A simple carbon isotope model for reconstructing prehistoric human diet

A compilation of experimental animal data shows that neither delta13C(collagen) nor delta13C(apatite) nor Delta13C(CO-AP) indicate diagnostic reconstructions of diet, diet energy and diet protein. In contrast, plots of delta13C(collagen) against delta13C(apatite) provide a model of three regression lines (C3, C4, and marine diet protein) where position on each line indicates the energy source (C3, C4, or mixed). Neither body size nor trophic position appears to affect these relationships. Modern free-ranging, terrestrial fauna do not fit the model perhaps because they, unlike the experimental fauna, mainly use fermentation rather than digestion during energy metabolism. Archaeological humans fall as expected based on associated floral and faunal evidence. Foraging people plot at positions expected from associated C3 fauna and plants. Those from Cahokia plot, as expected, from associated deer, nuts, and maize whereas people from nearby smaller sites plot in positions consistent with eating more fish. Agriculturists from Ontario and Grasshopper Pueblo plot consistent with dependence on fish by the former and on turkeys by the latter. In Tierra del Fuego, people from interior regions ate more terrestrial fauna, as suggested by ethnohistoric reports, than did people from the coast. In the Southwestern Cape in South Africa individuals late in the sequence have pure C3 diets whereas ones early in the sequence ate marine protein as suggested by independent archaeological evidence. People on San Nicolas Island depended on C4 plants in contrast to other islands off California's coast. This simple model provides more detailed and precise dietary information than do individual isotopic measures.     

青铜时代中晚期辽西地区农业活动特征

辽西地区城子山遗址和夏家店遗址农作物种子遗存研究显示,城子山地区青铜时代中期以旱作农业种植为主.粟的栽培比例要明显高于黍.青铜时代晚期的夏家店地区属半农半牧区,存在黍与粟为主的旱作农业种植,但黍的栽培比例要远高于青铜时代中期的城子山地区.干旱化可能是导致夏家店地区青铜时代晚期黍栽培比例升高的主要原因.城子山和夏家店地区农业种植结构在青铜时代晚期可能已有所不同,但这2个地区农业种植的差异究竟从何时开始,仍是一个需要继续深入研究的问题.     

Human impact during the Bronze Age on the vegetation at Lago Lucone (northern Italy)

Lake-sediment records were used to reconstruct human impact on the landscape around Lago Lucone (45°33′N, 10°29′E, 249 m a.s.l.), a former lake in the western amphitheatre system of the Lago di Garda. Presence of prehistoric human populations is attested by pile-dwelling settlements from the Early-Middle Bronze Age, with one settlement at a distance of only 100 m from the coring site. Pollen, plant-macrofossil and microscopic charcoal analyses were applied to a 250 cm sediment core with four dates providing the time control. A mixed oak forest that was important during the Early-Middle Holocene was cleared and replaced by open vegetation during the Bronze Age (∼2000–1100 b.c.) when open lands were estimated to have covered more than 60% of the total relevant pollen-source area. During a phase of high human impact, independent climatic proxies suggest warm and dry climatic conditions. Later, ca. 1100 b.c., palaeobotanical evidence indicates a sharp decrease in human pressure in the Lago Lucone area. The comparison with other sedimentary palaeocultural records shows that the period 1300–1100 b.c. was characterised by general declines of agricultural activities both south and north of the Alps. These declines have been previously attributed to a change towards wetter and colder climatic conditions in and around the Alps. However, the decline in human impact around Lago Lucone cannot be exclusively attributed to climatic variation. Therefore other forcing factors independent of climatic changes, such as cultural crises or changes in spatial organisation of the habitats, cannot be ruled out under the present state of knowledge.     

Stable isotope evidence for impala Aepyceros melampus diets at Akagera National Park,Rwanda

Stable isotope analysis of tooth enamel was used to investigate the relative proportions of grass and browse in seasonal and overall diets of impala Aepyceros melampus at Akagera National Park, Rwanda. Bulk enamel samples suggest that on average, impala ate c. 86% C₄ grass year‐round, far more than in most previously studied impala populations across Africa. Intra‐tooth samples show that seasonal changes in the proportion of C₄ grass versus C₃ browse are minimal (c. 10%), the diet being dominated by C₄ grass year‐round in contrast to other impala populations that consume ≥50% browse during the dry season. Intra‐tooth oxygen isotope values track carbon isotope changes to a moderate degree, but are not patterned clearly enough to permit identification of wet versus dry seasons. As other studies have shown that impala select high‐protein diets, the foraging behaviour at Akagera is probably because of the availability of palatable grass for much of the year in the edaphic grasslands around the lacustrine environments of the eastern portions of Akagera National Park.     

Stable isotope analyses of collagen in fish scales: limitations set by scale architecture

Comparisons between the stable isotope composition of carbon in collagen excized from juvenile (freshwater) and adult (marine) portions of scales from Atlantic salmon Salmo salar demonstrated that c. 75% of carbon analysed in the 'juvenile' portion of the scale derives from later formed collagen. Scale collagen analyses were effectively restricted to the last season of growth.     

内蒙古中南部地区青铜—早期铁器时代居民的龋病研究

本文对内蒙古中南部地区青铜—早期铁器时代5个考古地点出土人骨的龋病患病情况做了研究, 在与其他国内材料对比的基础上, 探讨了文化类型与龋病患病率之间的关系。龋病在以农业经济为主的人群中患病率最高, 在农牧兼营的人群中龋病率其次, 在以畜牧业为生的游牧人群中患病率最低。龋病是反映内蒙古地区该时段古代居民经济模式的一个有效指标。     

Disease and mortality in the Early Bronze Age people of Bab edh-Dhra, Jordan.

During the 1977 field season at the Early Bronze Age site of Bab edh-Dhra 92 individuals were recovered from underground shaft tomb chambers. Morbid conditions found in these skeletons include trauma, possibly two cases of tuberculosis, osteomyelitis, post-menopausal osteoporosis and congenital anomalies. Of the 92 skeletons recovered 56 (61%) were 18 years of age or older, 28 (30%) were between 1 and 18 years of age and 8 (9%) were less than one year of age.     

Stable isotope evidence for sex- and status-based variations in diet and life history at medieval Trino Vercellese, Italy

The medieval period in Europe was a time of unprecedented social complexity that affected human diet. The diets of certain subgroups-for example, children, women, and the poor-are chronically underrepresented in historical sources from the medieval period. To better understand diet and the distribution of foods during the medieval period, we investigated stable carbon and nitrogen isotope ratios of 30 individuals from Trino Vercellese, Northern Italy (8th-13th c.). Specifically, we examined diet differences between subgroups (males and females, and high- and low-status individuals), and diet change throughout the life course among these groups by comparing dentine and bone collagen. Our results show a diet based on terrestrial resources with input from C(4) plants, which could include proso and/or foxtail millet. Diets of low-status males differ from those of females (both status groups) and of high-status males. These differences develop in adulthood. Childhood diets are similar among the subgroups, but sex- and status-based differences appear in adulthood. We discuss the possibility of cultural buffering and dietary selectivity of females and high-status individuals.     

Lapita diet and subsistence strategies on Watom Island,Papua New Guinea: New stable isotope evidence from humans and animals

Stable isotope ratios (δ¹³C and δ¹⁵N) were analyzed from the bone collagen of individuals (n = 8) from a Lapita burial ground (ca. 2800–2350 BP) on Watom Island, located off northeast New Britain in the Bismarck Archipelago. The aim of this study was to assess the diet and subsistence strategies of humans that lived during the later Lapita period in Near Oceania. To aid in the interpretation of the human diet we analyzed the stable isotope ratios of faunal material from the site (n = 27). We also aim to assess methods of animal husbandry at the site over time from an analysis of the stable isotope ratios (δ¹³C and δ¹⁵N) of pig bones (n = 22) from different temporal periods (Lapita, post‐Lapita, and late prehistoric). The protein diet of the humans consisted of marine organisms from the inshore environment and some deep‐water species, most likely marine turtle, in addition to higher trophic level terrestrial foods, likely pig and native animals (e.g., fruit bat, Cuscus and bandicoot). Although the sample sizes were small, females (n = 4) displayed more variable δ¹³C and δ¹⁵N values compared with males (n = 4), which may be associated with the movement of adult females to the island. The stable isotope analysis of the pig bones indicated that there were few differences between the diets of the pigs from the Lapita and post‐Lapita layers, suggesting that the method of pig husbandry was similar between these two periods and was likely relatively free‐range. Am J Phys Anthropol 157:30–41, 2015. © 2015 Wiley Periodicals, Inc.     

Early agriculture and crop transmission among Bronze Age mobile pastoralists of Central Eurasia

Archaeological research in Central Eurasia is exposing unprecedented scales of trans-regional interaction and technology transfer between East Asia and southwest Asia deep into the prehistoric past. This article presents a new archaeobotanical analysis from pastoralist campsites in the mountain and desert regions of Central Eurasia that documents the oldest known evidence for domesticated grains and farming among seasonally mobile herders. Carbonized grains from the sites of Tasbas and Begash illustrate the first transmission of southwest Asian and East Asian domesticated grains into the mountains of Inner Asia in the early third millennium BC. By the middle second millennium BC, seasonal camps in the mountains and deserts illustrate that Eurasian herders incorporated the cultivation of millet, wheat, barley and legumes into their subsistence strategy. These findings push back the chronology for domesticated plant use among Central Eurasian pastoralists by approximately 2000 years. Given the geography, chronology and seed morphology of these data, we argue that mobile pastoralists were key agents in the spread of crop repertoires and the transformation of agricultural economies across Asia from the third to the second millennium BC.     

新疆于田流水墓地青铜时代人类牙齿非测量性状

我国新疆地区自古以来即是东西方文明相互交融的摇篮,以往的考古学、体质人类学研究表明,该区域内不同文化之间的互通有无早在我国青铜-早期铁器时代便已经发生。关于这种交流与融合产生的原因,目前学术界仍未有定论。新疆于田流水墓地(2950±50 BP)是由中国社会科学院考古研究所于2003-2005年主持发掘的青铜时代墓葬群,该墓地共发掘墓葬65座,被视为是昆仑山北麓发现的最早人类文化遗存。本文从采集自流水墓地108例人骨标本的19项牙齿非测量性状研究入手,将其与欧亚大陆范围内的古今人群进行比较研究,并进行史密斯生物学距离的计算以及主成分分析。结果表明:生活在新疆流水地区的古代人类与南西伯利亚地区、日本绳纹、阿富汗/巴基斯坦、中国姜家梁地区人群之间在牙齿非测量性状方面存在某种程度上的相似性,这或许可以说明至少在3000年前,我国新疆西南部地区可能已经存在了东西方的人群迁徙。     

新疆喀什下坂地墓地青铜时代人群颅骨的测量性状

下坂地墓地青铜时代居民是帕米尔高原区早期人群的代表。通过颅骨测量性状特征对该人群来源和流向问题的讨论,为建立欧亚大陆青铜时代人群的流动、变迁史提供了新的素材。与欧亚大陆青铜时代时空相关人群对比分析的结果表明,下坂地青铜组居民的祖先人群,可能是来自东欧南部草原地带的洞室墓文化居民。他们在安德罗诺沃文化的繁盛期,自东欧草原地带迁徙到帕米尔高原区,逐渐发展为安德罗诺沃文化的一个地方变体。     

Analysis of the fuel wood used in Late Bronze Age and Early Iron Age copper mining sites of the Schwaz and Brixlegg area (Tyrol,Austria)

Charcoal analysis was carried out as part of an interdisciplinary project focusing on the copper mining history of the former mining area of Schwaz and Brixlegg, a region pivotal as a copper source in prehistoric Europe. The goal was to use remains of carbonised wood to investigate environmental implications of prehistoric mining, as well as to gain new insight about the ancient mining technique of fire-setting. Charcoal samples from seven copper mining sites (Late Bronze Age to Early Iron Age) were analysed. The results reveal a strong preference for coniferous wood as fuel in fire-setting, but not in ore smelting/roasting processes. Species composition at the ore-processing sites indicates moderate forest degradation processes caused by human intervention.     

A palaeocarpological study of Neolithic and Bronze Age levels of the Buraco da Pala rock-shelter (Bragança,Portugal)

Palaeocarpological (archaeobotanical) analysis of Neolithic and Bronze Age levels of the Buraco da Pala site (Bragança, Portugal) provides evidence of considerable agricultural activity. Triticum, Hordeum and Vicia predominated, though Pisum, Lens, Vitis, Linum and Papaver were also found. Most wheat grains were spheroidal and were identified as Triticum aestivum subsp. sphaerococcum, in disagreement with recent suggestions that taxa with spheroidal grains have never been present in the Iberian Peninsula. Quercus and Pinus seed indicated that gathering activities supplemented agricultural production.     

Mobility in Central European Late Eneolithic and Early Bronze Age: femoral cross-sectional geometry

Some scholars explain the absence of settlements in the Bohemian and Moravian Late Eneolithic (Corded Ware archaeological culture) as a consequence of pastoral subsistence with a high degree of mobility. However, recent archaeological studies argued that the archaeological record of the Late Eneolithic in Central Europe exhibits evidence for sedentary subsistence with mixed agriculture, similar to the subsequent Early Bronze Age. Because the archaeological data do not allow us to address unambiguously the mobility pattern in these periods, we used cross-sectional analysis of the femoral midshaft to test mobility directly on the human skeletal record. The results of femoral midshaft geometry do not support a high degree of mobility in the Late Eneolithic in Central Europe. This conclusion is supported mainly by no significant differences in male groups between the Late Eneolithic and Early Bronze Age in mechanical robusticity and shape of the femoral midshaft, although Corded Ware males still exhibit the highest absolute mean values of the diaphyseal shape (I(A-P)/I(M-L)) ratio and antero-posterior second moment of area. However, Late Eneolithic females have significantly higher torsional and overall bending rigidity because of a significantly higher medio-lateral second moment of area. This finding cannot be directly linked with a higher degree of long-distance mobility for these females. A significant difference was also found in overall decrease of size parameters of the femoral midshaft cross section for one of the Early Bronze Age samples, the Wieselburger females. Since the decrease of size and mechanical robusticity for Wieselburger females does not correspond with the parameters of Early Bronze Age females, we can expect a mosaic pattern of changes during the Late Eneolithic and Early Bronze Age period, instead of a simple unidirectional (diachronic) change of the mechanical environment.