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Author Topic: Kefi's ancient Taforalt haplogroups
Tukuler
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Thanks to Kefi's actual Maurusian era Taforalt
mtDNA study there's no doubt Eurasian lineage
existed in coastal and tell Mechta-Afalou ages
well before Islamic white slave trade or even
chalcolithic trade in non-human goods between
North Africa and South Europe.

Kefi's data, though limited where it differs
from rCRS by no more than a three variant
haplotype in 12 samples, is authentic. The
problem is her obvious bias against Africa
sub-Sahara.

Even though she admits one sample possibly
is L, M, or N, she nonetheless ignores it and
categorically states there was no SSA contribution.

This led me to wonder how far her bias
prejudiced the haplogroup assignments
of the non-rCRS samples.

The fact is some polymorphisms are associated
with more than one haplogroup.

Using Watson 1997's full sequences of over
150 control region haplotypes with their
associated L haplogroups I present valid
alternatives to Kefi's interpretation which,
without decisive coding region data as in
Herrnstadt (2002), are just as possible.

 -

I appreciate and solicit any corrections, precisions, or updates to Watson (1997).


There's only an ~1500 year difference in
the coalescence ages of H1 and H3 in the
Maghreb and Iberia (the elder and source
of no little then 50% of those markers per
Frigi 2010).

Haplogroups must not be confused for skin
colour, facial features, or phenotype. Nor
does mtDNA alone tell the complete deep
ancestry story, nrY chromosomes must
also be considered.

Whereever any coastal to tell Maghrebi
and pre-Sahara NW Africa genetics may
have originated, by historic times there
are written observations on the majority
colour of the Maurs, Numidians, and
Aithiops of the region which can't be
ignored. Painted and plastic art reveals
some types were not dark and there were
types whose facial profiles' do resemble
western Eurasians.

A look at today's uniparentals in the
region will conclude the prominence of
the African components despite major
phenotype similarities to Arabian
penisulars or South Europeans.

 -
NOTE: Ennafaa's Libyan nrY seems to mistake J as A,B,E(xEb1b1a,b).


Supra-Saharan North Africans are of
African stock at base, increasingly
augumented by Eurasian settlers,
colonistss, and conquerers spanning
the entire Holocene epoch all the way
from Maurusian to modern times.

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beyoku
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What is the source of that second image. I would like to see the details.

Thanks,

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Doug M
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Unfortunately the whole problem with any discussion of ancient North African genes always goes back to the populations used in the samples and the geographic definition of North Africa. If North Africa is to be considered as only the most coastal Areas of North Africa not extending more than a few hundred miles inland, then it isn't an accurate reflection of the complete picture and skews the influence of said "Eurasian" populations. North Africa spans an area larger than western Europe and America combined and includes all of the Sahara desert, which itself is larger than the continental United States. Therefore, focusing on populations closest to the coast is not a reflection of all North African populations and historic population movements.
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Tukuler
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@Beyoku - Ennafaa 2011 mtDNA nrY Tunisia

@DougM - I've clearly defined coastal, tell, and
pre-Sahara NW Africa and this thread particularly
focuses on Maurusian Taforalt just across from
Iberia and possible "sub-Sahara" gene profiles
so there should be no confusion. Stick to the
definitions, deal with the data, no problem.

That is unless you don't like the data.
In which case chose a report and broach
a thread to analyse what's in it. See if
you can escape H1 and H3 anywhere in the
Sahara proper from Ghadames, Hoggar, and
Air westwards.

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Doug M
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quote:
Originally posted by Tukuler:
@Beyoku - Ennafaa 2011 mtDNA nrY Tunisia

@DougM - I've clearly defined coastal, tell, and
pre-Sahara NW Africa and this thread particularly
focuses on Maurusian Taforalt just across from
Iberia and possible "sub-Sahara" gene profiles
so there should be no confusion. Stick to the
definitions, deal with the data, no problem.

That is unless you don't like the data.
In which case chose a report and broach
a thread to analyse what's in it. See if
you can escape H1 and H3 anywhere in the
Sahara proper from Ghadames, Hoggar, and
Air westwards.

I probably meant to post this in the other thread on North African back migrations.
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beyoku
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quote:
Originally posted by Tukuler:
@Beyoku - Ennafaa 2011 mtDNA nrY Tunisia

@DougM - I've clearly defined coastal, tell, and
pre-Sahara NW Africa and this thread particularly
focuses on Maurusian Taforalt just across from
Iberia and possible "sub-Sahara" gene profiles
so there should be no confusion. Stick to the
definitions, deal with the data, no problem.

That is unless you don't like the data.
In which case chose a report and broach
a thread to analyse what's in it. See if
you can escape H1 and H3 anywhere in the
Sahara proper from Ghadames, Hoggar, and
Air westwards.

Hmm so there is no supplemental material to see the direct frequencis of A,B,E,(xE1b1b)? That is dissapointing.
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Tukuler
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What's disappointing about tables S5 and S6?

--------------------
I'm just another point of view. What's yours? Unpublished work © 2004 - 2023 YYT al~Takruri
Authentic Africana over race-serving ethnocentricisms, Afro, Euro, or whatever.

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beyoku
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quote:
Originally posted by Tukuler:
What's disappointing about tables S5 and S6?

Just now saw that.
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Explorador
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Recapitulating some personal observations posted elsewhere:

The authors started out with 31 EpiPaleolithic specimens, and they tell the reader that they were left with working with 26 specimens after eliminating certain named specimens for one reason or the other, which was then reduced to first 24 and then 23 specimens. Yet, we come to learn that even those 23 specimens were reduced further down to just 21 specimens that were used in the final analysis. In the above, the authors named yet another two specimens, both alleged to be closely related to one specimen retained in the final analysis; the names of the three related specimen were given above as follows; Taf V-5, Taf V-7 and Taf V-20. One of these, we are not told specifically which one, was to have been considered in the final analysis, while the other two [again, we are not told which two of the three closely related specimens] would have been eliminated from the study.

Perhaps a relatively minor issue, it is of note that Taf V-5's and Taf V-20's fragment sequences start earlier and end earlier than that of Taf V-7, with the former's sequences between positions 16054 and 16317 having been compared against those of the Cambridge Reference Sequence, while the latter's was read from 16081 and 16404; what if mutations in positions prior to 16081 in Taf V-7's case and after 16317 in either Taf V-5's or Taf V-20's case were different from those of either Taf V-5 or Taf V-20, and V-7 respectively; could there be mutations here that could drastically alter what the authors would call the "most likely haplogroups" that these specimens' markers fall into? Something to ponder, but at any rate, along with the earlier named three contaminated specimens, the aforementioned two closely-related specimens would have amounted to five specimens being eliminated, reducing the 31 specimens down to 26. However, the authors provide the reader with a table consisting of 23 individual specimens, and all three of those closely related individuals were in it! What they did not tell the reader, nor did they identify them by name or tag, and hence, possibly leaving an unsuspecting reader scratching his/her head, is that five more specimens were excluded from the study, which were not included in the aforementioned table. These undeclared left-out specimens are namely; Taf VI-9, Taf XVII-18, Taf XIX-7, Taf XXI, and Taf I—missing specimens not named! The reader is not offered explanation on why these were not made part of the study, and so left on his/her own, to wonder what might have been wrong with them. They could have been damaged, degraded or contaminated; any or a combination of any of these could have affected sequences of those specimens. Had the authors therefore eliminated those aforementioned specimens with inconsistent and therefore dubious sequences, they would have been left with fairly small amount of individual DNA material to work with, and even then, the results would not be unequivocal, given that a good deal of their overall sample size would have been purged from the final analysis; the integrity of the so-called "good" DNA would have been put to question as well. Through it all, the authors could not even get themselves to firmly assign the sequences into a specific haplogroup set.

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Tukuler
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quote:
Originally posted by Tukuler:

Thanks to Kefi's actual Maurusian era Taforalt
mtDNA study there's no doubt Eurasian lineage
existed in coastal and tell Mechta-Afalou ages
well before Islamic white slave trade or even
chalcolithic trade in non-human goods between
North Africa and South Europe.

Kefi's data, though limited where it differs
from rCRS by no more than a three variant
haplotype in 12 samples, is authentic. The
problem is her obvious bias against Africa
sub-Sahara.

Even though she admits one sample possibly
is L, M, or N, she nonetheless ignores it and
categorically states there was no SSA contribution.


The fact is some polymorphisms are associated
with more than one haplogroup.

Using Watson 1997's full sequences of over
150 control region haplotypes with their
associated L haplogroups I present valid
alternatives to Kefi's interpretation which,
without decisive coding region data as in
Herrnstadt (2002), are just as possible.

 -

I appreciate and solicit any corrections, precisions, or updates to Watson (1997).

.
A few years ago I showed Kefi's data confirms
so-call subSaharan Africa L in nascent Holocene
Taforalt.

Now Secher is pointing out the same. However,
no word on the other possible L I identified.

It soon come.


  • Primary and secondary radiations of U6 branches with different coalescence ages were
    tentatively correlated with different North African lithic cultures, such as the Aterian,
    Dabban, Iberomaurusian or Capsian; and perhaps more speculatively, with the spread of the
    Afroasiatic language family. The Aterian was thought to have existed between 40–20 kya but
    recent archaeological age determinations, based on thermal luminescence, have pushed back
    this period, to 90–40 kya [14-16]. As the estimated age for the whole of haplogroup U6 is
    around 35 kya
    , this removes the Aterian from consideration for association with the genetic
    signal for dispersal in North Africa [8,9]. However, as U6 persists in modern day African
    populations we can assume a maternal continuity since around 35 kya, the age of this
    haplogroup. This continuity has received some support from ancient DNA studies on
    iberoMaurusian remains, with an age around 12 kya, exhumed from the archaeological site of
    Taforalt in Morocco
    [17]. In this analysis, haplotypes tentatively assignable to haplogroups
    H, JT, U6 and V
    were identified, pointing to a local evolution of this population and a genetic
    continuity in North Africa. On the other hand, only one haplotype harbored the 16223
    mutation, which if assigned to an L haplogroup would represent a sub-Saharan African
    influence of about 4%
    . This would equate to a frequency five times lower than that found in
    current Moroccan populations (20%) and would support the proposal that the penetration of
    sub-Saharan mtDNA lineages to North Africa mainly occurred since the beginning of the
    Holocene onwards [18].


    Bernard Secher with Fregel González et al
    The history of the North African mitochondrial DNA haplogroup
    U6 gene flow into the African, Eurasian and American continents

    BMC Evolutionary Biology 2014, 14:109
    doi:10.1186/1471-2148-14-109

Secher's last sentence above attempts to
restrict, or lesser qualify, a supposed
SSA influence which quantified is minor
nearly insignificant at 4%.

But his L age comment "mainly occurred
since the beginning of the Holocene onwards"

applies not to L alone but to all the Taforalt
fossil data except U6 and maybe JT. The much
flaunted H is not earlier than the L. It too is from
the Holocene onwards. Tunisian L goes back 20k
per Frigi (2010). Why wouldn't Taforalt L too?

North African L2 is old enough to be at
the very beginning of Maurusian industry
unlike H1 and H3.

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