Temporal range: Late Pleistocene to Early Holocene, 0.06–0.011 Ma
(Stock & Furlong, 1928)
The pygmy mammoth or Channel Islands mammoth (Mammuthus exilis) is an extinct species of dwarf elephant descended from the Columbian mammoth (M. columbi) of mainland North America. This species went extinct during the Quaternary extinction event in which many megafauna species went extinct due to changing conditions to which the species could not adapt. A case of island or insular dwarfism, from a recent analysis in 2010 it was determined that M. exilis was on average, 1.72 m (5.6 ft) tall at the shoulders and 760 kg (1,680 lb) in weight, in stark contrast to its 4.3 m (14 ft) tall, 9,100 kg (20,100 lb) ancestor. Another estimate gives a shoulder height of 2.02 m (6.6 ft) and a weight of 1,350 kg (2,980 lb).
Mammoth remains have been known on the northern Channel Islands of California since 1856. They were first reported in scientific literature in 1873.
In 1994 the National Park Service called in scientists to inspect an uncovered, unidentified skeleton found on the northeast coast of Santa Rosa Island. They found bones of the axial skeleton of a large land vertebrate on the Santa Rosa Island. They decided there was enough evidence to start to excavate and dig up the skeleton. They recovered 90% of a mature male pygmy mammoth's skeleton. The mammoth was about 50 years old when it died. The small bones were preserved in life position, which represented that it had died where it was found rather than being scattered around the island. The bones were returned to the Santa Barbara Museum of Natural History. After the discovery of the skeleton, a pedestrian survey of the island was started, which resulted in the discovery of 160 new locations of mammoth remains, the vast majority being found on Santa Rosa Island. This was the first discovery of a nearly complete specimen of the pygmy mammoth. Fortunately enough, the skeleton of the mammoth was only missing a foot, a tusk, and a couple of vertebrae. The remains were covered by a sand dune, which prevented the bones from scattering and kept them intact.
Remains of M. exilis have been discovered on three of the northern Channel Islands of California since 1856: Santa Cruz, Santa Rosa, and San Miguel, which together with Anacapa were the highest portions of the now mostly submerged superisland of Santa Rosae. The late Pleistocene elephant appears to have survived on the islands until the arrival of the humans associated with Arlington Springs Man around 13,000 years ago and the last known mammoth occurrence was 13–12.9 thousand years ago which predates the later Chumash people's arrival during the early Holocene, between 10,800 and 11,300 years ago. Radiocarbon dating indicates M. exilis existed on the island for at least 47,000 years prior (which is the approximate limit of the dating method).
Modern elephants are excellent swimmers, and the ancestors of M. exilis most likely swam the 4 mi (6.4 km) to Santa Rosae. As the population of mammoths increased, the lack of large predators such as the dire wolf, Smilodon and the American lion and the loss of habitat caused by the rise of sea levels at the end of the ice age as Santa Rosae split into four islands favored smaller animals. Because of this, the pygmy mammoths began evolving through generations as a survival mechanism to stay alive on the ever-shrinking Santa Rose Island, their body size became smaller in order to require less food and resources to keep them energized and alive. After this evolution is when the species became its own distinct species, the pygmy mammoth.
M. exilis should not be confused with the mammoths of Wrangel Island or Saint Paul Island, which were small races of the woolly mammoth (M. primigenius) and which died out around 1700 B.C. and 4000 B.C., respectively.
The pygmy mammoth was able to thrive in all of the many different ecosystems found on Santa Rosae, such as high elevation plateaus to dune, grassland, riparian and steppe-tundra ecosystems. Their fossils are found in the Channel Islands and in the California Channel. The evidence of their habituation in all of those diverse dwellings is revealed by the pollen and plant pieces found in sediments and in dung. In addition, each habitat has a specific isotope mark from the unique types of soil, plants and water. These mammoths sometimes modified their habitats, specifically in Channel Islands, where they created more spacious grassland in result of their roaming.
Land bridges were once theorized to have connected the northern Channel Islands to the mainland, because it was assumed the mammoths could not swim. "A land bridge between the mainland and Santa Rosae did not exist during the Quaternary"; however, the distance to the mainland was reduced to 7 km. When the Ice Age caused the sea levels to lower, the four northern Channel Islands formed a single island that was closer to the mainland and also larger in size. Pygmy mammoths are descendants of the Columbian mammoth. These were capable swimmers able to swim to the new island and adapt to the new environment.
The pygmy mammoths lived on Santa Rosae island which was beginning to shrink due to rising sea levels. The pygmy mammoths evolved through generations in order to survive on the ever-shrinking Santa Rosae Island. Smaller bodies require less food and resources to remain healthy in a smaller territory and allowed for less competition among the species, which is an example of island dwarfism. Also, their mainland predators such as the dire wolves, the Smilodon and the American lion were not present. After this evolution is when the species became its own distinct species, the pygmy mammoth. Despite popular belief, the evolution and dwarfing of the Pygmy mammoth took a long period of time. The process took over 30,000 years but as the mammoths adapted to the new land and restricted food supply they slowly became only half as tall as their Columbian mammoth predecessors.
Like most elephant species, the males have a somewhat larger skeletal structure, especially in the legs, skull and tusks. The female pygmy elephant has a different pelvic structure, allowing her to give birth.
The cause of extinction of the pygmy mammoth is unknown, but it could have been caused by over-hunting by humans, wildfire, climate change, or some combination thereof.
While human interference often has a greater effect on island species than on continental species, there is no evidence that humans on Santa Rosa hunted the pygmy mammoth. "Mammoths were still extant on the islands when humans arrived" and mammoth remains were associated with charcoal of the same radiocarbon date. Two mammoth skulls with the brain removed were found adjacent to a fire pit, of the 100 fire pits at least a third contained mammoth bones. "More complex ecological explanations involving a combination of climate change and human predation are the most viable." 
"Abrupt ecosystem disruption is evident on the Northern Channel Islands" with the onset of biomass burning and resulting mass sediment wasting of the landscape. "These wildfires coincide with the extinction of the pygmy mammoth]."
Climate change - sea level rise
Climate change which changed sharply in California and which affected the sea level likely played a part in the extinction, as the sea level rose about 61% of the area of the islands were submerged. About 4,000 years before extinction the island had an area of about 1,900 km2, (about the size of modern Sardinia). Then the sea level rose even more leaving four smaller islands and the landmass of these islands shrank by nearly eighty percent. Post-glacial warming reduced the available fresh water and food sources for the pygmy mammoth, putting a great strain on the population, and making them vulnerable to other adverse effects.
A controversial explanation of the pygmy mammoth's extinction is that of a cosmic impact affecting a large part of the western United States. Douglas Kennett and his colleagues hypothesized that an impact may have caused rapid ecosystem disruption, triggering megafaunal extinctions of and reducing the population of the pygmy mammoth. However, geological data supporting or contradicting the an impact is inconclusive.
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