noun a geological epoch that lasted from about 2,588,000 to 11,700 years ago, characterized by the presence of humans and the extinction of many large mammals
The Pleistocene is a geological epoch that lasted from about 2.6 million to 11,700 years ago, characterized by repeated glaciations.
Biologists may study the Pleistocene to understand the impact of environmental changes on the evolution of species.
Archaeologists often study the Pleistocene period to learn about early human ancestors and their way of life.
The Pleistocene is studied in climate science to understand past climate changes and their effects on Earth's ecosystems.
In paleontology, the Pleistocene is an important period as it marks the appearance and evolution of many modern mammal species.
In the field of paleontology, writers may discuss the Pleistocene epoch in articles, books, or research papers about prehistoric life and climate change.
Geologists use the term Pleistocene when studying the Earth's history and the formation of various geological features during this epoch.
Biologists may refer to the Pleistocene when studying the evolution of species, including human ancestors, and the impact of climate change on biodiversity.
Climate scientists analyze data from the Pleistocene era to understand past climate patterns and predict future climate trends.
Archaeologists study artifacts and human remains from the Pleistocene era to learn about early human societies and cultural practices.