Articles | Volume 14, issue 8
Clim. Past, 14, 1253–1273, 2018
Clim. Past, 14, 1253–1273, 2018
Research article
 | Highlight paper
20 Aug 2018
Research article  | Highlight paper | 20 Aug 2018

Climate impact on the development of Pre-Classic Maya civilisation

Kees Nooren et al.

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Cited articles

Akers, P. D., Brook, G. A., Railsback, L. B., Liang, F., Iannone, G., Webster, J. W., Reeder, P. P., Cheng, H., and Edwards, R. L.: An extended and higher-resolution record of climate and land use from stalagmite MC01 from Macal Chasm, Belize, revealing connections between major dry events, overall climate variability, and Maya sociopolitical changes, Palaeogeogr. Palaeocl., 459, 268–288, 2016. 
Amador, J. A., Alfaro, E. J., Lizano, O. G., and Magaña, V. O.: Atmospheric forcing of the eastern tropical Pacific: A review, Prog. Oceanogr., 69, 101–142, 2006. 
Anselmetti, F. S., Hodell, D. A., Ariztegui, D., Brenner, M., and Rosenmeier, M. F.: Quantification of soil erosion rates related to ancient Maya deforestation, Geology, 35, 915–918, 2007. 
Arnold III, P. J.: Settlement and subsistence among the Early Formative Gulf Olmec, J. Anthropol. Archaeol., 28, 397–411, 2009. 
Banco Nacional de Datos de Aguas Superficiales, Conagua: os/Portada BANDAS.htm, last access: January 2017. 
Short summary
We present two new palaeoclimatic records for the central Maya lowlands, adding valuable new insights to the impact of climate change on the development of Maya civilisation. Lake Tuspan's diatom record is indicative of precipitation changes at a local scale, while a beach ridge elevation record from the world's largest late Holocene beach ridge plain provides a regional picture.