Characterizing spatial and temporal trends in net sediment accumulation in seagrass meadows

dc.contributor.author Haviland, Katherine Ann
dc.contributor.author Howarth, Robert W.
dc.contributor.author Hayn, Melanie
dc.contributor.author Giblin, Anne E.
dc.date.accessioned 2024-12-24T17:09:26Z
dc.date.available 2024-12-24T17:09:26Z
dc.date.issued 2024-05-18
dc.description © The Author(s), 2024. This article is distributed under the terms of the Creative Commons Attribution License. The definitive version was published in Haviland, K., Howarth, R., Hayn, M., & Giblin, A. (2024). Characterizing spatial and temporal trends in net sediment accumulation in seagrass meadows. Estuaries and Coasts, 1–11, https://doi.org/10.1007/s12237-024-01365-4.
dc.description.abstract Seagrass meadows are known as hot spots for carbon accumulation, but there is limited field data on the variability of sediment accumulation across time and space. We developed a method to assess spatial and temporal heterogeneity in net sediment accumulation in seagrass meadows using small, inexpensive samplers, allowing for over 200 unique measurements across multiple transects within our study site. Using this method, we assessed sediment accumulation across seagrass meadow edges, and in varying weather conditions. We found the greatest accumulation of sediment 5 m outside of seagrass meadow edges, with sediment accumulation rates averaging just under 100 g m−2 day−1, though rates were highly variable. Carbon accumulation from settled sediment was generally greater outside of seagrass meadow edges than within the bed, especially at sites undergoing recent expansion. Measurements made during tropical storms showed both scouring of sediment away from sites, and increased accumulation, depending on site properties as well as individual tropical storm characteristics. In the storm that had a measurable storm surge, scouring of sediment was a more dominant mechanism, whereas deposition dominated in the storm that had high winds but no associated storm surge. Our data demonstrate the necessity of including measurements that characterize both spatial and meteorological variability to develop a more holistic understanding of the movement of sediment and particulate organic carbon associated with seagrass meadows, especially as meadow area becomes increasingly fragmented with human activity and global change.
dc.description.sponsorship Funding for this work came from the National Science Foundation Biocomplexity, GRFP, and LTREB programs (grants 0420575, 1654845, and 2018241438), and the Woods Hole SeaGrant program. Robert Howarth’s position at Cornell is supported through an endowment given by David R. Atkinson.
dc.identifier.citation Haviland, K., Howarth, R., Hayn, M., & Giblin, A. (2024). Characterizing spatial and temporal trends in net sediment accumulation in seagrass meadows. Estuaries and Coasts, 1–11.
dc.identifier.doi 10.1007/s12237-024-01365-4
dc.identifier.uri https://hdl.handle.net/1912/71050
dc.publisher Springer
dc.relation.uri https://doi.org/10.1007/s12237-024-01365-4
dc.rights Attribution 4.0 International
dc.rights.uri http://creativecommons.org/licenses/by/4.0/
dc.subject Sediment accumulation
dc.subject Edge effects
dc.subject Organic matter
dc.subject Zostera marina
dc.subject Spatial heterogeneity
dc.title Characterizing spatial and temporal trends in net sediment accumulation in seagrass meadows
dc.type Article
dspace.entity.type Publication
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