Sediment deposition and production in SE-Asia seagrass meadows

E. Gacia*, C. M. Duarte, N. Marbà, J. Terrados, H. Kennedy, M. D. Fortes, N. H. Tri

*Corresponding author for this work

Research output: Contribution to journalArticlepeer-review

123 Scopus citations


Seagrass meadows play an important role in the trapping and binding of particles in coastal sediments. Yet seagrass may also contribute to sediment production directly, through the deposition of detritus and also the deposition of the associated mineral particles. This study aims at estimating the contribution of different seagrass species growing across an extensive range of deposition to inorganic (carbonate and non-carbonate) and organic sediment production. Total daily deposition measured with sediment traps varied from 18.8 (±2.0)g DW m-2d-1 in Silaqui (Philippines) to 681.1 (±102)g DW m-2d-1 in Bay Tien (Vietnam). These measurements correspond to a single sampling event and represent sedimentation conditions during the dry season in SE-Asia coastal areas. Enhalus acoroides was the most common species in the seagrass meadows visited and, together with Thalassia hemprichii, was present at sites from low to very high deposition. Halodule uninervis and Cymodocea species were present in sites from low to medium deposition. The mineral load in seagrass leaves increased with age, and was high in E. acoroides because it had the largest and long-lived leaves (up to 417 mg calcium carbonate per leaf and 507 mg non-carbonate minerals per leaf) and low in H. uninervis with short-lived leaves (4 mg calcium carbonate per leaf and 2 mg non-carbonate minerals per leaf). In SE-Asia seagrass meadows non-carbonate minerals accumulate at slower rates than the production of calcium carbonate by the epiphytic community, consequently the final loads supported by fully grown leaves were, as average, lower than calcium carbonate loads. Our results show that organic and inorganic production of the seagrasses in SE-Asia represents a small contribution (maximum of 15%) of the materials sedimented on a daily base by the water column during the sampling period. The contribution of the carbonate fraction can be locally significant (i.e. 34% in Silaqui) in areas where the depositional flux is low, but is minor (<1%) in sites were siltation is significant (i.e. Umalagan and all the visited sites in Vietnam).

Original languageEnglish (US)
Pages (from-to)909-919
Number of pages11
JournalEstuarine, Coastal and Shelf Science
Issue number5-6
StatePublished - Apr 1 2003
Externally publishedYes

Bibliographical note

Funding Information:
This research was funded by project PREDICT (contract IC18-CT98-0292) of the INCO program of the European Commission. We are grateful to the PREDICT colleagues for the great time and continuous support during the 1999 fieldtrip. HK wishes to thank The Ministry of Education and Culture, Spain for support during the preparation of this manuscript. We also thank three anonymous reviewers for their criticisms that helped to improve a former version of the manuscript.


  • Deposition
  • Leaf production
  • Seagrass
  • Sediment
  • Siltation

ASJC Scopus subject areas

  • Oceanography
  • Aquatic Science


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