Abstract
The distribution of seagrass beds has often been described in the literature as if these communities were naturally static components of coastal ecosystems (Larkum, 1977; McRoy and McMillan, 1977; Orth and Moore, 1983; Kirkman and Kuo, 1990), disturbed only by human influences.Aparadigm of seagrass bed stability, developed for large bed-forming seagrasses such as Posidonia as in the Mediterranean Sea (Boudouresque et al., 1980), and thewestern and southern coasts of Australia (Larkum, 1976; Larkum andWest, 1983; Kirkman, 1978), suggested that sea level had been stable for the last 5–8,000 years and assumed that these large monospecific seagrass beds were static for that period.
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Walker, D.I., Kendrick, G.A., McComb, A.J. (2007). Decline and Recovery of Seagrass Ecosystems— The Dynamics of Change. In: SEAGRASSES: BIOLOGY, ECOLOGYAND CONSERVATION. Springer, Dordrecht. https://doi.org/10.1007/978-1-4020-2983-7_23
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DOI: https://doi.org/10.1007/978-1-4020-2983-7_23
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