TY - JOUR
T1 - IZAPA'S INDUSTRIAL HINTERLAND
T2 - The EASTERN SOCONUSCO MANGROVE ZONE during ARCHAIC and FORMATIVE TIMES
AU - Neff, Hector
AU - Burger, Paul H.
AU - Culleton, Brendan James
AU - Kennett, Douglas James
AU - Jones, John G.
PY - 2018/9/1
Y1 - 2018/9/1
N2 - Archaeological survey and excavations in the mangrove-estuary zone south of Izapa have generated an understanding of how the environment and human exploitation patterns changed during the Archaic and Formative periods. Archaic-period archaeological remains are not present, but the sedimentary record shows that Archaic people were clearing the coastal-plain forest for agricultural purposes. This activity augmented delivery of sediments to the littoral zone, which expanded the mangrove forest and created a productive environment that could be colonized by Early Formative villagers by around 1600 cal b.c. Population growth during the Early Formative created conditions that favored emergence of specialized pyro-industries, especially salt production, by around 1000 cal b.c. Production intensity increased thereafter, especially during the Late Formative period, coincident with the apogee of Izapa. Salt production became more episodic during the Terminal Formative period, when interior populations were declining to a nadir after cal a.d. 250.
AB - Archaeological survey and excavations in the mangrove-estuary zone south of Izapa have generated an understanding of how the environment and human exploitation patterns changed during the Archaic and Formative periods. Archaic-period archaeological remains are not present, but the sedimentary record shows that Archaic people were clearing the coastal-plain forest for agricultural purposes. This activity augmented delivery of sediments to the littoral zone, which expanded the mangrove forest and created a productive environment that could be colonized by Early Formative villagers by around 1600 cal b.c. Population growth during the Early Formative created conditions that favored emergence of specialized pyro-industries, especially salt production, by around 1000 cal b.c. Production intensity increased thereafter, especially during the Late Formative period, coincident with the apogee of Izapa. Salt production became more episodic during the Terminal Formative period, when interior populations were declining to a nadir after cal a.d. 250.
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U2 - 10.1017/S0956536118000299
DO - 10.1017/S0956536118000299
M3 - Review article
AN - SCOPUS:85059853132
SN - 0956-5361
VL - 29
SP - 395
EP - 411
JO - Ancient Mesoamerica
JF - Ancient Mesoamerica
IS - 2
ER -