The Geological Record of Ocean Acidification¶
Hönisch. (2012). The Geological Record of Ocean Acidification.
Cited by¶
1 citation across 1 artifact.
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Domain-specific¶
- Ocean Acidification
- Ocean chemistry — the mechanistic core: the four-variable carbonate system (pH, total alkalinity, dissolved inorganic carbon, pCO₂), the Revelle buffer factor, and the aragonite-versus-calcite saturation horizons that fix the load-bearing saturation-state diagnostic. Calcifier biology and reef ecology — the biological train: saturation state relative to a named mineral phase predicts which corals, pteropods, oysters, urchins, coccolithophorids, and foraminifera thin, fail to calcify, or dissolve, with aragonite-builders crossing into danger before calcite-builders. Climate science — the ocean as carbon sink: uptake of roughly a quarter of cumulative anthropogenic CO₂, the buffering decline as the Revelle factor rises, and the warming-versus-uptake feedbacks that set the chemistry's trajectory. Paleoceanography — past acidification events as analogues: the PETM and end-Permian recovered from boron-isotope and B/Ca proxies, read to anticipate present-day calcifier responses
This sourceA review of ocean-acidification events over the past ~300 million years, including the PETM and end-Permian, using boron-isotope and B/Ca proxies to infer past seawater carbonate chemistry.
Supported in partVerified against the work's full text
“the boron isotopic composition (d11B) of marine carbonates reflects changes in seawater pH, the trace element (such as B, U, and Zn)–to-calcium ratio of benthic and planktic foraminifer shells records ambient [CO23−]”
- Ocean chemistry — the mechanistic core: the four-variable carbonate system (pH, total alkalinity, dissolved inorganic carbon, pCO₂), the Revelle buffer factor, and the aragonite-versus-calcite saturation horizons that fix the load-bearing saturation-state diagnostic. Calcifier biology and reef ecology — the biological train: saturation state relative to a named mineral phase predicts which corals, pteropods, oysters, urchins, coccolithophorids, and foraminifera thin, fail to calcify, or dissolve, with aragonite-builders crossing into danger before calcite-builders. Climate science — the ocean as carbon sink: uptake of roughly a quarter of cumulative anthropogenic CO₂, the buffering decline as the Revelle factor rises, and the warming-versus-uptake feedbacks that set the chemistry's trajectory. Paleoceanography — past acidification events as analogues: the PETM and end-Permian recovered from boron-isotope and B/Ca proxies, read to anticipate present-day calcifier responses
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Registry ID ref:bf438c896173 · see in the full table