Jeffrey Pine Shrubland

Jeffrey pine shrubland.
Colder temperatures at higher elevations support shrubs that hug the ground to conserve energy. Surface cobbles and rocks are more dispersed where slopes are gentle. Western white pine (Pinus monticola) is a common component that can attain relative large size despite extreme winter conditions. Pinemat manzanita (Arctostaphylos nevadensis) grows in a somewhat continuous, low layer where slopes are flatter. Photo by Susan Erwin.

Jeffrey pine shrubland.
Stunted growth can be seen in both young and old trees. Large boulders have risen to the soil surface over many centuries. These provide perches for small mammals and reptiles that find cover close by in the dense cover of pinemat manzanita (Arctostaphylos nevadensis). Raptors and other birds make use of Jeffrey pine branches to scan for prey in the understory. Photo by Susan Erwin.

The Jeffrey pine shrubland is the mesic end of a continuum whose other, more xeric end is the Jeffrey pine savanna. Whittaker describes this continuum as a "two-phase character of essentially closed shrub cover alternating with shrub-less openings with grasses and other herbs." As grass cover falls below 50% in more moist sites, the shrubby openings form the continuous phase with discontinuous grassy patches, until a shrubland is present.

Peridotite and serpentinized peridotite comprise the primary soils in Jeffrey pine shrublands found just below flattened or broad ridgetops that support Jeffrey pine savanna communities. Soils are deeper and are composed of material that has eroded from higher elevations and ridgetops over time. Jeffrey pine shrublands occur between 1,400 and 5,000 feet.

Stunted Jeffrey pines (Pinus jeffreyi) and incense cedars (Calocedrus decurrens) characterize the overstory, which is interspersed throughout with discrete shrub, grass, and herbaceous (forb) plant communities. This shrubland community exists as a vegetative mosaic due to localized differences in soil moisture, soil depth, and degree of peridotite serpentinization. It is composed of drought-tolerant, woody, or leathery species, such as buckbrush (Ceanothus cuneatus), California coffeeberry (Rhamnus californica), hoary manzanita (Arctostaphylos canescens), pinemat manzanita (Arctostaphylos nevadensis), leatheroak (Quercus durata), birchleaf mountain-mahogany (Cercocarpus betuloides), and dwarf silktassel (Garrya buxifolia). Nested within the shrublands are open patches of grasses such as Idaho fescue (Festuca idahoensis), squirreltail (Elymus elymoides), and California melicgrass (Melica californica). Herbaceous openings often concentrate patches of Jeffrey pine and incense cedar and carry a diversity of forbs including Blue Mountain buckwheat (Eriogonum strictum), Yolla Bolly bedstraw (Galium ambiguum), serpentine phacelia (Phacelia corymbosa), Green’s blue-eyed Mary (Collinsia greenei), flame ragwort (Senecio greenei), serpentine milkweed (Asclepias solanoana) and sicklefruit jewelflower (Streptanthus drepanoides). Many of these forbs are found in herbaceous openings of the Jeffrey pine savanna community as well.

The Jeffrey pine and incense cedar overstory, generally from 20% to upwards of 30%, can vary from either species being dominant to the two being codominant, but total canopy cover is always greater than that seen in the Jeffrey pine savanna community. Jeffrey pines in this community can reach 300 to 400 years of age and incense cedars typically develop a contorted appearance with age. The canopy cover of the shrub layer can approach 80% (Whittaker 1960). Grassy openings appear as a pebble and rock gardens with tufts of Idaho fescue and scattered herbs. In the Jeffrey pine shrubland one may encounter rare species including Peanut sandwort (Minuartia rosei), serpentine goldenbush (Ericameria ophitidis), Trinity phacelia (Phacelia dalesiana), Tedoc Mountain linanthus (Leptosiphon nuttallii ssp. howellii), and threadleaf beardtongue (Penstemon filiformis).

Jeffrey pine shrubland.
Jeffrey pine shrublands at mid-elevation support shrubs of larger stature. Huckleberry oak (Quercus vaccinifolia) and greenleaf manzanita (Arctostaphylos patula) can persist under winter snowloads. Where slopes are steeper, erosional forces encourage peridotite cobbles and boulders to rise to the surface and accumulate at the bottom of slopes. Photo by Susan Erwin.

Jeffrey pine shrubland.
Shrubs that can tolerate the unusual serpentine soil chemistry and hot, dry summers are stout and woody. Wedgeleaf ceanothus (Ceanothus cuneatus) in the foreground has small, waxy leaves to reflect sun and reduce transpirational water loss. Few herbaceous species are tolerant of these conditions as seen in the large, bare spaces between shrubs and trees. Photo by Susan Erwin.

Photo Gallery

Jeffrey pine savanna
Jeffrey pine shrubland. Photo by Tom Kaye.

Jeffrey pine woodland
Jeffrey pine shrubland. Photo by Jenny Moore.

Siskiyou National Forest serpentine view
View from a jeffrey pine shrubland on the Siskiyou National Forest. Photo by Lee Webb.

Siskiyou National forest serpentine landscape
Jeffrey pine serpentine shrubland on the Siskiyou National Forest. Photo by Lee Webb.

Orthocarpus pachystachyus habitat
Orthocarpus pachystachyus habitat. Photo by Julie Kierstead Nelson.

Penstemon filiformis
Penstemon filiformis. Photo by Dr. Dean William Taylor, Jepson Herbarium.

Our thanks to CalPhotos and its many contributors for many of the pictures in this photo gallery.