In the previous sections of this three-part series, we explored why humans, not climate, played the much larger part in the extinction of Late Quaternary megafauna. However, this rather obvious reality has been obscured by a swathe of scientific papers with questionable conclusions. In this final piece of my series, I will aim to foster […]
In the first section of this three part series, we examined the background and defining characteristics of the Late Quaternary Extinctions and explored the nuances of climate change and ecology. In doing so, we showed that the support for climate as the central driver of the disappearance of so many species over the past few
Like many other people, the natural world has fascinated me from a very young age. I spent countless hours in my childhood drawing, reading about, and watching documentaries on animals such as tigers, brown bears, lions, various species of deer, buffalo, and so much more. I learned about the diets, physical attributes, and geographic distributions
On this blog, we’ve explored key aspects of the Pleistocene across multiple regions—South America, North America, Australia, and part of Asia. Today, we turn to Europe, a continent that has received perhaps the most attention in paleontological and Paleolithic research. The disproportionate wealth of information we have about Europe’s history is not only because of
Pleistocene Ice Ages conjure up notions of intense cold, massive glaciers, and an endless wilderness hosting a large and diverse community of animals. Most people understand that it was a very different world. Yet, if a layman were to go tens of thousands of years back in time, the landscapes they would encounter would not
See the forests in the pictures above? They are located in the Sikhote-Alin mountains in the Russian Far East. While undoubtedly scenic, a person not familiar with biodiversity in this part of the world may not understand what is so special about them. After all, they more or less just resemble forests in much of
Welcome to part 2 of this series on Late Pleistocene American extinctions. In Part 1, we introduced the debate regarding the Late Pleistocene extinctions in the Americas and thoroughly explained why humans were not simply a factor, but the main factor in the demise of megafauna. In this section, we will explore the evidence for
Nowhere is more central to the subject of the Late Pleistocene extinctions than the Americas. It was based on the staggering losses of megafauna here that an American geoscientist, Paul Martin, proposed his theory that the first humans to enter the New World were responsible for the elimination of most large-bodied species through overhunting, also
There are few places on the planet as distinctive as Australia. With its isolated geographical location and iconic landscapes, it captures the imagination of people the world over. Picturesque red deserts, glistening beaches, and Eucalyptus woodlands may provide its most characteristic scenery, but arcane rainforests, snow-covered mountains, and much more can be found on the
The world was a very different place during the height of last ice age-known as the Last Glacial Maximum (LGM)-with very different climates, landscapes, and floral and faunal distributions compared to our current epoch, the Holocene. The exact chronology of this period varies according to the source but it is generally considered to be the