The stream reach concept and the macro‐scale study of riverine agriculture in arid and semiarid environments

Datos Bibliográficos

ID12133751
AutoresFred L Nials (Archaeology Southwest, autor de correspondencia), David A Gregory (0000-0003-2489-5462, Archaeology Southwest), J Brett Hill (Archaeology Southwest)
Año2011
Volumen26
Número5
Páginas724-761
Fecha de publicación2011-08-04
Peer ReviewedSí
Open AccessSí
TipoARTICLE
RevistaGeoarchaeology (JOURNAL)
Identificadores de la revistaISSN: 0883-6353 • E-ISSN: 1520-6548
EditorialWiley (PUBLISHER • GB)
DOI10.1002/gea.20371
OpenAlexW1991165351
IdiomaEN
Citas recibidas21
Referencias citadas50

Maize agriculture appears to have been introduced into the semiarid southern part of the North American Southwest ca. 2200–2000 B.C., at a time when valley bottoms were aggrading. Although small‐scale, high‐risk agriculture might have been practiced in many landscape positions, valley‐bottom locations having particular geomorphic and/or hydrologic conditions would have provided the places most risk‐free for farming. These places, associated with what are here called reach boundaries, have conditions that cause elevated water tables or enhance stream discharge, and have floodplain areas suitable for farming. Reach boundaries are easily identified, are relatively predictable in location and occurrence, and are early settled and/or long occupied. Deposition has been the dominant process in most valley bottoms in the southern Southwest for the last ca. 6000 years. Many streams across the region, however, experienced approximately synchronous periods of erosion when deeply incised channels (arroyos) formed in valley bottoms. Each of these periods of erosion, except for that which began in the late 1800s, was followed by a longer period of arroyo‐filling and floodplain aggradation, completing a so‐called alluvial cycle. Valley‐bottom conditions related to alluvial cycles would have greatly influenced the location, water availability, water management technology, and yield of agricultural ventures. Here we identify more than 280 reach boundaries in parts of the middle and upper Gila River and Mimbres River watersheds in Arizona and New Mexico. Spatial analysis shows a strong 4000‐year‐long correspondence between reach boundaries and agricultural sites where data are available. Identification and characterization of these locations may prove useful for locating yet unknown, deeply buried early agricultural sites (ca. 2200 B.C.–A.D. 200), in addition to providing explanations for prehistoric settlement patterns through time. © 2011 Wiley Periodicals, Inc

Aggradation · Agriculture · Alluvial plain · Alluvium · Archaeology · Arid · Deposition (geology · Erosion · Floodplain · Fluvial · Geography · Geomorphology · Hydrology (agriculture · Sediment · STREAMS · Structural basin · Geology and Paleoclimatology Research · Hydrology and Sediment Transport Processes · Tree-ring climate responses · Geology