BIOL 305 — Lecture (Unit 3)
Geology
- Study of rocks, minerals
- Geological time scale, gradualism
- Basic components of earth’s crust:
- 46.6%: Oxygen
- 27.7%: Silica
- 8.1%: Aluminum
- 5.0%: Iron
- Others:
- 3.6%: Calcium
- 2.8%: Sodium
- 2.6%: Potassium
- 2.1%: Magnesium
- Other elements are found at lower percentages: precious metals, etc.
Minerals
- Element: One molecule composed of specific atomic units
- Mineral: One compound composed of one or more elements
- Nutrients necessary for organisms to process for survival
- Rocks release minerals through weathering and erosion
Weathering
- Chemical process of releasing minerals
- Affected by several agents
Water
- Chemical acidity
- Lattice structure of water → expansion when changing forms → surface tension
- Expansion when freezing breaks down chunks of rocks
Chemical Weathering
- Gases: CO2, Carbonic Acid
- Carbonic acid breaks down marble, limestone, rocks, etc. via acidity
- Chemical reactions dissolve rock
Rainwater
- Effective weathering agent
- Normal rainwater, not acid rain; is slightly acidic
- Mixes with CO2 to form Carbonic Acid
- Mixes with decaying material to form Carbonic Acid and Nitric Acid (stronger acid)
Acid Rain
- Severe acidity
- Sulfur dioxide released in the atmosphere
- Sulfur dioxide and water forms sulfuric acid (battery acid)
- Nitrogen Oxide from cars and water forms Nitric Acid
Erosion
- Physical processes
- Physically breaking apart/away sediments
- The faster water flows (higher velocity, higher energy) the more material it can carry; slower water releases materials
- Sierra Nevada wears down by 1” every thousand years
Water Erosion
- Hurling particles causing breakdown
- Carving and altering land shapes
Splash Erosion
- The impact of water drops (raindrops) on bare ground dislodges portions of the ground
Sheet Erosion
- Water on a mostly flat, inclined area gathers volume and velocity, eroding land under it
Gully Erosion
- Advanced sheet erosion
- Greater velocity
Wind Erosion
- Geological pressures
- Tornadoes and hurricanes are extreme wind erosion
Santa Ana Winds
- High wind pressure
- Altitude in air
- High pressure in Nevada, low in Southern California; vacuum-like position of pressure on ground level
- Wind flows down into ground that is being pulled upwards: wind travels faster to try to replace volume
- Wind picks up sand/sediment and blows it into objects
- Santa Rosa firestorms
- The stronger the difference between air pressures, the stronger the wind/breeze that fills in
Glacial Ice Erosion
- Glaciers in CA (~100), up to 1km
- Snow that does not melt fully, leaving behind an ice layer; some is left as runoff
- Glacier: Large block of ice pulled downwards with gravity
- Last ice age had glaciers on Sierra Nevada, Klamath, Cascade 10000 yrs ago; Yosemite carved valleys
- Sierra, Mt. Shasta, Trinity Alps
- Glacier depletion in CA, Alaska, etc. in retreat: extensive erosion/exposure of soils causing positive loop of melting
Gravitational Erosion
Rock Sediments
- Different subsections of three major types
- Sedimentary rock, igneous rock, metamorphic rock
Sedimentary Rock
- Secondary rock
- Particles from weathering and erosion reform/compress into a new rock
- Sandstone
- Makes up ¾ of rocks found on surface and only 5% of those in crust
- Large amounts of sedimentary rock in CA as a result of exposure and covering by water through Ice Age and tectonic events from rising oceans/coasts
- Central Valley: Water washed out, 1000ft sediments
- Mountains have been uplifted and wearing down for millions of years; sediments end in Central Valley
Sierra Nevada Sedimentary Rock
- Many exposed rocks are igneous; sedimentary rock has eroded
- Still visible in areas of low rainfall: “spine”/crest at high elevation is present
Igneous Rock
- Volcanic/plutonic rock
- Primary rocks formed from basal materials of magma and lava
- Formed above and under ground; many of it is underground
- Granite, basalt, pumice, obsidian
- Examples
- Sierra Nevada granite batholith
- batholith: large intrusion of igneous rock that cools over time; uplifted and eroded
- Mount Lassen, Mount Shasta, Devil’s Postpile, Modoc Plateau, Sutter Buttes
- Active cascading volcanoes
- Basalt cooling
Slow-Cooling
- “Salt and pepper” look in granite
- “Coarse-grained”
- Larger crystals formed in rocks
Rapid-Cooling
- Some small or no crystals at all
- “Fine-grained”
- Pumice: Air bubbles
- Basalt
- Gaseous; dissolved gases inside and high pressure
- “Bubbling out” and rapidly cooling
- Obsidian: black glass with no gas inside
- Secondary rock
- Begins as igneous or sedimentary; tectonic activity causes them to be shoved underground towards heat sources and they change forms/characteristics
- Limestone → Marble; Shale → Slate
- Partially remelted and changed
- Mountainous areas common
Rock Cycle
- Igneous → Metamorphic → Sedimentary
- Weathering agents/Exogenous forces act on igneous rocks and break them into sedimentary minerals
- Sediment is compressed into sedimentary rocks: Lithification
- Sedimentary rocks exposed to high heat from tectonic convergence, friction, and pressure bakes and changes into metamorphic rocks
- Exogenous forces can break all rocks into sediment
- Mantle through subduction → Igneous and metamorphic rocks
Plate Tectonics
- Three plates: Juan de Fuca, Pacific, North American
- Pacific moves west; Juan de Fuca moves east
- Grinding/friction; rocks melt
- Volcanoes: Lassen, Shasta, Plateau
- San Andreas Fault
- Pacific Plate has a ring that intersects with various other intercontinental plates: Ring of Fire
- High earthquake zones and volcanic activity on plate faults
- Devil’s hole
Faults
- Foot-walls and hanging walls
- Ridge collapses
- Various deep faults under South California
- San Andreas Fault
- Fracture zones
- Base of transverse range
- Faults are unknown forms; large cause of urban destruction and utility risk
Normal Fault
- Foot-wall is higher than hanging wall
Reverse Fault
- Hanging wall is higher than foot-wall
- Overhang
Strike-Slip Fault
- Foot-wall and hanging wall move horizontally away from each other
- 1906 earthquake
Weather and Climate
- Weather: Daily, present variations in temperature, precipitation, winds, etc.
- Climate: Long-term and annual patterns in temperature, precipitation, winds, etc. in a region
- Climate is affected by:
- Air masses moving across and around counties/locations; density of air masses and variables of air masses
- Oceans and ocean currents; temperature, moisture, density
- Topography and movement around topography
- Latitude and angles of sunlight
- Hemispheric seasons and angles
Adiabatic Cooling
- Altitude is not elevational movement; altitude regards atmosphere
- Warm air rises; warm air molecules are lighter and less dense, less close
- Ground warms accepting heat
- Directly above ground level is the warmest
- Air gets denser as it cools and enlarges
- Adiabatic cooling is present most in areas of rainfall, adiabatic warming is present in areas of desert
Ocean Currents and Maritime Climate
- Cool water is bordered by denser air that is not heated by it and less moisture
- California maritime climate
- Warm water is bordered by less dense air and more moisture
- Florida thunderstorms
- Sierra Nevada, especially at night
- Atmospheric effect
Mediterranean Climate
- Seasonality of warm dry summers and cool wet winters
- Created by cold water current off coast and air masses moving from coast onto land alongside mountainous topography
- Mediterranean, California coast, North Africa, Chile, Southern and West Australia
- Close to 40*N and S
Orographic Precipitation
- Rain shadows
- Orographic effect
- Topographical
- Mountain ranges force air up which causes adiabatic cooling → rainfall
- West side of mountain ranges:
- Air rises
- Adiabatic cooling
- Condensation and precipitation
- East side:
- Adiabatic warming
- Desert
- Peninsular Range
- Transverse Range
- Southern Sierra Nevada
- Sierra Nevada
- Cascade Range
- Big Sur area in Bakersfield
- Rain shadow effect
- Evaporation from compression and warming
- Air expands and dries; less relative humidity
- No condensation or precipitation
Coastal Regions
Waves
- Rogue waves
- Intersection points of different waves exponentially increase wave energy
- Non-sequential
- High waves
- Massive gradualist coastal erosion
- Cliffs; Pacifica, CA
- Riff-raff armored to prevent further erosion
- Breaker waves
- Coastal deposition: large amounts of sediment displaced and deposited by incoming waves downstream from inland river sediment
- Creates beaches
- Prohibited by damming; cleans sediments in water
- Lack of beach development; Huntington Beach
- Contracted cargo bay dredging and shipping
Tides
- Coastal erosion
- Gravitational pull of Moon (2/3), spinning inertia, and Sun (1/3)
- Moon is much closer than Sun
- Tidal bulges rotate around Earth
- Two low tides and two high tides experienced every lunar day; one lunar day is 24 hours, 50 minutes
- Peak highs experienced approximately every 6 hours
- Spring and neap tides occur every fourteen days per; monthly, not seasonal
High Tides
- Gravity is significantly greater or less than the center of the Earth
Low Tides
- Gravity is equal to the center of the Earth
Spring Tides
- Moon and sun are parallel to each other to Earth
- New and full moons
- Most maximal tides
Neap Tides
- Moon and sun are perpendicular with regard to Earth as the origin
- Quarter moon phases
- Most minimal tides
Upwelling
- Winds push warm surface water away from the coast
- Deep cold water rises on continental coast and displaces surface water
- Nutrient-rich
- Pulls to surface
- Aids in phytoplankton production and biodiversity
- Four major upwelling zones
- Two in Atlantic
- Off coast of Western Africa
- Off coast of Southern Africa
- Two in Eastern side of Pacific
- Off coast of California
- Off coast of Peru
- Produces 20% of fishery catch worldwide
Tidal Zonation
Supertidal Zone
Upper Intertidal/Littorina Zone
- Encompasses supertidal and part of intertidal
- High tide occurs in middle of littorina
- 7 to 2.5 ft above sea level
- “Supralittoral fringe”
Intertidal Zone
- 2.5 to 0 ft above sea level
- “Midlittoral zone”
Middle Intertidal Zone
- Majority of Intertidal Zone
- Barnacles, rockweed, mussels
- Low tide occurs at end of zone
- “Infralittoral fringe”
Subtidal Zone
- 0 to -1.6 ft below sea level
Lower Intertidal Zone
- Variable populations
- Partial intertidal, all of subtidal
Biodiversity
Deep Sea Organisms
- Aphotic adaptations
- Anglerfish, Pacific Black Dragon
- Cnidarians; Blood Belly Comb Jelly
- Fangtooth
- Red Mysid
- Bioluminescence
- Attracting prey
- Dispelling/blinding predators
- Red fully dispelled underwater; blood belly comb jelly is hidden underwater
- Air-filled compressible bladder in water column; distended at higher sea levels
- Anglerfish males are parasitic; chew into females and grow into respiratory system and release sperm
- Monterey canyon
Kelp Forests
- Over 220 species depend on kelp in California
- Require upwelling conditions
- Large seawater filtration
- Water brings in nutrients and displaces waste products
- Cold water allows higher levels of oxygen to dissolve
- Spores
- Water motion rips exposed kelp pieces and pulls upward holdfasts; creates kelp shape
- Macrocystis grows best in well-mixed waters on coastlines that experience wave action vs. bays
- East coast of pacific
- South America
- Australia
- New Zealand
- South Africa
- Similarities to terrestrial forests
- Canopic and floor structures
- Three-dimensional weightless state in kelp forests
- Kelp can grow quickly with nutrients; foot and a half a day
Coastal Organisms
Mammals
Orcas
- Transient
- Follows and predates whales
- Migrates from Alaska to Baja California
- Native
- Territorial pods on West Coast
- Predate fish, sometimes larger mammals, otters
- Otter diet caused by overfishing
Sea Otters
- Recolonizing
- Abundant until 1700s: Japan, Alaska, Baja California, British Columbia, West Coast
- 300,000+ animals; 20,000 in California
- 1741: Russian, colonial fur trade
- 150 years of fur trade
- Aleut/Inuit enslavement in Russians
- Peaked in California: 500-600 in one week in San Francisco Bay
- 1911: International Fur Seal Treaty
- Only 1,000-2,000 left
- One colony in Alaska and one in Big Sur
- ~50 in B.S.
- Discovered in 1938; Highway 1
- 1970s: Gill netting bycatch
- Modern California sea otter population has low genetic diversity
- Dependent on kelp forests
- Shelter, Cover, Food, Loafing, Grooming
- Californian and Alaskan otters
- Fur has heavy insulative properties
- Velvety
- 1m follicles per square inch
- Vulnerable to oil pollution and oil spills
- Federal Oil Pollution Acts
- Cat poop: Leptospirosis
- Flu-like symptoms
- Exacerbated by stress
- Shooting
- Monterey Bay, Newport Bay, Vancouver Aquariums
Vertebrates
- Wolf Eel
- Shiner Surf Perch
Sharks
- Great White is offshore
- Coastal: Leopard, Horn Sharks
Invertebrates
- Bat Star
- Brittle Star
- Sea Anemone
- Sand Dollars
- Mussels
- Crabs
- Cuttlefish
- Chromatophores in pigmented sacs in radial muscles
- Jellyfish
- 85-95% composition water
- Nematocysts
- Nudibranchs
- Vampire Squid
- Pigbutt Worm
Octopuses
- Pacific Giant Octopus
- Dumbo Octopus
- Flapjack Octopus
- MBARI
- Benthic
- Photophores
Mudflats and Marshes
- Eelgrass
- Submerged marshplants
- Rock crevices in rocky environments
- Mudflats
- Pipefish camouflaged in grass
- Flat Innkeeper Worm
- Long-billed curlew
- Killdeer
Elkhorn Slough
- Monterey Bay
- Estuary systems
- Species richness and biodiversity
- Surrounded by farms
- Salinas Valley
- High pollution; fertilizer runoff/eutrophication
- Algal blooms and decomposition die-off → anoxic ecosystems
- Coats eelgrass and prevents photosynthesis
- Death prevented by various organisms
- Dungeness crabs
- Sea hares (Giant seaslugs); Aplesia
- Sea otters
- Algae and Eelgrass → Aplesia → Dungeness crabs → Sea otters
Coastal Forests
Coastal Interface
- Inward loses influence of salt spray and erosion; forested environments
- inward after McClure’s Beach on Point Reyes
- Westernmost extension of coastal forest
Oak Woodland
- Easternmost extension of coastal forest
- Past top/over Coast Ranges
- Oak range, dry conditions
- Adiabatic cooling, orthographic precipitation form deep-rooted plants and grassland
- Valley oak
- Kellogg Creek, Livermore; Brushy Peak
- Oaks range towards mountains because they accumulate more water
Coastal Scrub
- Southern environment
- Sandy, but out from coast; drier conditions
- Sand does not retain water in shallow column; percolates deeper
- Coastal Scrub plants vs. trees; not enough water
- Dennery Canyon, Otay Mesa, near San Diego (150m)
Chaparral
- Coastal chaparral
- Northern environment
- Airmass causes adiabatic warming over Napa Valley slopes onwards
- Drought-adapted
- Mount George east of Napa Valley (500m)
Coastal Prairie
- Vast grassland with forested trees; conifers on edges
- Mendocino
- Volcanic activity caused ashflow that pooled in prairie areas and solidified into hard, concrete-like layers beneath surface
Coastal Redwood Forest
- Margin of coast with high rainfall
- Redwoods need 80m+ rainfall
- Jedediah Smith Redwoods Smith Park
- Coast Redwoods are some of oldest sp. in age and evolution; tallest species
- Fog reliance
- Ground level condensation and redwood interception on leaf interface
- Low taproots that do not rely on ground water
- Fog drip
- Secondary/third growth of redwoods
- 200-240ft tall; tallest 370
- thin, small foliage and cones
- Pyrophytic
- Older redwoods are fire-resistant; fire-retardant, thick bark
- Shredded bark used as insulation
- Stump sprouting; root remains and small trees grow via secondary growth
- Trunks grow into each other; crown shapes
- Flood-adapted
- Lateral upwards branching of roots
- Roots develop upwards towards soil surface and prevent asphyxiation
- Tree ring data of fire (fire scarring) and age
Closed-Cone Forests
- Closed-cone pines
- Glue pitch holds together
- Fires dry out pitch and cause brittleness
- Cone scales burst apart and eject seeds
Biodiversity
Tanoaks
- Lithocarpus densiflorus: Tanoak
- Acorns
- Coastal endemic
- Native American dumpsites in villages in Nevada and Arizona; trading
Douglas-fir
- Pseudotsuga menziesii: Douglas-fir
- Lumber/logging
- 25-35 years of growth → Harvest
- Industrial building
- Mousebutt cones; seed bracts
- Wind pollination
Rhododendron
- Low sunlight; high shades, buildings, high irrigation
- Base of mountains
Roosevelt Elk
- Largest elk ssp. in North America
- Northwestern portion endemic; Oregon, British Columbia
- Antlers
Banana Slug
- Ariolimax columbianus
- Muir Woods
- Large
- Emblem mascot for UCSC
- Moist forest environments
- Deaden tongue; analgesic/Novocaine
Central Valley
- Tilt Block
- Large flat valley in majority of CA
- Northern portion is Sacramento Valley, southern is San Joaquin
- Known for high agriculture
- ¼ food in US grown in Central Valley
- $40b, 15% CA jobs, 30% economy
- Tulare Lake shrunk
- Signature riparian forests
- Freshwater marshes
- No large trees; inundation by water
- Tules
- Used to extend by 2 million+ acres
- Levee draining, agriculture
- Foothill belt
Vernal Pools
- Hard pan layer
- Spring pools
- Mediterranean climate
- Specific ancient soil foundations in Baja California and California, esp. Central Valley
- Pools only drained by evaporation and transpiration; perched water
Small Flora
- Valley Downingia (Downingia pulchella)
- Pink onions (Allium hyalinum)
- Goldfields (Lasthenia sp.)
- Contra Costa goldfields (Lasthenia conjugens)
- Meadow foam (Limnathes douglasii)
- Pincushion Navarettia (Navarretia myersii)
- Tricolor monkeyflower (Mimulus tricolor)
- Sand spurrey (Spergularia macrotheca)
- Alkali Milkvetch (Astragalus tener var. tener)
- Succulent Owl’s Clover (Castilleja campestris ssp. succulentus)
- Chinese Camp Brodiaea (Brodiaea pallida)
- Colusa grass (Neostapfia colusana)
- Slender Orcutt grass (Orcuttia tenuis)
- State endangered/federally threatened
Animals
- Tadpole Shrimp (Lepidurus packardii)
- Federally endangered
- Encysted
- Vernal Pool Fairy Shrimp (Branchinecta lynchi)
- California Linderiella (Linderiella occidentalis)
- California Tiger Salamander (Ambystoma californiense)
- Eggs laid
- Burrows, estivation
- Great Egret, Great Blue Heron, Mallard
- Wading birds and waterfowl
- Crustaceans
- Tule Elk
- Low genetic diversity
- From ranch
Examples
- Jepson Prairie
- Vacaville
- Vernal pool complex
- 15-20 acre pools
- Mather Vernal Pools
- Mather field; Sunrise, Douglas Blvds.
- Phoenix Field
- Fair Oaks; Hazel Ave.
- 25 acres
- ½ myo