Boron isotope evidence for oceanic carbon dioxide leakage during the last deglaciation
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- Type
- article
- Published
- 2015-02-11
- Cited by
- 196
- References
- 104
- OpenAlex
- https://openalex.org/W2012604679
- Semantic Scholar
- https://api.semanticscholar.org/CorpusID:2510709
Keywords
Deglaciation, Oceanography, Geology, Carbon dioxide in Earth's atmosphere, Deep sea
References
- Climatological mean and decadal change in surface ocean pCO2, and net seaair CO2 flux over the global oceans
- Ground-truthing the boron-based proxies
- The Seesaw Effect
- Diatom productivity in the equatorial Pacific Ocean from the last glacial period to the present: A test of the silicic acid leakage hypothesis
- Constraint of the CO2 rise by new atmospheric carbon isotopic measurements during the last deglaciation
- Preferential dissolution of benthic foraminiferal calcite during laboratory reductive cleaning
- Eastern equatorial Pacific cold tongue during the Last Glacial Maximum as seen from alkenone paleothermometry
- Treatise on geochemistry
- A global ocean carbon climatology: Results from Global Data Analysis Project (GLODAP)
- Multispecies approach to reconstructing eastern equatorial Pacific thermocline hydrography during the past 360 kyr
- Calibration of Mg/Ca thermometry in planktonic foraminifera from a sediment trap time series
- Palaeoceanography: Antarctic stratification and glacial CO2
- Links between iron supply, marine productivity, sea surface temperature, and CO2 over the last 1.1 Ma
- Radiocarbon age anomaly at intermediate water depth in the Pacific Ocean during the last deglaciation
- Carbon dioxide effects of Antarctic stratification, North Atlantic Intermediate Water formation, and subantarctic nutrient drawdown during the last ice age: Diagnosis and synthesis in a geochemical box model
- Quantitative interpretation of atmospheric carbon records over the last glacial termination
- Deep water formation in the North Pacific and deglacial CO2 rise
- Boron and magnesium isotopic composition of seawater
- A study of cleaning procedures used for foraminiferal Mg/Ca paleothermometry
- El Niño–Southern Oscillation–like variability during glacial terminations and interlatitudinal teleconnections
Cited by
- Southwest Pacific deep water carbonate chemistry linked to high southern latitude climate and atmospheric CO2 during the Last Glacial Termination
- An Early Pleistocene atmospheric CO2 record based on pedogenic carbonate from the Chinese loess deposits
- Proxy Development and Application for Reconstructing the Surface Ocean Carbonate System
- Efficient separation of boron using solid-phase extraction for boron isotope analysis by MC-ICP-MS
- A new method for calibrating a boron isotope paleo‐pH proxy using massive Porites corals
- The last termination in the central South Atlantic
- Synchronous centennial abrupt events in the ocean and atmosphere during the last deglaciation
- Geochemistry: When carbon escaped from the sea
- Revisiting carbonate chemistry controls on planktic foraminifera Mg / Ca: implications for sea surface temperature and hydrology shifts over the Paleocene–Eocene Thermal Maximum and Eocene–Oligocene Transition
- Reconstructing Ocean pH with Boron Isotopes in Foraminifera
- Links between eastern equatorial Pacific stratification and atmospheric CO2 rise during the last deglaciation
- A New method for identifying possible causal relationships between CO2, total solar irradiance and global temperature change
- Deep‐sea coral δ13C: A tool to reconstruct the difference between seawater pH and δ11B‐derived calcifying fluid pH
- A review on the determination of isotope ratios of boron with mass spectrometry.
- CO2 over the past 5 million years : Continuous simulation and new δ11B-based proxy data
- Covariation of deep Southern Ocean oxygenation and atmospheric CO2 through the last ice age
- A record of Neogene seawater δ11B reconstructed from paired δ11B analyses on benthic and planktic foraminifera
- Evolution of the stable carbon isotope composition of atmospheric CO2 over the last glacial cycle
- Planktic foraminifer and coccolith contribution to carbonate export fluxes over the central Kerguelen Plateau
- Capture of Hyperthermal CO2 by Amorphous Water Ice via Molecular Embedding.
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