Pygmy mammoth

Species of mammothTemplate:SHORTDESC:Species of mammoth

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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 became extinct during the Quaternary extinction event in which many megafauna species became 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, 9,070 kg (20,000 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).

## Discovery

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 and decided 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 began. This 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, the skeleton 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.

## Habitat

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 Rosa Island; their body size became smaller because it required less food and resources to remain energized and alive. After this evolutionary period, the mammoth had become a 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.

## Evolution

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 kilometres (4.3 mi). 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 evolutionary period, the mammoth had become a distinct species, the pygmy mammoth. The pygmy mammoth's evolution on Santa Rosae took over 30,000 years.

The pigmy mammoth is not the only example of island dwarfism in mammoth: another example is *Mammuthus lamarmorai* in the Mediterranean island of Sardinia.

## Extinction

The cause of extinction of the pygmy mammoth is unknown, but it could have been caused by over-hunting by humans, wildfires, climate change, or some combination thereof.

### Humans

Human interference often has a greater effect on island species than on continental species, and there is evidence that Native Americans hunted the pygmy mammoth on Santa Rosa. "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."

### Wildfires

"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

A shift in sea level driven by climate change likely played a part in the extinction: as the sea level rose, about 61% of the island land-mass was submerged. Some 4,000 years prior to extinction the island had an area of roughly 1,900 square kilometres (730 sq mi), (about the size of the island of **Maui**). Further increase in sea levels left four smaller islands of nearly eighty percent less total landmass. Post-glacial warming reduced available fresh water and food sources for the pygmy mammoth, pressuring the remnant population and making it vulnerable to other adverse effects.

### Comet impact

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 and reducing the population of the pygmy mammoth. However, geological data supporting or contradicting an impact is inconclusive.

## See also

* Paleontology portal

* Dwarf elephant

## Notes

1. ↑ Chester Stock and E. L. Furlong (1928). "The Pleistocene elephants of Santa Rosa Island, California" (PDF). *Science*. **68** (1754): 140–141. Bibcode:1928Sci....68..140S. doi:10.1126/science.68.1754.140. PMID 17772244.
2. ↑ Agenbroad 2010, p. 1.
3. ↑ Torben 2012, p. 3.
4. ↑ Agenbroad, L. D. (2010). ". Mammuthus exilis from the California Channel Islands: Height, Mass and Geologic Age" (PDF). *Proceedings of the 7th California Islands Symposium*. p. 17. Retrieved 13 June 2012.
5. ↑ 5.0 5.1 "The pygmy mammoth". *Channel Islands National Park*. U.S. Department of the Interior National Park Service. 2006-09-01. Retrieved 2008-06-14.
6. ↑ Larramendi, A. (2016). "Shoulder height, body mass and shape of proboscideans" (PDF). *Acta Palaeontologica Polonica*. **61**. doi:10.4202/app.00136.2014 . Retrieved November 21, 2015.
7. ↑ Agenbroad, L.D. (2003). "New absolute dates and comparisons for California's Mammuthus exilis". *Deinsea*. **9**: 1–16.
8. ↑ 8.0 8.1 8.2 Agenbroad, L.D.; Johnson J.; Morris D.; Stafford T.W. "Mammoths and Humans as Late Pleistocene Contemporaries on Santa Rosa Island" (PDF). *Proceedings of the American Geophysical Union*. Spring Meeting 2007.
9. ↑ 9.0 9.1 9.2 Agenbroad, Larry D.; Don P. Morris. "Giant Island/Pygmy Mammoths:The Late Pleistocene Prehistory of Channel Islands National Park" (PDF). *National Park Service Paleontological Research*. **4**: 35–39. Archived from the original (PDF) on 2014-02-19. Retrieved 2013-10-23.
10. ↑ anonymous, anonymous. "Stranded on Santa Monica". *Discover*. **16**: 1. ProQuest 206020333.
11. ↑ Fitzgerald, Richard; Rondeau, Michael (2012). "A Fluted Projectile Point from Crystal Cove State Park, Orange County, Alta California". *PaleoAmerica*. **4** (2): 247–256. doi:10.1179/cal.2012.4.2.247.
12. ↑ 12.0 12.1 12.2 12.3 Kennett, D.J.; Kennett, J.P.; West, G.J.; Erlandson, J.M. (2008). "Wildfire and abrupt ecosystem disruption on California's Northern Channel Islands at the Ållerød–Younger Dryas boundary (13.0–12.9 ka)". *Proceedings of the National Academy of Sciences*. **104** (27–28): 2530–2545. Bibcode:2008QSRv...27.2530K. doi:10.1016/j.quascirev.2008.09.006.
13. ↑ Rocha, Veronica (16 September 2016). "Well-preserved mammoth skull unearthed on Channel Islands puzzles scientists". *Los Angeles Times*. http://www.latimes.com/local/lanow/la-me-ln-mammoth-fossil-channel-islands-20160915-snap-story.html.
14. ↑ Agenbroad, L. D. (2001-10-19). "Channel Islands (USA) pygmy mammoths (*Mammuthus exilis*) compared and contrasted with *M. columbi*, their continental ancestral stock". Rome: Consiglio Nazionale delle Ricerche. pp. 473–475. ISBN 88-8080-025-6. http://www.cq.rm.cnr.it/elephants2001/pdf/473\_475.pdf.
15. ↑ Agenbroad, Larry D.; J. Mead. "Distribution and palaeoecology of central and western North American Mammuthus". *National Park Service Paleontological Research*.
16. ↑ Koch, P. L. (1988). "The diet of Pleistocene proboscideans and its role in their extinction". *Geological Society of America 1988 Centennial Celebration Program*. **21**: A378.
17. ↑ Johnson, D. "Landscape evolution on San Miguel Island, California".
18. ↑ 18.0 18.1 Hollon, Tom. "Two weeks in the Pit as Indiana Jones". *The Scientist*. **16**: 1–2. ProQuest 200018191.
19. ↑ Agenbroad 2001, p. 473.
20. ↑ Agenbroad, p. 473.
21. ↑ "Channel Islands: The Pygmy Mammoth" (web). *National Park Service*.
22. ↑ Agenbroad 1998, p. 1.
23. ↑ Agenbroad, Larry D; Johnson, John R.; Morris, Don; Stafford Jr., Thomas W. (2005). "Mammoths and humans as late Pleistocene contemporaries on Santa Rosa Island". *Proceedings of the Sixth California Islands Symposium. Institute for Wildlife Studies, Arcata, CA*: 3–7.
24. ↑ Orr, Phil C; Berger, Rainer (1966). "The Fire Areas on Santa Rosa Island, California". *Proc. Natl. Acad. Sci*. **56** (5): 1409–1416. Bibcode:1966PNAS...56.1409O. doi:10.1073/pnas.56.5.1409 . PMC 219987 . PMID 16591389.
25. ↑ Berger, Rainer; Orr, Phil C. (1966). "The Fire Areas on Santa Rosa Island, California, II". *Proc. Natl. Acad. Sci*. **56** (6): 1678–1682. Bibcode:1966PNAS...56.1678B. doi:10.1073/pnas.56.6.1678 . PMC 220154 . PMID 16591403.
26. ↑ Rick, Torben C.; Hoffman, C. A.; Braje, T. J.; Maldonado, J. E.; Sillett, T. S.; Danchisko, K.; Erlandson, J. M. (2012). "Flightless ducks, giant mice and pygmy mammoths: Late Quaternary extinctions on California's Channel Islands". *World Archaeology*. **44**: 3–20. doi:10.1080/00438243.2012.646101.
27. ↑ Kennett, Douglas J.; Kennett, James P.; West, Allen; West, G. James; Bunch, Ted E.; Culleton, Brendan J.; Erlandson, Jon M.; Que Hee, Shane S.; Johnson, John R.; Mercer, Chris; Shen, Feng (2009-08-04). "Shock-synthesized hexagonal diamonds in Younger Dryas boundary sediments". *Proceedings of the National Academy of Sciences*. **106** (31): 12623–12628. doi:10.1073/pnas.0906374106 . PMC 2722287 . PMID 19620728.

## References

* Agenbroad, L.D. (2001). "Channel Islands (USA) pygmy mammoths (*Mammuthus exilis*) compared and contrasted with *M. columbi*, their continental ancestral stock", *World of Elephants*, 473
* Torben, Rick (2012). "Flightless ducks, giant mice and pygmy mammoths: Late Quaternary extinctions on California's Channel Islands", 3