Columbian mammoth

Listen to this article
Source: Wikipedia, the free encyclopedia.

Columbian mammoth
Temporal range: Pleistocene
Composite male skeleton in the Page Museum at the La Brea Tar Pits
Scientific classification Edit this classification
Domain: Eukaryota
Kingdom: Animalia
Phylum: Chordata
Class: Mammalia
Order: Proboscidea
Family: Elephantidae
Genus: Mammuthus
Species:
M. columbi
Binomial name
Mammuthus columbi
(Falconer, 1857)
Approximate North American ranges of the Columbian mammoth (red) and woolly mammoth (blue) during the Late Pleistocene inferred from fossil finds
Synonyms
List
  • Elephas jacksoni Mather, 1838
  • Mammuthus jacksoni Mather, 1838
  • Parelephas jacksoni Mather, 1838
  • Elephas columbi Falconer, 1857
  • Euelephas columbi Falconer, 1857
  • Parelephas columbi Falconer, 1857
  • Mammuthus (Parelephas) columbi Falconer, 1857
  • Elephas primigenius columbii Falconer, 1857
  • Elephas texianus Owen, 1858
  • Elephas imperator Leidy, 1858
  • Mammuthus imperator Leidy, 1858
  • Euelephas imperator Leidy, 1858
  • Archidiskodon imperator Leidy, 1858
  • Mammuthus (Archidiskodon) imperator Leidy, 1858
  • Elephas jeffersonii Osborn, 1922
  • Parelephas jeffersonii Osborn, 1922
  • Mammuthus jeffersonii Osborn, 1922
  • Elephas roosevelti Hay, 1922
  • Parelephas roosevelti Hay, 1922
  • Elephas washingtonii Osborn, 1923
  • Parelephas washingtonii Osborn, 1923
  • Elephas maibeni Barbour, 1925
  • Elephas eellsi Hay, 1926
  • Elephas floridanus Osborn, 1929
  • Parelephas floridanus Osborn, 1929
  • Mammuthus floridanus Osborn, 1929
  • Archidiskodon sonoriensis Osborn, 1929
  • Parelephas progressus Osborn, 1942

The Columbian mammoth (Mammuthus columbi) is an

extant relative of the Columbian and other mammoths is the Asian elephant
.

Reaching 3.72–4.2 m (12.2–13.8 ft) at the shoulders and 9.2–12.5 metric tons (10.1–13.8 short tons) in weight, the Columbian mammoth was one of the largest species of mammoth. It had long, curved tusks and four

sedges, grasses, and other plants. It did not live in the Arctic regions of Canada, which were instead inhabited by woolly mammoths. The ranges of the two species may have overlapped, and genetic evidence suggests that they interbred. Several sites contain the skeletons of multiple Columbian mammoths, either because they died in incidents such as a drought
, or because these locations were natural traps in which individuals accumulated over time.

For a few thousand years prior to their extinction, Columbian mammoths coexisted in North America with

climate change
, hunting by humans, or a combination of both.

Taxonomy

Large mammoth tooth
1863 lithograph of the partial holotype molar from Georgia

The Columbian mammoth was first

British Museum of Natural History) was reported in 2012, and could help shed more light on that specimen, since doubts about its adequacy as a holotype have been raised.[2]

In the early 20th century, the taxonomy of extinct elephants became increasingly complicated. In 1942, paleontologist

endemic to the Americas (as other species lived both there and in Eurasia). The idea that species such as M. imperator (the imperial mammoth) and M. jeffersoni (Jefferson's mammoth) were either more primitive or advanced stages in Columbian mammoth evolution was largely dismissed, and they were regarded as synonyms. In spite of these conclusions, Agenbroad cautioned that American mammoth taxonomy is not yet fully resolved.[5]

Evolution

Henry F. Osborn's 1942 diagram of evolutionarily "progressive" mammoth skulls of species he grouped in the genus Parelephas; the North American species are now considered junior synonyms
of M. columbi

The earliest known members of Proboscidea, the

manatees) and the hyraxes (an order of small, herbivorous mammals). The family Elephantidae existed six million years ago in Africa, and includes the living elephants and the mammoths. Among many now extinct clades, the mastodon (Mammut) is only a distant relative, and part of the distinct family Mammutidae, which diverged 25 million years before the mammoths evolved.[6] The Asian elephant (Elephas maximus) is the closest extant relative of the mammoths.[7] The following cladogram shows the placement of the Columbian mammoth among other elephantids, based on a 2018 genetic study:[8]

Mammut americanum
(American mastodon)

Elephantidae

Mammuthus columbi (Columbian mammoth)

Mammuthus primigenius
(woolly mammoth)

Elephas maximus
(Asian elephant)

Palaeoloxodon antiquus
(straight-tusked elephant)

Loxodonta cyclotis
(African forest elephant)

Loxodonta africana
(African bush elephant)

Channel Islands

Since many remains of each species of mammoth are known from several localities, reconstructing the evolutionary history of the genus is possible through

lamellar plates) on their molars; primitive species had few ridges, and the number increased gradually as new species evolved to feed on more abrasive food items. The crowns of the teeth became taller in height and the skulls became taller to accommodate this. At the same time, the skulls became shorter from front to back to reduce the weight of the head.[9][10] The short, tall skulls of woolly and Columbian mammoths are the culmination of this process.[6]

The first known members of the genus Mammuthus are the African species M. subplanifrons from the Pliocene, and M. africanavus from the Pleistocene. The former is thought to be the ancestor of later forms. Mammoths entered Europe around 3 million years ago. The earliest European mammoth has been named M. rumanus; it spread across Europe and China. Only its molars are known, which show that it had 8–10 enamel ridges. A population evolved 12–14 ridges, splitting off from and replacing the earlier type, becoming M. meridionalis about 2.0–1.7 million years ago. In turn, this species was replaced by the steppe mammoth (M. trogontherii) with 18–20 ridges, which evolved in eastern Asia around 2.0–1.5 million years ago.[9] The Columbian mammoth evolved from a population of M. trogontherii that had crossed the Bering Strait and entered North America about 1.5-1.3 million years ago; it retained a similar number of molar ridges. Mammoths derived from M. trogontherii evolved molars with 26 ridges 400,000 years ago in Siberia and became the woolly mammoth (M. primigenius). Woolly mammoths entered North America about 100,000 years ago.[6]

A population of Columbian mammoths that lived between 80,000 and 13,000 years ago on the

decreased in size due to the limited food provided by the islands' small areas. Bones of larger specimens have also been found on the islands, but whether these were stages in the dwarfing process, or later arrivals of Columbian mammoths is unknown.[7][12][13]

Hybridization

A 2011

mitochondrial genome (inherited through the female line) showed that two examined Columbian mammoths, including the morphologically typical "Huntington mammoth", were grouped within a subclade of woolly mammoths. This suggests that the two populations interbred and produced fertile offspring. One possible explanation is introgression of a haplogroup from woolly to Columbian mammoths, or vice versa. A similar situation has been documented in modern species of African elephant (Loxodonta), the African bush elephant (L. africana) and the African forest elephant (L. cyclotis). The authors of the study also suggest that the North American type formerly referred to as M. jeffersonii may have been a hybrid between the two species, as it is apparently morphologically intermediate.[14] These findings were unexpected, and other researchers requested further study to clarify the situation.[15]

A 2015 study of mammoth molars confirmed that M. columbi evolved from Eurasian M. trogontherii, not M. meridionalis as had been suggested earlier, and noted that M. columbi and M. trogontherii were so similar in morphology that their classification as separate species may be questionable. The study also suggested that the animals in the range where M. columbi and M. primigenius overlapped formed a metapopulation of hybrids with varying morphology.[16] In 2016, a genetic study of North American mammoth specimens confirmed that the mitochondrial diversity of M. columbi was nested within that of M. primigenius and suggested that both species interbred extensively, were both descended from M. trogontherii, and concluded that morphological differences between fossils may, therefore, not be reliable for determining taxonomy. The authors also questioned whether M. columbi and M. primigenius should be considered "good species", considering that they were able to interbreed after supposedly being separated for a million years, but cautioned that more specimens need to be sampled.[17]

In 2021, DNA older than a million years was sequenced for the first time, from two steppe mammoth-like teeth of

Middle Pleistocene, resulting in the Columbian mammoths of the Late Pleistocene having around 40-50% ancestry from the Krestovka lineage, and 50-60% related to woolly mammoths. Later woolly and Columbian mammoths also interbred occasionally, and mammoth species perhaps hybridized routinely when brought together by glacial expansion. The study also found that genetic adaptations to cold environments, such as hair growth and fat deposits, were already present in the steppe mammoth lineage, and was not unique to woolly mammoths.[18][19]

Description

Colored silhouette of a mammoth, relative in size to a human and past and present elephants
Size (blue) compared to a human and other mammoths
Side-on view of a skeleton of a 3.7 metre tall adult male Columbian mammoth

Larramendi 2016 estimated the average male Columbian mammoth to have had a shoulder height of 3.75 m (12.3 ft) and a weight of 9.5 tonnes (10.5 short tons), though large males may have reached 4.2 m (13.8 ft) in shoulder height and 12.5 tonnes (13.8 short tons) in weight.

spinous processes (protrusions) of the back vertebrae decreasing in length from front to rear. Juveniles, though, had convex backs like Asian elephants.[21][20] Other skeletal features include a short, deep rostrum (front part of the jaws), a rounded mandibular symphysis (where the two halves of the lower jaw connected) and the coronoid process of the mandible (upper protrusion of the jaw bone) extending above the molar surfaces.[22]

Nebraska State Museum of Natural History
, with life restoration (right) based on same; the extent of the fur is hypothetical

Apart from its larger size and more primitive molars, the Columbian mammoth also differed from the woolly mammoth by its more downturned mandibular symphysis; the

dental alveoli (tooth sockets) of the tusks were directed more laterally away from the midline.[14] Its tail was intermediate in length between that of modern elephants and the woolly mammoth. Since no Columbian mammoth soft tissue has been found, much less is known about its appearance than that of the woolly mammoth. It lived in warmer habitats than the woolly mammoth, and probably lacked many of the adaptations seen in that species. Hair thought to be that of the Columbian mammoth has been discovered in Bechan Cave in Utah, where mammoth dung has also been found. Some of this hair is coarse, and identical to that known to belong to woolly mammoths; however, since this location is so far south, it is unlikely to be woolly mammoth hair. The distribution and density of fur on the living animal is unknown, but it was probably less dense than that of the woolly mammoth due to the warmer habitat.[6][21] An additional tuft of Columbian mammoth hair is known from near Castroville in California, the hair was noted to be red-orange and was described as being similar in colour to a Golden Retriever.[23]

Dentition

Columbian mammoths had very long tusks (modified incisor teeth), which were more curved than those of modern elephants. Their tusks are among the largest recorded in proboscideans, with some reaching over 4 metres (13 ft) in length and 200 kilograms (440 lb) in weight, with some historical reports of tusks up to 4.88–5.1 metres (16.0–16.7 ft) long and masses of around 230–250 kilograms (510–550 lb).[24] Columbian mammoth tusks were usually not much larger than those of woolly mammoths, which reached 4.2 m (14 ft). The tusks of females were much smaller and thinner. About a quarter of the tusks' length was inside the sockets; they grew spirally in opposite directions from the base, curving until the tips pointed towards each other, and sometimes crossed. Most of their weight would have been close to the skull, with less torque than straight tusks would have generated. The tusks were usually asymmetrical, with considerable variation; some tusks curved down, instead of outwards, or were shorter due to breakage. Columbian mammoth tusks were generally less twisted than those of woolly mammoths. At six months of age, calves developed milk tusks a few cms long, which were replaced by permanent tusks a year later. Annual tusk growth of 2.5–15 cm (0.98–5.91 in) continued throughout life, slowing as the animal reached adulthood.[21]

Columbian mammoths had four functional molar teeth at a time, two in the upper jaw and two in the lower. A mammoth's molars were replaced five times over the animal's lifetime, with a total of six succeeding molars on each half of the jaws. About 23 cm (9.1 in) of the crown was within the jaw, and 2.5 cm (1 in) was above. The teeth had separated ridges (lamellae) of enamel, which were covered in "prisms" directed towards the chewing surface. Wear-resistant, they were held together with cementum and dentin. The crowns of the lower jaw were pushed forward and up as they wore down, comparable to a conveyor belt. The first molars were about the size of those of a human, 1.3 cm (0.51 in); the third ones were 15 cm (5.9 in) long, and the sixth ones were about 30 cm (1 ft) long and weighed 1.8 kg (4 lb). With each replacement, the molars grew larger and gained more ridges; the number of plates varied between individuals.[21][25][26] There was typically 18-21 ridges on each third molar, similar to those of M. trogontherii, but less than the 24-28 typical of woolly mammoths.[16] Growing 18 cm (7.1 in) of ridge took about 10.6 years.[27]

Paleobiology

mastodons

Like that of modern elephants, the mammoth's sensitive, muscular trunk was a limb-like organ with many functions. It was used for manipulating objects and social interaction. Although healthy adult mammoths could defend themselves from predators with their tusks, trunks, and size, juveniles and weakened adults were vulnerable to pack hunters such as wolves and big cats. Bones of juvenile Columbian mammoths, accumulated by Homotherium (the scimitar-toothed cat), have been found in Friesenhahn Cave in Texas. Tusks may have been used in intraspecies fighting for territory or mates and for display, to attract females and intimidate rivals. Two Columbian mammoths that died in Nebraska with tusks interlocked provide evidence of fighting behavior. The mammoths could use their tusks as weapons by thrusting, swiping, or crashing them down, and used them in pushing contests by interlocking them, which sometimes resulted in breakage. The tusks' curvature made them unsuitable for stabbing.[28][29]

Although to what extent Columbian mammoths migrated is unclear, an isotope analysis of Blackwater Draw in New Mexico indicated that they spent part of the year in the Rocky Mountains, 200 km (120 mi) away. The study of tusk rings may aid further study of mammoth migration. On Goat Rock Beach in Sonoma Coast State Park, blueschist and chert outcrops (nicknamed "Mammoth Rocks") show evidence of having been rubbed by Columbian mammoths or mastodons. The rocks have polished areas 3–4 m (9.8–13.1 ft) above the ground, primarily near their edges, and are similar to African rubbing rocks used by elephants and other herbivores to rid themselves of mud and parasites. Similar rocks exist in Hueco Tanks, Texas, and on Cornudas Mountain in New Mexico.[28][30]

Social behavior

Remains of a mammoth buried
Female "mammoth W" (left) and male "Q", with juveniles "R" and "T" (right), at the Waco Mammoth National Monument

Like modern elephants, Columbian mammoths were probably social and lived in

trackway similar to that left by modern elephants leads to one of the skeletons. The mammoth may have made the trackway before it died, or another individual may have approached the dead or dying animal—similar to the way modern elephants guard dead relatives for several days.[21][31][32]

Mammoth jaw with other bones on the ground
Skulls (left) and mandible (right) in a lahar deposit at the Paleontological Museum in Tocuila

Accumulations of modern elephant remains have been called "

Texcoco, Mexico, where a volcanic lahar mudflow covered at least seven individuals 12,500 years ago. How many mammoths lived at one location at a time is unknown, but the number likely varied by season and lifecycle. Modern elephants can form large herds, sometimes consisting of multiple family groups, and these herds can include thousands of animals migrating together. Mammoths may have formed large herds more often than modern elephants, since animals living in open areas are more likely to do this than those in forested areas. [21][31][33]

Natural traps

Hot Springs Mammoth Site

Many specimens also accumulated in natural traps, such as sinkholes and tar pits. The Mammoth Site in Hot Springs, South Dakota, is a 26,000-year-old, roughly 40 m (130 ft)-long sinkhole that functioned for 300 to 700 years before filling with sediment. The site is the opposite scenario of that in Waco; all but one of the at least 55 skeletons—additional skeletons are excavated each year—are male, and accumulated over time rather than in a single event. Like modern male elephants, male mammoths primarily are assumed to have lived alone, to be more adventurous (especially young males), and to be more likely to encounter dangerous situations than the females. The mammoths may have been lured to the hole by warm water or vegetation near the edges, slipping in and drowning or starving. Isotope studies of growth rings have shown that most of the mammoths died during spring and summer, which may have correlated with vegetation near the sinkhole. One individual, nicknamed "Murray", lies on its side, and probably died in this pose while struggling to get free. Deep footprints of mammoths attempting to free themselves from the sinkhole's mud can be seen in vertically excavated sections of the site.[21][31]

dire wolves fighting over a Columbian mammoth carcass in the La Brea Tar Pits, by Robert Bruce Horsfall
, 1911

Since the early 20th century, excavations at the

felids. Fossils of different animals are found stuck together when they are excavated from the pits.[31] The tar pits do not preserve soft tissue, and a 2014 study concluded that asphalt may degrade the DNA of animals mired in it after an attempt was made to extract DNA from a Columbian mammoth.[34]

A site in an airport construction area in Mexico nicknamed "mammoth central" is believed to have been the boggy shores of an ancient lake bed where animals were trapped 10,0000 to 20,000 years ago. Human tools have been found at the site. It remains unclear whether the 200 Columbian mammoths found there died of natural causes and were then carved by humans. Some have hypothesized that humans drove the Columbian mammoths into the area to kill them. The site is only 12 miles (19 km) from artificial pits which were once used by humans to trap and kill large mammals.[35][36]

Diet

University of Wyoming Geological Museum
(right)

An adult Columbian mammoth would have needed more than 180 kg (400 lb) of food per day, and may have foraged for 20 hours a day. Mammoths chewed their food using their powerful jaw muscles to move the mandible forward and close the mouth, then backward while opening; the sharp enamel ridges thereby cut across each other, grinding the food. The ridges were wear-resistant, enabling the animal to chew large quantities of food that contained grit. The trunk could be used for pulling up large tufts of grass, picking buds and flowers, or tearing leaves and branches from trees and shrubs, and the tusks were used to dig up plants and strip bark from trees. Digging is indicated on preserved tusks by flat, polished sections of the surface that would have reached the ground.[21] Isotope studies of Columbian mammoths from Mexico and the United States have shown that their diet varied by location, consisting of a mix of C3 (most plants) and C4 plants (such as grasses), and they were not restricted to grazing or browsing.[37][38][39] Even individual Columbian mammoths from the same geographic location show major differences in dental mesowear, indicating extensive variation in dietary habits between different individuals within the same population.[40]

Stomach contents from Columbian mammoths are rare, since no carcasses have been found, but plant remains were discovered between the pelvis and ribs of the "Huntington mammoth" when it was excavated in Utah. Microscopy showed that these chewed remains consisted of sedges, grasses, fir twigs and needles, oak, and maple.[41] A large amount of mammoth dung has been found in two caves in Utah. The dry conditions and stable temperature of Bechan Cave (bechan is Navajo for "large faeces") has preserved 16,000- to 13,500-year-old elephant dung, most likely from Columbian mammoths.[42] The dung consists of 95% grasses and sedges, and varies from 0 to 25% woody plants between dung boluses, including saltbush, sagebrush, water birch, and blue spruce. This is similar to the diet documented for the woolly mammoth, although browsing seems to have been more important for the Columbian mammoth. The cover of dung is 41 cm (16 in) thick, and has a volume of 227 m³ (8,000 cubic ft), with the largest boluses 20 cm (7.9 in) in diameter. The Bechan dung could have been produced by a small group of mammoths over a relatively short time, since adult African elephants drop an average of 11 kg (24 lb) of dung every two hours and 90–135 kg (198–298 lb) each day.[21][43]

Giant North American fruits of plants such as the Osage-orange, Kentucky coffeetree, pawpaw and honey locust have been proposed to have evolved in tandem with now-extinct American megafauna such as mammoths and other proboscideans, since no extant endemic herbivores are able to ingest these fruits and disperse their seeds. Introduced cattle and horses have since taken over this ecological role.[44][45][46]

Life history

Young mammoth skeleton, with a large skull relative to its body
Mammoth skeleton with long, curved tusks, in front of a painted prehistoric backdrop
Skeleton of a juvenile (left) and cast of the male "Huntington mammoth" (right), which was old and sick when it died, both at the Natural History Museum of Utah

The lifespan of the Columbian mammoth is thought to have been about 80 years. The lifespan of a mammal is related to its size; Columbian mammoths are larger than modern elephants, which have a lifespan of about 60 years. The age of a mammoth can be roughly determined by counting the growth rings of its tusks when viewed in cross section. However, ring-counting does not account for a mammoth's early years; early growth is represented in tusk tips, which are usually worn away. In the remainder of the tusk, each major line represents a year, with weekly and daily lines found in between. Dark bands correspond to summer, making determining the season in which a mammoth died possible. Tusk growth slowed when foraging became more difficult, such as during illness or when a male mammoth was banished from the herd (male elephants live with their herds until about the age of 10).[21]

Mammoths continued growing during adulthood, as do other elephants. Males grew until age 40, and females until age 25. Mammoths may have had gestation periods of 21–22 months, like those of modern elephants. Columbian mammoths had six sets of molars in the course of a lifetime. At 6–12 months, the second set of molars would erupt, with the first set worn out at 18 months of age. The third set of molars lasted for 10 years, and this process was repeated until the sixth set emerged at 30 years of age. When the last set of molars wore out, the animal would be unable to chew, and would die of starvation.[21]

Almost all vertebrae of the "Huntington mammoth", a very aged specimen, were deformed by arthritic disease, and four of its lumbar vertebrae were fused; some bones also indicate bacterial infection, such as osteomyelitis.[21] The condition of the bones suggests the specimen died of old age and malnutrition.[41]

Distribution and habitat

Painting of animals around a lake
Environment of what is now White Sands National Park, with Columbian mammoth herd in the background

Columbian mammoths inhabited the much of North America, ranging from southern Canada[47] to Central America (where it was largely confined to the vicinity of the Pacific coast), with its southernmost record being in northern Costa Rica.[48] The environment in these areas may have had more varied habitats than those inhabited by woolly mammoths in the north (the mammoth steppe). Some areas were covered by grasses, herbaceous plants, trees, and shrubs; their composition varied from region to region, and included grassland, savanna, and aspen parkland habitats. Wooded areas also occurred; although mammoths would not have preferred forests, clearings in them could provide the animals with grasses and herbs.[21]

The Columbian mammoth shared its habitat with other now-extinct Pleistocene mammals such as

competitive exclusion as a result of the greater grazing efficiency of Columbian mammoths,[49] with competition with mammoths also suggested to be the reason for the contraction of the northern part of the range of the generalist gomphothere Cuvieronius.[50]

Relationship with humans

Drawing of humans hunting an elephant-like mammoth, who is lifting a human with its trunk
Fanciful restoration of a Columbian mammoth hunt, J. Steeple Davis, 1885

Towards the end of the Late Pleistocene, around or after 16,000 years ago,

cleaver choppers made from a mammoth shoulder blade; the choppers had been used to butcher the mammoths. At the same site, a flake knife made from a long mammoth bone was also found wedged against mammoth vertebrae. At Murray Springs, archeologists discovered a 13,100-year-old object made from a mammoth femur; the object is thought to be a shaft wrench, a tool for straightening wood and bone to make spear-shafts (the Inuit use similar tools).[52][53]

Although some sites potentially documenting human interactions with Columbian mammoths have been reported from as early 20,000 years ago, these have been criticised, as they lack stone tools, and the supposed human-made marks on the bones are potentially the result of natural processes.

Naco-Mammoth Kill Site in Arizona, found with eight Clovis points near its skull, shoulder blade, ribs, and other bones, is considered the most convincing evidence for hunting. In modern experiments, replica spears have been able to penetrate the rib cages of African elephants with reuse causing little damage to the points.[55][56]

Other sites show more circumstantial evidence of mammoth hunting, such as piled bones bearing butcher marks. Some of these sites are not closely associated with Clovis points. The Dent site (the first evidence of mammoth hunting in North America, discovered in 1932) and the Lehner Mammoth-Kill Site, where multiple juvenile and adult mammoths have been found with butcher marks and in association with Clovis points, were once interpreted as the killing of entire herds by Clovis hunters. However, isotope studies have shown that the accumulations represent individual deaths at different seasons of the year, so are not herds killed in single incidents. Many other such assemblages of bones with butcher marks may also represent accumulations over time, so are ambiguous as evidence for large-scale hunting.[55][57]

A 2021 article by the American paleontologist Metin I. Eren and colleagues suggested mammoths were not very susceptible to Clovis point weapons due to their thick skin, hair, muscles, ribs, and fat, which would have impeded most types of attacks humans could pull off at that time. Experiments wherein most spear points used to calculate their effectiveness against simulated mammoth skin shattered on impact rather than penetrating, suggested to these researchers that ancient humans probably preferred to scavenge mammoth carcasses for their meat and other resources and threw spears to drive other scavengers away from carcasses before butchering the corpse with their stone tools. While the study does not rule out the hunting of mammoths by early humans, it instead indicates that such an event was probably rare and potentially more dangerous and less rewarding than scavenging. In response, other scientists found no reason to abandon the traditional idea that Clovis points were used to hunt big-game, one suggesting that such spears could have been thrown or thrust at areas of the torso that were not protected by ribs, with the wounds not killing the mammoths instantly, but the hunters could follow their prey until it had bled to death.[58][59]

petroglyphs from Utah supposedly depicting mammoths and a bison
(right), though it may have been made after mammoths went extinct

San Juan River in Utah have been suggested to be 11,000–13,000-years old and to include depictions of two Columbian mammoths; the mammoths' domed heads distinguish them from mastodons. They are also shown with two "fingers" on their trunks, a feature known from European depictions of mammoths. The tusks are short, which may indicate they are meant to be females. A carving of a bison (possibly the extinct Bison antiquus) is superimposed on one of the mammoth carvings and may be a later addition.[62] Geological dating of the San Juan River depictions in 2013 have shown them to be less than 4000 years old, after mammoths and mastodons went extinct, and they may instead be an arrangement of unrelated elements.[61][63] Other possible depictions of Columbian mammoths have been shown to be either misinterpretations or fraudulent.[62]

The Columbian mammoth is the state fossil of Washington[64] and South Carolina.[65] Nebraska's state fossil is "Archie", a Columbian mammoth specimen found in the state in 1922. "Archie" is currently on display at Elephant Hall in Lincoln, Nebraska, and is the largest mounted mammoth specimen in the United States.[66]

Extinction

Clovis points at the Dent site, the first evidence of mammoth hunting in America, Carnegie Museum of Natural History (left), and 13,500–13,000 year old Clovis points at Cleveland Museum of Natural History
(right)

Columbian and woolly mammoths both disappeared from mainland North America by the latest Pleistocene, with no recorded Holocene survival, alongside most other latest Pleistocene megafauna of North America. The latest calibrated radiocarbon date of the Columbian mammoth is in the locality of the Dent site in Colorado which dates to 12,124–12,705 years Before Present, during the onset of the Younger Dryas cold phase (12,900-11,700 years BP) and Clovis culture (13,200-12,800 years BP). Its younger calibrated date compared to most other extinct latest Pleistocene species suggests that it was one of the last North American megafauna to have gone extinct.[67] Amongst the most recent Columbian mammoth remains have been dated around 10,900 years ago, although the date is uncalibrated and therefore is actually older in age.[68][69][70] This extinction formed part of the Late Pleistocene extinctions of North America, which coincided with both Clovis culture and the Younger Dryas.[55] Scientists do not know whether these extinctions happened abruptly or were drawn out.[68][71] During this period, 40 mammal species disappeared from North America, almost all of which weighed over 40 kg (88 lb); the extinction of the mammoths cannot be explained in isolation.[55]

Scientists are divided over whether climate change, hunting, or a combination of the two, drove the extinction of the Columbian mammoths. According to the climate-change hypothesis, warmer weather led to the shrinking of suitable habitat for Columbian mammoths, which turned from parkland to forest, grassland, and semidesert, with less diverse vegetation. The "overkill hypothesis" attributes the extinction to hunting by humans, an idea first proposed by geoscientist Paul S. Martin in 1967; more recent research on this subject has varied in conclusions.[55][72]

A 2002 study concluded that the archeological record did not support the "overkill hypothesis", given that only 14 Clovis sites (12 with mammoth remains and two with mastodon remains) out of 76 examined provided strong evidence of hunting.[73] In contrast, a 2007 study found that the Clovis record indicated the highest frequency of prehistoric exploitation of proboscideans for subsistence in the world, and supported the "overkill hypothesis".[74] A 2019 study that used mathematical modelling to simulate correlations between migrations of humans and Columbian mammoths also supported the "overkill hypothesis".[75] Whatever the actual cause of extinction, large mammals are generally more susceptible to hunting pressure than smaller ones due to their smaller population size and low reproduction rates.[55] On the other hand, large mammals are generally less vulnerable to climatic stresses since they have greater fat deposits at their disposal[76] and can migrate long distances to escape food shortages.[77]

References

  1. ^ Falconer, H.; Murchison, C. (1868). Palaeontological memoirs and notes of H. Falconer, with a biographical sketch of the author. Vol. 2. London: Robert Hardwicke. pp. 212–239.
  2. S2CID 83716210
    .
  3. ^ Osborn, H. F. (1942). Percy, M. R. (ed.). Proboscidea: A monograph of the discovery, evolution, migration and extinction of the mastodonts and elephants of the world. Vol. 2. New York: J. Pierpont Morgan Fund. pp. 935–1115.
  4. JSTOR 1379357
    .
  5. .
  6. ^ a b c d e Lister & Bahn 2007, pp. 12–43.
  7. ^ .
  8. .
  9. ^ .
  10. ^ Ferretti, M. P. (2003). "Structure and evolution of mammoth molar enamel". Acta Palaeontologica Polonica. 3. 48: 383–396.
  11. ^ Rocha, Veronica (September 16, 2016). "Well-preserved mammoth skull unearthed on Channel Islands puzzles scientists". Los Angeles Times. Retrieved September 24, 2016.
  12. S2CID 128894735
    .
  13. .
  14. ^ .
  15. .
  16. ^ .
  17. .
  18. .
  19. . Retrieved February 17, 2021.
  20. ^ .
  21. ^ a b c d e f g h i j k l m n Lister & Bahn 2007, pp. 77–95.
  22. .
  23. ^ Pastino, Blake de (September 3, 2014). "First Columbian mammoth with hair discovered on California farm". Western Digs. Archived from the original on November 28, 2022. Retrieved March 28, 2020.
  24. ISSN 0891-2963
    .
  25. .
  26. .
  27. .
  28. ^ a b Lister & Bahn 2007, pp. 96–111.
  29. .
  30. .
  31. ^ a b c d Lister & Bahn 2007, pp. 45–75.
  32. S2CID 132347949
    .
  33. .
  34. .
  35. ^ Carrillo, Geraldo (September 3, 2020). "'Mammoth central' found at Mexico airport construction site". Associated Press. Retrieved September 6, 2020.
  36. ^ "Mexico City's new airport site becomes 'mammoth central'". Mexico News Daily. September 4, 2020. Retrieved September 6, 2020.
  37. .
  38. .
  39. . Retrieved March 31, 2024 – via Elsevier Science Direct.
  40. . Retrieved March 31, 2024 – via Elsevier Science Direct.
  41. ^ .
  42. . Retrieved February 1, 2016.
  43. .
  44. .
  45. .
  46. ^ Connie Barlow (2001). "Anachronistic Fruits and the Ghosts Who Haunt Them" (PDF). Harvard University Arboretum. Archived (PDF) from the original on February 12, 2013. Retrieved December 5, 2012.
  47. .
  48. .
  49. ^ Spencer LG 2022. The last North American gomphotheres. N Mex Mus Nat Hist Sci. 88:45–58.
  50. ISSN 0094-8373
    .
  51. .
  52. ^ a b Lister & Bahn 2007, pp. 113–139.
  53. JSTOR 4064981
    .
  54. .
  55. ^ a b c d e f Lister & Bahn 2007, pp. 141–163.
  56. S2CID 163601718
    .
  57. .
  58. .
  59. ^ Bower, B. (January 11, 2022). "Clovis hunters' reputation as mammoth killers takes a hit".
  60. .
  61. ^ .
  62. ^ a b Malotki, E.; Wallace, H. D. (2011). "Columbian mammoth petroglyphs from the San Juan River near Bluff, Utah, United States". Rock Art Research: The Journal of the Australian Rock Art Research Association. 2. 28: 143–152.
  63. ^ McBride, Diane (2013). "Archaeology group to discuss mammoth petroglyphs". The Journal. Retrieved October 20, 2022.
  64. ^ "Washington State Fossil". State Symbols USA. April 28, 2014. Retrieved August 11, 2017.
  65. ^ "South Carolina State Fossil". State Symbols USA. October 24, 2014. Retrieved August 11, 2017.
  66. ^ "Nebraska State Fossil". State Symbols USA. October 5, 2014. Retrieved August 11, 2017.
  67. .
  68. ^ .
  69. .
  70. .
  71. .
  72. .
  73. .
  74. .
  75. .
  76. .
  77. .

Bibliography

External links