Geohistorical records of the Anthropocene in Chile

Author:

Gayo Eugenia M.123,McRostie Virginia B.4,Campbell Roberto4,Flores Carola156,Maldonado Antonio576,Uribe-Rodriguez Mauricio8,Moreno Patricio I.19,Santoro Calogero M.10,Christie Duncan A.111,Muñoz Ariel A.112,Gallardo Laura113

Affiliation:

1. Center for Climate and Resilience Research (CR2, FONDAP 15110009), CL

2. Laboratory for Stable Isotope Biogeochemistry, Departamento de Oceanografía, Universidad de Concepción, Concepción, CL

3. Center of Applied Ecology and Sustainability (CAPES), CL

4. Programa de Antropología, Instituto de Sociología, Pontificia Universidad Católica de Chile, Santiago, CL

5. Centro de Estudios Avanzados en Zonas Áridas (CEAZA), La Serena, CL

6. Departamento de Biología Marina, Universidad Católica del Norte, Coquimbo, CL

7. Instituto de Investigación Multidisciplinario en Ciencia y Tecnología, Universidad de La Serena, La Serena, CL

8. Departamento de Antropología, Facultad de Ciencias Sociales, Universidad de Chile, Santiago, CL

9. Instituto de Ecología y Biodiversidad, Departamento de Ciencias Ecológicas, Universidad de Chile, Santiago, CL

10. Instituto de Alta Investigación, Universidad de Tarapacá, Arica, CL

11. Instituto de Conservación Biodiversidad y Territorio, Universidad Austral de Chile, Valdivia, CL

12. Institute of Geography, Pontificia Universidad Católica de Valparaíso, Valparaiso, CL

13. Departamento de Geofísica, Universidad de Chile, Santiago, CL

Abstract

The deep-time dynamics of coupled socio-ecological systems at different spatial scales is viewed as a key framework to understand trends and mechanisms that have led to the Anthropocene. By integrating archeological and paleoenvironmental records, we test the hypothesis that Chilean societies progressively escalated their capacity to shape national biophysical systems as socio-cultural complexity and pressures on natural resources increased over the last three millennia. We demonstrate that Pre-Columbian societies intentionally transformed Chile’s northern and central regions by continuously adjusting socio-cultural practices and/or incorporating technologies that guaranteed resource access and social wealth. The fact that past human activities led to cumulative impacts on diverse biophysical processes, not only contradicts the notion of pristine pre-Industrial Revolution landscapes, but suggests that the Anthropocene derives from long-term processes that have operated uninterruptedly since Pre-Columbian times. Moreover, our synthesis suggests that most of present-day symptoms that describe the Anthropocene are rooted in pre-Columbian processes that scaled up in intensity over the last 3000 years, accelerating after the Spanish colonization and, more intensely, in recent decades. The most striking trend is the observed coevolution between the intensity of metallurgy and heavy-metal anthropogenic emissions. This entails that the Anthropocene cannot be viewed as a universal imprint of human actions that has arisen as an exclusive consequence of modern industrial societies. In the Chilean case, this phenomenon is intrinsically tied to historically and geographically diverse configurations in society-environment feedback relationships. Taken collectively with other case studies, the patterns revealed here could contribute to the discussion about how the Anthropocene is defined globally, in terms of chronology, stratigraphic markers and attributes. Furthermore, this deep-time narrative can potentially become a science-based instrument to shape better-informed discourses about the socio-environmental history in Chile. More importantly, however, this research provides crucial “baselines” to delineate safe operating spaces for future socio-ecological systems.

Publisher

University of California Press

Subject

Atmospheric Science,Geology,Geotechnical Engineering and Engineering Geology,Ecology,Environmental Engineering,Oceanography

Reference282 articles.

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