Northern Australia

The Far East, one of the twelve divisions of the Earth, encompasses northern Australia, the entire Indonesian archipelago (excluding Aceh and Sumatra), the Philippines, the island of New Guinea, mainland Southeast Asia, the Malay Peninsula, eastern and southern China (China proper), Taiwan, the Korean Peninsula, the southern portion of the Russian Far East, and most of the Japanese archipelago, except for Hokkaido.

The southeastern boundary runs through Micronesia and Melanesia, dividing these regions into eastern and western subregions.

The northwestern boundary follows a line that separates Mongolia from China and delineates the division between Xinjiang and Tibet from China proper. It extends from its northernmost point, just beyond the northern arc of the Amur River—which marks China’s border with Russia—to its westernmost point, at the tri-border junction of Burma, India, and the Bay of Bengal.

The northeastern boundary distinguishes the extreme southern portion of the Russian Far East from the rest of the district and separates most of Hokkaido from Honshu, Kyushu, and Shikoku.

The southwestern boundary encompasses nearly all of Southeast Asia, with the exception of Aceh, which juts into the Indian Ocean and forms the southern shore of the Strait of Malacca, historically the key maritime gateway to the East.

HistoryAtlas contains 4,553 entries for The Far East from the Paleolithic period to 1899.

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Australia is possibly occupied by at least 174,000 BCE (a date suggested by archaeological fieldwork in Western Australia’s Kimberley district).

The Moderns are taller, more slender, and less muscular than the Neanderthals, with whom they share—perhaps uneasily—the Earth.

Though their brains are smaller in overall size, they are heavier in the forebrain, a difference that may allow for more abstract thought and the development of complex speech.

Yet, the inner world of the Neanderthals remains a mystery—no one knows the depths of their thoughts or how they truly expressed them.

The history of indigenous Australians is thought to have spanned forty thousand to forty-five thousand years, although some estimates have put the figure at up to seventy thousand years before European settlement.

A genetic study of one hundred and eleven Aboriginal Australians, published in the journal Nature on March 8, 2017 (Aboriginal mitogenomes reveal 50,000 years of regionalism in Australia), implies that "the settlement of Australia comprised a single, rapid migration along the east and west coasts that reached southern Australia by 49–45 ka. After continent-wide colonization, strong regional patterns developed and these have survived despite substantial climatic and cultural change during the late Pleistocene and Holocene epochs. Remarkably, we find evidence for the continuous presence of populations in discrete geographic areas dating back to around 50 ka, in agreement with the notable Aboriginal Australian cultural attachment to their country.”

For most of this time, the Indigenous Australians lived as nomads and as hunter-gatherers with a strong dependence on the land and their agriculture for survival.

Only Africa has older physical evidence of habitation by modern humans.

There is also evidence of a change in fire regimes in Australia, drawn from reef deposits in Queensland, between seventy thousand years and one hundred thousand years years ago, and the integration of human genomic evidence from various parts of the world supports a date of before sixty thousand years for the arrival of Australian Aboriginal people in the continent.

Modern humans reach Australia by at least 58,000 BCE.

In 1990, a date of sixty thousand years was suggested for a rock shelter in the Northern Territory, but the finding, based on the use of a recently developed technique called thermoluminescence, is still being evaluated.

The first settlement would have occurred during an era of lowered sea levels, when there was an almost continuous land bridge between Asia and Australia, but watercraft must have been used at some points.

The descendants of the immigrants to West Asia who had remained in the south (or taken the southern route) had spread generation by generation around the coast of Arabia and the Iranian plateau until they reached India.

One of the groups that had gone north (east Asians were the second group) had ventured inland and radiated to Europe, eventually displacing the Neanderthals.

They had also radiated to India from Central Asia.

The former group headed along the southeast coast of Asia, reaching Australia between fifty-five thousand and thirty thousand years ago, with most estimates placing it about forty-six thousand to forty-one thousand years ago.

Sea level is much lower during this time, and most of Maritime Southeast Asia is one land mass known as the lost continent of Sunda.

The settlers probably continued on the coastal route southeast until they reached the series of straits between Sunda and Sahul, the continental land mass that was made up of present-day Australia and New Guinea.

The widest gaps are on the Weber Line and are at least ninety kilometers wide, indicating that settlers had knowledge of seafaring skills.

Archaic humans such as Homo erectus never reached Australia.

If these dates are correct, Australia was populated up to ten thousand years before Europe.

This is possible because humans avoided the colder regions of the North favoring the warmer tropical regions to which they were adapted given their African homeland.

Another piece of evidence favoring human occupation in Australia is that about forty-six thousand years ago, all large mammals weighing more than one hundred kilograms suddenly became extinct.

The new settlers were likely to be responsible for this extinction.

Many of the animals may have been accustomed to living without predators and become docile and vulnerable to attack (as will occur later in the Americas).

Some settlers cross into Australia, while others may have continued eastwards along the coast of Sunda eventually turning northeast to China and finally reaching Japan, leaving a trail of coastal settlements.

This coastal migration leaves its trail in the mitochondrial haplogroups descended from haplogroup M, and in Y-chromosome haplogroup C.

Thereafter, it may have become necessary to venture inland, possibly bringing modern humans into contact with archaic humans such as H. erectus.

Recent genetic studies suggest that Australia and New Guinea were populated by one single migration from Asia as opposed to several waves.

The land bridge connecting New Guinea and Australia became submerged approximately eight thousand years ago, thus isolating the populations of the two landmasses.

The small population of moderns had spread from the Near East to South Asia by fifty thousand years ago, and on to Australia by forty thousand years ago, Homo sapiens for the first time colonizing territory never reached by Homo erectus.

It has been estimated that from a population of two thousand to five thousand individuals in Africa, only a small group, possibly as few as one hundred and fifty to one thousand people, crossed the Red Sea.

Of all the lineages present in Africa only the female descendants of one lineage, mtDNA haplogroup L3, are found outside Africa.

Had there been several migrations one would expect descendants of more than one lineage to be found outside Africa.

L3's female descendants, the M and N haplogroup lineages, are found in very low frequencies in Africa (although haplogroup M1 is very ancient and diversified in North and Northeast Africa) and appear to be recent arrivals.

A possible explanation is that these mutations occurred in East Africa shortly before the exodus and, by the founder effect, became the dominant haplogroups after the exodus from Africa.

Alternatively, the mutations may have arisen shortly after the exodus from Africa.

Some genetic evidence points to migrations out of Africa along two routes.

However, other studies suggest that only a few people left Africa in a single migration that went on to populate the rest of the world, based in the fact that only descents of L3 are found outside Africa.

From that settlement, some others point to the possibility of several waves of expansion.

Australasia (49,293 – 28,578 BCE): Upper Pleistocene I — Continental Shelves, Fire Country, and the Unpeopled Islands of the Far South

Geographic & Environmental Context

During the long glacial prime of the Late Pleistocene, Australasia stretched as a single vast, connected super-land: the Sahul continent, where Australia, New Guinea, and Tasmania were joined by the broad Arafura and Carpentaria shelves, while across the Tasman Sea, the New Zealand–Norfolk–Kermadec arc stood isolated, volcanically active, and entirely uninhabited by humans.

The region’s physiography displayed extremes of exposure and contrast:

• To the north, tropical savannas and monsoon coasts extended from Kimberley and Arnhem Land through Cape York to the low divide of southern New Guinea, while the Gulf of Carpentaria held a vast inland sea–wetland complex.

• Across central and southern Australia, vast dune fields, salt lakes, and desert basins alternated with fertile riverine corridors like the Murray–Darling and the Willandra Lakes.

• In the south, the Bassian Plain connected the mainland to Tasmania, while New Zealand remained beyond human reach—its forests, volcanic zones, and seabird cliffs untouched.

Sea level lay ~100 m below present, enlarging the continental shelves and exposing wide coastal plains, which were colonized by both humans (in Australia) and dense faunal populations.

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Climate & Environmental Shifts

• Early Glacial Phase (~49–35 ka): Gradual cooling, declining precipitation in continental interiors, and expansion of arid belts; forest contraction in the tropics and southeast.

• Approach to the Last Glacial Maximum (~35–28 ka): Sharper temperature drop, stronger seasonality, and intensified westerlies and trade winds. Northern monsoons weakened, and interior lakes fell or dried episodically.

• Regional Contrasts:
  • Northern Australia remained humid enough for monsoon-driven wet–dry cycles, sustaining aquatic ecosystems along rivers and coasts.
  • Southern Australia and Tasmania cooled markedly, with snowfall on upland ranges and alpine conditions in the Great Dividing Range and Tasmanian highlands.
  • New Zealand entered full glaciation: the Southern Alps carried expanded glaciers, and snowlines dropped by hundreds of meters.

The climate oscillated between long cold stasis and short, mild interstadials—conditions that defined both human adaptive strategies and the evolutionary dynamics of uninhabited island ecologies.

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Human Presence and Lifeways

Human societies were firmly established across the Australian continent and the connected Sahul landmass, but absent east of the Tasman frontier.

Northern Australasia (Sahul Tropics)

• Occupation and Range:
  Continuous habitation in Arnhem Land, the Kimberley, Cape York, and the Gulf lowlands; movement extended across the Arafura Plain into southern New Guinea.

• Economy:
  Broad-spectrum foraging—fish, shellfish, turtles, dugong, and small terrestrial game. During glacial lowstands, coastal groups ranged across the now-submerged shelf flats, exploiting estuaries and reefs.

• Technology:
  Sophisticated flake–blade industries, hafted points, resin adhesives, and early ground ochre use; fiber and wooden implements (spears, nets, traps) widely employed.

• Symbolism:
  Earliest rock art phases—engraving and pigment painting—appeared in the Kimberley and Arnhem Land, along with structured burials and cremations.

• Resilience:
  Estate-based mobility tracked monsoon pulses; access to the flooded Carpentaria lowland and inland freshwater refugia buffered against droughts.

Southern Australasia (Southern Australia, Tasmania, South Island New Zealand)

• Australia:
  Long-settled communities adapted to harsh continental variability. Along the Willandra Lakes and Murray–Darling Basin, people fished, hunted marsupials, collected seeds and tubers, and practiced ceremonial cremation and burial rites (Mungo).
  On the expanded southern shelf coasts, foragers harvested shellfish, seals, pinnipeds, and stranded whales, while inland hunters pursued kangaroos, emus, and small marsupials.
  The use of fire to manage vegetation—so-called fire-stick farming—maintained open grasslands and supported reliable game.

• Tasmania (then mainland-connected):
  Populations ranged across the Bassian Plain, exploiting riverine corridors and coastal flats for waterfowl and fish; early cold-adapted hearth traditions emerged.

• New Zealand and sub-Antarctic arcs:
  Entirely uninhabited, though South Island glaciers carved fjords and plains later to support Holocene ecosystems.

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Unpeopled Frontiers: South Polynesia and Oceanic Arcs

East of Sahul, the South Polynesian sector (New Zealand, Norfolk, Kermadec, Chatham Islands) remained a wilderness of volcanic highlands, periglacial coasts, and seabird colonies.
The Oruanui eruption (c. 25.5 ka BP) from the Taupō caldera in New Zealand blanketed the North Island and offshore ridges with tephra, reshaping soils, lakes, and drainage systems.
Forests shifted between podocarp–broadleaf canopies and scrub–grassland mosaics; moa and Haast’s eagle dominated terrestrial food webs, while offshore seabird realms thrived on predator-free islets.

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Technology & Material Culture

Across Sahul, technology mirrored a mature foraging economy:

• Stone: flake–blade cores, backed microliths, and grindstones; heat treatment and resin hafting.

• Organic: spears, clubs, nets, and wooden shields; fiber technology for carrying and trapping.

• Pigment and ornament: widespread ochre use for painting, body decoration, and burial; shell and tooth ornaments signal social identity.

• Fire technology: mastery of landscape burning as a central environmental tool.

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Movement & Interaction Corridors

• Land and River Networks: the Murray–Darling, Willandra, and Lake Eyre basins functioned as arteries linking interior and coast.

• Shelf and Coast Routes: mobile bands traversed the exposed Sahul shelves, harvesting estuarine resources and migrating seasonally.

• Northern Gateways: travel between northern Australia and southern New Guinea maintained genetic and cultural interchange across the connected shelf.

• Southern Pathways: the Bassian Plain allowed movement between mainland and Tasmania until postglacial flooding severed the link.

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Cultural & Symbolic Expressions

• Ritual landscapes: rock shelters and burial grounds (e.g., Willandra) reveal early ceremonial organization.

• Artistic innovation: hand stencils, engraved motifs, and ochre figurative painting predate 30 ka in northern Australia.

• Fire and mythic space: controlled burning likely embedded in cosmological understanding of land stewardship.

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Environmental Adaptation & Resilience

Australasia’s Pleistocene societies mastered the ecology of variability:

• Mobility with continuity: shifting among waterholes, estuaries, and resource belts on seasonal rhythms.

• Storage through knowledge: environmental mapping replaced physical storage—knowing when and where resources renewed was key.

• Fire as technology: selective burning maintained mosaics that sustained wildlife and plant yields.

• Refugia strategies: wetlands and monsoon belts offered fallback zones through glacial droughts.

The unpeopled islands to the east, by contrast, evolved ecological self-sufficiency—volcanic fertility, avian abundance, and intact forests awaiting future colonists.

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Transition Toward the Next Epoch

By 28,578 BCE, the Australasian world stood poised at the threshold of deglaciation:

• Sea-level minima connected lands and compressed ecologies into wide continental shelves.

• Human societies in Sahul had adapted to every climate zone, from arid interior to reef coast, with rich symbolic traditions already in place.

• Islands beyond the Sahul frontier—New Zealand, Norfolk, Chatham, Kermadec—remained avian kingdoms without humans.

As ice sheets began their slow retreat, the landscapes and coastlines that would shape the Holocene—estuaries, islands, and archipelagos—were already being prepared by the patient interplay of fire, flood, and time.