The Evolution of Agrarian Landscapes in the Tropical Andes

被引:0
|
作者
Shadik, Courtney R. [1 ]
Bush, Mark B. [1 ]
Valencia, Bryan G. [2 ]
Rozas-Davila, Angela [1 ]
Plekhov, Daniel [3 ]
Breininger, Robert D. [1 ]
Davin, Claire [4 ]
Benko, Lindsay [1 ]
Peterson, Larry C. [5 ]
Vanvalkenburgh, Parker [6 ]
机构
[1] Florida Inst Technol, Inst Global Ecol, Melbourne, FL 32901 USA
[2] Univ Reg Amazon Ikiam, Fac Ciencias Tierra & Agua, Ikiam 150150, Ecuador
[3] Portland State Univ, Dept Anthropol, Portland, OR 97201 USA
[4] Univ Richmond, Dept Math, Richmond, VA 23173 USA
[5] Univ Miami, Rosenstiel Sch Marine Atmospher & Earth Sci, Miami, FL 33149 USA
[6] Brown Univ, Dept Anthropol, Providence, RI 02915 USA
来源
PLANTS-BASEL | 2024年 / 13卷 / 07期
关键词
climate change; fossil pollen; lake sediment; terracing; crops; pastoralism; Sporormiella; charcoal; XRF; HOLOCENE CLIMATE-CHANGE; ENVIRONMENTAL-CHANGES; VEGETATION CHANGE; PERUVIAN ANDES; LAKE TITICACA; HIGHLANDS; SEDIMENTS; HISTORY; RECORD; DOMESTICATION;
D O I
10.3390/plants13071019
中图分类号
Q94 [植物学];
学科分类号
071001 ;
摘要
Changes in land-use practices have been a central element of human adaptation to Holocene climate change. Many practices that result in the short-term stabilization of socio-natural systems, however, have longer-term, unanticipated consequences that present cascading challenges for human subsistence strategies and opportunities for subsequent adaptations. Investigating complex sequences of interaction between climate change and human land-use in the past-rather than short-term causes and effects-is therefore essential for understanding processes of adaptation and change, but this approach has been stymied by a lack of suitably-scaled paleoecological data. Through a high-resolution paleoecological analysis, we provide a 7000-year history of changing climate and land management around Lake Acopia in the Andes of southern Peru. We identify evidence of the onset of pastoralism, maize cultivation, and possibly cultivation of quinoa and potatoes to form a complex agrarian landscape by c. 4300 years ago. Cumulative interactive climate-cultivation effects resulting in erosion ended abruptly c. 2300 years ago. After this time, reduced sedimentation rates are attributed to the construction and use of agricultural terraces within the catchment of the lake. These results provide new insights into the role of humans in the manufacture of Andean landscapes and the incremental, adaptive processes through which land-use practices take shape.
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页数:19
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