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Pagel. (and ;1. 515) - Foothill Woodland <br /> The author describes 3 kinds of foothill oak woodland: savannah, the <br /> closed canopy Brovelli Woods, and riparian woodland. <br /> The savannah that the author describes is better characterized as a valley D67 <br /> oak woodland sensu Holland (1986). This plant association is found primarily on <br /> the north central portion of the property. Within the predominately valley oak <br /> (Ouercugt labata community are found scattered Individuals of interior live oak <br /> Quem us wislize , blue oak (Qum douglasii , coastal live oak (Quercus <br /> agdfofla) and California buckeye (qua caljfQUUca). The author failed to <br /> notice the poor health of many of these trees, evidently the result of drought and <br /> the indirect Impacts from grazing such as soil compaction. <br /> The Biotics Study is confusing about the status of the community type in <br /> the closed canopy Brovelli Woods. Both the terms foothill woodland and riparian <br /> are used. K was correctly pointed out that interior live oak predominates valley <br /> oak by a 4:1 ratio, with fewer Individuals of ash (Fraxinus jam, elderberry <br /> (Sambucus meq$), cottonwood (Populus frgMont11), and willows (Saa spp.). <br /> The understory Is dominated by poison oak (Toxicodendron diversilobum), <br /> sedge (Carex fie, blackberry (Rubusprocerus,g. urcinatus , and <br /> California grape Qdtla califomicus). <br /> The vegetation of the Brovelli Woods does not conform to the classic <br /> riparian community type. Under pristine conditions, the classic valley riparian <br /> forests are formed by meandering streams and rivers having unconfined, low in <br /> elevation banks. During periods of flooding, erosion (degradation) occurs on the Dss <br /> outside banks, and deposition of sediments (aggradation) occurs on the inside <br /> banks and on the adjacent, low floodplains. As flood waters recede, willows, <br /> cottonwoods, ash, boxelder (Am a$gWadp , and valley oaks regenerate on the <br /> adjacent floodplains away from the river's edge. <br /> The Brovelli Woods do not fit this classic pattern of riparian vegetation. <br /> The reason for this is that the banks of the Mokelumne River, In comparison to <br /> classic meandering valley streams (e.g., the Cosumnes River), are relatively high <br /> In elevation thus serving to confine the river's course. As a consequence, the <br /> vegetation at this site is found on a relatively stable landform not subject to river <br /> meandering. Being higher in elevation, the site Is comparatively dry. Even In pre- <br /> dam conditions, the Mokelumne River at this location would not have flooded as <br /> extensively as would other rivers such as the Cosumnes. This explains why the <br /> woods consist predominately of interior live oak, a comparatively upland species, <br /> with fewer numbers of valley oak. Only a few scattered riparian species, such as <br /> willows, cottonwoods, and ash are found In moist depressions. The Brovelli <br /> Woods therefore approximates a foothill interior live oak woodland sensu Holland <br /> (1986) and is not a riparian kind of vegetation. <br /> The reason that these comments are Important to note Is that the Brovelli <br /> Woods are lacking in several key structural components of riparian forests such <br /> as trees of the intermediate size -- ash and boxekier-- and additionally in having <br /> a poor representation of willows and cottonwoods. This comparative lack of plant <br /> height, structure, and diversity results in less bird diversity compared to true <br /> riparian systems. <br /> 3 <br /> VI-83 <br />