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19 results on '"Cauvy-Fraunie, S."'

1. Local climate modulates the development of soil nematode communities after glacier retreat

Author

Guerrieri, A, Cantera, I, Marta, S, Bonin, A, Carteron, A, Ambrosini, R, Caccianiga, M, Anthelme, F, Azzoni, R, Almond, P, Alvizgazitua, P, Cauvy-Fraunie, S, Ceballoslievano, J, Chand, P, Chandsharma, M, Clague, J, Cochachinrapre, J, Compostella, C, Cruzencarnacion, R, Dangles, O, Deline, P, Eger, A, Erokhin, S, Franzetti, A, Gielly, L, Gili, F, Gobbi, M, Hagvar, S, Khedim, N, Meneses, R, Peyre, G, Pittino, F, Proietto, A, Rabatel, A, Urseitova, N, Yang, Y, Zaginaev, V, Zerboni, A, Zimmer, A, Taberlet, P, Diolaiuti, G, Poulenard, J, Fontaneto, D, Thuiller, W, Ficetola, G, Guerrieri A., Cantera I., Marta S., Bonin A., Carteron A., Ambrosini R., Caccianiga M., Anthelme F., Azzoni R. S., Almond P., AlvizGazitua P., Cauvy-Fraunie S., CeballosLievano J. L., Chand P., ChandSharma M., Clague J., CochachinRapre J. A., Compostella C., CruzEncarnacion R., Dangles O., Deline P., Eger A., Erokhin S., Franzetti A., Gielly L., Gili F., Gobbi M., Hagvar S., Khedim N., Meneses R. I., Peyre G., Pittino F., Proietto A., Rabatel A., Urseitova N., Yang Y., Zaginaev V., Zerboni A., Zimmer A., Taberlet P., Diolaiuti G. A., Poulenard J., Fontaneto D., Thuiller W., Ficetola G. F., Guerrieri, A, Cantera, I, Marta, S, Bonin, A, Carteron, A, Ambrosini, R, Caccianiga, M, Anthelme, F, Azzoni, R, Almond, P, Alvizgazitua, P, Cauvy-Fraunie, S, Ceballoslievano, J, Chand, P, Chandsharma, M, Clague, J, Cochachinrapre, J, Compostella, C, Cruzencarnacion, R, Dangles, O, Deline, P, Eger, A, Erokhin, S, Franzetti, A, Gielly, L, Gili, F, Gobbi, M, Hagvar, S, Khedim, N, Meneses, R, Peyre, G, Pittino, F, Proietto, A, Rabatel, A, Urseitova, N, Yang, Y, Zaginaev, V, Zerboni, A, Zimmer, A, Taberlet, P, Diolaiuti, G, Poulenard, J, Fontaneto, D, Thuiller, W, Ficetola, G, Guerrieri A., Cantera I., Marta S., Bonin A., Carteron A., Ambrosini R., Caccianiga M., Anthelme F., Azzoni R. S., Almond P., AlvizGazitua P., Cauvy-Fraunie S., CeballosLievano J. L., Chand P., ChandSharma M., Clague J., CochachinRapre J. A., Compostella C., CruzEncarnacion R., Dangles O., Deline P., Eger A., Erokhin S., Franzetti A., Gielly L., Gili F., Gobbi M., Hagvar S., Khedim N., Meneses R. I., Peyre G., Pittino F., Proietto A., Rabatel A., Urseitova N., Yang Y., Zaginaev V., Zerboni A., Zimmer A., Taberlet P., Diolaiuti G. A., Poulenard J., Fontaneto D., Thuiller W., and Ficetola G. F.

Abstract

The worldwide retreat of glaciers is causing a faster than ever increase in ice-free areas that are leading to the emergence of new ecosystems. Understanding the dynamics of these environments is critical to predicting the consequences of climate change on mountains and at high latitudes. Climatic differences between regions of the world could modulate the emergence of biodiversity and functionality after glacier retreat, yet global tests of this hypothesis are lacking. Nematodes are the most abundant soil animals, with keystone roles in ecosystem functioning, but the lack of global-scale studies limits our understanding of how the taxonomic and functional diversity of nematodes changes during the colonization of proglacial landscapes. We used environmental DNA metabarcoding to characterize nematode communities of 48 glacier forelands from five continents. We assessed how different facets of biodiversity change with the age of deglaciated terrains and tested the hypothesis that colonization patterns are different across forelands with different climatic conditions. Nematodes colonized ice-free areas almost immediately. Both taxonomic and functional richness quickly increased over time, but the increase in nematode diversity was modulated by climate, so that colonization started earlier in forelands with mild summer temperatures. Colder forelands initially hosted poor communities, but the colonization rate then accelerated, eventually leveling biodiversity differences between climatic regimes in the long term. Immediately after glacier retreat, communities were dominated by colonizer taxa with short generation time and r-ecological strategy but community composition shifted through time, with increased frequency of more persister taxa with K-ecological strategy. These changes mostly occurred through the addition of new traits instead of their replacement during succession. The effects of local climate on nematode colonization led to heterogeneous but predictable patt

Published
2024

3. The retreat of mountain glaciers since the little ice age: A spatially explicit database

Author

Marta, S, Azzoni, R, Fugazza, D, Tielidze, L, Chand, P, Sieron, K, Almond, P, Ambrosini, R, Anthelme, F, Alviz Gazitua, P, Bhambri, R, Bonin, A, Caccianiga, M, Cauvy-Fraunie, S, Lievano, J, Clague, J, Rapre, J, Dangles, O, Deline, P, Eger, A, Encarnacion, R, Erokhin, S, Franzetti, A, Gielly, L, Gili, F, Gobbi, M, Guerrieri, A, Hagvar, S, Khedim, N, Kinyanjui, R, Messager, E, Morales-Martinez, M, Peyre, G, Pittino, F, Poulenard, J, Seppi, R, Sharma, M, Urseitova, N, Weissling, B, Yang, Y, Zaginaev, V, Zimmer, A, Diolaiuti, G, Rabatel, A, Ficetola, G, Marta S., Azzoni R. S., Fugazza D., Tielidze L., Chand P., Sieron K., Almond P., Ambrosini R., Anthelme F., Alviz Gazitua P., Bhambri R., Bonin A., Caccianiga M., Cauvy-Fraunie S., Lievano J. L. C., Clague J., Rapre J. A. C., Dangles O., Deline P., Eger A., Encarnacion R. C., Erokhin S., Franzetti A., Gielly L., Gili F., Gobbi M., Guerrieri A., Hagvar S., Khedim N., Kinyanjui R., Messager E., Morales-Martinez M. A., Peyre G., Pittino F., Poulenard J., Seppi R., Sharma M. C., Urseitova N., Weissling B., Yang Y., Zaginaev V., Zimmer A., Diolaiuti G. A., Rabatel A., Ficetola G. F., Marta, S, Azzoni, R, Fugazza, D, Tielidze, L, Chand, P, Sieron, K, Almond, P, Ambrosini, R, Anthelme, F, Alviz Gazitua, P, Bhambri, R, Bonin, A, Caccianiga, M, Cauvy-Fraunie, S, Lievano, J, Clague, J, Rapre, J, Dangles, O, Deline, P, Eger, A, Encarnacion, R, Erokhin, S, Franzetti, A, Gielly, L, Gili, F, Gobbi, M, Guerrieri, A, Hagvar, S, Khedim, N, Kinyanjui, R, Messager, E, Morales-Martinez, M, Peyre, G, Pittino, F, Poulenard, J, Seppi, R, Sharma, M, Urseitova, N, Weissling, B, Yang, Y, Zaginaev, V, Zimmer, A, Diolaiuti, G, Rabatel, A, Ficetola, G, Marta S., Azzoni R. S., Fugazza D., Tielidze L., Chand P., Sieron K., Almond P., Ambrosini R., Anthelme F., Alviz Gazitua P., Bhambri R., Bonin A., Caccianiga M., Cauvy-Fraunie S., Lievano J. L. C., Clague J., Rapre J. A. C., Dangles O., Deline P., Eger A., Encarnacion R. C., Erokhin S., Franzetti A., Gielly L., Gili F., Gobbi M., Guerrieri A., Hagvar S., Khedim N., Kinyanjui R., Messager E., Morales-Martinez M. A., Peyre G., Pittino F., Poulenard J., Seppi R., Sharma M. C., Urseitova N., Weissling B., Yang Y., Zaginaev V., Zimmer A., Diolaiuti G. A., Rabatel A., and Ficetola G. F.

Abstract

Most of the world’s mountain glaciers have been retreating for more than a century in response to climate change. Glacier retreat is evident on all continents, and the rate of retreat has accelerated during recent decades. Accurate, spatially explicit information on the position of glacier margins over time is useful for analyzing patterns of glacier retreat and measuring reductions in glacier surface area. This information is also essential for evaluating how mountain ecosystems are evolving due to climate warming and the attendant glacier retreat. Here, we present a non-comprehensive spatially explicit dataset showing multiple positions of glacier fronts since the Little Ice Age (LIA) maxima, including many data from the pre-satellite era. The dataset is based on multiple historical archival records including topographical maps; repeated photographs, paintings, and aerial or satellite images with a supplement of geochronology; and own field data. We provide ESRI shapefiles showing 728 past positions of 94 glacier fronts from all continents, except Antarctica, covering the period between the Little Ice Age maxima and the present. On average, the time series span the past 190 years. From 2 to 46 past positions per glacier are depicted (on average: 7.8).

Published
2021

4. Topsoil organic matter build-up in glacier forelands around the world

Author

Khedim, N, Cecillon, L, Poulenard, J, Barre, P, Baudin, F, Marta, S, Rabatel, A, Dentant, C, Cauvy-Fraunie, S, Anthelme, F, Gielly, L, Ambrosini, R, Franzetti, A, Azzoni, R, Caccianiga, M, Compostella, C, Clague, J, Tielidze, L, Messager, E, Choler, P, Ficetola, G, Khedim N., Cecillon L., Poulenard J., Barre P., Baudin F., Marta S., Rabatel A., Dentant C., Cauvy-Fraunie S., Anthelme F., Gielly L., Ambrosini R., Franzetti A., Azzoni R. S., Caccianiga M. S., Compostella C., Clague J., Tielidze L., Messager E., Choler P., Ficetola G. F., Khedim, N, Cecillon, L, Poulenard, J, Barre, P, Baudin, F, Marta, S, Rabatel, A, Dentant, C, Cauvy-Fraunie, S, Anthelme, F, Gielly, L, Ambrosini, R, Franzetti, A, Azzoni, R, Caccianiga, M, Compostella, C, Clague, J, Tielidze, L, Messager, E, Choler, P, Ficetola, G, Khedim N., Cecillon L., Poulenard J., Barre P., Baudin F., Marta S., Rabatel A., Dentant C., Cauvy-Fraunie S., Anthelme F., Gielly L., Ambrosini R., Franzetti A., Azzoni R. S., Caccianiga M. S., Compostella C., Clague J., Tielidze L., Messager E., Choler P., and Ficetola G. F.

Abstract

Since the last glacial maximum, soil formation related to ice-cover shrinkage has been one major sink of carbon accumulating as soil organic matter (SOM), a phenomenon accelerated by the ongoing global warming. In recently deglacierized forelands, processes of SOM accumulation, including those that control carbon and nitrogen sequestration rates and biogeochemical stability of newly sequestered carbon, remain poorly understood. Here, we investigate the build-up of SOM during the initial stages (up to 410 years) of topsoil development in 10 glacier forelands distributed on four continents. We test whether the net accumulation of SOM on glacier forelands (i) depends on the time since deglacierization and local climatic conditions (temperature and precipitation); (ii) is accompanied by a decrease in its stability and (iii) is mostly due to an increasing contribution of organic matter from plant origin. We measured total SOM concentration (carbon, nitrogen), its relative hydrogen/oxygen enrichment, stable isotopic (13C, 15N) and carbon functional groups (C-H, C=O, C=C) compositions, and its distribution in carbon pools of different thermal stability. We show that SOM content increases with time and is faster on forelands experiencing warmer climates. The build-up of SOM pools shows consistent trends across the studied soil chronosequences. During the first decades of soil development, the low amount of SOM is dominated by a thermally stable carbon pool with a small and highly thermolabile pool. The stability of SOM decreases with soil age at all sites, indicating that SOM storage is dominated by the accumulation of labile SOM during the first centuries of soil development, and suggesting plant carbon inputs to soil (SOM depleted in nitrogen, enriched in hydrogen and in aromatic carbon). Our findings highlight the potential vulnerability of SOM stocks from proglacial areas to decomposition and suggest that their durability largely depends on the relative contributio

Published
2021

5. Global CO2 emissions from dry inland waters share common drivers across ecosystems

Author

Keller, P. S., Catalan, 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., Paranaiba, J. R., Linkhorst, A., del 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., Gómez-Gener, Lluís, Leigh, C., Zhang, Q., Marce, R., Keller, P. S., Catalan, 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., Paranaiba, J. R., Linkhorst, A., del 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., Gómez-Gener, Lluís, Leigh, C., Zhang, Q., and Marce, 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
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6. Global CO2 emissions from dry inland waters share common drivers across ecosystems

Author

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

7. Une influence glaciaire réduite conditionne la composition et la qualité du périphyton dans les cours d'eau alpins

Author

Niedrist, G.H., Bonnineau, C., Condom, T., Cauvy Fraunie, S., UNIVERSITY OF INNSBRUCK AUT, Partenaires IRSTEA, Institut national de recherche en sciences et technologies pour l'environnement et l'agriculture (IRSTEA)-Institut national de recherche en sciences et technologies pour l'environnement et l'agriculture (IRSTEA), RiverLy (UR Riverly), Institut national de recherche en sciences et technologies pour l'environnement et l'agriculture (IRSTEA), Institut des Géosciences de l’Environnement (IGE), Institut national des sciences de l'Univers (INSU - CNRS)-Centre National de la Recherche Scientifique (CNRS)-Institut polytechnique de Grenoble - Grenoble Institute of Technology (Grenoble INP )-Institut de Recherche pour le Développement (IRD)-Université Grenoble Alpes [2016-2019] (UGA [2016-2019]), and Irstea Publications, Migration

Subjects
[SDE] Environmental Sciences, fungi, [SDE]Environmental Sciences, COURS D'EAU ALPIN
Abstract

International audience; Glacier retreat alters both physical and chemical characteristics of glacially influenced streams, with consequences on the biological communities colonizing these headwaters. While reduced glacial influence is known to alter the structure of alpine stream invertebrate communities, effects on other biotic groups such as primary producers remain poorly quantified. In 68 study sites along a gradient of glacial influence, we characterized both periphyton community structure [biomass and the relative abundance of diatoms (+ chrysophytes), green algae, and cyanobacteria] and functioning (photosynthetic and enzymatic activities), and measured algal growth rate. Using comprehensive data sets from glacier-fed streams in the Eastern and the Western Alps we linked these periphyton features to climate-change associated environmental modifications. In addition to known effects of declining glaciers on algal diversity, we here provide quantitative estimations of periphyton quality and the relative coverage of algal and bacterial groups on streambed surfaces in response to environmental changes. We found, for example, that harsh environmental conditions (e.g., cold water temperatures and high turbidity) favor the dominance of diatoms and chrysophytes within the periphyton, which groups are considered to be of higher nutritional quality for grazing invertebrates when compared to cyanobacteria. These results will thus help to anticipate changes in food resources, and thereby food webs in alpine catchments as response to declining glaciers.

Published
2019

8. Sediment Respiration Pulses in Intermittent Rivers and Ephemeral Streams

Author

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
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9. 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

10. Sediment Respiration Pulses in Intermittent Rivers and Ephemeral Streams

Author

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, MO, Stubbington, R, Albarino, R, Allen, DC, Altermatt, F, Arce, M, Arnon, S, Banas, D, Banegas-Medina, A, Beller, E, Blanchette, ML, Blanco-Libreros, JF, Blessing, J, Boechat, IG, Boersma, KS, Bogan, MT, Bonada, N, Bond, NR, Brintrup, K, Bruder, A, Burrows, RM, Cancellario, T, Carlson, SM, Cauvy-Fraunie, S, Cid, N, Danger, M, de Freitas Terra, B, Dehedin, A, De Girolamo, AM, del Campo, R, Diaz-Villanueva, V, Duerdoth, CP, Dyer, F, Faye, E, Febria, C, Figueroa, R, Four, B, Gafny, S, Gomez, R, Gomez-Gener, L, Graca, MAS, Guareschi, S, Gucker, B, Hoppeler, F, Hwan, JL, Kubheka, S, Laini, A, Langhans, SD, Leigh, C, Little, CJ, Lorenz, S, Marshall, J, Martin, EJ, McIntosh, A, Meyer, E, Milisa, M, Mlambo, MC, Moleon, M, Morais, M, Negus, P, Niyogi, D, Papatheodoulou, A, Pardo, I, Paril, P, Pesic, V, Piscart, C, Polasek, M, Rodriguez-Lozano, P, Rolls, RJ, Sanchez-Montoya, MM, 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, MO, Stubbington, R, Albarino, R, Allen, DC, Altermatt, F, Arce, M, Arnon, S, Banas, D, Banegas-Medina, A, Beller, E, Blanchette, ML, Blanco-Libreros, JF, Blessing, J, Boechat, IG, Boersma, KS, Bogan, MT, Bonada, N, Bond, NR, Brintrup, K, Bruder, A, Burrows, RM, Cancellario, T, Carlson, SM, Cauvy-Fraunie, S, Cid, N, Danger, M, de Freitas Terra, B, Dehedin, A, De Girolamo, AM, del Campo, R, Diaz-Villanueva, V, Duerdoth, CP, Dyer, F, Faye, E, Febria, C, Figueroa, R, Four, B, Gafny, S, Gomez, R, Gomez-Gener, L, Graca, MAS, Guareschi, S, Gucker, B, Hoppeler, F, Hwan, JL, Kubheka, S, Laini, A, Langhans, SD, Leigh, C, Little, CJ, Lorenz, S, Marshall, J, Martin, EJ, McIntosh, A, Meyer, E, Milisa, M, Mlambo, MC, Moleon, M, Morais, M, Negus, P, Niyogi, D, Papatheodoulou, A, Pardo, I, Paril, P, Pesic, V, Piscart, C, Polasek, M, Rodriguez-Lozano, P, Rolls, RJ, Sanchez-Montoya, MM, 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

11. Stratégies d'échantillonnages optimisées en cours d'eau (études long terme, restauration écologique)

Author

Lamouroux, Nicolas, Cauvy Fraunie, S., Vaudor, L., Olivier, J.M., Trenkel, Verena, Maire, A., Forcellini, Maxence, Roset, N., RiverLy (UR Riverly), Institut national de recherche en sciences et technologies pour l'environnement et l'agriculture (IRSTEA), Université Claude Bernard Lyon 1 (UCBL), Université de Lyon, Institut Français de Recherche pour l'Exploitation de la Mer (IFREMER), Risques, Ecosystèmes, Vulnérabilité, Environnement, Résilience (RECOVER), Aix Marseille Université (AMU)-Institut national de recherche en sciences et technologies pour l'environnement et l'agriculture (IRSTEA), Agence Française pour la Biodiversité (AFB), and ANR-11-LABX-0010,DRIIHM / IRDHEI,Dispositif de recherche interdisciplinaire sur les Interactions Hommes-Milieux(2011)

Subjects
ZABR - OBSERVATOIRE OHM VALLEE DU RHONE, education, [SDE]Environmental Sciences, bacteria, equipment and supplies, complex mixtures, health care economics and organizations
Abstract

[Departement_IRSTEA]Eaux [TR1_IRSTEA]QUASARE [ADD1_IRSTEA]Systèmes aquatiques soumis à des pressions multiples; International audience; Optimizing biological monitoring (long-term surveys, restoration assessments) in large rivers and other environments.

Published
2018

12. Optimizing biological monitoring (long-term surveys, restoration assessments) in large rivers and other environments

Author

Lamouroux, N, Cauvy-fraunie, S, Vaudor, L., Olivier, J.m, Trenkel, Verena, Maire, A, Forcellini, M, and Roset, N

Subjects
statistical power analysis, monitoring design, ecological restoration, Abundance time series
Abstract

Studies of the efficiency vs. the cost of long-term biological monitoring strategies are particularly infrequent and needed in large rivers. We used recent studies concerning the long-term monitoring of fish and macroinvertebrates in the Rhône River to discuss the potential and limits of monitoring strategies in large rivers and other environments. A first study is a numerical analysis of the probability to detect changes in fish abundance after flow restoration in the river. A second study concerns the detection of "most expected" relationships in annual fish time series, such as fish cohort follow-ups. It involves a comparison of the Rhône results with those obtained in smaller rivers (where sampling is easier) or in the ocean (where sampling is even more difficult). Results indicate that the long-term biological strategies used in the Rhône River are efficient for detecting major inter-annual trends, but are limited for detecting annual events. Such studies apply to other systems than large rivers and we hope that they will contribute to an increased efficiency and a reduced cost of monitoring strategies., Les études comparant l'efficacité vs. le coût des suivis biologiques de long-terme sont peu fréquentes et particulièrement utiles en grandes rivières. Nous nous basons sur des analyses récentes des données collectées dans le cadre des suivis de poissons et de macroinvertébrés du fleuve Rhône pour discuter du potentiel et des limites des stratégies d'échantillonnage mise en place en grands fleuves et dans d'autres milieux. Une première étude concerne une analyse numérique de la probabilité de détecter des changements d'abondance (poissons, invertébrés) après des mesures de restauration des débits à l'aval des barrages. Une seconde étude concerne la détection des patterns les plus attendus dans les séries annuelles d'abondance de poissons, comme les suivis de cohortes. Cette étude compare les résultats du Rhône avec ceux obtenus sur de petits cours d'eau (où l'échantillonnage est meilleur) et en mer (plus difficile). Les résultats montrent que les échantillonnages en cours permettent de détecter les tendances interannuelles majeures, mais sont limités pour discuter des évènements à l'échelle annuelle. Ces études s'appliquent à d'autres systèmes que les grandes rivières et peuvent conduire à la mise en place de stratégies de suivi plus efficaces et moins coûteuses

Published
2018

13. Optimisation des échantillonnages biologiques (suivis long-terme, évaluations de restauration) en grands fleuves et autres milieux

Author

Lamouroux, N, Cauvy-fraunie, S, Vaudor, L., Olivier, J.m, Trenkel, Verena, Maire, A, Forcellini, M, Roset, N, Lamouroux, N, Cauvy-fraunie, S, Vaudor, L., Olivier, J.m, Trenkel, Verena, Maire, A, Forcellini, M, and Roset, N

Abstract

Studies of the efficiency vs. the cost of long-term biological monitoring strategies are particularly infrequent and needed in large rivers. We used recent studies concerning the long-term monitoring of fish and macroinvertebrates in the Rhône River to discuss the potential and limits of monitoring strategies in large rivers and other environments. A first study is a numerical analysis of the probability to detect changes in fish abundance after flow restoration in the river. A second study concerns the detection of "most expected" relationships in annual fish time series, such as fish cohort follow-ups. It involves a comparison of the Rhône results with those obtained in smaller rivers (where sampling is easier) or in the ocean (where sampling is even more difficult). Results indicate that the long-term biological strategies used in the Rhône River are efficient for detecting major inter-annual trends, but are limited for detecting annual events. Such studies apply to other systems than large rivers and we hope that they will contribute to an increased efficiency and a reduced cost of monitoring strategies., Les études comparant l'efficacité vs. le coût des suivis biologiques de long-terme sont peu fréquentes et particulièrement utiles en grandes rivières. Nous nous basons sur des analyses récentes des données collectées dans le cadre des suivis de poissons et de macroinvertébrés du fleuve Rhône pour discuter du potentiel et des limites des stratégies d'échantillonnage mise en place en grands fleuves et dans d'autres milieux. Une première étude concerne une analyse numérique de la probabilité de détecter des changements d'abondance (poissons, invertébrés) après des mesures de restauration des débits à l'aval des barrages. Une seconde étude concerne la détection des patterns les plus attendus dans les séries annuelles d'abondance de poissons, comme les suivis de cohortes. Cette étude compare les résultats du Rhône avec ceux obtenus sur de petits cours d'eau (où l'échantillonnage est meilleur) et en mer (plus difficile). Les résultats montrent que les échantillonnages en cours permettent de détecter les tendances interannuelles majeures, mais sont limités pour discuter des évènements à l'échelle annuelle. Ces études s'appliquent à d'autres systèmes que les grandes rivières et peuvent conduire à la mise en place de stratégies de suivi plus efficaces et moins coûteuses

Published
2018

14. A global analysis of terrestrial plant litter dynamics in non-perennial waterways

Author

Datry, T., Foulquier, A., Corti, R., von Schiller, D., Tockner, K., Mendoza-Lera, C., Clement, J. C., Gessner, M. O., Moleon, M., Stubbington, R., Gucker, B., 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. J., Boechat, I. G., Boersma, K. S., Bogan, M. T., Bonada, N., Bond, N. R., Brintrup Barria, K. C., Bruder, A., Burrows, R. M., Cancellario, T., Canhoto, C., Carlson, S. M., Cauvy-Fraunie, S., Cid, N., Danger, M., Terra, Bianca de Freitas, De Girolamo, A. M., de La Barra, Evans, del Campo, R., Diaz-Villanueva, V. D., Dyer, F., Elosegi, A., Faye, E., Febria, C., Four, B., Gafny, S., Ghate, S. D., Gomez, R., Gómez-Gener, Lluís, Graca, M. A. S., Guareschi, S., Hoppeler, F., Hwan, J. L., Jones, J. , I, Kubheka, S., Laini, A., Langhans, S. D., Leigh, C., Little, C. J., Lorenz, S., Marshall, J. C., Martin, E., McIntosh, A. R., Meyer, E. , I, Milisa, M., Mlambo, M. C., Morais, M., Moya, N., Negus, P. M., Niyogi, D. K., Papatheodoulou, A., Pardo, I, Paril, P., Pauls, S. U., Pesic, V, Polasek, M., Robinson, C. T., Rodriguez-Lozano, P., Rolls, R. J., Sanchez-Montoya, M. M., Savic, A., Shumilova, O., Sridhar, K. R., Steward, A. L., Storey, R., Taleb, A., Uzan, A., Vander Vorste, Ross, Waltham, N. J., Woelfle-Erskine, C., Zak, D., Zarfl, C., Zoppini, A., Datry, T., Foulquier, A., Corti, R., von Schiller, D., Tockner, K., Mendoza-Lera, C., Clement, J. C., Gessner, M. O., Moleon, M., Stubbington, R., Gucker, B., 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. J., Boechat, I. G., Boersma, K. S., Bogan, M. T., Bonada, N., Bond, N. R., Brintrup Barria, K. C., Bruder, A., Burrows, R. M., Cancellario, T., Canhoto, C., Carlson, S. M., Cauvy-Fraunie, S., Cid, N., Danger, M., Terra, Bianca de Freitas, De Girolamo, A. M., de La Barra, Evans, del Campo, R., Diaz-Villanueva, V. D., Dyer, F., Elosegi, A., Faye, E., Febria, C., Four, B., Gafny, S., Ghate, S. D., Gomez, R., Gómez-Gener, Lluís, Graca, M. A. S., Guareschi, S., Hoppeler, F., Hwan, J. L., Jones, J. , I, Kubheka, S., Laini, A., Langhans, S. D., Leigh, C., Little, C. J., Lorenz, S., Marshall, J. C., Martin, E., McIntosh, A. R., Meyer, E. , I, Milisa, M., Mlambo, M. C., Morais, M., Moya, N., Negus, P. M., Niyogi, D. K., Papatheodoulou, A., Pardo, I, Paril, P., Pauls, S. U., Pesic, V, Polasek, M., Robinson, C. T., Rodriguez-Lozano, P., Rolls, R. J., Sanchez-Montoya, M. M., Savic, A., Shumilova, O., Sridhar, K. R., Steward, A. L., Storey, R., Taleb, A., Uzan, A., Vander Vorste, Ross, Waltham, N. J., Woelfle-Erskine, C., Zak, D., Zarfl, C., and Zoppini, A.

Abstract

Perennial rivers and streams make a disproportionate contribution to global carbon (C) cycling. However, the contribution of intermittent rivers and ephemeral streams (IRES), which sometimes cease to flow and can dry completely, is largely ignored although they represent over half the global river network. Substantial amounts of terrestrial plant litter (TPL) accumulate in dry riverbeds and, upon rewetting, this material can undergo rapid microbial processing. We present the results of a global research collaboration that collected and analysed TPL from 212 dry riverbeds across major environmental gradients and climate zones. We assessed litter decomposability by quantifying the litter carbon-to-nitrogen ratio and oxygen (O2) consumption in standardized assays and estimated the potential short-term CO2 emissions during rewetting events. Aridity, cover of riparian vegetation, channel width and dry-phase duration explained most variability in the quantity and decomposability of plant litter in IRES. Our estimates indicate that a single pulse of CO2 emission upon litter rewetting contributes up to 10% of the daily CO2 emission from perennial rivers and stream, particularly in temperate climates. This indicates that the contributions of IRES should be included in global C-cycling assessments.

Published
2018
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15. Ecological responses to experimental glacier-runoff reduction in alpine rivers

Author

Cauvy Fraunie, S., Andino, P., Espinosa, R., Calvez, R., Jacobsen, D., Dangles, O., Évolution, génomes, comportement et écologie (EGCE), Centre National de la Recherche Scientifique (CNRS)-IRD-Université Paris-Sud - Paris 11 (UP11), Escuela de Ciencias Biologicas, Pontificia Universidad Catolica del Ecuador, Escuela de Ciencas Biologicas, Gestion de l'Eau, Acteurs, Usages (UMR G-EAU), Centre de Coopération Internationale en Recherche Agronomique pour le Développement (Cirad)-AgroParisTech-Institut national d’études supérieures agronomiques de Montpellier (Montpellier SupAgro), and Institut national d'enseignement supérieur pour l'agriculture, l'alimentation et l'environnement (Institut Agro)-Institut national d'enseignement supérieur pour l'agriculture, l'alimentation et l'environnement (Institut Agro)-Institut national de recherche en sciences et technologies pour l'environnement et l'agriculture (IRSTEA)-Institut de Recherche pour le Développement (IRD)

Subjects
mountainous area, glacier, COURS D'EAU, [SDE]Environmental Sciences, population dynamics, DYNAMIQUE DE POPULATION, environmental impact, ZONE DE MONTAGNE, rivers, IMPACT SUR L'ENVIRONNEMENT
Abstract

International audience; Glacier retreat is a worldwide phenomenon with important consequences for the hydrological cycle and downstream ecosystem structure and functioning. To determine the effects of glacier retreat on aquatic communities, we conducted a 4-year flow manipulation in a tropical glacier-fed stream. Compared with an adjacent reference stream, meltwater flow reduction induces significant changes in benthic fauna community composition in less than 2 weeks. Also, both algal and herbivore biomass significantly increase in the manipulated stream as a response to flow reduction. After the flow reduction ceased, the system requires 14-16 months to return to its pre-perturbation state. These results are supported by a multi-stream survey of sites varying in glacial influence, showing an abrupt increase in algal and herbivore biomass below 11% glacier cover in the catchment. This study shows that flow reduction strongly affects glacier-fed stream biota, prefiguring profound ecological effects of ongoing glacier retreat on aquatic systems.

Published
2016

18. The Retreat of Mountain Glaciers since the Little Ice Age: A Spatially Explicit Database

Author

Marta, Silvio, Azzoni, Roberto, Fugazza, Davide, Tielidze, Levan, Chand, Pritam, Sieron, Katrin, Almond, Peter, Ambrosini, Roberto, Anthelme, Fabien, Alviz Gazitúa, Pablo, Bhambri, Rakesh, Bonin, Aurélie, Caccianiga, Marco, Cauvy-Fraunié, Sophie, Ceballos Lievano, Jorge, Clague, John, Cochachín Rapre, Justiniano, Dangles, Olivier, Deline, Philip, Eger, Andre, Cruz Encarnación, Rolando, Erokhin, Sergey, Franzetti, Andrea, Gielly, Ludovic, Gili, Fabrizio, Gobbi, Mauro, Guerrieri, Alessia, Hågvar, Sigmund, Khedim, Norine, Kinyanjui, Rahab, Messager, Erwan, Morales-Martínez, Marco, Peyre, Gwendolyn, Pittino, Francesca, Poulenard, Jerome, Seppi, Roberto, Chand Sharma, Milap, Urseitova, Nurai, Weissling, Blake, Yang, Yan, Zaginaev, Vitalii, Zimmer, Anaïs, Diolaiuti, Guglielmina, Rabatel, Antoine, Ficetola, Gentile, Università degli Studi di Milano [Milano] (UNIMI), Victoria University of Wellington, University of Central Punjab, Universidad Veracruzana, Lincoln University, New Zealand, Botanique et Modélisation de l'Architecture des Plantes et des Végétations (UMR AMAP), Centre de Coopération Internationale en Recherche Agronomique pour le Développement (Cirad)-Université de Montpellier (UM)-Centre National de la Recherche Scientifique (CNRS)-Institut de Recherche pour le Développement (IRD [France-Sud])-Institut National de Recherche pour l’Agriculture, l’Alimentation et l’Environnement (INRAE), Universidad de los Lagos (Chile), Heidelberg University, Riverly (Riverly), Institut National de Recherche pour l’Agriculture, l’Alimentation et l’Environnement (INRAE), Simon Fraser University (SFU.ca), Centre d’Ecologie Fonctionnelle et Evolutive (CEFE), Université Paul-Valéry - Montpellier 3 (UPVM)-Centre international d'études supérieures en sciences agronomiques (Montpellier SupAgro)-École pratique des hautes études (EPHE), Université Paris sciences et lettres (PSL)-Université Paris sciences et lettres (PSL)-Université de Montpellier (UM)-Centre National de la Recherche Scientifique (CNRS)-Institut de Recherche pour le Développement (IRD [France-Sud])-Institut national d’études supérieures agronomiques de Montpellier (Montpellier SupAgro), Institut national d'enseignement supérieur pour l'agriculture, l'alimentation et l'environnement (Institut Agro)-Institut national d'enseignement supérieur pour l'agriculture, l'alimentation et l'environnement (Institut Agro)-Institut National de Recherche pour l’Agriculture, l’Alimentation et l’Environnement (INRAE), Environnements, Dynamiques et Territoires de la Montagne (EDYTEM), Centre National de la Recherche Scientifique (CNRS)-Université Savoie Mont Blanc (USMB [Université de Savoie] [Université de Chambéry]), Università degli Studi di Milano-Bicocca [Milano] (UNIMIB), Laboratoire d'Ecologie Alpine (LECA ), Université Savoie Mont Blanc (USMB [Université de Savoie] [Université de Chambéry])-Centre National de la Recherche Scientifique (CNRS)-Université Grenoble Alpes (UGA), Norwegian University of Life Sciences (NMBU), Universidad de los Andes [Bogota] (UNIANDES), University of Pavia, National Academy of Sciences of Kyrgyz Republic, The University of Texas at San Antonio (UTSA), University of Texas at Austin [Austin], Institut des Géosciences de l’Environnement (IGE), Université Grenoble Alpes (UGA)-Centre National de la Recherche Scientifique (CNRS)-Institut national des sciences de l'Univers (INSU - CNRS)-Institut de Recherche pour le Développement (IRD)-Institut polytechnique de Grenoble - Grenoble Institute of Technology (Grenoble INP ), Université Grenoble Alpes (UGA), Marta, S, Azzoni, R, Fugazza, D, Tielidze, L, Chand, P, Sieron, K, Almond, P, Ambrosini, R, Anthelme, F, Alviz Gazitua, P, Bhambri, R, Bonin, A, Caccianiga, M, Cauvy-Fraunie, S, Lievano, J, Clague, J, Rapre, J, Dangles, O, Deline, P, Eger, A, Encarnacion, R, Erokhin, S, Franzetti, A, Gielly, L, Gili, F, Gobbi, M, Guerrieri, A, Hagvar, S, Khedim, N, Kinyanjui, R, Messager, E, Morales-Martinez, M, Peyre, G, Pittino, F, Poulenard, J, Seppi, R, Sharma, M, Urseitova, N, Weissling, B, Yang, Y, Zaginaev, V, Zimmer, A, Diolaiuti, G, Rabatel, A, Ficetola, G, Università degli Studi di Milano = University of Milan (UNIMI), RiverLy - Fonctionnement des hydrosystèmes (RiverLy), Université Paul-Valéry - Montpellier 3 (UPVM)-École Pratique des Hautes Études (EPHE), Université Paris sciences et lettres (PSL)-Université Paris sciences et lettres (PSL)-Université de Montpellier (UM)-Centre National de la Recherche Scientifique (CNRS)-Institut de Recherche pour le Développement (IRD [France-Sud])-Institut National de Recherche pour l’Agriculture, l’Alimentation et l’Environnement (INRAE)-Institut Agro - Montpellier SupAgro, Institut national d'enseignement supérieur pour l'agriculture, l'alimentation et l'environnement (Institut Agro)-Institut national d'enseignement supérieur pour l'agriculture, l'alimentation et l'environnement (Institut Agro), Environnements, Dynamiques et Territoires de Montagne (EDYTEM), Université Savoie Mont Blanc (USMB [Université de Savoie] [Université de Chambéry])-Centre National de la Recherche Scientifique (CNRS), Università degli Studi di Milano-Bicocca = University of Milano-Bicocca (UNIMIB), Università degli Studi di Pavia = University of Pavia (UNIPV), and Institut de Recherche pour le Développement (IRD)-Institut national des sciences de l'Univers (INSU - CNRS)-Centre National de la Recherche Scientifique (CNRS)-Université Grenoble Alpes (UGA)-Institut polytechnique de Grenoble - Grenoble Institute of Technology (Grenoble INP )

Subjects
climate change, [SDV.EE.ECO]Life Sciences [q-bio]/Ecology, environment/Ecosystems, global scale, little ice age, pre-satellite era, [SDV.BV.BOT]Life Sciences [q-bio]/Vegetal Biology/Botanics, [SDE.BE]Environmental Sciences/Biodiversity and Ecology, Glacier retreat, [SDV.BID.SPT]Life Sciences [q-bio]/Biodiversity/Systematics, Phylogenetics and taxonomy, glacier retreat, Bibliography. Library science. Information resources
Abstract

International audience; Most of the world’s mountain glaciers have been retreating for more than a century in response to climate change. Glacier retreat is evident on all continents, and the rate of retreat has accelerated during recent decades. Accurate, spatially explicit information on the position of glacier margins over time is useful for analyzing patterns of glacier retreat and measuring reductions in glacier surface area. This information is also essential for evaluating how mountain ecosystems are evolving due to climate warming and the attendant glacier retreat. Here, we present a non-comprehensive spatially explicit dataset showing multiple positions of glacier fronts since the Little Ice Age (LIA) maxima, including many data from the pre-satellite era. The dataset is based on multiple historical archival records including topographical maps; repeated photographs, paintings, and aerial or satellite images with a supplement of geochronology; and own field data. We provide ESRI shapefiles showing 728 past positions of 94 glacier fronts from all continents, except Antarctica, covering the period between the Little Ice Age maxima and the present. On average, the time series span the past 190 years. From 2 to 46 past positions per glacier are depicted (on average: 7.8)

Published
2021

19. Topsoil organic matter build-up in glacier forelands around the world

Author

Khedim, Norine, Cécillon, Lauric, Poulenard, Jérôme, Barré, Pierre, Baudin, François, Marta, Silvio, Rabatel, Antoine, Dentant, Cédric, Cauvy‐Fraunié, Sophie, Anthelme, Fabien, Gielly, Ludovic, Ambrosini, Roberto, Franzetti, Andrea, Azzoni, Roberto Sergio, Caccianiga, Marco Stefano, Compostella, Chiara, Clague, John, Tielidze, Levan, Messager, Erwan, Choler, Philippe, Ficetola, Gentile Francesco, Khedim, N, Cecillon, L, Poulenard, J, Barre, P, Baudin, F, Marta, S, Rabatel, A, Dentant, C, Cauvy-Fraunie, S, Anthelme, F, Gielly, L, Ambrosini, R, Franzetti, A, Azzoni, R, Caccianiga, M, Compostella, C, Clague, J, Tielidze, L, Messager, E, Choler, P, Ficetola, G, Environnements, Dynamiques et Territoires de la Montagne (EDYTEM), Centre National de la Recherche Scientifique (CNRS)-Université Savoie Mont Blanc (USMB [Université de Savoie] [Université de Chambéry]), Étude et compréhension de la biodiversité (ECODIV), Université de Rouen Normandie (UNIROUEN), Normandie Université (NU)-Normandie Université (NU), Laboratoire de géologie de l'ENS (LGENS), Institut national des sciences de l'Univers (INSU - CNRS)-Centre National de la Recherche Scientifique (CNRS)-Département des Géosciences - ENS Paris, École normale supérieure - Paris (ENS Paris), Université Paris sciences et lettres (PSL)-Université Paris sciences et lettres (PSL)-École normale supérieure - Paris (ENS Paris), Université Paris sciences et lettres (PSL)-Université Paris sciences et lettres (PSL), Institut des Sciences de la Terre de Paris (iSTeP), Centre National de la Recherche Scientifique (CNRS)-Sorbonne Université (SU)-Institut national des sciences de l'Univers (INSU - CNRS), University of Milan, Institut des Géosciences de l’Environnement (IGE), Université Grenoble Alpes (UGA)-Centre National de la Recherche Scientifique (CNRS)-Institut national des sciences de l'Univers (INSU - CNRS)-Institut de Recherche pour le Développement (IRD)-Institut polytechnique de Grenoble - Grenoble Institute of Technology (Grenoble INP ), Université Grenoble Alpes (UGA), Parc national des Ecrins, Riverly (Riverly), Institut National de Recherche pour l’Agriculture, l’Alimentation et l’Environnement (INRAE), Botanique et Modélisation de l'Architecture des Plantes et des Végétations (UMR AMAP), Centre de Coopération Internationale en Recherche Agronomique pour le Développement (Cirad)-Université de Montpellier (UM)-Centre National de la Recherche Scientifique (CNRS)-Institut de Recherche pour le Développement (IRD [France-Sud])-Institut National de Recherche pour l’Agriculture, l’Alimentation et l’Environnement (INRAE), Laboratoire d'Ecologie Alpine (LECA ), Université Savoie Mont Blanc (USMB [Université de Savoie] [Université de Chambéry])-Centre National de la Recherche Scientifique (CNRS)-Université Grenoble Alpes (UGA), Simon Fraser University (SFU.ca), Victoria University of Wellington, Emergence(s) Programme Ville de Paris-European Community Horizon 2020 Programme : 772284-LabEx OSUG@2020 : ANR10 LABX56, Environnements, Dynamiques et Territoires de Montagne (EDYTEM), Université Savoie Mont Blanc (USMB [Université de Savoie] [Université de Chambéry])-Centre National de la Recherche Scientifique (CNRS), École normale supérieure - Paris (ENS-PSL), Université Paris sciences et lettres (PSL)-Université Paris sciences et lettres (PSL)-École normale supérieure - Paris (ENS-PSL), Institut national des sciences de l'Univers (INSU - CNRS)-Sorbonne Université (SU)-Centre National de la Recherche Scientifique (CNRS), Università degli Studi di Milano = University of Milan (UNIMI), Institut de Recherche pour le Développement (IRD)-Institut national des sciences de l'Univers (INSU - CNRS)-Centre National de la Recherche Scientifique (CNRS)-Université Grenoble Alpes (UGA)-Institut polytechnique de Grenoble - Grenoble Institute of Technology (Grenoble INP ), and RiverLy - Fonctionnement des hydrosystèmes (RiverLy)

Subjects
Nitrogen, Temperature, [SDV.BV.BOT]Life Sciences [q-bio]/Vegetal Biology/Botanics, [SDV.BID.SPT]Life Sciences [q-bio]/Biodiversity/Systematics, Phylogenetics and taxonomy, Primary Research Articles, Carbon, chronosequence, Soil, [SDV.EE.ECO]Life Sciences [q-bio]/Ecology, environment/Ecosystems, soil organic matter, climate sensitivity, Primary Research Article, Ice Cover, topsoil development, [SDE.BE]Environmental Sciences/Biodiversity and Ecology, carbon stability
Abstract

Since the last glacial maximum, soil formation related to ice‐cover shrinkage has been one major sink of carbon accumulating as soil organic matter (SOM), a phenomenon accelerated by the ongoing global warming. In recently deglacierized forelands, processes of SOM accumulation, including those that control carbon and nitrogen sequestration rates and biogeochemical stability of newly sequestered carbon, remain poorly understood. Here, we investigate the build‐up of SOM during the initial stages (up to 410 years) of topsoil development in 10 glacier forelands distributed on four continents. We test whether the net accumulation of SOM on glacier forelands (i) depends on the time since deglacierization and local climatic conditions (temperature and precipitation); (ii) is accompanied by a decrease in its stability and (iii) is mostly due to an increasing contribution of organic matter from plant origin. We measured total SOM concentration (carbon, nitrogen), its relative hydrogen/oxygen enrichment, stable isotopic (13C, 15N) and carbon functional groups (C‐H, C=O, C=C) compositions, and its distribution in carbon pools of different thermal stability. We show that SOM content increases with time and is faster on forelands experiencing warmer climates. The build‐up of SOM pools shows consistent trends across the studied soil chronosequences. During the first decades of soil development, the low amount of SOM is dominated by a thermally stable carbon pool with a small and highly thermolabile pool. The stability of SOM decreases with soil age at all sites, indicating that SOM storage is dominated by the accumulation of labile SOM during the first centuries of soil development, and suggesting plant carbon inputs to soil (SOM depleted in nitrogen, enriched in hydrogen and in aromatic carbon). Our findings highlight the potential vulnerability of SOM stocks from proglacial areas to decomposition and suggest that their durability largely depends on the relative contribution of carbon inputs from plants., In glacier forelands all over the world, the organic matter build‐up during the initial stages of topsoil development is strongly modulated by climate: a warmer climate accelerates accumulation of organic matter. We also detected a decreasing thermal stability of soil organic matter along the chronosequences. The observed changes in soil organic matter elemental stoichiometry, aromaticity and stable isotope signature with soil organic matter accumulation suggest an increasing contribution of organic matter from plant origin during the first centuries of topsoil development.

Published
2021

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