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Y-DNA · Väterliche Linie

R1B1A1B2

Y-DNA Haplogroup R1B1A1B2

Ein Referenzprofil für einen Abstammungszweig. Gemeinsame Haplogruppen begründen weder eine familiäre Beziehung noch eine kulturelle Identität.

Referenzprofil

Hintergrund des Zweigs

Historischer Kontext für den Y-DNA-Abstammungszweig R1B1A1B2

Origins and Evolution

Y-DNA haplogroup R1b1a1b2 is a subclade within the broader R1b paternal lineage, which belongs to the ancient R branch of the Y-chromosome tree. Because it sits deep within the western Eurasian side of R1b, it is best understood as an early-diverging lineage that predates the much more widely expanded R1b branches associated with later prehistoric population movements in Europe.

Current population-genetic evidence suggests that lineages in this part of the tree likely formed during the late Paleolithic to early Holocene, in or near West Eurasia. The exact age of R1b1a1b2 is not well constrained in the published literature, but as a descendant of an already ancient parent clade, it is reasonable to place its origin in the mid-Holocene or earlier, likely around 15 thousand years ago as a broad estimate. This does not imply a single rapid expansion; rather, it reflects gradual diversification within small, structured hunter-gatherer and early postglacial populations.

Subclades

As an intermediate branch, R1b1a1b2 helps connect older ancestral R1b diversity to younger downstream lineages. In many cases, such subclades are rare and incompletely sampled, so the internal branching structure may still be refined as more Y-chromosome data becomes available.

Key points about its phylogenetic context:

  • It is part of the deep internal structure of R1b.
  • It likely represents a non-dominant survivor lineage rather than a lineage of large demographic expansion.
  • It may include further rare descendant branches that are geographically scattered.

Geographical Distribution

This haplogroup is expected to be found at low frequency across a broad but discontinuous area of West Eurasia. Like many deep Y-lineages, its presence today often reflects ancient local continuity, drift, and limited founder effects, rather than a single historically documented migration.

Reported or plausible regions include:

  • Western Europe, including the British Isles, France, Iberia, and the Low Countries
  • Southern Europe, including Italy and the Balkans
  • Anatolia and the Caucasus, where deep Eurasian paternal lineages often persist at low levels
  • The Levant and North Africa, likely through long-term regional admixture and ancient gene flow
  • Some Central Asian and steppe-adjacent populations, where old West Eurasian paternal lineages can survive in minority form

Because this lineage is uncommon, its distribution should be interpreted as patchy and probabilistic rather than diagnostic of any one population.

Historical and Cultural Significance

Unlike the famous R1b expansions associated with the Bronze Age and the spread of steppe-derived paternal ancestry in parts of Europe, R1b1a1b2 is more important as a phylogenetic and historical anchor. It represents the kind of deep ancestry that helps researchers reconstruct the prehistory of western Eurasian male lineages before the rise of large, later-successful clades.

Its persistence across widely separated regions suggests that:

  • ancestral R1b diversity was once more widespread than the modern distribution of major downstream branches indicates;
  • later demographic events repeatedly reshaped Y-chromosome variation, leaving only scattered remnants of older lineages;
  • low-frequency survival of such clades can illuminate population continuity across the Mesolithic, Neolithic, and Bronze Age transitions.

Conclusion

R1b1a1b2 is a rare, ancient subclade of the western Eurasian R1b tree that likely formed long before the major historical expansions of R1b in Europe. Its modern pattern of low-frequency, geographically broad occurrence makes it a useful marker for studying deep paternal ancestry, population structure, and the survival of prehistoric Y-chromosome diversity.

Wichtige Punkte

  • Origins and Evolution
  • Subclades
  • Geographical Distribution
  • Historical and Cultural Significance
  • Conclusion
Referenzprofil

Baum und Verwandtschaft

Phylogenetischer Kontext und Subkladen

Entwicklungsweg

Folgen Sie den erfassten übergeordneten Zweigen bis R1B1A1B2. Die Daten sind Schätzungen und können sich ändern, wenn Referenzdaten überarbeitet werden.

Schritte Haplogruppe Altersschätzung Archäologische Epoche Vergangene Zeit Unmittelbare Nachkommen Getestete moderne Nachkommen Antike Verknüpfungen
1 R1B1A1B2 Aktuell ~15,000 years ago Mesolithic 15,000 Jahre 1 0 0
2 R1B1A1B ~18,000 years ago Mesolithic 18,000 Jahre 2 2,317 31
3 R1B1A1 ~18,000 years ago Mesolithic 18,000 Jahre 2 2,321 0
4 R1B1A ~18,000 years ago Mesolithic 18,000 Jahre 2 4,020 39
5 R1B1 ~18,000 years ago Mesolithic 18,000 Jahre 2 4,166 0
6 R1b ~20,000 years ago Mesolithic 20,000 Jahre 2 4,262 126

Geschwisterzweige (1)

Weitere Zweige derselben übergeordneten Haplogruppe

Referenzprofil

Verbreitung weltweit

Geografische Verbreitung und moderne Präsenz

Erfasster Ursprung

West Eurasia

Moderne Verbreitung

The populations where Y-DNA haplogroup R1b1a1b2 is found include:

  1. Irish and British populations
  2. French, Iberian, and Low Countries populations
  3. Italian and Balkan populations
  4. Caucasus and Anatolian populations
  5. Levantine and North African populations
  6. Some Central Asian and steppe-related populations

Regionale Präsenz

Western Europe High
Iberian Peninsula High
Central Europe Moderate
Eastern Europe Low
North Africa (coastal) Low
Near East / Caucasus Low
Central Asia Low
North America (diaspora) Low
Southern Europe Low
Anatolia Low
Caucasus Low
Levant Low
North Africa Low
Historischer Kontext

Ein Zweig durch die Zeit

Geschätzte Entstehung in einer breiten historischen Zeitleiste. Zeitmarken liefern Kontext und implizieren keine Verbindung zu bestimmten Kulturen.

  1. ~20k Jahre zurück

    Letztes glaziales Maximum

    Höhepunkt der letzten Eiszeit, isolierte Bevölkerungen

  2. ~15k Jahre zurück

    Haplogruppe R1B1A1B2

    Geschätzte Entstehung dieses Y-DNA-Zweigs; Daten und Orte sind Referenzschätzungen.

    Dieser Zweig
  3. ~10k Jahre zurück

    Neolithische Revolution

    Beginn der Landwirtschaft und feste Siedlungen

  4. ~5k Jahre zurück

    Bronzezeit

    Metallverarbeitung, Schrift und frühe Zivilisationen

  5. ~3k Jahre zurück

    Eisenzeit

    Eisenwerkzeuge und ausgedehnte Handelsnetze

  6. ~2.5k Jahre zurück

    Klassische Antike

    Blüte griechischer und römischer Kulturen

  7. Gegenwart

    Gegenwart

    Moderne Zeit

Referenzprofil

Archäologischer Kontext

Erfasste archäologische Zuordnungen für den Y-DNA-Zweig R1B1A1B2

Erfasste Zuordnungen

Diese Bezeichnungen beschreiben archäologische Kontexte erfasster Referenzproben mit Bezug zu R1B1A1B2. Eine Zuordnung bedeutet nicht, dass alle Träger einer Kultur angehörten oder einer bestimmten Migrationsroute folgten.

Afanasievo Culture Bulgarian Chalcolithic Denmark_Lillevasby_LN Romania_EBA_Yamnaya Russia_Altai_Eneolithic_Afanasievo Russia_Volgograd_EBA_Yamnaya-o Yamnaya Culture
Kulturzuordnungen basieren auf dem archäologischen Kontext antiker DNA-Proben und können regionale Verknüpfungen in bestimmten Zeiträumen widerspiegeln.
PATERNAL LINEAGE · ANCIENT DNA

Ancient lineage evidence map

Follow parent clades toward this branch and explore where ancient carriers were found.

Loading ancient observations…

Markers are archaeological find locations. A dashed connector is an uncertain, proposed geographic transition between consecutive branches supported by multiple dated observations; it is not an exact travel route, birthplace or proof of direct descent. Parent-clade samples may belong to other descendant branches. Gaps remain where evidence is insufficient. Sample dates differ from haplogroup formation dates.

Daten

Daten und Herkunft

Quellenangaben und Datenqualität

Zuletzt aktualisiert 2026-06-17
Konfidenzwert 50/100
Abdeckung Low

Datenquelle

Klassifikation, geschätzte Daten und geografischer Kontext spiegeln die erfassten Referenzdaten wider und können sich bei überarbeiteten Belegen ändern. Die Probenabdeckung ist ungleichmäßig; erfasste Orte und archäologische Zuordnungen begründen weder persönliche Herkunft noch kulturelle Identität.