CHRONOLOGY and THEMES: Paleolithic Era c. 6.5 million BP-9,000 Before Present (BP), Humans as hunter-gatherers


    About 6.5 million BP a population of African apes split into two distinct species. One of these evolved into human beings. The other to chimpanzees.

    About 4 million BP the hominid species, Australopithecus, began walking predominantly in an upright stance.

    Around 2 million BP homo erectus began fashioning tools

    Emergence of Modern Humans in Africa; ca. 200000 BP; earliest migrations out of Africa, ca. 150,000 BP

    Pleistocene Era ca. 2 million-9000 BP; influence of climate changes on human development

    Neolithic Revolution c. 8000-7000 BC in the Near East, domestication of plants and animals


The purpose of this chapter is to explore human development from its origins through to the advent of settled agricultural existence. Human settlement, based on the domestication of plants and animals, has long been identified as having occurred around 8000/7000 BC in ancient Iraq, This region is known to scholars as the Ancient Near East or as Mesopotamia. The latter term is the ancient Greek word for the land between two rivers, namely, the Euphrates and the Tigris. During prehistoric times the Ancient Near East functioned as a land bridge between Africa where modern humans originated around 200,000 BP and other regions of human habitation, including Eurasia, East Asia, Australia, and the Americas. According to the available evidence modern humans migrated from Africa as far as the Americas between 150,000 and 24000 BP. The evidence for these conclusions is susceptible to revision due to the accelerated pace of discovery during the past decade. Alongside traditional analysis of archaeological assemblages of prehistoric remains, current investigators utilize an array of tools to reconstruct this history, including genetic mapping -- of both humans and other organisms -- climatology (to explain human migration during the ice Age) -- and linguistics (using language history to confirm the results of the other methods). To be certain, much of this research is speculative and subject to intense debate even among specialists. However, the unquestioned reliance placed on DNA evidence in judicial procedures as well as the importance of climatological evidence to the current debate regarding global warming demonstrates the need to take this data seriously.


Before proceeding there is need to address the issue of deep seated religious beliefs and to reassure the reader that the purpose of this work is not to challenge these. The objective here is to present a summary of scientific data obtained through empirical research that addresses human origins. These findings in no way deny questions of faith. As will become apparent, this book exhibits a healthy respect for all religious world views. Along with fields such as philosophy and astrophysics, religion is one of a few disciplines that asks the vital questions, why are we here, where did we come from, and where are we going. Having said this, the increasingly consistent record that is emerging for human origins, confirmed by a bewildering array of scientific data, inevitably confronts the written record of ancient religious texts. The latter were compiled by humans, however divinely inspired, without the benefit of modern science or technology. If anything, the scientific data has demonstrated that human origins are far more complicated that religious thinkers writing around 1000 BC in ancient Israel, for example, could have conceived. These findings in no way discard essential questions regarding the existence of god. As we contemplate the significance of the 'Big Bang' some 10 billion years ago, the finite character of the universe expanding through a limitless void of space, or the formation of the planet earth some 4 billion years ago, it becomes difficult to comprehend the purpose of existence by other means than faith.


Prehistoric Africa

Africa is the second largest landmass in the world. It is also the highest and the oldest landmass in the world. The continent presents itself as a vast plateau, rising steeply on all sides from various coastal strips and extending along a north-south axis. Mountains and divides form basins in various regions, most notably the basin of the Congo River, at the Equator, where the rain forests are very dense. The vast unbroken extent of the African plateau causes rivers to drain through cataracts and magnificent waterfalls on their way to the sea. Apart from the Nile, no African rivers are navigable beyond the coast. The continent's most remarkable feature remains the Great Rift Valley, formed by the tectonic movement of the Arabian landmass away from Africa. Over tens of millions of years this earth movement created long, deep valleys southward through the African plateau. Several of these valleys form large enclosed highland lakes. Lake Victoria, sitting 3700 ft above sea level, is the third largest lake in the world. Waters beginning in this region flow northward 4000 miles to form the two branches (White and Blue) of the Nile, the longest river in the world. The Great Rift actually extends beyond the continent under the Red Sea all the way to the Dead Sea/Jordan River valleys of Israel. It is here along the cliffs of the Great Rift Valley in Africa that the earliest remains of humans have survived.


As the accompanying table displays, DNA analysis indicates that archaic humans or hominids evolved from African primates approximately 6.5 million BP. DNA of modern humans has been demonstrated to be 99% compatible to that of Chimpanzees, for example.





35 million BP


30 million BP


10 million BP 97%


8 million BP 99%


 6.5 mill. B 100%


Many attributes that primates hold in common with humans -- including stereoscopic vision, sexual pairing to care for young, group social behavior, and the tendency to use fore limbs to perform tasks other than locomotion -- clearly facilitated human development. Around 4 million BP hominids known as Australopithecus descended permanently from the canopy of the African rain forest to walk in an upright manner. Apart from the obvious advantage this had in freeing hands to perform work and to fashion tools (and thus render food gathering and preparation more amenable), the most significant development in this regard was the anatomical transformation associated with upright posture. By balancing the cranium on the spinal column, hominids reduced the need for massive muscular structures that quadrupeds utilize to suspend their heads out in front of their forelimbs. When one looks at images of apes and other mammals such as horses, lions, and cows, the size of their neck and shoulder muscles is striking especially in comparison with those human. These muscles are connected to the skull by means of bundled sinews of ligament and tendon the weight of which, suspended, actually restricts the size of the skull. By balancing the cranium on the spinal cord through upright poster, archaic humans reduced the need and therefore the size of these muscle parts, albeit gradually and imperceptibly over millions of years. As muscles receded cranial capacity (and brain size) expanded, enabling hominids to gain in intelligence and advance ahead of their primate relatives. Advances in tool use and manufacture, emerging social formations based on extended clans, hunting bands, and tribes, and even the harnessing of fire by 350000 BP all reflect advances made by archaic human species during Paleolithic times in Africa, all prior to the advent of modern humans.




Australopithecus hominid, 6-2 mill. BP

Theoretically, upright posture resulted in anatomical changes; front limbs were freed for tool use and food preparation, reducing muscular structure of skull and expanding cranial capacity.

A second factor in human development during prehistory was climatic; namely, the Pleistocene Era, 2 million - 9000 BP

(Ice Ages) see below

Homo Erectus, 1.6 mill.-400,000 BP, first out of Africa 1.2 million BP (Europe, China).



More than a dozen species of archaic humans existed in Africa during this period, most of which wandered off into extinction. Populations of hominids appear to have risen and collapsed as they confronted changing environmental conditions. Approximately 2 million BP hominids known as Homo erectus began to fashion stone tools (chipped and flaked stone tools, bone tools, and fire) and to enjoy greater mobility. By 1.2 million BP elements of this species migrated out of Africa, wandering as far as East Asia by 400,000 BP. Climatological evidence indicates that the impetus for this migration was environmental, originating with the advent of the Pleistocene era (Ice Age) around 2.5 million BP. Recent analysis of climatological and paleoenvironmental data now demonstrates that the intensely variable climate that occurred globally between 2.5 million and 9000 BP played a defining role in human development, at the very least by limiting and shifting the habitable regions of the globe. The timing of the movement of Homo erectus out of Africa in association with the emergence of the Ice Age is too uncanny, for example, for these to have been coincidence. This needs to be sorted out more fully before proceeding with any discussion of human origins.

Pleistocene Era

Researchers since the 1950s have greatly revised our understanding of the Pleistocene era, a geological time period characterized by variable climate punctuated by extreme changes between colder and warmer weather globally. Analysis of numerous indicators, including measurements of oxygen isotopes in artic ice cores, vestiges of highly sensitive organisms in sea floor sediments, residue of tree and grass pollen from lake sediments, and even remains of climatically sensitive materials such as beetle remains and cave deposits (speleotherms), all demonstrate a trend toward global cooling during this period. This trend was reflected by steeper latitudinal climate gradients and increased seasonality and variability. The causes of global cooling are so complex and interrelated that they defy simple explanation. Potential factors include lithospheric plate motions, vertical tectonism, weathering reactions, fluctuating atmospheric CO2 content, volcanism, biologic evolution, changes in oceanic circulation, and cyclic variations in the earth's orbit around the sun. The geomorphic results have been spectacular, culminating in a series of ice ages that repeatedly covered as much as 30% of the land area with glaciers (Bloom 1998; 49). Since the reversal of the earth's magnetic field about 750000 years ago the planet has undergone at least seven phases of glaciation. Ice cores obtained from Antarctica indicate that cold prevailed for much of this period, especially during the last 400000 years. Sustained periods of cold climate were interspersed by much shorter warm periods known as interglacials. The pattern was clearly a global phenomenon as the same features are evident in the data obtained from ocean sediment cores in the tropics as they are from polar ice cores. Since around 400000 BP, the pattern has been broadly consistent. Each ice age ended rapidly and was followed by an interglacial lasting around 10000 years. The climate then slipped back into long sustained periods of glacial coldness, thus lending the temperature record a remarkable saw tooth appearance. (see chart)


As opposed to today, where sea water is evaporated and deposited on land as rain eventually to work its way back to the sea, Ice Age atmospheric moister was deposited on land surfaces as snow and gradually accumulated into ice sheets that at their peak in 27000 BP rose to more than 3km in altitude. In the northern hemisphere, where most of the planet's landmass is situated, the ice extended southward to form a line of glaciers extending from Chicago across the north Atlantic to Glasgow and Stockholm. At their greatest extent these massive ice sheets not only made higher latitudes much colder than today, especially during winter, but their great height meant that weather systems flowed around their fringes rather than northward across the artic basin in confluence with deep-water ocean currents. This had the effect of shifting all weather systems farther south. At the same time, as more and more sea water evaporated and became permanently deposited on land surfaces, the sea level plunged as low as 130m below current levels, exposing some 25 million km2 of coastal shelf. Neighboring regions such as Britain and Europe, Indonesia and Australia, Siberia and Alaska became linked through now submerged land bridges. These exposed coastal lowlands and land bridges formed passageways for human migration and survival during Paleolithic times. The extreme variability of the Pleistocene era needs to be emphasized. The interdecadal variance in temperature and its impact were some tenfold greater than today, rendering the Pleistocene climate immeasurably more demanding. Early humans and the life forms they depended on for survival had little choice but to adapt to a flexible and migratory lifestyle in order to survive.


During sustained periods of intense cold, areas such as Europe north of the Pyrenees, the North American plains, the Middle East, and the Sahara became extremely cold, arid and uninhabitable. Flora and fauna in these regions either migrated to more habitable environments or went extinct. Discernible patterns have emerged regarding which areas supported human life during these long periods of intense cold. Habitable regions included the more temperate lands near the equator such as central Africa, southeast China, Indonesia, Australia, and New Zealand, all of which show evidence of moderate cooling at worst. They also included coastal lowlands of the Mediterranean, Red Sea, Indian and Pacific Oceans, where the presence of the sea helped to moderate cold temperatures and furnished early humans with aquatic food sources. In addition, early humans came to inhabit extensive east-west trending regions of grassland and tundra in eastern Russia and southern Siberia. As difficult as this may be to comprehend, these regions were too distant from large bodies of water for ice sheets to accumulate. Archaeological remains indicate that they teemed with animal life, particularly large herbivores such as mammoths and reindeer, thus enabling populations of hunter gatherers to flourish. Lastly, even in the frigid cold of Europe various refugia, or isolated pockets of wetlands, sustained human and other forms of life in mountainous regions along the northern shore of the Mediterranean and the Balkans.



Global cooling, and with it a trend toward steeper latitudinal climate gradients and increased seasonality and variability, seems to have been the climatic trend through the Cenozoic era (65 mill.BP-present). The causes are so complex and interrelated that they defy simple explanation. Potential factors include lithospheric plate motions, vertical tectonism, weathering reactions, fluctuating atmospheric CO2 content, volcanism, biologic evolution, changes in oceanic circulation, and cyclic variations in the earth's orbit around the sun. The geomorphic results have been spectacular, culminating during the last 2.5 million years in a series of ice ages that repeatedly covered as much as 30% of the land area with glaciers. Even today, in what some refer to as "postglacial' time with excessive optimism) 10% of the land remains ice covered, including the entire continent of Antarctica and most of the larges t island, Greenland. We are living in an ice age although all 6000 years of recorded human history have been within the Holocene epoch, one of the numerous brief interglacial intervals when the extent of the ice cover has been reduced. (AL Bloom, Geomorphology a Systematic Analysis of Late Cenozoic Landforms (Prentice Hall, 1998), 49)


Burroughs, 26: the view of the ice age changed tremendously in 1950s with advent of new research methods -- tree rings, pollen records, ocean sediments and ice cores., known as proxy data, measurements of the properties of these sources provided new insights into the properties of climate change. The ability to drill cores from sediments from the bottom of the deepest ocean basins transformed the nature of the world around us.


Burroughs, 27: ocean sediments, ratio of oxygen isotopes in the calcium carbonate in the skeletons of the foraminifera living in the deep water. Changes in this ratio are a longer term consequence of how the isotope concentration of precipitation locked into the icecaps of Greenland and Antarctica. As the ice caps in the northern hemisphere grew the amount of o16 in the ice was proportionately greater than the amount of 018. The ratio of these oxygen isotopes in the ocean changed as the amount of ice rose and fell. These variations were reflected in the shells of foraminifera which formed using oxygen in the ocean. This means that changes in the ratio of o16/018 are a measure of the size of the ice sheets at high latitudes and hence indirectly of fluctuations in global temperatures.


During periods of sustained cold the effects of climate change were felt even in warmer regions such as equatorial Africa. Food resources which archaic humans depended on for survival diminished and populations accordingly declined, entering into genetic moments known as "bottlenecks". Eras of climatic intensity imposed extraordinary stress on human development, compelling archaic humans to adapt, by developing stone tools, for example, and by migrating.


Homo erectus, for example, migrated out of Africa via the Middle East around 1.2 million BP, and pursued an eastward trending route along the more temperate, exposed coastal lowlands of the Indian and Pacific Oceans all the way to China. This route was repeatedly utilized by early humans in following millennia. By 500000 BP a species known as Neanderthal migrated out of Africa into the Middle East and northward into Europe where they adapted to the harsh climate and survived as hunter-gatherers until around 30000 BP. Surviving primarily off large mammals these people enjoyed enormous stature (on average 30% larger than modern humans), tremendous body strength, and cranial capacity in fact larger than modern humans. Modern humans in turn appear to have migrated repeatedly out of Africa, first around 150000 BP, then around 74000 BP, and finally around 50000 BP.




Burroughs, 104: Principle underlying the mapping of genetic markers is that the difference in the frequency of the form of a gene in different populations is a measure of the time since these populations separated. This difference in frequency is usually termed the genetic distance and is best measured using the largest number of genes that is practically possible. Generally the genetic distance increases with geographical distance although physical barriers such as seas and mountain barriers complicate this measure. Molecular anthropologists learned to focus on those genes that are haplotypes, these occur in chromosomes or sequences of DNA that are haploid rather than diploid. Haploid chromosomes contain genetic information from only one parent whereas diploid chromosomes contain information provided from both mother and father in each generation. mtDNA from mother, y-chromosome passes down through male lineage.


Homo sapiens






















DNA analysis indicates that modern humans (Homo sapiens sapiens) originated around 200000 BP in the region of the African Great Rift. This is confirmed by the discovery of human remains in Ethiopia, dated to 160000 BP. Geologically this coincides with the penultimate era of glaciation that occurred from 330000-130000 BP. The period was characterized by extreme desiccation across much of Africa and probably led to widespread population collapse among archaic humans living in the continent at the time.


Through analysis of mitochondrial DNA obtained from females of various ethnic backgrounds, researchers have determined that all humans alive today descended from one female, commonly referred to as 'Eve', who lived approximately 7600 generations ago. Analysis of male Y chromosome samples obtained from throughout the globe reveals the existence of some 10 "descent groups" or haplotypes that presumably descended from a common male ancestor who mated with Eve. Eve, her hypothetical mate, and these 10 males were not the first, nor the only modern humans living in Africa at that time. Rather, these were the only people from a much wider population of modern humans whose progeny survived until today. Due to the challenges of intense climate change and variability, these elements also began to move about the landscape. Some 20 haplogroups have been identified based on lineage sequences in male Y chromosomes. One haplogroup moved southward in Africa to become the Khoisan or Bushman people, apparently the group most closely descended from the earliest modern humans. Others settled in the rain forests to become pygmies and others still, living in the grasslands north of the central African rain forest survived as Negroid elements who as Bantu speaking cultures came to dominate sub-Saharan Africa.


FOOTNOTE: [haplotypes vs. Haplogroups; Using what is called phylogenic networks or trees in which mutations are classified in hierarchical levels , it is possible to estimate relationships among lineages. Basal mutations are shared for clusters of lineages defined as haplogrooups whereas those at the tips characterize individuals.]


Most early modern human population remained in Africa, but some small portion of the population migrated to the Middle East around 150,000 BP. The remains of this culture have been found in caves at Skhuyl and Quafzeh in modern Israel, dated to 100000 BP, in close vicinity to Neanderthal settlements.




Both cultures utilized the same stone and bone tools and thrived on the same mixed food sources of shellfish, wild game, and grains, nuts, and fruit. The dates of these modern human settlements, 100000 BP, were obtained using thermoluminescence and electron spin resonance.


According to the data obtained from genetic mapping, however, this first migration ultimately failed, probably due to a prolonged phase cooling that set in around 100000 BP. When this era of advancing glaciation reached its minimum temperatures around 87000 BP the Middle East ceased to be inhabitable. Intriguingly, mtDNA research of dog chromosomes indicates that dogs separated from wolves at approximately the same time. Conceivably this genetic marker records the moment at which dogs began to cohabitate with humans, though the earliest actual evidence for this does not emerge until 14000 BP.


Human assemblages found on the Red Sea coast of Africa, dated to 125000 BP, combined with the evidence of genetic-mapping indicate that a second migration out of Africa occurred around 80000 BP, possibly as a result of dramatic sea level decline. As opposed to the first attempt at migration, elements of this migration successfully moved along the shores of the Red Sea, Indian Ocean and the Pacific, utilizing land bridges and narrowed seas to arrive in Australia by 60,000 BP, and Southeast Asia by 40-35,000 BP. The genetic evidence indicates once again, however, that many elements of this second wave -- apparently all those dwelling in regions west of Indonesia and east of Africa -- disappeared as well. Another dramatic cooling event, dated by ice cores to 75-70000 BP, and intensified possibly by the eruption of a super volcano, Mt. Toba in Malaysia in 71000 BP, appears to caused another mass extinction. Like Homo erectus, however, those modern humans who had successfully migrated beyond Malaysia to Indonesia, Australia and New Zealand appear to have survived. Genetic mapping of Y chromosome data indicates that a third migration out of Africa occurred around 55000 BP during a warming trend. This migration repopulated the Middle East and continued on through central Asia into Siberia by 40000 BP. These elements then diverged in separate directions. Some headed westward along the northern shores of the Caspian and Black Seas in to Europe, arriving around 40,000-35,000 BP. Others headed eastward through Siberia, China, and Mongolia to Beringia, where the existence of a land bridge enabled them to cross into Alaska and North American by 25000 BP. Other migrating elements independently moved eastward along the Indian Ocean to repopulate those areas abandoned during the earlier migration. This is the only viable explanation for the marked genetic divide that exists between people living today in east Asia, New Guinea, and Australia, and those living in India and farther west. This picture is complicated even more by genetic markers indicating that other humans descended from the time of the earlier migration in 84000 BP had by this time likewise made their way to China and Japan. These humans also migrated across Beringia into the Americas. Before this occurred, however, another glacial era descended on the planet between 35000 and 24000 BP.


Known as the Last Glacial Movement, or LGM, this final phase of the Pleistocene era represented the most intense period of glaciation in human experience. The millennia between 20000 and 18000 BP in particular represented a period of unrelenting cold throughout the planet, culminating in the 3km tall ice sheets mentioned above. In comparison with today's global ice cover of 30 million km3 the ice cover of the LGM was literally 3 fold, or 90 million km3. Sea levels plunged by 130m. The LGM appears to have wiped out the Neanderthal populations in Europe and unquestionably impaired the progress of modern humans as well. Fortunately, these latter populations were sufficiently well situated by this time, and adequately armed with tools and technologies to hunker down in their various regions of the world and survive.


Origins of Race

It is important to recognize that the bulk of the modern human population remained in Africa throughout these eras. This had an enormous impact on the way humans evolved. One researcher compared the repeated exodus of small groups of modern humans to the equivalent of removing the playing cards, 7, 8, and 9, from a deck of 52. Those populations that remained in central Africa, by and large thrived in its moderate climate, continued to mix their gene pool, and otherwise developed attributes of "complex societies." Already before 70000 BP (the period during which modern humans migrated as far as Australia), African cultures exhibited components of what is referred to as a "Paleolithic Revolution," including blade and microlithic technology, bone tools, increased geographic range, specialized hunting, exploitation of aquatic resources, long distance exchange networks, systematic processing of pigment, art and body decoration. Although the archaeological evidence for these attributes of modern human cultures does not occur in combination at any one place or time in Africa, the overall picture suggests that their packaging was assembled prior to the departure of migrating bands to distant continents around 84000 BP. These same attributes become manifested as rock art in Australia, cave art in Spain and France, a bone flute found in Germany (39000 BP), kiln-fired ceramic figurines in Moravia (20000 BP), kiln-fired pottery in Japan (14000 BP), and exotic grave good in the Middle East and Europe (dates?), the last mentioned demonstrating the existence of social hierarchy and trading networks.


Small groups of modern humans obviously carried these attributes out of Africa prior to their becoming isolated by insurmountable barriers of mountain, desert, glacier, and ocean, only to lose contact with one another for tens of thousands of years. What is more, the variability of the Pleistocene era with its repeated, sustained periods of intense cold inevitably reduced those populations that migrated out of Africa significantly. Fluctuations in human populations had a huge impact on the rate at which natural selection operated, leading to a phenomenon known as genetic drift. During genetic drift decline in breeding numbers induced changes in the genetic composition of an isolated human population. As population levels fell to very low numbers, simple chance allowed some genetic variations to spread through the surviving population in lieu of others that disappeared altogether. In such a situation, genetic drift or founder's effect influenced the genetic record of this group not so much through "survival of the fittest" as "survival of the luckiest." (Burroughs 139) Another theoretical outcome of widespread population decline was the occurrence of genetic bottlenecks (noted above). As human populations declined everywhere except Africa around 100000 BP, for example, those who survived would have found themselves dispersed into geographically separated groups. As populations rebounded tens of thousands of years later, each group started from what was essentially a separate genetic base. In Africa the DNA evidence indicates that these separated elements of modern humans continued to mix with one another as their populations expanded and merged. However, those handfuls of groups that migrated out of Africa inevitably colonized the rest of the world based in their particular group's unique genetic heritage. In essence they forged a genetic bottleneck out of which all non African based populations of modern humans ultimately arose.


It is generally assumed, for example, that such a bottleneck occurred around 80-70000 BP for the reasons given above. The genetic evidence indicates that the global human population crashed at this time to a maximum of 40000 people. The genetic lineage of the resurgent populations who began migrating around 50000 BP was inevitably different from that of earlier migrating humans. Climatically induced changes in their level of development are likely. Researchers mapping the mtDNA of human body lice have determined, for example, that the particular species of louse that infests human populations evolved at approximately the same time (70000 BP). Since the genetic lineage of this particular louse directly descends from animal lice, the evolution of human head lice is presumed to mark the moment at which modern humans began to fashion clothing from animal skins to keep warm.



SIDEBAR: Dogs, Fur, and Human Head Lice in the Americas

DNA evidence of head lice, two genetic lineates that separated ca. 1.2 million BP. This coincides roughly with the time when archaic humans, Homo erectus, first ventured out of Africa. These humans lived in East Asia until about 50000 BP, and the only way modern humans could have picked up their form of louse is by some social contact. The geographical distribution of the two forms of louse is also interesting. One is found on people all over the world, the other is almost exclusive to the Americas. This suggests that the modern humans that crossed Beringia into the Americas carried the form of louse that had survived for so long on our human cousins, Homo erectus. (Borroughs 133). For the DNA mapping of dogs, Borroughs 129; Mexican hairless dogs, Borroughs 215;



Over time the natural process of genetic mutation caused isolated populations to "adapt" in various ways, particularly in terms of their physical appearance. Geneticists and molecular anthropologists have determined, for example, that the genetic variants that determine skin color and facial features involve only a few hundred of the billions of nucleotides in human DNA, a genetically insignificant number. Two classes of melanin, red/yellow and black/brown, are present in the epidermal layer of human skin and hair. The spectrum of pigmentation observed in different geographic regions of the world is the result of varied production, distribution, and packaging of these two classes of melanin among long isolated populations. Those most exposed to strong sunlight, such as humans dwelling in African grasslands near the equator, needed to generate large amounts of melanin to defend their bodies against harmful UVA sunlight. The genetic "hard-wiring" of people in these regions led to the evolution of Negroid peoples who eventually came to dominate most of sub-Saharan Africa. As isolated elements of modern humans migrated into less sunny climates, however, their body chemistry's need for melanin diminished in inverse proportion to the need to generate Vitamin D from diminished sunlight, and thereby avoid diseases such as rickets. The genetic markers that controlled melanin production for these people inevitably 'relaxed," enabling mutations in the direction of lighter colored hair and skin. As a result, northerly situated humans acquired lighter, paler skin, lighter colored eyes, and reddish and blond colored hair.


Similar transformations occurred with respect to body size and proportion that affect human thermoregulatory response to varying climates around the world. Longer slender frames were more suitable to hot climates, whereas, stocky, thicker frames that retain body heat were more suitable to cold. Similar explanations have been made for the shape of the nose, width of nostrils, and texture of hair. The time required for adaptations such as these to take hold was hardly brief, perhaps as many as 500 generations, but neither was this necessarily long in archaeological terms. Theories about genetic drift and bottlenecks furnish, therefore, not only some sense of proportion to the scale of the migration that left Africa, but it also demonstrates that all other people of the world, regardless of their appearance, descended from one and the same human stock, however separated by time, barriers, and distance.


The Emergence of Human Settlements

During the LGM enormous changes in human populations took root throughout the globe. Homo erectus was already extinct before 50000 BP, though not before coming in contact with modern humans heading toward the Americas. Neanderthal culture likewise went into extinction around 30000 BP. In Europe three distinct Paleolithic cultures of modern humans are discernible: Aurevignian in southern France and Spain, Gravettian in the Balkans and Black Sea area, and Solutrean in the Pyrenees/Basque region. Thriving on food sources of large herbivores and positioning themselves along their migration routes. These cultures exhibited advanced levels of culture and social organization, as demonstrated by their magnificent cave art, highly perfected stone and bone tools, and body decoration. With the end of the LGM around 16000 BP and the trend toward warmer climate this rather hearty lifestyle was overturned as their food sources migrated northward or were hunted into extinction. Rapidly changing climate conducive to population rise around 10000BP anticipated the final transformation in human development, commonly referred to as the Neolithic revolution.


FOOTNOTE [Add to previous section - 80% european dna; 20% me dna in europe, aurevignian, gravettian, solutrean, etc.]


Neolithic Revolution


The driving force of the Neolithic revolution is identified with a dramatic shift in climate at the end of the Pleistocene era, something known as the Younger Dryas era that occurred 12900-9500 BP. Prior to this period, around 15-13000 BP a dramatic warming trend generated expanding vegetation and more abundant yields of wild fruit, seed, and game animals in many parts of the globe. These in turn altered lifestyles for several modern human populations. In Europe north of the Mediterranean this meant the emergence of vast forests that severely reduced the available grazing territories of large herbivores. Animals such as mammoths quickly went into extinction while others such as reindeer migrated further northward as glacial ice sheets retreated leaving tundra and grasslands in their path. Big-game hunter gathering as a lifestyle thus became threatened. The inhabitants of this region were compelled to radically change their diet from one dominated by reindeer to one dominated by forest-oriented deer, boar, and oxen. A likely indication of this is afforded by the genetic lineage of Basque, Celtic, and Finnish peoples, which has now been shown to be directly related. Apparently, at the end of the LGM, those populations surviving in the Pyrenees (today known as the Basques) migrated northward through France, Britain, Ireland, and Scandinavia following their animal food sources. Investigators theorized that this migration continued southeastward into the Baltic region of central Europe, thus imparting the ancient Celtic population with its uniquely dispersed pattern of settlement. Other peoples migrated into the region from the Black Sea region as well as the Middle East; however, it is significant to observe that some 80% of the contemporary population of Europe owes its descent to the peoples who migrated into the continent from central Asia around 40000 BP, whereas, only 20% can trace its genetic lineage to the Middle East.


In more temperate regions such as the Middle East, China, and South America formerly arid landscapes became remarkably lush in plants and small game. Hunter gatherers dwelling in these regions adapted to harvesting these resources out of necessity. For example, the Natufian culture in Syria and Israel, 14.5-12000 BP, (a new settlement at Abu Hureya in northern Syria around 13500 BP), left in their assemblages evidence of agricultural implements such as querns, pounders, pestles, mortars, and sickles made of bone and flint. This culture had clearly adapted to a sedentary quasi-agricultural lifestyle. The Natufians benefited from the fact that that cereals readily susceptible to domestication, emmer wheat, barley, and einkorn, existed naturally in the well watered foothills of this region, with areas of wild cereal vegetation extending in a great arc from Israel northward to Anatolia and southeastward to the Zagros Mts. of Iran. Since these cereals tend to yield heavier seeds and denser seed heads naturally through repeated cycles of sowing, growing, and harvesting, their domestication through simple use was all but inevitable. Repeated production of these cereals had the effect, moreover, of selecting grains that exhibited less tough husks around the kernel, making the grain more suitable to digestion and thus life supporting.


Similar evidence has emerged for rice production in China. Phytoliths (fossilized grains) of rice have been identified in archaeological contexts dated to 13,900 BP. In the Americas equally early evidence of human cultivation of plants such as squash is emerging for this time period. The changing climate combined with the disappearance of animal food sources that peoples in these regions had depended on for millennia appear to have forced adaptations toward sowing and harvesting. Another likely source of compulsion was the presence of growing hunter gather populations in the vicinity, thus eliminating the time worn option of migration. In previous millennia when wild plants and animals became scarce, foraging peoples simply moved to new locations. Finding ways to use the land more intensively may have been a better alternative superior to conflict with neighbors (Olson 99). The end result appears to have been a pattern of sedentism at least in specific regions, compelling archaeologists to reevaluate assumptions about the dawn of agriculture.


As rapidly as this era of warmer wetter climate emerged, however, climatic conditions abruptly 'flickered" for a brief moment, reverting back to colder, drier conditions for approximately two millennia (11500-9000 BP). Populations of hunter gatherers that had adapted to a more sedentary lifestyle in sensitive regions such as China and the Middle East were compelled to transport their subsistence strategies to adjacent areas less affected by cooler climatic conditions. Especially in areas where precipitation levels differ appreciably over short distances -- for example, northern Mesopotamia -- decreased annual yields of wild cereals and game animals would have compelled cultures with unsustainable populations, such as the Natufians, to adopt a strategy of deliberate cultivation. In essence, they carried their newly invented agricultural technologies with them as they moved. Some have argued that the dearth of evidence for agriculturally based sedentism during the Younger Dryas era possibly resulted from a reversion in settlement to coastal lowlands, where possible remains of agricultural communities now lie submerged below the sea. The speed with which agriculture emerged with climate amelioration after 10000 BP suggests, nonetheless, that the Natufians and other groups retained their knowledge of agricultural technology throughout the Younger Dryas period and reapplied these to their respective environments as climatic conditions improved


Around 10000 BP a very steep warming period occurred which ultimately stabilized into the climate we know today. Weather systems changed dramatically throughout the globe. For our purposes what was particularly noticeable was a progressive phase of dessification that emerged, extending along an east-west axis from the Sahara, Arabia, Mesopotamia, across northern India, central Asia, and Mongolia. Sea levels likewise rose with sufficient rapidity to compel people settled along coastal lowlands to move their camps and settlements to higher ground with each succeeding generation. Violent storms and 100-year floods would have generated storm surges of such proportions that they possibly induced traditions of flood myths world wide. In addition, island populations became increasingly isolated as land bridges utilized to migrate to these outlying land masses became submerged beneath the seas.


As populations reemerged in this era their dependence on agricultural technologies could not be more evident. Rising local populations rapidly consumed available resources from a hunter-gatherer perspective, and the rise of neighboring populations precluded the possibility of migrating elsewhere. In the near East agricultural settlements such as K. Shahir, Shanidar, and the Belt Cave in the Zagros Mts. began to extend along the highlands of the Fertile Crescent by 9000 BP. People migrating into the eastern Sahara adapted to a hunting strategy of capturing and domesticating Barbary sheep between 9-8000 BP. Evidence of the resumption of rice culture in the Yellow and Yangtze River basins in China occurs around the same time, and the adaptation to maize cultivation in Mesoamerica and bean culture in Peru occurred only slightly later, ca. 7000 BP. Many investigators observe that the domestication of plants and animals in the Americas was all the more remarkable, not only because the possibility that the inhabitants acquired this technology from without (and hence through a process of "diffusion") was non existent, but also because the food sources harnessed by native Americans hold minimal nutritional value in their natural state, and thus required greater manipulation as food sources. Maize for example requires deliberate, methodical efforts at cross-pollination to generate sufficiently large ears of corn to suffice as a food source. The emergence of agriculture in the Americans confirms not only that the timing of this adaptation world wide was linked to the arrival of modern climate, but also that the Native Americans were extremely ingenious with agricultural experimentation.


The timing of this development throughout the globe and its increasingly identified connection to global warming at the end of the Ice Age has prompted the observation that geographical determinism played a large role in the emergence of Neolithic cultures where they did. Eurasia, with its east-west trending geography lying principally in the northern hemisphere, allowed for the spread of those food resources most suitable for domestication -- cereals such as emmer wheat and barley, and animals such as pigs, sheep, goats, cows, -- to extend along a broad band from the Mediterranean to central Asia, this being the global area where they naturally occurred. In fact, two thirds of the 50-60 cereals and grasses that can be domesticated occur naturally somewhere in western Eurasia, whereas, only 6 grow naturally in east Asia, and only 2 in Australia and South America. Of the 14 domesticable animals that survive on the globe (out of a possible 148 species), nine resided in the Near East, whereas, only 1 (the llama) existed in south America, and none at all in North and Central America, Australia, or sub-Saharan Africa. The north-south trending alignment of Africa and the Americans played a role in this. Natural and environmental barriers prevented the spread of domesticable plants and animals along the lengths of these continents. Without human help animals simply could not migrate across extensive environmental terrain harmful to their survival. Moreover, from an agricultural standpoint progress in Africa and in other equatorial climates was impeded by obstacles such as poor soil conditions (owing to a lack of frost that selectively enforces dormancy on pests, parasites, and disease vectors and aids in topsoil formation) and labor-crippling diseases such as malaria. From an agricultural standpoint some regions of the globe have clearly been blessed with greater advantages in this regard than others.


Nonetheless, the highly Eurocentric character of archaeological research should not be allowed to disguise the fact that rising sedentism and adaptation to the domestication of plants and animals was a global phenomenon. As the modern climate took root, human elements worldwide were compelled to accept new subsistence strategies entailing sedentism. In this respect the decline in climatic variability played a formative role in the development more settled societies. Agriculture simply could not be achieved in a Pleistocene climate characterized by intense variability.




Farming in the foothills of neighboring mountains was largely dependent on patterns of rainfall, the limits of which tended to restrain carrying capacity. As soil nutrients became depleted, farmers tended to move to more productive terrain, by employing an environmentally destructive "slash and burn" strategy of land clearance. As sedentism took root unique confluences of resource, climate, and location enabled dense populations bordering on urban societies to develop. Two Ancient Near Eastern communities in particular vie for the title of the earliest cities on the globe, Jericho in Israel and Chatal Huyuk in Anatolia.


Jericho was situated below sea level in the extremely arid environment of the Dead Sea Valley where a large spring opens onto the valley furnishing a lush environment for wild grasses. Today it survives as a mound some 8m tall and 80m across. Elements of the Natufian culture first saw the advantages of this site but quickly abandoned it, probably during the coldest phase of the Younger Dryas. Around 8000 BC a permanent settlement of perhaps 12000 inhabitants developed on the site. Although they remained predominantly hunter gatherers they clearly experimented with agricultural production of wheat, barley, lentils, and chickpeas in the watered vicinity of the spring. The culling of male animals from herds (as indicated by remains of animal bones) points to the domestication of animals as well. The scale of this site and evidence of imported wealth (obsidian, turquoise, cowrie shells) clearly set Jericho apart from other communities emerging throughout the region. Their wealth and prosperity apparently earned the inhabitants unwelcome attention. Before 7000 BC they constructed a massive wall around their town some 3m wide at base, 4m tall, and 215m in circumference. At one end of the bastion stood a tower three stories tall. Surrounding the wall was a moat 9m wide and 10 ft deep. Although some have argued that the purpose of these structures was flood control, the location of this wealthy settlement, situated as it was along one of the main migration routes of the Ancient near East, appears to exposed it to repeated attacks of invaders, compelling its inhabitants to engage in the massive defensive construction that have survived. (Olson, 97)


Chatal Huyuk (7300-6200 BC) survives as a mound some 32 acres broad situated on the flat plain of the Anatolian plateau about 30km south of modern day Konya. To sustain themselves the estimate 5000-6000 inhabitants practiced cereal farming and sheep and goat herding as well as hunting in nearby plains. They constructed flat-roofed mud brick houses in tightly arranged circular rows that possibly offered a means of defense. Access to the houses was obtained through apertures adjacent roofs. Evidence of stone knapping seems to have been ubiquitous throughout the site, indicating that the inhabitants fashioned blades and tools from obsidian obtained from nearby mountains. Since these artifacts have emerged in archaeological assemblages as far removed as Israel, this activity seems to have played a formative role in the development of this community. Most significant among the archaeological findings is the widespread evidence of religion inside the dwellings. Clay figurines of female goddesses call to mind the Venus figurines of Gravettian culture. A shrine adorned with bulls' heads points to the existence of organized cultic activity.


Jericho and Chatal Huyuk offer crucial signposts to the transitions underway in Neolithic cultures. Sedentism and domestication of plants and animals enabled societies to develop into food producers as opposed to food gatherers. Food production inevitably led to surpluses capable of sustaining populations through fallow winter months; stable food supplies also enabled populations (or some elements thereof) to focus on activities unrelated to food production, such as obsidian production for export purposes at Chatal Huyuk. Other innovations such as weaving, ceramic production (wheel turned pottery by 6000 BC, metallurgy (copper tools by 5000 BC), rapidly followed. Theorists argue that several additional cognitive and physiological innovations occurred during this transition as well. Since a family of four consumes essentially a metric ton of grain/year the need for food storage facilities became similarly important and possibly helped to stimulate concepts of ownership and private property. Similarly settled agricultural existence arguably altered gender roles. Abundant food supplies and sedentary lifestyles possible raised levels of female body fat, thus shortening the time between pregnancies. Since increased pregnancies produced more labor for farm work this change was probably viewed as advantageous by emerging farmers. However, the evidence also indicates that it led to higher overall maternal mortality.


It remains important to recognize that the Neolithic Revolution marks a transitional phase in human existence, not an era. It occurred first in the highlands of Mesopotamia c. 9000-7000 BC. The technology then radiated outward to neighboring regions. It did not occur on the Nile River in Egypt until c. 5000 BC. The Indus/ Ganges River cultures adapted to agriculture c. 7-6000 BC, the Yangtze (Yellow) River settlements in (China) devised a rice-based agricultural technology independently c. 5000 BC. Rise of agriculture in Britain did not occur until 2000 BC; in Australia, 1000 AD. In South America, Neolithic culture emerged totally in isolation by 5000 BC. The date of this development would seem to point to necessity (possibly as a result of climate change) as the engine to human adaptation to agricultural technology world wide before 5000 BC. Bronze metallurgy arose by 3500 BC. Bronze Tools, in turn, facilitated riverine cultures consisting of large dense settlements




AL Bloom, Geomorphology a Systematic Analysis of Late Cenozoic Landforms (Prentice Hall, 1998


W. J. Burroughs, Climate Change in Prehistory: The End of the Reign of Chaos. Cambridge, 2005


J. Diamond, Guns, Germs, and Steel, The Fates of Human Societies, ny, Norton, 1997


Steve Olson, Mapping Human History: Genes, Race and our Common origins: Boston, NY, Houghton Mifflin/mariner, 2003


R. J. Wenke, Patterns in prehistory. Humankind's First 3 Million Years. 4th ed., Oxford, 1999