Ecological site group description

Provisional. A provisional ecological site description has undergone quality control and quality assurance review. It contains a working state and transition model and enough information to identify the ecological site.

Physiography

This ESG is associated with basins, depressions, and floodplains where water and fine sediments are often deposited with slopes ranging from 0 to 2 percent at elevations from 10 to 2000 feet.

Climate

The average annual precipitation in this area is typically 11 to 39 inches (280 to 1000 millimeters). Some areas can get as low as 6 inches (150 millimeters), while the areas at higher elevations can reach up to 88 inches (2235 millimeters) on average. Snowfall is common in the northern half of the part north of San Francisco and rare elsewhere. Precipitation is evenly distributed throughout fall, winter, and spring but is very low in summer. Coastal areas receive some moisture from fog in summer. Most of the rainfall occurs as low- or moderate-intensity, Pacific frontal storms during the period October to May. The average annual temperature is 52 to 65 degrees F (11 to 18 degrees C), decreasing from south to north. The freeze-free period averages 275 days and ranges from 180 to 365 days, decreasing in length with elevation and from south to north.

Soil features

Soils in this ESG consist of mainly very deep, moderately well and well drained clayey soils that have slickensides and formed in alluvium from mixed rock sources.
The soils that represent this ESG include:

Clear Lake, a fine, smectitic, thermic Xeric Endoaquerts
Capay, a fine, smectitic, thermic Typic Haploxererts

Vegetation dynamics

This ESG covers the areas of the valleys in MLRA 15 that were at one time part of a vast complex of marshes, tidal flats, estuaries, wetlands and wet meadows. The urbanized landscape in the valleys within this MLRA that exists today makes it difficult to imagine the natural landscape prior to human development.

These clayey bottoms were likely the fine-textured depressional and deposition areas and isolated oxbows that were created from the network of freshwater and salt marshes, rivers and streams that ran through these valleys as their seasonal and tidally influenced flood waters stretched across the floodplains and terraces in spring and deposited sediment as they receded during summer. Once the area began to be settled, many of these water-dominated ecosystems were drained, leveed, cleared for crops and other agriculture, and urbanized.

As this landscape was de-watered and houses and agriculture took over, the water table for many of these habitats was lowered, creating soils that would no longer offer the available soil moisture for many of the plants that had evolved with the hydrologic function of the natural system that no longer existed. These clayey basins may have remained wetter than many of the surrounding soils, due to their high water-holding capacity and their depressional location on the landscape. The clays of this ESG are high shrink-swell clays that dry out in the summer when the water table recedes and develop cracks and low soil pores spaces making them less hospitable for many of the native perennial grasses that existed within the drier surrounding grasslands.

Historically, this site may have looked similar to the CWHR wet meadow classification, however with the introduction of non-native annual grasses and the impacts from fragmentation, continued de-watering, and human alterations such as homes and roads, this site now reflects a lower producing, dry, annual grassland.

Sourced from:
California Wildlife Habitat Relationships System
California Department of Fish and Game
California Interagency Wildlife Task Group
Raymond D. Ratliff

Major Land Resource Area

MLRA 015X
Central California Coast Range

Stage

Provisional

Contributors

Kendra Moseley

Darren Pinnegar