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dc.contributor.authorBau', V
dc.contributor.authorBorthwick, Alistair
dc.contributor.authorPerona, P
dc.date.accessioned2021-08-22T10:35:44Z
dc.date.available2021-08-22T10:35:44Z
dc.date.issued2021-05-16
dc.identifier.issn0094-8276
dc.identifier.issn1944-8007
dc.identifier.urihttp://hdl.handle.net/10026.1/17642
dc.description.abstract

<jats:title>Abstract</jats:title><jats:p>Freshwater ecosystems along river floodplains host among the greatest biodiversity on Earth and are known to respond to anthropic pressure. For water impounded systems, resilience to changes in the natural flow regime is believed to be bidirectional. Whether such resilience prevents the system from returning to pristine conditions after the flow regime changes reverse is as yet unclear, though widely documented. In this work, we show that temporal irreversibility of river floodplains to recover their status may be explained by the dynamics of riparian water‐tolerant plant roots. Our model is a quantitative tool that will benefit scientists and practitioners in predicting the impact of changing flow regimes on long‐term river floodplain dynamics.</jats:p>

dc.languageen
dc.language.isoen
dc.publisherAmerican Geophysical Union (AGU)
dc.titlePlant Roots Steer Resilience to Perturbation of River Floodplains
dc.typejournal-article
dc.typeJournal Article
plymouth.issue9
plymouth.volume48
plymouth.publication-statusPublished
plymouth.journalGeophysical Research Letters
dc.identifier.doi10.1029/2021gl092388
plymouth.organisational-group/Plymouth
plymouth.organisational-group/Plymouth/Faculty of Science and Engineering
plymouth.organisational-group/Plymouth/Users by role
plymouth.organisational-group/Plymouth/Users by role/Academics
dcterms.dateAccepted2021-04-18
dc.rights.embargodate2021-8-25
dc.identifier.eissn1944-8007
dc.rights.embargoperiodNot known
rioxxterms.versionofrecord10.1029/2021gl092388
rioxxterms.licenseref.urihttp://www.rioxx.net/licenses/all-rights-reserved
rioxxterms.licenseref.startdate2021-05-16
rioxxterms.typeJournal Article/Review


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