4.8 Article

Early human impacts and ecosystem reorganization in southern-central Africa

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SCIENCE ADVANCES
卷 7, 期 19, 页码 -

出版社

AMER ASSOC ADVANCEMENT SCIENCE
DOI: 10.1126/sciadv.abf9776

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资金

  1. National Geographic-Waitt Foundation [W115-785 10]
  2. Australian Research Council Discovery Project [DP110101305]
  3. Wenner-Gren Foundation [8539]
  4. University of Queensland Archaeological Field School
  5. Korean Research Foundation Global Research Network Grant [2012032907]
  6. Deutsche Forschungsgemeinschaft [MI 1748/3-1, ME 4406/1-1]
  7. Emory University
  8. Belmont Forum [1929563]
  9. Purdue University
  10. Research Council of Norway, through its Centres of Excellence funding scheme, SFF Centre for Early Sapiens Behaviour (SapienCE) [262618]
  11. Canadian Social Sciences and Humanities Research Council [895-2016-1017]
  12. Institute of Human Origins and Hyde Family Foundations
  13. International Continental Scientific Drilling Program
  14. [NSF-EAR-0602350]

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Archaeological and environmental data from northern Malawi reveal that early Homo sapiens started significant ecosystem modifications during the Late Pleistocene, with the use of fire and climate changes leading to an ecological transition to an early anthropogenic landscape.
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.

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