Investigating economic specialization on the central Peruvian coast: A reconstruction of Late Intermediate Period Ychsma diet using stable isotopes.

OBJECTIVES: Hypothetical models of socioeconomic organization in pre-Columbian societies generated from the rich ethnohistoric record in the New World require testing against the archaeological and bioarchaeological record. Here, we test ethnohistorian Maria Rostworowski's horizontality model of socioeconomic specialization for the Central Andean coast by reconstructing dietary practices in the Late Intermediate Period (c. AD 900-1470) Ychsma polity to evaluate complexities in social behaviors prior to Inka imperial influence. MATERIALS AND METHODS: Stable carbon and nitrogen isotope analysis of archaeological human bone collagen and apatite (δ13 Ccol[VPDB], δ15 Ncol[AIR] , δ13 Cap[VPDB] ) and locally available foods is used to reconstruct the diets of individuals from Armatambo (n = 67), associated ethnohistorically with fishing, and Rinconada Alta (n = 46), associated ethnohistorically with agriculture. RESULTS: Overall, mean δ15 Ncol[AIR] is significantly greater at Armatambo, while mean δ13 Ccol[VPDB] and mean δ13 Cap[VPDB] are not significantly different between the two sites. Within large-scale trends, adult mean δ13 Cap[VPDB] is significantly greater at Armatambo. In addition, nearly one-third of Armatambo adults and adolescents show divergent δ15 Ncol[AIR] values. DISCUSSION: These results indicate greater reliance on marine resources at Armatambo versus Rinconada Alta, supporting the ethnohistoric model of socioeconomic specialization for the Central Andean coast. Deviations from large-scale dietary trends suggest complexities not accounted for by the ethnohistoric model, including intra-community subsistence specialization and/or variation in resource access.

Formate as an energy source for microbial metabolism in chemosynthetic zones of hydrothermal ecosystems.

Formate, a simple organic acid known to support chemotrophic hyperthermophiles, is found in hot springs of varying temperature and pH. However, it is not yet known how metabolic strategies that use formate could contribute to primary productivity in hydrothermal ecosystems. In an effort to provide a quantitative framework for assessing the role of formate metabolism, concentration data for dissolved formate and many other solutes in samples from Yellowstone hot springs were used, together with data for coexisting gas compositions, to evaluate the overall Gibbs energy for many reactions involving formate oxidation or reduction. The result is the first rigorous thermodynamic assessment of reactions involving formate oxidation to bicarbonate and reduction to methane coupled with various forms of iron, nitrogen, sulfur, hydrogen, and oxygen for hydrothermal ecosystems. We conclude that there are a limited number of reactions that can yield energy through formate reduction, in contrast to numerous formate oxidation reactions that can yield abundant energy for chemosynthetic microorganisms. Because the energy yields are so high, these results challenge the notion that hydrogen is the primary energy source of chemosynthetic microbes in hydrothermal ecosystems.

Palaeococcus helgesonii sp. nov., a facultatively anaerobic, hyperthermophilic archaeon from a geothermal well on Vulcano Island, Italy.

A novel, hyperthermophilic archaeon was isolated from a shallow geothermal well that taps marine waters on the Island of Vulcano in the southern Tyrrhenian Sea, Italy. The cells were irregular cocci, 0.6-1.5 microm in diameter, with multiple polar flagella. Growth was observed at temperatures from 45 to 85 degrees C (optimum at approximately 80 degrees C), pH 5-8 (optimum at 6.5), and 0.5-6.0% NaCl (optimum at approximately 2.8%). The minimum doubling time was 50 min. The isolate was obligately chemoheterotrophic, utilizing complex organic compounds including yeast or beef extract, peptone, tryptone, or casein for best growth. The presence of elemental sulfur enhanced growth. The isolate grew anaerobically as well as microaerobically. The G+C content of the genomic DNA was 42.5 mol%. The 16S rRNA sequence indicated that the new isolate was a member of the Thermococcales within the euryarchaeota, representing the second species in the genus Palaeococcus. Its physiology and phylogeny differed in several key characteristics from those of Palaeococcus ferrophilus, justifying the establishment of a new species; the name Palaeococcus helgesonii sp. nov. is proposed, type strain PI1 (DSM 15127).