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Biogeochemical and community ecology responses to the wetting of non-perennial streams

  • Adam Nicholas Price
  • , Margaret Ann Zimmer
  • , Anna Bergstrom
  • , Amy Jo Burgin
  • , Erin Cedar Seybold
  • , Corey Anne Krabbenhoft
  • , Sam Zipper
  • , Michelle Hope Busch
  • , Walter Kennedy Dodds
  • , Annika Walters
  • , Jane Sarah Rogosch
  • , Rachel Stubbington
  • , Richard Harry Walker
  • , James Christian Stegen
  • , Thibault Datry
  • , Mathis Messager
  • , Julian Olden
  • , Sarah Elizabeth Godsey
  • , Margaret Shanafield
  • , David Lytle
  • Ryan Burrows, Kendra Elena Kaiser, George Henry Allen, Meryl Christine Mims, Jonathan Douglas Tonkin, Michael Bogan, John Christopher Hammond, Kate Boersma, Allison Nicole Myers-Pigg, Amanda DelVecchia, Daniel Allen, Songyan Yu, Adam Ward
  • United States Department of Agriculture
  • University of California at Santa Cruz
  • University of Kansas
  • SUNY Buffalo
  • Kansas State University
  • United States Geological Survey
  • Nottingham Trent University
  • University of Tennessee System
  • Pacific Northwest National Laboratory
  • INRAE
  • University of Washington
  • Idaho State University
  • Flinders University
  • Oregon State University
  • University of Melbourne
  • Boise State University
  • Virginia Polytechnic Institute and State University
  • University of Canterbury
  • University of Arizona
  • University of San Diego
  • University of North Carolina at Chapel Hill
  • Pennsylvania State University
  • Griffith University Queensland

Research output: Contribution to journalArticlepeer-review

20 Scopus citations

Abstract

Transitions between dry and wet hydrologic states are the defining characteristic of non-perennial rivers and streams, which constitute the majority of the global river network. Although past work has focused on stream drying characteristics, there has been less focus on how hydrology, ecology and biogeochemistry respond and interact during stream wetting. Wetting mechanisms are highly variable and can range from dramatic floods and debris flows to gradual saturation by upwelling groundwater. This variation in wetting affects ecological and biogeochemical functions, including nutrient processing, sediment transport and the assembly of biotic communities. Here we synthesize evidence describing the hydrological mechanisms underpinning different types of wetting regimes, the associated biogeochemical and organismal responses, and the potential scientific and management implications for downstream ecosystems. This combined multidisciplinary understanding of wetting dynamics in non-perennial streams will be key to predicting and managing for the effects of climate change on non-perennial ecosystems.

Original languageEnglish
Pages (from-to)815-826
Number of pages12
JournalNature Water
Volume2
Issue number9
DOIs
StatePublished - Sep 2024

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