Search engine for discovering works of Art, research articles, and books related to Art and Culture
ShareThis
Javascript must be enabled to continue!

Hierarchical organization of a Sardinian sand dune plant community

View through CrossRef
Coastal sand dunes have attracted the attention of plant ecologists for over a century, but they have largely relied on correlations to explain dune plant community organization. We experimentally examined longstanding hypotheses that sand binding, interspecific interactions, abiotic factors and seedling recruitment are drivers of sand dune plant community structure in Sardinia, Italy. Removing foundation species from the fore, middle and back dune habitats over 3 years led to erosion and habitat loss on the fore dune and limited plant recovery that increased with dune elevation. Reciprocal species removals in all zones suggested that interspecific competition is common, but that dominance is transient, particularly due to sand burial disturbance in the middle dune. A fully factorial 2-year physical factor manipulation of water, nutrient availability and substrate stability revealed no significant proximate response to these abiotic factors in any dune zone. In the fore and middle dune, plant seeds are trapped under adult plants during seed germination, and seedling survivorship and growth generally increase with dune height in spite of increased herbivory in the back dune. Sand and seed erosion lead to limited seed recruitment on the fore dune while high summer temperatures and allelopathy lead to competitive dominance of woody plants in the back dune. Our results suggest that Sardinian sand dune plant communities are hierarchically organized, structured by sand binding foundation species on the fore dune, sand burial in the middle dune and increasingly successful seedling recruitment, growth and competitive dominance in the back dune.
Title: Hierarchical organization of a Sardinian sand dune plant community
Description:
Coastal sand dunes have attracted the attention of plant ecologists for over a century, but they have largely relied on correlations to explain dune plant community organization.
We experimentally examined longstanding hypotheses that sand binding, interspecific interactions, abiotic factors and seedling recruitment are drivers of sand dune plant community structure in Sardinia, Italy.
Removing foundation species from the fore, middle and back dune habitats over 3 years led to erosion and habitat loss on the fore dune and limited plant recovery that increased with dune elevation.
Reciprocal species removals in all zones suggested that interspecific competition is common, but that dominance is transient, particularly due to sand burial disturbance in the middle dune.
A fully factorial 2-year physical factor manipulation of water, nutrient availability and substrate stability revealed no significant proximate response to these abiotic factors in any dune zone.
In the fore and middle dune, plant seeds are trapped under adult plants during seed germination, and seedling survivorship and growth generally increase with dune height in spite of increased herbivory in the back dune.
Sand and seed erosion lead to limited seed recruitment on the fore dune while high summer temperatures and allelopathy lead to competitive dominance of woody plants in the back dune.
Our results suggest that Sardinian sand dune plant communities are hierarchically organized, structured by sand binding foundation species on the fore dune, sand burial in the middle dune and increasingly successful seedling recruitment, growth and competitive dominance in the back dune.

Related Results

Sand Production Management
Sand Production Management
Abstract Sand production may be inevitable in many fields that have a relatively lower formation strength. Sand erosion and settling predictions and sand monitori...
Modelling river dune length adaptation during variable flow conditions
Modelling river dune length adaptation during variable flow conditions
<p>River dune modelling ranges from linear stability analysis to analyse the initial growth of the dunes (Fredsøe, 1983) up to three dimensional numerica...
Temporal resolution of echosounding measurements for assessing bedload transport rates via dune tracking
Temporal resolution of echosounding measurements for assessing bedload transport rates via dune tracking
<p>Assessment of bedload transport rates is of great importance for river morphology. Over the years, many efforts have been made to get a realistic estimate of the b...
Modelling the Influence of Vegetation on the Stochastic Dynamics of Coastal Dunes
Modelling the Influence of Vegetation on the Stochastic Dynamics of Coastal Dunes
ABSTRACT Coastal dunes are the highest natural features on a barrier island, where they protect beach communities, infrastructure and low‐energy back‐barrier ecos...
Patterns of island fox habitat use in sand dune habitat on San Clemente Island
Patterns of island fox habitat use in sand dune habitat on San Clemente Island
Identifying areas of high-quality habitat is often a critical first step for the recovery and management of species of conservation concern, yet patterns of high density in an area...
Holocene stratigraphy and chronology of the Casper Dune Field, Casper, Wyoming, USA
Holocene stratigraphy and chronology of the Casper Dune Field, Casper, Wyoming, USA
Activation chronologies of dune fields within the North American Great Plains are significant sources of paleoclimate information. Although many regional chronologies exist, severa...
Eolian landforms and processes on Titan and role in material movement 
Eolian landforms and processes on Titan and role in material movement 
The surface of Titan is composed of varied geomorphic units indicative of a vivid depositional, erosional and tectonic history. Dominant at Titan's equatorial regions are vast eoli...
Alongshore Varying Dune Retreat at a Barrier Island
Alongshore Varying Dune Retreat at a Barrier Island
Abstract. Barrier islands often exhibit spatially uneven morphological change due to alongshore variations in wave exposure, sediment supply, and dune morphology, which are influen...

Back to Top