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Biogeochemistry
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🪨biogeochemistry review

14.2 Ocean Acidification and Marine Ecosystems

Citation:

Ocean acidification is a growing concern as our oceans absorb more CO2 from the atmosphere. This process lowers seawater pH, making it harder for marine life to build shells and skeletons. It's like the ocean is getting a bad case of heartburn.

The impacts ripple through marine ecosystems, affecting everything from tiny plankton to big fish. Scientists are working hard to understand and address this issue, studying how different species cope and exploring ways to protect our oceans from further damage.

Understanding Ocean Acidification

Definition of ocean acidification

  • Ocean acidification decreases pH in world's oceans through absorption of atmospheric carbon dioxide (CO2)
  • Increased atmospheric CO2 levels stem from burning fossil fuels, deforestation, and land-use changes
  • Chemical reactions in seawater produce carbonic acid ($CO2 + H2O → H2CO3$)
  • Carbonic acid dissociates into hydrogen and bicarbonate ions ($H2CO3 → H+ + HCO3-$)
  • Carbonate system in seawater maintains equilibrium between CO2, HCO3-, and CO32- ions
  • pH decrease shifts equilibrium towards more HCO3- and fewer CO32- ions

Impacts on marine ecosystems

  • Calcifying organisms struggle to form calcium carbonate shells and skeletons (corals, mollusks, crustaceans)
  • Certain plankton species affected (coccolithophores)
  • Physiological stress disrupts acid-base balance in marine organisms
  • Increased energy expenditure for internal pH maintenance
  • Behavioral changes alter sensory perception and decision-making in fish
  • Impaired predator-prey interactions
  • Primary production potentially increases in some phytoplankton species
  • Calcifying phytoplankton experience decreased productivity
  • Nutrient cycling alters nitrogen fixation rates and phosphorus availability

Consequences and Research on Ocean Acidification

Consequences for biodiversity

  • Biodiversity loss leads to decline in species reliant on calcium carbonate structures
  • Community composition shifts
  • Food web disruption changes prey availability for higher trophic levels
  • Potential collapse of certain fisheries
  • Ecosystem services impacted through reduced coastal protection from coral reef degradation
  • Decreased carbon sequestration by calcifying organisms
  • Economic losses in fisheries and aquaculture industries
  • Synergistic effects with other stressors exacerbate impacts (ocean warming, deoxygenation, pollution)

Role of biogeochemical research

  • Monitoring and data collection involve long-term pH and carbonate chemistry measurements
  • Global observation networks established
  • Experimental studies include mesocosm experiments simulating future ocean conditions
  • Laboratory studies focus on individual species responses
  • Modeling efforts develop predictive models for future ocean acidification scenarios
  • Ecosystem models assess long-term impacts
  • Mitigation strategies explore carbon dioxide removal techniques
  • Restoration of coastal blue carbon ecosystems (mangroves, seagrasses)
  • Policy implications inform international climate agreements
  • Local and regional adaptation strategies developed
  • Interdisciplinary collaboration integrates biogeochemistry with marine biology and ecology
  • Social scientists contribute to socio-economic impact assessment