artist: Giovanni Caselli

Haplogroup L-161

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The long history of DNA Haplogroup L-161, now known as I2a1a2a

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A speculative extrapolation of the currently known facts

by J Danel






Oct 2016 under revision
(ver. 11)


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Introduction


W hen someone gets back the results of a DNA test that shows L-161.1 as the haplogroup, one of the first questions is what does it mean. One quickly discovers that it means he is in a subgroup of Haplogroup I, the main group defining Germans and Scandinavians. That is probably a surprise because the subjects male ancestors have probably been in Britain or Ireland as far back as is known.

Well, Scandinavians in Britain, eh? That means Viking ancestry, doesn't it? Sorry to disappoint. While for some subgroups of Haplogroup I it may mean that, but in the specific case of L-161, probably not. The L-161 group is very small. It is less than 1% of the population in general. So how did a tiny group of Germanic ancestry get to be widely dispersed throughout Great Britain and Ireland? I will try to answer that question.

Who were these people?

The original humans began almost 2 million years ago, eventually evolving into Neanderthals in Europe, Denisovans in Asia and early humans in Africa. About 250,000 years ago, people like us emerged and thrived in Africa. Their descendants spread out into Europe and Asia until the Mt. Toba eruption changed everything.

They survived the Mt. Toba volcanic eruption

The Mt. Toba eruption was the largest in the past 25 million years. It caused a centuries long "winter" and an enduring ice age that killed almost all the humans on earth. The survivors were a few modern humans, a few Neanderthals in Europe and a few Denisovans in Asia. Some humans in Europe and Asia held on for a while, but then later went extinct. The surviving haplogroups were A, BT, and CT, all located in Africa

They migrated Out of Africa to Europe and became the Cro-Magnons

The ice age after Mt. Toba lowered sea levels enough to allow Haplogroup CT to lead a small migration Out of Africa about 60,000 years ago. The track went across southern Arabia to the Tigris/Euphrates river and the Persian Gulf. There they found a well-watered paradise. The population expanded and more haplogroups emerged:, CT led to CF which led to F which led to IJ and I. Haplogroup I migrated north re-populating Europe and interbreeding with the Neanderthals. They came to be known as the Cro-Magnons. These people produced the famous cave paintings in Lascaux, France and the "Venus" figurines found from Spain to Siberia.
They are our ancestors. We are descendants of the Cro-Magnons and of the Neanderthals.

They survived the ice ages and migrated northwest to Doggerland

The Cro-Magnons flourished until driven out of northern Europe by the Late Glacial Maximum ice age about 25,000 years ago. Some haplogroup I took refuge in Ukraine. When the ice retreated, they migrated northwest to the productive lakes and marshes in Doggerland, an area three times the size of Ireland. Sometime before or during this migration, the SNP called L-161 developed.
  They enjoyed a comfortable mesolithic life in Doggerland for about 2,000 years. Then suddenly, with no warning, it was all over and most of them were dead. Three immense tsunamis wiped out most of the population in Doggerland and left it almost completely submerged. Other simultaneous events caused the climate to turn cold, sea level to abruptly rise 4 meters (13 ft.), and the food chain to collapse. There were only a few survivors. The whole catastrophe is called the "8.2 kiloyear event"

They washed up on the shorelines and spread to Ireland and Scotland

The few survivors of L-161 were split. One small group washed up on the shores of England becoming Isles A. They have remained in the British Isles ever since. Another group, Isles B washed up on the eastern shore and later migrated to Britain with the Bell Beaker folk. Isles B has since generated Isles C and D in Ireland.
  Isles A, Isles C, and Isles D are found almost exclusively on the northern and western fringes of Ireland and Great Britain, while Isles B is scattered more evenly across the whole area. This paper presents an explanation for that very peculiar distribution.

That is the very brief and over-simplified history of L-161.1

For more detail, I will start much further back, with the development of a creature called Proconsul.

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Table of contents


  • Introduction
  • Pre-Humans and Archaic Humans: "Lucy", H. habilis, H. erectus, H. heidelburgensis, Neanderthals
  • Modern Humans: Perry, Omo, Idaltu, Ice Age, Mt. Toba, Out of Africa, Mesopotamia, Haplogroup F
  • Haplogroup I: Repopulate Europe, Cro-Magnons, Neanderthal absorbtion, Aurignacian, Gravettian
  • P37, M423, and Y3104: Oldest Dryas ice age, Ukraine refugium, warming, Younger Dryas
  • L161: Founding near Moldova, migration to Doggerland, "8.2 ky event", near extinction, on Britain
  • Branching of the subclades: Isles A, B, C, and D
  • The current situation
  • Haplogroup List
  • Climate and Volcanic Event List
  • Tools of the Cultures
  • Geological Setting: Dinosaur extinction, Azolla event, planetary cooling, Proconsul, the apes
  • Timeline - significant events in the history of L-161

    (y.a. = years ago, ice ages, warm periods, Direct Ancestors of L161)
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    Our Pre-Human Ancestors


    Proconsul was about the size of a 1 yr. old child

    Our oldest known ancestor


    25 million y.a., there was a small primate known as Proconsul. Agreement that Proconsul may be our oldest yet known ancestor is not unanimous, but if it was not Proconsul, it was a creature very much like it. Proconsul was very small - about 10 kg. or 22 lbs.

    23 million y.a., End of the Oligocene - start of the Miocene Epoch, which extends from about 23 to 5 million years ago. It is roughly coincident with the timespan from Proconsul to the Australopicithenes.

    Branching off of the apes.
    Proconsul survived and evolved slowly* into larger primates. Now and then a group would branch off and go on a separate evolutionary path of their own. Monkeys branched off about 40 million years ago, long before Proconsul existed. We did not descend from monkeys.
    We all descended from Proconsul or from another creature very much like him.

    • 16 million y.a. - The Hylobates left, evolving into modern gibbons.
    • 14 million y.a. - The Pongo group left, evolving into modern orangutans.
    • 12 million y.a. - The gorillas separated.
    •  7 million y.a. - The Pan group separated, evolving into chimpanzees and bonobos.

    The speed of evolution

    Lucy was about 1,300 mm tall or roughly four feet. Proconsul was about 300 mm tall. Evolution has very, very slowly increased the height of these creatures by about 1,000 mm over a span of 20,000,000 years. That is about
    1 millimeter every 20,000 years.

    5.3 million y.a.: The Pliocene Epoch extends from 5.3 million to 2.6 million years before present. It is roughly coincident with the span from H. ardipithecus and H. australopithecus (the famous fossil "Lucy", disscussed below) to Homo habilis. It was a time of global cooling after the warmer Miocene. The cooling and drying of the global environment may have contributed to the enormous spread of grasslands and savannas during this time.

    5.3 million y.a.: Founding of Ardipithecus ramidus
    Ardipithecus was the first bipedal hominin and the first to begin to develop language abilities.
    5 million y.a.: Founding of the Australopithecenes
    Australopithecus generated several dead-end branches, but Australopithecus anamenis seems to have evolved into the A. afarensis that left us the famous fossil "Lucy".
    3.2 million y.a.: "Lucy", the famous Australopithecus afarensis
    It is thought the A. afarensis lived over a wide area in East Africa. Fossils and footprints have been found many places, but the best fossils were found in the Afar Region of Ethiopia. Some of them may have used the Lomekwi culture of stone tools found near Lake Turkana, Kenya. There is debate as to whether A. afarensis is actually a different species from the preceeding A. anamensis. If they are the same, then the date is pushed back to about 5 million years.
    2.5 million y.a.: Australopithecus africanus lived in southern Africa.

    Until recently, there has been no consensus that A. africanus is a human ancestor except for the convenient time located about halfway between A. afarensis and Homo habilis, but a very recent discovery of A. africanus fossils seems to support that placement.

    2.5 million y.a.: Australopithecus garhi lived in Afar, Ethiopia.

    A. garhi fits neatly into a time slot located about halfway between A. afarensis and Homo habilis and is from the same area.
    Variations on the family tree of Proconsul's descendants may be seen here.
    Proconsul
    Family Tree
    These differ mostly as to whether Ergaster and Erectus are the same and which came first. There are others.
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    Archaic Humans


    2.5 million y.a.: Beginning of the Paleolithic and the Pleistocene Epoch.

    2.3 million y.a.: Homo habilis, an ancestor of Homo sapiens lived.
    Homo habilis developed the Oldowan technology for making stone tools. Habilis lived in Africa and was possibly descended from Australopithecus africanus or A. garhi.
    Homo erectus
    1.9 - 0.07 mya
    1.9 million y.a.: Homo erectus (1.9–0.07 Mya) emerged in Africa and spread widely.
    He was an ancestor of Homo Sapiens. This was a very successful creature surviving over a broad range in Asia (Java Man, Peking Man), Europe, and Africa for almost 2 million years until as recently as 70,000 years ago. That date suggests the Mt. Toba eruption may have had a significant role in the demise of the Erectus.
    Descendants of Homo habilis

    • H. habilis (2.8–1.5 Ma),
    • H. erectus (1.9–0.7 Ma),
    • H. ergaster (1.9–1.3 Ma),
    • H. rudolphensis (1.9 Ma),
    • H. gautengensis (1.9–0.6 Ma),
    • H. georgicus (1.8 Ma),
    • H. antecessor (1.2–0.8 Ma),
    • H. heidelburgensis (0.7–0.2 Ma),
    • H. denisova (0.6–0.075 Ma),
    • H. neanderthalensis (0.5-.025 Ma),
    • H. rhodesiensis (0.4–0.12 Ma),
    • H. sapiens (0.35 Ma - present),
          and
    • Anatomically Modern Humans, (0.27 Ma)


    Undoubtedly there were many more.


    Erectus developed the Acheulian stone tool technology and used it for about 1.7 million years. They used spoken language and the ability to use fire. They had dark hairless skin, rich in melanin, and abundant sweat glands that evolved about 1.2 million years ago to regulate body temperature.
    1.5 million y.a.: Descendants of H. erectus
    We know of six more advanced species generated by Erectus during his reign. These are H. antecessor, H. ergaster, H. heidelburgensis = H. rhodesiensis, proto-neanderthals, the Red Deer Cave people, and the Omo people. Undoubtedly there were many more that are unknown.
    1.5 million y.a.: The Karymshina volcano in Russia erupted at a VEI 8 intensity.
    It was the fourth largest eruption in the last 2 million years. It undoubtedly has worldwide effects. The thinning of the numbers of H. erectus offshoots, e.g. H. georgicus, H. rudolphensis , etc. could have been caused by Karymshina.
    900,000 y.a.: The Zhamanshin impact in Russia.
    The largest impact in the last one million years is the 14-km Zhamanshin crater in Kazakhstan which has been described as being capable of producing a nuclear-like winter, but it was not sufficiently large to have caused a mass extinction.
    866,000 y.a.: Start of the Cromerian complex interglacial, a relatively warm period.
    The climate was generally warm, but the period is divided into three glacials and four interglacials, which are equivalent to Marine Isotope stages 13 to 21. Before this time it becomes very difficult to determine the dates of climate events with any accuracy.
    800,000 y.a.: Footprints left by H. antecessor
    Footprints left by a small group of people, including several children and one adult male, have been found at Happisburgh on the coast of Norfolk, England.
    700,000 y.a. Homo heidelburgensis or Heidelburg Man, emerged in Europe.
    The ancestor of Neanderthals, Denisovans, and modern humans, developed from Erectus in Europe and lived in a wide range across Europe from England to Asia. H. heidelbergensis could hunt herd animals that can run faster than a human, and this suggests that they had sophisticated hunting strategies, a complex social structure and developed forms of communication (language ability). H. heidelbergensis therefore already had intellectual and cognitive skills like anticipatory planning thinking and acting that so far have only been attributed to modern man. Some migrated into Africa where he later developed as H. rhodesiensis. (Modern science holds that H. heidelburgensis was geographically split into the European group and into the African group which is known as H. rhodesiensis. The two names are only geographical and do not refer to a different species.) It was the European branch that developed the Clactonian stone tool technology.
    600,000 y.a.: Clactonian stone tool technology developed.
    The European branch of Heidelburgensis improved on the Acheulean technology and developed the Clactonian technology that was later adopted by Neanderthals. Clactonian technology was used for over 300,000 years until it was replaced by the Mousterian technology developed by the Neanderthals about 160,000 years ago.
    500,000 y.a.: Proto-Neanderthals branched off from H. heidelburgensis.
    They colonized the middle east as well as Europe and part of Asia.
    488,000 y.a.: End of the Cromerian interglacial stage


    400,000 y.a.: Start of the Elster-Riss- Saale ice age glaciation (400 - 133 kya).
    The glacial coverage of Europe was even more extensive than during the later Weichsellian ice age. The areas where London and Amsterdam sit were under deep ice. The huge amounts of water tied up in glaciers dropped sea level and caused hyper-aridity in northern Africa. Migration into and out of Africa was blocked.
    400,000 y.a.: H. heidelburgensis in Africa differentiated into H. rhodesiensis.

    Later, modern man emerged in Africa, so the human ancestor was H. rhodesiensis
    .

    400,000 y.a.: The Proto-Neanderthals split during the severe Saale ice age.
    The western group became the Neanderthals who later shared Europe with, and learned the Clactonian stone tool technology from, Heidelburgensis. They colonized most of the colder parts of Europe that were not ice covered and parts of Asia. They survived until as recently as 25,000 years ago in southern Spain. Here is a listing and a map of the major sites.

    The eastern branch of proto-neanderthals developed into the Denisovans who went on to colonize Asia (and, later, inter-breed with humans).
    The timing of the division between Neanderthals and Denisovans and the extinction of the proto-neanderthals is very close to the start of the Elster-Saale glaciation. The ice pushed the populations south and split them, so then founder effect caused the separate evolution.
    Intelligence of the Archaic humans

    Homo erectus is estimated to have had an IQ of between 50 and 60, based on brain size and on tool making abilities. Modern humans have an IQ around 100. Over the past 2,000,000 years, we have gained 40 points. That is about 1 point each 50,000 years. That means we are only 6 points smarter than the early Neanderthals, 4 points smarter than the Omo people - the first AMH - and less than one single point smarter than the Cro-Magnons.

    A difference that small is very hard to measure.
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    Modern Humans


    280,000 y.a.: Haroharo Caldera of the Taupo volcanic zone erupts in a VEI 7 outburst, and then at 254,000 y.a. the VEI 8 of the Whakamaru eruption.

    270,000 y.a.: Perry's DNA suggests Anatomically Modern Humans, abbreviated AMH, were emerging 270,000 years ago
    This discovery has caused the geneticists to assign new names to the early haplogroups. Haplogroup A used to be the oldest, but now they have added A0 and A00. Haplogroup A00 probably developed from Rhodesiensis which is the same as Heidelburgensis.
    254,000 y.a.: Whakamaru Caldera of the Taupo volcanic zone erupts in a VEI 8, outburst.
    Two enormous volcanic eruptions occurred during the timespan that includes the AMH emergence. The eruptions were in the Taupo volcanic zone of New Zealand: 280,000 years ago Haroharo Caldera (VEI 7) and 254,000 years ago Whakamaru Caldera (VEI 8). Two such enormous eruptions had worldwide effects on the flora and fauna and on the evolution of humans. The volcanic "winter", lasting decades or even centuries would have pruned the family tree back to a few especially hardy and well-situated bands, so it seems very likely that 'founder effects', the driver of evolution, could have been a major factor in the emergence of the AMH.
    240,000 y.a.: Body Hair gene KRTHAP1 loss occurred 240,000 years ago

    220,000 y.a.: Puy de Sancy volcanic eruption in France
    This very large eruption in the heart of Neanderthal country had, no doubt, dire consequences on the Neanderhal populations in Europe. This ancient stratovolcano has become the highest mountain in the Massif Central of France.
    195,000 y.a.: The Omo people were living in Africa.
    Fossils 195,000 years old have been found at the Omo Kibish site in Ethiopia, the oldest AMH fossils found so far. Eventually it may be proven that these the founding Haplogroup A0 fossils. (Perhaps there should be a term Homo Omo for these people).
    190,000 y.a.: The first(?) of several migrations of modern humans from Africa
    They took the northern route across the Sinai. These modern humans colonized much of Eurasia during several of the long wet periods in the 20,000 year long North African climate cycle, leaving fossils that present intriguing questions about interbreeding and development of these early modern humans.
    185,000 y.a.: Modern(ish) humans were living in Misliya cave near Haifa, Israel.

    160,000 y.a.: Homo sapiens idaltu, modern humans, developed.
    Homo Sapiens
    Idaltu
    The fossilized remains of H. s. idaltu were discovered at Herto Bouri near the Middle Awash site of Ethiopia‘s Afar Triangle.
    These specimens are argued to represent the direct ancestors of modern Homo sapiens sapiens. They were AMH - Anatomically Modern Humans. They were not the knuckle-dragging stereotypes of 'cavemen', but were esentially just like us. There were some differences in their bones, their skin was brown, blonds were very rare, and blue eyes did not exist.

    Founded as Haplogroup A, continuing diversification of the gene pool led them through the sequential development of Haplogroups A1 and A1b.

    160,000 y.a.: Neanderthals develop the Mousterian industry in Europe

    133,000 y.a.: End of the Saale ice age. Beginning of the Eemian Interglacial Warm Period.
    The climate was warmer than the current climate. Forests reached as far north as Cap Nord, Norway and Oulu, Finland. Sea level rose 20 to 30 feet higher than today.
    133,000 y.a.: Start of the Abbassia Pluvial wet period in the Sahara
    It was a wet period that caused the Sahara and the Sinai to bloom with lush vegetation fed by lakes, swamps, and river systems. This unblocked the route north out of Africa. The route stayed open for 30,000 years. These wet cycles occurred several times and are the basis of the "Sahara Pump Theory" about how the earlier people were able to cross what is now a very harsh route out of Africa several times in relative comfort.
    130,000 y.a.: Migration of humans from Africa began via the northern route.
    The track was across the Sinai which was also benefitting from the Abbassia Pluvial wet period. These modern humans colonized much of Eurasia during the 30,000 year long wet period. Fossils have been found at the Qafzeh and Es-Skhul sites near Nazareth and Haifa in Israel and at Jebel Faya near Dubai dating to about 120 kya. They were probably Haplogroup A1 or A1b or even older haplotypes. The route stayed open for 30,000 years until the Weichselian ice age changed the global climate. Then the Sahara reverted to desert as a result of the retreat of the West African Monsoon southwards. The desert again blocked the northern route out of, and into, Africa. The Qafzeh/Es Shkul hominids had died out by 80 kya because of drying and cooling conditions of the Weichselian ice age.
    115,000 y.a.: The " Last Glacial Period ", the lethal Weichselian Ice Age began its advance.
    This long, extremely severe ice age drove all of the human settlements of the various earlier "Out of Africa' migrations to extinction. They left fossils, tools, and archaeological evidence, but no known surviving descendants except for perhaps a few hybrid Neanderthals in Europe and, in Asia, some Denisovans and H. erectus groups.
    Meanwhile, back in Africa:
    115,000 y.a.: Haplogroup BT emerged from Haplogroup A1b.
    100,000 y.a.: Haplogroup CT evolved from Haplogroup BT
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    Early Migrations from Africa and the
    Mt. Toba catastrophe


    The early migrations of modern humans from Africa were complete failures.*


    There were probably many early migrations out of Africa - Misliya, Qafzeh, Es-Skhul, Jebel Faya, and others yet undiscovered - but they all eventually failed. The extremely severe Weichselian ice age and the Mt. Toba eruption exterminated all the earlier migrants. They left fossils and archaeological sites, but no descendants except a few hybrid Neanderthals, Denisovans and a few Homo erectus.

    Beginning about 200,000 years ago small groups of Idaltu type people - Haplogroups A, A1, and A1b - began to find a way out of Africa. They moved out on the northern route across the Sinai as suggested by the "Sahara Pump Theory". The warm, moist conditions of "Abbassia Pluvial" type climate periods made that area much less formidible than it is today. It is not known whether the climate changes triggered the movements or just made it possible. These small migrations continued for at least 130,000 years. They spread to India and on to southeast Asia by 80,000 years ago.

    The competition and the struggle for survival may have been fierce and deadly. The space they were moving into was occupied by several varieties of genus Homo entrenched there, in some cases, for more than a million years. Homo Erectus still thrived, as did Heidelburgensis, Neanderthals, and Denisovans.

    Mega-fauna as food sources included: woolly mammoth, steppe mammoth, straight-tusked elephant, aurochs, steppe bison, Irish elk, equus, and Elasmotherium, but these are all large and dangerous to hunt with just primitive weapons such as spears and clubs.

    There were dangerous predators that hunted the migrants. These included: wolf, cave lion, cave bear, cave hyena, saber-toothed tigers, and giant polar bears among others. Other hazards would have included a new assortment of deadly germs, poisonous plants, insects, and snakes.

    Life for these pioneers would never have been very easy
    and then things got very much worse.
    115,000 y.a.: The " Last Glacial Period " began its advance.
    It is known in Europe as the Weichselian Ice Age. This long, severe ice age drove all of the human settlements of the "Out of Africa' migration to extinction.
    Meanwhile, back in Africa:
    As the 'abbassia pluvial' was phasing out and the ice age was phasing in, Africa experienced hyper-aridity because of the change in the monsoon flow and low sea levels because the water was tied up in glaciers.

    115,000 y.a.: Founder effects caused by the hostile climate may have resulted in Haplogroup BT emerging from A1b.

    100,000 y.a.: Haplogroup CT evolved from Haplogroup BT

    100,000 y.a.: Hyper-aridity enlarged the Sahara and blocked the northern route out of and back into Africa.

    Mt. Toba catastrophe

    It was the largest volcanic eruption of the last 25 million years


    75,000 y.a.: The Mount Toba eruption
    Mt. Toba
    VEI 8
    eruption
    A vast amount of ash and noxious gases (six gigatons of sulfur dioxide and 3,000 cubic kilometers of rock) were emitted, causing extinctions of food sources and centuries of famine.
    It was followed by a thousand year long cold period.
    The Mt. Toba eruption nearly caused extinction of Homo Sapiens. The number of humans was reduced to a very small population of between 1,000 and 10,000 breeding pairs, total, worldwide. Most of the few survivors were scattered from Ethiopia to southern Asia at an average population density less than one person per linear mile. The population reduction did not happen instantanouusly. Many surviving groups were well below the population threshhold necessary to survive in the ordinary course of events. Maintaining a tribal life and finding mates would have been very difficult, inbreeding would have been rife, so they slowly went extinct.

    The Mt. Toba catastrophe had major effects, not just in the near-extinction of the modern humans, but also on the populations of Homo Erectus. Homo Heidelburgensis, Neanderthals, Denisovans and other inhabitants of Asia and Europe. It may have been the final cause of the extinction of Homo Erectus and others of these groups.

    One ironic effect was that the populations of the large predators - saber-toothed cats, cave bears, etc. - were sharply reduced. Some went extinct. The smaller prey animals were also reduced, but in the new low-predator environment they rebounded quickly. Plants also quickly rebounded, taking advantage of the soil improvement by the volcanic ash. Food was abundant and the competition was low, allowing the following "Out of Africa"* migration to be resoundingly successful. Haplogroup CT, migrating from Africa, found itself to be the new 'Top Predator' in the new low-competition environment of southwest Asia.

    Repopulation of Asia and Europe began with the descendants of Haplogroup CT.*

    * The "Out of Africa" or "Recent African Origins (RAO)" hypothesis.

    Repopulation of Asia and Europe began with the descendants of Haplogroup CT. This is the current consensus about the repopulation of Europe and Asia. There are many other hypotheses. One is that some groups in southeast Asia, upwind of Mt. Toba, survived and that from there a migration to the west resulted in the modern human population of Europe and Asia and of Haplogroup E in Africa This could be called the "Out of Indochina" model. Another is that survivors everywhere all simultaneously evolved into H. Sapiens. It is called the "Multiregional" model. There are other models. This is a subject of great and heated argument.
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    Out of Africa


    70,000 y.a.: The main migration Out of Africa began via the southern route. The much lower sea levels, as much as 200 feet lower, during this time allowed the small groups to cross the Bab el-Mandeb Strait to Arabia.

    * The word 'invasion' drastically overstates the case. It was a small group or probably several small groups spread out over a considerable period of time. In an attempt to figure out how many individuals there might have been, the variation in mito-DNA was studied. The result suggests that there were only about 600 females who survived to be sucessful breeders, so the combined total size of all the groups would be about 2,000: 600 men, 600 wives, 500 other women, and say 300 children, many of whom would not live long enough to make an impact. A paleolithic paradise was still a brutal place.
    50,000 y.a.: The wet, warm climate of the Mousterian Pluvial was a favorable environment.

    Migration
    Out of Africa
    The much lower sea levels, as much as 200 feet lower, during this time allowed the small groups to cross the Bab el-Mandeb Strait to Arabia. Then they travelled through the warm and verdant "Green Arabia" or they followed the coastline eastward to the Persian Gulf and the Indus river. These modern humans colonized much of southern Asia.
    The early migrants were mainly Haplogroup CT. Several new groups quickly emerged and diverged from CT to become extremely successful in the bountiful enviroment:

  • C - most went to southern India, Indo-china, Indonesia, and Australia, but some went to Europe.
  • D - went to southern China and on to Japan
  • E - returned to Africa where E-P147 became the predominant haplogroup
  • F - the ancestor of L-161, took up residence in the the Ur-Shatt and Indus river valleys.
  • Migration of the Haplogroups
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    Haplogroup F


    65,900 y.a.: Haplogroup F, emerged from Haplogroup CF.
    Haplogroup F probably developed in the Tigris/Euphrates delta in the Persian Gulf or perhaps in the Indus River delta. In that part of the Weichselian ice age, the sea level was much lower, so the Persian Gulf was dry land to the south past the Strait of Hormuz.
    Migration to
    The Ur-Shatt
    The area is sometimes known as the Ur-Shatt, or old Shatt river valley. The area was a well watered plain surrounding fresh-water lakes. There were abundant resources to support hunter-gatherers.
    (SNP M89, defines Haplogroup F).

    ----

    Haplogroup F was very successful. Many small groups formed and migrated outward following the coast and the rivers. These groups evolved into 14 of the main haplogroups known today. Haplogroup F is ancestral to about 90% of non-African men worldwide.



    This "Grandfather's Path" graphic illustrates the route followed by the ancestors of L161 from the time Haplogroup F occupied the Persian Gulf about 65,000 years ago.




    55,000 y.a.: Haplogroup F, diverged through stages to Haplogroup IJ
    Haplogroup IJ was located somewhere in the northern end of the huge area occupied by Haplogroup F. Considering the dry climate, water resources would have been critical. They would have found good conditions in the area between the Tigris and Euphrates, now known as Baghdad. Groups G, H, and K branched off and are not ancestors of L-161.
    50,000 y.a.: The Mousterian Pluvial warm wet climate period began.
    50,000 y.a.: The Glinde and Moershoofd Interstadial warm climate period begins.
    Including the following Hengelo and Denekamp warm periods, there was a span of about 20,000 years of mostly good weather. Haplogroup I made good use of the time to repopulate most of Europe.

    Haplogroup I


    45,000 y.a.: Haplogroups I and J split from IJ in Persia or Kurdestan.
    The group that would become Haplogroup I went north and split going around both sides of Lake Pontus, the Black Sea in a fresh water phase. From there they re-populated Europe during the 10,000 year long Glinde-Moershoofd warm period. The timing was from from 50,000 to 39,400 years ago. (J spread from Kurdestan mostly to the south and west, populating the entire eastern and southern Mediterranean region.) There are still significant populations of subgroups of I and J remaining in Kurdestan. Here is a link to a map of the modern distribution of Haplogroup I. Kurdestan is at the lower right. (SNP M170 defines this group and is the key marker for the expansion of Cro-Magnons in Europe.)
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    Cro-Magnons


    45,000 y.a.: Cro-Magnons, an early group of Haplogroup I, colonized Europe.
    The distribution maps suggest that Haplogroup I1 - M253 went to the east of the Black Sea to the far north and then were driven back south (up the Rhine, down the Danube) into the Balkan Refugium by the return of the ice about 28,000 years ago.
    L-161 ancestors, the Cro-Magnons of Haplogroup I2- M438, went west of the Black Sea and north to the area that is now Ukraine and Moldova. From there, they populated most of Europe.

    Cro-Magnon

    Cro-Magnons were just like us
    except the genes for blond hair [11 kya],
    blue eyes [10 kya] and pale skin [18 kya]
    had not yet developed.

      The term Cro-Magnon does not have a real definition and has fallen out of favor. It is used generally to refer to Anatomically Modern Humans (AMH) or Early European Modern Humans (EEMH) with the SNP M170 dna marker using the Mousterian or Aurignacian technology before the Gravettian technology was developed about 30,000 years ago. They were not the stereotypical knuckle-dragging cave men. Their brain capacity was about 1,600 cc (98 cu in), which is larger than the average for modern humans


    50,000 y.a.: Cro-Magnons began arriving in the Caucasus where they met and mixed with Neanderthals. By 43,000 years ago, they had gone all the way to England.

    Archaeological evidence left by Cro-Magnons is spread over the entire continent:
    43,000 y.a.: Grotta del Cavallo in Liguria Italy.

    43,000 y.a.: Kent's Cavern in England

    42,000 y.a.: Pestera cu Oase cave in Romania .
    The cave is near the area of Lepenski Vir which is on the Serbian shore of the Danube. (The painting of Lepenski Vir at the top of the page is near the 'Iron Gates' on the Danube.) The fossils in this cave show admixture with Neanderthals up to 50%.
    40,000 y.a.: Mamontovaya Kurya in the Russian Arctic.

    38,000 y.a.: Cro-Magnons developed the Aurignacian stone tool technology. In many of the locations, there was evidence of occupation by both Cro-Magnons and Neanderthals, though perhaps at separate times.

    33,000 y.a.: Cro-Magnons domesticated dogs in Russia at the Kostyonki site.

    32,000 y.a.: Cave paintings dating from the Aurignacian at Chauvet Cave in France.

    and many others.
    39,400 y.a.: The Huneborg Stadial ice age or cold period began and lasted over 5,500 years.
    During the various ice ages, the conditions in northern Europe were too severe for primitive people to survive. They either died or were able to retreat to the south into areas of better climate.
    Refugia
    There were three such areas called "refugia": (1) the Ukraine refugium around the Black Sea, (2) the Balkan refugium along the Danube River and the Dalmatian coast, and (3) the Franco-Iberian refugium in Cantabria and the Aquitaine. Italy is blocked off by the Alps and so could not effectively function as a refuge. Further east was the Siberian refugium, but it is geographically reemoved trom our subject.
    39,000 y.a.: Campi Flegrei caldera volcano near Naples Italy erupted as a VEI 7.
    A decade of extreme cold weather as a result of the dust cloud may have been significant in the extinction of the Neanderthals. It was the biggest volcanic eruption in Europe in the last 200,000 years. (The Mt. Toba, 75 kya, and Mt. Thera, 3.5 kya, eruptions were much larger but were outside Europe).
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    Neanderthals


    When modern humans first encountered Neanderthals, it was the Neanderthals who had the advanced culture and the modern humans were the more primitive.

    The Cro-Magnons coming to Europe were using the very ancient Acheulean technology developed by Homo Erectus. The Neanderthals had developed and were using the more advanced Mousterian technology. After a few thousand years, the Cro-Magnons had learned the Mousterian from the Neanderthals and then used it for the next several thousand years. Eventually the Cro-Magnons improved the Mousterian developing the Aurignacian technology from (very roughly) 38,000 to 29,000 years ago and taught it to the Neanderthals. The Cro-Magnons spread the Aurignacian all across Europe.

    Neanderthals and Cro-Magnons shared Europe for less than 20,000 years. The estimates of total Neanderthal population vary from as many as 70,000 to as few as 3,000.

    50,000 y.a.: Neanderthals inter-bred and probably inter-married with Cro-Magnons
      Besides cultural exchange, things were sometimes more personal. DNA shows there was significant inter-breeding with Neanderthals near the Caucasus and all across Europe about this time. The result is that present-day humans of European stock have 1-4% Neanderthal DNA.
      We seek to understand how these two activities - the teaching of technology and the DNA exchange - happened. A number of suggestions have been made - rape, kidnapping, etc., but none of these would provide enough DNA to get to 4%. One reasonable explanation is that they may have been a result of exogamous, patrilocal marriage practices generally used by hunter-gatherers, including (as shown by archaeology, DNA studies, and the strontium ratios in Cro-Magnon female bones) the Cro-Magnons and Neanderthals. In this situation, Neanderthal brides would marry Cro-Magnon men and bring their knowledge of the Mousterian with them to live with their husband's family and teach them the better methods, and then the reverse. This was how the Cro-Magnons first learned the Mousterian and also how the Neanderthals later learned the improved Aurignacian technology. This hypothesis provides a workable mechanism for the cultural and DNA exchanges to have taken place.
    45,000 y.a.: Neanderthals taught the Mousterian to the Cro-Magnons

    Aurignacian
    and
    Cro-Magnon
    38,000 y.a.: Cro-Magnons developed the Aurignacian technology.
    The Neanderthals had developed the Mousterian technology and, in western Europe, were improving on it: there were localities in France using the advanced Chatelperronian and, in Italy, Uluzzian methods. These advanced styles did not spread significantly indicating isolation of the Neanderthal groups from each other. These advanced tool styles were far ahead of anything the Cro-Magnons had for the next 10,000 years until the development of the Aurignacian. Cro-Magnons taught the Aurignacian to the Neanderthals.
    37,000 y.a.: Date of the last find of a clearly Neanderthal site.
    The radiocarbon date is in dispute. It may be as recent as 24,000 years ago. The location is Gorham's Cave in the Rock of Gibraltar.
    24,000 y.a.: Neanderthals became extinct (or were fully absorbed).

    Neanderthal family

    A fictional, but probably realistic scenario is presented in Jean Auel's Earth's Children, an award-winning fiction series about a Cro-Magnon woman adopted into a Neanderthal tribe. An accompaniment to the Earth's Children books is Don's Maps a website by Don Hitchcock, an excellent and fascinating collection of source and resource materials related to the archaeology of the time.

    Neanderthal Marriages

    Consider this: 4% Neanderthal DNA means that 4 of 100 ancestors were Neanderthal. Those 100 ancestors would have made 50 marriages, with 4 of them having a Neanderthal partner. Fifty divided by four means one of every 12.5 marriages had a Neanderthal partner! (In the earlier phases of the repopulation of Europe, the ratio may have been even higher - as much as one in five. see below) If we accept Dunbar's number of about 50 for the normal size of a hunter-gatherer band, then two to five members of the band (all females, considering patrilocality) were Neanderthal. That is not rare at all, it is frequent or even commonplace. It was so commonplace that it raises a high probability that the reason the Neanderthals disappeared is that Cro-Magnons married all their women. The inescapable conclusion is:

    The Neanderthals did not go extinct;

    they were absorbed by the Cro-Magnons


    Neanderthal DNA

    It seems that the DNA percentage was much higher, perhaps around 10%, shortly after Cro-Magnons entered Europe. That would be equivalent to one marriage in five having a Neanderthal partner.
    The percentage has declined since then for at least two reasons. One is that continuing dilution from new migrants reduces the amount. Another is much more complicated. The DNA is eliminating itself. There may be several causes. The 'parts do not fit', so the DNA is selectively being eliminated. Or, there is evidence that there is some 'allergic reaction' that causes more spontaneous in-utero deaths. Or that the hybrids have low fertility. This is all under intense study and changes come almost weekly.


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    Gravettians


    30,000 y.a.: Gravettian culture and stone tool technology.
    (The term 'Cro-Magnon' is not used for people living after the Aurignacian.)

    The Gravettian was the culture developed from the Aurignacian.

    Venus Figurines

    People in the Gravettian period used nets to hunt small game and small pointed blades for big-game hunting (bison, horse, reindeer and mammoth). They are noted for their many carvings of 'Venus figurines'. The Gravettian was spread from Ukraine to Spain probably by Haplogroup I The area was so large that the culture developed a western version in France and an eastern version for Central Europe and Russia. In eastern Europe there is a long gap between the "end" of the Gravettian and the development of the Hamburg Culture. During that gap, the culture in use was the Epi-Gravettian.

    Northern Gravettian children

    28,000 y,a.: _End of the Denekamp warm period. The ice returned with a vengeance.

    27,500 y,a.: _ Haplogroup I2 - M438 developed in Anatolia or in the Ukraine refugium.

    26,500 y.a.: The Oranui (VEI 8) eruption of New Zealand's Taupo Volcano
    It was the world's largest known eruption in the past 70,000 years since Mt. Toba.(except perhaps Tierra Blanco Joven, about 500 A.D.). It may have been a significant contributing cause of the following Late Glacial Maximum (LGM).
    24,500 y.a.: Maximum ice coverage (LGM).
    All northern European populations were driven south where they survived living in "refugia". There were three main refuge areas: Ukraine, Balkan and Iberian. Mean Sea Levels are believed to be 110 to 120 meters (361 to 394 ft) lower than present.

    Life in the refugia

    Life in the refugia was probably very difficult in the over-populated areas that also had severe, but not lethal climates. All of the Rev. Malthus dire predictions may have prevailed. One would expect disease, starvation, and war, to result in what is called a Malthusian catastrophe. The catastrophe would return population to a lower, more "sustainable", level. The population was, in fact, drastically reduced by about 75%. Another expected outcome would be Founder Effects, which we see in the spread of the mutation causing pale skin.
    21,700 y.a.: I2-M438 split into subgroups L596 and L460 surviving the Older Dryas in the refugium.

    20,000 y.a.: End of the LGM.
    The very short Meiendorf Interstadial warm period began.
    The populations cooped up in the refugia broke out into open territory. Unfortunately, it was a climate trap. Only a thousand years later - about forty generations - the situation became very severe with the beginning of the Oldest Dryas ice age, the coldest and most lethal of all.
    20,000 y.a.: Haplogroup I2a1, called 'P37', originated from L460 in or near Ukraine.
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    P37 and the Oldest Dryas


    20,000 y.a.: Haplogroup I2a1, called 'P37', originated from L460 in or near Ukraine.
    Founded during the rather short (1,000 year) Meiendorf Interstadial warm period, various groups of P37 spread quickly westward up the Danube and north up the various Ukrainian rivers. The timing of the move north was unfortunate since the next climate change was a quick change to a very severe cold period - the Oldest Dryas - and they could not survive. Those who settled along the Danube all the way to France - P37-west - fared better because they were able to retreat to Iberia, the Franco-Cantabrian area, the Danube valley, and the Dalmatian coast to find refuge. Those who stayed in the Ukraine refuge - P37-east - dug in and held on. Those who went north - died.
    (SNP P37.2 defines this group)
    19,000 y.a.: Oldest Dryas ice age began producing a very severe cold climate
    The Oldest Dryas was the coldest and most lethal of the ice ages. A treeless "polar desert" 300 miles (500 km) wide developed across the entire width of Europe. It was similar to Arctic tundra. The onset of the cold was severe enough and fast enough that most of the northern populations perished before they were able to migrate south to the refugia. It was the second major extinction period in human history. Total population was reduced by more than 75%.
    18,300 y.a.: Vesuvius erupted at VEI 6 magnitude making a very bad situation worse.

    18,200 y.a.: Haplogroup M-423 , emerged from P37 in the Ukraine Refugium.

    18,000 y.a.: The few survivors all retreat to the various refugia
    The extreme climate lasted for almost 4,000 years. In the refugia, once again the Malthusian catastrophe played out. FTDNA suggests the Oldest Dryas was a major extinction period. The Haplogroup I population was reduced to just eight haplotypes. This, of course, led to major 'founder effects' .
    18,000 y.a.: One of the founder effects was the development of the genes for pale skin
    It is the mutation of two genes - SLC24A5 and SLC45A2 - that leads to depigmentation. (These genes are different from the genes that cause Albinism: OCA1, OCA2, and OCA3). Pale skin originated in a subset of the population in the refuge. The small groups that went north out of the refuge at the end of the Oldest Dryas contained a large percentage of this pale skin subset. The trait spread slowly throughout the population.


    L460 subclades, the descendants of M438
    I2-M438 and its several descendant subclades L460, M223, M26, P37, and M423 survived the extreme climate of the Oldest Dryas in the Ukraine refugium, in the Balkan refugium, in protected valleys along the length of the Danube and in the Ibero-Franco-Cantabrian refugium.




    17,800 y.a.: 'Alpine' branched off P37-west in the Danube basin. West Isles, and "France" were some of the other splinter branches.

    16,000 y.a.: Vesuvius erupted at VEI 5 magnitude

    15,500 y.a.: 'Western' emerged from P37-west in the upper end of the Rhine or Danube.

    14,670 y.a.: End of the Oldest Dryas ice age

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    M423


    Most of modern Haplogroup M423 descendants are in the Balkans. Another 10% is spread out over eastern Europe. These groups are shown as the yellow tracks in the diagram. The tiny remainder are the Disles and L161 Isles haplogroups in Britain, shown as the green line.

    18,200 y.a.__ Haplogroup M-423 , emerged from P37 in the Ukraine Refugium.
    The founding was during the last millenium of the Oldest Dryas ice age, so it must have happened in a refugium. About 90% of modern Haplogroup M423 is in the Balkans. The other 10% is spread out over eastern Europe, with traces in western Europe and the Isles. (These groups are shown with yellow boxes and arrows in the diagram below). There is some disagreement as to whether it was the Balkan refugium or the Ukraine refugium. It could have been either one, but the complexities of getting the P37 up the Danube to found M26 in western France and then get M423 back down the Danube to found the Dinaric and Y3104 is a very complicated scenario. The simple scenario is that P37 was spread out over both the upper Danube and the Ukraine refugium at the same time.

    Distribution of M423, Haplogroup I2a1b

    15,500 y.a.: 'Western' emerged from P37-west in the upper end of the Rhine or Danube.

    14,670 y.a.: End of the Oldest Dryas ice age;
    the Bølling-Allerød interstadial, began.
    The warm, moist period, the Bølling-Allerød, only lasted 1,750 years. Of the two periods, Bølling and Allerød, the Bølling is the warmer and came on more suddenly. Although the duration was quite short, the impact was immense: sea level rose about 35 m (!) due to glacial melt and also to the drainage of Lake Bonneville. Ice uncovered large parts of north Europe and temperate forests covered Europe from 29 deg. to 41 deg. north latitude. During this time, late Pleistocene animals quickly spread northward from refugia: reindeer, horse, saiga, antelope, bison, woolly mammoth, wooly rhinoceros, red deer, and smaller animals, such as fox, wolf, hare and squirrel. They were immediately followed by hunting groups that, over the next thousand years, developed the 'Hamburg' reindeer hunting culture. Today it is commonly accepted that the Hamburgian, featured by "Shouldered Point" lithics, is a techno-complex rooted in the Magdalenian. The Magdalenian was brought north by people migrating north from the Franco-Iberian refugium. The people migrating north from the Ukraine refugium, our ancestors the M423, were still using the Gravettian or Epi-gravettian culture. There was cultural intermixing involved in the development of the Hamburg culture, as would be expected.
    14,500 y.a.: M26-Sardinian branched off from P37-west in eastern France

    14,000 y.a.: Post-glacial re-population of Southern England began

    13,800 y.a.: Y3104 branched off from M423

    13,500 y.a.: Hamburg / Ahrensburg culture was established in the north German plains.
    The 'Hamburg (a nomadic reindeer hunting culture) evolved into the similar Ahrensburg culture and stone tool technology. The earliest archaeological find of bow and arrow artifacts is in the Ahrensburg. Ahrensburg culture is normally associated with the Younger Dryas glacialization and the Pre-boreal period.
    Donsmaps has an excellent writeup on these ice age hunters.
    13,350 y.a.: the relatively mild Older Dryas cold period lasted a brief time.
    Glacial Lake Candona drained to the North Atlantic. This surge of meltwater to the North Atlantic 13,350 years ago is believed to have triggered the reduction in thermohaline circulation and the short-lived Northern Hemisphere Intra-Allerød cold period, e.g. the Older Dryas.
    13,000 y.a.: L621-Dinaric branched off P37-east, perhaps near the Danube delta.

    12,900 y.a.: _The Younger Dryas little ice age began abruptly.
    There is evidence that it was perhaps caused by a collision with a comet, and compounded by one of the drainages of Lake Agassiz and by the eruption of the Campi Flegri supervolcano. The sharp cold lasted 1,300 years, but was not as severe as the Oldest Dryas. Some small groups were able to 'winter through' and survive in small villages as far north as Hamburg Germany. Most, though, were driven back into or near the refugia. I show Y3104 as being just north of the Ukraine refugium during the Younger Dryas after having been further north on the plains. England was depopulated during the Younger Dryas.
    12,000 y.a.: Campi Flegri erupted at VEI 6(?) magnitude

    11,660 y.a.: End of the Younger Dryas
    marks the
    11,660 y.a.: End of the Pleistocene and the
    11,660 y.a.: End of the Paleolithic.
    11,660 y.a.: Roughly correlated with Bond Event 8

    11,660 y.a.: Beginning of the Boreal climate period
    From the end of the Younger Dryas, the glaciers have been in retreat. It was the beginning of the Boreal climate period with a climate similar to today's.
    11,660 y.a.: Beginning of the Mesolithic
    The difference between the paleolithic and the mesolithic is based on their technology and lifestyle. Paleolithic peoples used crude stone tools made by chipping and lived nomadically in crude shelters and caves. In the mesolithic, better stone tools were shaped and polished by grinding, pottery was coming into use, and some permanent housing structures were built.
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    Haplogroup L-161


    11,660 y.a.: Beginning of the Mesolithic

    11,600 y.a.: As glaciers retreated, M423 migrated north from the Ukraine Refugium.
    The Don, the Dniester, the Dnieper, the Vistula, the Volga, and the Prut - all these rivers would lead northward allowing these migrants to reach the shores of a huge freshwater lake called Lake Ancylus (the Baltic Sea in a freshwater phase).
    11,200 y.a.: Haplogroup L-161 currently known as I2a1a2a branched off from M423 or Y3104.
    The founding location was somewhere between Lake Pontus (the Black Sea in a freshwater phase) and Doggerland. The founding was in the Boreal normal climate phase, so the geographic possibilities for the location are numerous. There were five major river deltas in that area, so the environment for hunter-gatherers was ideal.
    (SNP L-161.1 defines this group)
    L-161 moved westward along the shore of Lake Ancylus and into Doggerland, a huge marshland three times the size of Ireland where the mesolithic lifestyle was relatively easy. They participated in developing and using the emerging mesolithic Maglemosian culture and stone tool technology.

    Doggerland, a mesolithic paradise

    11,000 y.a.: The Maglemosian culture was established around the shores of Lake Ancylus
    and westward across Doggerland. The Maglemosian lasted 3,000 years until the catastrophic "8.2 kiloyear event".
    11,000 y.a.: Vesuvius erupted at VEI 4 magnitude

    11,000 y.a.: The hair color gene MC1R causing blond hair developed in northern Europe.
    There are several other gene variations that cause blond and other colors of hair that occur randomly across the entire world.
    10,000 y.a.: A genetic mutation caused blue eyes.
    This was a unique event affecting the OCA2 gene occured in one woman, resulting in blue eyes. This unique gene is transmitted mitochondrially. All blue-eyed people have this woman as an ancestor.
    9,000 y.a.: Post-glacial re-population of Ireland began in Cork across a landbridge
    Several subgroups of Haplogroup I2a coming north from the Iberian refugium would have been among the pioneers to cross the landbridge as the ice retreated.
      
    In the Irish legends about the arrival of various groups in Ireland, there were always people present before the immigrants arrived - similar to the 'discovery' of America when natives were already there. In Ireland those 'natives' would be the Fomorians of legend. They were subgroups of Haplogroup I2a who had come north from the Iberian refugium crossing the short-lived landbridge to Ireland about 10,500 years ago.
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    L-161 and the Doggerland Disaster


    Haplogroup L161 was living an easy life in Doggerland, Resources were abundant and the mesolithic methods provided a good living. It was almost paradise. Then, with no warning at all,
    it was all gone and most of them were dead. The 8.2 kiloyear event was not just one event, but are nine separate catastrophic events forming a 600 year long series of disasters.
    The '8.2 kiloyear event' series was:

    • the drainage of Lake Agassiz, which raised sea level 3 meters and triggered
    • three major Storegga tsunamis
    • a change in ocean currents caused by the drainage.
    • a VEI 6 eruption of Mt. Vesuvius.
    • a 400 year long cold period caused by deviated ocean currents and the Vesuvius eruption
    • collapse of the food chains, both land-based and freshwater
    • mass starvation and
      near (98%) extinction
    This is correlated with
    Bond Event 5
    8,200 y.a.: _The 8.2 kiloyear event
    The dreadful sequence began with the drainage of Lake Agassiz which caused sea level to rise 2 to 4 meters (7 to 13 feet) over about thirty days. The rising sea flowed back into Lake Ancylus, changing it from fresh water into the saline Littorina (Baltic) Sea. The climate abruptly turned cold and stayed cold for 400 years. The entire food chain collapsed.
    8,200 y.a.: Storegga landslide tsunamis and Flooding of Doggerland.
    There were three main tsunamis over a 200 year span. The shoreline waves were estimated to be over 100' high (32 m.). In Scotland, traces of the tsunami have been recorded, with deposited sediment being discovered in Montrose Basin, the Firth of Forth, 50 miles (80 km) inland. These were much larger in scale, scope and fatalities to the devastating 2004 Indian Ocean earthquake and tsunami. Many northern Haplogroups show evidence of a major 'population bottleneck' event at just this time. Haplogroup L161 shows evidence of a very severe 'population bottleneck' event at exactly this time - with a 98% extinction rate. The '8.2 ky events' are the 'Mt. Toba' of northern Europe, so it must be a major factor in that extinction.

    Similar events happened simultaneously around the world. Lake Pontus was flooded to change it from a fresh water lake to the saline Black Sea. The Ur-Shatt valley was flooded with salt water to become the Persian Gulf. The freshwater food chain collapsed leading to famine among those shore dwellers that survived the flood. (Some suggest these events are the inspiration for Noah's flood stories worldwide).

    Disaster in Doggerland



    The simultaneous timing of the population bottleneck and the 8.2 kiloyear disasters is very strong evidence for concluding that L161 was in Doggerland - no other explanation is available as to why that extremely severe bottleneck happened exactly then. Without such an explanation, we can rule out the various other suggested migrations of L161 to Britain: with the Celts, the Anglo-Saxons, the Halstadt people, or with the Cord-ware people, etc. Furthermore, there are essentially no traces of L161 in the original locations of these other people - Celts, Saxons, etc. The idea of bringing 100% of the Isles AB-S2639 population along from these areas, leaving no traces behind, is very difficult to accept.)
    8,200 y.a.: The few survivors of L-161 were forced south
    The splitting
    of L-161
    There were remaining dry parts of Doggerland still formed a landbridge near what are now the Dogger Banks in the North Sea. Southeast of there, the Rhine river came out of Europe and joined the Thames as they both flowed far south to the Atlantic ocean.
    8,000 y.a.: Vesuvius erupted at VEI 6 magnitude

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    Recovery


    Haplogroup L161 had been living an easy life in Doggerland until the "8.2 kiloyear event" almost exterminated them. The few survivors washed up on the shorelines to recover: Isles A and some Isles B on the west, the rest of Isles B on the eastern shore of what are now the North Sea. A very few L-161, Y13331(?), were left behind along the route of migration.
      The recovery was helped by the arrival of the especially warm climate of the 'Atlantic' period. It was impeded by the cultural isolation caused by the open water barrier of the English Channel.
    8,000 y.a.: Kongemose culture was developing in Doggerland.
    The survivors of the 8.2 kiloyear event took that culture with them. With the shoreline resources devastated, they concentrated more on hunting red deer, roe deer and wild boar with stone axes and spears. The microlith tools that were made on the continent are very reminiscent of those made along the English shoreline - hypothetically - by the L-161 survivors. English technology did not advance until the neolithic revolution about 6,500 y.a.
    7,500 y.a.: Pale skin became ubiquitous in northern Europe


    7,500 y.a.: The Atlantic climate period began, warmer than the present.(7,500-5,000 y.a.)

    7,000 y.a.: Haplogroup S2639 formed and spread east-west along the shoreline.
    S2639 quickly developed two main subgroups Isles A Y12072 and Isles B L1498. The continuing rise of sea level caused a continued migration that split the people of S2639.
    6,800 y.a.: Isles B - L1498 emerged and quickly generated three new branches.
    These groups, Y12993, A10029 and Y3749 were located along the south shore of the North Sea. This abrupt proliferation is indicative of a benevolent environment. The south shore during the Atlantic climate period would have been just such a place.
    6,800 y.a.: Isles A - Y12072 emerged from S2639.
    Isles A, in stark contrast, did not produce a single surviving branch for 3,700 years. This is indicative of a very hostile environment keeping the whole population on the edge of extinction the entire time. It is not clear why East Anglia would have been so hostile. Starting from a very small population base, perhaps just one man or a small family, operating in a competitive tribal situation might have been the cause.
    6,500 y.a.: The English Channel opened, becoming an open water barrier and splitting Y3749.
    Sea level continued to rise which changed the geography. The English Channel, previously not much more than a swamp - passable with some difficulty, but passable - became a serious open water obstacle. Britain became isolated. Haplogroup Y3749 was split by the new obstacle. Those on the east side became S2742 and those on the west became Y3722 around 6,400 ybp.
    The splitting of Y3479 provides a date the English Channel opened: 6,800 - 6,400 ybp.
    Previous estimates cover a span of about 3,000 years, but this genetic split seems to nail it down to a time after the 6,800 ybp founding of Y3749 and before the 6,400 ybp founding of the subclades S2742 on the east side and Y3722 on the west side.
    6,500 y.a.: Mesolithic / Neolithic transition on the continent.
    In an astonishingly short period of about 200 years all the mesolithic groups adopted an entirely new way of life involving keeping domestic animals, cutting hay to feed the animals, ability to milk the animals, pottery to hold the milk, the ability to make cheese, and many other things known as the "secondary products revolution". By natural selection, Lactose tolerance begins to evolve among dairy herders. The whole cluster of advances is lumped together as the "neolithic revolution. The blazing fast speed of the transition was perhaps aided by exogamous patrilocal marriage practices in which the bride took her dowry of a calf and the knowledge of dairy practices and pottery making to her new husband's home.
    6,500 y.a.: Alghaffar branched off a remnant of L-161, perhaps back in the Ukraine refugium
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    The Isles Groups in Albion


    6,500 y.a.: The Mesolithic / Neolithic transition happened very slowly in Albion.
    The major obstacle presented by the newly opened English Channel seems to have sloweded the new ideas from crossing and quickly making a successful foothold as they had done elsewhere. The Kongemose-like mesolithic culture stayed in use alongside the neolithic improvements in farming for another thousand years.
    6,000 y.a.: Farming and stone circles introduced into England
    Stone
    Circles
    The farmers were genetically similar to Iberians. It is thought they were haplogroup I who migrated north from the Iberian refugium. The stone circle 'religion', if it was one, remains a mystery. Stone circle construction seems to have started in northern England coastal areas and progressed southward along the west coast.
    5,370 y.a.: TMRCA of continental group of Isles B
    TMRCA = Time to Most Recent Common Ancestor
    5,000 y.a.: End of the Atlantic very warm climate period


    Stonehenge


    5,000 y.a.: Construction began at Stonehenge
    The Windmill Hill culture, perhaps an "East Anglian tribe", began construction of the immense Stonehenge complex and the other nearby sites: Woodhenge, Durrington Walls henge, and the connecting pathways, etc.
    Stonehenge and the end of the Atlantic Period

    The timing of the ending of the Atlantic warm period with the simultaneous beginning of construction of Stonehenge with is striking. Surely that can not be coincidental. The cooling would have led to many adjustments to their lifestyle. There may have been crop failures, game reductions, and obvious weather changes that could have sparked a resurgence of religious fervor in an attempt to appease the gods and stop the changes. The immense amount of labor that went into Stonehenge must have had some serious motivation far beyond the ordinary course of events.

    Construction continued for just over a thousand years. It ended coincident with the arrival of the Bell Beaker folk who caused a 97% replacement of the Y haplogroups building the site and who also brought a complete change of culture and religion.
    4,800 y.a.: Mt. Pleasant henge was constructed in Dorset

    4,740 y.a.: TMRCA of the Isles B British group

    4,700 y.a.: The start of the Bell Beaker invasion and the very short Chalcolithic.

    4,500 y.a.: Bronze Age began in Britain, copper mining in Cork and tin mining in Cornwall

    4,500 y.a.: Lactose tolerance dominant throughout Europe

    4,500 y.a.: Domestic horses in Britain brought by the Bell Beaker folk.

    4,300 y.a.: Eruption of Hekla 4 Volcano (VEI 4) in Iceland. "Ireland was thirty years waste".

    4,200 y.a.: Bond Event 3, glaciers increase worldwide.

    4,050 y.a.: Seahenge constructed in Norfolk, the last gasp of the old religion?

    3,800 y.a.: Vesuvius erupted at VEI 5 magnitude

    3,630 y.a.: Eruption of Mt. Thera (VEI 7) in Santorini Greece.
    Geologists think it may be the strongest explosion ever witnessed by modern humans.
    The 'Avelino' VEI 6 eruption of Mt. Vesuvius occurred around the same time. Both caused catastrophic environmental problems known as the '1627 BC events'.
    3,400 y.a.: TMRCA of Isles CD - Y3734

    3,350 y.a.: King Tut ruled in Egypt

    3,200 y.a.: Isles C-Y5450 branched off from Y3722(Y3734) in the Dal Riata area.

    3,200 y.a.: Isles D-Y4660 branched off from Y3722(Y3734) in Ireland, perhaps near Rathcroghan

    3,000 y.a.: Eruption of Hekla 3 (VEI 5) in Iceland
    There was an 18 yr. temperature drop in the northern hemisphere.
    2,800 y.a.: The Iron Age began in Britain

    2,200 y.a.: TMRCA of Isles C - Y5450
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    500 Years of Catastrophe




    2,000 y.a.: The beginning of a 500 year long series of catastrophies.
    All Europe suffered. The population dropped by 25% from 36 million in 200 AD to 27 million in 500 AD. It took another 500 years for the population to climb back to what it was in 200 AD. It seems clear that the subgroups of L161 were not spared. The TMRCA of Isles C and D indicate some fairly serious bottlenecking. Isles A was very close to extinction.
    2,000 y.a.: Small invasions by the Angles, Saxons, Jutes, and Danes began and continued for 500 years.

    1,973 y.a.: The Roman invasion and conquest (43 AD) under the Emperor Claudius began a 350 year long series of rebellions and guerilla warfare.

    1,937 y.a.: The VEI 5 eruption of Mt. Vesuvius (79 AD) caused crop failures as well as burying Pompeii.

    1,850 y.a.: The Antonine Plague and Britain's Great Plague.

    1,750 y.a.: The Plagues of Cyprian and Aurellian wreaked havoc for 20 years.

    1,600 y.a.: The Roman withdrawal (410 AD) left a power vacuum that was soon filled by the invading Angles, Saxons, Jutes and Danes.

    1,500 y.a.: TMRCA of Isles D - Y4660

    1,500 y.a.: Main Anglo-Saxon invasion. - Cerdic the Saxon became King of Wessex
    The invasions were propeled by some frigid years of crop failure - a result perhaps of the TBJ volcanic eruption (next pagagraph). The slave trade flourished selling native Britons (including Isles B) to the European continent. This could account for most of those rare Isles B individuals found there. In 577 AD, Cerdic's great-grandson Ceawlin completed the Saxon conquest of England with his victory at the battle of Deorham (in the suburbs of Bristol). (If you are of British stock, Ceawlin is your approximately 40th great-grandfather.)
    1,500 y.a.: The enormous Tierra Blanco Joven - "TBJ" eruption
    The eruption of the Ilopango volcano in El Salvador had disasterous effects killing millions worldwide. New findings would make it the second-largest volcanic eruption in the last 260,000 years (After Mt. Toba, VEI 8 - 73 kya, and tied for second/third place with the Oranui eruption, VEI 8 - 26.5 kya, and the Whakamaru eruption, VEI 8 - 254 kya, of New Zealand's Taupo volcanic zone,.
    1,500 y.a.: Bond Event 1.

    1,500 y.a.: AD 536 Events" caused two decades of famine.

    1,500 y.a.: The Plague of Justinian killed at least 25 million Europeans
    950 y.a.: TMRCA of Isles A - PF4135
    The 500 year long series of catastrophies from 2,000 to 1,500 years ago drove Isles A to the brink of extinction as is shown by the shockingly low TMRCA of 950 years.
    By 500 A.D. there may have been only three families of Isles A left alive. They were located in the area of Cork and Bantry Bay in southern Ireland. The three families were the A13364, the Y11772, and the A11374. The most successful group was A13664 who made Cork their home and there they prospered, becoming the famous and powerful Driscolls. Y11772 developed two subgroups that migrated north, Y12075 and A11115. Y12075 successfully established a home in Scotland. A11115 went to the Isle of Man, Northern Ireland, and Scotland. All the A11374 seem to have migrated to America. One individual of A11115 settled in Wiltshire, south of Bristol, England. His great-grandson emigrated from Bristol to Virginia in 1635 so that group is now, so far as we have evidence, extinct in the British Isles, but there are about 50 individuals in the US.
    ----------------------- Page 20 ----------------------
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    The current situation


    Haplogroup L-161 is a tiny group that comprises less than 1% of the European population. It is found predominately - more than 95% - in the British Isles. For that reason, the label "Isles" has become attached.

    The branches of Haplogroup I that have led to the modern L161 subclades are:

    M170—I
     ⤷—➤ M438—I2
    ——— ⤷—➤ P37—I2a1a
    ————— ⤷—➤ M423—I2a1a2
    ——————— [⤷—➤ Y3104 —I2a1b2 removed by ISOGG 2018, retained by Yfull ]
    ———————⤷—➤ L161—I2a1a2a
    —————————⤷—➤ S2639—I2a1a2a1 —Isles AB
    —————————————↓  ⤷—————➤ Y12072 I2a1a2a1b ➤ PF4135 - Isles A I2a1a2a1b1
    ————————————— ⤷———————➤L1498 - Isles B I2a1a2a1a
    ——————————————— ⤷—➤ Y3734 - I2a1b1a1a1b3
    —————————————————↓  ⤷—➤Y5450 - Isles C - I2a1b1a1a1b3a
    ————————————————— ⤷———➤  Y4665 - Isles D - I2a1b1a1a1b3b


    Isles A is concentrated around Cork and is present, but rare in Ireland, Isle of Man, and Scotland.
    Isles B is now found all across the British isles and to a very minor degree on the continent.
    Isles C is located mostly in the north of England, Scotland, Ulster and western Ireland.
    Isles D is relatively strong in the northwestern parts of Ireland, especially around Rathcroghan.


    The I Group as a whole has a very different current distribution. Most are in Europe sandwiched between Haplogroup R1a on the east and R1b on the west. It is not at all clear how that came to be. There are many diverging opinions

    Predominant European Haplogroups

    ----------------------- Page 21 ----------------------
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    ---------------------- Page 22 ---------------------

    Climate, Culture, and Volcanic Events


    Climate  from  to  Name  Y Haplogroup  Culture
    cold  2.6  2.4  Pre-Tiglian complex  Homo habilis  Lomekwian
    cold  1.8  1.6  Biber glaciation Eboronian  Homo erectus  Oldowan
    ....VEI 8  1.5 .  Karymshina Russia VEI 8 eruption .  Acheulean
    warm  1.4  1.1  Biber-Danube interglacial . .
    cold  1.1  866  Danube glaciation . .
    warm  866  676  Danube-Gunz interglacial  Homo antecessor  Acheulean
    cold  676  621  Gunz glaciation  H heidelburgensis  Acheulean
    warm  600  540  Gunz-Haslach interglacial . .
    cold  540  500  Haslach glaciation  Proto neanderthals  Clactonian
    warm  500  478  Haslach-Mindel=Cromerian interglacial . .
    cold  478  424  Mindel Glaciation  Proto-neanderthals .
    warm  424  347  Holstein=Mindel-Riss Warmzeit  H rhodesiensis  Acheulean
    cold  347  230  Riss Saale; split proto-neanderthals  A00, "Perry" .
    ....VEI 7  280 ..  Haroharo Caldera VEI 7 . .
    ....VEI 8  254 ..  Whakamaru Caldera VEI 8 . .
    cold  230  133  Saale = Riss  A0, "Omo" .
    ....VEI 7+?  220 ..  Puy de Sancy volcano in France VEI 7+?  A, Neanderthals .
    warm  130  115  Eemian Interglacial  A, Homo idaltu .
    warm, wet  133  100  Abbassia Pluvial in the Sahara  CT .
    cold  115  50  Weichselian ice age  CT - F .
    ....VEI 8  75 ..  Mount Toba, largest eruption in 25 million yr.  CT .
    warm  50  41.3  Glinde and Moershoofd Interstadial  F - I .
    warm  41.3  39.4  Hengelo Interstadial  I, Cro-Magnons  Acheulean
    cold  39.4  34  Huneborg Stadial .  Mousterian
    ....VEI 7  39 ..  Campi Flegrei (1) caldera VEI 7 .  Aurignacian
    warm  32  26.5  Denekamp interstadial  I2  Gravettian
    ....VEI 8  26.5 ..  Oranui VEI 8  I2a .
    cold  26.5  20  LGM - Last Glacial Maximum  P37 .
    warm  20  19  Meiendorf Interstadial .  Epi-Gravettian
    cold  19  14.7  Oldest Dryas,   (major extinction event)  M423 .
    ....VEI 6  18.3 ..  Vesuvius (1) VEI 6  M423 .
    ....VEI 5  16 ..  Vesuvius (2) VEI 5 .  Magdalenian
    warm  14.7  12.8  Bolling-Allerod interstadial  Y3104  Hamburg
    cool  13.7  13.5  Older Dryas . .
    ....VEI 6  12.9 ..  Lacher See VEI 6 . .
    cold  12.8  11.7  Younger Dryas  L161  Ahrensburg
    ....VEI 5?  12 ..  Campi Flegrei (2) VEI 5? . .
    normal  11.7  8.2  Boreal climate  L161  Maglemosian
    ....VEI 4  11 ..  Vesuvius (3) VEI 4 . .
    cold  8.2  7.8  The 8.2 kiloyear events  S2639  Kongemose
    ....VEI 6  8 ..  Vesuvius (4) VEI 6  S2639 .
    warm  7.5  5  Atlantic climate  Y12072, L1498  Mesolithic
    dry, warm  5  2.5  Subboreal climate .  Chalcolithic
    ....VEI 4  4.3 ..  Hekla 4 VEI 4 .  Bronze Age
    ....VEI 5  3.8 ..  Vesuvius (5) VEI 5 . .
    ....VEI 7  3.5 ..  Mt. Thera (Santorini); "1623 bc events"  Y5450, Y4665 .
    ....VEI 5  3 ..  Hekla 3; "Bronze Age Collapse"  PF4135 .
    normal  2.5  now  Subatlantic climate .  Iron Age
    ....VEI 5  1.9 ..  Vesuvius (6) VEI 5; buried Pompeii . .
    ....VEI 7+  1.5 ..  Ilopango 'TBJ'; "Migration Period" in Europe  A13664, Y11772  Y12075, A11115
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    Haplogroup List

    Pre-human
    Ancestor Emerged Location, approximate Name
    "Ardi" 5.5 mya Afar, Ethiopia Ardipithecus ramidus
    "Lucy" 3.2 mya Afar, Ethiopia Australopithecus afarensis
    "Africanus" 2.5 mya South Africa Australopithecus africanus
    "Garhi" 2.5 mya Afar, Ethiopia Australopithecus garhi

    Archaic humans (ice ages, warm periods)
    Ancestor Emerged Location, approximate Name
    Handy man 2.5 Olduvai Gorge, Tanzania H. habilis
    Upright man 1.9 Java, Kenya, China, Hungary H. erectus
    Heidelburg man 700 kya Germany, Spain, England H. heidelburgensis
    Rhodesian man 600 kya Zambia, Ethiopia, Tanzania H. rhodesiensis =
    H. heidelburgensis

    Modern humans - AMH
    Haplogroup Emerged * Location, approximate SNP SNP Date
    A00a Perry bef. 270 Western Cameroon L1149 270
    A0-T bef. 200 Omo Kibish, Ethiopia L1085 "Omo?" 235.9
    A1 170 Afar Ethiopia P305 H. sapiens idaltu 161.3
    A1b 150 East Africa P114 H. s. sapiens 133.4
    BT 140 Ethiopia M91 130.7
    CT 100 East Africa M168 88
    CF 80 Ur-Shatt P143 68.5
    F 70 Ur-Shatt M89 65.9
    GHIJK 65 Mesopotamia F1329 48.8
    HIJK 60 Mesopotamia F929 48.5
    IJK 55 Mesopotamia L15 48.5
    IJ 50 Baghdad M429 47.2
    I - Cro-Magnon 45 Kurdestan M170 42.9
    I1 40 Ukraine refugium M253 27.5
    I2 40 Anatolia M438 27.5
    I2a1a** 25 Ukraine refugium P37.2 18.7
    I2a1a2** 20 Ukraine refugium M423 18.5
    I2a1a2** 15.8 Ukraine refugium Y3104 (L161, L621) 13.4
    L161.1 (I2a1a2a*) 13.5 Moldova L161.1 (S2639, Y13338/1) 10.6
    Isles AB  (hg tree) 10 Doggerland S2639 6.9
    Isles A 7 East Anglia ➤ Cork Y12072 ➤ PF4135 ➤ Y12073(A2) ➤ Y19285 6.7
    Isles B 7.2 Rhine River Delta L1498 ➤ Y3749 ➤ Y3722 ➤ Y3734 6.6
    Isles C 6.5 Dal Riata Y5450➤ Y18393(C1) & Y5451(C2) 3.4
    Isles D 4.2 Rathcroghan Ireland Y4660(D) ➤ Y5280 3.2

    * The 'emerged' date in this table is my estimate of the date the "Dunbar group" began its journey to separation. It is the date of the 'spark' that started events moving forward. That date must be, by definition, before any archaeologically or genetically calculated dates. The SNP dates are from www.yfull.com

    ** The alphanumeric designators for haplogroups are listed by the ISOGG and are subject to change every year, so they are useless over time. The actual SNP name does not change, so that is the preferred designator.

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    Timeline


    (y.a. = years ago, ice ages)

    250,000 y.a.: Anatomically Modern Humans begin to develop. 195,000 year old fossils found at the Omo site in Ethiopia [54]
    110,000 y.a.: The "Last Glacial Period" begins and lasts until about 10,000 y.a. with warmer interludes [34]
    70,000 y.a.: Mount Toba VEI 8 eruption nearly causes extinction of Homo Sapiens [49]
    ooa
    f
    cro-magnon
    nean
    43,000 y.a.: Homo Sapiens occupied Kent's Cavern in Devonshire England
    32,000 y.a.: Weichsellian
    interstadial warm period begins. Humans spread farther into the north and west.
    30,000 y.a.: M170 - Haplogroup I founded southeast of the Black Sea [Map of Human expansion]
    30,000 y.a.: Gravettian culture (30,000 - 20,000 BC) spread from Ukraine to Spain perhaps by M170 - Hg I,
    28,000 y.a.: M253 - I1 founded probably in the Ukraine Refugium
    26,500 y.a.: Oruanui VEI 8 eruption [51] Largest eruption since Mt. Toba. Cause of LGM?
    26,000 y.a.: Maximum ice coverage (LGM). Population living in refugia
    25,000 y.a.: Neanderthals extinct [52]
    21,500 y.a.: M438 - I2 founded probably in the Ukraine Refugium
    20,500 y.a.: L460 - I2a(M223) founded probably in the Ukraine Refugium
    20,000 y.a.: End of LGM
    . Post-Weichsellian warm period begins, allowing populations to occupy parts of Europe
    20,000 y.a.: P37 - I2a1 founded, in or near the Ukraine refugium, spread quickly westward (up Danube?).
    19,000 y.a.: Oldest Dryas ice age [40] begins, severe cold producing a treeless Europe similar to Arctic tundra
    18,000 y.a.: FTDNa suggests major extinction period reducing haplogroup I population to just eight haplotypes
    18,000 y.a.: Surviving populations retreat to the various refugia
    17,800 y.a.: Alpine branches off P37 - west in the Danube basin
    15,800 y.a.: M423 - I2a1b branched off P37 - east in the Ukraine Refugium
    15,500 y.a.: Western branched off the P37 - west in the upper end of the Rhine or Danube or France
    14,670 y.a.: End of Oldest Dryas ice age
    ; the Bolling-Allerod interstadial, a warm, moist period begins abruptly [35]
    14,500 y.a.: M26 - Sardinian branches off P37 - west in southern France
    14,000 y.a.: Post-glacial repopulation of Southern England begins
    13,500 y.a.: L161 - I2a1b2 branches off M423, perhaps near the Black Sea [1]
    13,000 y.a.: L621 - Dinaric branches off P37 - east, perhaps near or north of the Black Sea
    12,800 y,a,: The Younger Dryas little ice age begins lasting 1,300 years
    11,660 y.a.: End of the Younger Dryas
    11,660 y.a.: End of paleolithic
    and beginning of mesolithic. [48] Beginning of Boreal warm period.
    10,600 y,a,: L-161 branches off from M423 somewhere in northern or eastern Europe
    9,000 y.a: Post-glacial repopulation of Ireland begins in Cork [13]
    8,200 y.a.: Storegga Slide tsunamis and Flooding of Doggerland [2][3][4]
    7,500 y.a: Atlantic climate period begins, warmer than the present.(7,500-5,000 y.a.)
    6,700 y.a.: Isles B branches off from Isles AB, probably in Doggerland
    6,700 y.a.: Isles A branches off from Isles AB, probably in Essex
    6,500y.a.: English Channel opened - Isles B on the east and Isles A on the west
    6,500 y.a: Mesolithic / Neolithic transition - The "secondary products revolution" [12]
    6,500 y.a: Alghaffar branches off L161 - East
    6,200 y.a.: Isles C branches off from Isles CD in the Northern England-Scotland-Ulster area?
    6,200 y.a.: Isles D branches off from Isles CD in Ireland, perhaps near Rathcroghan [33]
    6,000 y.a: Farming introduced into England
    5,370 y.a: TMRCA of continental group of Isles B derived from Bronze Age traders?
    5,000 y.a: End of Atlantic very warm climate period
    5,000 y.a: Windmill Hill culture-East Anglian tribe (Isles B?) begin constructing Stonehenge [6]
    4,800 y.a: Mt. Pleasant henge constructed in Dorset (by Isles B?) [5]
    4,740 y.a: TMRCA Isles B British group
    4,500 y.a: Bronze Age begins in Britain [32], copper mining in Cork [11] and tin mining in Cornwall
    4,500 y.a: The horse domesticated in Britain [31]
    4,300 y.a: Eruption of Hekla 4 Volcano in Iceland. "Ireland was thirty years waste".
    4,050 y.a: Seahenge constructed in Norfolk (Isles B? or Isles A?) [7]
    3,000 y.a: Eruption of Hekla 3 in Iceland - 18 yr. temperature drop in the northern hemisphere, probable famines.
    2,800 y.a: Iron Age begins in Britain
    2,730 y.a: TMRCA of Isles C
    2,520 y.a: TMRCA of Isles D
    1,850 y.a: The great Antonine Plague [20][21]
    1,750 y.a: The Plagues of Cyprian and Aurelian - 20 years of plagues [24]
    1,500 y.a: TMRCA of Isles A
    1,500 y.a: Anglo-Saxon invasion, slave trade flourishes [10]
    1,480 y.a: Plague of Justinian [8] , TBJ [9] erupts. "AD 536 Events" [16] Two decades of famine.
    1,450 y.a: The near-extinction and diaspora of Isles A

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    Tools of the cultures




    Oldowan tools


    (early paleolithic)

    used in Africa by

    Homo habilis

    and perhaps by

    Australopithecus

    2.6 - 1.7 ma


    Acheulian tools

    (early paleolithic)

    used in Asia, Europe, and Africa by

    Homo erectus and Cro-Magnons

    1.8 ma - 100 kya


    Mousterian tools

    (middle paleolithic)

    used in Europe and the Middle East by

    Homo heidelburgensis,

    Neanderthals, and

    Cro-Magnons


    600 - 40 kya


    Aurignacian tools

    (upper paleolithic)

    used in Europe by

    Neanderthals and Cro-Magnons

    38 - 29 kya


    Gravettian tools

    (upper paleolithic)

    used in Europe by the

    EEMH of Haplogroup I

    Gravettian: 30 - 22 kya,
    Epigravettian: 22 - 14 kya


    Hamburg / Ahrensburg tools

    (upper paleolithic)

    used in northern Europe by

    Haplogroup L161

    14,000 - 11,000 ya


    Maglemosian tools

    (mesolithic)

    used in Doggerland and northern Europe by

    L161 and Isles AB

    11,000 - 8,000 ya


    Kongemose tools

    (mesolithic)

    used on North Sea shoreline by

    L161 and Isles AB

    8,000 - 7,200 y.a.


    Neolithic tools

    used by

    Isles B

    after 6,500 y.a.


    Bronze Age tools

    used in Britain and Ireland by

    Isles A, B, C, and D

    after 4,500 y.a.
    ----------------------- Page 25 ----------------------
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    Table of Contents


    1. Cover
    2. Introduction
    3. Table of Contents
    4. Pre-Humans
    5. Archaic humans
    6. Modern Humans
    7. Early migration from Africa
    8. Out of Africa
    9. Haplogroups F to I
    10. Cro-Magnons
    11. Neanderthals
    12. Gravettian Culture
    13. P37 and the Oldest Dryas
    14. M423
    15. L-161, our ancestral haplogroup
    16. Doggerland disaster
    17. Recovery from disaster
    18. Isles haplogroups in Albion
    19. The Bell Beaker invasion
    20. 500 years of catastrophe
    21. Current situation
    22. Climate, Culture, and Volcanic events
    23. Haplogroup list
    24. Timeline
    25. Tools of the cultures
    26. Misc Notes
    27. Geological Setting

    Illustrations

    Grandfathers
    Path
    Doggerland
    16,000-8,000
    y.a.
    Storm in
    Doggerland
    8,200 y.a.
    Lepenski
    Vir site
    9,000 y.a.
    Bell Beaker
    Invasion
    4,700 y.a.
    Stonehenge
    5,000-3,500
    y.a.
    P37 and
    subclades
    migration
    M-423 and
    L-161
    migration
    Three
    Refugia
    Main
    Haplogroups
    in Europe
    Aurignacian
    range
    47-41 kya
    Neanderthal
    range
    50 kya
    Anglo-Saxon
    Invasion
    400-600 AD
    Proconsul
    family tree
    (Boaz)
    H. sapiens
    family tree
    (Mara et al)
    Australopithecus
    afarensis

    Lucy, 3.2 mya
    Lucy
    reconstruction
    H. erectus

    1.9 mya
    Neanderthals 400 kya
    Homo Sapiens
    Idaltu

    160,000 y.a.
    Cro-Magnon

    45,000 y.a.
    Gravettians

    30,000 y.a.
    Venus
    Figurines
    25 kya
    Out
    of
    Africa
    Haplo
    routes
    Lakes and
    rivers in
    Green Arabia
    Migration
    to the
    Ur-Shatt
    H. sapiens
    family tree
    (Stringer)
    Homo sapiens
    family tree
    (Reid)

    Keyword Index


    Keywords

  • Abbassia Pluvial
  • Acheulian tools
  • Ahrensburg culture
  • Anglo-Saxon Invasion
  • Apes
  • Archaic humans
  • Atlantic Climate Period
  • Auel, Jean
  • Aurignacian culture
  • Australopithicene
  • Azolla event
  • Balkan Refugium
  • Black Sea
  • Blond hair
  • Blue eyes
  • Bølling-Allerød
  • Boreal Climate Period
  • Bottleneck
  • Branching of the Isles subclades
  • Bronze Age
  • Cave painting
  • Chicxulub
  • Clactonian tools
  • Climate and volcanics
  • Cro-Magnon
  • Cultures:
  • Dal Riata
  • Denisovan
  • Dinaric
  • Disles
  • Doggerland
  • East Anglia
  • Eemian warm period
  • English Channel
  • Eocene
  • Eocene extinction
  • Eruptions:
  • Farming reaches Britain
  • Fomorians
  • Franco-Iberian Refugium
  • FTDNA
  • Geological Setting
  • "Grandfathers Path"
  • Gravettian Culture
  • Hamburg culture
  • Haplogroup list
  • Haplogroup A00
  • Haplogroup CT
  • Haplogroup F
  • Homo habilis
  • Homo erectus
  • Homo erectus' descendants
  • Homo heidelburgensis
  • Homo neanderthalensis
  • Homo rhodesiensis
  • Homo sapiens idaltu
  • Homo sapiens Omo
  • Haplogroup I
  • I1
  • Haplogroup I2
  • Haplogroup I2a
  • I2a1
  • I2a1b
  • I2a1b2
  • I2a1b3
  • Ice Ages:
  • Idaltu
  • Intelligence of Archaic humans
  • Iron age
  • Isles AB
  • Isles A
  • Isles B
  • Isles C
  • Isles D
  • King Tut
  • Kongemose_culture
  • L161
  • L233
  • L460
  • L621
  • Lactose tolerance
  • Lake Agassiz
  • Lake Ancylus
  • Lake Pontus
  • LGM: Last Glacial Maximum
  • Lepenski Vir
  • Lucy
  • M26
  • M170
  • M423
  • M438
  • Maglemosian culture
  • Megaliths
  • Mesolithic
  • Mesolithic/neolithic transition
  • Mt. Toba
  • Mousterian culture
  • Neanderthals
  • Neanderthal inter-breeding
  • Neanderthal inter-marriage
  • Neolithic
  • Northern route out of Africa
  • Oldowan culture
  • Oldest Dryas ice age
  • Omo people
  • Out of Africa or RAO hypothesis
  • P37
  • Paleolithic/mesolithic transition
  • Pale skin
  • Plagues
  • Popigai impact series
  • Pre-humans
  • Proconsul
  • Proto-neanderthals
  • Perry's DNA
  • RAO - Recent African Origins
  • Rathcroghan
  • Repopulation of England
  • Repopulation of Ireland
  • Roman invasion
  • Sardinian
  • S2639
  • Saale ice age
  • "secondary products revolution"
  • slave trading
  • Speed of evolution
  • Stone Circles
  • Stonehenge
  • Storegga Tsunamis
  • TMRCA
  • TMRCA Isles AB, S2639 - 6,600
  • TMRCA Isles A, PF4135 - 950
  • TMRCA Isles B, L1498 - 6,600
  • TMRCA Isles CD, Y3734 - 3,400
  • TMRCA Isles C, Y5450 - 2,200
  • TMRCA Isles D, Y4660 - 1,500
  • Toba Catastrophe Theory
  • Tools of the cultures
  • Ukraine Refugium
  • Ur-Shatt
  • Viking
  • Volcanos: ,
  • Wash, the
  • Weichselian ice age
  • Y3104
  • Y3734
  • Younger Dryas
  • Zhamanshin impact
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    Notes


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    Geological Setting


    65.5 million years ago - the age of dinosaurs was ended by an asteroid hitting earth at Chicxulub . 75% of all species became extinct. That cleared way for the start of the age of mammals.

    65.5 million years ago - The beginning of the Paleocene Period and the Cenozoic Era. The climate was about 12° C (20° F) warmer than the present with an atmospheric carbon dioxide content about 5 times what it is now. At the beginning of the Paleocene, most mammals were tiny and rodent-like. With time, mammals grew in size, number, and diversity.

    54 million years ago - The beginning of the tropically warm Eocene Period.

    49 million years ago - the 'Azolla event' caused the carbon dioxide level to drop from 3,500 to 650 ppm. The draw-down of carbon dioxide has been speculated to have helped transform the planet from a "greenhouse Earth" state, hot enough for turtles and palm trees to prosper at the poles, to the "icehouse Earth" it has been since.

    34 million years ago - The end of the very warm Eocene and start of the Oligocene is marked by a major extinction event: about 90% of the species that inhabited our planet at that time fell off the biodiversity map. The extinction may have been caused by a series of meteor impacts similar to the 23 observed when the Shoemaker-Levy 9 comet broke up and collided with Jupiter. The four known major impacts were in Popigai Siberia, the Chesapeake Bay. Tom's Canyon New Jersey, and Mistastin Labrador. There may have been many more. Earth's temperature abruptly dropped by about 6° C. The temperature stayed down for about 7 million years. The Oligocene climate change caused a global increase in ice volume and a 55 m (181 feet) decrease in sea level. Temperate deciduous woodlands mostly replaced tropical and sub-tropical forests, while plains and deserts became more commonplace.