Spatial patterns of water-dispersed seed deposition along stream riparian gradients

• Published in: PloS one 2017-09, Vol.12 (9), p.e0185247-e0185247
• Main Authors: Fraaije, Rob G A, Moinier, Sophie, van Gogh, Iris, Timmers, Robert, van Deelen, Joost J, Verhoeven, Jos T A, Soons, Merel B
• Format: Article
• Language: English
• Subjects: Altitude; Biodiversity; Biology and Life Sciences; Biotic factors; Catchments; Colonization; Conservation; Deposition; Dispersal; Dispersion; Earth Sciences; Ecology and Environmental Sciences; Ecosystem; Ecosystem components; Ecosystems; Emergency preparedness; Endangered plants; Endangered species; Environmental aspects; Flooding; Floodplains; Floods; Flowers & plants; Harbors; Hydrology; Influence; Linear Models; Physical Sciences; Plant diversity; Recruitment; Restoration; Riparian environments; Riparian land; Riparian vegetation; Rivers; Seasons; Seed dispersal; Seed Dispersal - physiology; Seeds; Seeds - physiology; Species diversity; Species richness; Streams; Traps; Water; Water conservation; Water levels; Wildlife conservation
• ISSN: 1932-6203; 1932-6203
• DOI: 10.1371/journal.pone.0185247

Riparian ecosystems along streams naturally harbour a high plant diversity with many increasingly endangered species. In our current heavily modified and fragmented catchments, many of these species are sensitive to dispersal limitation. Better understanding of riparian plant dispersal pathways is required to predict species (re-)colonization potential and improve success rates of stream and riparian zone conservation and restoration. Dispersal by water (hydrochory) is an important mechanism for longitudinal and lateral dispersal of riparian species. Crucially for recruitment potential, it also influences the elevation along the riparian hydrological gradient where seeds become deposited. Due to the complex interplay between abiotic and biotic factors, however, it remains unclear how exactly patterns in seed deposition are formed. We compared hydrochorous and non-hydrochorous seed deposition, and quantified patterns of seed deposition along the bare substrate of newly created stream riparian gradients. Water levels were monitored and seed deposition was measured with seed traps along the full range of riparian hydrological conditions (from permanently flooded to never flooded). Average seed numbers and species richness were significantly higher in flooded than in non-flooded seed traps (5.7 and 1.5 times higher, respectively). Community-weighted trait means indicated that typically water-dispersed seeds were more dominant in flooded than in non-flooded seed traps and gradually decreased in concentration from the channel to the upland. Moreover, highly buoyant seeds accumulated at the average water line, and clear elevational sorting of non-buoyant seeds occurred within the floodplain. These results establish a critical role of flooding in shaping patterns of seed deposition along the riparian gradient, delivering many seeds of typical riparian species to riparian zones and depositing them at species-specific elevations as influenced by seed traits, suggesting species-specific dispersal pathways. This shows that hydrochory likely has important consequences for riparian vegetation development and that flooding forms a key process for successful restoration.