A discourse on habitability: The Anthropocene as ecological dyad

The Holocene, as depicted in Figure 1 below, is formally the current geological epoch and represents the previous ∼11,500 calendar years to present. During the Holocene, environmental change occurred naturally and Earth’s regulatory capacity maintained the conditions that enabled human development. Regular temperatures, freshwater availability and biogeochemical flows all stayed predominately in a narrow range. Now, in the primeval stages of the Anthropocene, human activities have reached Continue reading