The development of carbon isotopes at the bulk sediment,
foraminifera shell, and compound-specific (molecular)
level, especially when combined with complementary evidence on biota, nutrients, ocean chemistry and redox, and
modeling, has opened new pathways to unravel the complex interplay between fluctuations of the main carbon
pools between the atmosphere, the living biosphere, and
carbon buried in the sediments and their interactions with
and impact on global climate at multiple temporal and spatial scales.
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