Image - Cacao Pod Vessel - K6706 © Justin Kerr FAMSI © 2001:
Marion Popenoe de Hatch
 

Paleoclimatic Variation in the Valley of Guatemala during Precolumbian Times

AMS C14 Dates

In December we received the AMS radiocarbon dates from the Amatitlán cores, for which we are deeply indebted to the Center for Accelerator Mass Spectrometry at the Lawrence Livermore National Laboratory.

Location Depth C14 Date Approx. Cal. Year
AM-13-III-00 419-421 cm 660 ± 60 1290 A.D.
AM-14-III-00 541-543 cm 1650 ± 50 300 A.D.
AM-15-III-00 240 cm 710 ± 50 1240 A.D.
340 cm 2910 ± 130 960 B.C. (anomaly)
440 cm 1530 ± 190 420 A.D.
540 cm 2010 ± 100 60 A.D.
610 cm 2340 ± 110 390 B.C.
690 cm 2570 ± 40 620 B.C.

The dates are in general quite young, ranging from around 600 B.C. to sometime between 1200 and 1300 A.D.  The AM-15-III-00 date is apparently an anomaly, probably a reflection of the high sedimentation rates in the lake area. Although the dates will provide little information regarding post-Pleistocene climate changes, they will be highly relevant for correlating any climatic variation which may have affected the Kaminaljuyú irrigation system which existed between 600 B.C. and 200 A.D.

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