The Pleistocene or Ice Age extinction eventThe Ice Age extinction event is characterised by the extinction of many large mammals weighing more than 40 kg. In North America around 33 of 45 genera of large mammals became extinct, in South America 46 of 58, in Australia 15 of 16, in Europe 7 of 23, and in Subsaharan Africa only 2 of 44. The South American extinction witnessed the aftermath of the Great American Interchange. Only in South America and Australia did the extinction occur at family taxonomic levels or higher. There are two main hypotheses concerning the Pleistocene extinction:
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 marsupial Australian megafauna. Biologists note that comparable extinctions have not occurred in Africa, 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. The giant sloth survived on Cuba, Haiti, and Puerto Rico long after North American sloths were extinct. The disappearance of the island species coincides with the habitation of these islands by humans. Similarly the disappearance of woolly mammoths on the remote Wrangel Island did not occur until 7,000 years after their mainland extinction. An alternative to the theory of human responsibility is Alexander Tollmann's bolide theory, a more controversial hypothesis which claims that the Holocene was initiated by an extinction event caused by bolide impacts. Major megafaunal extinctionsEurope
The Woolly Mammoth became extinct around 12,000 years ago.
(circa 15,000 years ago) Mediterranean Islands(by 9000 years ago)
A Collared Peccary, surviving relative of the extinct Giant Peccary.
North America
The size of a short faced bear compared with a human.
During the last 50,000 years, including the end of the last glacial period, approximately 33 genera of large mammals have become extinct in North America. Of these, 15 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. Most other extinctions are poorly constrained in time, though some definitely occurred outside of this narrow interval.[1] Contrary to this, 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 imbalance between large mammals and small ones. The megafaunal extinctions include twelve genera of edible herbivores (H), and five large, dangerous carnivores (C). North American extinctions included
The survivors are as significant as the losses: bison, moose (recent immigrants through Beringia), elk, caribou, deer, pronghorn, muskox, bighorn sheep, mountain goat. All save the pronghorns descended from Asian ancestors that had evolved human predators.[2] 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 opposition to the "prehistoric overkill hypothesis" has been that population of humans such as the Clovis culture were too small to be ecologically significant. Other generalized evocations of climate change fail under detailed scrutiny. Lack of tameable megafauna was perhaps one of the reasons why Amerindian civilizations evolved differently than Old World ones.[3] Critics have disputed this by arguing that llama, vicuña, and bison were domesticated[4] South America
An illustration of Megatherium.
At the Pleistocene-Holocene transition South America, which had remained largely unglaciated except for increased mountain glaciation in the Andes, saw an extinction wave, which carried off many large species. Today there is no wild land mammal left on this continent weighing more than a modern tapir.
Australia
The Diprotodon became extinct around 50,000 years ago.
The sudden spate of extinctions occurred earlier than in the Americas. Most evidence points to the period immediately after the first arrival of humans — thought to be a little under 50,000 years ago — but scientific argument continues as to the exact date range. The Australian extinctions included:
Some extinct megafauna, such as the bunyip-like diprotodon, may be the sources of ancient cryptozoological legends. Younger extinctionsNew Zealandc. AD 1500, several species became extinct after Polynesian settlers arrived, including:
Pacific, including HawaiiRecent research, based on archaeological and paleontological digs on 70 different islands, has shown that numerous species went extinct as people moved across the Pacific, starting 30,000 years ago in the Bismarck Archipelago and Solomon Islands (Steadman & Martin 2003). It is currently estimated that among the bird species of the Pacific some 2000 species have gone extinct since the arrivial of humans (Steadman 1995). Among the extinctions were:
MadagascarStarting with the arrival of humans c. 2000 years ago, nearly all of the island's megafauna became extinct, including:
Indian Ocean IslandsStarting c. 500 years ago, a number of species became extinct upon human settlement of the islands, including:
Hunting hypothesisThe Hunting hypothesis suggests that humans hunted megaherbivores to extinction. As a result, carnivores and scavengers that depended upon those animals became extinct from lack of prey.[5][6][7] Therefore this theory holds Pleistocene humans responsible for the megafaunal extinction. One variant, often referred to as overkill, portrays humans as hunting the megafauna to extinction within a relatively short period of time. Some of the direct evidence for this includes: fossils of megafauna found in conjunction with human remains, embedded arrows and tool cut marks found in megafaunal bones, and 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, areas where early humans were non-existent. Based on this evidence, a picture arises of the megafauna of Asia and Africa evolving with 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 dangerous lack of fear of humans. Circumstantially, the close correlation in time between the appearance of humans in an area and extinction there provides weight to this theory. This is perhaps the strongest evidence, as it is almost impossible that it could be coincidental when science has so many data points. For example, the woolly mammoth survived on islands despite worsening 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 30,000 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.[8] World wide extinctions seem to follow the migration of humans and to be most severe where humans arrived most recently and least severe where humans were originally – Africa (see figure at right). This suggests that in Africa, where humans evolved, 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 (see figure at left). 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 [9][10][11] and by computer models by Mosimann and Martin,[12]and Whittington and Dyke,[13] and most recently by Alroy.[14] Eugene S. Hunn, President of the Society of Ethnobiology, offers a dissenting view. He 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.[15]. 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.[16] Conversely, "buffalo jumps"[17] featured indiscriminate killing of a herd. Overkill HypothesisThe overkill hypothesis, a variant of the hunting hypothesis, was proposed 40 years ago by Paul S. Martin, now Professor of Geosciences Emeritus at the Desert Laboratory of the University of Arizona. It sparked debate which continues today. In contrast to other hunting hypothesis it explains the megafaunal extinctions within a relatively short period of time. The most convincing evidence of his theory is that 80% of the North American large mammal species disappeared within 1000 years of the arrival of humans on the Western Hemisphere continents. Shortcomings of the Hunting HypothesisThe major objections to the theory are as follows:
Climate change hypothesesAt 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 Ice Ages in the evolutionary history of many of the megafauna, it is rather implausible that only after the last glacial would there be such extinctions. Some evidence weighs against this theory 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 likely 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.[19][20][21] Increased temperatureThe 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. Shortcomings of the Temperature HypothesisMore recent research has demonstrated 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, so the same large mammals survived similar temperature increases. Therefore warmer temperature alone is not a sufficient explanation.[22][23][24][25][26][27] In addition, numerous species such as mammoths survived in human-free refugia such as Wrangel Island[28] despite changes in climate. This is precisely the opposite of what would be expected if climate change were responsible. 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 spaceOther 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: geographicIt has been shown that vegetation changed from mixed woodland-parkland to separate prairie and woodland.[24][25][27] This may have affected the kinds of food available. If so, herbivores might not have found the plants with which they had evolved and thus would have fallen prey to the anti-herbivory toxins in the plants that remained 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.[29][30][31] 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: timeIncreased continentality resulted in reduced and less predictable rainfall limiting the availability of plants necessary for energy and nutrition.[32][33][34] Axelrod[35] and Slaughter[36] 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.[37] Shortcomings of the continentality hypothesesCritics have identified a number of problems with the continentality hypotheses.
The extinction of the megafauna could have caused the extinction 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, hoever he may be interpeting it backwards. 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 correspoding loss of dung is what led to low nutrient levels in modern day soil and therefore is why the landscape can no longer support a megafauna. Shortcomings of both Climate Change and OverkillNeither the Overkill sensu stricto nor Climate Change hypotheses explain several observations.
Because of the unsatisfactory nature of the Overkill or Climate Change hypotheses alone many scientists support some combination of Climate Change and Overkill. Hyperdisease HypothesisTheoryThe Hyperdisease Hypothesis attributes the extinction of large mammals during the late Pleistocene to indirect effects of the newly arrived aboriginal humans.[48][49][50] The Hyperdisease Hypothesis proposes that humans or animals traveling with them (e.g., 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.[48] 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. MacPhee is searching DNA in mammoth remains from Wrangel Island in Siberia; he hopes to find evidence of infection. 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.citation needed 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. Shortcomings of the Hyperdisease Hypothesis
Second-Order PredationScenarioThe Second-Order Predation Hypothesis says that as humans entered the New World they continued their policy of killing predators, which 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:
SupportThis has been supported by a computer model, the Pleistocene Extinction Model (PEM), which, using the same assumptions and values, compares hypotheses with Second-Order Predation. The findings are that Second Order-Predation is more consistent with extinction than is Overkill[52] (results graph at left). The PEM was run to 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 extinction[53] (results graph at right). Second-Order Predation and other theories
Shortcomings of the Second-Order Predation Hypothesis
References
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