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- W3089762312 abstract "<p>During the last glacial period atmospheric CO<sub>2</sub> and temperature in Antarctica varied together on millennial timescales, with CO<sub>2</sub> abruptly increasing by 10-20 ppm in <1000 years in some cases. The exact causes of these rapid CO<sub>2</sub> changes during a cold glacial climate remain unclear. Here we examine the role of ocean carbon storage and atmospheric exchange by applying the boron isotope-pH (CO<sub>2</sub>) proxy to Globigerina bulloides from core site TAN110628 located in the Pacific Sector of the Southern Ocean.&#160; By reconstructing the surface carbonate system at TAN110628 at high temporal resolution (1 sample every 1 kyr) from 30 to 64 kyr we are able to fully constrain the nature of carbon leakage from the Sub Antarctic Zone of the Southern Pacific Ocean associated with these millennial-scale changes in atmospheric CO<sub>2</sub>.&#160; This provides unique insights into the causes of abrupt changes in atmospheric CO<sub>2</sub> during Marine Isotope Stage 3 and the last termination.&#160;</p>" @default.
- W3089762312 created "2020-10-08" @default.
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- W3089762312 date "2020-03-10" @default.
- W3089762312 modified "2023-09-25" @default.
- W3089762312 title "Millennial-scale oceanic CO2 release during marine isotope stage 3" @default.
- W3089762312 doi "https://doi.org/10.5194/egusphere-egu2020-17440" @default.
- W3089762312 hasPublicationYear "2020" @default.
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