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Wave damping by giant kelp, Macrocystis pyrifera.
Elsmore, Kristen; Nickols, Kerry J; Miller, Luke P; Ford, Tom; Denny, Mark W; Gaylord, Brian.
Afiliação
  • Elsmore K; Bodega Marine Laboratory, University of California at Davis, 2099 Westshore Road, Bodega Bay, CA 94923, USA.
  • Nickols KJ; Department of Biology, California State University, Northridge, 18111 Nordhoff Street, Northridge, CA 91330, USA.
  • Miller LP; Department of Biology, San Diego State University, 5500 Campanile Drive, San Diego, CA 92182, USA.
  • Ford T; Coastal Research Institute, Loyola Marymount University, 1 Loyola Marymount Drive, Los Angeles, CA 90045, USA.
  • Denny MW; Hopkins Marine Station, Stanford University, 120 Ocean View Boulevard, Pacific Grove, CA 93950, USA.
  • Gaylord B; Bodega Marine Laboratory, University of California at Davis, 2099 Westshore Road, Bodega Bay, CA 94923, USA.
Ann Bot ; 133(1): 29-40, 2024 Mar 08.
Article em En | MEDLINE | ID: mdl-37463436
BACKGROUND AND AIMS: The increased likelihood and severity of storm events has brought into focus the role of coastal ecosystems in provision of shoreline protection by attenuating wave energy. Canopy-forming kelps, including giant kelp (Macrocystis pyrifera), are thought to provide this ecosystem service, but supporting data are extremely limited. Previous in situ examinations relied mostly on comparisons between nominally similar sites with and without kelp. Given that other factors (especially seafloor bathymetry and topographic features) often differ across sites, efforts to isolate the effects of kelp on wave energy propagation confront challenges. In particular, it can be difficult to distinguish wave energy dissipation attributable to kelp from frictional processes at the seabed that often covary with the presence of kelp. Here, we use an ecological transition from no kelp to a full forest, at a single site with static bathymetry, to resolve unambiguously the capacity of giant kelp to damp waves. METHODS: We measured waves within and outside rocky reef habitat, in both the absence and the presence of giant kelp, at Marguerite Reef, Palos Verdes, CA, USA. Nested within a broader kelp restoration project, this site transitioned from a bare state to one supporting a fully formed forest (density of 8 stipes m-2). We quantified, as a function of incident wave conditions, the decline in wave energy flux attributable to the presence of kelp, as waves propagated from outside and into reef habitat. KEY RESULTS: The kelp forest damped wave energy detectably, but to a modest extent. Interactions with the seabed alone reduced wave energy flux, on average, by 12 ±â€…1.4 % over 180 m of travel. The kelp forest induced an additional 7 ±â€…1.2 % decrease. Kelp-associated declines in wave energy flux were slightly greater for waves of longer periods and smaller wave heights. CONCLUSIONS: Macrocystis pyrifera forests have a limited, albeit measurable, capacity to enhance shoreline protection from nearshore waves. Expectations that giant kelp forests, whether extant or enhanced through restoration, have substantial impacts on wave-induced coastal erosion might require re-evaluation.
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Texto completo: 1 Base de dados: MEDLINE Assunto principal: Kelp / Macrocystis Idioma: En Ano de publicação: 2024 Tipo de documento: Article

Texto completo: 1 Base de dados: MEDLINE Assunto principal: Kelp / Macrocystis Idioma: En Ano de publicação: 2024 Tipo de documento: Article