TY - JOUR
T1 - Development and Disintegration of Maya Political Systems in Response to Climate Change
AU - Kennett, Douglas
AU - Breitenbach, Sebastian
AU - Aquino, Valorie V.
AU - Asmerom, Yemane
AU - Awe, Jaime
AU - Baldini, James
AU - Bartlein, P.
AU - Culleton, Brendan
AU - Ebert, C.
AU - Jazwa, Chris
AU - Macri, M.
AU - Marwan, Norbert
AU - Polyak, Victor
AU - Prufer, Keith
AU - Ridley, Harriet
AU - Sodemann, Harald
AU - Winterhalder, B.
AU - Haug, Gerald
PY - 2012/11/9
Y1 - 2012/11/9
N2 - The role of climate change in the development and demise of Classic Maya civilization (300 to 1000 C.E.) remains controversial because of the absence of well-dated climate and archaeological sequences. We present a precisely dated subannual climate record for the past 2000 years from Yok Balum Cave, Belize. From comparison of this record with historical events compiled from well-dated stone monuments, we propose that anomalously high rainfall favored unprecedented population expansion and the proliferation of political centers between 440 and 660 C.E. This was followed by a drying trend between 660 and 1000 C.E. that triggered the balkanization of polities, increased warfare, and the asynchronous disintegration of polities, followed by population collapse in the context of an extended drought between 1020 and 1100 C.E.
AB - The role of climate change in the development and demise of Classic Maya civilization (300 to 1000 C.E.) remains controversial because of the absence of well-dated climate and archaeological sequences. We present a precisely dated subannual climate record for the past 2000 years from Yok Balum Cave, Belize. From comparison of this record with historical events compiled from well-dated stone monuments, we propose that anomalously high rainfall favored unprecedented population expansion and the proliferation of political centers between 440 and 660 C.E. This was followed by a drying trend between 660 and 1000 C.E. that triggered the balkanization of polities, increased warfare, and the asynchronous disintegration of polities, followed by population collapse in the context of an extended drought between 1020 and 1100 C.E.
UR - https://www.scopus.com/pages/publications/84868531711
U2 - 10.1126/science.1226299
DO - 10.1126/science.1226299
M3 - Article
SN - 0036-8075
VL - 338
SP - 788
EP - 791
JO - Science
JF - Science
IS - 6108
ER -