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Environmental thresholds and the empirical reality of state collapse: a response to Erickson (1999)

Published online by Cambridge University Press:  02 January 2015

Alan L. Kolata ,
Michael W. Binford ,
Mark Brenner ,
John W. Janusek  and
Charles Ortloff
Alan L. Kolata
Affiliation:
Department of Anthropology, University of Chicago, Chicago IL 60637, USA [email protected]
Michael W. Binford
Affiliation:
Department of Geography, University of Florida, Gainesville FL 32611, USA [email protected]
Mark Brenner
Affiliation:
Department of Fisheries & Aquatic Sciences, University of Florida, Gainesville FL 32653, USA [email protected]
John W. Janusek
Affiliation:
Department of Anthropology, Vanderbilt University, Nashville, TN 37235 USA [email protected]
Charles Ortloff
Affiliation:
Corporate Technology Center/United Defense, 1205 Coleman Avenue, Santa Clara, CA 95052, USA [email protected]
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Extract

We are grateful for the opportunity to respondto Erickson's (1999) critique of our articles onhuman-environment interactions in the LakeTiticaca basin of Bolivia (Ortloff & Kolata 1993;Abbott et al. 1997; Binford et al. 1997). Hisdecision to publish this critique in ANTIQUITY,rather than in the journals in which our articlesappeared, permits us to reach a broaderaudience. Erickson labels our interpretationsa form of 'neo-environmental determinism', buthis rejection of our conclusions stems fromserious misunderstandings and is misleadingto readers who have not examined our originaldata. He (p. 634) claims:1 our research represents 'simplistic reductionistthinking' that treats humans as 'passivepawns' of environmental change;2 our dating of the chronic drought in the Andeanaltiplano after AD 1150 is impreciseand not correlated with the 12th-centurydisintegration of the Tiwanaku state; and3 the drought did not affect intensive agriculturalproduction.

Type
Papers
Information
Antiquity , Volume 74 , Issue 284 , June 2000 , pp. 424 - 426
Copyright
Copyright © Antiquity Publications Ltd. 2000

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References

Abbott, M., Binford, M. Brenner, M. & Kelts, K.. 1997. A3,500 14 C yr high-resolution sediment record of lake level changes in Lake Titicaca, Bolivia/Peru, Quaternary Research 47(2): 169–80.Google Scholar
Biesboer, D., Binford, M. & Kolata, A.. 1999. Nitrogen fixation in soils and canals of rehabilitated raised fields in the Bolivian altiplano, Biotropica 31: 255–67.Google Scholar
Binford, M., Kolata, A. Brenner, M. Janusek, J. Seddon, M. Abbott, M. & Curtis, J.. 1997. Climate variation and the rise and fall of an Andean civilization, Quaternary Research 47: 235–48.Google Scholar
Carney, H.J., Binford, M. Kolata, A. Marin, R. & Goldman, C.. 1993. Nutrient and sediment retention in Andean raised-field agriculture. Nature 364: 131–3.Google Scholar
Erickson, C. 1988. An archaeological investigation of raised fields in the Lake Titicaca Basin of Peru. Unpublished Ph.D dissertation, Department of Anthropology, University of Illinois, Champaign-Urbana (IL).Google Scholar
Erickson, C. 1999. Neo-environmental determinism and agrarian ‘collapse’ in Andean prehistory, Antiquity 73: 634–42.Google Scholar
Kolata, A. & Ortloff, C.. 1996. Agroecological perspectives on the decline of the Tiwanaku state, in Kolata, A. (ed.), Tiwanaku and its hinterland: archaeology and paleoecology of an Andean civilization 1:181–202. Washington (DC): Smithsonian Institution Press.Google Scholar
Ortloff, C. & Kolata, A. 1993. Climate and collapse: agroecological perspectives on the decline of the Tiwanaku state, Journal of Archaeological Science 20: 195–221.Google Scholar
Wirmann, D. & Oliveira Almeida, L.F.. 1987. Low Holocene level (7700 to 3650 years B.P.) of Lake Titicaca (Bolivia, South America), Palaeogeography, Palaeoclimatology, Palaeoecology 59:315–23.Google Scholar