Middle Miocene Climatic OptimumFrom Wikipedia, the free encyclopedia The Middle Miocene Climatic Optimum (MMCO), sometimes referred to as the Middle Miocene Thermal Maximum (MMTM),[1] was an interval of warm climate during the Miocene epoch, specifically the Burdigalian and Langhian stages.[2]
The Middle Miocene Climatic Optimum (MMCO), sometimes referred to as the Middle Miocene Thermal Maximum (MMTM),[1] was an interval of warm climate during the Miocene epoch, specifically the Burdigalian and Langhian stages.[2]