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  2. Beringia - Wikipedia

    en.wikipedia.org/wiki/Beringia

    Beringia sea levels (blues) and land elevations (browns) measured in metres from 21,000 years ago to present. Beringia is defined today as the land and maritime area bounded on the west by the Lena River in Russia; on the east by the Mackenzie River in Canada; on the north by 72° north latitude in the Chukchi Sea; and on the south by the tip of the Kamchatka Peninsula. [1]

  3. Southern Dispersal - Wikipedia

    en.wikipedia.org/wiki/Southern_Dispersal

    The southern route dispersal is primarily linked to the Initial Upper Paleolithic expansion of modern humans and "ascribed to a population movement with uniform genetic features and material culture" (Ancient East Eurasians), which was the major source for the peopling of the Asia–Pacific region.

  4. Great American Interchange - Wikipedia

    en.wikipedia.org/wiki/Great_American_Interchange

    Other groups of carnivorans did not arrive in South America until much later. Dogs and weasels appear in South America about 2.9 Ma ago, but do not become abundant or diverse until the early Pleistocene. [106] Bears, cats, and skunks do not appear in South America until the early Pleistocene (about 1 Ma ago or slightly earlier). [106]

  5. Pleistocene - Wikipedia

    en.wikipedia.org/wiki/Pleistocene

    The Pleistocene (/ ˈ p l aɪ s t ə ˌ s iː n,-s t oʊ-/ PLY-stə-seen, -⁠stoh-; [4] [5] referred to colloquially as the Ice Age) is the geological epoch that lasted from c. 2.58 million to 11,700 years ago, spanning the Earth's most recent period of repeated glaciations.

  6. Isolation by distance - Wikipedia

    en.wikipedia.org/wiki/Isolation_by_distance

    Dispersal trends and rates were compared by using both spatial genetic structure and direct measures of dispersal. A total of 29 populations from three spatially different rock pools were subjected to allozyme analysis for four loci to access genetic variation and estimates of gene flow between populations were generated using population ...

  7. Marine Isotope Stage 5 - Wikipedia

    en.wikipedia.org/wiki/Marine_Isotope_Stage_5

    Marine Isotope Stage 5 or MIS 5 is a marine isotope stage in the geologic temperature record, between 130,000 and 80,000 years ago. [1] Sub-stage MIS 5e corresponds to the Last Interglacial , also called the Eemian (in Europe) or Sangamonian (in North America), the last major interglacial period before the Holocene , which extends to the ...

  8. Upward Sun River site - Wikipedia

    en.wikipedia.org/wiki/Upward_Sun_River_site

    The Upward Sun River site, or Xaasaa Na’, is a Late Pleistocene archaeological site associated with the Paleo-Arctic tradition, located in the Tanana River Valley, Alaska. Dated to around 11,500 BP, [1] Upward Sun River is the site of the oldest human remains discovered on the American side of Beringia. [2] The site was first discovered in 2006.

  9. Calabrian (stage) - Wikipedia

    en.wikipedia.org/wiki/Calabrian_(stage)

    Calabrian is a subdivision of the Pleistocene Epoch of the geologic time scale, defined as 1.8 Ma—774,000 years ago ± 5,000 years, a period of ~. The end of the stage is defined by the last magnetic pole reversal (781 ± 5 Ka) and plunge into an ice age and global drying possibly colder and drier than the late Miocene through early Pliocene cold period. [4]