noun The Pleistocene is a geological epoch that lasted from about 2.6 million to 11,700 years ago, characterized by multiple ice ages and the presence of early humans.
adjective Pleistocene can also be used as an adjective to describe things related to or characteristic of this geological epoch.
The Pleistocene epoch is a geological time period that lasted from about 2.6 million to 11,700 years ago, characterized by multiple ice ages and the presence of large mammals such as mammoths and saber-toothed cats.
Ecologists study the Pleistocene to understand how past environmental changes influenced biodiversity and ecosystem dynamics.
The Pleistocene is relevant in biology for its impact on the evolution and distribution of plant and animal species.
Archaeologists often study Pleistocene sites to learn about early human cultures and their interactions with the environment.
Researchers study the Pleistocene to understand past climate changes and how they may relate to current climate patterns.
In paleontology, the Pleistocene is known for the extinction of many large mammal species and the emergence of early human ancestors like Homo erectus.
In the field of paleontology, writers may use the term 'Pleistocene' when discussing the geological epoch that lasted from about 2.6 million to 11,700 years ago.
Geologists may refer to the Pleistocene epoch when studying rock formations and sediment layers from that time period.
Biologists may use the term 'Pleistocene' when studying the evolution of plants and animals during that epoch.
Archaeologists may use the Pleistocene epoch as a reference point when dating ancient human artifacts and settlements.