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dc.contributor.authorAmano, Noel-
dc.contributor.authorFaulkner, Patrick-
dc.contributor.authorWedage, Oshan-
dc.contributor.authorClarkson, Chris-
dc.contributor.authorAmila, Dambara-
dc.contributor.authorVal Blanco, Miren del-
dc.contributor.authorJurkenas, Dovydas-
dc.contributor.authorKapukotuwa, Alexander-
dc.contributor.authorLópez, Gloria I.-
dc.contributor.authorParés, Josep María-
dc.contributor.authorPathmalal, M. M.-
dc.contributor.authorSmith, Tam-
dc.contributor.authorWright, Martin-
dc.contributor.authorRoberts, Patrick-
dc.contributor.authorPetraglia, Michael-
dc.contributor.authorBoivin, Nicole-
dc.date.accessioned2024-09-16-
dc.date.accessioned2024-11-05T10:07:56Z-
dc.date.issued2024-11-
dc.identifier.citationScientific Reports, 2024,14(1), 26693es_ES
dc.identifier.issn2045-2322-
dc.identifier.urihttps://cir.cenieh.es/handle/20.500.12136/3338-
dc.description.abstractThe island of Sri Lanka was part of the South Asian mainland for the majority of the past 115,000 years, and connected most recently during the Last Glacial Maximum via the now submerged Palk Strait. The degree to which rising sea levels shaped past human adaptations from the Pleistocene and into the mid to late Holocene in Sri Lanka has remained unclear, in part because the earliest reliable records of human occupation come from the island's interior, where cave sites have revealed occupation of tropical forest ecosystems extending back to 48 thousand years (ka). The island's earliest known open-air sites are all much younger in date, with ages beginning at 15 ka and extending across the Holocene. Here we report the earliest well-dated open-air coastal site in Sri Lanka, Pathirajawela, which records human occupation back to ca. 25,000 years ago. We show that humans at Pathirajawela consistently adapted to changing ecosystems linked to sea level transgression and coastal evolution from the Last Glacial Maximum into the Holocene. The presence of anthropogenic shell midden deposits at the site from ca. 4.8 ka, focused almost exclusively on a single taxon, indicates intensification of estuarine resource exploitation, as humans responded to opportunities presented by the formation of new coastal ecosystems.es_ES
dc.description.sponsorshipThe excavation of Pathirajawela was funded by the Max Planck Society and the University of Sri Jayewardenepura. The analyses of the shell deposits were initially funded by University of Sydney Faculty of Arts and Social Sciences Research Support Scheme and School Research Support Scheme grants in 2019. MW received funding from the Carlyle Greenwell Research Scholarship in Archaeology at the University of Sydney. PF is the recipient of an Australian Research Council Future Fellowship (FT200100464). Approvals for this research were granted by the Director General, Department of Archaeology, and the Director General, Department of Wildlife Conservation. We acknowledge K. K. Ruwan Pramod, P. G. Gunadasa, H. K. Suranga Jayasinghe, Tiran Ananda, Suranga Lakmal, Sadun Sri Kalpa and Manjula Pushapakumara of the Department of Archaeology, Government of Sri Lanka for their support during our fieldwork. We dedicate this paper to Professor Siran Deraniyagala, a pioneer of research into the prehistory of Sri Lanka. Prof. Deraniyagala graciously supported our project and visited us in Pathirajawela, relaying unpublished first-hand information from his 1970s excavations that helped us during our excavation of the sitees_ES
dc.language.isoenes_ES
dc.publisherNature Portfolioes_ES
dc.rightsinfo:eu-repo/semantics/openAccesses_ES
dc.rightsAtribución 4.0 International (CC BY 4.0)*
dc.rights.urihttps://creativecommons.org/licenses/by/4.0/*
dc.subjectSri Lankan coastales_ES
dc.subjectPleistocenees_ES
dc.subjectHolocenees_ES
dc.subjectGlacial Maximumes_ES
dc.subjectExcavation of Pathirajawelaes_ES
dc.subjectLithic materialses_ES
dc.titleEarly Sri Lankan coastal site tracks technological change and estuarine resource exploitation over the last ca. 25,000 yearses_ES
dc.typeArticlees_ES
dc.identifier.doi10.1038/s41598-024-77504-5-
dc.relation.publisherversionhttps://doi.org/10.1038/s41598-024-77504-5es_ES
dc.date.available2024-11-05T10:07:56Z-
Aparece en las colecciones: Arqueomagnetismo
Datación por Luminiscencia
Geocronología y Geología



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