Forest ecosystems are one of Earth’s primary biomes: they provide a diverse suite of ecosystems goods and services crucial for societal well-being and play a crucial role in our planet’s carbon cycle. However, great uncertainties exist regarding the quantification, dynamics, and driving processes of terrestrial carbon cycling, and thus also the fate of forested regions. Dendrochronological methods are remarkably well suited to investigate forest carbon cycling on long and temporally precise time-scales and at tree-level to continental spatial scales.