Seed retention by pioneer trees enhances plant diversity resilience on gravel bars: Observations from the river Allier, France. (July 2016)

• Record Type: Journal Article
• Authors: Corenblit, Dov; Vidal, Vincent; Cabanis, Manon; Steiger, Johannes; Garófano-Gómez, Virginia; Garreau, Alexandre; Hortobágyi, Borbála; Otto, Thierry; Roussel, Erwan; Voldoire, Olivier
• Is Part Of: Advances in water resources. Volume 93(2016)Part B
• Page Start: 182
• Page End: 192
• Publication Date: 2016-07
• Subjects: Biogeomorphology -- Seed bank -- Facilitation -- Ecosystem engineer -- Pioneer riparian species -- Sediment tails; Hydrology -- Periodicals; Hydrodynamics -- Periodicals; Hydraulic engineering -- Periodicals; 551.48
• DOI: 10.1016/j.advwatres.2016.02.015
• Languages: English
• ISSNs: 0309-1708

Abstract

Highlights: Results suggest biogeomorphic feedback between sediment and seed retention. Seeds deposited on sediment tails locally increase seed abundance on gravel bars. Sediment tails improve plant diversity resilience within dynamic river corridors. Abstract: Pioneer riparian trees which establish in river active tracts on gravel bars enhance fine sediment retention during high flows within their stands and in their lee side, forming obstacle marks. Fine sediment retention can be accompanied by deposition of seeds transported by water dispersal, i.e. by hydrochory. We tested the hypothesis that pioneer riparian trees significantly control seed deposition on gravel bars by forming sediment obstacle marks. We described the seed bank structure and compared samples collected from obstacle marks and bare coarse-grained bar surfaces. At the surface (at 2 cm depth), seed abundance ( N ) and richness ( S ) (expressed as mean ± sd) were significantly higher in areas directly affected by riparian trees, i.e. obstacle marks, ( N : 693 ± 391; S : 17 ± 3) than in bare surfaces ( N : 334 ± 371; S : 13 ± 5). Surface and sub-surface (at 20 cm depth) samples were also significantly different, with the sub-surface samples almost devoid of seeds (respectively N : 514 ± 413; S : 15 ± 5 and N : 3 ± 6; S : 1 ± 2). These results suggest a biogeomorphic feedback between sediment and associated seed retention mediated by hydrochory, vegetation growth and local seed dispersal mediated by barochory. Such feedback may improve plant diversity resilience on gravel alluvial bars of high-energy rivers.