noun a geological epoch which began at the end of the Pleistocene (around 11,700 years ago) and continues to the present
The Holocene is of particular interest in environmental science due to its significance in understanding past climate changes and human interactions with the environment.
The Holocene is a geological epoch that began approximately 11,700 years ago, following the last Ice Age. It is characterized by the presence of human activity and significant climate change.
In anthropology, the Holocene is often studied in relation to human evolution, cultural development, and the impact of humans on the environment.
Archaeologists study the Holocene period to uncover evidence of ancient civilizations, human behavior, and technological advancements during this time.
Climate scientists use data from the Holocene period to analyze long-term climate trends and fluctuations, as well as to predict future climate patterns.
The Holocene is often referenced in writings about climate change and environmental history, as it represents the current geological epoch characterized by human activity.
Geologists study the Holocene epoch to understand changes in Earth's climate, landscapes, and ecosystems during this relatively recent period.
Archaeologists use the Holocene epoch as a framework for dating and interpreting human history and cultural developments.
Ecologists study the impact of human activities on ecosystems and biodiversity during the Holocene epoch to inform conservation efforts and environmental management.
Historians analyze historical events and human societies within the context of the Holocene epoch to understand the long-term impacts of human civilization.