The Holocene epoch is a geologically defined period corresponding to the current interglacial warming period, having succeeded the Pleistocene epoch. This era is characterized by substantial global climate stability and significant changes in sea levels and global climate patterns compared to previous geological ages. The transition into the Holocene is often marked by a profound shift in terrestrial ecosystems, allowing for the development of complex biological and human societies. Studying this period is critical for understanding the mechanisms of orbital forcing, glacial-interglacial cycles, and the long-term response of the Earth system to climatic shifts.