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Early human impacts and ecosystem reorganization in southern-central Africa

Modern Homo sapiens engage in substantial ecosystem modification, but it is difficult to detect the origins or early consequences of these behaviors. Archaeological, geochronological, geomorphological, and paleoenvironmental data from northern Malawi document a changing relationship between forager...

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Detalles Bibliográficos
Autores principales: Thompson, Jessica C., Wright, David K., Ivory, Sarah J., Choi, Jeong-Heon, Nightingale, Sheila, Mackay, Alex, Schilt, Flora, Otárola-Castillo, Erik, Mercader, Julio, Forman, Steven L., Pietsch, Timothy, Cohen, Andrew S., Arrowsmith, J. Ramón, Welling, Menno, Davis, Jacob, Schiery, Benjamin, Kaliba, Potiphar, Malijani, Oris, Blome, Margaret W., O’Driscoll, Corey A., Mentzer, Susan M., Miller, Christopher, Heo, Seoyoung, Choi, Jungyu, Tembo, Joseph, Mapemba, Fredrick, Simengwa, Davie, Gomani-Chindebvu, Elizabeth
Formato: Online Artículo Texto
Lenguaje:English
Publicado: American Association for the Advancement of Science 2021
Materias:
Acceso en línea:https://www.ncbi.nlm.nih.gov/pmc/articles/PMC8099189/
https://www.ncbi.nlm.nih.gov/pubmed/33952528
http://dx.doi.org/10.1126/sciadv.abf9776
Descripción
Sumario:Modern Homo sapiens engage in substantial ecosystem modification, but it is difficult to detect the origins or early consequences of these behaviors. Archaeological, geochronological, geomorphological, and paleoenvironmental data from northern Malawi document a changing relationship between forager presence, ecosystem organization, and alluvial fan formation in the Late Pleistocene. Dense concentrations of Middle Stone Age artifacts and alluvial fan systems formed after ca. 92 thousand years ago, within a paleoecological context with no analog in the preceding half-million-year record. Archaeological data and principal coordinates analysis indicate that early anthropogenic fire relaxed seasonal constraints on ignitions, influencing vegetation composition and erosion. This operated in tandem with climate-driven changes in precipitation to culminate in an ecological transition to an early, pre-agricultural anthropogenic landscape.