Midterm 1 Flashcards
What is ecology?
The study of how organisms interact with each other and with the environment in which they live.
What is evolution?
The study of how heritable traits change in populations over
successive generations
Valuing biodiversity
•Market value
-US pharmaceutical research and development investments: >$50 billion annually
•Ecosystem services
•Tourism/recreation
•Cultural and intrinsic value
•Science/research
•Enjoyment
Weather
current, short-term atmospheric conditions (e.g. temperature, rain, wind)
• “What should I wear today?”
•A big winter storm.
Climate
average atmospheric conditions/patterns/cycles over many years/millennia
• “What clothes do I need to own for winter in Davis, California?”
•Typical patterns of flooding in a region
latitude
•Latitude is described in degrees north or south of the equator
•Each degree north or south corresponds to ~69 miles of distance
latitude
•towards th poles, more of the sun’s ray are absorbed because they must travel a longer distance through the atmosphere (north pole)
•At and near the equator, sunlight strikes Earth at a steep angel, delivering more heat and light per unit of area
•Towards the poles, the Sun’s rays strikes Earth at an oblique angel and are spread over a larger area, so that their energy is diffused (south pole)
Hadley Cells
Hadley Cells are these patterns of atmospheric
circulation, with air rising near the equator (and raining), then descending as dry air at 30°N and 30°S
Clouds
= moisture (rain)
Dates are the same everywhere, but seasons are different in Northern and Southern Hemisphere
Equinox- March 20
Solstice- June 21
Equinox- September 22
Solstice- December 21
Intertropical Convergence Zone (ITCZ) ≈ Thermal Equator
• The band of clouds/moisture/rain that shifts up and down periodically through the seasons
• The area with highest solar intensity
Solar energy, Hadley cells, and climate
• Hadley cells: humid air rises (and forms clouds) near equator, drops as dry air about 30 degrees North and South.
• Average trend of humid tropical rainforest at equator, dry regions at 30°N and 30°S
• Because Earth’s axis is tilted, location of ITCZ/thermal equator moves (northernmost in June/July, southernmost in December/January).
• The E-W band around the Earth with the most rainfall (and clouds) shifts North or South at different times of year
Rain Shadow
•Winds pick up moisture over the ocean
•on the windward side, air rises, cools, and releases moisture ae rain or snow, creating a wet climate
•On leeward side, dry air descends and warms, resulting in little rain and arid conditions
atmosphere
-the air around the Earth
greenhouse effect
Radiation from surface radiated back down to Earth
•Earth’s surface is warmed by incoming solar radiation and by back radiation from greenhouse gasses. this additional warming increases the outward radition from the surface.
•Greenhouse gasses in the atm absorb much of the surface reradition and radiate it back to the surface
Greenhouse gas concentrations
-CO2
-N2O
CH4
CFC-12
CFC-11
HCF-22
HFC-134a
CFC
any of a class of compounds of carbon, hydrogen, chlorine, and fluorine, typically gases used in refrigerants and aerosol propellants. They are harmful to the ozone layer in the earth’s atmosphere owing to the release of chlorine atoms on exposure to ultraviolet radiation.
CFCs, ozone, and the chain reaction
- ozone is depleted to O2
-Effect of Montreal protocol
CO2 is measured
This CO2 is measured directly by using ice cores – we can literally find ancient air and measure CO2 concentration.
California Golbal heat record
• California is also generally warming – particularly in Southern California
• Relatively less snow is accumulating in the Sierra Nevada
mountains each Winter
•Of the 20 largest fires in California’s history (since
1932), 18 have occurred since 2000
cryosphere
frozen water on Earth’s surface
Decrease in global sea ice
•Sea ice has a typical annual pattern of increase and decrease.
•But the extent of sea ice has been declining over decades.
Glaciers (+ ice sheets)
Glaciers- land based
Ice sheets- is the term for a large glacier (>50,000 km2)
sea ice (+ ice shelves)
Iceberg- open ocean
Ice shelf- part of the Ocean
Cryosphere to Hydrosphere
Melting of ice sheets and other glaciers
hydrosphere
-liquid water on Earth’s surface
-sea levels are rising, the melting of the ice sheets and other glaciers
-Ocean absorbs heat, taking up any extra energy
-ocean warming up but slowly, causing tropical storms
-Ocean absorbs CO2 and acidities:
CO2 interacts with water (H2O) to create carbonic acid and free hydrogen ions.
Free hydrogen ions bind to carbonate to make hard-to-use
bicarbonate (rather than the carbonate that many organisms
need)
-As the ocean becomes more acidic effets marine life like corals, since they use CO2 to reinforce their shells
Representative Concentration Pathways (RCP)
trajectories for greenhouse gas concentrations
• 4 possible climate futures
• Time at which the global greenhouse gas emission
peaks and starts dropping
• RCP 2.6: global annual GHG emissions peak 2010-
2020, then decline significantly
• RCP 4.5: global annual GHG emissions peak 2040
• RCP 6.0: global annual GHG emissions peak 2080
• RCP 8.5: global annual GHG emissions continue at
current level
The number (2.6, 4.5, ….) refers to the strength of greenhouse effect (called “radiative forcing”) predicted in year 2100
Bigger number means more greenhouse effect (because of more greenhouse gases)
Levels of biological diversity
Genetic diversity: different in genotypes of individuals of the same species
Species diversity: different species occupying same habitat at same time
Other levels: different species assemblages in different habitats/ecosystems, species sharing evolutionary history, diversity in organisms’ ecological roles
Biodiversity
-Not ever where
-most in the tropical
Valuing biodiversity
• Market value: make money of plants
•Ecosystem services: bee pollinating
• tourism/recreation: open money to go into parks
• cultural and intrinsic value: a part of us
•science research: discover, know things
• enjoyment: positive impacts on people mental health
Quantifying biodiversity
Diversity Index- D
Species richness= total # species in habitat
Species evenness= relative abundance of each species
𝐷 = (𝑝1^−𝑝1)(𝑝2^−𝑝2) (𝑝3^−𝑝3)…(𝑝𝑛^−𝑝𝑛)
p is the proportion of individuals of that species
If the proportions were the same, but there were 200 frogs, how would D change?
Nothing would change, it’s all about propotion
Quantifying biodiversity count
In most cases, you cannot directly count every organism
Instead, you may use quadrats or point counts, and then
extrapolate from this sample to the whole group
Rarefaction curves
Instead of diversity as a function of area, we can look at
diversity as a function of the # individuals sampled
plots of the number of individuals on the x-axis against the number of species on the y-axis.
Diversity curves and D
A higher D value = steeper curve
Vicariance
The geographic separation of a species into separate populations through some sort of physical barrier
• continents were one Pangea)
• plate tectonics: broke Pangea into continents
• land bridge
• people building roads
Most living tissues
•70% water by weight
•Ions and small molecules
• macromolecules
Every living organism contains about these some proportions by weight of the four kinds of macromolecules
• Proteins: are chains of amino acids
- 20 amino acids
-building blocks of: Carbon, Nitrogen, Hydrogen, Oxygen
• nucleic acids: DNA and RNA
-Nucleic acids include RNA (ribonucleic acid) as well as DNA (deoxyribonucleic acid). Both types of nucleic acids contain
the elements carbon, hydrogen, oxygen, nitrogen, and phosphorus.
• carbohydrates (polysacchorides): Glucose is C6 H12 O6
- starch and glycogen
• Lipids
Earth’s atmosphere
The atmosphere contains gaseous forms of carbon and nitrogen, but these are not easy to convert to more useable forms.
Carbon and nitrogen
Carbon and nitrogen have to be “fixed” to become useful to most organisms. This kind of fixation was limited to
prokaryotes (bacteria and archaeons).
Carbon fixation
Carbon fixation is storing the atmospheric carbon as a
carbohydrate, typically as glucose
Only bacteria could do this originally, but green plants gained
this ability through a symbiosis with a cyanobacterium. A
cyanobacterial symbiont became the chloroplast organelle
Nitrogen-fixation
Nitrogen-fixation also occurs in bacteria and some archaeons. Gaseous nitrogen is comprised of two molecules of nitrogen with a triple bond between them. This triple bond is very hard to break and requires the enzyme nitrogenase
The product of nitrogen fixation is ammonia. In this form, nitrogen is available to many other organisms