Holocene extinction

The Holocene or Anthropocene extinction is an ongoing extinction event caused by human activity during the current geological epoch, impacting diverse families of plants and animals, including mammals, birds, reptiles, amphibians, fish, and invertebrates, as well as both terrestrial and marine species. It is sometimes also called the sixth extinction (though this can also describe the Capitanian).

Current extinction rates are estimated at 100 to 1,000 times higher than natural background extinction rates. The Holocene extinction was preceded by the Late Pleistocene extinctions at the end of the last ice age (to which human activity also likely contributed) and the extinctions caused by Polynesian expansion.

The Holocene extinction continues into the 21st century, driven by anthropogenic climate change, destruction of wetlands, deforestation, overfishing, ocean acidification, human population growth, economic growth, and increasing consumption, particularly among affluent societies. Factors such as rising meat production and the destruction of critical habitats compound these issues. Other drivers include overexploitation of natural resources, pollution, and climate change-induced shifts in ecosystems.

Major extinction events during this period have been recorded across all continents, including Africa, Asia, Europe, Australia, North and South America, and various islands.