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The Role of Wind in Hydrochorous Mangrove Propagule Dispersal Open Access Open Access Earth System T EGU Journal Logos (RGB) Open Access Open Access Open Access Advances in Annales Nonlinear Processes Geosciences Geophysicae in Geophysics Open Access Open Access Natural Hazards Natural Hazards and Earth System and Earth System Sciences Sciences Discussions Open Access Open Access Atmospheric Atmospheric Chemistry Chemistry and Physics and Physics Discussions Open Access Open Access Atmospheric Atmospheric Measurement Measurement Techniques Techniques Discussions Open Access Biogeosciences, 10, 3635–3647, 2013 Open Access www.biogeosciences.net/10/3635/2013/ Biogeosciences doi:10.5194/bg-10-3635-2013 Biogeosciences Discussions © Author(s) 2013. CC Attribution 3.0 License. Open Access Open Access Climate Climate of the Past of the Past Discussions The role of wind in hydrochorous mangrove propagule dispersal Open Access Open Access Earth System T. Van der Stocken1,2,*, D. J. R. De Ryck1,2,*, T. Balke3, T. J. Bouma3,4, F. Dahdouh-GuebasEarth1,2 ,System and N. Koedam 1 1 Dynamics Laboratory of Plant Biology and Nature Management, Vrije Universiteit Brussel, Pleinlaan 2, 1050Dynamics Brussels, Belgium 2Laboratory of Systems Ecology and Resource Management, Universite´ Libre de Bruxelles, Av. F.D. Roosevelt 50, CPI 169, Discussions 1050 Brussels, Belgium 3 Open Access Deltares, PO Box 177, 2600 MH Delft, the Netherlands Geoscientific Open Access 4Royal Netherlands Institute for Sea Research (NIOZ-Yerseke; former NIOO-CEME), P.O. Box 140, 4400 AC Yerseke, Geoscientific the Netherlands Instrumentation Instrumentation *These authors contributed equally to this work. Methods and Methods and Correspondence to: T. Van der Stocken ([email protected]) Data Systems Data Systems Discussions Open Access Open Access Received: 18 December 2012 – Published in Biogeosciences Discuss.: 22 January 2013 Geoscientific Revised: 30 April 2013 – Accepted: 6 May 2013 – Published: 3 June 2013 Geoscientific Model Development Model Development Discussions Abstract. Although wind has been recognized to be an ules. The influence of wind on the dispersal of the horizon- important factor in the dispersal of hydrochorous man- tally floating C. tagal and R. mucronata dispersal units was Open Access Open Access grove propagules, and hence in the quantification of strong, comparable to thatHydrology of H. littoralis andpropagules. A dif- Hydrology and (meta)population dynamics, the species-specific sensitivity ferential effect of wind was found within elongated propag- to wind effects has not been studied. We combined obser- ules, which directly followsEarth from System the floating orientation of Earth System vations from a controlled experiment (flume tank) and in situ the propagules. While the dispersalSciences path of vertically float- Sciences experiments to understand wind and water current contribu- ing propagules was influenced by the strength and direction Discussions tions to dispersal potential as well as to estimate real disper- of the water currents and to a lesser extent by ambient wind Open Access Open Access sal ranges due to immediate response to tidal currents (two conditions, the dispersal path of horizontally floating propag- outgoing tides). This was done for 4 species with propagules ules was influenced by both strength and direction of the Ocean Science Ocean Science differing in morphological and buoyancy properties (i.e. Rhi- water currents and prevailing wind forces. To validate the Discussions zophora mucronata, Ceriops tagal, Heritiera littoralis and flume results, propagules of C. tagal and R. mucronata were Xylocarpus granatum). The flume experiments revealed that released during outgoing tide in a tidal creek in Gazi Bay Open Access the influence of wind depends on the density of a propagule (Kenya), followed by observation of their dispersalOpen Access distance (and hence its buoyancy characteristics) and that typical mor- and direction, while knowing the actual dominant wind di- phological characteristics of the dispersal unit are addition- rection. In line with the flume results, this study showed that Solid Earth Solid Earth ally important. H. littoralis propagules were influenced most, wind plays an important role in the dispersal distance of the Discussions because on the one hand their low density (613.58 g L−1; propagules. The present study provides important mechanis- n = 10) enables them to float on top of the water surface, and tic insight into the effect of wind on hydrochorous mangrove on the other hand their “sailboat-like” structure provides a propagule dispersal, thereby yielding an essentialOpen Access step to- Open Access relatively large surface area. The X. granatum fruits appeared wards the construction and optimization of (particle-based) to be the least influenced by ambient wind conditions, ex- hydrodynamic dispersalThe models. Cryosphere The Cryosphere plained by the smooth surface and spherical shape of which, Discussions because of the fruit’s high density (890.05 g L−1; n = 1), only a small part sticks above the water surface. Although the seeds of X. granatum are of a similar size class than H. 1 Introduction littoralis propagules, they are (like the X. granatum fruits) largely submerged due to their high density (870.66 g L−1; A series of publications have stressed the importance of n = 8), hence catching less wind than H. littoralis propag- dispersal in the evolution of plant population structure and composition (e.g. Duke et al., 1998; Cain et al., 2000; Published by Copernicus Publications on behalf of the European Geosciences Union. 3636 T. Van der Stocken et al.: The role of wind in hydrochorous mangrove propagule dispersal Nathan and Muller-Landau, 2000; Bowne and Bowers, species-specific differential behavior was not taken into ac- 2004; Caswell et al., 2003; Nathan et al., 2003; Clobert et count. al., 2012), where other reports emphasized the fundamental The role of prevailing wind conditions generally received need to study long-distance dispersal as a crucial mechanism only minor attention in existing hydrochorous dispersal stud- for understanding and predicting the adaptability of species ies, but those studies that are available point at the potential to cope with environmental and climate change (e.g. Pitelka importance of species-specific effects. For example, for a set et al., 1997; Higgins and Richardson, 1999; Nathan, 2001; of non-mangrove seeds it was shown that seed transport and Johst et al., 2002; Doyle et al., 2003). The spatial distribution sorting by hydrochory is strongly influenced by wind, de- of mangroves on a regional and global scale has been studied pending on the seed density and shape (Chambert and James, extensively (e.g. Ridley, 1930; van der Pijl, 1969; Duke et al., 2009). Stieglitz and Ridd (2001) investigated the dispersal of 1998), and the determining role of dispersal in spatiotempo- buoyant propagules of R. stylosa Griff., Bruguiera gymnor- ral changes of species distribution is a well-endorsed subject rhiza (L.) Lamk., Xylocarpus mekongensis Pierre and Heri- (Skellam, 1951; Duke, 1992; Clarke et al., 2001; Sousa et al., tiera littoralis Dryand. in the Normanby River estuary (Aus- 2007). Some authors used marked propagules (i.e. dispersal tralia). Besides the main finding that the distribution of these units) to investigate dispersal distances (Yamashiro, 1961; propagules is characterized by a density-driven secondary Komiyama et al., 1992; Clarke, 1993; McGuinness, 1997; circulation of water during the tropical dry season, wind- Breitfuss et al., 2003; Sousa et al., 2007; De Ryck et al., generated waves or wind drift seemed to have a negligible 2012). Though most propagules were found to disperse influence on their drift path (Stieglitz and Ridd, 2001). That over only short distances (up to tens of meters), some is, despite their distinct shapes and sizes, especially the ‘sail’ propagules dispersed over extensive ranges. Clarke (1993), of H. littoralis, propagules which enhance wind-driven dis- for example, recovered 3 Avicennia marina propagules at persal (Tomlinson, 1994), the dispersal path within the estu- more than 10 km and 1 propagule at more than 50 km. For ary was found to be similar for all propagules (Stieglitz and Rhizophora mucronata, Komiyama et al. (1992) found a Ridd, 2001). maximum dispersal distance of 1210 m. Nevertheless, the This study aims at investigating the importance of morpho- dynamics and controlling factors of mangrove propagule logical propagule traits and buoyancy behaviour in under- dispersal have remained understudied, mostly due to the standing the role of wind in hydrochorous mangrove propag- difficulty of the quantification of (long-distance) dispersal ule dispersal. This was studied by determining the dispersal (Nathan, 2001). Such knowledge is, however, essential in behaviour of propagules under different hydrodynamic and defining realistic dispersal kernels and improving existing wind conditions, both in a flume tank (controlled conditions), dispersal models, and thus for predicting the dispersal as well as in the field (natural conditions). We hypothesized route of mangrove propagules. This knowledge may in turn that the influence of wind will be more pronounced for: improve the success of future restoration projects. (i) propagules with lower density; (ii) propagules with high Mangrove propagules are hydrochorous, meaning that surface roughness; and (iii) horizontally floating propagules the hydrodynamics of tides and (ocean) currents constitute compared to vertically oriented ones, in the case of elongated the dominant dispersal vector. Dispersal
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