Ocean Acidification Flashcards
Atmospheric CO2: now and in the past
- Charles Keeling (San Diego’s Scripps Institution of Oceanography) receives the Medal of Science in 2001.
- Increase of ~ 2.7 ppm/year in the last 15 years.
- 415 ppm is thought to have been attained 4.5 million years ago in the Pliocene.
Causes and mechanism
- Fossil fuel combustion and deforestation are the two main contributors.
- Total emissions since the industrial revolution exceed 1,500 billion tons.
- 50% of total emitted CO2 remains in the atmosphere, 25-30% is absorbed by the oceans, and 20-25% by land.
Issue of OA to Calcifying Organisms
- Chemical reactions: CO2(aq) + H2O H2CO3; H2CO3 HCO3- + H+; HCO3- CO32- + H+; CaCO3(s) Ca2+ + CO32-.
- Ocean Acidification: CO2 (aq) + H2O + CO32- 2HCO3-.
- Impact on marine organisms: pteropods, foraminifera, coccolithophores, corals, mussels, sea urchins, brittlestars, algae, and more.
Issue of OA to Fishes
Physiological implications: hypercapnia symptoms, metabolic performance, activity, reproduction, early life survival and growth, neurosensory and cognitive impairment, respiratory acid-base disturbances.
Overall
pH decrease from 8.2 to 8.1 since pre-industrial times (26% increase in H+).
Predicted reduction of pH by 0.15-0.45 units by 2100.
pH of 7.8 not experienced in seawater for the last 50 million years.
pH decrease from 8.2 to 7.7 triples the concentration of [H+].
Historical Facts
Charles Keeling’s research on atmospheric CO2 levels.
CO2 emissions since the industrial revolution.
Human release of CO2 in 2019.
Is Ocean Acidification Happening?
pH decreasing at a rate of about 0.0012-0.002/year.
Trends observed at Station ALOHA and the Hawai‘i Ocean Time-series (HOT) Program
Proof of OA affecting Calcifying Organisms
Impact on corals, coccolithophores, pteropods, Dungeness crabs, gastropods, and more.
Experimental manipulation studies showing varied responses to increasing levels of seawater CO2.
What does ocean acidification do ?
decreases pH and carbonate ion concentration, affecting calcifying organisms’ ability to build their shells and skeletons.
What are the chemical equations?
CaCO3(s) Ca2+ + CO32-
Solubility product (Ksp) determines saturation levels:
If W > 1, supersaturation.
If W < 1, undersaturation
Types of Carbonate Minerals
- Calcite and Aragonite
- Aragonite is about 1.5 times more soluble than calcite
Aragonite saturation depth
- Varies widely across oceans
Pressure affects solubility; harder to calcify at depth - In some shallow areas, sediments accumulate carbonate minerals, while dissolution occurs in deeper areas.
Impact of Antropogenic CO2
Shallowing of saturation depth with OA observed
Differences between oceans due to biological respiration
OA in coastal waters
pH changes expectations from CO2 uptake alone
Various drivers: CO2, light, upwelling, chlorophyll, temperature, alkalinity, salinity, PDO
Direct and Indirect Causes of OA in Coastal Waters
Direct: CO2 increase, acid rain, upwelling
Indirect: Nutrient inputs, freshwater delivery, trace metal bioavailability