Early Neolithic agriculture in Ambrona, Provincia Soria, central Spain

The early Neolithic sites of La Lámpara and La Revilla del Campo in the Meseta Norte (Northern Meseta) plateau in central Spain produced evidence for early agriculture from the last third of the 6th millennium B.C. The hulled wheats Triticum monococcum (einkorn) and T. dicoccum (emmer) were identified from carbonised plant remains as well as from imprints in pottery and daub. Single finds of charred remains of Hordeum vulgare (barley), Papaver somniferum/setigerum (poppy) and Linum usitatissimum (linseed) indicated other cultivated crops. The wild plants mainly indicated arable weeds, partly from less fertile soils, and garrigue vegetation from poor pastures. The spectrum of crops from the Ambrona sites was compared to other inner Iberian sites as well as to Mediterranean sites. Sediment samples as well as mineral crusts from graves were analysed from the Neolithic tumulus of La Peña de la Abuela. Its diachronic collective burials had originated from a period of time during the first third of the 4th millennium B.C. Probably no crops, but many green vegetative parts of pine, oak, and juniper had been used as funeral gifts. Oak cupula development indicated early summer activities in the grave-mound. Wickerwork made of willow was used for embedding the dead bodies.     

Tooth wear and compensatory modification of the anterior dentoalveolar complex in humans

In populations living in environments where teeth wear severely, some compensatory modification of the dentoalveolar complex is thought to occur during life whereby functional occlusion is maintained as tooth substance is lost by wear. This study investigates one aspect of this modification process: Changes in the anterior dentoalveolar complex that are accompanied with wear were examined in a series of Japanese skeletal samples. In the prehistoric Japanese hunter-gatherer population heavy wear occurs over the entire dentition. The following changes were demonstrated to have occurred in the anterior segment of the dentition accompanied by wear on the anterior teeth: The anterior teeth tip lingually with wear up to a nearly upright position to fill in interproximal spaces that would have been generated by wear, and to maintain contact relations between adjacent teeth. At the same time, the anterior surface of the maxillary alveolar process also inclines lingually to a certain extent. The amount of lingual tipping is greater in the maxillary anterior teeth than in their mandibular antagonists. It is because of this discrepancy that, with age, the horizontal component of the overlap between maxillary and mandibular anterior teeth decreases, and their bite form changes from scissor bite to edge-to-edge bite. Lesser degrees of lingual tipping of the anterior teeth were also detected in the prehistoric agriculturists and historic Japanese populations. The variation in the degree of lingual tipping observed among the samples is explained by inter-population variation in severity and pattern of tooth wear. This and other evidence suggests that mechanisms that compensate for wear in the anterior dentition may be characteristic of all living human populations, independently of the degree of wear severity endured in their environments.     

Population affinities of Neolithic Siberians: a snapshot from prehistoric Lake Baikal

Archaeological evidence supports the inhabitation of the Lake Baikal region since the Paleolithic. Both metric and nonmetric osteological studies suggest that Neolithic Cis-Baikal populations are the ancestors of contemporary inhabitants of the region. To date, ancient DNA data have not been used to corroborate this biological continuity hypothesis. This study presents a temporal snapshot of the Cis-Baikal Neolithic by examining mtDNA diversity in two cemetery populations situated on the Angara River downstream of Lake Baikal. The 800 years separating the use of the two cemeteries is thought to represent a biocultural hiatus in the Cis-Baikal region, one that ended when a new group migrated into the area. To assess the likelihood that genetic continuity exists between these two Neolithic groups, we examined both mtDNA coding region and hypervariable region I (HVI) polymorphisms from skeletal remains excavated from both cemeteries (Lokomotiv and Ust'-Ida). The mtDNA haplogroup distributions of the two cemetery populations differ significantly, suggesting that they were biologically distinct groups. When the biological distance between these Neolithic groups is compared with modern Siberian and other East Eurasian groups, the posthiatus group (Serovo-Glazkovo) generally aligns with contemporary Siberians, while the prehiatus (Kitoi) individuals are significantly different from all but modern Kets and Shorians living in the Yenisey and Ob River basins to the west of Lake Baikal. These results suggest that the Lake Baikal region experienced a significant depopulation event during the sixth millennium BP, and was reoccupied by a new immigrant population some 800 years later.     

Tooth wear and dental pathology of the Bronze-Iron Age people in Xinjiang, Northwest China: Implications for their diet and lifestyle

Tooth wear and dental pathology related to diet and lifestyle were investigated in the human dental remains unearthed from three archaeological sites of Bronze Age and Iron Age in Xinjiang of northwest China, and in comparative samples from two Neolithic sites in Henan and Shanxi in central China along the Yellow River.Our results indicate that the average tooth wear on most tooth types in the three Xinjiang sites was close to those of the Neolithic samples from central China. The variation within the Xinjiang samples was also explored. Some special wear patterns such as severe wear on the first molar and relatively heavy wear of anterior teeth were observed on the specimens from the Xinjiang sites. Obvious differences in caries and antemortem tooth loss were found between Xinjiang and comparative samples with higher frequencies of caries observed in samples from central China and higher antemortem tooth loss in samples from the Xinjiang sites. Strongly developed exostoses (tori) were also identified on mandibles and maxillae of the specimens from Xinjiang.The authors believe that the differences in tooth wear and dental pathology between Xinjiang and central China were caused by differences in diet and lifestyle. Food of a harder texture was consumed by the people who lived in Xinjiang than by the people in Henan and Shanxi of central China. The higher occurrence of heavily worn anterior teeth and some other special wear patterns, antemortem tooth loss and presence of exostoses on jaw bones in Xinjiang suggest that the people in Xinjiang lived in a relatively harsh environment, frequently gnawing hard objects, or using teeth as some kind of tools. All these activities put masticatory organs under a heavy load. The differences in caries frequencies between the frontier and central areas of China indicate that food richer in carbohydrates was consumed by the people in the central areas.It is proposed that about 3000-2000 years BP in many areas of frontier Xinjiang, people mainly relied on the type of hunter-gatherer economy with agriculture playing a smaller role in their lifestyle.     

Tool use in animals: Cognition and ecology. Edited by Crickette M. Sanz,Josep Call,and Christophe Boesch. New York,NJ: Cambridge University Press. 2013. 313 pp. ISBN 978‐1‐107–01119‐9. $110 (hardcover).

Enamel thickness has been linked to functional aspects of masticatory biomechanics and has been demonstrated to be an evolutionary plastic trait, selectively responsive to dietary changes, wear and tooth fracture. European Late Paleolithic and Mesolithic hunter‐gatherers mainly show a flat wear pattern, while oblique molar wear has been reported as characteristic of Neolithic agriculturalists. We investigate the relationships between enamel thickness distribution and molar wear pattern in two Neolithic and medieval populations. Under the assumption that dietary and/or non‐dietary constraints result in directional selective pressure leading to variations in enamel thickness, we test the hypothesis that these two populations will exhibit significant differences in wear and enamel thickness patterns. Occlusal wear patterns were scored in upper permanent second molars (UM2) of 64 Neolithic and 311 medieval subadult and adult individuals. Enamel thickness was evaluated by microtomography in subsamples of 17 Neolithic and 25 medieval individuals. Eight variables describing enamel thickness were assessed. The results show that oblique molar wear is dominant in the Neolithic sample (87%), while oblique wear affects only a minority (42%) of the medieval sample. Moreover, in the Neolithic molars, where buccolingually directed oblique wear is dominant and greatest enamel lost occurs in the distolingual quadrant, thickest enamel is found where occlusal stresses are the most important—on the distolingual cusp. These results reveal a correlation between molar wear pattern and enamel thickness that has been associated to dietary changes. In particular, relatively thicker molar enamel may have evolved as a plastic response to resist wear. Am J Phys Anthropol 155:162–172, 2014. © 2014 Wiley Periodicals, Inc.     

The Neolithic of the southern Levant

The Neolithic period of the southern Levant was an era of tremendous change. Over the course of the Neolithic, the gradual transition from foraging to agriculture involved not merely economic innovations, but also profound shifts in population size, social organization, and technology. This represents possibly the earliest, and certainly one of the earliest, instances of the transition to agriculture. The advent of farming altered human demography, health, and diversity; it shaped the spread of the world's dominant cultures, genes, and languages. 1 , 2 It recast humans' relationship with the natural world, increasing modification of the environment. It both enabled and required the development of new social structures as humans learned how to live in increasingly large and densely packed groups. These transformations were not easily achieved. This paper traces the development of the southern Levantine Neolithic through two thousand years of socioeconomic elaboration and expansion; a major social recalibration in the middle Neolithic; and a final millennium‐and‐a‐half of smaller‐scale and materially simpler adaptations.     

Ancient DNA Analysis of 8000 B.C. Near Eastern Farmers Supports an Early Neolithic Pioneer Maritime Colonization of Mainland Europe through Cyprus and the Aegean Islands

The genetic impact associated to the Neolithic spread in Europe has been widely debated over the last 20 years. Within this context, ancient DNA studies have provided a more reliable picture by directly analyzing the protagonist populations at different regions in Europe. However, the lack of available data from the original Near Eastern farmers has limited the achieved conclusions, preventing the formulation of continental models of Neolithic expansion. Here we address this issue by presenting mitochondrial DNA data of the original Near-Eastern Neolithic communities with the aim of providing the adequate background for the interpretation of Neolithic genetic data from European samples. Sixty-three skeletons from the Pre Pottery Neolithic B (PPNB) sites of Tell Halula, Tell Ramad and Dja''de El Mughara dating between 8,700–6,600 cal. B.C. were analyzed, and 15 validated mitochondrial DNA profiles were recovered. In order to estimate the demographic contribution of the first farmers to both Central European and Western Mediterranean Neolithic cultures, haplotype and haplogroup diversities in the PPNB sample were compared using phylogeographic and population genetic analyses to available ancient DNA data from human remains belonging to the Linearbandkeramik-Alföldi Vonaldiszes Kerámia and Cardial/Epicardial cultures. We also searched for possible signatures of the original Neolithic expansion over the modern Near Eastern and South European genetic pools, and tried to infer possible routes of expansion by comparing the obtained results to a database of 60 modern populations from both regions. Comparisons performed among the 3 ancient datasets allowed us to identify K and N-derived mitochondrial DNA haplogroups as potential markers of the Neolithic expansion, whose genetic signature would have reached both the Iberian coasts and the Central European plain. Moreover, the observed genetic affinities between the PPNB samples and the modern populations of Cyprus and Crete seem to suggest that the Neolithic was first introduced into Europe through pioneer seafaring colonization.     

Changes in the pattern of tooth wear from prehistoric to recent periods in Japan

Although a number of studies have been performed on interpopulational variation of tooth wear patterns in recent humans, the major interest in the study of tooth wear so far has been in reconstructing the subsistence and behavior of prehistoric populations, and hence research on wear pattern changes in historic times has been superficial. The present study investigated temporal change in the pattern of wear on the permanent dentition of the Japanese through comparison of the following five groups: prehistoric hunter-gatherers, prehistoric agriculturists, medieval, premodern, and recent populations. The pattern of reduction of occlusal wear severity across thesechronological groups was not similar between the anterior and posterior portions of the dentition. Occlusal wear on the anterior teeth was noticeably lighter in the prehistoric agriculturists and later populations than in the prehistoric hunter-gatherers, while clear reduction of occlusal wear on the posterior teeth occurred after medieval times. The temporal variations in the degree of mesiodistal crown diameter loss due to wear and its anterior-posterior gradient within the dentition are generally consistent with those observed in the occlusal wear pattern. Possible causative factors of these temporal changes in the wear pattern are discussed. Am J Phys Anthropol 109:501–508, 1999. © 1999 Wiley-Liss, Inc.     

Studies on the vegetation history of Lake Varna region,northern Black Sea coastal area of Bulgaria

On the basis of pollen analytical investigations of two cores from Lake Varna and Lake Beloslav, the vegetation history of the Lake Varna region is traced back to the beginning of the 6th millennium B.C. A two-fold zoning system is used whereby the pollen diagrams are divided into pollen zones, based on tree migration patterns, and settlement periods. Pollen zone 1 is characterised by the absence of Carpinus betulus and Fagus sylvatica. The spread of hornbeam started at ca. 6500 B.C. (pollen zone 2) and beech at ca. 6200 B.C. (pollen zone 3), the latter being the last tree to spread into the region and considerably enrich the forests of the study area. Of the many pollen taxa representing plants that are favoured by open habitats and hence potentially indicative of human impact, only a few taxa are regarded as reliable indicators of human activity. These include above all Triticum-type, and also Secale and to a certain extent Plantago lanceolata, Rumex and Polygonum aviculare. The spatial pattern of settlements is somewhat different in the areas represented by the two profiles. At both sites the first period of settlement occurred during the 6th millennium B.C. (early Neolithic). After the Neolithic period, the main settlement periods of the Eneolithic and the Early and Middle Bronze Age are recorded. On the other hand, land-use history during the Greek and Roman periods is poorly recorded. Studies on the stratigraphy, diatoms and molluscs indicate that the sixth Black Sea transgression (6500–5800 B.C.), which reached –10 m, had considerable influence on the limnological environment.     

Morphological studies of free-threshing wheat ears from a Neolithic site in southwest Germany, and the history of the naked wheats

Two hundred and seventy carbonized naked wheat ears from the Neolithic pile dwelling at Hornstaad-Hörnle IA/Lake Constance (Germany) were analysed. The characteristics of internodes and glumes show that only tetraploid naked wheat types were cultivated. Following the history of free-threshing wheats it seems conceivable that the tetraploid naked wheats spread from their point of origin in the Middle East (7th/8th millennium B.C.) via a Mediterranean route to southwest Europe, reaching the northern foothills of the Alps about 4000 B.C.     

Origins and spread of agriculture in Italy: a nonmetric dental analysis

Dental morphological traits were employed in this study as direct indicators of biological affinities among the populations that inhabited the Italian peninsula from the Upper Paleolithic-Mesolithic to Medieval times. Our analysis aims at contributing to the ongoing debate regarding the origin and spread of agriculture in the peninsula by contrasting the dental evidence of archaeological and modern molecular samples. It is not possible to generalize given the complex and dynamic nature of these populations. However, the results from the principal component analysis, maximum likelihood, mean measure of divergence, and multidimensional scaling do indicate a net separation of the Paleo-Mesolithic sample from the other groups that is not related to dental reduction. This suggests that the shift in dental morphology was the product of Neolithic populations migrating into the peninsula from other areas. Nonetheless, the Paleo-Mesolithic populations share several discriminative traits with the Neolithic group. The biological relevance of such evidence suggests that, to some minor extent, the spread of agriculture did not occur by total population replacement. Because of regional small sample sizes, this hypothesis cannot be tested on a micro-regional scale. It is, however, feasible to depict a scenario where processes of genetic mixture or replacement probably took place at different rates on a macro-regional level.     

Quand ils ne vivaient pas seulement de la chasse : preuves de domestication ancienne dans les gisements néolithiques d’Atxoste et de Mendandia (Pays Basque)

The combination of use wear analyses on lithic assemblages, palaeontological data and the presence of a quern-stone is considered direct and indirect proof of economic practices of production in the Neolithic sites of Atxoste and Mendandia. We also discuss the role that in this picture is suggested by a recent study on the genetics of the bovids from Mendandia. Both sites are rock-shelters seasonally occupied where the main economic vectors, but not the only ones, are hunting activities: they are integrated in a network created during the Mesolithic but still in use during the Early Neolithic until the mid sixth millennium cal BC when information on farming accumulates in the territory.     

Tooth wear and dental pathology at the advent of agriculture: new evidence from the Levant

Differences in patterns of diet and subsistence through the analysis of dental pathology and tooth wear were studied in skeletal populations of Natufian hunter-gatherers (10,500-8300 BC) and Neolithic populations (8300-5500 BC, noncalibrated) from the southern Levant. 1,160 Natufians and 804 Neolithic teeth were examined for rate of attrition, caries, antemortem tooth loss, calculus, periapical lesions, and periodontal processes. While the Natufian people manifest a higher rate of dental attrition and periodontal disease (36.4% vs. 19%), Neolithic people show a higher rate of calculus. Both populations manifested low and similar rates of caries (6.4% in the Natufian vs. 6.7% in the Neolithic), periapical lesions (not over 1.5%), and antemortem tooth loss (3.7% vs. 4.5%, respectively). Molar wear pattern in the Neolithic is different than in the Natufian. The current study shows that the dental picture obtained from the two populations is multifactorial in nature, and not exclusively of dietary origin, i.e., the higher rate and unique pattern of attrition seen in the Natufian could result from a greater consumption of fibrous plants, the use of pestles and mortars (which introduce large quantities of stone-dust to the food), and/or the use of teeth as a "third hand." The two major conclusions of this study are: 1) The transition from hunting and gathering to a food-producing economy in the Levant did not promote changes in dental health, as previously believed. This generally indicates that the Natufians and Neolithic people of the Levant may have differed in their ecosystem management (i.e., gathering vs. growing grains), but not in the type of food consumed. 2) Changes in food-preparation techniques and nondietary usage of the teeth explain much of the variation in tooth condition in populations before and after the agricultural revolution.     

Stable isotopes and dietary adaptations in humans and animals at pre-pottery Neolithic Nevalli Cori, southeast Anatolia

Human and animal bones from the Pre-Pottery Neolithic B site of Nevali Cori (southeast Anatolia) were analyzed with regard to stable carbon and nitrogen isotopes in bone collagen, and stable carbon and oxygen isotopes in bone carbonate. The reconstruction of the vertebrate food web at this site revealed that humans may have faced difficulties with meat procurement, since their stable-isotope ratios reflect a largely herbivorous diet. This is in contrast with the preceding Pre-Pottery Neolithic A contexts and late Neolithic sites in the Fertile Crescent, where humans are located at the top of the food chain. Conceivably, Nevali Cori represents a community in the transition from a hunting and gathering subsistence to an economy with agriculture and animal husbandry, since domesticated einkorn and sheep, pigs, and probably also goats are in evidence at the site. In the second half of the 9th millennium calibrated (cal.) BC, however, the contribution of stock on the hoof to the human diet still seems modest. Animals kept under cultural control obviously had a dietary spectrum different from their free-ranging relatives. We conclude that these animals had been deliberately nourished by their owners, whereby the overall low delta(15)N-signatures in both humans and livestock might result from the consumption of protein-rich pulses.     

Relationships between lower limb cross-sectional geometry and mobility: the case of a Neolithic sample from Italy

This study investigates the relationships between lower limb robusticity and mobility in a Neolithic sample (LIG) from Italy (6th millennium BP). This study tests the hypothesis that the high femoral robusticity previously observed in the LIG sample is a consequence of the subsistence strategy (i.e., high mobility on uneven terrain) practiced by LIG. Cross-sectional geometric properties of the femur and tibia at midshaft of LIG (eight males and eight females) were collected and results compared to Late Upper Paleolithic (12 males, five females), Mesolithic (24 males, 8 females), and Eneolithic (28 males, 17 females) samples from other sites throughout Europe. The results show that the LIG sample does not show the reduction of lower limb robusticity that is characteristic of the Eneolithic sample, but rather that the LIG sample is most similar to the earlier, highly mobile, populations. This high level of robusticity in the LIG sample could reflect both their pastoral subsistence strategy combined with a rugged environment, as well as their earlier temporal position within the Neolithic. The results of this study further point to significant variation in male-female mobility patterns in the region, also possibly related to pastoral behavioral patterns.     

Dental modifications and tool use in the western Great Basin

Nondietary function is an important concern in the study of the human dentition and its role in adaptation. The purpose of the present investigation is to describe and interpret a pattern of dental wear in the anterior dentition of precontact hunter-gatherers that inhabited the western Great Basin. These data are discussed in light of ethnographic documentation as a means by which the archaeological record is linked with associated behavior of the representative populations. A series of 171 dentitions from a group of archaeological localities was examined. Of 1,931 teeth observed, 16 of these showed narrow (0.4-2.0 mm) transverse grooves located on the midocclusal surfaces of anterior teeth. The grooves were restricted in occurrence to five older adult males. Documentation of prehistoric and historic western Great Basin aboriginal populations indicates an adaptation that involves use of plant materials in the production of a variety of utilitarian objects, such as fish nets, basketry, funerary bags, fowling bags, and rope. In postcontact contexts, the anterior dentition has been shown to play an important role in the preparation of materials used for the production of this equipment. It seems most likely, then, that the grooves observed herein resulted directly from the use of the dentition as part of the tool assemblage for the production of other tools.     

Typologie et provenance de l’obsidienne du site néolithique d’A Guaita (NW Cap Corse,Corse, France)

The provenance of a large fraction of the obsidians from the Neolithic site of A Guaita was determined for its three chronocultural layers, between the second half of the 6th millennium and the beginning of the 4th millennium. The elemental composition of 140 samples was obtained by scanning electron microscopy (SEM–EDS) and/or ion beam analysis (PIXE). One hundred and thirty-eight obsidians were found to come from Sardinia and the remaining two from Palmarola Island. This result confirms the almost unique presence of Sardinian obsidians in Corsica and extends this observation to the northern end of the island. The three main Sardinian obsidian types, SA, SB2, and SC, are represented at A Guaita, with a predominance of SB2 and SC. The occurrence of two obsidians from Palmarola suggests that occasional contacts with the Italian Peninsula were in effect from the 6th millennium, in agreement with previous data from ceramics.     

Population Genomic Analysis of Ancient and Modern Genomes Yields New Insights into the Genetic Ancestry of the Tyrolean Iceman and the Genetic Structure of Europe

Genome sequencing of the 5,300-year-old mummy of the Tyrolean Iceman, found in 1991 on a glacier near the border of Italy and Austria, has yielded new insights into his origin and relationship to modern European populations. A key finding of that study was an apparent recent common ancestry with individuals from Sardinia, based largely on the Y chromosome haplogroup and common autosomal SNP variation. Here, we compiled and analyzed genomic datasets from both modern and ancient Europeans, including genome sequence data from over 400 Sardinians and two ancient Thracians from Bulgaria, to investigate this result in greater detail and determine its implications for the genetic structure of Neolithic Europe. Using whole-genome sequencing data, we confirm that the Iceman is, indeed, most closely related to Sardinians. Furthermore, we show that this relationship extends to other individuals from cultural contexts associated with the spread of agriculture during the Neolithic transition, in contrast to individuals from a hunter-gatherer context. We hypothesize that this genetic affinity of ancient samples from different parts of Europe with Sardinians represents a common genetic component that was geographically widespread across Europe during the Neolithic, likely related to migrations and population expansions associated with the spread of agriculture.     

Major population expansion of East Asians began before neolithic time: evidence of mtDNA genomes

It is a major question in archaeology and anthropology whether human populations started to grow primarily after the advent of agriculture, i.e., the Neolithic time, especially in East Asia, which was one of the centers of ancient agricultural civilization. To answer this question requires an accurate estimation of the time of lineage expansion as well as that of population expansion in a population sample without ascertainment bias. In this study, we analyzed all available mtDNA genomes of East Asians ascertained by random sampling, a total of 367 complete mtDNA sequences generated by the 1000 Genome Project, including 249 Chinese (CHB, CHD, and CHS) and 118 Japanese (JPT). We found that major mtDNA lineages underwent expansions, all of which, except for two JPT-specific lineages, including D4, D4b2b, D4a, D4j, D5a2a, A, N9a, F1a1'4, F2, B4, B4a, G2a1 and M7b1'2'4, occurred before 10 kya, i.e., before the Neolithic time (symbolized by Dadiwan Culture at 7.9 kya) in East Asia. Consistent to this observation, the further analysis showed that the population expansion in East Asia started at 13 kya and lasted until 4 kya. The results suggest that the population growth in East Asia constituted a need for the introduction of agriculture and might be one of the driving forces that led to the further development of agriculture.     

湖北郧县青龙泉新石器时代居民牙齿磨耗及健康状况

位于湖北省郧县境内的青龙泉遗址出土有仰韶、屈家岭和石家河等不同文化类型遗存, 被认为是中国新石器时代南、北文化交流的过渡地带。有关学者通过考古发现和同位素测试分析认为, 生活在青龙泉遗址的新石器时代居民已经具有发达的农业、家畜饲养业和渔猎,稻粟农业和肉类对居民的食物构成都有贡献, 但并不确定农业或渔猎是否占主导地位。本文通过对87例个体1075枚青龙泉新石器时代居民牙齿的磨耗、龋齿病、牙齿生前脱落、颌骨粗壮程度的观察、分析和对比, 试图从另一个侧面提供当时居民食物构成和经济模式的信息。本研究发现, 相比于其他中国新石器时代人类, 青龙泉居民的牙齿磨耗程度总体偏轻、臼齿磨耗角度多呈倾斜状、龋齿病出现率高、与生活状态相关的牙齿生前脱落出现率低、颌骨粗壮程度不明显。这些发现提示居民的食物较精细,加工程度高, 富含碳水化合物。基于本文发现, 作者认为农业经济在距今5000年左右的长江中游地区已经比较发达, 在居民食物构成中居主导地位,居民可能已经具有较高的食物制作加工技术。