What is Mass Extinction?
A mass extinction refers to a short period of geological time in which a very high percentage of biodiversity, or distinct species including bacteria, amphibians, fish, fungi, plants, mammals, birds, reptiles, and invertebrates die in very high numbers. Here, it is important to note that a “short” period in geological time consists of thousands or millions of years.
Extinctions are a part of the evolution process, which occur naturally and periodically and there is a background rate at which the extinctions occur. But in mass extinction events, the extinction rate is much higher than normal. In a mass extinction, at least 75% of species go extinct within a relatively (by geological standards) short period.
6th Mass Extinction – Holocene Extinction
The Holocene extinction is also known as the 6th mass extinction. It is characterized by the massive extinction of biodiversity due to human activities. It is an ongoing process that began around 11,700 years ago.
According to scientists, we are currently in the middle of Holocene extinction. Understanding and addressing the causes of the Holocene extinction is crucial for the long-term health of ecosystems and the well-being of the planet.
Table of Content
- Holocene Extinction?
- What is Mass Extinction?
- Holocene Extinction Timeline
- Human Activity in Holocene Extinction
- Results of Holocene Extinction
- Can Holocene Extinction be Stopped?
- Conclusion – Holocene Extinction
- FAQs on Holocene Extinction
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