STABLE CARBON AND NITROGEN ISOTOPE STUDIES IN THE PARANÁ RIVER DELTA (ARGENTINA): AN APPROACH TO PREHISPANIC DIETS

2017 ◽  
Vol 28 (1) ◽  
pp. 105-126 ◽  
Author(s):  
Mariano Bonomo ◽  
Clara Scabuzzo ◽  
Gustavo G. Politis ◽  
Alejandro F. Zucol

We focus on prehispanic paleodiets among the indigenous populations who inhabited the delta of the Paraná River during the Late Holocene. Stable isotope analyses of δ13C—from collagen and apatite fractions— and δ15N were performed on human bones from sites assigned to different archaeological entities (mainly Goya-Malabrigo and Guaraní). We contextualize the isotopic data with results from the study of zooarchaeological and archaeobotanical materials from these sites. The Guaraní case shows a greater reliance on C4plants (maize or wild C4plants). By contrast, for most Goya-Malabrigo individuals, δ13C values indicate a predominant consumption of C3plants that could include both domesticated and wild species. Through the integration of archaeofaunal, archaeobotanical, and isotopic information, we conclude that the Goya-Malabrigo case shows a mixed economy. Furthermore, small-scale horticulture of the maize-squash-bean triad supplemented a diet of wild resources procured through hunting, fishing, and gathering.

2016 ◽  
Vol 7 ◽  
pp. 18-27 ◽  
Author(s):  
Cheng-Yi Lee ◽  
Maa-Ling Chen ◽  
Peter Ditchfield ◽  
Li-Hung Lin ◽  
Pei-Ling Wang ◽  
...  

2017 ◽  
Vol 10 (8) ◽  
pp. 2123-2135 ◽  
Author(s):  
Chelsea Budd ◽  
Necmi Karul ◽  
Songül Alpaslan-Roodenberg ◽  
Alfred Galik ◽  
Rick Schulting ◽  
...  

2021 ◽  
Author(s):  
Robert Patalano ◽  
Jing Hu ◽  
Qing Leng ◽  
Weiguo Liu ◽  
Huanye Wang ◽  
...  

Abstract Plant material used in the construction of segments and beacon towers of the ancient Great Wall in northwestern China contain untapped potential for revealing paleoenvironmental conditions. Here, we characterize the molecular preservation and stable carbon and nitrogen isotope compositions of common reeds (Phragmites) collected from Great Wall fascines dated to the Han Dynasty in today’s Gansu and Xinjiang provinces using a combination of chromatographic techniques and isotope analyses. Our data demonstrates that ancient reeds were harvested from local habitats that were more diverse than exist today. The isotope data also capture differential rates of environmental deterioration along the eastern margin of the Tarim Basin, leading to the intense evaporative stress on modern plants. This study demonstrates the wealth of environmental and climate information obtainable from site-specific organic building material of ancient walls, which have received considerably less attention than the iconic brick and stone masonry walls of the later Ming Dynasty.


2008 ◽  
Vol 10 (3) ◽  
pp. 189-194 ◽  
Author(s):  
JC Denadai ◽  
C Ducatti ◽  
JR Sartori ◽  
AC Pezzato ◽  
C Móri ◽  
...  

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