Seagrasses develop extensive beds at the interface between the water column and sediment in tidal or subtidal environments. The height of seagrass canopy ranges from a few centimetres to more than a meter (Koch et al., Chapter 8), and seagrass rhizospheres may penetrate from centimetres (e.g. Halophila sp; Duarte et al., 1998) to a few meters (e.g. Posidonia oceanica; Mateo et al., 1997) into the sediment, depending on the species. Seagrass beds may support large above- and below-ground biomasses (Fig. 1), and they rank amongst the most productive marine primary producers (Duarte and Chiscano, 1999; Mateo et al., Chapter 7). © 2006/2007 Springer. All Rights Reserved.
CITATION STYLE
Marbà, N., Holmer, M., Gacia, E., & Barron, C. (2006). Seagrass beds and coastal biogeochemistry. In Seagrasses: Biology, Ecology and Conservation (pp. 135–157). Springer Netherlands. https://doi.org/10.1007/978-1-4020-2983-7_6
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