Pleistocene megafauna is the set of large animals that lived on Earth during the Pleistocene epoch. Pleistocene megafauna became extinct during the Quaternary extinction event resulting in substantial changes to ecosystems globally. The role of humans in causing Pleistocene megafaunal extinctions is controversial.
Megafauna are any animals with an adult body weight of over 45 kilograms (99 lb). Pleistocene megafauna include the straight-tusked elephant, cave bear (Ursus spelaeus), interglacial rhinoceros (Stephanorhinus), heavy-bodied Asian antelope (Spirocerus), Eurasian hippopotamuses, woolly rhinoceros, mammoths, giant deer, sabre-toothed cat (Homotherium), cave lion, and the leopard in Europe.
List of Pleistocene megafauna
|American lion||North America|
|Woolly mammoth||Eurasia and North America|
The last glacial period, commonly referred to as the 'Ice Age', spanned 125,000 to 14,500 years ago and was the most recent glacial period within the current ice age which occurred during the final years of the Pleistocene epoch. The Ice Age reached its peak during the last glacial maximum, when ice sheets commenced advancing from 33,000 years BP and reached their maximum positions 26,500 years BP. Deglaciation commenced in the Northern Hemisphere approximately 19,000 years BP, and in Antarctica approximately 14,500 years BP which is consistent with evidence that this was the primary source for an abrupt rise in the sea level 14,500 years ago.
A vast mammoth steppe stretched from the Iberian peninsula across Eurasia and over the Bering land bridge into Alaska and the Yukon where it was stopped by the Wisconsin glaciation. This land bridge existed because more of the planet's water was locked up in glaciation than now and therefore the sea levels were lower. When the sea levels began to rise this bridge was inundated around 11,000 years BP. During the last glacial maximum, the continent of Europe was much colder and drier than it is today, with polar desert in the north and the remainder steppe or tundra. Forest and woodland was almost non-existent, except for isolated pockets in the mountain ranges of southern Europe.
The fossil evidence from many continents points to the extinction mainly of large animals at or near the end of the last glaciation. These animals have been termed the Pleistocene megafauna. Scientists frequently define megafauna as the set of animals with an adult body weight of over 45 kg (or 99 lbs). Across Eurasia, the straight-tusked elephant became extinct between 100,000 and 50,000 years BP. The cave bear (Ursus spelaeus), interglacial rhinoceros (Stephanorhinus), heavy-bodied Asian antelope (Spirocerus), and the Eurasian hippopotamuses died out between 50,000 and 16,000 years BP. The woolly rhinoceros and mammoths died out between 16,000 and 11,500 years BP. The giant deer died out after 11,500 BP with the last pocket having survived until about 7,700 years BP in western Siberia. A pocket of mammoths survived on Wrangel Island until 4,500 years BP. As some species became extinct, so too did their predators. Among the top predators, the sabre-toothed cat (Homotherium) died out 28,000 years BP, the cave lion 11,900 years BP, and the leopard in Europe died out 27,000 years BP. The Late Pleistocene was characterized by a series of severe and rapid climate oscillations with regional temperature changes of up to 16 °C, which has been correlated with megafaunal extinctions. There is no evidence of megafaunal extinctions at the height of the LGM, indicating that increasing cold and glaciation were not factors. Multiple events appear to also involve the rapid replacement of one species by one within the same genus, or one population by another within the same species, across a broad area.
The ancestors of modern humans first appeared in East Africa 195,000 years ago. Some migrated out of Africa 60,000 years ago, with one group reaching Central Asia 50,000 years ago. From there they reached Europe, with human remains dated to 43,000-45,000 years BP discovered in Italy, Britain, and in the European Russian Arctic dated to 40,000 years ago. Another group left Central Asia and reached the Yana River, Siberia, well above the Arctic circle, 27,000 years ago. Remains of mammoth that had been hunted by humans 45,000 YBP have been found at Yenisei Bay in the central Siberian Arctic. Modern humans then made their way across the Bering land bridge and into North America between 20,000 and 11,000 years ago, after the Wisconsin glaciation had retreated but before the Bering land bridge became inundated by the sea. However, there remains no consensus among scholars on the timing of human migration into the Americas. In the Fertile crescent the first agriculture was developing 11,500 years ago.
Ecological consequences of megafaunal extinctions
Community and ecosystem changes
Megafauna extinctions resulted in global changes to ecosystem structure and function. Extinction of megafauna broadly restructured ecological communities and species interactions. The extinction of megafauna affected mutualist species, resulting in co-extinctions. Evidence from fossil pollen indicates that megafaunal extinctions may have resulted in the development of novel plant communities, and altered fire regimes on a global scale. Some evidence, however, suggests that vegetation changes preceded megafaunal extinctions.
Pleistocene grazers limited wildfire by consuming biomass in grassland ecosystems; the decline of these grazers increased grassland fire frequency. Some hypothesize that forbs in modern grasslands are adapted to disturbance by large herbivores on former mammoth steppes, and are currently in decline due to the extinction of Pleistocene megafauna. In Europe, evidence from the pollen record suggests that megafauna promoted open vegetation with shifting mosaics of forest and grassland, however this hypothesis is debated. In the Yukon region of Canada, the decline of Mammuthus and Equus may have contributed to the development of woody flora. In Siberia and Beringia, the extinction of mammoths may have contributed to the expansion of Betula (birch) tree cover. In Australia, however, megafaunal extinction may not have caused significant changes in fire regimes or vegetation. Some argue that modern ecosystems can be understood by considering the effects of extinct megafauna.
Some extant plants have adaptations resulting from interactions with Pleistocene megafauna, including defenses against Pleistocene megaherbivores, and large fruits adapted to dispersal by megaherbivores. Such species are termed anachronistic plants. Members of the plant family Rosaceae (including Malus, apples) evolved large fruits as an adaptation to dispersal by megafaunal herbivores. Megafaunal extinction caused the decline of Cucurbita species which relied on megaherbivores for dispersal. Cucurbita fruits contain cucurbitacins, bitter compounds that are toxic to small herbivores but can be tolerated by megafauna; Cucurbita seeds have been found in fossil mastodon dung. Some argue that plant adaptations to megafauna resulted in traits that allowed for domestication. Human dispersal may have prevented the range contraction of Neotropical species with fruit formerly dispersed by megafauna.
Effects on climate
Megafaunal extinction may have caused global cooling of the Earth's climate due to reduced methane emissions from megaherbivores and increased woody vegetation associated with reduced trampling and browsing. Smith et al. suggest that megafaunal extinctions in the Americas contributed to the Younger Dryas cooling event.
Four theories have been advanced as likely causes of these extinctions: hunting by the spreading humans (or overkill hypothesis, initially developed by geoscientist Paul S. Martin), the change in climate at the end of the last glacial period, disease, and an extraterrestrial impact from an asteroid or comet. These factors are not necessarily exclusive: any or all may have combined to cause the extinctions. Of these, climate change and the overkill hypothesis have the most support, with evidence weighing towards the overkill hypothesis.
Although not mutually exclusive, which factor was more important remains contested. Where humans appeared on the scene, megafauna went extinct; but at the same time, the climate was also warming. Large body size is an adaptation to colder climes, so a warming climate would have provided a stressor for these large animals; however, many fauna simply evolved a smaller body size over time. There is overwhelming archaeological evidence that humans did indeed hunt some or many of the now extinct species, such as the mammoth in North America; while evidence of hunting is necessary for the overhunting hypothesis, it is not sufficient to prove that human hunting drove the extinctions. The primary cause of Pleistocene megafauna extinctions may vary among regions and species (see below).
Effects and causes by continent
Background and scope
While North America was most notably impacted by the Pleistocene Megafaunal extinction, Eurasia, Africa and the Insular regions were also affected and experienced some extinction towards the end of the Pleistocene period. Megafaunal losses are poorly understood on continental Africa during both the Late Pleistocene and the Holocene periods. During the late Pleistocene and early Holocene period an estimated breadth of 24 large mammal species, of greater than 45 kg, were lost from continental Africa. These losses are best understood to have occurred between 13,000 and 6,000 years ago. The species of megafauna which were lost in continental Africa are best understood to have been grazers who lived on grasslands. However, other sources report that over 27 species were lost in the last million years. Sources vary in the breadth of the issue, however it is clear that significant biodiversity loss occurred in Africa.
At sites in Africa such as Olduvai, Olorgesailie, Kariandusi, Hopefield, Islmilia, and the Vaal River gravels most genera found were found in stratigraphic association with hand tools wielded by early human ancestors. These artifacts were from Acheulean origins. Acheulean tools include handaxes made from stone. These hand tools were made with a distinctly pear shaped morphology. Homo erectus was thought to wield these hand tools for a variety of purposes. Hand axes could be used to butcher and skin game, cut, chop, scrape, cut other instruments, digging in soil, cutting wood, cutting plant material. These tools were first discovered in 1847. These handaxes have been discovered on multiple continents including Southern Africa, Northern Europe, Western Europe and the Indian sub-continent. These Acheulean tools were found to have been being produced and utilized for roughly a million years. The earliest Acheulean artifacts were discovered in Africa to have existed for over 1.6 million years ago whereas the earliest Archulean tools are thought to have existed in Europe as early as 800,000 years ago. These hand axes measure 12–20 cm long. There is notable difference in the size, quality and efficacy of these tools depending on the workmanship of the crafter.
Arguments have existed regarding whether these early humans could have contributed significantly to megafauna extinction in Africa, Eurasia, and North America utilizing stone tools such as the Archulean hand tools which have been discussed. It is important to note that these analyses are considered incomplete by many contemporary scholars. However, despite the lack of scientific consensus surrounding this theory, this is being applied to contemporary biodiversity losses.
"A growing body of literature proposes that our ancestors contributed to large mammal extinctions in Africa long before the appearance of Homo sapiens, with some arguing that premodern hominins (e.g., Homo erectus) triggered the demise of Africa's largest herbivores and the loss of carnivoran diversity. Though such arguments have been around for decades, they are now increasingly accepted by those concerned with biodiversity decline in the present-day, despite the near complete absence of critical discussion or debate. To facilitate that process, here we review ancient anthropogenic extinction hypotheses and critically examine the data underpinning them. Broadly speaking, we show that arguments made in favor of ancient anthropogenic extinctions are based on problematic data analysis and interpretation, and are substantially weakened when extinctions are considered in the context of long-term evolutionary, ecological, and environmental changes." At the present moment - according to this source, there is no definitive empirical evidence to suggest that hominins have had widespread impact on the biodiversity of Pleistocene Africa.
Other sources propose alternate hypotheses: "To our knowledge, the earliest proposal of ancient hominin impacts in Africa can be traced to J. Desmond Clark's (1959) overview of southern African prehistory. Referring to a handful of large herbivores whose last appearances in southern Africa are now known to range in age from ∼1 Ma to the onset of the Holocene (Brink et al., 2012; Faith, 2014; Klein et al., 2007), including Stylohipparion (= Eurygnathohippus cornelianus), Griquatherium (= Sivatherium maurusium), and Homoioceras (= Syncerus antiquus), Clark (1959:57) suggested that "[t]heir final extinction may well have been due to man's improved methods of hunting these overspecialized and probably clumsy beasts." Clark did not specify which hominin species was to blame, but from the evidence available to him at the time, it was clear that at least some of these extinct taxa (e.g., Stylohipparion and Griquatherium) disappeared long before the Pleistocene-Holocene transition (Clark, 1959:54) and were associated with hominins that preceded the emergence of H. sapiens, including H. heidelbergensis (Drennan, 1953)". This discussion of Megafaunal losses in Africa during the Pleistocene period would suggest that anthropogenic influence could have been a significant impetus for extinction.
Another hypothesis suggests a more environmentally focused cause for the megafaunal extinction in Pleistocene Africa, "The current lack of evidence (for hominin attributed extinction) does not preclude it from being produced in the future, though we are not optimistic that it will be. Looking to the last ∼100,000 years-a time interval encompassing massive demographic and technological change among human populations-it is clear that African megafaunal extinctions are readily explained by environmental changes (Faith, 2014). In particular, grassland herbivores disappeared following alterations in the structure, distribution, or productivity of their habitats (Faith, 2014), consistent with broader changes in herbivore community composition spanning the last 1 Myr (Faith et al., 2019)". Environmental factors implicated in this explanation include structure, distribution and biological productivity of the environment. This explanation minimizes human impact and emphasizes environmental factors.
African Pleistocene megafauna losses
African primate species from the Early Middle Pleistocene (1.0-2.0 million years ago) included Gorgopithecus, Dinopithecus, Cercopithecoidea, Australopithecus, Paranthropus, Telanthropus, Parapapio. Primates that existed during the Late Middle Pleistocene extinction period (100,000 years) included Semnopithecus. Living genera in Africa include Pan, Gorilla and Mandrillus. African Carnivora from the Early Middle Pleistocene included Lycaon, Megantereon, and Homotherium. Carnivores that existed during the Late Middle Pleistocene extinction period included Machairodus. Living genera in Africa include Acinonyx, Panthera, Hyaena, and Crocuta. Interestingly, no Tubulidentata existed during the Early Middle or Late Middle Pleistocene periods. However, Orycteropus is included in the living African genera. Similarly no Hippopotamidae existed during the Early Middle or Late Middle Pleistocene periods. However, Hippopotamus and Choeropsis are present in the living African genera. Bovidae from the Early Middle Pleistocene include Pultiphagonides and Numidocapra. Bovidae that existed during the Late Middle Pleistocene extinction period included Homoioceras, Bulcharus, Pelorovis, Lunaloceras, Megalotragus, Makapania and Phenacotragus. Living Bovidae genera include Tragelaphus, Taurotragus, Syncerus, Cephalophus, Kobus, Redunca, Hippotragus, Oryx, Addax, Damaliscus, Alcelaphus, Beatragus, Connochaetes, Aepyceros, Litocranius, Gazella, Eudorcas, Nanger, Capra, Ammotragus.
The summary of mammalian megafaunal extinction and survival can be discussed as well comparing Africa and North America. Living genera (50 kg+) in Africa include 40 and 14 in the US and Canada (North America). Later Pleistocene extinction genera include 26+ in Africa and 35 in the US and Canada. Earlier Pleistocene extinction genera include 19 in Africa and 13 in the US and Canada. Later Pleistocene Megafaunal Extinction Intensity was 39% for Africa, and 71% for the US and Canada. It is evident through this analysis that North America underwent a more intense later Pleistocene Megafaunal Extinction.
Contrasting Africa's losses with North America
The rate of extinction in the Pleistocene period between Africa and North America shows striking differences. In America, an estimated 35 genera of large mammals disappeared at the end of the Rancholabrean period. Most of these animals were lost within the last 12,000 years. However, in the preceding one to two million years before the end of the Rancholabrean period, an estimated 13 genera of megafauna were lost. This may be attributed to a poor understanding of fauna that existed before to this period. To compare this rate of megafaunal loss with Africa, the differences between the earlier, middle and later Pleistocene faunal losses are less drastic to compare. In the first 1.5 million years 19 megafaunal genera were lost. Within the last 100,000 years 26 or more genera were lost. This rate of megafaunal extinction in Africa in the last 100,000 years was an estimated 20 times greater in magnitude as the losses that occurred within the preceding 1.5 million years.
Sub-Saharan Africa is the region of the world with the highest amount of Pleistocene megafauna surviving to the present day. These surviving species include the bush elephant (Loxodonta africana), the forest elephant (Loxodonta cyclotis), the black rhinoceros (Diceros bicornis), the white rhinoceros (Ceratotherium simum) and the hippopotamus (Hippopotamus amphibius). All of these species maintained populations in sub-Saharan Africa even after many of them were extirpated from Eurasia during the early Holocene. This means that all of the largest herbivore genera present in Pleistocene Africa are still present today. Overall, estimates as to the proportion of Africa’s Quaternary megafauna which went extinct range from 5% to 18%, much lower than for all the other continents.
Multiple reasons have been suggested by scientists as to why Africa apparently had a much milder experience during the Quaternary extinction. First, some have suggested that the Late Quaternary extinction has been comparatively less studied in Africa than in other regions. As a result of this lack of studying, there is little evidence that paleontologists are able to draw upon when trying to develop a timeline of extinctions in Sub-Saharan Africa. This hypothesis therefore also argues that further investigation into sites with Late Quaternary fossils in Sub-Saharan Africa will reveal previously-undiscovered extinct taxa of African megafauna.
Other scientists have suggested an explanation for the relative lack of extinction among Africa’s Pleistocene megafauna which follows the overkill hypothesis as the cause of the Quaternary extinction. According to this hypothesis, many of the extinctions during this time period were due to overhunting by humans who had recently migrated to their continents. In sub-Saharan Africa, the megafauna species had evolved alongside the different species of hominids present in Quaternary Africa. As a result, these species had adapted to withstand the predation pressure from humans. This meant that both humans and megafauna were able to coexist, and the high levels of extinction seen in the Americas and Australasia were not seen in Africa.
While one of the popular explanations for the Quaternary extinction is due to the changing climate of the time period, the climate of Africa has not been suggested as a potential cause. This is because of the high level of megafaunal extinction in South America during this time period. Since Sub-Saharan Africa has about the same types of climate as South America, but South America had many more extinctions of megafauna taxa, climate was not deemed by these scientists to be a sufficient cause to explain the relative lack of extinctions in Africa.
Despite the high level of continuity present in Africa’s megafauna community from the Quaternary to the Holocene period, there were several species of megafauna which did go extinct during this time period. One such species was Pelorovis antiquus, the Long-horned African Buffalo. This species is theorized to either have gone extinct due to climate change, overhunting by humans, or both. It was extirpated from Sub-Saharan Africa about 12,000 years ago and became entirely extinct about 4,000 years before present. Another was the giant antelope that was very similar to a hartebeest or a wildebeest known as Megalotragus priscus. M. priscus was the last of its genus, and it died out approximately 7,500 years ago. Similarly, there was an extinct species of zebra known as the Cape Zebra, Equus capensis. The Cape zebra lived throughout Africa during the Quaternary period but went extinct by its end. One species of Quaternary megafauna would also go extinct later on after contact with European settlers, after having its range reduced during the Quaternary extinction event. This species was the blue antelope, Hippotragus leucophaeus. This species had its range restricted changing habitats during the early Holocene period, so that by the time European colonists arrived, they were restricted to one lone population. This population was then wiped out by habitat loss and hunting by European colonists. The blue antelope went extinct in 1800.
During the American megafaunal extinction event, around 12,700 years ago, North America lost 70% of its megafauna species. 90 genera of mammals weighing over 44 kilograms became extinct. The Late Pleistocene fauna in North America included giant sloths, short-faced bears, several species of tapirs, peccaries (including the long-nosed and flat-headed peccaries), the American lion, giant tortoises, Miracinonyx ("American cheetahs", not true cheetahs), the saber-toothed cat Smilodon and the scimitar-toothed cat Homotherium, dire wolves, saiga, camelids such as two species of now-extinct llamas and Camelops, at least two species of bison, the stag-moose, the shrub-ox and Harlan's muskox, 14 species of pronghorn (of which 13 are now extinct), horses, mammoths and mastodons, the beautiful armadillo and the giant armadillo-like Glyptotherium, and giant beavers, as well as birds like giant condors and teratorns.
The reasons for the extinction event are still debated, but it has largely been attributed to both climate change and human-driven extinction. Humans arrived in North America between 12 and 30 thousand years ago. There are various human impacts that could have put pressure on different megafauna species, including direct hunting and cascading trophic interactions. Some researchers attribute the extinction of megafauna to the presence of Clovis hunting, along with significant human population increases which would have increased hunting intensity and frequency, around 13,000 years ago. Contemporaneously, around 12,000 years ago, a global cooling event called the Younger Dryas (YD) occurred, which would have dramatically effected habitat area and food sources for many megafaunal species.
The role of humans, climate change, and other factors in driving megafauna extinction in North America is debated, with some scholars arguing in favor of climate change as the primary driver and others suggesting the possibility of direct and indirect human impacts. However, it can be difficult to generalize an extinction event for the continent as a whole when the climate and human impacts varied spatially, temporally, and seasonally so it is hard to generalize what triggered the event for the entire continent. Thus, it is important to consider that the causes can significantly vary for different species and different regions of North America. The extinction of megafauna and first appearance of humans did not completely correlate across North America, meaning that each area needs to be separately considered when attempting to determine the cause of extinction. Radiocarbon dating suggests that while extinctions followed human arrival in some areas (consistent with extinction due to hunting), in other regions megafauna species disappeared before humans arrived or persisted for as long as 3000 years in the presence of humans, suggesting factors other than humans drove extinctions. Similarly, a comparison of human vs megafauna population trends, again inferred from radiocarbon dating, found that extinctions were likely due to hunting for 3 species, from climate change for 5 species, and from a combination of hunting and climate change in one case.
Megafauna extinctions that are most consistent with human activity in North America are of the mammoth, horse, and saber-toothed cat. Humans directly impacted mammoth and horse species by overhunting, while Smilodon was pushed to extinction indirectly by humans overhunting of their prey. There are two species of megafauna whose extinctions appear to have no link to human hunting, they are the Shasta ground sloth and mastodon.
Alaska is situated in the northwestern most part of North America. Megafauna disappeared from these higher latitudes generally earlier than the rest of North America. This means that the megafauna in the region either went extinct locally or migrated south as a result of the YD cooling event. Megafauna species disappeared from Alaska approximately 1000 to 4000 years before there was significant human presence in Alaska, indicating that their demise likely resulted from climate change.
The Great Lakes Region
Megafauna species disappeared from Great Lakes Region considerably more recently than in higher latitudes, like Alaska. Additionally, the first appearances for human species were considerably older for this region compared to other regions in North America. Due to the overlaps of these two appearances, it has been suggested from the fossil record that humans and megafauna overlapped in the region for 7000 years. However, the presence of humans does not mean that the megafauna extinction event in the region was solely attributed to human impacts. There has been significant evidence into the cause of extinction in this area being related to the fact that both climate change and human impacts hit simultaneously.
The West/Pacific Coast
The Pacific Coast was one of the region where early Indigenous Peoples first migrated. This is due to the fact that humans may have migrated further south from Alaska through a pathway that went along the Pacific Coast. However, there appears to have been little overlap between humans and megafauna species in these region. One potential for this could be due to poor sampling due to sea-level rise that could have “obscured older coastal sites”.
Indigenous knowledge of Pleistocene megafauna
Indigenous knowledge of Pleistocene megafauna has survived via oral tradition and representations such as petroglyphs.
The Cayuse people of the Pacific Northwest has oral traditions and a dance centered around a story of mammoths migrating into their land. On the Umatilla Indian Reservation, where the Cayuse people lived historically and today, two mammoth teeth were discovered during construction of a golf course.
An Osage tradition tells about a battle between mastodons and mammoths in the Great Plains region. This battle left many animals dead and after the battle was over the Osage burned the dead animals. Later, after the Osage were forceable moved to a reservation, white settlers found mastodon and mammoth bones at this site.
Throughout western North America, there are many stories of large, black-winged birds, known as thunderbirds, which interacted with Indigenous people in both positive and negative ways. These stories of thunderbirds share similarities with species from the genus Teratornis, which are found throughout fossil record of the west coast.
About 10,000 years ago, the landscape of South America contained numerous species of megafauna, many of which have no modern species for comparison. South America was home to bears, sabertooth cats, large capybaras and llamas. Additionally, there were huge terrestrial sloths, armored glyptodonts (similar to an armadillo, but the size of a hippo), and animals similar to camels and rhinoceroses (macrauchenids and toxodonts). These animals went extinct during the Quaternary Period and all South American mammal species larger than 100 kg were lost. The explanation for their extinction has not been definitively answered, and is a topic of debate among scientists. Some suggest that human hunting may have been the dominant driver of megafaunal decline in South America.
The continent of South America was isolated for millions of years during the Cenozoic Period, which had a significant impact on its wildlife. This isolation helped foster species that were not found anywhere else on Earth. Approximately 3 million years ago, the Great American Biotic Interchange occurred due to the Isthmus of Panama, which allowed for the mixing of North and South American faunas. The mixing of faunas created new opportunities for expansion, competition, and replacement of species. South American wildlife in the Pleistocene varied greatly; an example is the giant ground sloth, Megatherium. The continent also had quite a few grazers and mixed feeders such as the camel-like litoptern Macrauchenia, Cuvieronius, Doedicurus, Glyptodon, Hippidion and Toxodon. There were also Stegomastodons, found as far south as Patagonia. The main predators of the region were Arctotherium and Smilodon. Before the interchange Phorusrhacids(terror birds) were also major predators.
As with South America, some elements of the Eurasian megafauna were similar to those of North America. Among the most recognizable Eurasian species are the woolly mammoth, steppe mammoth, straight-tusked elephant, European hippopotamuses, aurochs, steppe bison, cave lion, cave bear, cave hyena, Homotherium, Irish elk, giant polar bears, woolly rhinoceros, Merck's rhinoceros, narrow-nosed rhinoceros, and Elasmotherium. In contrast, today the largest European land mammal is the European bison or wisent.
By the advent and proliferation of modern humans (Homo sapiens) circa 315,000 BP, the most common species of the genus Homo in Eurasia were the Denisovans and Neanderthals (fellow H. heidelbergensis descendants), and Homo erectus in Eastern Asia. Homo sapiens is the only species of the genus Homo that remains extant.
Two major events towards the end of the Pleistocene era had ultimately impacted the species that were inhabiting Eurasia; the last glacial period and the introduction of Homo Sapiens from Old World Africa. These two events were responsible for the vastly selective and intense extinctions of the Eurasian large mammal species mentioned previously. The megafauna extinctions that occurred towards the end of the Pleistocene is believed to be largely due to human hunting and overkill. Overkill models that incorporate prey availability for Homo Sapiens have provided solid backing to that theory.
Hunters of the Upper Paleolithic had crafted tools and projectile weapons that were able to bring down prey as large as Mammoths. With the population of humans rapidly increasing, the consumption and hunting of meat grew just as rapidly. In addition to the growing numbers of human hunters, large terrestrial mammals in Eurasia had to combat detrimental climatic changes.
Northern Eurasia during the Middle and Upper Pleistocene (ca. 700000–10000 BP) was continuously facing a changing climate. The landscape and habitats of mammals saw phases ranging from extensive glaciation and cold stages to temperate climates and interglacials.
A majority of extinctions occurred during the Late glacial (ca. 15000–10000 BP) periods. This period was characterized by a major reformation of vegetation, mainly the replacement of open vegetation by forests. These changes were more profound than earlier in the Last Cold Stage and are believed to have played a critical role in the extinction of the Pleistocene megafauna. 
The most recent Ice Age occurred during the Pleistocene, and caused lower global sea levels. The lower sea level revealed the entire Sahul Shelf, connecting Australia with New Guinea and Tasmania. Most literature about Australian megafauna during the Pleistocene refers to the entirety of Sahul.
Australia was characterized by marsupials, monotremes, crocodilians, testudines, monitors and numerous large flightless birds. Pleistocene Australia also supported the giant short-faced kangaroo (Procoptodon goliah), Diprotodon (a giant wombat relative), the marsupial lion (Thylacoleo carnifex), the flightless bird Genyornis, the five-meter long snake Wonambi and the giant monitor lizard Megalania. Since 450 Ka, 88 Australian megafauna species have gone extinct.
There are several hypotheses that attempt to explain why Pleistocene Australian megafauna went extinct. Most studies point to either climate change or human activity as reasons for the die off, but there is not yet a consensus among scientists about which factor had a larger impact. A scarcity of reliably dated megafaunal bone deposits has made it difficult to construct timelines for megafaunal extinctions in certain areas, leading to a divide among researches about when and how megafaunal species went extinct.
Several studies provide evidence that climate change caused megafaunal extinction during the Pleistocene in Australia. One group of researchers analyzed fossilized teeth found at Cuddie Springs in southeastern Australia. By analyzing oxygen isotopes, they measured aridity, and by analyzing carbon isotopes and dental microwear texture analysis, they assessed megafaunal diets and vegetation. During the middle Pleistocene, southeastern Australia was dominated by browsers, including fauna that consumed C4 plants. By the late Pleistocene, the C4 plant dietary component had decreased considerably. This shift may have been caused by increasingly arid conditions, which may have caused dietary restrictions. Other isotopic analyses of eggshells and wombat teeth also point to a decline of C4 vegetation after 45 Ka. This decline in C4 vegetation is coincident with increasing aridity. Increasingly arid conditions in southeastern Australia during the late Pleistocene may have stressed megafauna, and contributed to their decline.
Human activity may have caused Australian megafaunal extinction during the Pleistocene, although this idea is hotly debated. To determine whether humans caused an extinction, three criteria must be met: (1) if megafauna species went extinct before a significant climate event but after human colonization, researchers can infer that the extinction was probably caused by humans; (2) if climate change during the studied epoch was not more significant than climate change during previous epochs, then any extinctions during that time were probably not caused by climate change; and (3) if all or most megafauna was still extant when humans arrived, then it is possible that human activity caused the extinction.
Some researchers believe that humans were probably not responsible for the megafaunal extinctions in Sahul. They contribute the extinctions to climate change, and argue that most megafaunal species do not appear in the fossil record within 95 Ka of human arrival. Additionally, they claim that long-term aridification of the continent resulted in staggered losses beginning by 130 Ka, and continued range contractions and extinctions throughout the rest of the Pleistocene. Researchers who do not believe that human actions were the primary cause of Pleistocene megafaunal extinctions in Australia do not exclude anthropogenic influence entirely. One article cites evidence of human interactions with megafauna at Cuddie Springs, but further explains that humans can only be held accountable for declines in the populations of the 13% of species that can be placed at that location. They argue that it will remain futile to determine the primary cause of megafaunal extinctions. Other researchers argue that, for most species, archaeological evidence of human hunting activity is rare and questionable. The major exception to this is the giant bird, Genyornis. Between 54 and 47 Ka, distinct charring patterns on Genyornis eggshells indicate that humans heated the eggs over campfires. This time period also corresponds to the decline and extinction of Genyornis. Similar charring patterns were found on emu eggs from widespread locations, also dating to this time period. These widespread charred eggshells indicate the arrival and fast spread of humans in Sahul. Despite the evidence of interactions between humans and Genyornis, there is not much evidence to indicate that there were significant interactions between humans and other megafaunal species. Many scientists interpret this lack of evidence of interaction as evidence that humans did not cause most megafaunal extinctions in Australia.
Other researchers disagree, and argue that there is sufficient evidence to determine that human activity was the primary cause for many of the megafaunal extinctions. They argue that the lack of evidence of hunting does not indicate that hunting during the Pleistocene was negligible. Rather, archaeological evidence of hunting of animals that went extinct soon after human arrival should be negligible, even if that hunting had an ecological impact. Because humans arrived on the continent so early, the period of interaction between humans and megafauna is very small relative to the entire archaeological record of Sahul. Furthermore, hunting rates would have been highest soon after the arrival of humans, when megafaunal populations were very large. Human populations would have been small during this time, and as a result, would not be as visible in the archaeological record. Researchers who believe that human activity was the primary cause of megafaunal extinction in Australia argue that the lack of evidence should not rule out human-megafauna interactions.
Many islands had a unique megafauna that became extinct upon the arrival of humans more recently (over the last few millennia and continuing into recent centuries). These included dwarf woolly mammoths on Wrangel Island, St. Paul Island and the Channel Islands of California; giant birds in New Zealand such as the moas and Hieraaetus moorei (a giant eagle); numerous species in Madagascar: giant ground-dwelling lemurs, including Megaladapis, Palaeopropithecus and the gorilla-sized Archaeoindris, three species of hippopotamuses, two species of giant tortoises, the Voay-crocodile and the giant bird Aepyornis; five species of giant tortoises from the Mascarenes; a dwarf Stegodon on Flores and a number of other islands; land turtles and crocodiles in New Caledonia; giant flightless owls and dwarf ground sloths in the Caribbean; giant flightless geese and moa-nalo (giant flightless ducks) in Hawaii; and dwarf elephants and dwarf hippos from the Mediterranean islands. The Canary Islands were also inhabited by an endemic megafauna which are now extinct: giant lizards (Gallotia goliath), giant rats (Canariomys bravoi and Canariomys tamarani) and giant tortoises (Geochelone burchardi and Geochelone vulcanica), among others. On the California Channel Islands, it is unclear whether humans caused the extinction of pygmy mammoths (Mammuthus exilis), the only species of megafauna which inhabited the area. Mammoth populations were in decline on the Channel Islands at the time of human arrival.
- Holocene extinction
- Quaternary extinction event
- Pleistocene rewilding
- Younger Dryas impact hypothesis
- Pavelková Řičánková, Věra; Robovský, Jan; Riegert, Jan (2014). "Ecological Structure of Recent and Last Glacial Mammalian Faunas in Northern Eurasia: The Case of Altai-Sayan Refugium". PLOS ONE. 9 (1): e85056. Bibcode:2014PLoSO...985056P. doi:10.1371/journal.pone.0085056. PMC 3890305. PMID 24454791.
- Intergovernmental Panel on Climate Change (UN). "IPCC Fourth Assessment Report: Climate Change 2007 - Palaeoclimatic Perspective". The Nobel Foundation. Archived from the original on 2015-10-30. Retrieved 2015-08-09.
- Clark, P. U.; Dyke, A. S.; Shakun, J. D.; Carlson, A. E.; Clark, J.; Wohlfarth, B.; Mitrovica, J. X.; Hostetler, S. W.; McCabe, A. M. (2009). "The Last Glacial Maximum". Science. 325 (5941): 710–4. Bibcode:2009Sci...325..710C. doi:10.1126/science.1172873. PMID 19661421. S2CID 1324559.
- Elias, Scott A.; Short, Susan K.; Nelson, C. Hans; Birks, Hilary H. (1996). "Life and times of the Bering land bridge". Nature. 382 (6586): 60. Bibcode:1996Natur.382...60E. doi:10.1038/382060a0. S2CID 4347413.
- Jonathan Adams. "Europe during the last 150,000 years". Oak Ridge National Laboratory, Oak Ridge, USA. Archived from the original on 2005-11-26.
- Meltzer, David J. (2015-10-21). "Pleistocene Overkill and North American Mammalian Extinctions". Annual Review of Anthropology. 44 (1): 33–53. doi:10.1146/annurev-anthro-102214-013854. ISSN 0084-6570.
- Stuart, Anthony John (1999). "Late Pleistocene Megafaunal Extinctions". Extinctions in Near Time. pp. 257–269. doi:10.1007/978-1-4757-5202-1_11. ISBN 978-1-4419-3315-7.
- Dale Guthrie, R. (2004). "Radiocarbon evidence of mid-Holocene mammoths stranded on an Alaskan Bering Sea island". Nature. 429 (6993): 746–749. Bibcode:2004Natur.429..746D. doi:10.1038/nature02612. PMID 15201907. S2CID 4394371.
- Reumer, Jelle W. F.; Rook, Lorenzo; Van Der Borg, Klaas; Post, Klaas; Mol, Dick; De Vos, John (2003). "Late Pleistocene survival of the saber-toothed cat Homotheriumin northwestern Europe". Journal of Vertebrate Paleontology. 23: 260–262. doi:10.1671/0272-4634(2003)23[260:LPSOTS]2.0.CO;2. S2CID 140187064.
- Barnett, R.; Shapiro, B.; Barnes, I. A. N.; Ho, S. Y. W.; Burger, J.; Yamaguchi, N.; Higham, T. F. G.; Wheeler, H. T.; Rosendahl, W.; Sher, A. V.; Sotnikova, M.; Kuznetsova, T.; Baryshnikov, G. F.; Martin, L. D.; Harington, C. R.; Burns, J. A.; Cooper, A. (2009). "Phylogeography of lions (Panthera leo ssp.) reveals three distinct taxa and a late Pleistocene reduction in genetic diversity". Molecular Ecology. 18 (8): 1668–1677. doi:10.1111/j.1365-294X.2009.04134.x. PMID 19302360. S2CID 46716748.
- Ghezzo, Elena; Rook, Lorenzo (2015). "The remarkable Panthera pardus (Felidae, Mammalia) record from Equi (Massa, Italy): Taphonomy, morphology, and paleoecology". Quaternary Science Reviews. 110: 131–151. doi:10.1016/j.quascirev.2014.12.020.
- Cooper, A.; Turney, C.; Hughen, K. A.; Brook, B. W.; McDonald, H. G.; Bradshaw, C. J. A. (2015). "Abrupt warming events drove Late Pleistocene Holarctic megafaunal turnover". Science. 349 (6248): 602–6. Bibcode:2015Sci...349..602C. doi:10.1126/science.aac4315. PMID 26250679. S2CID 31686497.
- White, T. D.; Asfaw, B.; Degusta, D.; Gilbert, H.; Richards, G. D.; Suwa, G.; Clark Howell, F. (2003). "Pleistocene Homo sapiens from Middle Awash, Ethiopia". Nature. 423 (6941): 742–7. Bibcode:2003Natur.423..742W. doi:10.1038/nature01669. PMID 12802332. S2CID 4432091.
- "A Human Journey:Migration Routes". The genographic project. National Geographic Society. 2015. Archived from the original on 19 May 2017. Retrieved 12 August 2015.
- Benazzi, S.; Douka, K.; Fornai, C.; Bauer, C. C.; Kullmer, O.; Svoboda, J. Í.; Pap, I.; Mallegni, F.; Bayle, P.; Coquerelle, M.; Condemi, S.; Ronchitelli, A.; Harvati, K.; Weber, G. W. (2011). "Early dispersal of modern humans in Europe and implications for Neanderthal behaviour". Nature. 479 (7374): 525–8. Bibcode:2011Natur.479..525B. doi:10.1038/nature10617. PMID 22048311. S2CID 205226924.
- Higham, T.; Compton, T.; Stringer, C.; Jacobi, R.; Shapiro, B.; Trinkaus, E.; Chandler, B.; Gröning, F.; Collins, C.; Hillson, S.; o’Higgins, P.; Fitzgerald, C.; Fagan, M. (2011). "The earliest evidence for anatomically modern humans in northwestern Europe". Nature. 479 (7374): 521–4. Bibcode:2011Natur.479..521H. doi:10.1038/nature10484. PMID 22048314. S2CID 4374023.
- Pavlov, Pavel; Svendsen, John Inge; Indrelid, Svein (2001). "Human presence in the European Arctic nearly 40,000 years ago". Nature. 413 (6851): 64–7. Bibcode:2001Natur.413...64P. doi:10.1038/35092552. PMID 11544525. S2CID 1986562.
- "Mamontovaya Kurya:an enigmatic, nearly 40000 years old Paleolithic site in the Russian Arctic" (PDF). Archived (PDF) from the original on 2015-08-14. Retrieved 2015-08-09.
- Pitulko, V. V.; Nikolsky, P. A.; Girya, E. Y.; Basilyan, A. E.; Tumskoy, V. E.; Koulakov, S. A.; Astakhov, S. N.; Pavlova, E. Y.; Anisimov, M. A. (2004). "The Yana RHS Site: Humans in the Arctic Before the Last Glacial Maximum". Science. 303 (5654): 52–6. Bibcode:2004Sci...303...52P. doi:10.1126/science.1085219. PMID 14704419. S2CID 206507352.
- Pitulko, V. V.; Tikhonov, A. N.; Pavlova, E. Y.; Nikolskiy, P. A.; Kuper, K. E.; Polozov, R. N. (2016). "Early human presence in the Arctic: Evidence from 45,000-year-old mammoth remains". Science. 351 (6270): 260–3. Bibcode:2016Sci...351..260P. doi:10.1126/science.aad0554. PMID 26816376. S2CID 206641718.
- Tamm, E.; Kivisild, T.; Reidla, M.; Metspalu, M.; Smith, D. G.; Mulligan, C. J.; Bravi, C. M.; Rickards, O.; Martinez-Labarga, C.; Khusnutdinova, E. K.; Fedorova, S. A.; Golubenko, M. V.; Stepanov, V. A.; Gubina, M. A.; Zhadanov, S. I.; Ossipova, L. P.; Damba, L.; Voevoda, M. I.; Dipierri, J. E.; Villems, R.; Malhi, R. S. (2007). Carter, Dee (ed.). "Beringian Standstill and Spread of Native American Founders". PLOS ONE. 2 (9): e829. Bibcode:2007PLoSO...2..829T. doi:10.1371/journal.pone.0000829. PMC 1952074. PMID 17786201.
- Potter, Ben A.; Baichtal, James F.; Beaudoin, Alwynne B.; Fehren-Schmitz, Lars; Haynes, C. Vance; Holliday, Vance T.; Holmes, Charles E.; Ives, John W.; Kelly, Robert L.; Llamas, Bastien; Malhi, Ripan S. (2018-08-03). "Current evidence allows multiple models for the peopling of the Americas". Science Advances. 4 (8): eaat5473. Bibcode:2018SciA....4.5473P. doi:10.1126/sciadv.aat5473. ISSN 2375-2548. PMC 6082647. PMID 30101195.
- Balter, M (4 July 2013). "Farming Was So Nice, It Was Invented at Least Twice". Science. Archived from the original on 31 May 2022. Retrieved 30 June 2022.
- Malhi, Yadvinder; Doughty, Christopher E.; Galetti, Mauro; Smith, Felisa A.; Svenning, Jens-Christian; Terborgh, John W. (2016-01-26). "Megafauna and ecosystem function from the Pleistocene to the Anthropocene". Proceedings of the National Academy of Sciences. 113 (4): 838–846. Bibcode:2016PNAS..113..838M. doi:10.1073/pnas.1502540113. ISSN 0027-8424. PMC 4743772. PMID 26811442.
- Gill, Jacquelyn L.; Williams, John W.; Jackson, Stephen T.; Lininger, Katherine B.; Robinson, Guy S. (2009-11-20). "Pleistocene Megafaunal Collapse, Novel Plant Communities, and Enhanced Fire Regimes in North America". Science. 326 (5956): 1100–1103. Bibcode:2009Sci...326.1100G. doi:10.1126/science.1179504. ISSN 0036-8075. PMID 19965426. S2CID 206522597. Archived from the original on 2022-05-20. Retrieved 2022-05-19.
- Tóth, Anikó B.; Lyons, S. Kathleen; Barr, W. Andrew; Behrensmeyer, Anna K.; Blois, Jessica L.; Bobe, René; Davis, Matt; Du, Andrew; Eronen, Jussi T.; Faith, J. Tyler; Fraser, Danielle (2019-09-20). "Reorganization of surviving mammal communities after the end-Pleistocene megafaunal extinction". Science. 365 (6459): 1305–1308. Bibcode:2019Sci...365.1305T. doi:10.1126/science.aaw1605. ISSN 0036-8075. PMID 31604240. S2CID 202699089. Archived from the original on 2022-05-05. Retrieved 2022-05-19.
- Galetti, Mauro; Moleón, Marcos; Jordano, Pedro; Pires, Mathias M.; Guimarães, Paulo R.; Pape, Thomas; Nichols, Elizabeth; Hansen, Dennis; Olesen, Jens M.; Munk, Michael; de Mattos, Jacqueline S. (May 2018). "Ecological and evolutionary legacy of megafauna extinctions: Anachronisms and megafauna interactions". Biological Reviews. 93 (2): 845–862. doi:10.1111/brv.12374. PMID 28990321. S2CID 4762203. Archived from the original on 2022-05-19. Retrieved 2022-05-19.
- Gill, Jacquelyn L. (March 2014). "Ecological impacts of the l ate Q uaternary megaherbivore extinctions". New Phytologist. 201 (4): 1163–1169. doi:10.1111/nph.12576. ISSN 0028-646X. PMID 24649488.
- Karp, Allison T.; Faith, J. Tyler; Marlon, Jennifer R.; Staver, A. Carla (2021-11-26). "Global response of fire activity to late Quaternary grazer extinctions". Science. 374 (6571): 1145–1148. Bibcode:2021Sci...374.1145K. doi:10.1126/science.abj1580. ISSN 0036-8075. PMID 34822271. S2CID 244660259. Archived from the original on 2022-05-20. Retrieved 2022-05-19.
- Monteath, Alistair J.; Gaglioti, Benjamin V.; Edwards, Mary E.; Froese, Duane (2021-12-28). "Late Pleistocene shrub expansion preceded megafauna turnover and extinctions in eastern Beringia". Proceedings of the National Academy of Sciences. 118 (52): e2107977118. doi:10.1073/pnas.2107977118. ISSN 0027-8424. PMC 8719869. PMID 34930836.
- Bråthen, Kari Anne; Pugnaire, Francisco I; Bardgett, Richard D (December 2021). "The paradox of forbs in grasslands and the legacy of the mammoth steppe". Frontiers in Ecology and the Environment. 19 (10): 584–592. doi:10.1002/fee.2405. ISSN 1540-9295. S2CID 230614023.
- Johnson, C.n. (2009-07-22). "Ecological consequences of Late Quaternary extinctions of megafauna". Proceedings of the Royal Society B: Biological Sciences. 276 (1667): 2509–2519. doi:10.1098/rspb.2008.1921. PMC 2684593. PMID 19324773.
- Murchie, Tyler J.; Monteath, Alistair J.; Mahony, Matthew E.; Long, George S.; Cocker, Scott; Sadoway, Tara; Karpinski, Emil; Zazula, Grant; MacPhee, Ross D. E.; Froese, Duane; Poinar, Hendrik N. (2021-12-08). "Collapse of the mammoth-steppe in central Yukon as revealed by ancient environmental DNA". Nature Communications. 12 (1): 7120. Bibcode:2021NatCo..12.7120M. doi:10.1038/s41467-021-27439-6. ISSN 2041-1723. PMC 8654998. PMID 34880234.
- Doughty, Christopher E.; Wolf, Adam; Field, Christopher B. (August 2010). "Biophysical feedbacks between the Pleistocene megafauna extinction and climate: The first human-induced global warming?: BIOPHYSICAL FEEDBACKS OF EXTINCTIONS". Geophysical Research Letters. 37 (15): n/a. Bibcode:2010GeoRL..3715703D. doi:10.1029/2010GL043985. S2CID 54849882.
- Johnson, Chris N.; Rule, Susan; Haberle, Simon G.; Kershaw, A. Peter; McKenzie, G. Merna; Brook, Barry W. (February 2016). "Geographic variation in the ecological effects of extinction of Australia's Pleistocene megafauna". Ecography. 39 (2): 109–116. doi:10.1111/ecog.01612. ISSN 0906-7590. Archived from the original on 2022-06-08. Retrieved 2022-06-08.
- Janzen, Daniel H.; Martin, Paul S. (January 1982). "Neotropical Anachronisms: The Fruits the Gomphotheres Ate". Science. 215 (4528): 19–27. doi:10.1126/science.215.4528.19. ISSN 0036-8075. PMID 17790450. S2CID 19296719. Archived from the original on 2022-06-08. Retrieved 2022-06-08.
- Spengler, Robert Nicholas (2019). "Origins of the Apple: The Role of Megafaunal Mutualism in the Domestication of Malus and Rosaceous Trees". Frontiers in Plant Science. 10: 617. doi:10.3389/fpls.2019.00617. ISSN 1664-462X. PMC 6545323. PMID 31191563.
- Kistler, Logan; Newsom, Lee A.; Ryan, Timothy M.; Clarke, Andrew C.; Smith, Bruce D.; Perry, George H. (2015-12-08). "Gourds and squashes ( Cucurbita spp.) adapted to megafaunal extinction and ecological anachronism through domestication". Proceedings of the National Academy of Sciences. 112 (49): 15107–15112. Bibcode:2015PNAS..11215107K. doi:10.1073/pnas.1516109112. ISSN 0027-8424. PMC 4679018. PMID 26630007.
- Spengler, Robert N.; Petraglia, Michael; Roberts, Patrick; Ashastina, Kseniia; Kistler, Logan; Mueller, Natalie G.; Boivin, Nicole (2021). "Exaptation Traits for Megafaunal Mutualisms as a Factor in Plant Domestication". Frontiers in Plant Science. 12: 649394. doi:10.3389/fpls.2021.649394. ISSN 1664-462X. PMC 8024633. PMID 33841476.
- van Zonneveld, Maarten; Larranaga, Nerea; Blonder, Benjamin; Coradin, Lidio; Hormaza, José I.; Hunter, Danny (2018-03-27). "Human diets drive range expansion of megafauna-dispersed fruit species". Proceedings of the National Academy of Sciences. 115 (13): 3326–3331. doi:10.1073/pnas.1718045115. ISSN 0027-8424. PMC 5879677. PMID 29531027.
- Smith, Felisa A.; Elliott, Scott M.; Lyons, S. Kathleen (June 2010). "Methane emissions from extinct megafauna". Nature Geoscience. 3 (6): 374–375. Bibcode:2010NatGe...3..374S. doi:10.1038/ngeo877. ISSN 1752-0908. Archived from the original on 2022-03-03. Retrieved 2022-05-19.
- Marc A. Carrasco, Anthony D. Barnosky, Russell W. Graham Quantifying the Extent of North American Mammal Extinction Relative to the Pre-Anthropogenic Baseline Archived 2014-12-14 at the Wayback Machine plosone.org December 16, 2009
- Firestone, R. B.; West, A.; Kennett, J. P.; Becker, L.; Bunch, T. E.; Revay, Z. S.; Schultz, P. H.; Belgya, T.; Kennett, D. J.; Erlandson, J. M.; Dickenson, O. J. (2007-10-09). "Evidence for an extraterrestrial impact 12,900 years ago that contributed to the megafaunal extinctions and the Younger Dryas cooling". Proceedings of the National Academy of Sciences. 104 (41): 16016–16021. Bibcode:2007PNAS..10416016F. doi:10.1073/pnas.0706977104. ISSN 0027-8424. PMC 1994902. PMID 17901202.
- Boissoneault, Lorraine. ""Are Humans to Blame for the Disappearance of Earth's Fantastic Beasts?"". Smithsonian. Archived from the original on 2019-12-10. Retrieved 2019-11-24.
- MacDonald, James (2018-05-14). "What Really Happened to the Megafauna". JSTOR Daily. Archived from the original on 2020-08-05. Retrieved 2019-11-24.
- Vignieri, S. (25 July 2014). "Vanishing fauna (Special issue)". Science. 345 (6195): 392–412. Bibcode:2014Sci...345..392V. doi:10.1126/science.345.6195.392. PMID 25061199.
Although some debate persists, most of the evidence suggests that humans were responsible for extinction of this Pleistocene fauna, and we continue to drive animal extinctions today through the destruction of wild lands, consumption of animals as a resource or a luxury, and persecution of species we see as threats or competitors.
- Cooper, Alan; Turney, Chris; Hughen, Konrad A.; Brook, Barry W.; McDonald, H. Gregory; Bradshaw, Corey J. A. (2015-08-07). "Abrupt warming events drove Late Pleistocene Holarctic megafaunal turnover". Science. 349 (6248): 602–606. Bibcode:2015Sci...349..602C. doi:10.1126/science.aac4315. ISSN 0036-8075. PMID 26250679. S2CID 31686497.
- Sandom, Christopher; Faurby, Søren; Sandel, Brody; Svenning, Jens-Christian (4 June 2014). "Global late Quaternary megafauna extinctions linked to humans, not climate change". Proceedings of the Royal Society B. 281 (1787): 20133254. doi:10.1098/rspb.2013.3254. PMC 4071532. PMID 24898370.
- Faurby, Søren; Svenning, Jens-Christian (2015). "Historic and prehistoric human‐driven extinctions have reshaped global mammal diversity patterns". Diversity and Distributions. 21 (10): 1155–1166. doi:10.1111/ddi.12369. hdl:10261/123512. S2CID 196689979. Archived from the original on 2020-06-10. Retrieved 2020-08-20.
- Smith, Felisa A.; et al. (April 20, 2018). "Body size downgrading of mammals over the late Quaternary". Science. 360 (6386): 310–313. Bibcode:2018Sci...360..310S. doi:10.1126/science.aao5987. PMID 29674591.
- Koch, Paul L.; Barnosky, Anthony D. (2006). "Late Quaternary Extinctions: State of the Debate". Annual Review of Ecology, Evolution, and Systematics. 37: 215–250. doi:10.1146/annurev.ecolsys.34.011802.132415. ISSN 1543-592X. JSTOR 30033832. S2CID 16590668.
- "Oldowan and Acheulean Stone Tools | Museum of Anthropology". anthromuseum.missouri.edu. Archived from the original on 2021-05-07. Retrieved 2021-05-07.
- Hoag, Colin; Svenning, Jens-Christian (2017-10-17). "African Environmental Change from the Pleistocene to the Anthropocene". Annual Review of Environment and Resources. 42 (1): 27–54. doi:10.1146/annurev-environ-102016-060653. ISSN 1543-5938.
- Faith, J. Tyler; Rowan, John; Du, Andrew; Barr, W. Andrew (July 2020). "The uncertain case for human-driven extinctions prior to Homo sapiens". Quaternary Research. 96: 88–104. Bibcode:2020QuRes..96...88F. doi:10.1017/qua.2020.51. ISSN 0033-5894. S2CID 225566468. Archived from the original on 2021-05-07. Retrieved 2021-05-07.
- Faith, J. Tyler (2014). "Late Pleistocene and Holocene mammal extinctions on continental Africa". Earth-Science Reviews. 128: 105–121. Bibcode:2014ESRv..128..105F. doi:10.1016/j.earscirev.2013.10.009.
- "Palaeontology and geological context of a Middle Pleistocene faunal assemblage from the Gladysvale Cave, South Africa". Palaeontologia Africana. 38: 99–114. Retrieved 2021-05-07.
- Rowland, Teisha (19 December 2009). "Ancient American Giants Extinct Megafauna of North and South America". Santa Barbara Independent. Archived from the original on 4 February 2021. Retrieved December 19, 2009.
- Martin, Paul S (22 October 1966). "Africa and Pleistocene overkill" (PDF). Nature. 212 (5060): 339–342. Bibcode:1966Natur.212..339M. doi:10.1038/212339a0. S2CID 27013299. Archived (PDF) from the original on 29 November 2020. Retrieved 15 May 2021.
- Stuart, Anthony John (May 2015). "Late Quaternary megafaunal extinctions on the continents: a short review: LATE QUATERNARY MEGAFAUNAL EXTINCTIONS". Geological Journal. 50 (3): 338–363. doi:10.1002/gj.2633. S2CID 128868400.
- Stuart, Anthony J. (1991). "Mammalian Extinctions in the Late Pleistocene of Northern Eurasia and North America". Biological Reviews. 66 (4): 453–562. doi:10.1111/j.1469-185X.1991.tb01149.x. ISSN 1469-185X. PMID 1801948. S2CID 41295526. Archived from the original on 2021-05-10. Retrieved 2021-05-07.
- G., Martin, Paul S. (Paul Schultz), 1928- Klein, Richard (1995). Quaternary extinctions : a prehistoric revolution. University of Arizona Press. ISBN 0-8165-1100-4. OCLC 851043302. Archived from the original on 2022-07-13. Retrieved 2021-05-07.
- Barnosky, A. D. (2004-10-01). "Assessing the Causes of Late Pleistocene Extinctions on the Continents". Science. 306 (5693): 70–75. Bibcode:2004Sci...306...70B. doi:10.1126/science.1101476. ISSN 0036-8075. PMID 15459379. S2CID 36156087. Archived from the original on 2022-06-07. Retrieved 2022-06-30.
- Turvey, Samuel T. (2009-05-28), "Holocene mammal extinctions", Holocene Extinctions, Oxford University Press, pp. 41–62, doi:10.1093/acprof:oso/9780199535095.003.0003, ISBN 978-0-19-953509-5, archived from the original on 2022-07-13, retrieved 2021-05-07
- Churcher, C. S. (January 2006). "Distribution and history of the Cape zebra ( Equus capensis ) in the Quarternary of Africa". Transactions of the Royal Society of South Africa. 61 (2): 89–95. doi:10.1080/00359190609519957. ISSN 0035-919X. S2CID 84203907. Archived from the original on 2022-07-13. Retrieved 2021-05-07.
- Kerley, Graham I. H.; Sims-Castley, Rebecca; Boshoff, André F.; Cowling, Richard M. (2009-04-28). "Extinction of the blue antelope Hippotragus leucophaeus: modeling predicts non-viable global population size as the primary driver". Biodiversity and Conservation. 18 (12): 3235–3242. doi:10.1007/s10531-009-9639-x. ISSN 0960-3115. S2CID 40104332. Archived from the original on 2022-07-13. Retrieved 2021-05-07.
- O'Keefe FR, Fet EV, Harris JM. 2009. Compilation, calibration, and synthesis of faunal and floral radiocarbon dates, Rancho La Brea, California. Contrib Sci 518: 1–16
- O'Keefe, F. Robin, Binder, Wendy J., Frost, Stephen R., Sadlier, Rudyard W., and Van Valkenburgh, Blaire 2014. Cranial morphometrics of the dire wolf, Canis dirus, at Rancho La Brea: temporal variability and its links to nutrient stress and climate. Palaeontologia Electronica Vol. 17, Issue 1;17A; 24p;  Archived 2018-12-16 at the Wayback Machine
- L. D. Martin. 1998. Felidae. In C. M. Janis, K. M. Scott, and L. L. Jacobs (eds.), Evolution of Tertiary Mammals of North America 1:236-242
- R. M. Nowak. 1991. Walker's Mammals of the World. Maryland, Johns Hopkins University Press (edited volume) II
- "North American Glyptodon". Archived from the original on June 24, 2006. Retrieved July 2, 2014.
- Broughton, Jack M.; Weitzel, Elic M. (2018). "Population reconstructions for humans and megafauna suggest mixed causes for North American Pleistocene extinctions". Nature Communications. 9 (1): 5441. Bibcode:2018NatCo...9.5441B. doi:10.1038/s41467-018-07897-1. PMC 6303330. PMID 30575758.
- Rasmussen, S. O.; Andersen, K. K.; Svensson, A. M.; Steffensen, J. P.; Vinther, B. M.; Clausen, H. B.; Siggaard-Andersen, M.-L.; Johnsen, S. J.; Larsen, L. B.; Dahl-Jensen, D.; Bigler, M. (2006). "A new Greenland ice core chronology for the last glacial termination". Journal of Geophysical Research. 111 (D6): D06102. Bibcode:2006JGRD..111.6102R. doi:10.1029/2005JD006079. ISSN 0148-0227.
- Emery-Wetherell, Meaghan M.; McHorse, Brianna K.; Byrd Davis, Edward (2017). "Spatially explicit analysis sheds new light on the Pleistocene megafaunal extinction in North America". Paleobiology. 43 (4): 642–655. doi:10.1017/pab.2017.15.
- Stewart, Mathew; Carleton, W. Christopher; Groucutt, Huw S. (2021-02-16). "Climate change, not human population growth, correlates with Late Quaternary megafauna declines in North America". Nature Communications. 12 (1): 965. doi:10.1038/s41467-021-21201-8. ISSN 2041-1723. PMC 7886903. PMID 33594059.
- Emery-Wetherell, Meaghan M.; McHorse, Brianna K.; Davis, Edward Byrd (2017). "Spatially explicit analysis sheds new light on the Pleistocene megafaunal extinction in North America". Paleobiology. 43 (4): 642–655. doi:10.1017/pab.2017.15. ISSN 0094-8373. S2CID 90330072. Archived from the original on 2022-01-20. Retrieved 2022-05-26.
- Broughton, Jack M.; Weitzel, Elic M. (2018-12-21). "Population reconstructions for humans and megafauna suggest mixed causes for North American Pleistocene extinctions". Nature Communications. 9 (1): 5441. doi:10.1038/s41467-018-07897-1. ISSN 2041-1723. PMC 6303330. PMID 30575758.
- Barnosky, A. D.; Koch, P. L.; Feranec, R. S.; Wing, S. L.; Shabel, A. B. (2004). "Assessing the Causes of Late Pleistocene Extinctions on the Continents". Science. 306 (5693): 70–75. Bibcode:2004Sci...306...70B. doi:10.1126/science.1101476. PMID 15459379. S2CID 36156087.
- Steeves, Paulette F. C. (2021). "Chapter 1: Decolonizing Indigenous Histories". The Indigenous Paleolithic of the Western Hemisphere. Lincoln, Nebraska: University of Nebraska Press. p. 163. ISBN 978-1-4962-0217-8. OCLC 1263182142. Archived from the original on 2022-07-13. Retrieved 2022-03-01.
- Cultural Resources Protection Program (March 2000). "A Review of Oral History Information of the Confederated Tribes of the Umatilla Indian Reservation". Department of Natural Resources, Confederated Tribes of the Umatilla Indian Reservation.
- Montagu, M. F. Ashley (1944). "An Indian Tradition Relating to the Mastodon". American Anthropologist. 46 (4): 568–571. doi:10.1525/aa.1944.46.4.02a00250. ISSN 0002-7294.
- Cruikshank, Julia (1980). Legend and landscape : convergence of oral and scientific traditions with special reference to the Yukon Territory, Canada. Scott Polar Research Institute. OCLC 70618191. Archived from the original on 2022-07-13. Retrieved 2022-03-01.
- Hall, Mark A. (2004). Thunderbirds America's living legends of giant birds. New York: Paraview Press. ISBN 1-931044-97-X. OCLC 493870454. Archived from the original on 2022-07-13. Retrieved 2022-03-01.
- Steeves, Paulette F. C. (2021). "Chapter 7: Genetics, Linguistics, Oral Traditions, and Other Supporting Lines of Evidence". The Indigenous Paleolithic of the Western Hemisphere. Lincoln, Nebraska: University of Nebraska Press. p. 10. ISBN 978-1-4962-0217-8. OCLC 1263182142. Archived from the original on 2022-07-13. Retrieved 2022-03-01.
- Samonds, Karen E. (2014-12-01). "Megafauna: Giant Beasts of Pleistocene South America". Journal of Mammalogy. 95 (6): 1308–1309. doi:10.1644/14-MAMM-R-132. ISSN 0022-2372.
- Prates, Luciano; Perez, S. Ivan (2021-04-12). "Late Pleistocene South American megafaunal extinctions associated with rise of Fishtail points and human population". Nature Communications. 12 (1): 2175. doi:10.1038/s41467-021-22506-4. ISSN 2041-1723. PMC 8041891. PMID 33846353.
- Webb, S. David (August 2006). "The Great American Biotic Interchange: Patterns and Processes1". Annals of the Missouri Botanical Garden. 93 (2): 245–257. doi:10.3417/0026-6493(2006)93[245:TGABIP]2.0.CO;2. ISSN 0026-6493. S2CID 198152030. Archived from the original on 2022-07-13. Retrieved 2021-05-01.
- A. E. Zurita, A. A. Carlini, G. J. Scillato-Yané and E. P. Tonni. (2004). Mamíferos extintos del Cuaternario de la Provincia del Chaco (Argentina) y su relación con aquéllos del este de la región pampeana y de Chile. Revista geológica de Chile 31(1):65-87 Archived 2017-03-17 at the Wayback Machine
- O. P. Recabarren, M. Pino, M. T. Alberdi. (2014). La Familia Gomphotheriidae en América del Sur: evidencia de molares al norte de la Patagonia chilena. Estudios Geológicos, Vol 70, No 1. Archived 2018-07-09 at the Wayback Machine
- Gunz, Philipp; Harvati, Katerina; Benazzi, Stefano; Cabec, Adeline Le; Bergmann, Inga; Skinner, Matthew M.; Neubauer, Simon; Freidline, Sarah E.; Bailey, Shara E. (June 2017). "New fossils from Jebel Irhoud, Morocco and the pan-African origin of Homo sapiens" (PDF). Nature. 546 (7657): 289–292. Bibcode:2017Natur.546..289H. doi:10.1038/nature22336. ISSN 1476-4687. PMID 28593953. Archived (PDF) from the original on 2020-01-08. Retrieved 2019-08-30.
- Hublin, Jean-Jacques; Ben-Ncer, Abdelouahed; Bailey, Shara E.; Freidline, Sarah E.; Neubauer, Simon; Skinner, Matthew M.; Bergmann, Inga; Le Cabec, Adeline; Benazzi, Stefano (2017-06-07). "New fossils from Jebel Irhoud, Morocco and the pan-African origin of Homo sapiens" (PDF). Nature. 546 (7657): 289–292. Bibcode:2017Natur.546..289H. doi:10.1038/nature22336. ISSN 0028-0836. PMID 28593953. Archived (PDF) from the original on 2020-01-08. Retrieved 2019-08-30.
- "These Early Humans Lived 300,000 Years Ago—But Had Modern Faces". 2017-06-07. Archived from the original on 2017-10-14. Retrieved 2017-10-13.
- Kaifu, Yousuke (2017). "Archaic Hominin Populations in Asia before the Arrival of Modern Humans: Their Phylogeny and Implications for the Southern Denisovans". Current Anthropology. 58 (17): 418–433. doi:10.1086/694318. S2CID 149397030. Archived from the original on 2020-06-10. Retrieved 2020-06-10 – via University of Chicago Press.
- Carotenuto, F. (July 1, 2018). "The well-behaved killer: Late Pleistocene humans in Eurasia were significantly associated with living megafauna only". Palaeogeography, Palaeoclimatology, Palaeoecology. 500: 24–32. Bibcode:2018PPP...500...24C. doi:10.1016/j.palaeo.2018.03.036. PMC 5263868. PMID 28106043.
- Stuart, Anthony (November 1991). "Mammalian Extinctions in the Late Pleistocene of Northern Eurasia and North America". Biological Reviews. 66 (4): 453–566. doi:10.1111/j.1469-185X.1991.tb01149.x. PMID 1801948. S2CID 41295526. Archived from the original on 2021-05-10. Retrieved 2021-05-09.
- Zimmermann, Kim Ann (29 August 2017). "Pleistocene Epoch: Facts About the Last Ice Age". livescience.com. Archived from the original on 2020-04-13. Retrieved 2021-05-05.
- Hirst, K. Kris. "What Did Australia Look Like When the First People Arrived?". ThoughtCo. Archived from the original on 2020-10-20. Retrieved 2021-05-05.
- "Australia's Megafauna". Archived from the original on 2018-03-24. Retrieved 2008-12-17.
- "Death of the Megafauna". Archived from the original on 2010-10-21. Retrieved 2008-12-17.
- DeSantis, Larisa R. G.; Field, Judith H.; Wroe, Stephen; Dodson, John R. (2017-01-26). "Dietary responses of Sahul (Pleistocene Australia–New Guinea) megafauna to climate and environmental change". Paleobiology. 43 (2): 181–195. doi:10.1017/pab.2016.50. ISSN 0094-8373.
- David, Bruno; Arnold, Lee J.; Delannoy, Jean-Jacques; Fresløv, Joanna; Urwin, Chris; Petchey, Fiona; McDowell, Matthew C.; Mullett, Russell; Mialanes, Jerome; Wood, Rachel; Crouch, Joe; Berthet, Johan; Wong, Vanessa N.L.; Green, Helen; Hellstrom, John; GunaiKurnai Land; Waters Aboriginal Corporation (2021-02-01). "Late survival of megafauna refuted for Cloggs Cave, SE Australia: Implications for the Australian Late Pleistocene megafauna extinction debate". Quaternary Science Reviews. 253: 106781. Bibcode:2021QSRv..25306781D. doi:10.1016/j.quascirev.2020.106781. ISSN 0277-3791. S2CID 234010059. Archived from the original on 2021-05-05. Retrieved 2021-05-05.
- Price, Gilbert J.; Zhao, Jian-xin; Feng, Yue-Xing; Hocknull, Scott A. (2009-02-01). "New U/Th ages for Pleistocene megafauna deposits of southeastern Queensland, Australia". Journal of Asian Earth Sciences. 34 (2): 190–197. Bibcode:2009JAESc..34..190P. doi:10.1016/j.jseaes.2008.04.008. ISSN 1367-9120. Archived from the original on 2021-05-05. Retrieved 2021-05-05.
- van der Kaars, Sander; Miller, Gifford H.; et al. (January 20, 2017). "Humans rather than climate the primary cause of Pleistocene megafaunal extinction in Australia". Nature Communications. 8: 14142. Bibcode:2017NatCo...814142V. doi:10.1038/ncomms14142. PMC 5263868. PMID 28106043.
- Wroe, Stephen; Field, Judith (2006-11-01). "A review of the evidence for a human role in the extinction of Australian megafauna and an alternative interpretation". Quaternary Science Reviews. 25 (21–22): 2692–2703. Bibcode:2006QSRv...25.2692W. doi:10.1016/j.quascirev.2006.03.005. ISSN 0277-3791. Archived from the original on 2021-05-05. Retrieved 2021-05-05.
- Johnson, C. N.; Alroy, J.; Beeton, N. J.; Bird, M. I.; Brook, B. W.; Cooper, A.; Gillespie, R.; Herrando-Pérez, S.; Jacobs, Z.; Miller, G. H.; Prideaux, G. J. (2016-02-10). "What caused extinction of the Pleistocene megafauna of Sahul?". Proceedings of the Royal Society B: Biological Sciences. 283 (1824): 20152399. doi:10.1098/rspb.2015.2399. ISSN 0962-8452. PMC 4760161. PMID 26865301.
- Extinct dwarf elephants from the Mediterranean islands Archived 2009-01-23 at the Wayback Machine;
- "North American Extinctions v. World". Archived from the original on 2019-09-27. Retrieved 2008-12-17.
- Mammoths and Humans as late Pleistocene contemporaries on Santa Rosa Island Archived 2017-12-02 at the Wayback Machine, Institute for Wildlife Studies 6th California Islands Symposium, Larry D. Agenbroad, et al, December 2003. Retrieved 8 November 2015
- Algunas extinciones en Canarias Archived 2009-12-28 at the Wayback Machine Consejería de Medio Ambiente y Ordenación Territorial del Gobierno de Canarias
- «La Paleontología de vertebrados en Canarias.» Archived 2018-10-01 at the Wayback Machine Spanish Journal of Palaeontology (antes Revista Española de Paleontología). Consultado el 17 de junio de 2016.
- Rick, Torben C.; Hofman, Courtney A.; Braje, Todd J.; Maldonado, Jesús E.; Sillett, T Scott; Danchisko, Kevin; Erlandson, Jon M. (2012-03-01). "Flightless ducks, giant mice and pygmy mammoths: Late Quaternary extinctions on California's Channel Islands". World Archaeology. 44 (1): 3–20. doi:10.1080/00438243.2012.646101. ISSN 0043-8243. S2CID 161764677.
- "Ice Age Bay Area". Archived from the original on 2008-12-26. Retrieved 2011-05-28.
- "The Extinct Late Pleistocene Mammals of North America". PBS.
- "End of the Big Beasts". PBS. Archived from the original on 2012-04-29. Retrieved 2017-09-08.
- "Of mice, mastodons and men: human-mediated extinctions on four continents" (PDF).
- "Return to the Ice Age: The La Brea Exploration Guide". Archived from the original on 2011-08-12.
- "Large Collection of European Ice Age Megafauna Fossils: The World Museum of Man Collection". Archived from the original on 2013-03-29.