Quaternary extinction event - wikipedia Quaternary extinction event Late Pleistocene landscape of northern Spain, by Mauricio Antón ( left to right - Equus ferus, Mammuthus primigenius, Rangifer tarandus, Panthera leo spelaea, Coelodonta antiquitatis ) The Quaternary period saw the extinctions of numerous predominantly megafaunal species, which resulted in a collapse in faunal density and diversity, and the extinction of key ecological strata across the globe. The most prominent event in the Late Pleistocene is differentiated from previous Quaternary pulse extinctions by the widespread absence of ecological succession to replace these extinct species, and the regime shift of previously established faunal relationships and habitats as a consequence. The earliest casualties were incurred at 130,000 BCE ( the start of the Late Pleistocene ), however the great majority of extinctions in Afro - Eurasia and the Americas occurred during the transition from the Pleistocene to the Holocene epoch ( 13,000 BCE to 8,000 BCE ). However, this extinction wave did not stop at the end of the Pleistocene, but continued, especially on isolated islands, in human - caused extinctions, although there is debate as to whether these should be considered separate events or part of the same event. Among the main causes hypothesized by paleontologists are overkill by the widespread appearance of humans and natural climate change. A notable modern human presence first appeared during the Middle Pleistocene in Africa, and started to establish continuous, permanent populations in Eurasia and Australasia from 80,000 BCE, and the Americas from 22,000 BCE. A variant of the former possibility is the second - order predation hypothesis, which focuses more on the indirect damage caused by overcompetition with nonhuman predators. Recent studies have tended to favor the human - overkill theory. Contents 1 Pleistocene or Ice Age extinction event 1.1 Africa and Asia 1.1. 1 Megafauna that disappeared in Africa and / or Asia during the Late Pleistocene 1.2 The Pacific ( Australasia and Oceania ) 1.3 Europe and Northern Eurasia 1.4 North America and the Caribbean 1.5 South America 2 Later extinctions 3 Hunting hypothesis 3.1 Overkill hypothesis 3.2 Objections to the hunting hypothesis 4 Climate change hypothesis 4.1 Increased temperature 4.2 Arguments against the temperature hypothesis 4.3 Increased continentality affects vegetation in time or space 4.3. 1 Vegetation changes : geographic 4.3. 2 Rainfall changes : time 4.4 Arguments against the continentality hypotheses 5 Arguments against both climate change and overkill 6 Hyperdisease hypothesis 6.1 Theory 6.2 Arguments against the hyperdisease hypothesis 7 Second - order predation 7.1 Scenario 7.2 Support 7.3 Second - order predation and other theories 7.4 Arguments against the second - order predation hypothesis 7.5 Arguments against the second - order predation plus climate hypothesis 8 Comet hypothesis 8.1 Arguments against / for the comet hypothesis 9 See also 10 References 11 External links 11.1 Hyperdisease hypothesis 11.2 Second - order predation 11.3 Other links Pleistocene or ice Age extinction event See also : Timeline of extinctions in the Holocene The Late Pleistocene extinction event saw the extinction of many mammals weighing more than 40 kg. The proportional rate of megafauna extinctions is consecutively larger the greater the migratory distance from Africa. In Subsaharan Africa, 8 of 50 ( 16 % ) genera of mammalian megafauna were driven to extinction. In Asia, 24 of 46 ( 52 % ) In Europe, or 23 of 39 ( 59 % ) In Australasia, 19 of 27 ( 71 % ) In North America, 45 of 61 ( 74 % ) In South America, 58 of 71 ( 82 % ) The extinctions in the Americas entailed the elimination of all the larger ( over 1000 kg ) mammalian species of South American origin, including those that had migrated north in the Great American Interchange. Only in the continents of Australia, North America, and South America did the extinction occur at family taxonomic levels or higher. The proportional rate of megafauna extinctions being incrementally bigger the larger the migratory distance from Africa might be related to non-African megafauna and Homo sapiens sapiens ( anatomically modern humans ) not having evolved as species alongside each other. For their part specifically, Australia, North America and South America, which respectively had the highest incremental extinction rates, had no known native species of Hominoidea ( apes ) at all, much less species of Hominidae ( greater apes ), and especially not native species of the Homo subgroup ( the genus Homo comprises the species Homo sapiens, which includes modern humans, as well as several extinct species classified as ancestral to or closely related to modern humans ; all indigenous human groups are ultimately descendants of anatomically modern humans recently migrated out of Africa in anthropological time scale ). The increased rate of extinction mirrors the sequential pattern of the migration of anatomically modern humans. The further away from Africa, the more recently the area has been inhabited by humans, and the less time the environments ( including its megafauna ) had had to accustomize to human arrival and vice versa. There is no evidence of megafaunal extinctions at the height of the Last Glacial Maximum, indicating that increasing cold and glaciation were not factors. There are three main hypotheses concerning the Pleistocene extinction : The animals died off due to climate change associated with the advance and retreat of major ice caps or ice sheets. The animals were exterminated by humans : the `` prehistoric overkill hypothesis '' ( Martin, 1967 ). The extinction of the woolly mammoth ( by whatever cause, perhaps by humans ) changed the extensive grasslands to birch forests, and subsequent forest fires then changed the climate. We now know that immediately after the extinction of the mammoth, birch forests replaced the grasslands and that an era of significant fire began. There are some inconsistencies between the current available data and the prehistoric overkill hypothesis. For instance, there are ambiguities around the timing of sudden extinctions of Australian megafauna. Biologists note that comparable extinctions have not occurred in Africa and South or Southeast Asia, where the fauna evolved with hominids. Post-glacial megafaunal extinctions in Africa have been spaced over a longer interval. Evidence supporting the prehistoric overkill hypothesis includes the persistence of certain island megafauna for several millennia past the disappearance of their continental cousins. Ground sloths survived on the Antilles long after North and South American ground sloths were extinct. The later disappearance of the island species correlates with the later colonization of these islands by humans. Similarly, woolly mammoths died out on remote Wrangel Island 1,000 years after their extinction on the mainland. Steller 's sea cows also persisted in seas off the isolated and uninhabited Commander Islands for thousands of years after they had vanished from the continental shores of the north Pacific. Alternative hypotheses to the theory of human responsibility include climate change associated with the last glacial period and the Younger Dryas event, as well as Tollmann 's hypothetical bolide, which claim that the extinctions resulted from bolide impact ( s ). Such a scenario has been proposed as a contributing cause of the 1,300 - year cold period known as the Younger Dryas stadial. This impact extinction hypothesis is still in debate due to the exacting field techniques required to extract minuscule particles of extraterrestrial impact markers such as iridium at a high resolution from very thin strata in a repeatable fashion, as is necessary to conclusively distinguish the event peak from the local background level of the marker. The debate seems to be exacerbated by infighting between the Uniformitarianism camp and the Catastrophism camp. The Chalicothere vanished in the early Pleistocene Eucladoceros cranium fossil, Museo di Paleontologia di Firenze Steppe Mammoth ( Mammuthus trogontherii ) dimensions Megantereon model. A Pachycrocuta bevirostris reconstruction The modern Jaguar ( Panthera onca ), although now restricted to the Americas, originated in Asia, before colonising both sides of Beringia - Europe in the form of the European jaguar, and in the Americas as the predecessors of today 's species. Amphicyon reconstruction. Paranthropus robustus family reconstruction, by Mauricio Antón. Homotherium restoration - although Homotherium were extirpated in Africa 1.5 mya, they had spread throughout Eurasia and the Americas, remaining in South America at least until the Middle Pleistocene, and perishing in all other continents during the late Pleistocene. Pelagornis sandersi comparison with the Andean condor ( Vultur gryphus ) and the Wandering albatross ( Diomeda exulans ) Steppe bison ( Bison priscus ) cave art. Reconstructions of 3 species of the Pleistocene bovid genus Pelorovis In the back is P. oldowayensis. Lying in front of it is P. turkanensis, with a horn - span of around 3 to 4 meters from tip to tip. Kneeling is the water buffalo - like P. antiquus. Life reconstruction of the extinct Megaloceros A woolly rhinoceros ( Coelodonta antiquitatis ) from a late Pleistocene landscape in northern Spain. A cave hyena ( Crocuta crocuta spelea ) reconstruction. Megalochelys atlas reconstruction Musk oxen, present from Spain to Greenland during the late Pleistocene, were completely extirpated in Eurasia by the subatlantic Holocene - recent reintroductions from the Nearctic have substantiated their range throughout the Arctic. Wall drawing in the cave Les Combarelles in Dordogne ( wild horse, cave bear, mammoth, cave lion ). Diprotodon became extinct around 50,000 years ago. Africa and Asia See also : List of African animals extinct in the Holocene and List of Asian animals extinct in the Holocene The Old World tropics were relatively spared the Late Pleistocene extinctions. Sub-Saharan Africa and southern Asia are the only regions that have terrestrial mammals weighing over 1000 kg today. However, there are indications of a megafaunal extinction events throughout the Pleistocene, particularly around 2 million years ago, which coincide with key stages of human evolution and climatic trends. The centre of human evolution and expansion, Africa and Asia were inhabited by advanced hominids by 2mya, with Homo habilis in Africa, and Homo erectus in both continents. By the advent and proliferation of Homo sapiens circa 298,000 BCE, dominant species included Homo heidelbergensis in Africa, and ( their descendants ) Denisovians and Neanderthals with Homo erectus in Asia. There is evidence of an early migration event 268,000 BCE within Neanderthal genetics, however the earliest dating for modern human inhabitation in Israel and China is 118,000 BCE, and 71,000 BCE in Indonesia. During the early, middle and late Pleistocene, megafaunal diversity was notably reduced from these regions, often without being replaced by comparable successor fauna. Climate change has been explored as a prominent cause of extinctions in Southeast Asia. Procoptodon goliath reconstruction Thylacoleo carnifex rock art Megalania priscus skeleton, Melbourne Museum Reconstruction of the Late Pleistocene mekosuchine crocodile, Mekosuchus inexpectans, of prehistoric Fiji. Comparison of the extinct Giant Fijian Iguana, Lapitiguana impensa, and two Viti Levu Giant Pigeons, Natunaornis gigoura, from prehistoric Fiji. The American flamingo ( Phoenicopterus ruber ) was one of four species of flamingo present in Australia in the Quaternary, all of which are now either extinct or extirpated. Australia is now the only inhabited continent in the world without flamingoes. A reconstruction of normative vegetation cover at the Last Glacial Maximum, circa 18,000 years ago, based on fossil pollen samples recovered from lake and bog sediments. Megafauna that disappeared in Africa or Asia during the Early and Middle Pleistocene include : Various giraffids ( e.g. Giraffa jumae ; Giraffa extirpated in Asia during the Middle Pleistocene ) Paracamelus Camelus moreli Soergelia Damalops Parmularius Various Gazella sp. ( e.g. Gazella psolea ) Makapania Dubois ' antelope ( Dubosia santeng ) Bos acutifrons Chalicotheres ( e.g. Ancylotherium, Nestoritherium ) A few species of warthog such as Metridiochoerus Kolpochoerus Giant Eurasian beaver ( Trogontherium ) Hypolagus Hippopotamus gorgops ( a giant hippopotamus ) Serengetilagus Various members of Equidae Equus stenonis Eurygnathohippus Hipparion Assorted members of Cervidae Broad fronted moose ( Cervalces latifrons ) Cervavitus Eucladoceros Libralces Praemegaceros Various members of the order Proboscidea Deinotheriidae ( e.g. Deinotherium ) Elephas celebensis Gompotheriidae sp. ( e.g. Anancus, Gomphotherium et Sinomastodon ) Mammuthus sp. Mammuthus africanavus Mammuthus meridionalis Mammuthus trogontherii Palaeoloxodon antiquus Tetralophodon Stegolophodon Zygolophodon Metaxytherium Running hyena ( Chasmaporthetes ) Giant hyena ( Pachycrocuta ) Bear Dog ( Amphicyon lydekkeri ) Giant predatory bear ( Agriotherium ) Auvergne bear ( Ursus minimus ) Dwarf panda ( Ailuropoda microta ) et Ailuropoda wulingshanensis Viverra leakeyi African bear otter ( Enhydriodon dikikae ) Canidae sp. Canis falconeri Lycaon sekowei Merriam 's dog ( Megacyon merriami ) Xenocyon lycaonoides Trinil Dog ( Mececyon trinilensis ) Giant cheetah ( Acinonyx pardinensis ) Owen 's Panther ( Puma pardoides ) Saber - toothed cats ( Machairodontinae ) Dinofelis Hemimachairodus Homotherium ( extirpated from Africa 1.5 mya ) Machairodus Megantereon Metailurus Panthera sp. European jaguar ( Panthera ( onca ) gombaszoegensis ) Mosbach lion ( Panthera leo fossilis ) Panthera palaeosinensis Wanhsien tiger ( Panthera tigris acutidens ) Trinil tiger ( Panthera tigris trinilensis ) Ngandong tiger ( Panthera tigris soloensis ) Panthera youngi Longdan tiger ( Panthera zdanskyi ) Crocodilia sp. Crocodylus sp. Crocodylus anthropophagus Kali Gedeh giant crocodile ( species inquirenda ) Crocodylus palaeindicus Crocodylus thorbjarnarsoni Euthecodon Gavialis bengawanicus Rimasuchus Toyotamaphimeia Australopithecus Giant ape ( Gigantopithecus ) Various Homo sp. Homo ergaster Homo gautengensis Homo habilis Homo heildenbergensis ( Homo rhodesiensis ) Homo naledi Homo sapiens idaltu Homo rudolfensis Parapapio Paranthropus Theropithecus brumpti et Theropithecus oswaldi Pelagornithidae ( e.g. Pelagornis ) Megafauna that disappeared in Africa and / or Asia during the Late Pleistocene Steppe bison ( Bison priscus ) European bison ( Bison bonasus, extirpated in Western Asia ) Leptobison hanaizumiensis Aurochs ( Bos primigenius ) Bos palaesondaicus Cebu tamaraw ( Bubalus cebuensis ) Bubalus groves Leptobos sp. Naemorhedus sumatraensis Giant hartebeest ( Megalotragus ) Dorcabune Megalovis Hippotragus gigas Giant long - horned buffalo ( Pelorovis ) Irish elk ( Megaloceros giganteus ) Sinomegaceros Various Gazella sp. Rusingoryx Spirocerus sp. ( e.g. S. kiakhtensis ) Hexaprotodon Sivatherium maurusium Giant tapir ( Megatapirus ) Giant pika ( Ochotona whartoni ) Aardvark ( Orycteropus afer, extirpated in South Asia circa 13,000 BCE ) Hippopotamus ( Hippopotamus amphibius, extirpated in the Western Asia circa 1,000 BCE ) Various members of Proboscidea Loxodonta atlantica Stegodon Woolly Mammoth ( Mammuthus primigenius ) Elephas sp. Elephas hysudricus Elephas hysudrindicus Elephas maximus rubridens Palaeoloxodon sp. Palaeoloxodon namadicus ( largest land mammal on record ) Palaeoloxodon naumanni Palaeoloxodon recki Paleoloxodon turkmenicus Rhinocerotidae Ceratotherium mauritanicum Woolly rhinoceros ( Coelodonta antiquitatis ) Elasmotherium ( Elasmotherium sibiricum ) Rhinoceros philippinensis et Rhinoceros sinensis, and the South Asian rhino ( Rhinoceros sivalensis ) Stephanorhinus sp. ( e.g. Merk 's and Narrow Nosed Rhinoceros ) Eurasian cave lion ( Panthera leo spelea ) Sri Lanka lion ( Panthera leo sinhaleyus ) Japanese Leopard ( Panthera pardus ssp. ) Japanese Tiger ( Panthera tigris japonicus ) Sivapanthera Homotherium Cave hyena ( Crocuta crocuta spelaea ) Megafaunal Wolves Beringian wolf Canis lupus spelaeus Paleolithic dog Various Ursus sp. Deninger 's bear ( Ursus deningeri ) Etruscan bear ( Ursus etruscus, ancestor to both the cave bear and brown bear ) Pleistocene small cave bear ( Ursus rossicus ) Cave bear ( Ursus spelaeus ) Giant polar bear ( Ursus maritimus tyrannus ) Ailuropoda baconi ( ancestor to the Giant Panda ) Wild Equids ( Equus sp. ) Equus capensis Wild horse ( e.g. Equus ferus ferus ) Equus hydruntinus Equus mauritanicus Equus namadicus Equus sivalensis Equus yunannensis Asian ostrich ( Struthio asiaticus ) Bennu Heron ( Ardea bennuides ) Hovacrex roberti Malagasy sheldgoose ( Centrornis majori ) Hipposideros besaoka Voay Aldabrachampsus Cylindrapsis Megalochelys ( largest recorded giant tortoise in existence ) Leptoptilos robustus Shiriyanetta ( Japanese flightless duck ) Canary Islands Quail ( Coturnix gomerae ) Gallotia goliath Canariomys Long - legged bunting ( Emberiza alcoveri ) Pongo hooijeri Macaca anderssoni, Macaca jiangchuanensis and the Robust Macaque ( Macaca robustus ) Gorgopithecus Various Homo sp. Archaic African hominins ( undescribed ) Homo erectus Homo floresiensis Homo neanderthalis Homo sp. altai Homo sp. longlin Homo sapiens balangodensis The Pacific ( Australasia and Oceania ) See also : Australian megafauna, List of extinct animals of the Hawaiian Islands, and List of extinct animals of New Zealand In Sahul ( a former continent composed of Australia and New Guinea ), the sudden and extensive spate of extinctions occurred earlier than in the rest of the world. Most evidence points to a 20,000 year period after human arrival circa 63,000 BCE, but scientific argument continues as to the exact date range. In the rest of the Pacific ( other Australasian islands such as New Caledonia, and Oceania ) although in some respects far later, endemic fauna also usually perished quickly upon the arrival of humans in the late Pleistocene and early Holocene. This section does not include any spate of extinctions post 1000 BCE ( e.g. subatlantic New Zealand or Hawaii ). The extinctions in the Pacific included : Various members of Diprotodontidae Diprotodon sp. ( giant relatives of the wombats ) Euowenia sp. ( diprotodont ) Euryzygoma dunense ( diprotodont ) Hulitherium tomasetti ( diprotodont ) Maokopia ronaldi ( diprotodont ) Nototherium sp. ( diprotodont ) Zygomaturus sp. ( a `` marsupial rhino '' ) Various members of Macropodidae Macropus sp. ( e.g. M. titan, M. pearsoni, giant kangaroo ) Procoptodon sp. ( e.g. P. goliath, hoof - toed, giant short - faced kangaroos ) Propleopus oscillans ( an omnivorous kangaroo ) Protemnodon sp. ( giant wallaby ) Simosthenurus sp. ( a giant kangaroo ) Sthenurus sp. ( a giant kangaroo ) Troposodon sp. ( wallaby ) Various members of Vombatidae Lasiorhinus angustidens ( giant wombat ) Phascolomys ( giant wombat ) Phascolonus sp. ( giant wombat ) Ramasayia magna ( giant wombat ) Vombatus hacketti ( Hackett 's wombat ) Warendja wakefieldi ( dwarf wombat ) Palorchestes sp. ( a marsupial `` tapir '' ) Zaglossus hacketti ( a giant echidna ) Phascolarctos stirtoni ( a giant koala ) Megalibgwilia ( oldest known echidna, same extinction period ) Wonambi ( a five - to - six - metre - long Australian constrictor snake ) Thylacoleo carnifex ( a lioness - sized marsupial carnivore ) Thylacinus cynocephalus ( extirpated on mainland Australia and New Guinea ) Sarcophilus laniarius et Sarcophilus moornaensis ( giant forms of the Tasmanian Devil ) Megalania prisca ( a giant predatory monitor lizard ) Crocodilia sp. Ikanogavialis ( the last fully marine crocodilian ) Mekosuchus sp. ( two meters long, last fully terrestrial crocodile, South Pacific Islands ) Pallimnarchus sp. ( a giant Australian freshwater crocodile ) Quinkana sp. ( giant Australian terrestrial crocodile ) Volia ( a two - to - three meter long mekosuchine crocodylian, apex predator of Pleistocene Fiji ) Meiolania et Ninjemys ( giant armoured tortoises ) Giant Iguana ( Lapitiguana et Brachylophus gibbonsi ) Pygmy Cassowary ( Casuarius lydekkeri ) Genyornis newtoni ( a three meter tall dromornthid, often referred to in vernacular as ' the last thunder bird ' ) Powerful goshawk and the Gracile goshawk ( Accipiter efficax et Accipiter quartus ) Sylviornis ( giant, flightless New Caledonian galliform - largest in existence ) Noble megapode ( Megavitornis altirostris ) New Caledonian gallinule ( Porphyrio kukwiedei ) Giant megapodes Giant malleefowl ( Leipoa gallinacea ) Pile - builder megapode ( Megapodius molistructor ) Consumed scrubfowl ( Megapodius alimentum ) Viti Levu scrubfowl ( Megapodius amissus ) New Caledonian ground dove ( Gallicolumba longitarsus ) New Caledonian snipe et Viti Levu snipe ( Coenocorypha miratropica et Coenocorypha neocaledonica ) Niue night heron ( Nycticorax kalavikai ) Marquesas cuckoo - dove ( Macropygia heana ) New Caledonian barn owl ( Tyto letocarti ) Various Galliraillus sp. Kaua'i mole duck ( Talpanas lippa, a blind, flightless, terrestrial Hawaiian duck ) Apteribis ( a giant, flightless ibis ) Lowland kagu ( Rhynochetos orarius ) Viti Levu giant pigeon ( Natunaornis gigoura ) American Flamingo ( Phoenicopterus ruber, extirpated in Australia ) Xenorhynchopsis minor et Xenorhynchopsis tibialis ( Australian flamingo ) Ocyplanus proeses ( Australian flamingo ) The woolly mammoth became extinct around 10,000 BCE -- except for diminutive relict populations on St. Paul Island and Wrangel Island, which humans did not colonise until 3,600 BCE and 2,000 BCE respectively. Cave bear ( Ursus spelaeus ) Models of the straight - tusked elephant ( Paleoloxodon antiquus ). Elasmotherium reconstruction Hippopotamuses ( Hippopotamus sp. ) inhabited Great Britain until 80,000 BCE, whence due to glacial shifts, hippopotamuses were restricted to Southern - Eastern Europe, Mediterranean islands and finally Western Asia until 1,000 BCE. Some extinct megafauna, such as the bunyip - like Diprotodon, may remain in folk memory or be the sources of cryptozoological legends. Europe and northern Eurasia The Leopard ( Panthera pardus ) inhabited the entire expanse of Afro - Eurasia below the 54th parallel north, from modern day Spain and the UK in the west, to South Africa in the south, and Siberia, Japan and Sundaland in the east during the Late Pleistocene. This geography spans the entirety of the European continent, and stretches into Northern Asia, through the Caucasus and Central Asia to Northern China, Siberia and Beringia. During the Late Pleistocene, this region was noted for its great diversity and dynamism of biomes, including the warm climes of the Mediterranean basin, open temperate woodlands, arid plains, mountainous heathland and swampy wetlands, all of which were vulnerable to the severe climatic fluctuations of the interchanges between glacial and interglacials periods ( stadials ). However, it was the expansive mammoth steppe which was the ecosystem which united and defined this region during the Late Pleistocene. One of the key features of Europe 's Late Pleistocene climate was the often drastic turnover of conditions and biota between the numerous stadials, which could set within a century. For example, during glacial periods, the entire North Sea was drained of water to form Doggerland. The final major cold spell occurred from 25,000 BCE to 18,000 BCE, and is known as the Last Glacial Maximum, when the Fenno - Scandinavian ice sheet covered much of northern Europe, while the Alpine ice sheet occupied significant parts of central - southern Europe. Europe, and in particular northern Eurasia, being far colder and drier than today, was largely hegemonized by the mammoth steppe, an ecosystem dominated by palatable high - productivity grasses, herbs and willow shrubs. This supported an extensive biota of grassland fauna, and stretched eastwards from Spain in the Iberian Peninsula to the Yukon in modern - day Canada. The area was populated by many species of grazers which assembled in large herds similar in size to those in Africa today. Populous species which roamed the great grasslands included the woolly mammoth, woolly rhinocerous, Elasmotherium, steppe bison, Pleistocene horse, muskox, Cervalces, reindeer, antelope ( Parabubalis, Procapra, Saiga, Spirocerus ) and steppe pika. Carnivores included cave lion, Homotherium, cave hyena, grey wolf, dhole, and the arctic fox. At the edges of these large stretches of grassland could be found more shrub - like terrain and dry conifer forests and woodland ( akin to forest steppe or taiga ). The browsing collective of megafauna included woolly rhinoceros, Irish elk, moose, Cervalces, tarpan, aurochs, woodland bison, camels and smaller deer ( Capreolus, Cervus, Moschus ). Brown bears, wolverines, cave bear, wolves, lynx, leopards, and red foxes also inhabited this biome. Tigers were at stages also present, from the edges of Eastern Europe around the Black Sea to Beringia. The more mountainous terrain, incorporating montane grasslands, subalpine conifer forests, alpine tundra and broken, craggy slopes, was occupied by several species of mountain - going animals like argali, chamois, ibex, mouflon, pika, wolves, leopards, Ursus sp. and lynx, with snow leopards, Baikal yak and snow sheep in Northern Asia. Arctic tundra, which lined the north of the mammoth steppe, reflected modern ecology with species such as the polar bear, wolf, reindeer and muskox. Other biomes, although less noted, were significant in contributing to the diversity of fauna in Late Pleistocene Europe. Warmer grasslands such as temperate steppes and Mediterranean savannahs hosted Stephanorhinus, gazelle, European wisent, asian ostriches, Leptobos, cheetahs, and onager. These biomes also contained an assortment of mammoth steppe fauna, such as saiga antelope, lions, Homotherium, cave hyenas, wolves, Pleistocene horse, steppe bison, Spirocerus, aurochs, and camels. Temperate coniferous, deciduous, mixed broadleaf and Mediterranean forests and open woodlands accommodated straight - tusked elephants, Praemegaceros, Stephanorhinus, wild boar, bovids such as European wisent, tahr and tur, species of Ursus such as the Etruscan bear, and smaller deer ( Capreolus, Cervus, Dama, Haploidoceros ) with several mammoth steppe species, such as lynx, tarpan, wolves, dholes, moose, Irish Elk, woodland bison, leopards, and aurochs. Woolly rhinoceros and mammoth occasionally resided in these temperate biomes, mixing with predominately temperate fauna to escape harsh glacials. In warmer wetlands, European water buffalo and hippopotamus were present. Although these habitats were restricted to micro refugia and to Southern Europe and its fringes, being in Iberia, Italy, the Balkans, Ukraine 's Black Sea basin, the Caucasus, and Western Asia, during inter-glacials these biomes had a far more northernly range. For example, hippopotamus inhabited Great Britain and straight - tusked elephant the Netherlands, as recently as 80,000 BCE and 42,000 BCE respectively. The first possible indications of habitation by hominins are the 7.2 million year old finds of Graecopithecus, and 5.7 million year old footprints in Crete - however established habitation is noted in Georgia from 1.8 million years ago, proceeded by Germany and France, via Homo erectus. Prominent co-current and subsequent species include Homo antecessor, Homo cepranensis, Homo heidelbergensis, Neanderthals and Denisovians, preceding human habitation circa 38,000 BCE. Europe 's Late Pleistocene biota went through two phases of extinction. Some fauna became extinct before 13,000 BCE, in staggered intervals, particularly between 50,000 BCE and 30,000 BCE. Species include cave bear, Elasmotherium, straight - tusked elephant, Stephanorhinus, water buffalo, Neanderthals, gazelle, and Homotherium. However, the great majority of species were extinguished, extirpated or experienced severe population contractions between 13,000 BCE and 9,000 BCE, ending with the Younger Dryas. At that time there were small ice sheets in Scotland and Scandinavia. The mammoth steppe disappeared from the vast majority of its former range, either due to a permanent shift in climatic conditions, or an absence of ecosystem management due to decimated, fragmented or extinct populations of megaherbivores. This led to a region wide extinction vortex, resulting in cyclically diminishing bio-productivity and defaunation. Insular species on Mediterranean islands such as Sardinia, Sicily, Malta, Cyprus and Crete, went extinct around the same time as humans colonised those islands. Fauna included dwarf elephantids, megacerines and hippopotamuses, and giant avians, otters and rodents. See also : List of extinct animals of Europe The ' Gallery of Lions ', representations of the Eurasian Cave Lion in Chauvet - Pont - d'Arc Cave. Homotherium restoration. Reconstruction of the five phenotypes of Pleistocene wild horse. The coat colours and dimensions are based on genetic evidence and historic descriptions. A model of an adult Neanderthal male head and shoulders on display in the Hall of Human Origins in the National Museum of Natural History in Washington, D.C. Modern cheetah ( Acinonyx jubatus ) replaced giant cheetah ( Acinonyx pardinensis ) in Eurasia after the Middle Pleistocene, and inhabited a range from Eastern Europe and the Balkans to China. Today, the critically endangered Eurasian cheetah are now restricted to Iran. Saiga antelope ( Saiga sp. ) inhabited a range from England and France to the Yukon in the Late Pleistocene, diversifying into two species. S. borealis is now extinct and the critically endangered S. tartica is now limited to steppe in Kazakhstan and Mongolia. ( 80,000 -- 4,000 years ago ) Woolly mammoth ( Mammuthus primigenius ) Dwarf Mammoth Cretan Dwarf Mammoth ( Mammuthus creticus ) Dwarf Sardinian Mammoth ( Mammuthus lamarmorai ) Straight Tusked Elephant ( Palaeoloxodon antiquus ) Asian Straight Tusked Elephant ( Paleoloxodon namadicus, Northern Asia ) Dwarf Elephant Palaeoloxodon chaniensis Palaeoloxodon cypriotes Palaeoloxodon falconeri Palaeoloxodon mnaidriensis Ochotona sp. ( e.g. Giant pika ( O. whartoni ) ) Woolly rhinoceros ( Coelodonta antiquitatis ) Stephanorhinus sp. ( e.g. Merk 's and Narrow Nosed Rhinoceros ) Elasmotherium ( Elasmotherium sibiricum ) Equus sp. ( e.g. Wild Horse ( E. ferus ssp. ) Equus cf. galllicus European Ass ( E. hydruntinus ) Equus cf. latipes Equus cf. lenensis Equus cf. uralensis Irish elk ( Megaloceros giganteus ) Praemegaceros Cretan dwarf megacerine ( Candiacervus ) Broad - fronted moose ( Cervalces latifrons ) Mediterranean deer ( Haploidoceros mediterraneus ) European tahr ( Hemitragus cedrensis ) Balearic Islands cave goat ( Myotragus balearicus ) Northern saiga antelope ( Saiga borealis ) Twisted - horn antelope ( Spirocerus kiakhtensis ) Goat - horned antelope ( Parabubalis capricornis ) Gazella sp. Steppe bison ( Bison priscus ) Pleistocene woodland bison ( Bison schoetensacki ) Baikal yak ( Bos baikalensis ) Giant Muskox ( Praeovibos priscus ) Leptobos sp. European water buffalo ( Bubalus murrensis ) Camelus knoblochi and other Camelus sp. Hippopotamus sp. European hippopotamus ( Hippopotamus antiquus ) Maltese Dwarf Hippopotamus ( Hippopotamus melitensis ) Cyprus Dwarf Hippopotamus ( Hippopotamus minor ) Sicilian Dwarf Hippopotamus ( Hippopotamus petlandi ) Balearic giant dormouse ( Hypnomys sp. ) Leithia sp. ( Maltese and Sicilian giant dormouse ) Robust Pleistocene European Otter ( Cyrnaonyx ) Pleistocene Mediterranean Otter ( Algarolutra ) Sardinian Giant Otter ( Megalenhydris barbaricus ) Sardinian Dwarf Otter ( Sardolutra ) European Ice Age Leopard ( Panthera pardus spelaea ) Sardinian Dhole ( Cynotherium sardous ) European Dhole ( Cuon alpinus europaeus ) Scimitar cat ( Homotherium sp. ) Lynx issiodorensis Mediterranean Cave Lynx ( Lynx spelaeus ) Cave lion ( Panthera leo spelaea ) Cave hyena ( Crocuta crocuta spelaea ) Various Ursus sp. Etruscan bear ( Ursus etruscus ) Deninger 's bear ( Ursus deningeri ) Gamssulzen Cave Bear ( Ursus ingressus ) Pleistocene small cave bear ( Ursus rossicus ) Cave bear ( Ursus spelaeus ) Giant polar bear ( Ursus maritimus tyrannus ) Asian Ostrich ( Struthio asiaticus ) Giant Swan ( Cygnus falconer i ) Cretan Owl ( Athene cretensis ) Yakutian Goose ( Anser djuktaiensis ) Pleistocene European Crane s ( Grus primigenia et Grus melitensis ) Neanderthals ( Homo neanderthalensis ), survived until about 40,000 years ago in the Iberian peninsula. Denisovians ( Homo sp. altai ) Many species extant today were present in areas either far to the south or west of their contemporary ranges - for example, all the arctic fauna on this list inhabited regions as south as the Iberian Peninsula at various stages of the Late Pleistocene. Recently extinct organisms are noted as †. Species extirpated from significant portions of or all former ranges in Europe and Northern Eurasia during the Quaternary extinction event include - † European Lion ( Panthera leo europaea ) Tiger ( Panthera tigris, from the Ukrainian Black Sea to Beringia ) Cheetah ( Acinonyx jubatus ) Persian Leopard ( Panthera pardus ciscaucasica ) Snow Leopard ( Panthera uncia ) Eurasian and Iberian Lynx ( Lynx lynx et Lynx pardinus ) Wolverine ( Gulo gulo ) Polar Bear ( Ursus maritimus ) Arctic Fox ( Vulpes lagopus ) Dhole ( Cuon alpinus ) Gray Wolf ( † Megafaunal et Beringian wolf, and the Paleolithic dog ( Canis lupus ) ) † Tarpan ( Equus ferus ferus ) Fallow Deer ( Dama dama ) Mouflon ( Ovis orientalis orientalis ) Chamois ( Rupicapra spp. ) West Caucasian Tur ( Capra caucasica ) Saiga Antelope ( Saiga tatarica ) Reindeer ( Rangifer tarandus ) Moose ( Alces alces ) Onager ( Equus hemionus ) † Aurochs ( Bos primigenius ) European Bison ( Bison bonasus ) Asian water buffalo ( Bubalus arnee ) Musk ox ( Ovibos moschatus ) Asian Elephant ( Elephas maximus, from the Black Sea to Northern China ) Steppe pika ( Ochotona pusilla ) Great Jerboa ( Allactaga major ) Hippopotamus ( Hippopotamus amphibius ) Northern Bald Ibis ( Geronticus eremita ) † Great Auk ( Pinguinus impennis ) Snowy Owl ( Bubo scandiacus ) Barbary Monkey ( Macaca sylvanus ) North America and the caribbean Short faced bear ( Arctodus simus ) Chendytes lawi et Oncorhynchus rastrosus Life restoration of the Yukon wild horse, Equus lambei. See also : List of North American animals extinct in the Holocene Reconstruction of the Western Camel, Camelops hesternus Life restoration of Cervalces scotti. Bison latifrons, fossil buffalo skeleton ( public display, Cincinnati Museum of Natural History & Science, Cincinnati, Ohio, USA ). Californian Turkey ( Meleagris californica ) and Megafaunal Californian Condor ( Gymnogyps amplus ) fossil displays at La Brea Tar Pits Reconstruction of the Cuban Giant Owl, Ornimegalonyx oteroi, of Pleistocene Cuba, with the carcass of a large solenodon. Life restoration of the Shasta Ground Sloth, Nothrotheriops shastensis. Glyptotherium reconstruction Mixotoxodon larenis reconstruction. Reconstruction of Smilodon fatalis Reconstruction of Panthera leo atrox Columbian Mammoth ( Mammuthus columbi ) reconstruction Graphical reconstruction of Mammut americanum. The Dhole, now restricted to the southern portions of Asia, was present from the Iberia to Mexico during the Late Pleistocene. A Chacoan peccary ( Catagonus wagneri ), believed to be the closest surviving relative of the extinct Platygonus. Size comparison of Smilodon fatalis ( purple ), S. popular ( green ), and S. gracilis ( orange ) with modern human for scale. Each grid segment = 1 square meter. Life restoration of Arctotherium bonariense. Reconstruction of Canis dirus with two possible aspects according to its probable geographic origin : North American or South American. Cuvieronius reconstruction Reconstruction of a Macrauchenia mother and calf, from Pleistocene South America. A Toxodon skull in an exhibition commemorating the 200th anniversary of Charles Darwin 's birth, Esplanada dos Ministérios, Brasília An illustration of Megatherium. Doedicurus clavicaudatus reconstruction, distributed in the temperate savannahs and woodlands of South America. Fossil reconstruction of Panochthus frenzelianus with metal model. Fossil skull of Hippidion, a genera of native South American horse which went extinct in the early Holocene ( 6,000 BCE ). The disputed Late Pleistocene remains of a phorusrhacid in Uruguay are similar in size to the above Pliocene age Procariama simplex. During the last 60,000 years, including the end of the last glacial period, approximately 51 genera of large mammals have become extinct in North America. Of these, many genera extinctions can be reliably attributed to a brief interval of 11,500 to 10,000 radiocarbon years before present, shortly following the arrival of the Clovis people in North America. Prominent paleontological sites include Mexico, ( 1 ) and Panama, the crossroads of the American Interchange. ( 2 ) Most other extinctions are poorly constrained in time, though some definitely occurred outside of this narrow interval. In contrast, only about half a dozen small mammals disappeared during this time. Previous North American extinction pulses had occurred at the end of glaciations, but not with such an ecological imbalance between large mammals and small ones. ( Moreover, previous extinction pulses were not comparable to the Quaternary extinction event ; they involved primarily species replacements within ecological niches, while the latter event resulted in many ecological niches being left unoccupied ). Such include the last native North American terror bird ( Titanis ), rhinoceros ( Aphelops ) and hyena ( Chasmaporthetes ). Human habitation commenced unequivacolly approximately 22,000 BCE north of the glacier, and 13,000 BCE south, however disputed evidence of southern human habitation exists from 130,000 BCE and 17,000 BCE onwards, at sites in California and Meadowcroft in Pennsylvania. The megafaunal extinctions include forty one genera of herbivores ( H ), and twenty carnivores ( C ). North American extinctions included : All forms of Pleistocene wild horse ( Equus ) ( H ) Equus alaskae ( H ) Equus cedralensis ( H ) Mexican horse ( Equus conversidens ) ( H ) Equus complicatus ( H ) Stilt - legged horse ( Equus francisci ) ( may be a synonym of Mexican horse ) ( H ) Tarpan ( Equus ferus ferus ) ( H ) Equus fraternus ( H ) Equus giganteus ( H ) Yukon horse ( Equus lambei ) ( H ) Equus mexicanus ( H ) Pacific Horse ( Equus pacificus ) ( H ) Western Horse ( Equus occidentalis ) ( H ) Equus semiplicatus ( H ) Hagerman horse ( Equus simplicidens ) ( H ) Scott 's horse ( Equus scotti ) ( H ) All members of North American tapir ( Tapirus, four species ) ( H ) California tapir ( Tapirus californicus ) ( H ) Cope 's tapir ( Tapirus copei ) ( H ) Merriam 's tapir ( Tapirus merriami ) ( H ) Vero tapir ( Tapirus veroensis ) ( H ) Various members of Camelidae Western camel ( Camelops hesternus ) ( H ) Stilt legged llama ( Hemiauchenia ) ( H ) Stout legged llama ( Paleolama ) ( H ) Three of the last four Antilocapridae genera, only pronghorns survived ) ( H ) Capromeryx ( H ) Stockoceros ( H ) Tetrameryx ( H ) American mountain deer ( Odocoileus lucasi ) ( H ) Stag - moose ( Cervalces scotti ) ( H ) Shrub - ox and Harlan 's muskox ( the Arctic Musk ox survived ) ( H ) Harrington 's mountain goat ( Oreamnos harringtoni, smaller and more southern distribution than its surviving relative ) ( H ) Bison ( only Bison bison in North America, and Bison bonasus in Eurasia, survived ) ( H ) Ancient bison ( Bison antiquus ) ( H ) Long - horned / Giant bison ( Bison latifrons ) ( H ) Steppe bison ( Bison priscus ) ( H ) Bison occidentalis ( H ) Californian beaver ( Castor cf. californicus ) Giant beaver ( Castoroides ohioensis et Castoroides leiseyorum ) ( H ) Aztlan rabbit ( Aztlanolagus sp. ) ( H ) Saiga antelope ( Saiga tatarica, extirpated ) ( H ) Giant tortoise ( Hesperotestudo sp. et Gopherus donlaloi ) ( H ) Teratorn ( Teratornithidae ) ( C ) Aiolornis incredibilis ( C ) Cathartornis gracilis ( C ) Oscaravis olsoni ( C ) Teratornis merriami ( C ) Teratornis woodburnensis ( C ) Clark 's Condor ( Breagyps sp. ) ( C ) La Brea / Asphalt Stork ( Ciconia maltha ) ( C ) storks ( Mycteria wetmorei ) Pleistocene Black Vulture ( Coragyps occidentalis ) ( C ) Megafaunal Californian Condor ( Gymnogyps amplus ) ( C ) Cuban Condor ( Gymnogyps varonai ) ( C ) American neophrone vulture ( Neophrontops americanus ) ( C ) Puerto Rican crow ( Corvus pumilis ) ( C ) Bahaman, Puerto Rican, Terrestrial caracara ( Caracara sp. ) ( C ) Cuban et Hispaniolan caracara ( Milvago sp. ) ( C ) Woodward 's Eagle ( Amplibuteo woodwardi ) ( C ) Cuban Great Hawk ( Buteogallus borrasi ) ( C ) Daggett 's Eagle ( Buteogallus daggetti ) ( C ) Fragile Eagle ( Buteogallus fragilis ) ( C ) Cuban Giant - Hawk ( Gigantohierax suarezi ) ( C ) Errant Eagle ( Neogyps errans ) ( C ) Grinnell 's Crested Eagle ( Spizaetus grinnelli ) Willett 's Hawk - eagle ( Spizaetus willetti ) Caribbean titan - hawk ( Titanohierax ) ( C ) Brea Miniature Owl ( Asphaltoglaux ) ( C ) Kurochkin 's Pygmy Owl ( Glaucidium kurochkini ) ( C ) Brea Owl ( Oraristix brea ) ( C ) Cuban Giant Owl ( Ornimegalonyx ) ( C ) Cope 's and Minute Flamingos ( Phoenicopterus minutus et Phoenicopterus copei ) ( C ) Jamaican Ibis ( Xenicibis xympithecus ) ( C ) Bermuda flightless duck ( Anas pachyscelus ) ( H ) Californian Flightless Sea Duck ( Chendytes lawi ) ( C ) Mexican Stiff - tailed Duck ( Oxyura zapatima ) Pleistocene Mexican Divers ( Plyolimbus baryosteus et Podiceps parvus ) Pleistocene Mexican Cormorants ( Phalacrocorax goletensis and P. chapalensis ) Dow 's Puffin ( Fratercula dowi ) ( C ) Bermuda flicker ( Colaptes oceanicus ) Nesotrochis sp. ( e.g. Nesotrochis debooyi ) ( C ) Barbados rail ( Incertae sedis ) ( C ) Cuban Flightless Crane ( Grus cubensis ) ( H ) La Brea Crane ( Grus pagei ) ( H ) Saint Croix Macaw ( Ara autocthones ) ( H ) Mexican thick - billed parrot ( Rhynchopsitta phillipsi ) Turkeys ( Meleagris californica et Meleagris crassipes ) ( H ) Sabertooth Salmon ( Oncorhynchus rastrosus ) ( C ) Pristine mustached bat ( Pteronotus ( Phyllodia ) pristinus ) ( C ) Antilles monkey ( Xenotrichini ) ( H ) Steller 's Sea Cow ( Hydrodamalis gigas, extirpated in North America ) ( H ) Neochoerus ( e.g. Pickney 's capybara, N. pinckneyi ) ( H ) Giant hutia ( Heptaxodontidae ) ( H ) Giant pika ( Ochotona whartoni ) ( H ) Giant anteater ( Myrmecophaga tridactyla, extirpated, range partially recolonised ) Eremotherium, a megatheriid ground sloth ( H ) Nothrotheriops ( ' Nothrotherium ' ), a nothrotheriid ground sloth ( H ) Megalonyx, Nohochichak, and Xibalbaonyx, megalonychid ground sloths ( H ) Paramylodon and Glossotherium, mylodontid ground sloth s ( H ) Greater Antillean Dwarf Ground Sloths ( Megalonychidae ) ( H ) Acratocnus ( H ) Habanocnus ( H ) Megalocnus ( H ) Megalonyx ( H ) Miocnus ( H ) Neocnus ( H ) Various members of Glyptodontidae Glyptotherium ( H ) Pachyarmatherium ( H ) Beautiful armadillo ( Dasypus bellus ) ( H ) Pampatheres ( e.g. Holmesina ) ( H ) Mixotoxodon ( H ) Californian sea otter ( Enhydra macrodonta ) ( C ) Short - faced skunk ( Brachyprotoma obtusata ) ( C ) Short - faced bear ( Arctodus simus et Arctodus pristinus, one of the largest terrestrial mammal carnivores of all time ) ( C ) Florida cave bear ( Tremarctos floridanus ) ( C ) South American short - faced bear ( Arctotherium ) ( C ) Giant polar bear ( Ursus maritimus tyrannus, a possible inhabitant ) ( C ) Saber - toothed cat ( Smilodon fatalis ) ( C ) Homotherium ( Homotherium serum ) ( C ) American lion ( Panthera leo atrox, endemic to North America after 340,000 BP ) ( C ) Eurasian cave lion ( Panthera leo spelea, present only as far as modern day Yukon ) ( C ) Pleistocene North American and South American Jaguars ( Panthera onca augusta et Panthera onca mesembrina, range semi-recolonised by other subspecies ) ( C ) American cheetah ( Miracinonyx, not a true cheetah ) ( C ) Cougar ( Puma concolor, megafaunal ecomorph extirpated from North America, South American populations recolonised former range ) ( C ) Jaguarundi ( Puma yagouaroundi, extirpated, range semi-recolonised ) ( C ) Margay ( Leopardus weidii, extirpated ) ( C ) Ocelot ( Leopardus pardalis, extirpated, range marginally recolonised ) ( C ) Dhole ( Cuon alpinus, extirpated ) ( C ) Various Canis sp. Dire wolf ( Canis dirus ) ( C ) Pleistocene coyote ( Canis latrans orcutti ) ( C ) Megafaunal wolf ( e.g. Beringian wolf ( Canis lupus ) ) ( C ) Gomphotheriidae sp. ( H ) Cuvieronius ( H ) Stegomastodon ( H ) Mammoth ( Mammuthus ) ( H ) Columbian mammoth ( Mammuthus columbi ) ( H ) Pygmy mammoth ( Mammuthus exilis ) ( H ) Woolly mammoth ( Mammuthus primigenius ) ( H ) American mastodon ( Mammut americanum ) ( H ) Flat - headed peccary ( Platygonus sp. ) and long - nosed peccary ( Mylohyus sp. ) ( H ) Pleistocene Yucatán peccary ( Muknalia minimus ) ( H ) Collared peccary ( Pecari tajacu, extirpated, range semi-recolonised ) ( H ) The survivors are in some ways as significant as the losses : bison ( H ), grey wolf ( C ), lynx ( C ), grizzly bear ( C ), American black bear ( C ), deer ( e.g. caribou, moose, waipiti ( elk ), Odocoileus sp. ) ( H ), pronghorn ( H ), white - lipped peccary ( H ), muskox ( H ), bighorn sheep ( H ), and mountain goat ( H ) ; the list of survivors also include species which were extirpated during the Quaternary extinction event, but recolonised at least part of their ranges during the mid-holocene from South American relict populations, such as the cougar ( C ), jaguar ( C ), giant anteater ( C ), collared peccary ( H ), ocelot ( C ), margay ( C ), and jaguarundi ( C ). All save the pronghorns and giant anteaters were descended from Asian ancestors that had evolved with human predators. Pronghorns are the second fastest land mammal ( after the cheetah ), which may have helped them elude hunters. More difficult to explain in the context of overkill is the survival of bison, since these animals first appeared in North America less than 240,000 years ago and so were geographically removed from human predators for a sizeable period of time. Because ancient bison evolved into living bison, there was no continent - wide extinction of bison at the end of the Pleistocene ( although the genus was regionally extirpated in many areas ). The survival of bison into the Holocene and recent times is therefore inconsistent with the overkill scenario. By the end of the Pleistocene, when humans first entered North America, these large animals had been geographically separated from intensive human hunting for more than 200,000 years. Given this enormous span of geologic time, bison would almost certainly have been very nearly as naive as native North American large mammals. The culture that has been connected with the wave of extinctions in North America is the paleo - Indian culture associated with the Clovis people ( q.v. ), who were thought to use spear throwers to kill large animals. The chief criticism of the `` prehistoric overkill hypothesis '' has been that the human population at the time was too small and / or not sufficiently widespread geographically to have been capable of such ecologically significant impacts. This criticism does not mean that climate change scenarios explaining the extinction are automatically to be preferred by default, however, any more than weaknesses in climate change arguments can be taken as supporting overkill. Some form of a combination of both factors could be plausible, and overkill would be a lot easier to achieve large - scale extinction with an already dying population due to climate change. Lack of tameable megafauna was perhaps one of the reasons why Amerindian civilizations evolved differently from Old World ones. Critics have disputed this by arguing that llamas, alpacas, and bison were domesticated. South America See also : List of South American animals extinct in the Holocene South America had been isolated as an island continent for many millions of years, and had a wide range of fauna found nowhere else, although many of them became extinct during the Great American Interchange about 3 million years ago, such as the Saparassodonta family. Those that survived the interchange included the ground sloths, glyptodonts, litopterns, pampatheres, phorusrhacids ( terror birds ) and notoungulates ; all managed to extend their range to North America. ( 3 ) In the Pleistocene, South America remained largely unglaciated except for increased mountain glaciation in the Andes, which had a two-fold effect - there was a faunal divide between the Andes, and the colder, arid interior resulted in the advance of temperate lowland woodlands, tropical savannas and deserts at the expense of rainforests. Within these open environments, megafauna diversity was extremely dense, with over 40 genera recorded from the Guerrero member of Luján Formation alone. Ultimately, by the mid-Holocene, all the preeminent genera of megafauna became extinct - the last specimens of Doedicurus and Toxodon have been dated to 4,555 BCE and 3,000 BCE respectively. Their smaller relatives remain, including anteaters, tree sloths, armadillos ; New World marsupials : opossums, shrew opossums, and the monito del monte ( actually more related to Australian marsupials ). Intense human habitation was established circa 11,000 BCE, however partly disputed evidence of pre-clovis habitation occurs since 46,000 BCE and 20,000 BCE, such as at the Serra da Capivara National Park ( Brazil ) and Monte Verde ( Chile ) sites. Today the largest land mammals remaining in South America are the wild camels of the Lamini group, such as the guanacos and vicuñas, and the Tapirus genus, of which Baird 's tapir can reach up to 400 kg. Other notable surviving large fauna are peccaries, marsh deer ( Capreolinae ), giant anteaters, spectacled bears, maned wolves, pumas, ocelots, jaguars, rheas, emerald tree boas, boa constrictors, anacondas, american crocodiles, caimans, and giant rodents such as capybaras. Sabre toothed cat ( Smilodon fatalis et Smilodon populator ) Pleistocene North American and South American jaguar ( Panthera onca augusta et Panthera onca mesembrina ) South American short - faced bear ( Arctotherium sp. include largest recorded bear ) Giant vampire bat ( Desmodus draculae ) Dire wolf ( Canis dirus ) Nehring 's wolf ( Canis nehringi ) Theriodictis Protocyon Dusicyon avus et Dusicyon cultridens Pleistocene bush dog ( Speothos pacivorus ) Neochoerus Capreolinae Antifer Agalmaceros blicki Odocoileus salinae Camelidae Eulamaops Hemiauchenia Palaeolama All Pleistocene wild horse genera ( Equidae ) Equus ( Amerhippus ) Equus andium Equus insulatus Equus neogeus Hippidion ( Onohippidium ) Hippidion devillei Hippidion principale Hippidion saldiasi Gomphotheridae Cuvieronius Notiomastodon ( et ' Haplomastodon ' ) Meridiungulata Litopterna Macrauchenia Macraucheniopsis Proterotheriidae sp. ( e.g. Neolicaphrium recens ) Xenorhinotherium Notoungulata Hegetotheriidae sp. Mesotheriidae sp. Mixotoxodon Toxodon Xenarthra gen. Folivora ( ground sloths ) Mylodontidae Catonyx Glossotherium Lestodon Mylodon Nematherium Octomylodon Orophodon Scelidotherium Megatheriidae Eremotherium Megatherium Nothrotheriidae Nothropus Nothrotherium Megalonychidae Ahytherium Australonyx Diabolotherium Megistonyx Proplatyarthrus Valgipes Cingulata Dasypodidae Beautiful armadillo ( Dasypus bellus ) Eutatus Pachyarmatherium Propaopus Chlamyphoridae ( Glyptodontinae ) Doedicurus Eleutherocercus Glyptodon ( et ' Chlamydotherium oliveirai ' ) Heteroglyptodon Hoplophorus Lomaphorus Neosclerocalyptus Neuryurus Panochthus Parapanochthus Plaxhaplous Sclerocalyptus Pampatheriidae Holmesina ( et ' Chlamytherium occidentale ' ) Pampetherium Tonnicinctus Caracara Venezuelan Caracara ( Caracara major ) Seymour 's Caracara ( Caracara seymouri ) Peruvian Caracara ( Milvago brodkorbi ) ' Phorusrhacid ' ( possible terror bird remains dated to the Late Pleistocene, but these are disputed ) Caiman venezuelensis Later extinctions Main article : Holocene extinction There is no general agreement on where the Holocene, or anthropogenic, extinction begins, and the Quaternary extinction event which includes climate change resulting in the end of the last ice age ends, or if they should be considered separate events at all. Some have suggested that anthropogenic extinctions may have begun as early as when the first modern humans spread out of Africa between 100,000 and 200,000 years ago, which is supported by rapid megafaunal extinction following recent human colonisation in Australia, New Zealand and Madagascar, in a similar way that any large, adaptable predator moving into a new ecosystem would. In many cases, it is suggested even minimal hunting pressure was enough to wipe out large fauna, particularly on geographically isolated islands. Only during the most recent parts of the extinction have plants also suffered large losses. Overall, the Holocene extinction can be characterised by the human impact on the environment. The Holocene extinction continues into the 21st century, with overfishing, ocean acidification and the amphibian crisis being a few broader examples of an almost universal, cosmopolitan decline of biodiversity. Hunting hypothesis This section possibly contains original research. Please improve it by verifying the claims made and adding inline citations. Statements consisting only of original research should be removed. ( December 2010 ) The hunting hypothesis suggests that humans hunted megaherbivores to extinction, which in turn caused the extinction of carnivores and scavengers which had preyed upon those animals. Therefore, this hypothesis holds Pleistocene humans responsible for the megafaunal extinction. One variant, known as blitzkrieg, portrays this process as relatively quick. Some of the direct evidence for this includes : fossils of some megafauna found in conjunction with human remains, embedded arrows and tool cut marks found in megafaunal bones, and European cave paintings that depict such hunting. Biogeographical evidence is also suggestive : the areas of the world where humans evolved currently have more of their Pleistocene megafaunal diversity ( the elephants and rhinos of Asia and Africa ) compared to other areas such as Australia, the Americas, Madagascar and New Zealand without the earliest humans. A picture arises of the megafauna of Asia and Africa evolving alongside humans, learning to be wary of them, and in other parts of the world the wildlife appearing ecologically naive and easier to hunt. This is particularly true of island fauna, which display a disastrous lack of fear of humans. Of course, it is impossible to demonstrate this naïveté directly in ancient fauna. Circumstantially, the close correlation in time between the appearance of humans in an area and extinction there provides weight for this scenario. For example, the woolly mammoth survived on islands despite changing climatic conditions for thousands of years after the end of the last glaciation, but they died out when humans arrived around 1700 BC. The megafaunal extinctions covered a vast period of time and highly variable climatic situations. The earliest extinctions in Australia were complete approximately 50,000 BP, well before the last glacial maximum and before rises in temperature. The most recent extinction in New Zealand was complete no earlier than 500 BP and during a period of cooling. In between these extremes megafaunal extinctions have occurred progressively in such places as North America, South America and Madagascar with no climatic commonality. The only common factor that can be ascertained is the arrival of humans. This phenomenon appears even within regions. The mammal extinction wave in Australia about 50,000 years ago coincides not with known climatic changes, but with the arrival of humans. In addition, large mammal species like the giant kangaroo Protemnodon appear to have succumbed sooner on the Australian mainland than on Tasmania, which was colonised by humans a few thousand years later. Worldwide, extinctions seem to follow the migration of humans and to be most severe where humans arrived most recently and least severe where humans originated -- in Africa ( see figure `` March of Man '' below ). This suggests that prey animals and human hunting ability evolved together, so the animals evolved avoidance techniques. As humans migrated throughout the world and became more and more proficient at hunting, they encountered animals that had evolved without the presence of humans. Lacking the fear of humans that African animals had developed, animals outside of Africa were easy prey for human hunting techniques. It also suggests that this is independent of climate change. Extinction through human hunting has been supported by archaeological finds of mammoths with projectile points embedded in their skeletons, by observations of modern naïve animals allowing hunters to approach easily and by computer models by Mosimann and Martin, and Whittington and Dyke, and most recently by Alroy. A 2015, a study supported the hypothesis further by running several thousand scenarios that correlated the time windows in which each species is known to have become extinct with the arrival of humans on different continents or islands. This was compared against climate reconstructions for the last 90,000 years. The researchers found correlations of human spread and species extinction indicating that the human impact was the main cause of the extinction, while climate change exacerbated the frequency of extinctions. The study, however, found an apparently low extinction rate in the fossil record of mainland Asia. Overkill hypothesis The timing of extinctions follows the `` March of Man '' The overkill hypothesis, a variant of the hunting hypothesis, was proposed 40 years ago by Paul S. Martin, Professor of Geosciences Emeritus at the Desert Laboratory of the University of Arizona. Objections to the hunting hypothesis The major objections to the theory are as follows : In predator - prey models it is unlikely that predators could over-hunt their prey, since predators need their prey as food to sustain life and to reproduce. This criticism has been rejected by many ecologists because humans have the widest dietary choice of any predator and are perfectly capable of switching to alternative prey or even plant foods when any prey species becomes rare. Humans have indisputably hunted numerous species to extinction, which renders any argument that human predators can never hunt prey to extinction immediately invalid. There is no archeological evidence that in North America megafauna other than mammoths, mastodons, gomphotheres and bison were hunted, despite the fact, that for example camels and horses are very frequently reported in fossil history. Overkill proponents, however, say this is due to the fast extinction process in North America and the low probability of animals with signs of butchery to be preserved. Additionally, biochemical analyses have shown that Clovis tools were used in butchering horses and camels. A study by Surovell and Grund concluded `` archaeological sites dating to the time of the coexistence of humans and extinct fauna are rare. Those that preserve bone are considerably more rare, and of those, only a very few show unambiguous evidence of human hunting of any type of prey whatsoever. '' A small number of animals that were hunted, such as a single species of bison, did not go extinct. This can not be explained by proposing that surviving bison in North America were recent Eurasian immigrants that were familiar with human hunting practices, since Bison first appeared in North America approximately 240,000 years ago and then evolved into living bison. Bison at the end of the Pleistocene were thus likely to have been almost as naive as their native North American megafaunal companions. The dwarfing of animals is not explained by overkill. Numerous authors, however, have pointed out that dwarfing of animals is perfectly well explained by humans selectively harvesting the largest animals, and have provided proof that even within the 20th century numerous animal populations have reduced in average size due to human hunting. Eurasian Pleistocene megafauna became extinct in roughly same time period despite having a much longer time to adapt to hunting pressure by humans. However, the extinction of the Eurasian megafauna can be viewed as a result of a different process than that of the American megafauna. This makes the theory less parsimonious since another mechanism is required. The latter case occurred after the sudden appearance of modern human hunters on a land mass they had never previously inhabited, while the former case was the culmination of the gradual northward movement of human hunters over thousands of years as their technology for enduring extreme cold and bringing down big game improved. Thus, while the hunting hypothesis does not necessarily predict the rough simultaneity of the north Eurasian and American megafaunal extinctions, this simultaneity can not be regarded as evidence against it. Eugene S. Hunn points out that the birthrate in hunter - gatherer societies is generally too low, that too much effort is involved in the bringing down of a large animal by a hunting party, and that in order for hunter - gatherers to have brought about the extinction of megafauna simply by hunting them to death, an extraordinary amount of meat would have had to have been wasted. It is possible that those who advocate the overkill hypothesis simply have not considered the differences in outlook between typical forager ( hunter - gatherer ) cultures and the present - day industrial cultures which exist in modernized human societies ; waste may be tolerated and even encouraged in the latter, but is not so much in the former. It may be noted that in relatively recent human history, for instance, the Lakota of North America were known to take only as much bison as they could use, and they used virtually the whole animal -- this despite having access to herds numbering in the millions. Conversely, `` buffalo jumps '' featured indiscriminate killing of a herd. However, Hunn 's comments are in reference to a hunter - prey equilibrium state reached after thousands of years of coexistence, and are not relevant to hunters newly arrived on a virgin land mass full of easily taken big game. The well - established practice of industrial - scale moa butchering by the early Maori, involving enormous wastage of less choice portions of the meat, indicates that these arguments are incorrect. The hypothesis that the Clovis culture represented the first humans to arrive in the New World has been disputed recently. ( See Settlement of the Americas. ) However, they were certainly the first to leave abundant widespread evidence of their presence. Climate change hypothesis At the end of the 19th and beginning of the 20th centuries, when scientists first realized that there had been glacial and interglacial ages, and that they were somehow associated with the prevalence or disappearance of certain animals, they surmised that the termination of the Pleistocene ice age might be an explanation for the extinctions. Critics object that since there were multiple glacial advances and withdrawals in the evolutionary history of many of the megafauna, it is rather implausible that only after the last glacial would there be such extinctions. However, this criticism is rejected by a recent study indicating that terminal Pleistocene megafaunal community composition may have differed markedly from faunas present during earlier interglacials, particularly with respect to the great abundance and geographic extent of Pleistocene Bison at the end of the epoch. This suggests that the survival of megafaunal populations during earlier interglacials is essentially irrelevant to the terminal Pleistocene extinction event, because bison were not present in similar abundance during any of the earlier interglacials. Some evidence weighs against climate change as a valid hypothesis as applied to Australia. It has been shown that the prevailing climate at the time of extinction ( 40,000 -- 50,000 BP ) was similar to that of today, and that the extinct animals were strongly adapted to an arid climate. The evidence indicates that all of the extinctions took place in the same short time period, which was the time when humans entered the landscape. The main mechanism for extinction was probably fire ( started by humans ) in a then much less fire - adapted landscape. Isotopic evidence shows sudden changes in the diet of surviving species, which could correspond to the stress they experienced before extinction. Evidence in Southeast Asia, in contrast to Europe, Australia, and the Americas, suggests that climate change and an increasing sea level were significant factors in the extinction of several herbivorous species. Alterations in vegetation growth and new access routes for early humans and mammals to previously isolated, localized ecosystems were detrimental to select groups of fauna. Some evidence obtained from analysis of the tusks of mastodons from the American Great Lakes region appears inconsistent with the climate change hypothesis. Over a span of several thousand years prior to their extinction in the area, the mastodons show a trend of declining age at maturation. This is the opposite of what one would expect if they were experiencing stresses from deteriorating environmental conditions, but is consistent with a reduction in intraspecific competition that would result from a population being reduced by human hunting. Increased temperature The most obvious change associated with the termination of an ice age is the increase in temperature. Between 15,000 BP and 10,000 BP, a 6 ° C increase in global mean annual temperatures occurred. This was generally thought to be the cause of the extinctions. According to this hypothesis, a temperature increase sufficient to melt the Wisconsin ice sheet could have placed enough thermal stress on cold - adapted mammals to cause them to die. Their heavy fur, which helps conserve body heat in the glacial cold, might have prevented the dumping of excess heat, causing the mammals to die of heat exhaustion. Large mammals, with their reduced surface area - to - volume ratio, would have fared worse than small mammals. A study covering the past 56,000 years indicates that rapid warming events with temperature changes of up to 16 ° C ( 29 ° F ) had an important impact on the extinction of megafauna. Ancient DNA and radiocarbon data indicates that local genetic populations were replaced by others within the same species or by others within the same genus. Survival of populations was dependent on the existence of refugia and long distance dispersals, which may have been disrupted by human hunters. Arguments against the temperature hypothesis Studies propose that the annual mean temperature of the current interglacial that we have seen for the last 10,000 years is no higher than that of previous interglacials, yet some of the same large mammals survived similar temperature increases. Therefore, warmer temperatures alone may not be a sufficient explanation. In addition, numerous species such as mammoths on Wrangel Island and St. Paul Island survived in human - free refugia despite changes in climate. This would not be expected if climate change were responsible ( unless their maritime climates offered some protection against climate change not afforded to coastal populations on the mainland ). Under normal ecological assumptions island populations should be more vulnerable to extinction due to climate change because of small populations and an inability to migrate to more favorable climes. Increased continentality affects vegetation in time or space Other scientists have proposed that increasingly extreme weather -- hotter summers and colder winters -- referred to as `` continentality '', or related changes in rainfall caused the extinctions. The various hypotheses are outlined below. Vegetation changes : geographic It has been shown that vegetation changed from mixed woodland - parkland to separate prairie and woodland. This may have affected the kinds of food available. Shorter growing seasons may have caused the extinction of large herbivores and the dwarfing of many others. In this case, as observed, bison and other large ruminants would have fared better than horses, elephants and other monogastrics, because ruminants are able to extract more nutrition from limited quantities of high - fiber food and better able to deal with anti-herbivory toxins. So, in general, when vegetation becomes more specialized, herbivores with less diet flexibility may be less able to find the mix of vegetation they need to sustain life and reproduce, within a given area. Rainfall changes : time Increased continentality resulted in reduced and less predictable rainfall limiting the availability of plants necessary for energy and nutrition. Axelrod and Slaughter have suggested that this change in rainfall restricted the amount of time favorable for reproduction. This could disproportionately harm large animals, since they have longer, more inflexible mating periods, and so may have produced young at unfavorable seasons ( i.e., when sufficient food, water, or shelter was unavailable because of shifts in the growing season ). In contrast, small mammals, with their shorter life cycles, shorter reproductive cycles, and shorter gestation periods, could have adjusted to the increased unpredictability of the climate, both as individuals and as species which allowed them to synchronize their reproductive efforts with conditions favorable for offspring survival. If so, smaller mammals would have lost fewer offspring and would have been better able to repeat the reproductive effort when circumstances once more favored offspring survival. In 2017 a study looked at the environmental conditions across Europe, Siberia and the Americas from 25,000 -- 10,000 YBP. The study found that prolonged warming events leading to deglaciation and maximum rainfall occurred just prior to the transformation of the rangelands that supported megaherbivores into widespread wetlands that supported herbivore - resistant plants. The study proposes that moisture - driven environmental change led to the megafaunal extinctions and that Africa 's trans - equatorial position allowed rangeland to continue to exist between the deserts and the central forests, therefore fewer megafauna species became extinct there. Arguments against the continentality hypotheses Critics have identified a number of problems with the continentality hypotheses. Megaherbivores have prospered at other times of continental climate. For example, megaherbivores thrived in Pleistocene Siberia, which had and has a more continental climate than Pleistocene or modern ( post-Pleistocene, interglacial ) North America. The animals that became extinct actually should have prospered during the shift from mixed woodland - parkland to prairie, because their primary food source, grass, was increasing rather than decreasing. Although the vegetation did become more spatially specialized, the amount of prairie and grass available increased, which would have been good for horses and for mammoths, and yet they became extinct. This criticism ignores the increased abundance and broad geographic extent of Pleistocene Bison at the end of the Pleistocene, which would have increased competition for these resources in a manner not seen in any earlier interglacials. Although horses became extinct in the New World, they were successfully reintroduced by the Spanish in the 16th century -- into a modern post-Pleistocene, interglacial climate. Today there are feral horses still living in those same environments. They find a sufficient mix of food to avoid toxins, they extract enough nutrition from forage to reproduce effectively and the timing of their gestation is not an issue. Of course, this criticism ignores the obvious fact that present - day horses are not competing for resources with ground sloths, mammoths, mastodons, camels, llamas, and bison. Similarly, mammoths survived the Pleistocene Holocene transition on isolated, uninhabited islands in the Mediterranean Sea and on Wrangel Island in the Siberian Arctic until 4,000 to 7,000 years ago. Large mammals should have been able to migrate, permanently or seasonally, if they found the temperature too extreme, the breeding season too short, or the rainfall too sparse or unpredictable. Seasons vary geographically. By migrating away from the equator, herbivores could have found areas with growing seasons more favorable for finding food and breeding successfully. Modern - day African elephants migrate during periods of drought to places where there is apt to be water. Large animals store more fat in their bodies than do medium - sized animals and this should have allowed them to compensate for extreme seasonal fluctuations in food availability. The extinction of the megafauna could have caused the disappearance of the mammoth steppe. Alaska now has low nutrient soil unable to support bison, mammoths, and horses. R. Dale Guthrie has claimed this as a cause of the extinction of the megafauna there ; however, he may be interpreting it backwards. The loss of large herbivores to break up the permafrost allows the cold soils that are unable to support large herbivores today. Today, in the arctic, where trucks have broken the permafrost grasses and diverse flora and fauna can be supported. In addition, Chapin ( Chapin 1980 ) showed that simply adding fertilizer to the soil in Alaska could make grasses grow again like they did in the era of the mammoth steppe. Possibly, the extinction of the megafauna and the corresponding loss of dung is what led to low nutrient levels in modern - day soil and therefore is why the landscape can no longer support megafauna. Arguments against both climate change and overkill It may be observed that neither the overkill nor the climate change hypotheses can fully explain events : browsers, mixed feeders and non-ruminant grazer species suffered most, while relatively more ruminant grazers survived. However, a broader variation of the overkill hypothesis may predict this, because changes in vegetation wrought by either Second Order Predation ( see below ) or anthropogenic fire preferentially selects against browse species. Hyperdisease hypothesis Theory The hyperdisease hypothesis attributes the extinction of large mammals during the late Pleistocene to indirect effects of the newly arrived aboriginal humans. The Hyperdisease Hypothesis proposes that humans or animals traveling with them ( e.g., chickens or domestic dogs ) introduced one or more highly virulent diseases into vulnerable populations of native mammals, eventually causing extinctions. The extinction was biased toward larger - sized species because smaller species have greater resilience because of their life history traits ( e.g., shorter gestation time, greater population sizes, etc. ). Humans are thought to be the cause because other earlier immigrations of mammals into North America from Eurasia did not cause extinctions. Diseases imported by people have been responsible for extinctions in the recent past ; for example, bringing avian malaria to Hawaii has had a major impact on the isolated birds of the island. If a disease was indeed responsible for the end - Pleistocene extinctions, then there are several criteria it must satisfy ( see Table 7.3 in MacPhee & Marx 1997 ). First, the pathogen must have a stable carrier state in a reservoir species. That is, it must be able to sustain itself in the environment when there are no susceptible hosts available to infect. Second, the pathogen must have a high infection rate, such that it is able to infect virtually all individuals of all ages and sexes encountered. Third, it must be extremely lethal, with a mortality rate of c. 50 -- 75 %. Finally, it must have the ability to infect multiple host species without posing a serious threat to humans. Humans may be infected, but the disease must not be highly lethal or able to cause an epidemic. One suggestion is that pathogens were transmitted by the expanding humans via the domesticated dogs they brought with them. Unfortunately for such a theory it can not account for several major extinction events, notably Australia and North America. Dogs did not arrive in Australia until approximately 35,000 years after the first humans arrived and approximately 30,000 years after the megafaunal extinction was complete and as such can not be implicated. In contrast numerous species including wolves, mammoths, camelids and horses had emigrated continually between Asia and North America over the past 100,000 years. For the disease hypothesis to be applicable in the case of the Americas it would require that the population remain immunologically naive despite this constant transmission of genetic and pathogenic material. Arguments against the hyperdisease hypothesis Generally speaking, disease has to be very virulent to kill off all the individuals in a genus or species. Even such a virulent disease as West Nile Virus is unlikely to have caused extinction. The disease would need to be implausibly selective while being simultaneously implausibly broad. Such a disease needs to be capable of killing off wolves such as Canis dirus or goats such as Oreamnos harringtoni while leaving other very similar species ( Canis lupus and Oreamnos americanus, respectively ) unaffected. It would need to be capable of killing off flightless birds while leaving closely related flighted species unaffected. Yet while remaining sufficiently selective to afflict only individual species within genera it must be capable of fatally infecting across such clades as birds, marsupials, placentals, testudines, and crocodilians. No disease with such a broad scope of fatal infectivity is known, much less one that remains simultaneously incapable of infecting numerous closely related species within those disparate clades. Second - Order Predation Combination Hypotheses : Climate Change, Overkill + Climate Change, Second - Order Predation + Climate Change Overkill Hypothesis and Second - Order Predation Scenario The Second - Order Predation Hypothesis says that as humans entered the New World they continued their policy of killing predators, which had been successful in the Old World but because they were more efficient and because the fauna, both herbivores and carnivores, were more naive, they killed off enough carnivores to upset the ecological balance of the continent, causing overpopulation, environmental exhaustion, and environmental collapse. The hypothesis accounts for changes in animal, plant, and human populations. The scenario is as follows : After the arrival of H. sapiens in the New World, existing predators must share the prey populations with this new predator. Because of this competition, populations of original, or first - order, predators can not find enough food ; they are in direct competition with humans. Second - order predation begins as humans begin to kill predators. Prey populations are no longer well controlled by predation. Killing of nonhuman predators by H. sapiens reduces their numbers to a point where these predators no longer regulate the size of the prey populations. Lack of regulation by first - order predators triggers boom - and - bust cycles in prey populations. Prey populations expand and consequently overgraze and over-browse the land. Soon the environment is no longer able to support them. As a result, many herbivores starve. Species that rely on the slowest recruiting food become extinct, followed by species that can not extract the maximum benefit from every bit of their food. Boom - bust cycles in herbivore populations change the nature of the vegetative environment, with consequent climatic impacts on relative humidity and continentality. Through overgrazing and overbrowsing, mixed parkland becomes grassland, and climatic continentality increases. Support This has been supported by a computer model, the Pleistocene Extinction Model ( PEM ), which, using the same assumptions and values for all variables ( herbivore population, herbivore recruitment rates, food needed per human, herbivore hunting rates, etc. ) other than those for hunting of predators. It compares the Overkill hypothesis ( predator hunting = 0 ) with Second - Order Predation ( predator hunting varied between 0.01 and 0.05 for different runs ). The findings are that Second Order - Predation is more consistent with extinction than is Overkill ( results graph at left ). The PEM is the only test of multiple hypotheses and is the only model to specifically test combination hypotheses by artificially introducing sufficient climate change to cause extinction. When Overkill and Climate Change are combined they balance each other out. Climate Change reduces the number of plants, Overkill removes animals, therefore fewer plants are eaten. Second - Order Predation combined with Climate Change exacerbates the effect of Climate Change. ( results graph at right ). The second - order predation hypothesis is supported by the observation above that there was a massive increase in bison populations. Second - Order Predation and other theories Climate Change : Second - Order Predation accounts for the changes in vegetation, which in turn may account for the increase in continentality. Since the extinction is due to destruction of habitat it accounts for the loss of animals not hunted by humans. Second - Order Predation accounts for the dwarfing of animals as well as extinctions since animals that could survive and reproduce on less food would be selectively favored. Hyperdisease : The reduction of carnivores could have been from distemper or other carnivore disease carried by domestic dogs. Overkill : The observation that extinctions follow the arrival of humans is consistent with the Second - Order Predation hypothesis. Arguments against the Second - Order Predation hypothesis The model specifically assumes high extinction rates in grasslands, but most extinct species ranged across numerous vegetation zones. Historical population densities of ungulates were very high in the Great Plains ; savanna environments support high ungulate diversity throughout Africa, and extinction intensity was equally severe in forested environments. It is unable to explain why large herbivore populations were not regulated by surviving carnivores such as grizzly bears, wolves, pumas, and jaguars whose populations would have increased rapidly in response to the loss of competitors. It does not explain why almost all extinct carnivores were large herbivore specialists such as sabre toothed cats and short faced bears, but most hypocarnivores and generalized carnivores survived. There is no historical evidence of boom and bust cycles causing even local extinctions in regions where large mammal predators have been driven extinct by hunting. The recent hunting out of remaining predators throughout most of the United States has not caused massive vegetational change or dramatic boom and bust cycles in ungulates. It is not spatially explicit and does not track predator and prey species separately, whereas the multispecies overkill model does both. The multispecies model produces a mass extinction through indirect competition between herbivore species : small species with high reproductive rates subsidize predation on large species with low reproductive rates. All prey species are lumped in the Pleistocene Extinction Model. Everything explained by the Pleistocene Extinction Model also is explained by the multispecies model, but with fewer assumptions, so the Pleistocene Extinction Model appears less parsimonious. However, the multispecies model does not explain shifts in vegetation, nor is it able to simulate alternative hypotheses. The multispecies model therefore necessitates additional assumptions and hence is less parsimonious. Arguments against the Second - Order Predation plus climate hypothesis It assumes decreases in vegetation due to climate change, but deglaciation doubled the habitable area of North America. Any vegetational changes that did occur failed to cause almost any extinctions of small vertebrates, and they are more narrowly distributed on average. Comet hypothesis Main article : Younger Dryas impact event First publicly presented at the Spring 2007 joint assembly of the American Geophysical Union in Acapulco, Mexico, the comet hypothesis suggests that the mass extinction was caused by a swarm of comets 12,900 years ago. Using photomicrograph analysis, research published in January 2009 has found evidence of nanodiamonds in the soil from six sites across North America including Arizona, Minnesota, Oklahoma, South Carolina and two Canadian sites. Similar research found nanodiamonds in the Greenland ice sheet. Arguments against / for the comet hypothesis Debate around this hypothesis has included, among other things, the lack of an impact crater, relatively small increased level of iridium in the soil, and the relative probability of such an event. However, if the bolide struck the Laurentide ice sheet as hypothesized by Firestone et al. ( 2007 ), we would not see the typical impact crater. A spike in platinum was found in the Greenland ice cores by Petaev et al. ( 2013 ), which they view as a global signal. Platinum has more recently been found in sediments by Christopher Moore ( 2017 ). There is a lack of evidence for a population decline among the Paleoindians at 12,900 ± 100 calBP as might be expected. But see the work of Dave Anderson, ref > http://www.tandfonline.com/doi/pdf/10.1179/2055556314Z.00000000012</ref >, There is evidence that the megafaunal extinctions that occurred across northern Eurasia, North America and South America at the end of the Pleistocene were not synchronous as the bolide theory would predict. The extinctions in South America appear to have occurred at least 400 years after those in North America. Additionally, some island megafaunal populations survived thousands of years longer than populations of the same or related species on nearby continents ; examples include the survival of woolly mammoths on Wrangel Island until 3700 BP, and the survival of ground sloths in the Antilles until 4700 cal BP. Several markers for the proposed impact event are disputed by most scientists. They have asserted that the carbon spherules originated as fungal structures and / or insect fecal pellets, and that the claimed nanodiamonds are actually misidentified graphene and graphene / graphane oxide aggregates. An analysis of a similar Younger Dryas boundary layer in Belgium also did not show evidence of a bolide impact. Researchers have also not found any extraterrestrial platinum group metals in the boundary layer ; this absence is inconsistent with the hypothesized impact event. 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In Brown, J. ; Miller, P.C. ; Tieszen, L.L. ; Bunnell, F.L. An Arctic ecosystem : the coastal tundra at Barrow, Alaska. US / IBP Synthesis. Stroudsburg, PA : Dowden Hutchinson & Ross. pp. 186 -- 219. 12. CS1 maint : Multiple names : authors list ( link ) Jump up ^ Whitney - Smith, Elin ( 2008 ). `` The Evolution of an Ecosystem : Pleistocene Extinctions ''. In Minai, Ali A. ; Bar - Yam, Yaneer. Unifying themes in complex systems IV proceedings of the Fourth International Conference on Complex Systems. Springer. ISBN 978 - 3 - 540 - 73849 - 7. ^ Jump up to : Whitney - Smith, E. ( 2006 ). Clovis and Extinctions -- Overkill, Second Order Predation, Environmental Degradation in a Non-equilibrium Ecosystem `` Clovis Age Continent ''. University of New Mexico Press. Jump up ^ Whitney - Smith, Elin ( 2012 ). `` Creating the tiniest bison : A system dynamics model of ecological evolution ''. In Mendes, Ricardo Evandro. Ruminants : Anatomy, Behavior, and Diseases. Nova Biomedical. ISBN 9781620810644. ^ Jump up to : MacFee, R.D.E. & Marx, P.A. ( 1997 ). `` Humans, hyperdisease and first - contact extinctions ''. In Goodman, S. & Patterson, B.D. Natural Change and Human Impact in Madagascar. Washington D.C. : Smithsonian Press. pp. 169 -- 217. ISBN 1 - 56098 - 683 - 2. Jump up ^ MacFee, R.D.E. & Marx, P.A. ( 1998 ). `` Lightning Strikes Twice : Blitzkrieg, Hyperdisease, and Global Explanations of the Late Quaternary Catastrophic Extinctions ''. American Museum of Natural History. Jump up ^ MacPhee, Ross D.E. ; Preston Marx ( 1997 ). `` The 40,000 - year Plague : Humans, Hyperdisease, and First - Contact Extinctions ''. Natural Change and Human Impact in Madagascar. Washington, D.C. : Smithsonian Institution Press. pp. 169 -- 217. Jump up ^ Fiedel, S ( 2005 ). `` Man 's best friend : mammoth 's worst enemy ? ''. World Archaeology. 37 : 11 -- 35. doi : 10.1080 / 0043824042000329540. Jump up ^ Lyons, K, Smith, F.A., Wagner, P.J., White, E.P., and Brown, J.H. ( 2004 ). `` Was a ' hyperdisease ' responsible for the late Pleistocene megafaunal extinction ? '' ( PDF ). Ecology Letters. 7 ( 9 ) : 859 -- 68. doi : 10.1111 / j. 1461 - 0248.2004. 00643. x. CS1 maint : Multiple names : authors list ( link ) Jump up ^ Whitney - Smith, E. ( 2004 ). `` Late Pleistocene extinctions through second - order predation ''. In Barton, C.M. ; Clark, G.A. ; Yesner, D.R. Settlement of the American Continents : A Multidisciplinary Approach to Human Biogeography. Tucson, AZ : University of Arizona Press. ISBN 0 - 8165 - 2323 - 1. Jump up ^ Whitney - Smith, E. ( 2009 ). The Second - Order Predation Hypothesis of Pleistocene Extinctions : A System Dynamics Model. Saarbruken, Germany : VDM Verlag. ISBN 978 - 3 - 639 - 11579 - 6. Jump up ^ Scott, E. ( 2010 ). `` Extinctions, scenarios, and assumptions : Changes in latest Pleistocene large herbivore abundance and distribution in western North America ''. Quat. Int. Jump up ^ Study links mammoth extinction, comets, USA Today, Updated 1 / 2 / 2009. Retrieved 4 April 2009 Jump up ^ The Extinction Debate, by Evan Hadingham, NOVA, Retrieved 4 April 2009. Jump up ^ Last Extinction, NOVA, TV Program Description, Original PBS Broadcast Date : March 31, 2009, Retrieved 4 April 2009. Jump up ^ http://www.pnas.org/content/110/32/12917.full Jump up ^ https://phys.org/news/2017-03-discovery-widespread-platinum-clovis-people.html Jump up ^ Buchanan B, Collard M, Edinborough K ( 19 August 2008 ). `` Paleoindian demography and the extraterrestrial impact hypothesis ''. Proc. Natl. Acad. Sci. U.S.A. 105 ( 33 ) : 11651 -- 4. Bibcode : 2008PNAS... 10511651B. PMC 2575318. PMID 18697936. doi : 10.1073 / pnas. 0803762105. Jump up ^ Haynes, Gary ( 2009 ). American megafaunal extinctions at the end of the Pleistocene. Springer. p. 125. ISBN 978 - 1 - 4020 - 8792 - 9. ^ Jump up to : Haynes, Gary ( 2009 ). `` Introduction to the Volume ''. In Haynes, Gary. American Megafaunal Extinctions at the End of the Pleistocene. Springer. pp. 1 -- 20. ISBN 978 - 1 - 4020 - 8792 - 9. doi : 10.1007 / 978 - 1 - 4020 - 8793 - 6_1. ^ Jump up to : Fiedel, Stuart ( 2009 ). `` Sudden Deaths : The Chronology of Terminal Pleistocene Megafaunal Extinction ''. In Haynes, Gary. American Megafaunal Extinctions at the End of the Pleistocene. Springer. pp. 21 -- 37. ISBN 978 - 1 - 4020 - 8792 - 9. doi : 10.1007 / 978 - 1 - 4020 - 8793 - 6_2. ^ Jump up to : Vergano, Dan ( 2009 - 01 - 02 ). `` Study links mammoth extinction, comets ''. USA Today. Gannett Company. Retrieved 2009 - 05 - 10. Jump up ^ Roach, John ( 2010 - 06 - 22 ). `` Fungi, Feces Show Comet Did n't Kill Ice Age Mammals ? ''. National Geographic Daily News. National Geographic Society. Retrieved 2010 - 06 - 25. Jump up ^ Daulton, T.L. ; Pinter, N. ; Scott, A.C. ( 2010 - 08 - 30 ). `` No evidence of nanodiamonds in Younger -- Dryas sediments to support an impact event ''. Proc. Natl. Acad. Sci. U.S.A. 107 ( 37 ) : 16043 -- 7. Bibcode : 2010PNAS... 10716043D. PMC 2941276. PMID 20805511. doi : 10.1073 / pnas. 1003904107. Jump up ^ Kerr, Richard A. ( 2010 - 10 - 30 ). `` Mammoth - Killer Impact Rejected ''. Science NOW. AAAS. Retrieved 2010 - 08 - 31. Jump up ^ Tian H, Schryvers D, Claeys P ( January 2011 ). `` Nanodiamonds do not provide unique evidence for a Younger Dryas impact ''. Proc. Natl. Acad. Sci. U.S.A. 108 ( 1 ) : 40 -- 4. Bibcode : 2011PNAS... 108... 40T. PMC 3017148. PMID 21173270. doi : 10.1073 / pnas. 1007695108. Jump up ^ Paquay FS, Goderis S, Ravizza G, et al. ( December 2009 ). `` Absence of geochemical evidence for an impact event at the Bølling - Allerød / Younger Dryas transition ''. Proc. Natl. Acad. Sci. U.S.A. 106 ( 51 ) : 21505 -- 10. Bibcode : 2009PNAS... 10621505P. PMC 2799824. PMID 20007789. doi : 10.1073 / pnas. 0908874106. Jump up ^ http://www.pnas.org/content/110/32/12917.full External links Hyperdisease hypothesis `` American Museum of Natural History ''. J.H. Brown ( University of New Mexico ). `` Was a hyperdisease responsible ? '' ( PDF ). Second - order predation Elin Whitney - Smith. `` Quaternary.Net ''. Other links `` Widespread Platinum across continent at Younger Dryas ''. `` Ice Age Bay Area ''. `` The Extinct Late Pleistocene Mammals of North America ''. Peter Tyson. `` End of the Big Beasts ''. S. Kathleen Lyons ; Felisa A. Smith ; James H. Brown ( 2004 ). `` Of mice, mastodons and men : human - mediated extinctions on four continents '' ( PDF ). Evolutionary Ecology Research. 6 : 339 -- 358. `` Return to the Ice Age : The La Brea Exploration Guide ''. Quaternary Pleistocene Holocene Early Middle Late Preboreal Boreal Atlantic Subboreal Subatlantic Preceded by Proterozoic Eon Phanerozoic Eon Paleozoic Era Mesozoic Era Cenozoic Era Cambrian Ordovician Silurian Devonian Carboniferous Permian Triassic Jurassic Cretaceous Paleogene Neogene 4ry Extinction Phenomena Background extinction rate Coextinction De-extinction Ecological extinction Extinct in the wild Functional extinction Genetic pollution Lazarus taxon Local extinction Pseudoextinction Models Extinction vortex Causes Genetic erosion Habitat destruction Human overpopulation Muller 's ratchet Mutational meltdown Overexploitation Theories & concepts Extinction debt Extinction risk from global warming Extinction threshold Field of Bullets Hypothetical species Latent extinction risk Major extinction events Ordovician -- Silurian Late Devonian Permian -- Triassic Triassic -- Jurassic Cretaceous -- Paleogene Holocene Timeline Other extinction events Great Oxygenation End - Ediacaran End - Botomian Dresbachian Cambrian -- Ordovician Ireviken Mulde Lau Carboniferous Olson 's End - Capitanian Carnian Pluvial Toarcian End - Jurassic or Tithonian Aptian Cenomanian - Turonian Eocene -- Oligocene Middle Miocene Pliocene -- Pleistocene Quaternary Extinct species Lists of extinct species Lists of extinct animals List of extinct plants IUCN Red List extinct species Organizations International Union for Conservation of Nature IUCN Species Survival Commission Voluntary Human Extinction Movement See also Decline in amphibian populations Human extinction Category Portal WikiProject Commons Retrieved from `` https://en.wikipedia.org/w/index.php?title=Quaternary_extinction_event&oldid=804841560 '' Categories : Extinction events Pleistocene Climate history Events that forced the climate Hidden categories : Pages with citations lacking titles CS1 maint : Multiple names : authors list CS1 errors : dates CS1 Portuguese - language sources ( pt ) CS1 maint : Uses authors parameter Pages with citations having bare URLs Wikipedia articles needing clarification from September 2017 All articles with unsourced statements Articles with unsourced statements from May 2012 Articles that may contain original research from December 2010 All articles that may contain original research Articles with unsourced statements from December 2010 All articles with specifically marked weasel - worded phrases Articles with specifically marked weasel - worded phrases from April 2011 Articles with unsourced statements from June 2010 Talk Contents About Wikipedia Afrikaans Čeština Deutsch Español فارسی Bahasa Indonesia 日本 語 Suomi Türkçe Українська 中文 Edit links This page was last edited on 11 October 2017, at 13 : 25. 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Question: when did the megafauna of north america go extinct
Answer: The Quaternary period