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Channel Islands (USA) Pygmy Mammoths (Mammuthus Exilis) Compared and Contrasted with M

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Channel Islands (USA) Pygmy Mammoths (Mammuthus Exilis) Compared and Contrasted with M Channel Islands (USA) pygmy mammoths (Mammuthus exilis) compared and contrasted with M. columbi, their continental ancestral stock L.D. Agenbroad Department of Geology, Northern Arizona University, Flagstaff, Hot Springs, Arizona, USA SUMMARY: Remains of the pygmy mammoth Mammuthus exilis have been known on the Channel Island of California since 1856. After initial colonization of Santa Rosa Island by M. columbi, the process of island adaptation noted as Foster's Rule came about. After the available radiocarbon chronology, it appears that they have been there, in essentially unchanged pygmy form, for more than 47,000 years (i.e. beyond the limits of radiocarbon chronology). They may have survived until the early Holocene colonization of the islands by the ancestors of the ancient Chumash people. With the reconsideration of the dwarf status place (Agenbroad 1998, 1999). During the of the woolly mammoths (M. primigenius) of nearly 30 year hiatus between the Orr’s work Wrangel Island (Mol 1995; Tikhonov 1997), and the 1990’s salvage excavations, amateur the only island dwelling truly diminutive mam- collecting was done by Boris Woolley, a mem- moths are those from the Channel Islands of ber of the ranching families in control of Santa California. Remains of these pygmy mam- Rosa Island. moths have been known on the islands since Beginning with the recovery of the 1994 discovered in 1856 by a coast and geodetic sur- skeleton, a methodical pedestrian survey of the vey. The first publication of the animals was in islands was begun, using Global Positioning a brief report in the Proceedings of the System (GPS) coordinates to pinpoint each dis- California Academy of Sciences (Stearns covery. This on-going system has produced 1873). Further paleontological studies were more than 140 new mammoth localities on the conducted by the City College of Los Angeles three outermost islands (a new locality being (Stock & Furlong 1928). Sporadic field collec- defined as one or more mammoth remains that tions by the Los Angeles County Museum were in all probability do not represent a previous halted with the advent of World War II. Phil location). The survey has tended to destroy Orr, of the Santa Barbara Museum of Natural some of the myths about the distribution and History, collected mammoth remains in the types of mammoth remains on the islands. 1950’s and 1960’s, to substantiate his archaeo- During the Pleistocene glacial advances logical theory that the ancestral Chumash water was held on the continents as snow, gla- Indians decimated the island proboscideans ciers, and ice sheets. As a result, sea level was (Orr 1956, 1968). Orr was unable to convince lowered by 100 to 125 m in the last major gla- his scientific peers and island paleontology met cial cycle. The lowering of sea level exposed a a hiatus until the 1990's with a salvage collec- large island off the coast of California, desig- tion of a San Miguel Island specimen, by Bob nated as ‘Santarosae’ in Phil Orr’s research. Gray of Santa Barbara City College, for the Postglacial warming caused melting of the con- National park Service (NPS). In 1994 the dis- tinental ice and snow, recharging the ocean, covery, excavation and recovery of a nearly causing sea level to rise to the current position. complete, adult, male, M. exilis skeleton took Santarosae became gradually inundated, leav- 473 The World of Elephants - International Congress, Rome 2001 ing only four islands which reflect the highest slopes. This gave smaller animals access to elevations of the Pleistocene ‘super island’. San upland pasturage which may have been crucial Miguel, Santa Rosa, Santa Cruz, and Las to survival in periods of climatic or dietary Anacapas Islands are all that remain exposed of stress. Bone metric analyses confirm Sondaar’s Santarosae. Seventy-six percent of the conclusions for M. exilis, the island adapted Pleistocene island is now submerged, with the mammoth. last connections between the island having Analyses of the femora, humerii and denti- been inundated between 12,000 and 11,000 tion reveal additional characteristics. Femora of radiocarbon years ago. Of the four modern the island mammoths are significantly longer, islands, all but Las Anacapas produce mam- as contrasted to the mean of the Hot Springs moth remains. Columbian mammoths, and the femoral cross After initial colonization of Santarosae by M. section of the pygmy mammoth is more circu- columbi, the process of island adaptation noted lar, as compared to the flat ellipse of the conti- as Foster’s Rule (Foster 1964) came about. nental mammoths. Studies of humeri suggest Large continental mammals became smaller rotation of some of the muscle functions and and small continental mammals became larger. attachments. The humerus takes on the added Pleistocene Santarosae had “giant” deer mice use, as a braking mechanism for a quadruped (Peromyscus) and “pygmy” mammoths (M. descending steep slopes. Analysis of dentition exilis). has produced a plot of all molar generations, In the island survey, a ratio of approximately which shows a line of best fit to be coinciden- 1:10 large mammoth remains/small mammoth tal for M. columbi and M. exilis, supporting the remains was encountered. All of the Columbian probable ancestral relationship of the mainland mammoth remains, thus far, have been located mammoth for the island form. Dental age in elevated marine terrace remnants. Pygmy assignments, on the relative, ‘African Elephant mammoth remains have been located in marine Year’scale, imply high mortality rates in the ‘0- terraces, alluvial stream terraces, and stream 30 year’ range; few individuals survive past ‘50 channels near the island uplands. Appro- years’ of age. Two individuals represent ani- ximately 50% of the island of Santa Rosa mals whose mandibular teeth were missing due consists of uplands, with slopes exceeding thir- to advanced age and wear, yet the animals con- ty degrees. Using Columbian mammoths of tinued to masticate against the jaw bone. Hot Springs, South Dakota as a representative Chronology for pygmy mammoths has been continental population (Agenbroad 1994), var- one of the weakest points of Channel Islands ious metric and morphological comparisons paleontology. Published dates have been were made with the island mammoths. obtained from charcoal associated with mam- Calculations based on the center of gravity of moth remains. Wenner et al. (1991) have brand- large and small mammoths revealed that the ed all such dates as ‘equivocal’ and suggest pygmy mammoths were able to negotiate they should be discarded. In part, this is slopes that were as much as 10 degrees steeper because it has been stated that all mammoth than Columbian mammoths could travel. This remains on the islands are secondarily deposit- suggests one of the reasons that the diminutive ed (Orr 1959, 1968; Cushing et al. 1986; Roth forms became the dominant island mammoth 1982, 1996; Wenner et al. 1991). They (Wenner population. It should be noted that pygmy et al. 1991) even go so far as to infer, “...there mammoths have not been discovered on the is no natural charcoal on the islands”. continental coast. The 1994 skeleton was sampled for bone In 1977, Paul Sondaar, studying stegodons in from the marrow-producing segment of the Indonesia, concluded there was a shortening of right femur. The resulting accelerator-mass lower limb bones, to allow “low gear locomo- spectrometry (AMS) date for the animal was tion” (akin to 4 wheel drive in modern vehicles) 12,840 +/- 410 yr BP (CAMS 24429). Not only needed in ascending and descending steep was this date from mammoth bone itself, there 474 Channel Islands (USA) Pygmy Mammoths (Mammuthus exilis) compared and contrasted with M. columbi... was no question as to the remains being in pri- the First International Mammoth Confe- mary deposition, as even the smallest bones of rence. Deinsea 6: 89-102. St. Petersburg, the phalanges were still in articular position. Russia. Since that time, other AMS dates on bone col- Cushing, J.E., Wenner, A.M., Noble, E. & lagen have been obtained, as well as dates from Daly, M. 1986. A groundwater hypothesis associated charcoal. Some samples differ as lit- for the origin of ‘fire areas’ on the Northern tle as 10 to 20 years between the bone date and Channel Islands, California. Quaternary the associated charcoal date. This tends to Research 26: 207-217. refute some of the claims made by Wenner et Foster, J.B. 1964. Evolution of mammals on al. (1991). islands. Nature 202: 234-235. Summarizing the available radiocarbon Mol, D. 1995. Over dwergolifanten en chronology of the Channel Island Mammoths, dwergmammoeten. Cranium 12: 38-40. it appears they have been on the islands, in Orr, P. 1956. Dwarf mammoths and man on pygmy form, essentially unchanged, for more Santa Rosa Island. University of Utah than 47,000 years (beyond the limits of radio- Anthropological Papers 26: 75-81. carbon chronology). It also appears that they Orr, P. 1968. Prehistory of Santa Rosa Island. may have survived until the early Holocene Santa Barbara Museum of Natural History. colonization of the islands by the ancestors of Roth, V.L. 1982. Dwarf mammoth from the the ancient Chumash people, first recorded Santa Barbara, California Channel between 10,800 and 11,300 years ago. Islands: size, shape, development, and evo- lution. Ph.D. dissertation. New Haven: Yale REFERENCES University. Roth, V.L. 1996. Pleistocene dwarf elephants Agenbroad, L.D. 1994. Taxonomy of North from the California Islands. In Shoshani, J. American Mammuthus columbi and bio- H. and P. Tassy (eds.), The Proboscidea: metrics of the Hot Springs mammoths. In 249-253. Oxford: University of Oxford Agenbroad, L. D. and J. I. Mead (eds.), The Press. Hot Springs Mammoth Site: a decade of Sondaar, P.Y. 1977. Insularity and its effect on field and laboratory research in paleontol- mammal evolution.
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