STOP EXTINCTION WITH A DONATION

We represent all the staff of the wildlife protection solution and the myriad wildlife species we are lucky to protect.

The good news is that we can stop mass extinction. There is no way to transfer the effects of unexpected asteroids or to stop the volcanic eruption, but the current extinction rate is boosted by human activities. In other words, this trend may be reversed by human activity. We can reduce the extinction rate through policy changes that can increase conservation efforts and reduce greenhouse gas emissions and thereby mitigate climate change. Research on the history of the earth may play a very important role in this research. If we can understand a series of events that led to extinction of large species in the past, we can better break this chain today. If we can understand the very fragile nature of the species during mass extinction, we may be able to focus more on our conservation efforts. Investigating the past extinction of the Earth may be one of the keys to protect future biodiversity

The distinction between "extinction" and "extinction of the background" is very important in understanding the importance of mass extinction. For thousands of years, scientists can expect that some species will be extinct - this is "extinction of the background". However, during mass extinction many species have been extinct in a shorter period of time. It can be said that life history on the earth is interrupted by "boredom" (the background is in danger) and "panic" (mass extinction). Back in Bd, Kolbert explored why fungi spread so quickly around the world. Because it is a component of a popular pregnancy test, some people think humans have misdirected Bd to the world in the 1960s. Others are guessing that after the human spread the bullfight in Asia, Africa and South America, the bullring of North America will spread to other continents.

Pleistocene extinction is one of the smaller extinctions and one of the relatively new extinctions. It is well known that North America, and to some extent Eurasian gigantic animals disappeared during the last glacial age. It seems that extinction has occurred in a relatively limited period from 10,000 to 120,000 years ago. In North America, losses are very large, such as furry mammoths (in isolated crowds about 4,000 years ago), mastodons, huge beavers, gigantic sloths, swords and cats, and camels in North America. There are several. The possibility of rapid extinction of these large animals was first proposed at the beginning of the 20th century due to over hunting; research on this hypothesis continues today. Over-hunting seems to be a factor of extinction in many parts of the world.