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Bio126 Bio126 The Great Central ValleyThe Great Central Valley
Great Central Valley Characteristics: Largest Plain West of the Rockies
430 miles long 75 miles wide (varies)
In Rainshadow of Coastal Mountains mostly dry land with ribbons of wet areas
along rivers. Spilt into Sacramento and San Joaquin
Valleys by Rivers, meet in Delta
Great Central Valley – topography: Broad flat plain Ringed with rolling foothills on all sides Slightly below sea level in middle, in the
Delta Region – salt water flows in. Rises to about 400 ft. elevation at extreme
southern and northern ends. Filled with deep alluvial layers. Remains of
proto (old) Sierras washed into former inland sea. Up to 30,000’ thick.
Great Central Valley –Latitudinal Rain Gradient Long enough to have differences in
annual rainfall due to Hadley cell positions. North- Redding 38” Central – Sacramento 18” South – Bakersfield 6”
Rainshadow makes inland drier than coastal areas of same latitude
Great Central Valley –The Major Community types: Grasslands
Had 22,000,000 acres Now just 1 % remain
Riparian Corridors Had 4,000,000 acres Now 6% remain
Fresh water marsh Had 975,000 Now 11% remain
Great Central Valley – Seasonal Changes Major flooding now rare. Most rivers diverted or dammed higher up – Rivers channelized Great seasonal lakes and marshes no longer
form. Early settlers moved around by boat in
winter. Cholera, etc, seasonal problems. Marshes
began to be drained.
Central Valley Drainage basin Drains west slope of Sierra
Many major rivers Drains east slope of coastal mountains
Smaller ‘rivers’, many called creeks Drains southern cascades
via Pit River into Shasta Lake then in Sacramento River
All drain into Delta, to SF Bay - Ocean
Sacramento Valley From the Delta North Sacramento River the major river fed
by: American Feather Yuba Shasta
San Joaquin Valley From the Delta South San Joaquin River the major river fed
by: Merced Tuolomne Stanislaus Mokelumne Cosumnes
River Deltas Delta formed at each of the river
junctions on a flat plain Large areas of marshland once
important part of Central Valley Ecology
Central Valley Grasslands Rapidly changed from perennial bunch
grasses to introduced annual grasses Pushed Blacktailed Deer and Tule Elk out of
valley Deer moved to foothills, migrating up into
and down from Sierras Tule Elk moved into marshes as a last
refuge. Last habitat as marshes were drained Fewer than 10 remained in lake Buena Vista
Perennial Bunch Grasses Slow growing, long lived Deep rooted, tall grasses Set seed in summer Poor competitors Evolved without grazers Large “fountains” or bunches of year-round
grayish green grass Lower fire intensity Open spaces in between bunches where
bulbs and annuals wildflowers grew.
Annual Grasses Brought over from Spain with cattle and
sheep in hides and feed Great competitors Rapid germination and seedling growth Shallow roots quickly dry out top soil Several hundred per square foot Short lived, not as nutritious
(Terrace) Vernal Pools A superficial clay hardpan layer in soil traps
water in depressions. Dry soil slowly exposed later in spring as
pool dries Water and lower soils become salty Many Endemic species Relict spp. left from moister climate with
summer rain. See also Text pg. 395-6
Fresh Water Marshlands Shallow areas flooded (at least
seasonally) with fresh water Commonly bordered large shallow
lakes Bands of vegetation:
Macrophytes – floating plants Reed-like Plant Border Higher ground – Riparian species
Macrophytes “Larger” than algae, but still small
plants Azolla a small water fern with nitrogen
fixing bacteria Lemma duckweed can completely
cover lakes in summer Water Hyacinth a new introduced pest
Reed-like plant border Deepest water (only up to 4’) has
cattails. Hollow Stems with “sausage-like” stalk of flowers / seeds
Bulrushes or Tules common Sedges have triangular stems
Higher Ground Has shrubs, and small trees like
willows
Riparian or Gallery Forests A nearly closed canopy forest with a river or
stream running down through it. Very narrow band along waterway, within sight of water.
Streams and rivers had many shallow branching courses, not in channels like today. SOME FORESTS UP TO 10 MILES THICK !
They remain wet year-round with snow melt run off.
Gallery forest photo
Riparian Forest Tree Species
Valley: Valley Oak, Cottonwood, Alder, Willows,
Oregon Ash, Boxelder, Walnut, Sycamores, Maple
CA Grape, Poison Oak, vines growing up tall trees.
Higher elevations: Alder, Willows, Aspen, Bigleaf Maple,
Dogwood
Riparian Forest Characteristics Cold air drainage with fog in winter.
Lows 32 – 38 F (-4 to 0 C) common Have broad flat leaves, need lots of
water, especially in the summer Many have Nitrogen fixing bacteria in
roots Wind currents carry pollen and later
cottony winged-seeds down stream Winter deciduous
Riparian Forest Trees Adapted to floods by sprouting
vigorously from stumps Broken limbs buried in floods can root
and sprout, dispersing the trees into new soil layers.
Remnants of Former Climates Migrated into California when climate
was much mild and wetter. From East Coast hardwood Forest: Maple, Boxelder, Ash, some Willows
From Semi-dry Climate, from southwest: Sycamore, Cottonwood, other Willows
Riparian Habitat Had many summer-flowing rivers V shaped valleys too desirable for
dams !! Super-fertile soils now mostly orchards Water from dams provides irrigation Most rivers mere remnants of flow and
size in flood controlled channels.
Southern Central Valley Lakes Lakes NOT flowing into San Joaquin Large Shallow lakes fed by winter rain, snow
melt Tremendous migratory bird populations 1,000’s acres of marsh along shores Slight rise in valley floor trapped water in
southern end of valley Tulare Lake fed by (N to S) Kings,Tulare and
Kaweah Rivers Buena Vista & Kern Lakes fed by Kern River
Foothill Ecotone Ecotones are abrupt meeting places of
different community types, not a gradual transition
Often have high species diversity Have species for each habitat, plus Have species only found in ecotone
Mix marsh, Riparian, Grassland species