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A tenfold slowdown in river meander migration driven by plant life


Meandering rivers are diagnostic landforms of hydrologically active planets, and their migration regulates the continental component of biogeochemical cycles that stabilize climate and allow for life on Earth. The rise of river meanders on Earth has been linked to riverbank stabilization driven by the Palaeozoic evolution of plant life about 440 million years ago. Here we provide a fundamental test for this hypothesis using a global analysis of active meander migrations that includes previously ignored unvegetated rivers from the arid interiors of modern continents. When normalized by channel size, unvegetated meanders universally migrate an order of magnitude faster than vegetated ones. While providing irrefutable evidence that vegetation is not required for meander formation, we demonstrate how profoundly vegetation transformed the pace of change for Earth’s landscapes, and we at last offer a mechanistic explanation for the radically distinct stratigraphic records of barren and vegetated rivers. We posit that the migration slowdown driven by the rise of land plants dramatically impacted biogeochemical fluxes and rendered Earth’s landscapes even more hospitable to life. Therefore, the tenfold faster migration of unvegetated rivers may be key to deciphering the environments of barren worlds such as early Earth and Mars.

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Fig. 1: Compilation of vegetated and unvegetated meandering rivers.
Fig. 2: Meander migration rates and morphometry.
Fig. 3: Morphometry of unvegetated and vegetated channels.

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Data availability

The authors declare that all data supporting the finding of this study are available within the article and its Supplementary Information files. The latter include a supporting discussion on flood-recurrence intervals, aggradation versus subsidence rates in alluvial basins and their relations to the dimensions of deposited channel bodies and the storage time of floodplain sediment and POC.


  1. Branagan, D. in The Origins of Geology in Italy Vol. 411 (eds Vai, G. B. & Caldwell, W. G. E.) 31–42 (Geological Society of America, 2006).

  2. Malin, M. C. & Edgett, K. S. Evidence for persistent flow and aqueous sedimentation on early Mars. Science 302, 1931–1934 (2003).

    Article  Google Scholar 

  3. Lorenz, R. D. et al. Fluvial channels on Titan: initial Cassini RADAR observations. Planet. Space Sci. 56, 1132–1144 (2008).

    Article  Google Scholar 

  4. Jackson, R. G. II Depositional model of point bars in the Lower Wabash River. J. Sediment. Pet. 46, 579–594 (1976).

    Google Scholar 

  5. Bathurst, J. C., Thorne, C. R. & Hey, R. D. Direct measurements of secondary currents in river bends. Nature 269, 504–506 (1977).

    Article  Google Scholar 

  6. Schumm, S. A. & Khan, H. R. Experimental study of channel patterns. Geol. Soc. Am. Bull. 83, 1755–1770 (1972).

    Article  Google Scholar 

  7. Johannesson, H. & Parker, G. in River Meandering Vol. 112 (eds Ikeda, S. & Parker, G.) 181–213 (Water Resources Monographs, 1989).

  8. Schumm, S. A. Speculations concerning paleohydrologic controls of terrestrial sedimentation. Geol. Soc. Am. Bull. 79, 1573–1588 (1968).

    Article  Google Scholar 

  9. Lovelock, J. E. & Margulis, L. Atmospheric homeostasis by and for the biosphere: the Gaia hypothesis. Tellus 26, 2–10 (1974).

    Article  Google Scholar 

  10. Davies, N. S. & Gibling, M. R. Cambrian to Devonian evolution of alluvial systems: the sedimentological impact of the earliest land plants. Earth Sci. Rev. 98, 171–200 (2010).

    Article  Google Scholar 

  11. Fuller, A. O. A contribution to the conceptual modelling of pre-Devonian fluvial systems. South Afr. J. Geol. 88, 189–194 (1985).

    Google Scholar 

  12. Li, J. et al. An ephemeral meandering river system: sediment dispersal processes in the Río Colorado, Southern Altiplano Plateau, Bolivia. Z. Geomorphol. 59, 301–317 (2015).

    Article  Google Scholar 

  13. Ielpi, A. Morphodynamics of meandering streams devoid of plant life: Amargosa River, Death Valley, California. Geol. Soc. Am. Bull. 131, 782–802 (2019).

    Article  Google Scholar 

  14. Long, D. F. G. in From River to Rock Record: The Preservation of Fluvial Sediments and Their Subsequent Interpretation Vol. 97 (eds. Davidson, S. K. et al.) 37–61 (SEPM Society for Sedimentary Geology, 2011).

  15. Santos, M. G. M. & Owen, G. Heterolithic meandering-channel deposits from the Neoproterozoic of NW Scotland: implications for palaeogeographic reconstructions of Precambrian sedimentary environments. Precambrian Res. 272, 226–243 (2016).

    Article  Google Scholar 

  16. Ielpi, A., Rainbird, R. H., Ventra, D. & Ghinassi, M. Morphometric convergence between Proterozoic and post-vegetation rivers. Nat. Commun. 8, 15250 (2017).

    Article  Google Scholar 

  17. Ielpi, A. River functioning prior to the rise of land plants: a uniformitarian outlook. Terra Nova 30, 341–349 (2018).

    Article  Google Scholar 

  18. Lauer, J. W. & Parker, G. Modeling framework for sediment deposition, storage, and evacuation in the floodplain of a meandering river: theory. Water Resour. Res. 44, W04425 (2008).

    Google Scholar 

  19. Galy, V., Peucker-Ehrenbrink, B. & Eglington, T. Global carbon export from the terrestrial biosphere controlled by erosion. Nature 521, 204–207 (2015).

    Article  Google Scholar 

  20. Torres, M. A. et al. Model prediction of long-lived storage of organic carbon in river deposits. Earth Surf. Dynam 5, 711–730 (2017).

    Article  Google Scholar 

  21. Ganti, V., Whittaker, A. C., Lamb, M. P. & Fischer, W. W. Low-gradient, single-threaded rivers prior to greening of the continents. Proc. Natl Acad. Sci. USA 116, 11652–11657 (2019).

    Google Scholar 

  22. Aalto, R., Lauer, J. W. & Dietrich, W. E. Spatial and temporal dynamics of sediment accumulation and exchange along Strickland River floodplains (Papua New Guinea) over decadal-to-centennial timescales. J. Geophys. Res. 113, F01S04 (2008).

    Article  Google Scholar 

  23. Smith, D. G. Effect of vegetation on lateral migration of anastomosed channels of a glacier meltwater river. Geol. Soc. Am. Bull. 87, 857–860 (1976).

    Article  Google Scholar 

  24. Limaye, A. B. & Lamb, M. P. Numerical simulations of bedrock valley evolution by meandering rivers with variable bank material. J. Geophys. Res. Earth 119, 927–950 (2014).

    Article  Google Scholar 

  25. McLelland, S. J. et al. in Fluvial Sedimentology VI Vol. 28 (eds Smith, N. D. & Rogers, J.) 43–57 (International Association of Sedimentologists, 1999).

  26. Jerolmack, D. J. & Mohrig, D. Conditions for branching in depositional rivers. Geology 35, 463–466 (2007).

    Article  Google Scholar 

  27. Mohrig, D., Heller, P. L., Paola, C. & Lyons, W. J. Interpreting avulsion process from ancient alluvial sequences: Guadalope–Matarranya system (northern Spain) and Wasatch Formation (western Colorado). Geol. Soc. Am. Bull. 112, 1787–1803 (2000).

    Article  Google Scholar 

  28. Bouchez, J. et al. Oxidation of petrogenic organic carbon in the Amazon floodplain as a source of atmospheric CO2. Geology 38, 255–258 (2010).

    Article  Google Scholar 

  29. Beck, H. E. et al. Present and future Köppen–Geiger climate classification maps at 1-km resolution. Sci. Rep. 5, 180214 (2018).

    Google Scholar 

  30. Dunne, K. B. J. & Jerolmack, D. J. Evidence of, and a proposed explanation for, bimodal transport states in alluvial rivers. Earth Surf. Dynam. 6, 583–594 (2018).

    Article  Google Scholar 

  31. Gran, K. & Paola, C. Riparian vegetation controls on braided stream dynamics. Water Resour. Res. 37, 3275–3283 (2001).

    Article  Google Scholar 

  32. Tal, M. & Paola, C. Dynamic single-thread channels maintained by the interaction of flow and vegetation. Geology 35, 347–350 (2007).

    Article  Google Scholar 

  33. Leopold, L. B. & Wolman, M. G. River Channel Patterns: Braided, Meandering, and Straight US Geological Survey Professional Paper 282-B (US Government Printing Office, 1957).

  34. Zimmerman, R. C., Goodlett, J. C. & Comer, G. H. in Symposium on River Morphology Vol. 75, 255–275 (International Association of Hydrological Sciences, 1967).

  35. Church, M. Geomorphic thresholds in riverine landscapes. Freshw. Biol. 47, 541–557 (2002).

    Article  Google Scholar 

  36. Eaton, B. C. & Giles, T. R. Assessing the effect of vegetation-related bank strength on channel morphology and stability in gravel-bed streams using numerical models. Earth Surf. Process. Landf. 34, 712–724 (2009).

    Article  Google Scholar 

  37. Ielpi, A. & Lapôtre, M. G. A. Biotic forcing militates against river meandering in the Bonneville Basin of Utah. Sedimentology 66, 1896–1929 (2019).

    Article  Google Scholar 

  38. Ielpi, A. & Lapôtre, M. G. A. Barren meandering streams in the modern Toiyabe Basin of Nevada, U.S.A., and their relevance to the study of the pre-vegetation rock record. J. Sediment. Res. 89, 399–415 (2019).

    Article  Google Scholar 

  39. Sylvester, Z., Durkin, P. & Covault, J. A. High curvatures drive river meandering. Geology 47, 263–266 (2019).

    Article  Google Scholar 

  40. Brice, J. C. Channel Patterns and Terraces of the Loup Rivers in Nebraska Geological Survey Professional Paper 422-D (US Government Printing Office, 1964).

  41. Lehner, B., Verdin, K. & Jarvis, A. New global hydrography derived from spaceborne elevation data. Eos 89, 93–94 (2008).

    Article  Google Scholar 

  42. Harvard WorldMap Database (Center for Geographic Analysis at Harvard Univ., accessed 15 January 2019);

  43. Farr, T. G. et al. The shuttle radar topography mission. Rev. Geophys. 45, RG2004 (2007).

    Article  Google Scholar 

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This research was supported by a Discovery Grant from the Natural Sciences and Engineering Research Council of Canada (A.I.) and by the John Harvard Distinguished Science Fellows Program within the FAS Division of Science of Harvard University (M.G.A.L.).

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Authors and Affiliations



A.I. and M.G.A.L. jointly conceived the study and conducted fieldwork in the Great Basin of the western United States, and they equally contributed to the preparation of the manuscript. The morphometric dataset of meander migrations was compiled by A.I.

Corresponding author

Correspondence to Alessandro Ielpi.

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The authors declare no competing interests.

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Peer review information Primary Handling Editor(s): Melissa Plail; Xujia Jiang.

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Supplementary information

Supplementary Information

Supplementary descriptions, Figs. 1–7 and Tables 1–4.

Supplementary Data 1

Migration rates from modern unvegetated channels.

Supplementary Data 2

Migration rates from modern vegetated channels.

Supplementary Data 3

Geographical coordinates for the river reaches measured in this study.

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Ielpi, A., Lapôtre, M.G.A. A tenfold slowdown in river meander migration driven by plant life. Nat. Geosci. 13, 82–86 (2020).

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