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- W4210607316 abstract "Abstract The carbon isotope 13 C is commonly used to attribute the last deglacial atmospheric CO 2 rise to various processes. Here we show that the growth of the world's largest reef system, the Great Barrier Reef (GBR), is marked by a pronounced decrease in δ 13 C in absolutely dated fossil coral skeletons between 12.8 and 11.7 ka, which coincides with a prominent minimum in atmospheric δ 13 CO 2 and the Younger Dryas. The event follows the flooding of a large shelf platform and initiation of an extensive barrier reef system at 13 ka. Carbon cycle simulations show the coral δ 13 C decrease was mainly caused by the combination of isotopic fractionation during reef carbonate production and the decomposition of organic land carbon on the newly flooded shallow‐water platform. The impacts of these processes on atmospheric CO 2 and δ 13 CO 2 , however, are marginal. Thus, the GBR was not contributing to the last deglacial δ 13 CO 2 minimum at ∼12.4 ka." @default.
- W4210607316 created "2022-02-08" @default.
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- W4210607316 date "2022-02-14" @default.
- W4210607316 modified "2023-10-18" @default.
- W4210607316 title "Role of the Deglacial Buildup of the Great Barrier Reef for the Global Carbon Cycle" @default.
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- W4210607316 doi "https://doi.org/10.1029/2021gl096495" @default.
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