However, this is only the beginning of a much more intricate story written in rock, ice, and fossil. This structure allows scientists to correlate rock layers across the globe and reconstruct the history of life and planetary change with remarkable precision.
Human Impact Defines the Current Geological Epoch, the Anthropocene
Many scientists argue that the Holocene has ended and that we have entered a new epoch called the Anthropocene. The most prominent of these is the Global Boundary Stratotype Section and Point (GSSP) in Varna, Italy, which marks a significant cooling event and the first appearance of certain cold-water marine fossils around 2.
Entering the Quaternary The Quaternary period is the most recent of the three periods of the Cenozoic Era, beginning approximately 2. The current interglacial period, which began roughly 11,700 years ago, is known as the Holocene epoch.
Human Impact Defines the Current Geological Epoch, the Anthropocene
This period is defined by a relatively stable and warm climate that allowed human civilizations to flourish, develop agriculture, and build cities. We currently reside in a specific epoch within this period, defined by the profound and lasting impact of a single species.
More About What geological period are we in
Looking at What geological period are we in from another angle can help expand the discussion and give readers a second clear paragraph under the same section.
More perspective on What geological period are we in can make the topic easier to follow by connecting earlier points with a few simple takeaways.
