Chapter 46 - Ecosystem Ecology Flashcards
Ecosystem Ecology
Ecosystem consists of organisms in a community and their physical environment, mutually influencing each other over time.
Carbon Cycle
The chemistry of life is, to a first approximation, the chemistry of carbon.
- Most carbon stored in sediments/sedimentary rock, then deep ocean water reservoirs
- Marine photosynthesis and respiration balance in terms of carbon
The Bends
Nitrogen doesn’t react with much
If you go too deep diving, nitrogen reacts in your blood makes you
“drunk” as it makes bubbles in your tissues and blood + bursts alveoli in as you swim to surface
Nitrogen cycle
Nitrogen is introduced through dead plants and animals and feces (becomes NH3) = ammonification
Is used by plants through roots OR converted to N2 through nitrification / annamox
Nitrogen fixation turns N2 from air into NH3 to be used by plants through roots too
Phosphorous
Found in mountains / rocks
Weathering = released and used by plants = animals eat plants = they die + poop out the phos = back into plants OR runoff into ocean
In ocean cycled / upwelled / becomes sediments that eventually become mountains again
Human Impact on CO2 Levels
Industrial Revolution led to a significant increase in CO2 levels.
Approximately half of human-generated CO2 enters the atmosphere, the rest accumulates in oceans!!!, vegetation, and soils.
Seasonal cycle of CO2 levels
Increase and decrease with higher rates of photosynthesis in the summer and the lower rates in the winter (except in regions near the equator)
Increase in CO2 leads to warming. Conversely, high temperatures can decrease CO2 levels as plants thrive in heat, leading to increased photosynthesis.
So… no plants + CO2 increase = warming
C-transfers and Trophic Levels
Local c transfers go up from primary carbon producers (ex. grass) at the first trophic level
Only 10% of biomass from each trophic level is passed up.
Explanation: Some biomass used for metabolism; temperature tends to follow CO2 levels.
Both energy and carbon are transferred
How do we know humans are the cause of CO2 increases
Atmospheric carbon lacking the isotope C13 is increasing - which comes from burning fossil fuels
Fossil fuels = no C13, C12
Ratio of C12 to C13 increasing
Timeline of oxygen
A time line shows:
- something releases O2 about 2
billion years ago
- then more about 600 million years
ago
- biotic actions changed conditions
→ coincided/predicated animal
evolution
The Keeling Curve
Keeling curve records changing CO2 levels in the atmosphere over time
CO2 cycles up and down over the year (max in April, min in September)
Observation: Keeling’s work showed a 25% increase in atmospheric CO2 levels over the past 50 years - steady increase
Autotrophs
Photosynthetic organisms (“self feeders”) - aka primary producers
Consumed by primary consumers