek, M., additional, Rodríguez‐Lozano, P., additional, Rolls, R. J., additional, Sánchez‐Montoya, M. M., additional, Savić, A., additional, Shumilova, O., additional, Steward, A., additional, Taleb, A., additional, Uzan, A., additional, Vander Vorste, R., additional, Waltham, N., additional, Woelfle‐Erskine, C., additional, Zak, D., additional, Zarfl, C., additional, and Zoppini, A., additional
- Published
- 2019
- Full Text
- View/download PDF
22. Emissions from dry inland waters are a blind spot in the global carbon cycle
- Author
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Marcé, R., Obrador, B., Gómez-Gener, L., Catalán, N., Koschorreck, Matthias, Arce, M.I., Singer, G., von Schiller, D., Marcé, R., Obrador, B., Gómez-Gener, L., Catalán, N., Koschorreck, Matthias, Arce, M.I., Singer, G., and von Schiller, D.
- Abstract
A large part of the world's inland waters, including streams, rivers, ponds, lakes and reservoirs is subject to occasional, recurrent or even permanent drying. Moreover, the occurrence and intensity of drying events are increasing in many areas of the world because of climate change, water abstraction, and land use alteration. Yet, information on the gaseous carbon (C) fluxes from dry inland waters is scarce, thus precluding a comprehensive assessment of C emissions including all, also intermittently dry, inland waters. Here, we review current knowledge on gaseous C fluxes from lotic (streams and rivers) and lentic (ponds, lakes, and reservoirs) inland waters during dry phases and the response to rewetting, considering controls and sources as well as implications of including ‘dry’ fluxes for local and global scale estimates. Moreover, knowledge gaps and research needs are discussed. Our conservative estimates indicate that adding emissions from dry inland waters to current global estimates of CO2 emissions from inland waters could result in an increase of 0.22 Pg C year−1, or ~10% of total fluxes. We outline the necessary conceptual understanding to successfully include dry phases in a more complete picture of inland water C emissions and identify potential implications for global C cycle feedbacks.
- Published
- 2018
23. Dry habitats sustain high CO2 emissions from temporary ponds across seasons
- Author
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Obrador, B., von Schiller, D., Marcé, R., Gómez-Gener, L., Koschorreck, Matthias, Borrego, C., Catalán, N., Obrador, B., von Schiller, D., Marcé, R., Gómez-Gener, L., Koschorreck, Matthias, Borrego, C., and Catalán, N.
- Abstract
Despite the increasing understanding of the magnitude and drivers of carbon gas emissions from inland waters, the relevance of water fluctuation and associated drying on their dynamics is rarely addressed. Here, we quantified CO2 and CH4 fluxes from a set of temporary ponds across seasons. The ponds were in all occasion net CO2 emitters irrespective of the presence or absence of water. While the CO2 fluxes were in the upper range of emissions for freshwater lentic systems, CH4 fluxes were mostly undetectable. Dry habitats substantially contributed to these emissions and were always a source of CO2, whereas inundated habitats acted either as a source or a sink of atmospheric CO2 along the year. Higher concentrations of coloured and humic organic matter in water and sediment were linked to higher CO2 emissions. Composition of the sediment microbial community was related both to dissolved organic matter concentration and composition, but we did not find a direct link with CO2 fluxes. The presence of methanogenic archaea in most ponds suggested the potential for episodic CH4 production and emission. Our results highlight the need for spatially and temporally inclusive approaches that consider the dry phases and habitats to characterize carbon cycling in temporary systems.
- Published
- 2018
24. A European Multi Lake Survey dataset of environmental variables, phytoplankton pigments and cyanotoxins
- Author
-
European Cooperation in Science and Technology, Hernández, Armand [0000-0001-7245-9863], Mantzouki, E., Campbell, James, van Loon, E., Visser, P., Konstantinou, I., Antoniou, M., Giuliani, G., Machado-Vieira, D., Gurjão de Oliveira, Alinne, Maronić, D.Š., Stević, F., Hiskia, A., Gkelis, S., Walusiak, E., Panou, M., McCarthy, V., Budzyńska, A., Perello, V.C., Kostrzewska-Szlakowska, I., Gonçalves, V., Skjelbred, B., Palomino, Roberto L., Obertegger, U., Boscaini, A., Flaim, G., Salmaso, N., Gagala, I., Cerasino, L., Mankiewicz-Boczek, J., Hansson, L. A., Grabowska, M., Karpowicz, M., Rodríguez-Pérez, E., Chmura, D., Nawrocka, L., Kozak, A., Kobos, J., Rosińska, J., Seelen, L., Toporowska, M., Pawlik-Skowronska, B., Urrutia-Cordero, Pablo, Niedźwiecki, M., Maliaka, V., Pęczuła, W., Wasilewicz, M., Napiórkowska-Krzebietke, A., Ochocka, A., Beklioğlu, M., Szeląg-Wasielewska, E., Domek, P., Teurlincx, S., Jakubowska-Krepska, N., Tavşanoğlu, ÜN., Carballeira, R., Kwasizur, K., Drastichova, I., Messyasz, B., Chomova, L., Soylu, E.N., Pasztaleniec, A., Jasser, I., Filiz, N., Antão-Geraldes, A. M., Bilgin, F., Camacho, A., Özen, A., Leira, M., Hernández, Armand, Vasconcelos, V., Remec-Rekar, S., Pfeiffer, T.Ž., Eleršek, Tina, Delgado-Martín, Jordi, Yağcı, M.A., García, D., Bezirci, G., Bláha, L., Bravo, Andrea G., Verstijnen, Y., Cereijo, J. L., Gomà, Joan, Trapote, M.C., Vegas-Vilarrúbia, Teresa, Obrador, B., García-Murcia, A., Real, M., Picazo, Antoni, Vucelić, I.B., Romans, E., Cesur, M., Çınar, Ş., Lürling, M., Levi, E., Noguero-Ribes, J., Duque, D.P., Fernández-Morán, E., Úbeda, B., Yağcı, A., Gálvez, J.Á., Marcé, Rafael, Catalán, N., Buck, Moritz, Pérez-Martínez, Carmen, Ramos-Rodríguez, E., Tsiarta, N., Žutinić, P., Iskin, U., Çapkın, K., Udovič, M.G., Cillero-Castro, C., Moreno-Ostos, Enrique, Blanco, J. M., Rodríguez, V., Plenković-Moraj, Anđelka, Montes-Pérez, J.J., Colom-Montero, W., Koreivienė, J., Rochera, C., Santamans, A. C., Ferriol, C., Romo, S., Faassen, E.J., Soria, J. M., Latour, D., Mazur-Marzec, Hanna, Mustonen, K., Pierson, D., Kasperovičienė, J., Yang, Y., Verspagen, Jolanda M. H., Çelik, K., de Senerpont Domis, L.N., Özhan, K., Dunalska, J., Carey, C.C., Paerl, Hans, Alcaraz-Párraga, P., Torokne, A., Goldyn, R., Karan, T., Bulut, C., Demir, N., Uysal, R., Pełechata, A., Karakaya, N., Koçer, M.A.T., Sieńska, J., Yilmaz, M., Bańkowska-Sobczak, A., Savadova, K., Maraşlıoğlu, F., Geriš, R., Fakioglu, Ö., Fránková, M., Morais, J., Köker, L., Bergkemper, V., Pełechaty, M., O'Leary, S., Nemova, H., Vitonytė, I., Wilk-Woźniak, E., Beirne, E., Cromie, H., Ibelings, Bas W., Christoffersen, K. S., Warming, T.P., Feldmann, T., Laas, A., Vale, M., Panksep, K., Frąk, M., Kokocinski, M., Krztoń, W., Szymański, D., Tuvikene, L., Kangro, K., Häggqvist, K., Salmi, P., Arvola, L., Fastner, J., Straile, D., Haande, S., Rothhaupt, K. O., Fonvielle, J., Krstić, S., Raposeiro, P. M., Kruk, M., Madrecka, B., Grossart, Hans-Peter, Avagianos, C., Kaloudis, T., Triantis, T., Aleksovski, B., Zervou, S. K., European Cooperation in Science and Technology, Hernández, Armand [0000-0001-7245-9863], Mantzouki, E., Campbell, James, van Loon, E., Visser, P., Konstantinou, I., Antoniou, M., Giuliani, G., Machado-Vieira, D., Gurjão de Oliveira, Alinne, Maronić, D.Š., Stević, F., Hiskia, A., Gkelis, S., Walusiak, E., Panou, M., McCarthy, V., Budzyńska, A., Perello, V.C., Kostrzewska-Szlakowska, I., Gonçalves, V., Skjelbred, B., Palomino, Roberto L., Obertegger, U., Boscaini, A., Flaim, G., Salmaso, N., Gagala, I., Cerasino, L., Mankiewicz-Boczek, J., Hansson, L. A., Grabowska, M., Karpowicz, M., Rodríguez-Pérez, E., Chmura, D., Nawrocka, L., Kozak, A., Kobos, J., Rosińska, J., Seelen, L., Toporowska, M., Pawlik-Skowronska, B., Urrutia-Cordero, Pablo, Niedźwiecki, M., Maliaka, V., Pęczuła, W., Wasilewicz, M., Napiórkowska-Krzebietke, A., Ochocka, A., Beklioğlu, M., Szeląg-Wasielewska, E., Domek, P., Teurlincx, S., Jakubowska-Krepska, N., Tavşanoğlu, ÜN., Carballeira, R., Kwasizur, K., Drastichova, I., Messyasz, B., Chomova, L., Soylu, E.N., Pasztaleniec, A., Jasser, I., Filiz, N., Antão-Geraldes, A. M., Bilgin, F., Camacho, A., Özen, A., Leira, M., Hernández, Armand, Vasconcelos, V., Remec-Rekar, S., Pfeiffer, T.Ž., Eleršek, Tina, Delgado-Martín, Jordi, Yağcı, M.A., García, D., Bezirci, G., Bláha, L., Bravo, Andrea G., Verstijnen, Y., Cereijo, J. L., Gomà, Joan, Trapote, M.C., Vegas-Vilarrúbia, Teresa, Obrador, B., García-Murcia, A., Real, M., Picazo, Antoni, Vucelić, I.B., Romans, E., Cesur, M., Çınar, Ş., Lürling, M., Levi, E., Noguero-Ribes, J., Duque, D.P., Fernández-Morán, E., Úbeda, B., Yağcı, A., Gálvez, J.Á., Marcé, Rafael, Catalán, N., Buck, Moritz, Pérez-Martínez, Carmen, Ramos-Rodríguez, E., Tsiarta, N., Žutinić, P., Iskin, U., Çapkın, K., Udovič, M.G., Cillero-Castro, C., Moreno-Ostos, Enrique, Blanco, J. M., Rodríguez, V., Plenković-Moraj, Anđelka, Montes-Pérez, J.J., Colom-Montero, W., Koreivienė, J., Rochera, C., Santamans, A. C., Ferriol, C., Romo, S., Faassen, E.J., Soria, J. M., Latour, D., Mazur-Marzec, Hanna, Mustonen, K., Pierson, D., Kasperovičienė, J., Yang, Y., Verspagen, Jolanda M. H., Çelik, K., de Senerpont Domis, L.N., Özhan, K., Dunalska, J., Carey, C.C., Paerl, Hans, Alcaraz-Párraga, P., Torokne, A., Goldyn, R., Karan, T., Bulut, C., Demir, N., Uysal, R., Pełechata, A., Karakaya, N., Koçer, M.A.T., Sieńska, J., Yilmaz, M., Bańkowska-Sobczak, A., Savadova, K., Maraşlıoğlu, F., Geriš, R., Fakioglu, Ö., Fránková, M., Morais, J., Köker, L., Bergkemper, V., Pełechaty, M., O'Leary, S., Nemova, H., Vitonytė, I., Wilk-Woźniak, E., Beirne, E., Cromie, H., Ibelings, Bas W., Christoffersen, K. S., Warming, T.P., Feldmann, T., Laas, A., Vale, M., Panksep, K., Frąk, M., Kokocinski, M., Krztoń, W., Szymański, D., Tuvikene, L., Kangro, K., Häggqvist, K., Salmi, P., Arvola, L., Fastner, J., Straile, D., Haande, S., Rothhaupt, K. O., Fonvielle, J., Krstić, S., Raposeiro, P. M., Kruk, M., Madrecka, B., Grossart, Hans-Peter, Avagianos, C., Kaloudis, T., Triantis, T., Aleksovski, B., and Zervou, S. K.
- Abstract
Under ongoing climate change and increasing anthropogenic activity, which continuously challenge ecosystem resilience, an in-depth understanding of ecological processes is urgently needed. Lakes, as providers of numerous ecosystem services, face multiple stressors that threaten their functioning. Harmful cyanobacterial blooms are a persistent problem resulting from nutrient pollution and climate-change induced stressors, like poor transparency, increased water temperature and enhanced stratification. Consistency in data collection and analysis methods is necessary to achieve fully comparable datasets and for statistical validity, avoiding issues linked to disparate data sources. The European Multi Lake Survey (EMLS) in summer 2015 was an initiative among scientists from 27 countries to collect and analyse lake physical, chemical and biological variables in a fully standardized manner. This database includes in-situ lake variables along with nutrient, pigment and cyanotoxin data of 369 lakes in Europe, which were centrally analysed in dedicated laboratories. Publishing the EMLS methods and dataset might inspire similar initiatives to study across large geographic areas that will contribute to better understanding lake responses in a changing environment.
- Published
- 2018
25. Under-ice dynamics of dissolved oxygen from lake Tovel (Italy) based on high frequency data from three winters
- Author
-
Obertegger, U., Obrador, B., and Flaim, G.
- Subjects
Cluster analysis ,Under-ice metabolism ,Depletion rate ,Settore BIO/07 - ECOLOGIA - Published
- 2017
26. Under-ice dynamics of dissolved oxygen from Lake Tovel (ltaly) based on high frequency data
- Author
-
Obertegger, U., Obrador, B., and Flaim, G.
- Subjects
Under-ice metabolism ,Depletion rate ,Settore BIO/07 - ECOLOGIA ,Oligotrophic - Published
- 2017
27. Biodegradation kinetics of dissolved organic matter chromatographic fractions in an intermittent river
- Author
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Catalan, N., Casas-Ruiz, J. P., von Schiller, D., Proia, L., Obrador, B., Zwirnmann, E., Marce, R., Catalan, N., Casas-Ruiz, J. P., von Schiller, D., Proia, L., Obrador, B., Zwirnmann, E., and Marce, R.
- Abstract
Controls on the degradation of dissolved organic matter (DOM) are complex but key to understand the role of freshwaters in the carbon cycle. Both the origin and previous degradation history have been suggested to determine DOM reactivity, but it is still a major challenge to understand the links between DOM composition and biodegradation kinetics. An appropriate context to study these links are intermittent rivers, as summer drought naturally diversifies DOM sources and sinks. Here we investigated the biodegradation kinetics of DOM in the main aquatic environments present in a temporary river. During dark incubations we traced the dynamics of bulk DOM and its main chromatographic fractions defined using LC-OCD: high molecular weight substances (HMWS), low molecular weight substances (LMWS), and humic substances and building blocks. Bulk DOM decay patterns were successfully fitted to the reactivity continuum (RC) biodegradation model. The RC parameters depicted running waters as the sites presenting a more reactive DOM, and temporary pools, enriched in leaf litter, as the ones with slowest DOM decay. The decay patterns of each DOM fraction were consistent throughout sites. LMWS and HMWS decayed in all cases and could be modeled using the RC model. Notably, the dynamics of LMWS controlled the bulk DOM kinetics. We discuss the mechanistic basis for the chromatographic fractions' kinetics during biodegradation and the implications that preconditioning and summer drought can have for DOM biodegradation in intermittent rivers.
- Published
- 2017
- Full Text
- View/download PDF
28. Delving deeper: Metabolic processes in the metalimnion of stratified lakes
- Author
-
Giling, D.P., Staehr, P.A., Grossart, H.P., Andersen, M.R., Boehrer, Bertram, Escot, C., Evrendilek, F., Gómez-Gener, L., Honti, M., Jones, I.D., Karakaya, N., Laas, A., Moreno-Ostos, E., Rinke, Karsten, Scharfenberger, U., Schmidt, S.R., Weber, Michael, Woolway, R.I., Zwart, J.A., Obrador, B., Giling, D.P., Staehr, P.A., Grossart, H.P., Andersen, M.R., Boehrer, Bertram, Escot, C., Evrendilek, F., Gómez-Gener, L., Honti, M., Jones, I.D., Karakaya, N., Laas, A., Moreno-Ostos, E., Rinke, Karsten, Scharfenberger, U., Schmidt, S.R., Weber, Michael, Woolway, R.I., Zwart, J.A., and Obrador, B.
- Abstract
Many lakes exhibit seasonal stratification, during which they develop strong thermal and chemical gradients. An expansion of depth-integrated monitoring programs has provided insight into the importance of organic carbon processing that occurs below the upper mixed layer. However, the chemical and physical drivers of metabolism and metabolic coupling remain unresolved, especially in the metalimnion. In this depth zone, sharp gradients in key resources such as light and temperature co-occur with dynamic physical conditions that influence metabolic processes directly and simultaneously hamper the accurate tracing of biological activity. We evaluated the drivers of metalimnetic metabolism and its associated uncertainty across 10 stratified lakes in Europe and North America. We hypothesized that the metalimnion would contribute highly to whole-lake functioning in clear oligotrophic lakes, and that metabolic rates would be highly variable in unstable polymictic lakes. Depth-integrated rates of gross primary production (GPP) and ecosystem respiration (ER) were modelled from diel dissolved oxygen curves using a Bayesian approach. Metabolic estimates were more uncertain below the epilimnion, but uncertainty was not consistently related to lake morphology or mixing regime. Metalimnetic rates exhibited high day-to-day variability in all trophic states, with the metalimnetic contribution to daily whole-lake GPP and ER ranging from 0% to 87% and < 1% to 92%, respectively. Nonetheless, the metalimnion of low-nutrient lakes contributed strongly to whole-lake metabolism on average, driven by a collinear combination of highlight, low surface-water phosphorous concentration and high metalimnetic volume. Consequently, a single-sensor approach does not necessarily reflect whole-ecosystem carbon dynamics in stratified lakes.
- Published
- 2017
29. Networking lake observatories in Europe: an overview
- Author
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Jennings, E., de Eyto, E., Flaim, G., George, D.G., Ibelings, B., Jones, I.D., Laas, A., Marce, R., Maberly, S., Obrador, B., Pierson, D., de Senerpont Domis, L., and Staehr, P.
- Subjects
Lakes ,Settore BIO/07 - ECOLOGIA ,NETLAKE - Published
- 2016
30. Biodegradation kinetics of dissolved organic matter chromatographic fractions in an intermittent river
- Author
-
Catalán, N., primary, Casas-Ruiz, J. P., additional, von Schiller, D., additional, Proia, L., additional, Obrador, B., additional, Zwirnmann, E., additional, and Marcé, R., additional
- Published
- 2017
- Full Text
- View/download PDF
31. Linking lakes across Europe
- Author
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Jennings, E., Ibelings, B., de Eyto, E., Pierson, D., Laas, A., Obrador, B., Jones, I., de Senorpont Domis, L., Flaim, G., Marcè, R., George, G., and Stronmberg, A.
- Subjects
High frequency data ,Settore BIO/07 - ECOLOGIA ,NETLAKE ,Tovel ,Dati ad alta frequenza - Published
- 2015
32. Sediment Respiration Pulses in Intermittent Rivers and Ephemeral Streams.
- Author
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Schiller, D., Datry, T., Corti, R., Foulquier, A., Tockner, K., Marcé, R., García‐Baquero, G., Odriozola, I., Obrador, B., Elosegi, A., Mendoza‐Lera, C., Gessner, M. O., Stubbington, R., Albariño, R., Allen, D. C., Altermatt, F., Arce, M. I., Arnon, S., Banas, D., and Banegas‐Medina, A.
- Subjects
EPHEMERAL streams ,RESPIRATION ,STRUCTURAL equation modeling ,SEDIMENTS ,RIVERS ,GROUND cover plants ,SOIL texture - Abstract
Intermittent rivers and ephemeral streams (IRES) may represent over half the global stream network, but their contribution to respiration and carbon dioxide (CO2) emissions is largely undetermined. In particular, little is known about the variability and drivers of respiration in IRES sediments upon rewetting, which could result in large pulses of CO2. We present a global study examining sediments from 200 dry IRES reaches spanning multiple biomes. Results from standardized assays show that mean respiration increased 32‐fold to 66‐fold upon sediment rewetting. Structural equation modeling indicates that this response was driven by sediment texture and organic matter quantity and quality, which, in turn, were influenced by climate, land use, and riparian plant cover. Our estimates suggest that respiration pulses resulting from rewetting of IRES sediments could contribute significantly to annual CO2 emissions from the global stream network, with a single respiration pulse potentially increasing emission by 0.2–0.7%. As the spatial and temporal extent of IRES increases globally, our results highlight the importance of recognizing the influence of wetting‐drying cycles on respiration and CO2 emissions in stream networks. Key Points: Sediment respiration in intermittent rivers and ephemeral streams increases substantially in response to rewettingRespiration pulses are driven by sediment properties, which, in turn, are influenced by climate and catchment characteristicsEffects of wetting‐drying cycles on respiration and CO2 emissions in stream networks need consideration in upscaling and modeling efforts [ABSTRACT FROM AUTHOR]
- Published
- 2019
- Full Text
- View/download PDF
33. Automatic high frequency monitoring for improved lake and reservoir management
- Author
-
Marcé, R., George, G., Buscarinu, P., Deidda, M., Dunalska, J., de Eyto, E., Flaim, G., Grossart, H.-P., Istvanovics, V., Lenhardt, M., Moreno-Ostos, E., Obrador, B., Ostrovsky, I., Pierson, D.C., Potužák, J., Poikane, S., Rinke, Karsten, Rodríguez-Mozaz, S., Staehr, P.A., Šumberová, K., Waajen, G., Weyhenmeyer, G.A., Weathers, K.C., Zion, M., Ibelings, B.W., Jennings, E., Marcé, R., George, G., Buscarinu, P., Deidda, M., Dunalska, J., de Eyto, E., Flaim, G., Grossart, H.-P., Istvanovics, V., Lenhardt, M., Moreno-Ostos, E., Obrador, B., Ostrovsky, I., Pierson, D.C., Potužák, J., Poikane, S., Rinke, Karsten, Rodríguez-Mozaz, S., Staehr, P.A., Šumberová, K., Waajen, G., Weyhenmeyer, G.A., Weathers, K.C., Zion, M., Ibelings, B.W., and Jennings, E.
- Abstract
Recent technological developments have increased the number of variables being monitored in lakes and reservoirs using automatic high frequency monitoring (AHFM). However, design of AHFM systems and posterior data handling and interpretation are currently being developed on a site-by-site and issue-by-issue basis with minimal standardization of protocols or knowledge sharing. As a result, many deployments become short-lived or underutilized, and many new scientific developments that are potentially useful for water management and environmental legislation remain underexplored. This Critical Review bridges scientific uses of AHFM with their applications by providing an overview of the current AHFM capabilities, together with examples of successful applications. We review the use of AHFM for maximizing the provision of ecosystem services supplied by lakes and reservoirs (consumptive and non consumptive uses, food production, and recreation), and for reporting lake status in the EU Water Framework Directive. We also highlight critical issues to enhance the application of AHFM, and suggest the establishment of appropriate networks to facilitate knowledge sharing and technological transfer between potential users. Finally, we give advice on how modern sensor technology can successfully be applied on a larger scale to the management of lakes and reservoirs and maximize the ecosystem services they provide.
- Published
- 2016
34. Drought-induced discontinuities in the source and degradation of dissolved organic matter in a Mediterranean river
- Author
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Casas-Ruiz, J.P., Tittel, Jörg, von Schiller, D., Catalan, N., Obrador, B., Gómez-Gener, L., Zwirnmann, E., Sabater, S., Marcé, R., Casas-Ruiz, J.P., Tittel, Jörg, von Schiller, D., Catalan, N., Obrador, B., Gómez-Gener, L., Zwirnmann, E., Sabater, S., and Marcé, R.
- Abstract
The composition of dissolved organic matter (DOM) in rivers results from the different sources and in-stream transformations along the land to ocean aquatic continuum. Riverine DOM sources are highly dependent on the hydrological connection between the river channel and the surrounding terrestrial ecosystems, but how the lack of this connectivity (e.g., during drought episodes) affects the sources and biodegradation of DOM in rivers remains unclear. Here we identified the DOM sources as well as the different DOM pools that are respired along a Mediterranean river during drought by combining absorbance-fluorescence spectroscopy, size-exclusion chromatography, biodegradation assays, and stable and radiocarbon isotopes. DOM composition was highly heterogeneous along the river in response to different sources and in-stream processes in each distinct aquatic environment (i.e., isolated water pools, running waters, and impounded waters in weirs). The reduced hydrological connectivity with terrestrial ecosystems promoted the influence of autochthonous DOM sources. Still, tree leaves from overhanging canopies stood out as an important terrestrial DOM source, especially in sites where water residence time was high such as isolated pools and weirs. Degradation of leaf leachates was a relevant process in these sites, whereas autochthonous DOM and groundwater millennial DOM (>1300 year B.P.) seemed to be degraded in running waters. Overall, our results highlight that the drought-induced hydrological disconnection entails a great spatial heterogeneity in the sources of DOM, which at the same time determines the different DOM pools that are respired in each environment along the river.
- Published
- 2015
35. Hot spots for carbon emissions from Mediterranean fluvial networks during summer drought
- Author
-
Gómez-Gener, L., Obrador, B., von Schiller, D., Marcé, R., Casas-Ruiz, J.P., Proia, L., Acuña, V., Catalán, N., Muñoz, I., Koschorreck, Matthias, Gómez-Gener, L., Obrador, B., von Schiller, D., Marcé, R., Casas-Ruiz, J.P., Proia, L., Acuña, V., Catalán, N., Muñoz, I., and Koschorreck, Matthias
- Abstract
During summer drought, Mediterranean fluvial networks are transformed into highly heterogeneous landscapes characterized by different environments (i.e., running and impounded waters, isolated river pools and dry beds). This hydrological setting defines novel biogeochemically active areas that could potentially increase the rates of carbon emissions from the fluvial network to the atmosphere. Using chamber methods, we aimed to identify hot spots for carbon dioxide (CO2) and methane (CH4) emissions from two typical Mediterranean fluvial networks during summer drought. The CO2 efflux from dry beds (mean ± SE = 209 ± 10 mmol CO2 m−2 d−1) was comparable to that from running waters (120 ± 33 mmol m−2 d−1) and significantly higher than from impounded waters (36.6 ± 8.5 mmol m−2 d−1) and isolated pools (17.2 ± 0.9 mmol m−2 d−1). In contrast, the CH4 efflux did not significantly differ among environments, although the CH4 efflux was notable in some impounded waters (13.9 ± 10.1 mmol CH4 m−2 d−1) and almost negligible in the remaining environments (mean <0.3 mmol m−2 d−1). Diffusion was the only mechanism driving CO2 efflux in all environments and was most likely responsible for CH4 efflux in running waters, isolated pools and dry beds. In contrast, the CH4 efflux in impounded waters was primarily ebullition-based. Using a simple heuristic approach to simulate potential changes in carbon emissions from Mediterranean fluvial networks under future hydrological scenarios, we show that an extreme drying out (i.e., a four-fold increase of the surface area of dry beds) would double the CO2 efflux from the fluvial network. Correspondingly, an extreme transformation of running waters into impounded waters (i.e., a twofold increase of the surface area of impounded
- Published
- 2015
36. Fluxos de carboni a les basses temporals de l’illa de Menorca
- Author
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Obrador, B., Catalan, N., Marcé, R., von Schiller, D., Koschorreck, Matthias, Gómez-Gener, L., Obrador, B., Catalan, N., Marcé, R., von Schiller, D., Koschorreck, Matthias, and Gómez-Gener, L.
- Abstract
En aquest estudi, s’han quantificat els fluxos de carboni en diferents basses temporals de l’illa de Menorca. Les basses s’han comportat com a emissores de diòxid de carboni (CO2) cap a l’atmosfera durant totes les fases del cicle hidrològic, amb fluxos de CO2 comparables als de sistemes lacustres no temporals, si bé els fluxos de metà són de menor importància. Destaca l’important paper de la fase seca d’aquests sistemes com a emissora de CO2. Les seccions no inundades de les basses han mostrat una elevada activitat de processament de carboni, emetent CO2 a intensitats significativament superiors a les observades des de la columna d’aigua.In this study, we evaluated the carbon fluxes in a set of temporary ponds in the island of Menorca. The ponds were net emitters of carbon dioxide (CO2) towards the atmosphere during the different phases of their hydrologic cycles. The measured CO2 fluxes were comparable to those from non-temporary lacustrinesystems, although methane presented lower values. We stress the relevant role of the dry phase of these systems as a net CO2 emitter. The non-flooded sections of the ponds showed a strong carbon processing activity, emitting CO2 at significantly higher intensity than the water column.
- Published
- 2015
37. Five-year follow-up of patients with chronic C hepatitis and sustained virological response
- Author
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Puig-del-Castillo, I., Miquel-Planas, M., Vergara-Gómez, M., Cebollero-Agustí, A., Gallach-Montero, M., Dalmau-Obrador, B., Gil-Prades, M., Casas-Rodrigo, M., Sánchez-Delgado, J., Tomás-Tutusaus, R., and Gavarró-Puig, A.
- Subjects
Chronic C hepatitis ,Ribavirin ,Ribavirina ,Pegylated interferon alfa-2a ,Interferón pegilado alfa-2a ,Pegylated interferon alfa-2b ,Interferón pegilado alfa-2b ,Hepatitis crónica C - Abstract
Objective: to assess persistence of sustained viral response at 5 years of follow-up in patients with chronic viral hepatitis C treated with pegylated interferon and ribavirin. Design: a descriptive study. Patients: from August 2001 to May 2004, all patients treated at our center with pegylated interferon and ribavirin who achieved a sustained viral response were consecutively enrolled (93 patients). Demographic, histological, biochemical, and virological data were collected during treatment and 5 years after achievement of the sustained viral response. Eighty-six percent of patients enrolled (n = 80) attended the control visit at 5 years. Results: mean age of enrolled patients was 41 years (standard deviation = 10 years), and 30.1% (n = 28) were women. Liver biopsy had been performed before treatment in 68.8% of patients (n = 64), showing no or mild fibrosis in 62.3% (F0 and F1) and significant fibrosis and cirrhosis in 37.7% (F ≥ 3). Genotype distribution was: 58.1% genotype 1 (n = 54); 8.6% genotype 2 (n = 8); 24.7% genotype 3 (n = 23); 7.5% genotype 4 (n = 7), and indeterminate in one patient. Only one patient experienced virological recurrence. All other patients had negative HCV RNA levels and, in the absence of other liver diseases, normal ALT levels. Conclusion: in patients treated with pegylated interferon and ribavirin with sustained viral response, long-term recurrence rate was very low. Objetivo: evaluar la persistencia de respuesta viral sostenida a los 5 años de seguimiento en pacientes con hepatitis crónica por virus C tratados con interferón pegilado y ribavirina. Diseño: estudio descriptivo. Pacientes: desde agosto de 2001 hasta mayo de 2004, se incluyeron de forma consecutiva todos los pacientes de nuestro centro tratados con interferón pegilado y ribavirina que alcanzaron respuesta viral sostenida (93 pacientes). Se recogieron datos demográficos, histológicos, bioquímicos y virológicos durante el tratamiento y a los 5 años de haber obtenido la respuesta viral sostenida. Se presentaron a la visita de control a los 5 años un 86% de los pacientes incluidos (n = 80). Resultados: los pacientes incluidos presentaron una edad media de 41 años (desviación estándar = 10 años); mujeres 30,1% (n = 28). En el 68,8% de los pacientes (n=64) se había realizado biopsia hepática previa al tratamiento, que mostraba ausencia de fibrosis o fibrosis leve en un 62,3% (F0 y F1) y fibrosis significativa o cirrosis en un 37,7% (F≥3). La distribución por genotipos fue: 58,1% genotipo 1 (n = 54); 8,6% genotipo 2 (n = 8); 24,7% genotipo 3 (n = 23); 7,5% genotipo 4 (n = 7) e indeterminado en un caso. Sólo uno de los pacientes presentó recurrencia virológica. El resto de pacientes presentaron niveles de ARN-VHC negativo y, en ausencia de otra hepatopatía, niveles de ALT normales. Conclusión: en pacientes tratados con interferón pegilado y ribavirina con respuesta viral sostenida la tasa de recurrencia a largo plazo es muy baja.
- Published
- 2011
38. The genus Ruppia L. (Ruppiaceae) in the Mediterranean region: An overview
- Author
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Mannino, Anna M., primary, Menéndez, M., additional, Obrador, B., additional, Sfriso, A., additional, and Triest, L., additional
- Published
- 2015
- Full Text
- View/download PDF
39. Carbon dioxide efflux during the flooding phase of temporary ponds. Flujos de dióxido de carbono durante la fase de inundación de estanques temporales
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Catalán, N., von Schiller, D., Marcé, R., Koschorreck, Matthias, Gomez-Gener, L., Obrador, B., Catalán, N., von Schiller, D., Marcé, R., Koschorreck, Matthias, Gomez-Gener, L., and Obrador, B.
- Abstract
Small water bodies, such as temporary ponds, have a high carbon processing potential. Nevertheless, despite the global occurrence of these systems, the carbon effluxes from such water bodies have been largely overlooked. In this study, we examined the intra- and intersystem variability of carbon dioxide (CO2) effluxes from a set of Mediterranean temporary ponds during the flooding phase, a hot-spot for biogeochemical cycling in temporary systems. The CO2 effluxes showed higher variability among the various sections of each pond (i.e., inundated, emerged-unvegetated and emerged-vegetated) than among the ponds. The emerged-vegetated sections showed the highest CO2 effluxes per unit area and tended to drive the total effluxes at the whole-ecosystem scale. The mean CO2 efflux (121.3 ± 138.1 mmol m–2 d–1) was in the upper range for freshwater ecosystems. The CO2 effluxes were not related to catchment properties but rather to the organic content of the sediments, especially in the emerged sections of the ponds. Our results indicate that temporary ponds, especially their emerged sections, are important sources of CO2 to the atmosphere, highlighting the need to include the dry phases of these and other temporary aquatic systems in regional carbon budgets.Los pequeños cuerpos de agua como los estanques temporales tienen un elevado potencial para procesar carbono. Sin embargo, a pesar de su presencia global, los flujos de carbono procedentes de estos sistemas han sido muy poco estudiados. En el presente trabajo, se estudió la variabilidad intra- e inter-sistémica de los flujos de dióxido de carbono (CO2) en un conjunto de estanques temporales mediterráneos durante su fase de inundación, un momento en que los ciclos biogeoquímicos en sistemas temporales se intensifican. Las emisiones de CO2 presentaron una mayor variabilidad entre las diferentes secciones dentro de cada estanque (es decir, inundada, emergida-sin vegetación y emergida-vegetada) que entre los diferentes estanque
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- 2014
40. Carbon dioxide emissions from dry watercourses
- Author
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von Schiller, D., Marcé, R., Obrador, B., Gómez-Gener, L., Casas-Ruiz, J.P., Acuña, V., Koschorreck, Matthias, von Schiller, D., Marcé, R., Obrador, B., Gómez-Gener, L., Casas-Ruiz, J.P., Acuña, V., and Koschorreck, Matthias
- Abstract
Temporary watercourses that naturally cease to flow and run dry comprise a notable fraction of the world’s river networks, yet estimates of global carbon dioxide (CO2) emissions from watercourses do not consider emissions from these systems when they are dry. Using data from a sampling campaign in a Mediterranean river during the summer drought period, we demonstrate that the CO2 efflux from dry watercourses can be substantial, comparable to that from adjacent terrestrial soils and higher than from running or stagnant waters. With an up-scaling approach, we show that including emissions from dry watercourses could increase the estimate of CO2 emissions from watercourses in our study region by 0.6–15%. Moreover, our results tentatively illustrate that emissions from dry watercourses could beespecially important in arid regions, increasing the estimate of global CO2 emissions from watercourses by 0.4–9%. Albeit relatively small, the contribution of dry watercourses could help to constrain the highly uncertain magnitude of the land carbon sink. We foresee that in many areas of the world, the expected increase in the extent of temporary watercourses associated with future global change will increase the relevance of CO2 emissions from dry watercourses.
- Published
- 2014
41. Five-year follow-up of patients with chronic C hepatitis and sustained virological response
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Puig-del-Castillo, I., primary, Miquel-Planas, M., additional, Vergara-Gómez, M., additional, Cebollero-Agustí, A., additional, Gallach-Montero, M., additional, Dalmau-Obrador, B., additional, Gil-Prades, M., additional, Casas-Rodrigo, M., additional, Sánchez-Delgado, J., additional, Tomás-Tutusaus, R., additional, and Gavarró-Puig, A., additional
- Published
- 2011
- Full Text
- View/download PDF
42. Diagnóstico y tratamiento de la encefalopatía hepática en España: resultados de una encuesta dirigida a hepatólogos
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Vergara-Gómez, M., primary, Flavià-Olivella, M., additional, Gil-Prades, M., additional, Dalmau-Obrador, B., additional, and Córdoba-Cardona, J., additional
- Published
- 2006
- Full Text
- View/download PDF
43. Sediment respiration pulses in intermittent rivers and ephemeral streams
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von Schiller, D., Datry, T., Corti, R., Foulquier, A., Tockner, K., Marcé, R., García-Baquero, G., Odriozola, I., Obrador, B., Elosegi, A., Mendoza‐Lera, C., Gessner, M. O., Stubbington, R., Albariño, R., Allen, D. C., Altermatt, F., Arce, M. I., Arnon, S., Banas, D., Banegas‐Medina, A., Beller, E., Blanchette, Melanie L., Blanco‐Libreros, J. F., Blessing, J., Boëchat, I. G., Boersma, K. S., Bogan, M. T., Bonada, N., Bond, N. R., Brintrup, K., Bruder, A., Burrows, R. M., Cancellario, T., Carlson, S. M., Cauvy‐Fraunié, S., Cid, N., Danger, M., de Freitas Terra, B., Dehedin, A., De Girolamo, A. M., del Campo, R., Díaz‐Villanueva, V., Duerdoth, C. P., Dyer, F., Faye, E., Febria, C., Figueroa, R., Four, B., Gafny, S., Gómez, R., Gómez‐Gener, L., Graça, M. A. S., Guareschi, S., Gücker, B., Hoppeler, F., Hwan, J. L., Kubheka, S., Laini, A., Langhans, S. D., Leigh, C., Little, C. J., Lorenz, S., Marshall, J., Martín, E. J., McIntosh, A., Meyer, E. I., Miliša, M., Mlambo, M. C., Moleón, M., Morais, M., Negus, P., Niyogi, D., Papatheodoulou, A., Pardo, I., Pařil, P., Pešić, V., Piscart, C., Polášek, M., Rodríguez‐Lozano, P., Rolls, R. J., Sánchez‐Montoya, M. M., Savić, A., Shumilova, O., Steward, A., Taleb, A., Uzan, A., Vander Vorste, R., Waltham, N., Woelfle‐Erskine, C., Zak, D., Zarfl, C., Zoppini, A., von Schiller, D., Datry, T., Corti, R., Foulquier, A., Tockner, K., Marcé, R., García-Baquero, G., Odriozola, I., Obrador, B., Elosegi, A., Mendoza‐Lera, C., Gessner, M. O., Stubbington, R., Albariño, R., Allen, D. C., Altermatt, F., Arce, M. I., Arnon, S., Banas, D., Banegas‐Medina, A., Beller, E., Blanchette, Melanie L., Blanco‐Libreros, J. F., Blessing, J., Boëchat, I. G., Boersma, K. S., Bogan, M. T., Bonada, N., Bond, N. R., Brintrup, K., Bruder, A., Burrows, R. M., Cancellario, T., Carlson, S. M., Cauvy‐Fraunié, S., Cid, N., Danger, M., de Freitas Terra, B., Dehedin, A., De Girolamo, A. M., del Campo, R., Díaz‐Villanueva, V., Duerdoth, C. P., Dyer, F., Faye, E., Febria, C., Figueroa, R., Four, B., Gafny, S., Gómez, R., Gómez‐Gener, L., Graça, M. A. S., Guareschi, S., Gücker, B., Hoppeler, F., Hwan, J. L., Kubheka, S., Laini, A., Langhans, S. D., Leigh, C., Little, C. J., Lorenz, S., Marshall, J., Martín, E. J., McIntosh, A., Meyer, E. I., Miliša, M., Mlambo, M. C., Moleón, M., Morais, M., Negus, P., Niyogi, D., Papatheodoulou, A., Pardo, I., Pařil, P., Pešić, V., Piscart, C., Polášek, M., Rodríguez‐Lozano, P., Rolls, R. J., Sánchez‐Montoya, M. M., Savić, A., Shumilova, O., Steward, A., Taleb, A., Uzan, A., Vander Vorste, R., Waltham, N., Woelfle‐Erskine, C., Zak, D., Zarfl, C., and Zoppini, A.
- Abstract
von Schiller, D., Datry, T., Corti, R., Foulquier, A., Tockner, K., Marcé, R., ... Zoppini, A. (2019). Sediment respiration pulses in intermittent rivers and ephemeral streams. Global Biogeochemical Cycles, 33(10), 1251-1263. Available here
44. Temperature effects explain continental scale distribution of cyanobacterial toxins
- Author
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Sigrid Haande, Christos Avagianos, Vítor Gonçalves, Lisette N. de Senerpont Domis, Carlos Rochera, Ana García-Murcia, Kerstin Häggqvist, Reyhan Akçaalan, Jordi Noguero-Ribes, Mariusz Pełechaty, Wojciech Krztoń, Hans-Peter Grossart, Jutta Fastner, Bárbara Úbeda, Wojciech Pęczuła, Nur Filiz, Justyna Kobos, Juan M. Soria, Elif Neyran Soylu, Lars-Anders Hansson, Filip Stević, Luděk Bláha, Hanna Mazur-Marzec, Jolanda M. H. Verspagen, Burçin Önem, Karl-Otto Rothhaupt, Nico Salmaso, Abdulkadir Yağcı, David Parreño Duque, Ksenija Savadova, Nusret Karakaya, Aleksandra Pełechata, Yvon Verstijnen, Carmen Pérez-Martínez, Pauliina Salmi, Gizem Bezirci, Tuğba Ongun Sevindik, Svetislav Krstić, Rahmi Uysal, Laura Seelen, Eloísa Ramos-Rodríguez, Spela Remec-Rekar, Sven Teurlincx, Monserrat Real, Meriç Albay, Donald C. Pierson, Susana Romo, Kristiina Mustonen, Kirsten Christoffersen, Valentini Maliaka, Estela Rodríguez-Pérez, Joanna Rosińska, Nilsun Demir, Mehmet Tahir Alp, Elvira Romans, João Morais, Daniel Szymański, Danielle Machado-Vieira, Damian Chmura, Evanthia Mantzouki, Teresa Vegas-Vilarrúbia, Antonio Picazo, Mikołaj Kokociński, Anastasia Hiskia, Christine Edwards, Yang Yang, Irma Vitonytė, Mehmet Cesur, Agnieszka Bańkowska-Sobczak, Iwona Kostrzewska-Szlakowska, Nikoletta Tsiarta, Anđelka Plenković-Moraj, Miquel Lürling, Ryszard Gołdyn, Kristel Panksep, Kemal Celik, Anna Kozak, Jose Luis Cereijo, Pablo Urrutia-Cordero, Petra M. Visser, Rodan Geriš, Uğur Işkın, Leonardo Cerasino, Kadir Çapkın, Victor C. Perello, Carmen Cillero-Castro, Arda Özen, Manel Leira, Enrique Moreno-Ostos, Şakir Çinar, Agnieszka Budzyńska, Faruk Maraşlıoğlu, Pedro M. Raposeiro, Theodoros M. Triantis, Agnieszka Pasztaleniec, Sevasti-Kiriaki Zervou, Elżbieta Wilk-Woźniak, Edward Walusiak, Kersti Kangro, Jorge Juan Montes-Pérez, Triantafyllos Kaloudis, Mari Carmen Trapote, Pablo Alcaraz-Párraga, José María Blanco, Marek Kruk, Hans W. Paerl, Lidia Nawrocka, Meryem Beklioglu, Antonio Camacho, Moritz Buck, Biel Obrador, Ilona Gagala, Lauri Arvola, Elżbieta Szeląg-Wasielewska, Petar Žutinić, Giovanna Flaim, Núria Catalán, R. Carballeira, Alinne Gurjão de Oliveira, Magdalena Frąk, Alo Laas, Magdalena Grabowska, Dubravka Špoljarić Maronić, Meral Apaydın Yağcı, Itana Bokan Vucelić, Ana Maria Antão-Geraldes, Tõnu Feldmann, Natalia Jakubowska-Krepska, Trine Perlt Warming, Armand Hernández, Anna C. Santamans, Fuat Bilgin, Cayelan C. Carey, Joana Mankiewicz-Boczek, Elísabeth Fernández-Morán, Mete Yilmaz, Iwona Jasser, Boris Aleksovski, Michał Wasilewicz, Agnieszka Ochocka, David García, Lea Tuvikene, Roberto L. Palomino, B.W. Ibelings, Hatice Tunca, Birger Skjelbred, Joan Gomà, Jūratė Karosienė, Maria G. Antoniou, Vitor Vasconcelos, Mehmet Ali Turan Koçer, Eti E. Levi, Markéta Fránková, Beata Madrecka, Barbara Pawlik-Skowrońska, Jeremy Fonvielle, Korhan Özkan, Maciej Karpowicz, Özden Fakioglu, Lucia Chomova, Magdalena Toporowska, Ülkü Nihan Tavşanoğlu, Jūratė Kasperovičienė, Latife Köker, Kinga Kwasizur, Koray Ozhan, Valeriano Rodríguez, William Colom-Montero, Ulrike Obertegger, Micaela Vale, Spyros Gkelis, Michał Niedźwiecki, Tunay Karan, Piotr Domek, Judita Koreivienė, Andrea G. Bravo, Justyna Sieńska, Jessica Richardson, Hana Nemova, Cafer Bulut, Jordi Delgado-Martín, Tanja Žuna Pfeiffer, Marija Gligora Udovič, Manthos Panou, Dietmar Straile, Rafael Marcé, Valerie McCarthy, Iveta Drastichova, Agnieszka Napiórkowska-Krzebietke, J. A. Gálvez, Tina Elersek, Beata Messyasz, Adriano Boscaini, Carmen Ferriol, Julita Dunalska, Freshwater and Marine Ecology (IBED, FNWI), BAİBÜ, Mühendislik Fakültesi, Çevre Mühendisliği Bölümü, Karakaya, Nusret, Universitat de Barcelona, Fakülteler, Fen - Edebiyat Fakültesi, Biyoloji Bölümü, Soylu, Elif Neyran, European Cooperation in Science and Technology, Université de Genève, Tokat Gaziosmanpaşa Üniversitesi, Lammi Biological Station, Doctoral Programme in Atmospheric Sciences, CIIMAR - Centro Interdisciplinar de Investigação Marinha e Ambiental, Yılmaz, Mete, Institute of Agricultural and Environmental Sciences, Mantzouki, Evanthia, Ibelings, Bastiaan Willem, Mantzouki, E, Lurling, M, Fastner, J, Domis, LD, Wilk-Wozniak, E, Koreiviene, J, Seelen, L, Teurlincx, S, Verstijnen, Y, Krzton, W, Walusiak, E, Karosiene, J, Kasperoviciene, J, Savadova, K, Vitonyte, I, Cillero-Castro, C, Budzynska, A, Goldyn, R, Kozak, A, Rosinska, J, Szelag-Wasielewska, E, Domek, P, Jakubowska-Krepska, N, Kwasizur, K, Messyasz, B, Pelechata, A, Pelechaty, M, Kokocinski, M, Garcia-Murcia, A, Real, M, Romans, E, Noguero-Ribes, J, Duque, DP, Fernandez-Moran, E, Karakaya, N, Haggqvist, K, Demir, N, Beklioglu, M, Filiz, N, Levi, EE, Iskin, U, Bezirci, G, Tavsanoglu, UN, Ozhan, K, Gkelis, S, Panou, M, Fakioglu, O, Avagianos, C, Kaloudis, T, Celik, K, Yilmaz, M, Marce, R, Catalan, N, Bravo, AG, Buck, M, Colom-Montero, W, Mustonen, K, Pierson, D, Yang, Y, Raposeiro, PM, Goncalves, V, Antoniou, MG, Tsiarta, N, McCarthy, V, Perello, VC, Feldmann, T, Laas, A, Panksep, K, Tuvikene, L, Gagala, I, Mankiewicz-Boczek, J, Yagci, MA, Cinar, S, Capkin, K, Yagci, A, Cesur, M, Bilgin, F, Bulut, C, Uysal, R, Obertegger, U, Boscaini, A, Flaim, G, Salmaso, N, Cerasino, L, Richardson, J, Visser, PM, Verspagen, JMH, Karan, T, Soylu, EN, Maraslioglu, F, Napiorkowska-Krzebietke, A, Ochocka, A, Pasztaleniec, A, Antao-Geraldes, AM, Vasconcelos, V, Morais, J, Vale, M, Koker, L, Akcaalan, R, Albay, M, Maronic, DS, Stevic, F, Pfeiffer, TZ, Fonvielle, J, Straile, D, Rothhaupt, KO, Hansson, LA, Urrutia-Cordero, P, Blaha, L, Geris, R, Frankova, M, Kocer, MAT, Alp, MT, Remec-Rekar, S, Elersek, T, Triantis, T, Zervou, SK, Hiskia, A, Haande, S, Skjelbred, B, Madrecka, B, Nemova, H, Drastichova, I, Chomova, L, Edwards, C, Sevindik, TO, Tunca, H, Onem, B, Aleksovski, B, Krstic, S, Vucelic, IB, Nawrocka, L, Salmi, P, Machado-Vieira, D, de Oliveira, AG, Delgado-Martin, J, Garcia, D, Cereijo, JL, Goma, J, Trapote, MC, Vegas-Vilarrubia, T, Obrador, B, Grabowska, M, Karpowicz, M, Chmura, D, Ubeda, B, Galvez, JA, Ozen, A, Christoffersen, KS, Warming, TP, Kobos, J, Mazur-Marzec, H, Perez-Martinez, C, Ramos-Rodriguez, E, Arvola, L, Alcaraz-Parraga, P, Toporowska, M, Pawlik-Skowronska, B, Niedzwiecki, M, Peczula, W, Leira, M, Hernandez, A, Moreno-Ostos, E, Blanco, JM, Rodriguez, V, Montes-Perez, JJ, Palomino, RL, Rodriguez-Perez, E, Carballeira, R, Camacho, A, Picazo, A, Rochera, C, Santamans, AC, Ferriol, C, Romo, S, Soria, JM, Dunalska, J, Sienska, J, Szymanski, D, Kruk, M, Kostrzewska-Szlakowska, I, Jasser, I, Zutinic, P, Udovic, MG, Plenkovic-Moraj, A, Frak, M, Bankowska-Sobczak, A, Wasilewicz, M, Ozkan, K, Maliaka, V, Kangro, K, Grossart, HP, Paerl, HW, Carey, CC, Ibelings, BW, Sakarya Üniversitesi/Fen-Edebiyat Fakültesi/Biyoloji Bölümü, Ongun Sevindik, Tuğba, Tunca, Hatice, Hitit Üniversitesi, Fen Edebiyat Fakültesi, Biyoloji Bölümü, and Fen Edebiyat Fakültesi
- Subjects
light climate ,0106 biological sciences ,thermocline ,Bacterial toxins ,toksiinit ,limit of quantitation ,Toxines bacterianes ,Microcystin-LR ,Toxicology ,01 natural sciences ,Anatoxin-a ,analogs and derivatives ,BLOOMS ,Direct Effects ,uracil ,Water Pollutants ,chemistry.chemical_classification ,Temperatures ,FRESH-WATER ,latitude ,maximum buoyancy frequency ,6. Clean water ,climate change ,Indirect effects ,EUTROPHICATION ,microcystin RR ,articles ,GROWTH ,lämpötila ,LAKES ,microcystin ,anatoxin ,cylindrospermopsin ,temperature ,direct effects ,indirect effects ,spatial distribution ,European Multi Lake Survey ,epilimnetic temperature ,ta1172 ,cyanobacteria, lakes, climate warming, microcystin ,Zoology ,Article ,water pollutant ,MICROCYSTIS-AERUGINOSA ,Alkaloids ,Settore BIO/07 - ECOLOGIA ,NATURAL SCIENCES. Biology ,Spatial distribution ,Microcystis aeruginosa ,Uracil ,lake ,syanobakteerit ,Indirect Effects ,liquid chromatography-mass spectrometry ,1172 Environmental sciences ,Ekologi ,nutrient ,010604 marine biology & hydrobiology ,lcsh:R ,microbiology ,Climatic changes ,microcystin LR ,Anatoxin ,Lakes ,Spatial Distribution ,chemistry ,nodularin ,microbial diversity ,phytoplankton ,ta1181 ,Cylindrospermopsin ,Tropanes ,Cyanobacteria ,Aquatic Ecology and Water Quality Management ,analysis ,Health, Toxicology and Mutagenesis ,lcsh:Medicine ,environmental parameters ,010501 environmental sciences ,medicine.disease_cause ,nitrogen ,chemistry.chemical_compound ,sea surface temperature ,environmental factor ,ddc:550 ,Canvi climàtic ,phosphorus ,PRIRODNE ZNANOSTI. Biologija ,limit of detection ,Ecology ,Cyanobacteria Toxins ,biology ,Temperature ,levinneisyys ,Nodularin ,tropane derivative ,Europe ,DAPHNIA-MAGNA ,İndirect Effects ,Direct effects ,microbial community ,Environmental Monitoring ,high performance liquid chromatography ,Microcystins ,Climate Change ,Bacterial Toxins ,Microcystin ,välittömät oikeusvaikutukset ,cyanobacterium ,ddc:570 ,geographic distribution ,medicine ,bacterial toxin ,controlled study ,ddc:610 ,Institut für Biochemie und Biologie ,0105 earth and related environmental sciences ,nonhuman ,WIMEK ,Toxin ,longitude ,PHYTOPLANKTON ASSEMBLAGES ,Aquatic Ecology ,NITROGEN AVAILABILITY ,anatoxin a ,Aquatische Ecologie en Waterkwaliteitsbeheer ,biology.organism_classification ,Climatic change ,CLIMATE ,13. Climate action ,response variable ,Canvis climàtics - Abstract
Insight into how environmental change determines the production and distribution of cyanobacterial toxins is necessary for risk assessment. Management guidelines currently focus on hepatotoxins (microcystins). Increasing attention is given to other classes, such as neurotoxins (e.g., anatoxin-a) and cytotoxins (e.g., cylindrospermopsin) due to their potency. Most studies examine the relationship between individual toxin variants and environmental factors, such as nutrients, temperature and light. In summer 2015, we collected samples across Europe to investigate the effect of nutrient and temperature gradients on the variability of toxin production at a continental scale. Direct and indirect effects of temperature were the main drivers of the spatial distribution in the toxins produced by the cyanobacterial community, the toxin concentrations and toxin quota. Generalized linear models showed that a Toxin Diversity Index (TDI) increased with latitude, while it decreased with water stability. Increases in TDI were explained through a significant increase in toxin variants such as MC-YR, anatoxin and cylindrospermopsin, accompanied by a decreasing presence of MC-LR. While global warming continues, the direct and indirect effects of increased lake temperatures will drive changes in the distribution of cyanobacterial toxins in Europe, potentially promoting selection of a few highly toxic species or strains. © 2018 by the authors. Licensee MDPI, Basel, Switzerland., The authors acknowledge COST Action ES 1105 “CYANOCOST—Cyanobacterial blooms and toxins in water resources: Occurrence impacts and management” and COST Action ES 1201 “NETLAKE—Networking Lake Observatories in Europe” for contributing to this study through networking and knowledge sharing with European experts in the field. Evanthia Mantzouki was supported by a grant from the Swiss State Secretariat for Education, Research and Innovation (SERI) to Bas Ibelings and by supplementary funding from the University of Geneva. We thank Clare Ahnlund, Ena Suarez and Irene Gallego for helping out with the Swiss survey. We thank Wendy Beekman and Els J. Faassen for the nutrient and toxin analysis.
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- 2018
45. Data Descriptor: A European Multi Lake Survey dataset of environmental variables, phytoplankton pigments and cyanotoxins
- Author
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Tunca, Hatice, Mantzouki, E, Campbell, J, van Loon, E, Visser, P, Konstantinou, I, Antoniou, M, Giuliani, G, Machado-Vieira, D, de Oliveira, AG, Maronic, DS, Stevic, F, Pfeiffer, TZ, Vucelic, IB, Zutinic, P, Udovic, MG, Plenkovic-Moraj, A, Tsiarta, N, Blaha, L, Geris, R, Frankova, M, Christoffersen, KS, Warming, TP, Feldmann, T, Laas, A, Panksep, K, Tuvikene, L, Kangro, K, Haggqvist, K, Salmi, P, Arvola, L, Fastner, J, Straile, D, Rothhaupt, KO, Fonvielle, J, Grossart, HP, Avagianos, C, Kaloudis, T, Triantis, T, Zervou, SK, Hiskia, A, Gkelis, S, Panou, M, McCarthy, V, Perello, VC, Obertegger, U, Boscaini, A, Flaim, G, Salmaso, N, Cerasino, L, Koreiviene, J, Karosiene, J, Kasperoviciene, J, Savadova, K, Vitonyte, I, Haande, S, Skjelbred, B, Grabowska, M, Karpowicz, M, Chmura, D, Nawrocka, L, Kobos, J, Mazur-Marzec, H, Alcaraz-Parraga, P, Wilk-Wozniak, E, Krzton, W, Walusiak, E, Gagala, I, Mankiewicz-Boczek, J, Toporowska, M, Pawlik-Skowronska, B, Niedzwiecki, M, Peczula, W, Napiorkowska-Krzebietke, A, Dunalska, J, Sienska, J, Szymanski, D, Kruk, M, Budzynska, A, Goldyn, R, Kozak, A, Rosinska, J, Szelag-Wasielewska, E, Domek, P, Jakubowska-Krepska, N, Kwasizur, K, Messyasz, B, Pelechata, A, Pelechaty, M, Kokocinski, M, Madrecka, B, Kostrzewska-Szlakowska, I, Frak, M, Bankowska-Sobczak, A, Wasilewicz, M, Ochocka, A, Pasztaleniec, A, Jasser, I, Antao-Geraldes, AM, Leira, M, Hernandez, A, Vasconcelos, V, Morais, J, Vale, M, Raposeiro, PM, Goncalves, V, Aleksovski, B, Krstic, S, Nemova, H, Drastichova, I, Chomova, L, Remec-Rekar, S, Elersek, T, Delgado-Martin, J, Garcia, D, Cereijo, JL, Goma, J, Trapote, MC, Vegas-Vilarrubia, T, Obrador, B, Garcia-Murcia, A, Real, M, Romans, E, Noguero-Ribes, J, Duque, DP, Fernandez-Moran, E, Ubeda, B, Galvez, JA, Marce, R, Catalan, N, Perez-Martinez, C, Ramos-Rodriguez, E, Cillero-Castro, C, Moreno-Ostos, E, Blanco, JM, Rodriguez, V, Montes-Perez, JJ, Palomino, RL, Rodriguez-Perez, E, Carballeira, R, Camacho, A, Picazo, A, Rochera, C, Santamans, AC, Ferriol, C, Romo, S, Soria, JM, Hansson, LA, Urrutia-Cordero, P, Ozen, A, Bravo, AG, Buck, M, Colom-Montero, W, Mustonen, K, Pierson, D, Yang, Y, Verspagen, JMH, Domis, LND, Seelen, L, Teurlincx, S, Verstijnen, Y, Lurling, M, Maliaka, V, Faassen, EJ, Latour, D, Carey, CC, Paerl, HW, Torokne, A, Karan, T, Demir, N, Beklioglu, M, Filiz, N, Levi, EE, Iskin, U, Bezirci, G, Tavsanoglu, UN, Celik, K, Ozhan, K, Karakaya, N, Kocer, MAT, Yilmaz, M, Maraslioglu, F, Fakioglu, O, Soylu, EN, Yagci, MA, Cinar, S, Capkin, K, Yagci, A, Cesur, M, Bilgin, F, Bulut, C, Uysal, R, Koker, L, Akcaalan, R, Albay, M, Alp, MT, Ozkan, K, Sevindik, TO, Tunca, H, Onem, B, Richardson, J, Edwards, C, Bergkemper, V, O'Leary, S, Beirne, E, Cromie, H, Ibelings, BW, Sakarya Üniversitesi/Fen-Edebiyat Fakültesi/Biyoloji Bölümü, and Tunca, Hatice
- Subjects
Science & Technology - Other Topics - Abstract
Under ongoing climate change and increasing anthropogenic activity, which continuously challenge ecosystem resilience, an in-depth understanding of ecological processes is urgently needed. Lakes, as providers of numerous ecosystem services, face multiple stressors that threaten their functioning. Harmful cyanobacterial blooms are a persistent problem resulting from nutrient pollution and climate-change induced stressors, like poor transparency, increased water temperature and enhanced stratification. Consistency in data collection and analysis methods is necessary to achieve fully comparable datasets and for statistical validity, avoiding issues linked to disparate data sources. The European Multi Lake Survey (EMLS) in summer 2015 was an initiative among scientists from 27 countries to collect and analyse lake physical, chemical and biological variables in a fully standardized manner. This database includes in-situ lake variables along with nutrient, pigment and cyanotoxin data of 369 lakes in Europe, which were centrally analysed in dedicated laboratories. Publishing the EMLS methods and dataset might inspire similar initiatives to study across large geographic areas that will contribute to better understanding lake responses in a changing environment.
- Published
- 2018
46. The genus Ruppia L. (Ruppiaceae) in the Mediterranean region: An overview
- Author
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Margarita Menéndez, Anna Maria Mannino, Biel Obrador, Adriano Sfriso, Ludwig Triest, Biology, General Botany and Nature Management, Mannino, AM, Menéndez, M, Obrador, B, Sfriso, A, and Triest, L
- Subjects
Settore BIO/07 - Ecologia ,Mediterranean climate ,Ruppia ,Aquatic angiosperms ,Brackish water ,Ecology ,Settore BIO/02 - Botanica Sistematica ,Overview ,Shallow waters ,Plant Science ,Aquatic Science ,Biology ,biology.organism_classification ,Habitat ,Genus ,Aquatic plant ,Ruppia cirrhosa ,Botany ,Aquatic angiosperms, Ruppia, Shallow waters, Mediterranean region, Overview ,Mediterranean region ,Ruppia maritima - Abstract
This paper reviews the current knowledge on the diversity, distribution and ecology of the genus Ruppia L. in the Mediterranean region. The genus Ruppia, a cosmopolitan aquatic plant complex, is generally restricted to shallow waters such as coastal lagoons and brackish habitats characterized by fine sediments and high salinity fluctuations. In these habitats Ruppia meadows play an important structural and functional role. Molecular analyses revealed the presence of 16 haplotypes in the Mediterranean region, one corresponding to Ruppia maritima L., and the others to various morphological forms of Ruppia cirrhosa (Petagna) Grande, all together referred to as the “R. cirrhosa s.l. complex”, which also includes Ruppia drepanensis Tineo. Populations of hybrid origin between R. maritima and R. cirrhosa and polyploidy have been detected.
- Published
- 2015
47. Multiple drying aspects shape dissolved organic matter composition in intermittent streams.
- Author
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Granados V, Arias-Real R, Gutiérrez-Cánovas C, Obrador B, and Butturini A
- Subjects
- Dissolved Organic Matter, Climate Change, Water, Carbon, Rivers chemistry, Ecosystem
- Abstract
Water availability is a fundamental driver of biogeochemical processing in highly dynamic ecosystems such as intermittent rivers and ephemeral streams (IRES), which are recognized as the most common fluvial ecosystem globally. Because of their global extent, IRES have a remarkable contribution to organic matter processing, which is expected to intensify as climate change and water extraction expand IRES extension. Nevertheless, the effect of the complexity of the drying process on river biogeochemistry remains unclear. This study investigated how drying aspects affect the dissolved organic carbon (DOC) concentration and composition in 35 streams along a wide flow-intermittence gradient in the NE Iberian Peninsula. To do that, four drying aspects: annual drying duration, annual frequency, duration of the last drying event, and time since the last drying event were characterized. Results showed that DOC concentration and the contribution of humic-like compounds were positively associated with intensifying drying conditions. In addition, protein-like compounds decreased over the drying gradient. More specifically, changes in DOC concentration were driven mainly by annual drying duration, whereas annual drying frequency and the duration of the last drying event jointly explained dissolved organic matter composition. These results suggest that the quantity and composition of dissolved organic matter in streams respond differently to the temporal aspects of the drying process. Our study can help to better anticipate changes in organic matter in the context of climate change., Competing Interests: Declaration of competing interest The authors declare no conflict of interest., (Copyright © 2022 The Authors. Published by Elsevier B.V. All rights reserved.)
- Published
- 2022
- Full Text
- View/download PDF
48. Cross-continental importance of CH 4 emissions from dry inland-waters.
- Author
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Paranaíba JR, Aben R, Barros N, Quadra G, Linkhorst A, Amado AM, Brothers S, Catalán N, Condon J, Finlayson CM, Grossart HP, Howitt J, Oliveira Junior ES, Keller PS, Koschorreck M, Laas A, Leigh C, Marcé R, Mendonça R, Muniz CC, Obrador B, Onandia G, Raymundo D, Reverey F, Roland F, Rõõm EI, Sobek S, von Schiller D, Wang H, and Kosten S
- Subjects
- Carbon Dioxide analysis, Lakes, Methane analysis, Nitrous Oxide analysis, Rivers, Greenhouse Gases analysis
- Abstract
Despite substantial advances in quantifying greenhouse gas (GHG) emissions from dry inland waters, existing estimates mainly consist of carbon dioxide (CO
2 ) emissions. However, methane (CH4 ) may also be relevant due to its higher Global Warming Potential (GWP). We report CH4 emissions from dry inland water sediments to i) provide a cross-continental estimate of such emissions for different types of aquatic systems (i.e., lakes, ponds, reservoirs, and streams) and climate zones (i.e., tropical, continental, and temperate); and ii) determine the environmental factors that control these emissions. CH4 emissions from dry inland waters were consistently higher than emissions observed in adjacent uphill soils, across climate zones and in all aquatic systems except for streams. However, the CH4 contribution (normalized to CO2 equivalents; CO2 -eq) to the total GHG emissions of dry inland waters was similar for all types of aquatic systems and varied from 10 to 21%. Although we discuss multiple controlling factors, dry inland water CH4 emissions were most strongly related to sediment organic matter content and moisture. Summing CO2 and CH4 emissions revealed a cross-continental average emission of 9.6 ± 17.4 g CO2 -eq m-2 d-1 from dry inland waters. We argue that increasing droughts likely expand the worldwide surface area of atmosphere-exposed aquatic sediments, thereby increasing global dry inland water CH4 emissions. Hence, CH4 cannot be ignored if we want to fully understand the carbon (C) cycle of dry sediments., Competing Interests: Declaration of competing interest The authors declare that they have no known competing financial interests or personal relationships that could have appeared to influence the work reported in this paper., (Copyright © 2021 Elsevier B.V. All rights reserved.)- Published
- 2022
- Full Text
- View/download PDF
49. The interruption of longitudinal hydrological connectivity causes delayed responses in dissolved organic matter.
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Granados V, Gutiérrez-Cánovas C, Arias-Real R, Obrador B, Harjung A, and Butturini A
- Abstract
Hydrology is the main driver of dissolved organic matter (DOM) dynamics in intermittent rivers and ephemeral streams. However, it is still unclear how the timing and the spatial variation in flow connectivity affect the dynamics of DOM and inorganic solutes. This study focuses on the impact of flow cessation on the temporal and spatial heterogeneity of DOM quantity and quality along an intermittent stream. We monitored a headwater intermittent stream at high spatial and temporal frequencies during a summer drying episode and analysed dissolved organic carbon (DOC) and its spectroscopic properties, inorganic solutes and dissolved CO
2 . The drying period determined the disruption of the fluvial continuum with a recession of stream continuum at a rate of ~60 m/d and the gradual formation of a patched system of isolated pools of different sizes. Our results showed that the period of time that had elapsed since isolated pool formation (CI-days) was an essential factor for understanding how drying shaped the biogeochemistry of the fluvial system. Overall, drying caused a high DOC concentration and an increase in the humic-like fluorescence signal. Additionally, solutes showed contrasting responses to hydrological disconnection. Electrical conductivity, for instance, is a clear "sentinel" of the fragmentation process because it starts to increase before the hydrological disruption occurs. In contrast, DOC, most spectroscopic DOM descriptors and CO2 showed delayed responses of approximately 5-21 days after the formation of isolated pools. Furthermore, the spatial location and volume of each isolated pool seemed to exert a significant impact on most variables. In contrast, the temperature did not follow a clear pattern. These findings indicate that the fragmentation of longitudinal hydrological connectivity does not induce a single biogeochemical response but rather stimulates a set of solute-specific responses that generates a complex biogeochemical mosaic in a single fluvial unit., Competing Interests: Declaration of competing interest All authors agree with the content of the manuscript and approve of its submission to Science of the Total Environment. The authors declare no conflict of interest., (Copyright © 2020 Elsevier B.V. All rights reserved.)- Published
- 2020
- Full Text
- View/download PDF
50. Reuniting biogeochemistry with ecology and evolution.
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Marcé R and Obrador B
- Subjects
- Fresh Water, Plants, Ecology, Photosynthesis
- Published
- 2019
- Full Text
- View/download PDF
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