CHAIR OF URALIC LANGUAGES, UNIVERSITY OF TARTU
INNOVATIVE VIEWS IN URALISTICS
We must remember that now the human genetics recognizes three
main methods for the researching of human genes:
1. nucleus DNA from parents to all children,
2. mitochondrial DNA (mtDNA) only from mothers to all children
(maternal
lineage),
3. Y chromosome (Y) only from fathers only to sons (paternal
lineage)
It is clear that the Finno-Ugrians share their maternal
lineages
with other Europoids (Caucasoids in the genetic terminology) and
not with Mongoloids, at least in any larger extent. The results of the
genetic research allow also to question the origin of Tat C allele of the
Y chromosome and to suggest that it has first occurred in Finno-Ugric
population
and only considerably later found its way to (some) Siberian populations.
The Tat C allele was found to be frequent not only among the European
Finno-Ugric
populations but also among Latvians and Lithuanians, who are
linguistically
both Indo-Europeans. Richard Villems work team write that "it turned out
that frequencies of the Tat C allele in both Latvian (Lahermo et al. 1999)
and Lithuanian (our results) Y chromosomes are close to those among
Estonians,
Karelians and Finns: i.e. significantly higher than among Russians and
much higher than among western Slavs: around 29% for Latvians and 33% for
Lithuanians. We consider this finding very interesting from the point of
view of the ethnogenesis of the extant Baltic and Finno-Ugric populations.
There is no apparent north-south frequency gradient of Tat C allele from
the Arctic Sea (Saamis) to Lithuanians but a sharp east-west cline both
in Scandinavia and on the Baltic area." (Rootsi et al. 2000: 152). The
work team also suggests that a high Tat C frequency among Latvians and
Lithuanians, in contrast to almost all other Indo-European-speaking
Europeans.
Particularly, both Poles and Belorussians differ sharply in this respect
from the two indicated Baltic populations, as well as from Russians. That
suggests very extensive admixture of Latvians and Lithuanians with
Finno-Ugric-speaking
populations up to an extent that language change hypothesis can be
discussed.
According to new scientific research, the ancestors
of modern population of the Baltic area arrived in this area at the end
of the Last Maximum of the Last Ice Age from the more southern regions
of Europe. They were Euripides by race and settled the territory of the
Baltic area after the glacier receded about 19,00013,000 years ago.
Modern Man, or Homo sapiens sapiens, started
migrating from eastern Africa 120,000-100,000 years ago and settled Europe
roughly 40,000 years ago, arriving during an inter-stadial (temporary
warming)
period in the Last Ice Age about more than 120,000 years ago. This
inter-stadial
covered the period for 40,000 to 30,000 years ago (the glacier, in the
coldest climate conditions, extended to the Black Sea). Human settlement
may have also occurred on Baltofennoscandinavian territory during a
temporary
period before the Last Maximum of the Last Ice Age, 23,000-19,500 years
ago. The advancing and receding glacier, which reached at least half a
kilometre in thickness on the edge in modern Lithuania and 2.5 kilometres
thick on the mountains of Scandinavia, along with the water flows off the
ice have destroyed all possible traces of human activity and inhabitation
in the Baltic area during that period.
According to archaeologist Pavel Dolukhanov's theory,
the ancestors of Finno-Ugric peoples formed the first wave of modern
people arriving in Europe from Africa, when then settled the Periglacial
zone at the southern edge of the glacier. The waves of immigrants who
followed
settled the southern, Mediterranean zone.
The final retreat of the glaciers about 19,000 years ago
drew human settlements northward, reaching the Arctic Ocean about
11,0009000
years ago. According to linguist Kalevi Wiik's theory, our Finno-Ugric
ancestors settled an area from the Atlantic Ocean to the Ural Mountains,
both during the Last Maximum of the Last Ice Age and thereafter.
The population of hunters and fishers living in the
Periglacial zone was small and spread out, as is took roughly ten square
kilometres of land to support one person. No large migrations occurred
within the populated area. Extensive population movement took place only
onto the unpopulated land that was freed from beneath the glacier as it
moved northward.
Natural disasters also forced the population to
move. After humans populated Europe, these natural disasters included
volcanic
activity in the central part of Europe what is now western Germany on the
Eiffel plateau, 100,000 to 11,000 years ago. The most interesting volcanic
activity, in regard to human migration, occurred 13,000 to 11,000 years
ago, when a large part of what is now Germany was covered with ash and
rocks. The most powerful explosion was by the Laach volcano 13,000 years
ago, which seriously damaged local plant cover and drove away game animals.
Archaeologist Hans-Peter Schulz theorizes that people also fled the disaster
area, and, based on archaeological finds, may have fled as far as what
is now central Russia. It could be expected that during this flight people
also arrive in the Baltic area.
After a volcanic eruption, vegetation is restored
relatively
quickly even within a human generation or so. Because of this, we can
assume that populations wandered back and forth between the area of the
natural disaster and the neighbouring territories for a thousand years.
This tendency served to mix together various human populations and
allowed for the consolidation of human genetic types and numerous incidents
of language contact throughout the heart of Europe.
We have no conclusive information concerning how long
ago modern humans, or Homo sapiens sapiens, was able to speak.
Experts believe that human language is at least 50,000 years old, but we
can consider it quite probable that our ancestors could speak even earlier,
perhaps 100,000 or more years ago.
Today roughly 6000 languages are spoken around the world.
About 10,000 years ago, when human had not begun to shift from food
consumption
(hunting and fishing) to food production (farming and livestock) that
created
the conditions for a marked increase in population, humans numbered
about 5-10 million in the whole world.
At that time humans were speaking a record number
of distinct languages, about 12,000. This average number is based on the
assumption that 10,000 years ago each language collective included 500-1000
people, as is true of Australian aborigines in modern times. It is possible
that within the past few millennia more languages have died out than are
currently alive today and that most languages today are not spoken by their
original users. The original inhabitants of New Guinea hold the record
for the largest number of languages relative to the population and
linguistic
divergence has long been the rule on the island. Currently there are very
few languages in northern Europe, the result of millennia of linguistic
convergence.
The comparative method of Indo-European linguists, which
has become the widely accepted paradigm for historical linguistics in
general,
is based upon the principle that related languages diverge with
the passage of time. In 1997 linguist Robert M. W. Dixon has developed
a general model of long-term linguistic equilibrium within an enduring
linguistic area, followed by an episode of drastic change. He sees the
punctuation episode, when the dispersal is actuated that triggers the
divergence
underlying the family tree (Sprachbaum) formation, as a rather special
event. The more normal situation is one where convergence processes
prevail. In 1999 Dixon's standpoints are relied on by linguist Daniel
Nettle.
He argues that when humans migrated from Africa there would be a great
variety of available geographical niches and the population would fission
repeatedly and often. The newly split languages would go on changing until
they were sufficiently different to be identified as different language
families. But then Nettle follows Dixon's convergence approach and predicts
a decrease in number of apparent language families.
Earlier I have evoked my conviction that Dixon's model
of punctuated equilibrium is the best for explaining emergence of language
families and, particularly, the Uralic language family. Likewise, I see
the only possible way for a further development of historical linguistics
in its symbiosis with genetics and archaeology, which, in turn,
supports Dixon's model. The formation of intergrated Uralic languages by
way of convergence has been supposed also by linguists János Pusztay
and Kalevi Wiik.
Two types of geographic areas may be discerned
in the world. One type - for example, the Eurasian steppe belt and at one
time the Bering Isthmus that connected Eurasia and America - encouraged
the easy spread and exchange of languages, and could have been at least
temporarily linguistically unified. The other - for example, the Caucasus
Mountains and the hilly island of New Guinea - preserved linguistic
diversity
and no one language was able to spread across the whole area.
If indeed only one language had existed 100,000 years
ago, based on the Indo-European language divergence model there should
be about 10 million billion billion billion languages in the world today.
As that is not the case, we have to assume that language exchange
has been the rule, not the exception in human history.
The Periglacial zone was rich with biomass and
this created conditions favourable for large game animals, such as mammoth,
bison, elk etc. Large game hunting and close contact between various human
populations helped either to preserve the original similarity between
Finno-Ugric
languages or to make other languages similar to Finno-Ugric languages.
In the latter case, it is possible that a lingua franca or common language
of exchange was used.
In either case, the result was that throughout the
Periglacial
zone there was a relatively high level of language unity, which is to say
that people spoke Finno-Ugric languages. (Absolute language unity
in such a large area - from the Atlantic Ocean to the Ural Mountains
is inconceivable. In such a geographic expanse even the complete unity
of the theoretical Finno-Ugric lingua franca is inconceivable.)
In the southern Mediterranean zone this process
of language convergence did not occur or was not as extensive as in the
Periglacial zone. Of the non-Indo-European languages that were once spoken
in the Mediterranean zone only the Basque language in the Pyrenees and
the Caucasian languages in the Caucasian Mountains are preserved. But of
course many non-Indo-European languages were once spoken in the areas
between
the Pyrenees and the Caucasus.
Roughly 10,000 years ago agriculture began to spread
from Turkey into the Mediterranean zone and then into the rest Europe,
and livestock herding began to follow the same path from steppes of Europe
and Asia. (According to archaeologist Valter Lang, the first signs of
agriculture,
for example, on Estonian territory are about 5000 years old.)
The appearance of Indo-European languages in the
Mediterranean zone about 7500 years ago changed the European distribution
of languages. The Indo-European languages pushed the unknown languages
out of centre of the Mediterranean zone became the eastern neighbours of
the Basque type languages and the southern neighbours of the Finno-Ugric
languages. The major flood, in particular, which could have happened about
7500 years ago, deserves attention. The oceanic water, risen as a result
of the melting continental ice cap, broke through the barriers at the
Bosporus
from the direction of the Mediterranean Sea and passed on to the Black
Sea whose level was rising very fast - about 15 cm a day - to 107 metres
higher than earlier. (It is quite possible that the Biblical Flood is a
reminiscence about the catastrophe of that period.) The population of the
shores of the Black Sea were forced to flee from the waters in all
directions
about which some archaeological evidence has supposedly been found. As
supposed, the fleeing was most intensive from the north-western shelving
shores of the Black Sea where at present the depth of the sea is only 30-60
metres and thus the flood was most extensive. (This Black Sea phenomenon
under observation is to a certain extent comparable to the Laach volcanic
phenomenon only without the back-and-forth movement of the population.)
Hereby it is important that those who escaped from the
shores of the Black Sea had already dealt with agriculture and animal
husbandry
and so the Black Sea phenomenon could accelerate the spread of these manners
of subsistence to the areas of hunters and fishers in Central Europe
where Finno-Ugric-speaking populations could have located. Everything
related
to the phenomenon under observation needs a more profound research but
the result of the phenomenon is sure to be extremely interesting,
particularly
from the view of language contacts.
Wiik theorizes that northern Indo-European languages
(Germanic,
Baltic and Slavic), which differ greatly from other Indo-European languages,
were created when Finno-Ugric speakers learned Indo-European language form.
But, as is always case with learning foreign languages, they made errors
in pronunciation, word forms and sentence structure. In other words,
Germanic,
Baltic and Slavic languages are full of Finno-Ugric influences, or more
exactly substrata. Among the substrata, however, almost no
Finno-Ugric
loan words are found. The lack of loan words is characteristic of the
language
exchange process, as is basically the same as the process of learning a
foreign language. When we learn a foreign language we don't use words from
our mother tongue but we do mistakes in pronunciation, declination,
conjugation,
number use and sentence construction based on the norms of our mother
tongue.
The Finno-Ugric substratum is most apparent in the Slavic languages, through
southernmost areas where they appear, and most disputable in the Germanic
languages.
In the past few years Wiik's theory has been the subject
of heated discussion, especially, as can be expected, in relation
to the Germanic languages. Incidentally, this has been enlivened by the
fact that about a third of the Germanic vocabulary is of non-Indo-European
origin but does not suggest modern Finno-Ugric vocabulary. This third
includes
many words relation to sea travel, military action and societal
organisation.
Wiik's theory has been criticized also for its language
typology aspect: some of the theoretically Finno-Ugric substrata in
the Germanic languages includes phenomena that are very common in Europe
and in the whole world and therefore could have arisen in the Germanic
and Finno-Ugric languages independently.
Of course, lost languages that are entirely unknown
to us might have one time been spoken in the Periglacial zone, the same
is true in the Mediterranean zone. These might not have been at all similar
to Finno-Ugric languages. On the other hand, we cannot forget that
Finno-Ugric
languages and the level of development of their speakers might varied widely
within the Periglacial zone, and some of these languages are now lost,
i.e. replaced with Indo-European languages.
Currently scientists are moving away from the old
understanding
that shifts in material and spiritual culture throughout human history
have been caused always by relatively large population migration.
Material and spiritual culture (including language) could have been
transferred
- and for the most part have transferred - from one group to another without
any population migration at all. The movement of a few cultural pioneers
(including language pioneers) is more likely. It has been convincingly
posited that agriculture, as one example, has spread throughout the world
almost entirely without the help of population migration. Wiik stresses
that this also occurred in Europe.
It is interesting, therefore to note that Wiik has pointed
out that agriculture spread through Europe first, followed about a thousand
years later by Indo-European languages. Linguist Jean-Luc Moreau has
suggested
that Indo-European language-speakers were not the ones who spread
agriculture
but professional bandits with sophisticated military technology
who arrived in the areas that had grown rich on agriculture and subjected
the local farmers to their own power.
Agriculture allowed humans to gain about fifty times
more sustenance from an area than did hunting and fishing. The shift
to agriculture's end result was explosive population growth in Europe and
around the globe. Their is no clear evidence that the spread of agriculture
from Turkey first to southern Europe and from there northward before the
Black Sea flood phenomenon would have caused the massive migration of
southern
populations. Why this was, we still cannot satisfactorily explain. (Possible
explanations may include the destructive epidemics that spread easily among
the dense human populations of the farmers and the looting and wars that
took place among the farming populations.)
In Wiik's approximation, Baltic population are mainly
typical north-western Europeans, characterized by the height, large
head, oval face and light skin, hair and eyes. The reasons for the arousal
of the anthropological factors is not entirely clear, nor do we know why
this type of human is so common to north-western Europe. It has be posited
that the cause may be natural selection among Nordic farmers. Researcher
Valdar Parve supposes that the original meat-eating inhabitants of
Baltofennoscandinavia
differed considerably from present day inhabitants of this area. Nutrition
habits on the territory of Baltofennoscandinavia changed considerably when
a transition to agriculture and more and more vegetarian way of nutrition
took place. The resulting deficiency in fat-soluble vitamins is believed to be a
Darwinian
factor of selection. Deficiency in vitamin D and rachitis, deficiency in
vitamin K and disturbances in blood clotting, deficiency in vitamin E and
weakness of uterus contractions - all this caused the death of young
pigmented
women at childbirth. This kind of situation was favourable to individuals
with large area of light skin. Their body mass was small in relation to
the body area, allowing the access of ultraviolet radiation, which is scarce
in northern regions but forms an essential factor for synthesizing
fat-soluble
vitamins from provitamins of vegetable origin. So the key to the origination
of depigmented population lies in the change of nutrition habits.