China Camp State Park. Photo by Rene Rivers.

USGS: A review of sediment transport across a natural tidal salt marsh in Northern San Francisco Bay

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.

 

Charts depicting water flux through a tidal creek during flood and ebb tides
Water flux through a tidal creek with a small, moderate, and extreme tide range during (A) a flood tide and (B) an ebb tide. Creek velocity legend applies to all tide ranges.
Maps showing China Camp Marsh study area with inset showing suspended sediment measurements
Map of study area: China Camp State Park and the adjacent shallows of San Pablo Bay. Black and gray bathymetry lines indicate the location of mean higher high water (MHHW) and mean lower low water (MLLW), respectively. The white box is the area shown on the right: Discrete measurements of suspended-sediment concentration (SSC in mg L– 1) at three locations (black dots) in the bay shallows at (A) high tide and (B) low tide during both a wavy condition (30-cm wave height at the farthest offshore station) and a calm condition (6-cm wave height at the farthest offshore station).

The monograph also highlights the nuanced role of marsh vegetation. Plant species and seasonal growth cycles significantly affect how much sediment is trapped and retained. Denser vegetation in spring and summer, for instance, can slow water flow and promote sediment deposition—but this effect varies widely by plant type and inundation level.

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.

Click here to read this paper.

Always know what’s going on in California water.

Subscribe to Maven’s Notebook.

It’s free!