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Meaningful interpretation of archaeobotanical assemblages in the Near East often includes determination of whether dung fuel is the source of some or all of the recovered plant remains. In the years since Miller (Economy and Environment of Malyan, a Third Millennium B.C. Urban Center in Southern Iran. Ph.D. Dissertation, Department of Anthropology, University of Michigan, Ann Arbor, 1982; Paleorient 10:71–79, 1984) and Miller and Smart (J Ethnobiol 4:15–28, 1984) first identified archaeological plant remains from Malyan (Iran) as those of burned dung, subsequent archaeobotanical, experimental, and ethnographic research has been undertaken to test and expand her criteria for its recognition. A key criterion of Miller’s was a high ratio of weed seeds to wood charcoal (or a low ratio of charcoal to weed seeds). When used together with other quantitative measures based on standardizing ratios, this measure can help to illuminate variability in the sources of the recovered carbonized plant remains and some of the taphonomic processes that contributed to the resulting assemblage. Using the Late Early Halaf dataset from Fistikli Hoyuk, Turkey, as a case study, non-parametric statistical analysis was applied to eight such measures, including a new Fragmentation Index (FI), density measures (per litre of sediment) for charcoal, cereal grains, weed seeds, chaff, non-wood items, and cereal-type indeterminate non-wood items, and a relative density measure of charcoal to weed seeds. Each measure was calculated on the basis of 35 samples (n = 8,532). The results of this analysis indicate that these measures, when used in combination with Miller’s weed seed to charcoal ratio, implemented here as the relative density of charcoal to weed seeds, can reveal recovery context-related variations in formation processes that help to clarify both the role of dung fuel in assemblage formation and to differentiate the remains of cereal processing from those of burned fuel.

Cereals were a significant part of the Roman diet, yet knowledge about their cultivation, distribution and consumption in certain regions is particularly lacking. In Europe, studies generally suggest that from the Iron Age to the Roman period there was a reduction in barley cultivation, an increase in spelt over emmer, a preference for free-threshing wheat over glume wheats, as well as the increased cultivation of rye and oats. Up till now, there was little evidence on crop cultivation in Croatia, but the discovery of around 24,000 cereal grains from the oven of a 2nd-4th c. AD Roman villa in the modern town of Osijek provides important insights into diet and subsistence in the Roman province of Pannonia. Here, the dominance of free-threshing wheat, spelt and rye with only a relatively small amount of other cereals, chaff and weeds corresponds well with this pattern seen elsewhere in Europe. The relatively clean grain deposit suggests that this sample represents processed grain ready for final food preparation and consumption at the villa. The morphological variation and overlap seen between the carbonised spelt and free-threshing wheat grains, as well as the identification of ‘stunted’ cereal grains, is also discussed.

We present new evidence of the intentional use of cereal by-products at Stare gmajne, an Eneolithic pile-dwelling site in Slovenia, dated approximately 3160–3100 cal bc. The chaff material, which had been used for tempering, was discovered inside one of the largest discovered loom-weights and analysed. Clay, which was used by the dwellers to make the weight, was tempered with cereal chaff to reinforce it. The practice of tempering, not necessarily for loom weights, has already been proven for earlier settlements, mostly in arid areas where firewood, grazing and building material were scarce. However, tempering has rarely been found in European prehistoric sites. More than 1,800 carbonised and half-carbonised, excellently preserved and well identifiable cereal plant macroremains in less than 1 l of waterlogged clayey material were sorted and counted. Among the recognized plant macroremains, barley rachis fragments and glume wheat (emmer and einkorn) by-products such as spikelet forks and glume bases prevailed. A few grains were also found. Cultivation of the main crops of emmer, einkorn and barley at Slovenian Eneolithic pile-dwelling sites was confirmed again. Among the chaff, a new “strange type” of Triticum dicoccum (emmer) spikelet forks was discovered. The size of the weight and the intentional local use of cereal by-products as temper suggest that late Neolithic (Eneolithic) pile-dwelling societies all around the Alps were highly organized and developed due to expansion of crop production and processing.

Earth buildings are among the richest sources of archaeobotanical materials from the recent past. Thus, mudbrick constructions are extremely rich in plant materials, especially chaff, straw, fruits and seeds. Recovery of these remains enables us to gain a comprehensive insight into the contemporary floras of past settlements and their surroundings. Mudbricks from southwest Hungary which were 100–150 years old and were used there as traditional natural building materials, were examined in this research from an archaeobotanical point of view. Techniques were used that mostly come from modern seed bank research, and the most efficient processing methods were tested and further developed. Different flotation procedures were compared and the minimum sample volume was also determined. A new sodium chloride (common salt) flotation method was developed, providing a useful separation procedure for the recovery of plant remains and diaspores (seeds) from mudbrick. The effectiveness of sodium chloride is similar to other chemicals used in seed bank research, but much more economical. The minimum and optimum sample volumes are 2,500–3,500 cm3; these are necessary to recover most of the taxa preserved in the bricks. A trend in the recovery of different sized seeds was also observed, revealing that the recovery of smaller seeds was less successful. Using the sodium chloride method, more than 18,000 desiccated diaspores were recovered and identified from 212 kg of mudbrick samples, from the period between 1850 and 1930. A total of 249 taxa were identified, most of which are weedy taxa connected to cereal and ruderal weed plant communities.

Archaeobotanical material was recovered in two contiguous compartments of a compound in Monte Mozinho (Penafiel, northern Portugal). These areas comprise storage facilities from three different typologies—dolium, pits and above-ground quadrangular structures in the corner of the compartments. Few carpological materials were found inside the storage structures and all these are cereals which were most likely stored as clean grain. Recovered grains are probably remnants of the last stored crops prior to abandonment of the area. A radiocarbon date obtained on grains of rye positions this event at a time within the 3rd century and the beginning of the 4th century a.d. Outside the structures from compartment 2, abundant crop processing by-products, mostly weeds and chaff, were recovered. Since traditional agricultural communities tend not to waste such organic material, it is likely that it was kept in the area to be used as fodder. Data is ambiguous regarding the possible existence of fodder crops mixed with these by-products. Overall, there is a predominance of millets (Panicum miliaceum and Setaria italica) and rye (Secale cereale), but naked wheat (Triticum aestivum) is also a relevant crop. The presence of oat (Avena) is significant but it is difficult to interpret due to its exclusive presence alongside weeds and chaff. Grape pips (Vitis vinifera) were also found, but these are rare. The Late Roman carpological material from Monte Mozinho is of great relevance on a regional level. It documents and dates the presence of rye and testifies to a multifunctional system in which plant husbandry and animal breeding were intertwined.

Archaeobotanical studies were undertaken at the Yuergou site, which is located in the Turpan basin in Xinjiang, China, and which has been dated to around 2300–2400 years b.p. Altogether 21 taxa were identified. Four cereal remains were identified, Triticum aestivum, Hordeum vulgare var. coeleste, Panicum miliaceum and Setaria italica. The first three were probably cultivated while the last one may not have been grown deliberately, but probably grew together with plants of P. miliaceum. A fruit stone of Ziziphus jujuba (Chinese date) was discovered, which showed that this may have been cultivated around the site during that time. Charcoal of Picea sp. was found, from wood which must have been used as fuel by the indigenous people. Fifteen taxa of wild plants were also identified, most of which can be considered as weeds, and which grew near the site. Burs of Xanthium strumarium were discovered. As nearly all of them were broken, the seeds may have been used by the ancient inhabitants. Since most of the cereal remains consisted of chaff, they must represent by-products. Furthermore, grains of Echinochloa crus-galli may also have been exploited as complementary food resources. All the above indicate that both cultivated and wild plants were used for cereals, fuel, or other purposes, and plant resources played important roles in the daily life of the ancient inhabitants of the Yuergou site.

Analyses of charred remains and impressions of chaff in pise (mudbrick) from the Neolithic sites of Aratashen and Aknashen (sixth millennium cal b.c.) situated in the Ararat valley in Armenia demonstrate that naked barley and possible naked (free-threshing) wheat together with emmer and hulled barley were common. Two lesser known crucifers, Camelina microcarpa (false flax) and Alyssum desertorum (alyssum) were found in the form of crop processing residues. These were frequent in the pise, indicating their use perhaps as an oil source. Lens culinaris (small-seeded lentil) and Vicia ervilia (bitter vetch) were recovered both as carbonized seeds and from crop processing residues in the pise. False flax and bitter vetch were less common than alyssum and lentil. Two charred pips of Vitis vinifera (wild vine) were recovered, suggesting the early use of vines in the region. Flotation samples alone would have provided limited data; examination of crop processing residues used for tempering pise provided important evidence of the plant economy at these two sites.

Plant material like threshing remains has been used systematically as filling and insulation material in buildings for a long time. Such plant material can be found in several places, for example in floor cavities (internal floor deposits, Fehlboden) or in beam holes. For the first time in Switzerland, desiccated plant material like this has been investigated. In this article the analysis of the material from three different sites is presented, each dated to a different period, from the late medieval period to the time just before the industrial revolution. The samples consisted of chaff from Triticum spelta in bulk, and smaller amounts of other cereals such as T. monococcum, Avena sativa, Panicum miliaceum and Secale cereale, plus various weeds. The assemblages in the late medieval samples show evidence of three-field rotation: the high percentage of grassland species is interpreted as an indicator of the fallow land phase within the three-field system. A higher ratio of annual to perennial plants in the more modern samples indicates the development of more intensive tillage and cultivation. Methodological questions regarding sampling strategies of the floor cavity subsamples are investigated. The analyses suggest that the volume of these subsamples should be more than two litres.

This paper presents the archaeobotanical results of three samples from the Gallo-Roman site of Dourges, which probably represents a relay post along an important Roman road from Paris to the Belgo-Dutch basin. One of the samples studied comes from the floor of a burnt stable where the imprints of hooves, most probably from horses, covered the floor. The sample is composed of cereals, crop treatment by-products and straw. A comparison with known dung and litter compositions shows that this deposit most probably consists of stable manure, a mixture of dung and litter, the latter mainly consisting of straw and chaff. Two other samples with large amounts of carbonised cereal remains from a ditch near the burnt stable showed some similarities with the dung and litter remains. This suggests that they represent mostly remnants of animal fodder, which was composed of cereal by-products and sprouted grains of naked wheat and emmer. However, a direct connection of the samples from the ditch with those from the stable could not be proven.

Distinguishing human food from fodder in the archaeobotanical record is a difficult task. These categories are culturally defined and, therefore, not obvious from the plant species represented in archaeological samples, while context, such as storage area or container is not necessarily distinctive for each category. While grain can be consumed as either human food or fodder, depending on the particular needs of a given society, chaff is less suitable for human consumption and more appropriate for other uses, one of which is fodder. Archaeobotanical assemblages from two Late Neolithic sites in northern Greece (Makriyalos and Makri) are dominated by glume-wheat chaff, often in association with fig seeds. This material may well represent the remains of dung, but it was not known if the cereal component was eaten by livestock or mixed with the dung to form dung cakes. Our contribution presents the results of an experiment involving the feeding of einkorn grain and chaff (whole and pounded spikelets) and figs to goats to investigate the effect of livestock digestion on plant material. The implications of this work for the interpretation of archaeobotanical assemblages that may derive from animal dung are considered using the Greek Neolithic assemblages.

Recent archaeobotanical investigations of Late Neolithic sites in northern Greece have revealed a pattern as regards the crop parts represented at each site. Some sites appear to be dominated by chaff, mainly glume wheat chaff, while other sites are mainly characterised by cereal grain and pulses. This pattern could be the outcome of various factors: a. pre-depositional differential treatment of crops selecting for one category of plant remains to arrive at the site, b. depositional, therefore related to the type of activity represented at the excavated contexts and the use of space in relation to plants, and c. post-depositional factors such as erosion, or the type of features sampled. These alternative factors are considered in light of the preliminary results of the archaeobotanical investigation of seven Late Neolithic (5500–4000 cal. B.C.) sites from northern Greece. It is suggested that this pattern is the outcome of a differential use of space in relation to plants (storage, processing/food preparation, refuse disposal), probably related to aspects of the socioeconomic organisation of the settlements.

Three types of experiments were carried out. In the first series of experiments emmer wheat grains (Triticum dicoccum Schubl), var. AR, and peas (Pisum sativum L.), var. RE, were heated at temperatures ranging from 130–700 °C under controlled anoxic conditions for a maximum of 120 min. For each temperature a separate experiment was carried out in a pre-heated tube oven. Image acquisition was carried out on a flat bed scanner with a transparency adapter; for the analysis the image program IMAGE J 1.27 was used. Various size and shape factors are discussed and the definitions of the selected size and shape factors are given. The size and shape were measured and the mean calculated from thirty of the untreated specimens and the charred residues heated at each temperature. The results show a change of size and shape as a function of the temperature. The changes for wheat grains and peas are not identical. It is suggested that the presence of the pericarp enclosing the wheat grains causes this difference. In a second series of experiments it was shown that untreated grains of emmer wheat, bread wheat and macaroni wheat can be separated by measuring the shape, but size varies too much within each species, probably the result of different growing conditions, to be useful for separation purposes. As a result of heating at temperatures higher than 290 °C the shape of the three species becomes identical. This implies that the three species can no longer be separated after being heated, solely on the basis of size and shape. Finally, both emmer wheat grains enclosed by chaff and without chaff were heated under similar conditions. After removal of the chaff from the former, the size and shape of the grains were measured. The results show no significant difference in size and shape between both types.

Since Jones et al. (2000) drew attention to a "new" type of glume wheat from Neolithic and Bronze Age sites in northern Greece, several finds of this morphologically distinct tetraploid wheat form have been made across central and southeastern Europe. Charred remains of this wheat, dating from 819–1031 cal b.c., have also been discovered in a storage pit at late Bronze Age Stillfried, eastern Austria. As both chaff and grains were found, it was not only possible to match the diagnostic features of the spikelet bases to the "new" form, but also to examine the grains, which are strikingly long, slender and flat. A dorsal ridge is absent and there is no hump above the embryo. The embryo angle is relatively low and compression lines are much more distinct. Within the Stillfried store "new" glume wheat grains were also easily separable from two-grained einkorn and spelt grains. The morphology of the grains is not inconsistent with the suggestion that the "new" type glume wheat might correspond to modern Triticum timopheevi. In Stillfried "new" glume wheat was grown as a winter crop, and it seems to have been cultivated as a maslin (mixed crop) together with T. monococcum (einkorn).

Chaff and straw is extensively used as a source of fuel, building material and fodder in arid zones, but this by-product of the cereal harvest is generally under-represented in the archaeobotanical record from north-west Europe. While this is partially a result of differential preservation, the evidence from a number of North African sites suggests that dissimilarities between the two regions in the availability of firewood, grazing and building material play an important role too. Differences in the way wheat and barley were used may represent an additional factor. Three types of use are distinguished: casual ‘use’, intentional local use and use as a commercial commodity, and these can be linked to scales of production and organization in the agricultural system.

Pise (daub or building earth) from Jerf el Ahmar and Mureybet was examined and found to contain plant impressions made by the fine fraction of cereal chaff which had been added to the pise as a tempering medium. Four wild grasses were identified from impressions, while over fifty taxa were identified from charred remains. Chaff tempering was present in all samples examined and was composed of spikelet bases and fragments of spikelets. Several aspects of these findings complement results obtained from charred remains. The sheer quantity of building material with chaff implies that cereals were widely available. De-husking and winnowing appear to have been carried out on a large scale, probably near the site. Firm evidence for wild rye confirms previous identifications for this period in the middle Euphrates, rye being difficult to distinguish from wild einkorn if only grain is available for identification. The quality of the chaff provides some evidence of crop processing.