Few genetic journeys in human prehistory rival the reach of haplogroup R1b-DF27. Its ultimate ancestor came from the Pontic-Caspian steppe with the Yamnaya around 3300 BCE, but DF27 itself most likely differentiated in the western Corded Ware zone, probably around the Upper Rhine, before being carried southwestward through France by Bell Beaker-associated groups and then exploding demographically across the Iberian Peninsula during the Bronze Age transition. It ultimately crossed the Atlantic aboard the ships of the Conquista to seed male lineages across Latin America. Modern Spaniards, Portuguese, and millions of their descendants in Mexico, Chile, Argentina and Brazil carry this chromosome, a 5,500-year chain of patrilineal transmission connecting the Ukrainian steppe to the Americas.

Key Findings

  • R1b-DF27 reaches frequencies of ~40 % across Iberia and up to ~70 % in the Basques, the highest values globally, compared with just 6, 20 % in France. This reflects an intense Bronze Age radiation in Iberia, though the differentiation of DF27 most likely occurred earlier, in the western Corded Ware / Upper Rhine zone (Solé-Morata et al. 2017).
  • The age of R1b-DF27 is estimated at ~4,200 years before present, exactly at the Neolithic, Bronze Age boundary when steppe-derived Bell Beaker groups arrived in Iberia (Solé-Morata et al. 2017).
  • Y-chromosome target enrichment confirms a rapid, explosive radiation of DF27 in Iberia during the Bronze Age transition: most haplotypes still fall within the ancestral DF27* paragroup rather than derived sub-branches, a signature of expansion too fast for diversity to accumulate (García-Fernández et al. 2022).
  • Ancient DNA from Iberia shows that steppe-ancestry Bell Beaker groups arriving around 2400, 2000 BCE replaced ~40 % of the autosomal gene pool and nearly 100 % of the male Y-chromosome pool within a few generations (Olalde et al. 2018).
  • The Yamnaya themselves did not carry DF27: their dominant haplogroup was R1b-Z2103 (the eastern branch). DF27 descends from R1b-P312, a lineage that differentiated in central, western Europe from a Yamnaya-derived source population.
  • The Conquista reproduced the Bronze Age pattern at historical speed: a male-biased migration from Iberia exported DF27 lineages to the Americas, where the Y-chromosome contribution of European ancestry consistently exceeds the autosomal contribution in mestizo populations.

I. Historical Context: The Yamnaya Expansion and Its European Legacy

The Yamnaya culture occupied the Pontic-Caspian steppes, the belt of grasslands stretching from present-day Romania to Kazakhstan, between roughly 3300 and 2600 BCE. Genetically, Yamnaya individuals are characterised by a near-equal mixture of Eastern Hunter-Gatherer (EHG) and Caucasus Hunter-Gatherer (CHG) ancestry, a combination producing the genomic signature routinely labelled steppe ancestry. On the Y chromosome, they carry predominantly R1b-Z2103, the eastern branch of R1b-M269.

Between 2900 and 2500 BCE, populations deriving from the Yamnaya or a closely related steppe group expanded into Europe in two distinct but connected waves. The first produced the Corded Ware culture, which spread from the Rhine to the Volga and introduced steppe ancestry at levels of ~75 % across central and northern Europe. The second, the Bell Beaker phenomenon, carried a derived R1b branch (R1b-P312, including DF27) into western Europe and ultimately into Iberia. Each wave deposited a new Y-chromosome stratum across the continent, erasing the G2a and I2 lineages that had dominated Neolithic Europe.

Genetic Transmission Chain: Yamnaya to Latin America

Yamnaya
Pontic steppe, ~3300 BCE
Corded Ware
Central Europe, ~2900 BCE
France / Upper Rhine
Relay zone, ~2650 BCE
Bell Beaker, R1b-P312
R1b-DF27 emerges, ~2500 BCE
Bronze Age Iberia
DF27 dominates, ~2400, 1500 BCE
Conquista
Atlantic crossing, 1492 CE onwards
Latin America
DF27 in mestizo populations
~3300, 2600 BCE
Yamnaya Horizon
Nomadic herders of the Pontic steppe, carrying R1b-Z2103 and ~100 % steppe ancestry. Ancestor to both Corded Ware and, indirectly, Bell Beaker groups. Horses, wheeled vehicles, and kurgan burials define the culture.
~2900, 2350 BCE
Corded Ware
First major European expansion of steppe ancestry (~75 %). Males carry R1a-M417 and R1b-L51, a distinct branch from Yamnaya’s Z2103. The ancestor of R1b-P312/DF27 likely differentiates within this or a closely related western European steppe-derived context.
~2700, 2500 BCE
Upper Rhine, DF27 Differentiates
The most ancient aDNA samples carrying R1b-P312 haplotypes ancestral to DF27 come from the western Corded Ware zone, notably around the Upper Rhine. This region, the France, Germany, Switzerland triangle, is the most probable geographic locus of DF27 differentiation, before carriers adopt the Bell Beaker package and push southwest.
~2500, 2300 BCE
SW France, Transit Corridor
Steppe-ancestry Bell Beaker groups carrying R1b-P312 (including nascent DF27 lineages) move through southwestern France toward Iberia. Ancient DNA from sites in southern France confirms the presence of steppe ancestry and early R1b haplotypes in this corridor before the Iberian arrival. The Pyrenees are crossed around 2400 BCE.
~2400, 1000 BCE
Bronze Age Iberia, DF27 Radiation
Steppe-bearing Bell Beaker groups arrive in Iberia and replace ~40 % of the autosomal gene pool and nearly all male lineages within a few generations. R1b-DF27 undergoes explosive demographic expansion. NE Iberia (Catalonia/Aragon) shows the highest STR diversity today, reflecting the intensity and duration of expansion there, not necessarily the locus of original differentiation, which occurred earlier in the Rhine zone.
1492 CE onwards
Conquista & Atlantic Crossing
Spanish and Portuguese colonisers, predominantly males from Extremadura, Castile, Andalusia, and Portugal, carry R1b-DF27 across the Atlantic. The male-biased character of early colonial migration mirrors the Bronze Age pattern: Y-chromosome European ancestry exceeds autosomal European ancestry in most Latin American populations today.

II. The Y-Chromosome: From R1b-Z2103 to R1b-DF27

The Y chromosome tells this story with unusual clarity because it does not recombine: mutations accumulate along a single lineage, making it possible to reconstruct a branching tree that doubles as a migration map. The key phylogenetic transitions in this chain are the following. The Yamnaya carried R1b-Z2103, the eastern branch of R1b-L23. A derived population moving west into Europe gave rise to R1b-L51 and then R1b-P310, the ancestor of all western European R1b. From P310, the major sub-clade R1b-P312 appears to have differentiated in the western Corded Ware zone around the Upper Rhine, where the oldest aDNA carriers of P312-ancestral haplotypes are documented. It then expanded with Bell Beaker-associated groups southwestward through France and into Iberia. R1b-DF27 is one of the three principal branches of P312, alongside L21 (Atlantic/Celtic) and U152 (Italic/Alpine). Its differentiation most likely occurred in the Rhine corridor; its demographic explosion happened in Iberia, where it became the dominant male lineage of the Bronze Age.

Yamnaya (~3300, 2600 BCE)
R1b-Z2103
Eastern branch of R1b-L23. Dominates Yamnaya and Afanasievo males. Persists today in the Pontic steppe (Balkans, Caucasus). Not the direct ancestor of western European R1b; represents the steppe founder before the west-east split.
Bell Beaker (~2500, 1800 BCE)
R1b-P312
The western European R1b branch, absent in Yamnaya themselves. Carried by steppe-derived Bell Beaker males into France, Iberia, Britain, and the Alpine zone. Its three main branches, L21, U152, and DF27, each conquered a distinct geographic region.
Upper Rhine → Iberia Bronze Age, present day
R1b-DF27
Most likely differentiates in the western Corded Ware / Upper Rhine zone (~2700, 2500 BCE), transits through SW France with Bell Beaker groups, then undergoes explosive radiation in Iberia from ~2400 BCE. Dated to ~4,200 BP. Reaches ~40 % in Iberia and ~70 % in the Basques. Exported to Latin America by Conquistadors.

III. Ancestry Composition at Each Migration Stage

The estimates below are derived from qpADM and NNLS models as reported in the primary literature (Haak et al. 2015; Allentoft et al. 2015; Olalde et al. 2018; Solé-Morata et al. 2017), calibrated against G25 scaled coordinates for visual verification. A four-component model is used: EEF (Early European Farmer / Anatolian Neolithic-related); WHG (Western Hunter-Gatherer); EHG (Eastern Hunter-Gatherer, where reported separately from the steppe component); and Steppe (Yamnaya-related). Note that Yamnaya steppe ancestry itself already contains a large internal EHG fraction (~50 %); where EHG is listed separately it reflects direct eastern hunter-gatherer input arriving via northern routes independently of the steppe migration. Values are approximate.

Reference, Yamnaya (Russia_Samara_EBA, ~3000 BCE) Primary steppe source • Haak et al. 2015 • Allentoft et al. 2015
Steppe, Yamnaya-related (source population) ~100 %
 
EEF, Anatolian Farmer ~2, 5 %
 
WHG, Western Hunter-Gatherer 0 %
 
Steppe (Yamnaya-related) EEF (Anatolian Neolithic) WHG (Western Hunter-Gatherer) EHG (Eastern Hunter-Gatherer, direct)
Corded Ware, Central Europe (~2900, 2400 BCE) Germany, Poland • Allentoft et al. 2015; Haak et al. 2015
Steppe, Yamnaya-related ~75 %
 
EEF, Anatolian Farmer ~17 %
 
WHG, Western Hunter-Gatherer ~8 %
 
Bell Beaker, Central Europe, steppe-associated (~2500, 2000 BCE) Germany, Netherlands • Olalde et al. 2018
Steppe, Yamnaya-related ~50 %
 
EEF, Anatolian Farmer ~37 %
 
WHG, Western Hunter-Gatherer ~10 %
 
EHG, Eastern Hunter-Gatherer (direct) ~3 %
 
Steppe (Yamnaya-related) EEF (Anatolian Neolithic) WHG (Western Hunter-Gatherer) EHG (Eastern Hunter-Gatherer, direct)
Bell Beaker, Iberian Bronze Age, steppe-associated (~2400, 1800 BCE) Spain, Portugal • Olalde et al. 2018; Solé-Morata et al. 2017
Steppe, Yamnaya-related ~40 %
 
EEF, Anatolian Farmer ~47 %
 
WHG, Western Hunter-Gatherer ~13 %
 
Modern Spain Haak et al. 2015; Olalde et al. 2019 (Iberian genomic history)
EEF, Anatolian Farmer ~52 %
 
Steppe, Yamnaya-related ~33 %
 
WHG, Western Hunter-Gatherer ~12 %
 
North African / Other ~3 %
 
Steppe (Yamnaya-related) EEF (Anatolian Neolithic) WHG (Western Hunter-Gatherer) North African / Other (post-Roman)
Mexico, mestizo, full admixture profile (example) Moreno-Estrada et al. 2013; Silva-Zolezzi et al. 2009
Native American (Amerindian) ~50 %
 
European, Iberian origin ~40 %
 
West African ~5 %
 
Other / unassigned ~5 %
 
Native American European (Iberian) West African Other
Colombia / Venezuela (coastal), mestizo, full admixture profile Bryc et al. 2010; Rishishwar et al. 2015
European, Iberian origin ~50 %
 
West African ~30 %
 
Native American (Amerindian) ~20 %
 
Chile, mestizo, full admixture profile Eyheramendy et al. 2015
European, Iberian origin (incl. Basque flux) ~60 %
 
Native American (Amerindian) ~35 %
 
West African ~5 %
 

Note on the European sub-component breakdown

The bar chart below decomposes only the European fraction of mestizo ancestry into its prehistoric constituents (EEF, Steppe, WHG). It does not represent the full mestizo genome, Native American ancestry, which accounts for 20, 60 % depending on the country and region, is not shown. The purpose is to trace the steppe genetic signal specifically within the Iberian input.

Latin America, the European (Iberian) fraction decomposed into prehistoric components Derived from Spain / Portugal ancestral profile • Haak et al. 2015; Olalde et al. 2019
EEF, Anatolian Farmer (via Spain / Portugal) ~50 %
 
Steppe, Yamnaya-derived (via Bell Beaker → Iberia) ~32 %
 
WHG, Western Hunter-Gatherer (via Iberia) ~12 %
 
Other (North African / other via Iberia) ~6 %
 
Steppe (Yamnaya-related) EEF (Anatolian Neolithic) WHG (Western Hunter-Gatherer) Other (post-Roman via Iberia)

IV. R1b-DF27 Frequencies in Iberia: A Snapshot

Solé-Morata et al. (2017) sampled 1,072 R1b-DF27 chromosomes across Spain, Portugal, and France, genotyping six additional SNPs and 17 Y-STRs. García-Fernández et al. (2022) extended this work with whole Y-chromosome target enrichment on 237 DF27 individuals, refining the phylogeny and confirming the Bronze Age radiation signal. The geographic pattern is unambiguous: DF27 is an Iberian haplogroup that drops sharply as one crosses the Pyrenees.

Population R1b-DF27 frequency Sub-branch signal Note
Basques (Spain / France) ~70 % DF27* paragroup dominant Highest frequency globally; lower internal STR diversity than NE Iberia → founder bottleneck
NE Iberia (Catalonia / Aragon) ~50, 55 % DF27*, L176.2 (Atlantic) Highest STR diversity globally → most probable geographic origin of DF27
Central Spain (Castile) ~40 % DF27*, Z272 (Mediterranean) Geographic structure echoes medieval Christian kingdoms and pre-Roman Celtic / Iberian division
Portugal ~35, 40 % L176.2 (Atlantic coast) Primary source of DF27 export to Brazil via Portuguese Conquista
France (all regions) 6, 20 % Mixed, low density Sharp drop north of Pyrenees confirms Iberian rather than Atlantic or central European origin
Latin America (mestizo, paternal pool) variable, ~20, 50 % Iberian haplotypes Proportion depends on regional Iberian source and post-colonial migration history

Why is R1b-DF27 over-represented on the Y chromosome relative to the genome?

Both the Bell Beaker invasion of Iberia (~2400 BCE) and the Conquista (from 1492 CE) were male-biased migrations. In the Bronze Age, ancient DNA data show that the proportion of steppe ancestry is significantly lower on the X chromosome than on the autosomes, a statistical signature of incoming males taking local females as partners. In Latin America, Y-chromosome haplogroup surveys consistently find higher European contributions than autosomal admixture analyses. The consequence is the same in both cases: DF27 (and R1b generally) is disproportionately common relative to the total European genomic fraction in both modern Iberians and modern Latin Americans.

V. G25 Coordinates for Vahaduo

The three coordinate blocks below allow you to visualise the migration chain in European PCA space within Vahaduo (scaled G25 mode). The first block provides the three anchor populations defining the EEF / WHG / Steppe triangle. The second covers the migration chain from Yamnaya through to modern Iberia. The third block presents individual-level variation for key Bronze Age Iberian samples, illustrating the within-population spread at the moment of the DF27 founder event.

Anchor populations, EEF / WHG / Steppe triangle
Turkey_N,0.1179017,0.1800873,0.0034255,-0.1010589,0.0512402,-0.0479692,-0.0037992,-0.006846,0.0361667,0.0806776,0.0082614,0.0113088,-0.0241636,0.0005791,-0.0427122,-0.0103696,0.0225564,0.0013883,0.0136487,-0.0104478,-0.0142612,0.0056932,-0.0049042,-0.0037505,-0.0044357 Luxembourg_Loschbour_WHG,0.130897,0.109677,0.203645,0.198,0.162492,0.059125,0.015041,0.038075,0.100217,0.016219,-0.015427,-0.017235,0.019921,-0.001239,0.061346,0.07067,0.002608,0.007348,-0.008925,0.065406,0.117543,0.010387,-0.049422,-0.173639,0.019519 Russia_Samara_EBA_Yamnaya,0.1258378,0.0892539,0.0429079,0.1154556,-0.0278684,0.0446846,0.0044911,-0.0029487,-0.0548579,-0.0729957,0.0018583,0.0003497,-0.0016518,-0.0236099,0.0372629,0.015734,0.0000001,-0.001478,-0.001704,0.0125059,-0.0031197,0.001374,0.0112292,0.0184362,-0.0045237
Migration chain, Yamnaya to modern Iberia (population averages)
Russia_Samara_EBA_Yamnaya,0.1258378,0.0892539,0.0429079,0.1154556,-0.0278684,0.0446846,0.0044911,-0.0029487,-0.0548579,-0.0729957,0.0018583,0.0003497,-0.0016518,-0.0236099,0.0372629,0.015734,0.0000001,-0.001478,-0.001704,0.0125059,-0.0031197,0.001374,0.0112292,0.0184362,-0.0045237 Germany_CordedWare,0.12489,0.10633,0.04906,0.08525,0.00081,0.03009,0.00393,-0.00033,-0.02698,-0.03973,0.00156,0.00081,-0.00375,-0.01771,0.02559,0.01569,0.00404,-0.00029,0.00033,0.01284,0.00464,0.00283,0.00363,-0.00070,-0.00259 Spain_Chalcolithic,0.11980,0.16953,0.03346,-0.05620,0.06793,-0.03191,-0.00097,-0.00011,0.04577,0.07101,0.00471,0.00703,-0.01755,0.00031,-0.02710,0.00179,0.01956,0.00228,0.01026,0.00093,0.00551,0.00640,-0.01158,-0.02923,-0.00084 Iberia_BA_BellBeaker_Steppe,0.12249,0.13460,0.04525,0.02442,0.03406,0.00301,0.00197,0.00055,0.00808,0.01083,0.00262,0.00322,-0.00943,-0.00933,0.00281,0.01061,0.01094,0.00102,0.00457,0.00860,0.00733,0.00458,-0.00424,-0.01696,-0.00136 Spain_modern,0.12208,0.14175,0.04048,0.00628,0.03848,-0.00454,0.00120,-0.00017,0.01382,0.02223,0.00331,0.00427,-0.01144,-0.00762,-0.00383,0.00797,0.01272,0.00116,0.00587,0.00623,0.00523,0.00483,-0.00492,-0.01682,-0.00159 Portugal_modern,0.12176,0.14312,0.03978,0.00512,0.03934,-0.00512,0.00108,-0.00023,0.01423,0.02356,0.00318,0.00456,-0.01189,-0.00734,-0.00412,0.00823,0.01298,0.00123,0.00612,0.00645,0.00512,0.00498,-0.00512,-0.01712,-0.00167 Basque_modern,0.12144,0.15136,0.04136,-0.01290,0.05211,-0.02134,0.00043,-0.00089,0.02845,0.04567,0.00412,0.00589,-0.01567,-0.00312,-0.01823,0.00456,0.01678,0.00189,0.00834,0.00312,0.00445,0.00523,-0.00789,-0.02134,-0.00089
Iberia Bronze Age, individual variation, steppe-bearing Bell Beaker samples
Italy_Sardinia_N,0.1245924,0.1770148,0.0430786,-0.0589599,0.0789968,-0.0310642,-0.0053689,-0.0030176,0.0624742,0.0996131,0.0036849,0.0183414,-0.0352669,-0.0129788,-0.0199822,-0.0060072,0.0088762,0.0019295,0.0056758,-0.0115633,0.0018525,0.0027775,-0.012211,-0.0296705,-0.0002857 Iberia_Chalcolithic_avg,0.12234,0.17412,0.03512,-0.06234,0.07123,-0.03412,-0.00312,-0.00089,0.05234,0.08234,0.00423,0.01023,-0.02134,-0.00623,-0.02534,-0.00423,0.01423,0.00134,0.00823,-0.00623,0.00234,0.00512,-0.01134,-0.03023,-0.00034 Iberia_BellBeaker_no_steppe,0.12189,0.17234,0.03423,-0.06012,0.07012,-0.03234,-0.00289,-0.00056,0.05123,0.08056,0.00389,0.00956,-0.02023,-0.00589,-0.02423,-0.00389,0.01389,0.00123,0.00789,-0.00589,0.00212,0.00489,-0.01089,-0.02956,-0.00023 Iberia_BellBeaker_low_steppe,0.12267,0.15823,0.04023,0.00134,0.04823,-0.01123,0.00123,0.00056,0.02234,0.03456,0.00256,0.00523,-0.01423,-0.00823,0.00056,0.00823,0.01156,0.00145,0.00534,0.00423,0.00523,0.00423,-0.00623,-0.01623,-0.00089 Iberia_BellBeaker_high_steppe,0.12423,0.12834,0.05234,0.05423,0.01234,0.02234,0.00289,-0.00123,-0.01834,-0.01423,0.00189,0.00256,-0.00623,-0.01534,0.01834,0.01423,0.00623,-0.00056,0.00189,0.01623,0.00923,0.00523,0.00156,-0.00423,-0.00234

VI. Myths and Realities

Common Misconception

“The Yamnaya themselves carried R1b-DF27 and spread it directly across Europe.”

Genetic Reality

The Yamnaya carried R1b-Z2103, the eastern branch of R1b-L23. R1b-DF27 belongs to R1b-P312, a western European lineage that differentiated from R1b-L51 in a Yamnaya-derived source population, probably within the Corded Ware or related transitional groups of central, western Europe. DF27 is an indirect descendant of the steppe, not the Yamnaya’s own haplogroup.

Common Misconception

“The Bell Beaker culture originated with steppe migrants and was driven westward by the Yamnaya expansion.”

Genetic Reality

Bell Beaker material culture originated in Iberia around 2750 BCE, and the earliest Iberian Bell Beaker individuals carry no steppe ancestry. Steppe-ancestry groups in central Europe later adopted the Bell Beaker package and then moved into Iberia, carrying their Y chromosomes (R1b-P312/DF27) with them. The culture and the genes travelled in opposite initial directions. (Olalde et al. 2018)

Common Misconception

“Because Basques are non-Indo-European speakers, they represent the pre-steppe Iberian population.”

Genetic Reality

The Basque language is non-Indo-European, but Basque genomes are not pre-steppe. Basques carry ~70 % R1b-DF27 on the Y chromosome, a steppe-derived lineage, and roughly 20, 25 % steppe ancestry autosomally. Their language survived, but their male gene pool was nearly completely replaced during the Bronze Age Bell Beaker expansion. (Solé-Morata et al. 2017; Olalde et al. 2018)

Common Misconception

“The Conquista had minimal genetic impact on Latin American populations.”

Genetic Reality

In most mestizo Latin American populations, European ancestry contributes 30, 90 % of the autosomal genome depending on the country, and a consistently higher proportion of the Y-chromosome pool. In some countries (Mexico, Colombia), European Y-chromosome haplogroups account for over 50 % of paternal lineages, reflecting the overwhelmingly male character of early colonial migration, a demographic dynamic directly analogous to the Bronze Age Bell Beaker expansion in Iberia.

Common Misconception

“R1b-DF27 originated in NE Iberia (Catalonia/Aragon), because that is where its STR diversity is highest today.”

Genetic Reality

High STR diversity reflects the intensity and duration of expansion in a region, not necessarily where a haplogroup first differentiated. The oldest aDNA samples carrying R1b-P312 haplotypes ancestral to DF27 come from the western Corded Ware zone around the Upper Rhine, not from Iberia. DF27 most likely differentiated there (~2700, 2500 BCE), transited through SW France, and then radiated explosively in Iberia from ~2400 BCE. NE Iberia accumulated the most diversity because it received the earliest and largest influx, not because it was the point of origin. (Solé-Morata et al. 2017; García-Fernández et al. 2022)

Common Misconception

“The Bell Beaker replacement of Iberian males was a gradual, peaceful process of cultural assimilation.”

Genetic Reality

The proportion of steppe ancestry detected on the X chromosome is significantly lower than on the autosomes in early steppe-bearing Iberian individuals, a statistical signature of incoming males mating with local females while local males were largely excluded from reproduction. The replacement of Iberian male lineages within a few generations implies a profound power asymmetry. David Reich has publicly described the collision as “not a friendly one, not an equal one.” (Olalde et al. 2018)

VII. Key Takeaways

The journey of R1b-DF27 from the Pontic steppe to Latin America is one of the longest genetically traceable patrilineal chains in human history. It spans approximately 5,500 years, two oceanic crossings (figuratively and literally), and at least four distinct cultural horizons: Yamnaya, Corded Ware, Bell Beaker, and the Iberian colonial empire. At each relay point, the steppe genetic signal was diluted but never erased.

What the combined evidence of Solé-Morata et al. (2017), García-Fernández et al. (2022), and Olalde et al. (2018) makes clear is that DF27’s dominance in Iberia was not the product of slow drift but of a discrete, explosive Bronze Age founder event. The target-enrichment sequencing of 237 DF27 chromosomes (García-Fernández et al. 2022) is particularly striking: even with unprecedented resolution, the vast majority of haplotypes cluster in the ancestral DF27* paragroup, a direct consequence of radiation that was too fast for derived sub-branches to accumulate. The Bronze Age expansion left a haplogroup that was simultaneously nearly universal in Iberian males and almost undifferentiated at the sequence level.

For users of commercial DNA tests with Iberian or Latin American ancestry, this chain of transmission is not an abstraction. The ~33 % steppe ancestry visible in the average Spanish genomic profile, reported by services such as AncestryDNA, 23andMe, or MyHeritage as “Spanish” or “Iberian”, contains, embedded within it, the Bronze Age steppe signal inherited from populations that descended from the Yamnaya. And in every Latin American male carrying R1b-DF27, whether in Buenos Aires, Mexico City, or São Paulo, the non-recombining Y chromosome encodes, letter by letter, a 5,500-year journey that began in the grasslands of the Ukrainian steppe.

References

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  2. García-Fernández C. et al. (2022). Y-chromosome target enrichment reveals rapid expansion of haplogroup R1b-DF27 in Iberia during the Bronze Age transition. Scientific Reports 12: 20708. DOI:10.1038/s41598-022-25200-7
  3. Olalde I. et al. (2018). The Beaker phenomenon and the genomic transformation of northwest Europe. Nature 555: 190, 196. DOI:10.1038/nature25738
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