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Y-DNA · Väterliche Linie

C1B2A1

Y-DNA Haplogroup C1B2A1

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 C1B2A1

Origins and Evolution

Y-DNA haplogroup C1B2A1 is a derived subclade of C1B2A, itself nested within the broader C1b2 branch. Given the phylogenetic position of C1B2A and observed geographic concentrations, C1B2A1 most plausibly originated in the Wallacea region (eastern Indonesia / Island Southeast Asia) during the transition from the Late Pleistocene into the Early Holocene (on the order of ~14 kya in this account). Its emergence represents a continuation of deep Paleolithic male lineages that were established in Island Southeast Asia and Near Oceania during the late Pleistocene coastal and island colonization events.

Divergence of C1-derived lineages in Wallacea and Near Oceania is compatible with a model in which early C lineages spread along island chains and coastal refugia, with C1B2A1 forming as a localized branch that later contributed to the paternal pool of both Wallacean islanders and populations east into Near Oceania.

Subclades (if applicable)

At present, available population and phylogenetic data indicate C1B2A1 contains further downstream diversity that is primarily localized and often private to island populations. Many of these downstream variants have low sample counts in published databases, reflecting limited sampling and the patchy preservation of ancient DNA in tropical island contexts. Future high-resolution sequencing and targeted surveys are likely to further resolve regional subbranches that distinguish populations of Sulawesi, the Maluku Islands, Nusa Tenggara, and Near Oceanian islands.

Geographical Distribution

C1B2A1 shows a strongly island-centered distribution concentrated in Wallacea and parts of Near Oceania. Modern and population-genetic surveys report the haplogroup at high to moderate frequencies in eastern Indonesian islands (Sulawesi, Maluku, Nusa Tenggara) and detectable frequencies in Near Oceanian groups (Papua New Guinea, Bismarck Archipelago, Solomon Islands). The lineage is also observed at lower frequencies among some Melanesian groups, coastal Austronesian-speaking communities in eastern Indonesia, and sporadically in the Philippines, Taiwan, and southern Japan — consistent with maritime contact, Austronesian expansion, and later admixture. Trace occurrences appear in diasporic and admixed Southeast Asian groups.

The restriction of higher frequencies to island and coastal populations is consistent with a history of maritime mobility, founder effects on islands, and long-term genetic continuity of male lineages in relatively isolated island communities.

Historical and Cultural Significance

C1B2A1 is informative for reconstructing human prehistory in a complex contact zone where deep Paleolithic lineages met expanding Holocene groups. The pattern — localized deep-rooting paternal lineages persisting into the present — aligns with archaeological and linguistic evidence for long-term occupation of Wallacea and Near Oceania by pre-Austronesian hunter-gatherer populations and later admixture with Austronesian-speaking farmers and Lapita-associated communities. Where C1B2A1 is present at appreciable frequency, it often marks paternal ancestry that predates the Austronesian agricultural expansion, making it useful for disentangling pre-Neolithic substrata from later demic movements in genetic studies.

Because ancient DNA from tropical islands is sparse, interpretations rely heavily on modern population sampling and comparisons to better-sampled Papuan and Melanesian groups. The haplogroup therefore serves as a target for future genetic and archaeological integration to better resolve timing and routes of island dispersals.

Conclusion

Y-DNA haplogroup C1B2A1 is a regionally important paternal lineage in Wallacea and Near Oceania that preserves a signal of late Pleistocene–Early Holocene island colonization and subsequent interaction with Holocene migrations. Its present distribution — concentrated in island Southeast Asia and parts of Near Oceania with scattered occurrences elsewhere — reflects a history of maritime settlement, founder effects on islands, and later admixture with Austronesian and other regional populations. Continued high-resolution Y-chromosome sequencing and expanded sampling in underrepresented islands will clarify its internal structure and deepen understanding of island prehistory.

Wichtige Punkte

  • Origins and Evolution
  • Subclades (if applicable)
  • Geographical Distribution
  • Historical and Cultural Significance
  • Conclusion
Referenzprofil

Baum und Verwandtschaft

Phylogenetischer Kontext und Subkladen

Entwicklungsweg

Folgen Sie den erfassten übergeordneten Zweigen bis C1B2A1. 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 C1B2A1 Aktuell ~14,000 years ago Mesolithic 14,000 Jahre 0 4 0
2 C1B2A ~18,000 years ago Mesolithic 18,000 Jahre 1 7 0
3 C1B2 ~28,000 years ago Paleolithic 28,000 Jahre 1 7 0
4 C1B ~35,000 years ago Paleolithic 35,000 Jahre 2 28 0
5 C1 ~45,000 years ago Paleolithic 45,000 Jahre 2 92 0
6 C ~60,000 years ago Paleolithic 60,000 Jahre 3 406 35

Subkladen (0)

Endzweig ohne erfasste Subkladen

Referenzprofil

Verbreitung weltweit

Geografische Verbreitung und moderne Präsenz

Erfasster Ursprung

Wallacea (Island Southeast Asia)

Moderne Verbreitung

The populations where Y-DNA haplogroup C1B2A1 is found include:

  1. Wallacean island populations (e.g., Sulawesi, Maluku, Nusa Tenggara)
  2. Near Oceanian groups (Papua New Guinea, Bismarck Archipelago, Solomon Islands)
  3. Melanesian populations at varying frequencies
  4. Austronesian-speaking coastal communities in eastern Indonesia
  5. Selected insular South Asian/Timorese populations at low frequency
  6. Sporadic occurrences in parts of the Philippines, Taiwan, and southern Japan
  7. Diasporic or admixed groups across Southeast Asia and Oceania (trace occurrences)

Regionale Präsenz

Near Oceania / Melanesia High
Australia (Indigenous groups) Moderate
Southeast Asia (eastern islands / Wallacea) Low
Near Oceania (Papua New Guinea, Bismarcks, Solomon Islands) Moderate
Melanesia (wider) Moderate
East Asia (Philippines, Taiwan, southern Japan) Low
Insular South Asia (Timor and nearby islands) 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. ~14k Jahre zurück

    Haplogruppe C1B2A1

    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 C1B2A1

Erfasste Zuordnungen

Diese Bezeichnungen beschreiben archäologische Kontexte erfasster Referenzproben mit Bezug zu C1B2A1. Eine Zuordnung bedeutet nicht, dass alle Träger einer Kultur angehörten oder einer bestimmten Migrationsroute folgten.

1983 Ancient Polynesian Botocudo Historic Polynesian Hoabinhian Late Vanuatu Post-Lapita Vanuatu Saudeleur Culture Vanuatu Historical
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 2026-06-15
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.