Ocean acidification
node · earth · Global ocean
The change in seawater carbonate chemistry caused by the ocean absorbing a large share of the carbon dioxide emitted to the atmosphere — roughly a quarter to a third of anthropogenic emissions. Dissolved carbon dioxide forms carbonic acid, which dissociates and releases hydrogen ions; those ions react with carbonate ions to form bicarbonate. Two things therefore happen at once: pH falls, and the concentration of the carbonate ion that corals need to build aragonite falls with it. Surface ocean pH has declined by roughly 0.1 units since the pre-industrial period, which on a logarithmic scale is an increase in hydrogen ion concentration of about thirty per cent. For a reef the operative quantity is the aragonite saturation state: as it drops, calcification costs the coral more energy and net reef accretion slows even where no coral has died. Acidification and bleaching share a cause and share nothing else — different timescale, different mechanism, different tissue. A reef can be entirely unbleached and still be losing its carbonate budget.
Read in · 1
Evidence · 2
Timeline
No dated observations are stored for this object. Atlas shows what was observed and when — it does not infer a history.
Connections · 1
- Reef carbonate budgetaffects
Assembled narrative · 1
Assembled from 15 blocks · 2 evidence · 5 related
- Story
- The change in seawater carbonate chemistry caused by the ocean absorbing a large share of the carbon dioxide emitted to the atmosphere — roughly a quarter to a third of anthropogenic emissions. Dissolved carbon dioxide forms carbonic acid, which dissociates and releases hydrogen ions; those ions react with carbonate ions to form bicarbonate. Two things therefore happen at once: pH falls, and the concentration of the carbonate ion that corals need to build aragonite falls with it. Surface ocean pH has declined by roughly 0.1 units since the pre-industrial period, which on a logarithmic scale is an increase in hydrogen ion concentration of about thirty per cent. For a reef the operative quantity is the aragonite saturation state: as it drops, calcification costs the coral more energy and net reef accretion slows even where no coral has died. Acidification and bleaching share a cause and share nothing else — different timescale, different mechanism, different tissue. A reef can be entirely unbleached and still be losing its carbonate budget.
- Knowledge
- Reef carbonate budget
- Ocean acidification
- Connections
- Coral calcification
- Reef carbonate budget
- A measured decline in Great Barrier Reef coral calcification is published
- Coral calcification
- Ocean acidification
- Parrotfish (Scarinae)
- Evidence
- The ocean has absorbed a large share of anthropogenic carbon dioxide emissions and surface ocean pH has declined by roughly 0.1 units since the pre-industrial period, corresponding to an increase in hydrogen ion concentration of around thirty per cent. V55 verification basis: not consulted in this session; these are standard assessed figures stated from the producing model's knowledge of the assessment, not read from the chapter, and no confidence language from the report is reproduced.
- Calcification in massive Porites on the Great Barrier Reef declined by about fourteen per cent from 1990, a change the authors described as without precedent in the preceding four centuries of the skeletal record. V55 verification basis: not consulted; the figure is stated from the producing model's knowledge. This result has been the subject of subsequent methodological debate that could not be reviewed here.
Observed changes · 0
No public Signals are attached to this object. Signals show what changed and when it was observed — never a direction or a rank.
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