
© Natural Earth
Map showing eastern Beringia during the Last Glacial Maximum (LGM; ~23–19 ka B.P.) when eustatic sea level was ~120 m below its present level1. Megafauna fossils of this study were initially collected between 1940 and 1954 from mining operations near Fairbanks, Alaska, and more recently from the Klondike mining district near Dawson City in the Yukon Territory. Permafrost zones, discriminated by dashed purple curves, are continuous (CPZ, >90% frozen ground), discontinuous (DPZ, >50%), and sporadic (SPZ, <50%)35. White curves outline areas of both continental and mountain glaciation with the latter having occurred in the Brooks Range of northern, and the Alaskan Range of southern, Alaska70. Dashed red curve indicates the Arctic Circle. Chukotka is an autonomous district (Okrug) in easternmost Russia.
During the time period leading up to the Last Glacial Maximum (~23-19 ka B.P.), when eustatic sea level was substantially lower, Alaska and the Yukon Territory were part of the largest circumarctic area to remain unglaciated, called Beringia (Fig.
1), which extended from eastern Siberia (Chukotka) across the exposed Bering Strait region into Alaska and western Canada
1,
2.
The glacial steppe environment of Beringia3 was a refugium for Plio-Pleistocene tundra-grassland plant communities4 as well as for the now-extinct mammalian megafauna 5.
Relict permafrost within the region 6,
7,
8,
9 has preserved an extraordinary frozen record of plant, pollen, insect, and vertebrate fossil remains, as well as their ancient DNA 1,
10,
11.
Early expeditions to Alaska
12,
13,
14 and the Yukon Territory
14,
15 found large quantities of megafaunal bones along beaches, riverbanks, and in minor-stream valleys
8. Even greater collections of these fossils were made after industrial-scale placer-gold mining operations began in the Fairbanks and Klondike districts in the early 20th century
16. Otto W. Geist undertook extensive fossil collecting in Alaska on behalf of the American Museum of Natural History (AMNH), and in a typical year (1938) shipped more than eight thousand select specimens, weighing nearly eight tons (~7257 kg), to New York City
8.
The fossil bones collected included those of bison, mammoth, horse, musk ox, moose, lynx, lion, camel, mastodon, bear, and caribou, with
many of these animals also appearing as frozen partial carcasses or mummies1,
8,
17. The three most common genera found were bison, mammoth, and horse, which represent more than 90% of Beringia's large mammalian biomass
18. Many tens of thousands of specimens were collected in the 20th century from Alaska and the Yukon Territory
5,
8,
19, and hundreds to thousands more are still being recovered every year from mines in the Klondike district alone
1.
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