By the USGS Coastal and Marine Hazards and Resources Program
Tidal salt marshes—vital ecosystems that protect coastlines, remove excess nutrients and pollutants from coastal waters, and provide habitat for fish and wildlife—depend on a steady supply of inorganic sediment to keep pace with rising sea levels. But how, exactly, does this sediment get to the marsh? And what factors influence this process?
The findings, drawn from a range of field studies, tell a complex and variable story of sediment movement. One major takeaway: shallow areas of the bay serve as an important—though inconsistent—source of sediment for the marsh. Sediment is delivered across the bay-marsh boundary primarily during flood tides and through wave action, in addition to transport through tidal creeks. In some cases, creeks may even export sediment instead of importing it.
As sea-level rise and human alterations continue to reshape estuaries, these insights are particularly important for assessing tidal marsh resilience. Sediment management is a key factor in whether tidal marshes can survive future climate conditions. For land managers and restoration practitioners, the study offers actionable information for planning sediment interventions—such as enhancing natural sediment delivery or restoring marsh-edge processes.
China Camp’s relatively unaltered condition makes it a valuable reference point, but researchers emphasize that broader studies across different marsh types are essential. Every estuary has its own sediment-flux dynamics; understanding that variability is crucial for protecting these ecosystems.
RESEARCH ARTICLE: Marsh Sediment in Translation: A Review of Sediment Transport Across a Natural Tidal Salt Marsh in Northern San Francisco Bay
By Foster-Martinez, Madeline; Ferner, Matthew; Callaway, John; Goeden, Brenda; Lacy, Jessica
Abstract: Deposition of inorganic sediment is essential for the sustainability of tidal salt marshes. Understanding variability in sediment sources and the processes of sediment delivery to salt marshes are high priorities for decision-makers responsible for managing sediment and conserving and restoring marshes. Research on sediment transport to marshes is published in technical journals, but these scientific findings must be translated and communicated to inform critical decisions related to managing sediment in estuaries.
We convened a diverse group of collaborators—including natural-resource managers, regulators, scientists, and restoration planners and practitioners—to review and interpret the results of previously published field investigations on and around the salt marsh at China Camp State Park in Marin County, California. We discussed and translated key results of those studies using new graphics and more accessible language.
Here, we present a general introduction to the topic of sediment delivery to salt marshes, background descriptions of the China Camp marsh and the physical processes that we characterized there, key scientific conclusions, and proposed management implications. Key conclusions include (1) bay shallows are an important but variable source of marsh sediment, (2) flood tides and waves move sediment across the bay–marsh edge, (3) tidal creeks may not always import sediment to the marsh platform, and (4) protective effects of marsh vegetation depend on species and season.
China Camp marsh is one of the last remaining pre-colonial salt marshes in the San Francisco Estuary and is unique in being relatively unmodified by humans and in retaining an unimpeded transition into natural uplands. Additional studies in a variety of marshes with different attributes and sediment regimes will broaden understanding of how best to conserve, manage, and restore tidal marshes that provide numerous ecosystem services to for humans and wildlife.




