Authors
Oleksandra Shumilova
Dominik Zak
Thibault Datry
Daniel von Schiller
Roland Corti
Arnaud Foulquier
Biel Obrador
Klement Tockner
Daniel C. Allan
Florian Altermatt
María Isabel Arce
Shai Arnon
Damien Banas
Andy Banegas‐Medina
Erin Beller
Melanie L. Blanchette, Edith Cowan UniversityFollow
Juan F. Blanco‐Libreros
Joanna Blessing
Iola Gonçalves Boëchat
Kate Boersma
Michael T. Bogan
Núria Bonada
Nick R. Bond
Kate Brintrup
Andreas Bruder
Ryan Burrows
Tommaso Cancellario
Stephanie M. Carlson
Sophie Cauvy‐Fraunié
Núria Cid
Michael Danger
Bianca de Freitas Terra
Anna Maria De Girolamo
Ruben del Campo
Fiona Dyer
Arturo Elosegi
Emile Faye
Catherine Febria
Ricardo Figueroa
Brian Four
Mark O. Gessner
Pierre Gnohossou
Rosa Gómez Cerezo
Lluís Gomez‐Gener
Manuel A.S. Graça
Simone Guareschi
Björn Gücker
Jason L. Hwan
Skhumbuzo Kubheka
Simone Daniela Langhans
Catherine Leigh
Chelsea J. Little
Stefan Lorenz
Jonathan Marshall
Angus McIntosh
Clara Mendoza‐Lera
Elisabeth Irmgard Meyer
Marko Miliša
Musa C. Mlambo
Marcos Moleón
Peter Negus
Dev Niyogi
Athina Papatheodoulou
Isabel Pardo
Petr Paril
Vladimir Pešić
Pablo Rodriguez‐Lozano
Robert J. Rolls
Maria Mar Sanchez‐Montoya
Ana Savić
Alisha Steward
Rachel Stubbington
Amina Taleb
Ross Vander Vorste
Nathan Waltham
Annamaria Zoppini
Christiane Zarfl
Document Type
Journal Article
Publication Title
Global Change Biology
Publisher
Wiley
School
Mine Water and Environment Research Centre / School of Science
RAS ID
28924
Funders
Funding information available at: https://doi.org/10.1111/gcb.14537
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 global biogeochemical cycles, especially because prevalence of IRES will increase due to increasing severity of drying events.
DOI
10.1111/gcb.14537
Creative Commons License
This work is licensed under a Creative Commons Attribution 4.0 License.
Comments
Shumilova, O., Zak, D., Datry, T., von Schiller, D., Corti, R., Foulquier, A., ... Zarfl, C. (2019). Simulating rewetting events in intermittent rivers and ephemeral streams: a global analysis of leached nutrients and organic matter. Global Change Biology. 25(5), 1591-1611. Available here