Stalagmite evidence from Belize indicating significant droughts at the time of Preclassic Abandonment, the Maya Hiatus, and the Classic Maya collapse

Palaeogeography, Palaeoclimatology, Palaeoecology

Volumn 250, Issue 1-4, 2007, Pages 1-17

  Webster, James W ^a   Brook, George A ^b   Railsback, L Bruce ^b   Cheng, Hai ^c   Edwards, R Lawrence ^c   Alexander, Clark ^d   Reeder, Philip P ^e  

^a U S ENVIRONMENTAL PROTECTION AGENCY   (United States)

^b UNIVERSITY OF GEORGIA   (United States)

^c UNIVERSITY OF MINNESOTA   (United States)

^d Skidaway Institute of Oceangraphy   (United States)

^e UNIVERSITY OF SOUTH FLORIDA   (United States)

Author keywords

Belize; Caves; Classic Maya collapse; Drought; Paleoclimates; Stalagmites

Indexed keywords

CIVILIZATION; DROUGHT; PALEOCLIMATE; PALEOENVIRONMENT; PALEOGEOGRAPHY; POPULATION DENSITY; STABLE ISOTOPE; STALAGMITE;

BELIZE [CENTRAL AMERICA]; CENTRAL AMERICA;

EID: 34249340065     PISSN: 00310182     EISSN: None     Source Type: Journal    
DOI: 10.1016/j.palaeo.2007.02.022     Document Type: Article

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