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The extracted microfossils from the dental calculus of ancient teeth are a new form of archaeological evidence which can provide direct information on the plant diet of a population. Here, we present the results of analyses of starch grains and phytoliths trapped in the dental calculus of humans who occupied the Bronze Age site of Shilinggang (∼2500 cal yr BP) in Yunnan Province, southwestern China. The results demonstrate that the inhabitants consumed a wide range of plants, including rice, millet, and palms, together with other food plants which have not previously been detected in Yunnan. The discovery of various underground storage organs (USOs; tubers, roots, bulbs, and rhizomes) and acorns complements the application of conventional macrofossil and isotope studies to understand the diet of the Bronze Age human population of Yunnan. The wide variety of plant foods consumed suggests that the inhabitants adopted a broad-spectrum strategy of gathering food and cultivating crops in northwest Yunnan Province in the late Bronze Age at a time when agricultural societies were developed in the central plains of China. [ABSTRACT FROM AUTHOR]

• The population trend of late Pleistocene-Holocene hunter-gatherers changed its trajectory ca. 2,300 cal years BP coincident with the adoption of domesticates. • After 2,300 cal years BP, a significant increase in human population occurred. We observe population increases ("booms") followed by notable drops ("busts"). • Stable isotope (ẟ13C) on human bone follow a similar trend, indicating an increased consumption of maize during the "boom" periods and a decreased consumption during the "bust" periods. • We propose that human population changes during the last 2,300 cal years BP correlate with levels of maize consumption. This paper explores the relationships between population change and human diet after the adoption of domesticated resources in northwest Mendoza, a subregion of central western Argentina (CWA). To estimate population, we used summed probability distributions of radiocarbon ages (RC-SPD). We used carbon and nitrogen stable isotope values (ẟ13C co , ẟ13C ca , and ẟ15N) obtained on human bone (collagen and carbonate) to reconstruct human diet. The population trend of late Pleistocene-Holocene hunter-gatherers changed its trajectory ca. 2300 cal years BP coincident with the adoption of domesticates. After this date, a significant increase in human population occurred. We observe population increases ("booms") followed by notable drops ("busts"). Stable isotopes (ẟ13C) on human bone follow a similar trend, indicating an increased consumption of maize during the "boom" periods and a decreased consumption during the "bust" periods. Based on the association between estimated changes in human population and changes in human bone isotope values over the last 2300 cal years BP, we propose that levels of maize consumption emerge from human predator–prey and plant-herbivore interactions. The use of maize, thus, is not part of a social evolutionary stage, but, rather, an outcome of continuous social-ecological process in which maize use may increase or decrease over time. [ABSTRACT FROM AUTHOR]

Recent work in three major research themes involving molluscs is reviewed: 1. molluscs in past human diets and subsistence systems, sclerochemistry and seasonality studies on mollusc harvesting times using stable isotopes of oxygen; 2. the impact of foraging on mollusc populations, resource management strategies, and settlement patterns and mobility of coastal foragers; and 3. mollusc shells as artefacts and personal ornaments, including manufacture and use, provenance studies and exchange systems, and human cognition. Most of the discussion is about marine molluscs and their shells, although land snails and freshwater shells are also considered, where appropriate. [ABSTRACT FROM AUTHOR]

Temporal trends in prehistoric millet consumption are investigated in two regions of northern China, in the Wei River valley and a northern zone that encompasses north-eastern Shaanxi, western Shanxi and south-central Inner Mongolia. By directly radiocarbon dating each sample investigated, inferences about the timing of dietary shifts inferred from stable carbon and nitrogen isotope compositions can be made with a high degree of precision. Evidence presented here indicates that humans living around 4000 years ago in both the Wei River valley and the northern zone were heavily dependent on millet for their subsistence. By ca. 2500 cal. yr BP, a major diversification of diet had occurred in the Wei River valley, with some consuming much larger proportions of C3 foods than previously. These C3 foods may have included the western-derived cereals – wheat, barley and oats – and also rice. [ABSTRACT FROM AUTHOR]

Abstract: We present a geometric model for examining the macronutrient contributions of insects in the diets of pre-agricultural humans, and relate the findings to some contemporary societies that regularly eat insects. The model integrates published data on the macronutrient composition of insects and other foods in the diets of humans, recommended human macronutrient intakes, and estimated macronutrient intakes to examine the assumption that insects provided to pre-agricultural humans an invertebrate equivalent of vertebrate-derived meats, serving primarily as a source of protein. Our analysis suggests that insects vary more widely in their macronutrient content than is likely to be the case for most wild vertebrate meats, spanning a broad range of protein, fat and carbohydrate concentrations. Potentially, therefore, in terms of their proportional macronutrient composition, insects could serve as equivalents not only of wild meat, but of a range of other foods including some shellfish, nuts, pulses, vegetables and even fruits. Furthermore, humans might systematically manipulate the composition of edible insects to meet specific needs through pre-ingestive processing, such as cooking and selective removal of body parts. We present data suggesting that in modern societies for which protein is the more limiting macronutrient, pre-ingestive processing of edible insects might serve to concentrate protein. It is likely, however, that the dietary significance of insects was different for Paleolithic hunter–gatherers who were more limited in non-protein energy. Our conclusions are constrained by available data, but highlight the need for further studies, and suggest that our model provides an integrative framework for conceiving these studies. [Copyright &y& Elsevier]

Abstract: Central western Argentina is the southern boundary of prehispanic maize in the archaeological record. This paper explores the stable isotope information from human bone (δ13C, from collagen and δ13C from apatite) and tooth (δ13C from enamel) samples in order to characterize the temporal and spatial trends of these isotopes and to understand them in terms of human diet. We analyzed 104 human individuals from the last 6000 years. Using the model the results shows a high variation in human diet with few human individuals with a notably high significance of C4 plants (probably maize) as an energy source and these samples have a chronology around ca. 1000 years BP. On the other hand a high variation in an individual’s dietary life history is shown by differences between δ13C collagen, apatite and enamel. [Copyright &y& Elsevier]

Abstract: Barnacles of the species Pollicipes pollicipes are crustaceans that nowadays live on wave-beaten rocky substrates in the intertidal and low-shore zones on the coasts of Atlantic Europe and North Africa. At the present time, the exploitation of this species is profitable, especially in northern Spain where this sea-food is highly valued, as well as expensive. However, the gathering of this resource, which is carried out manually by the percebeiros or “goose barnacle fishers” entails great risks. The exploitation of goose barnacles is, however, not a recent activity, as evidence of it has been seen in southwest Europe in the Mesolithic (about 8000 BP), and above all from the early Neolithic (about 6000 BP). This paper analyses the archaeological evidence of barnacles (tergum, scutum and carina, calcareous plates located in the capitulum) that have been found at one Spanish Neolithic site located in the north of the Iberian Peninsula (Los Gitanos Cave, in Cantabrian Spain). [Copyright &y& Elsevier]

Abstract: During the last glacial maximum, the west European modern humans adapted to adverse conditions and their populations subsisted exploiting the natural resources available. Fish were always present as a source of animal protein, although their importance in the human diet and their contribution to the expansion of humans has not been fully explored. Based on the compilation of zooarchaeological evidences from north Spanish sites we have discovered a constant pattern of exploitation of freshwater fish (Salmonids) with high incidence in the human diet during the Upper Paleolithic. Shifts in the exploitation of marine resources can be explained by climate-related geographical changes. The characteristics of salmonids that make them target species for supporting human survival in adverse climate periods are identified and discussed. [Copyright &y& Elsevier]

The Final Gravettian in Europe overlapped with the cold and dry climatic event of Heinrich 2 (ca. 27–23.5 kyr cal BP), which caused the contraction of human distribution over refuge regions in the southern peninsulas of Europe. Here, we consider the human subsistence in the northeast Iberian Peninsula, where an extensive range of small to large prey was available. Four human remains from the Serinyà caves were investigated using the stable isotope ratios of carbon, nitrogen, and sulfur of bulk collagen (δ 13C coll , δ 15N coll , δ 34S coll) and of phenylalanine and glutamine amino acids (δ 15N Phe , δ 15N Glu). Direct AMS dating of the human and animal remains from the Final Gravettian levels of Mollet III, Reclau Viver, and Arbreda at Serinyà confirmed their chronological position from 27.5 to 22.6 kyr cal BP and the occurrence of four different human individuals. The δ 13C coll and δ 15N coll values showed a large contribution of terrestrial prey to the dietary protein of the individuals. The δ 34S coll values were consistent with a subsistence based on the local continental resources, without detectable contribution of marine resource. The δ 15N Phe and δ 15N Glu values confirm that freshwater resources were not a substantial component of the diet of the considered individuals. Contrast in the isotopic amounts in bulk collagen could be interpreted as the result of different proportions of terrestrial prey in human diet at Serinyà. Altogether, the isotopic investigation reveals the importance of terrestrial over aquatic resources in the subsistence of the studied Final Gravettian individuals from the Serinyà caves in northeastern Iberia during the Last Glacial Maximum. It would be consistent with a scenario of a productive enough terrestrial ecosystem to sustain hunter-gatherer subsistence in this refuge region. [ABSTRACT FROM AUTHOR]

Nitrogen (N) fertilizers are very important for global food self-sufficiency (FSS), particularly for Africa, where the N input in agriculture is very low. This is the first work which studies and calculates the amount of N fertilizer that each country in Africa needs to feed itself by 2050. In this study, we used five different scenarios of inorganic fertilizer N (IFN) use and human diets to calculate the amount of N fertilizer needed to achieve FSS in Africa by 2050 and analyze the changes in N budget; N losses and N use efficiency (NUE). These scenarios include 1) business as usual (BAU), 2) equitable diet (EqD; self-sufficiency), 3) an IFN input 20% less than the EqD (S1), 4) an IFN input 40% less than the EqD (S2), and 5) a 20% increase in IFN input relative to the EqD (S3). Under the BAU scenario, production trends continue as they have over the past five decades, including an unhealthy human diet. In the EqD scenario, the priority is to meet the local demand for both animal and plant proteins with a healthy human diet. Under the EqD scenario, increasing the total N input from 35 kg N ha−1 yr−1 to 181 kg N ha−1 yr−1 during 2016–2050 is needed to achieve FSS in Africa. This increase in N fertilizer use represents unprecedented N inputs to African terrestrial ecosystems — at least 52 Tg N yr−1 — which would lead to inevitable increases in N losses. We also found that the NUE would decrease from 63% during 2010–2016 to 50% by 2050, whereas the total N surplus would increase from 13 kg N ha−1 yr−1 to 90 kg N ha−1 yr−1 by 2050. The estimated gaseous emissions would increase from 8 kg N ha−1 yr−1 to 61 kg N ha−1 yr−1 by 2050. Our findings conclude that, it is very important to consider the high N losses in Africa if the EqD scenario is applied. The S1 and S2 scenarios result in much less environmental N loss, and better NUE compared with the EqD scenario. Therefore, based on these findings we can recommend the implementation of the S2 scenario with an IFN dose of 77 kg N ha−1 yr−1, in parallel with the use of modern agricultural techniques and the increased use of organic inputs. • Africa needs 181 kg nitrogen (N) ha−1 yr−1 to feed itself by 2050. • Total N surplus would be 90 kg N ha−1 yr−1 by 2050 based on the food self-sufficiency scenario (FSS). • N use efficiency would decrease from 63% to 50% during 2016–2050 based on the FSS scenario. • Gaseous emissions would be 61 kg N ha−1 yr−1 by 2050 based on the FSS scenario. • The inorganic fertilizer N dose of 77 kg N ha−1 yr−1 is suitable for current African conditions. [ABSTRACT FROM AUTHOR]