The diet of Eneolithic (Copper Age, Fourth millennium cal b.c.) pile dwellers and the early formation of the cultural landscape south of the Alps: a case study from Slovenia

Analyses were performed of plant remains from the Late Neolithic (in Slovenian terminology corresponding to Eneolithic or Copper Age, ca. 4300–2300 b.c.) pile dwelling Hočevarica in the Ljubljansko barje (Ljubljana Moor), Slovenia. This settlement existed between ca. 3650 and 3550 cal b.c. Seeds, fruits, wooden piles, macroscopic charcoal and pollen from the cultural layers were analysed. The remains of domestic plants such as charred grains of Hordeum vulgare (barley), Triticum monococcum, T. dicoccum (einkorn and emmer wheat) and Papaver somniferum (poppy seeds), as well as seeds of weeds such as Chenopodium album-type indicate early cultivation in the area. In addition, numerous remains of nuts and berries, especially of Quercus sp., Cornus mas, Rubus fruticosus and Corylus avellana demonstrate that the gathering of wild plants was an important part of subsistence. Palaeoecological and archaeobotanical data from Hočevarica further suggest that cleared land was used for agriculture and pastures during the Neolithic, and that different wood was cut for construction and for fuel. The species assemblage from Hočevarica is very similar to those recovered from northern Alpine lake dwelling sites, however, several new taxa (e.g. Lathyrus sativus, Vicia sp.) appear in the assemblage. One of the most surprising finds is the seed of wild grape (Vitis vinifera ssp. sylvestris), which are the oldest on-site remains of grapevine from Slovenia.     

The long history of Cannabis and its cultivation by the Romans in central Italy, shown by pollen records from Lago Albano and Lago di Nemi

The cores from the Albano and Nemi lakes, near Rome, were studied within the European Union funded PALICLAS project and provided high resolution records of the Late-glacial and Holocene. Pollen evidence of increasing human influence on vegetation was recorded in the Holocene parts of both diagrams, and the Cannabis (hemp) curve was one of the major signs. In this paper we present unambiguous pollen evidence from the Cannabaceae records for the cultivation of hemp in central Italy by the Romans. The oldest records of Cannabis and Humulus (hop) date from to the Late-glacial. Hop pollen values rise during the mid Holocene, while hemp pollen becomes more abundant from ca. 3000 cal B.P. onwards. The highest earliest hemp peak (21%) is dated to the 1st century A.D. This ‘Cannabis phase’, with the abrupt rise of hemp pollen soon after the rise of cultivated trees (Castanea, Juglans and Olea) is associated with the increase in cereals and ruderal plants. This unambiguous proof of cultivation by Romans around 2000 B.P. occurs as well as a long lasting pre-Roman presence of hemp in the area, which is natural and possibly also anthropogenic. Subsequent clear episodes of cultivation in the medieval period were found. Received February 4, 2002 / Accepted September 13, 2002 Correspondence to: Anna Maria Mercuri, e-mail: mercuri.annamaria@unimo.it     

An experimental approach to Neolithic shifting cultivation

Archaeobotanical data from Late Neolithic lake-shore dwellings (4300-3500 cal B.C.) in the northern Pre-alpine lowlands are interpreted in different ways. The presence of permanent arable fields as well as arable fields with short fallow phases and shifting cultivation with slash-and-burn has been discussed. To test these hypotheses experimentally we have been conducting tests in a forest northeast of Stuttgart since 1994. The slightly south-exposed experimental area of approximately 4.5 ha on a loess soil is covered by mixed deciduous forest, is available for at least 20 years and has been divided into 34 plots of 30 × 30 m. Up to 2001, five plots were used for experiments. The normal procedure is clearing, burning the dry small timber (less than 10 cm in diameter) and then growing winter cereals (bread wheat) for one season. The yields were between 2000 and 4000 kg grains per ha. The harvest was more or less free from weeds. First attempts with summer crops gave much lower yields of about 1100 kg grains per ha. Continuous cereal growing on the same place in the following years resulted in minimal to zero yields, mainly due to vigorous weed growth. These weeds are not crop weeds, but forest perennials of clearings and forest fringes. Ploughing to remove the weeds is not possible, because of the presence of roots and tree-stumps, most of them still living. Weed regulation by hoeing, burning or cattle grazing remains to be tested. Protection of the crop from game and birds is by fences and nets, but protection from mice seems difficult. In the spectra from the pollen traps, clearing and burning are strongly indicated, but cereal growing only slightly. Received July 31, 2001 / Accepted April 9, 2002     

Some aspects of Late Iron Age agriculture based on the first results of an archaeobotanical investigation at Corvin tér, Budapest, Hungary

Until now, very little was known about the agriculture of the Late Iron Age in Hungary. This paper describes the first results of an archaeobotanical examination of a late Iron Age, Celtic settlement in Budapest. It is the first systematically sampled and representatively investigated site of this time period in Hungary. Most of the samples come from different types of pits, which were subjectively sampled. The macrofossils were carbonised and, apart from many seeds and fruit stones, consisted mostly of charcoal. Among the seed remains both cultivated and wild species were present. The spectrum of cultivated plants was marked by a large number of cereals. The dominant cereals were Triticum spelta L. (spelt wheat) and Panicum millaceum L. (broomcorn millet), but also common were Avena sativa L., Avena sp. (oats), Triticum monococcum L. (einkorn), Hordeum vulgare L. (barley); Triticum aestivum/durum/turgidum L./Desf./L., incl. T. compactum Host. (bread wheat, including club wheat). Secale cereale L. (rye) and Triticum dicoccum (Schrank) Schübl. (emmer) were rare and seemed to be less important. The weeds and synanthropic vegetation, including ruderals, were represented by many taxa, and some of them also occurred in large amounts. The main cereals were sown as winter crops, judging from the rarely occurring of plants accompanying the cereals. Wild fruits contributed to the daily diet, too – as seen from the stones of Cornus mas (cornelian cherry), Crataegus sp. (hawthorn) and Prunus spinos (sloe, blackthorn). There were no finds of cultivated fruits. Received October 19, 2001 / Accepted January 30, 2002     

Archaeobotanical analysis of some early Neolithic settlements in the Kujawy region, central Poland, with potential plant gathering activities emphasised

Neolithic settlements in the Kujawy region of central Poland are represented by seven archaeological sites which have botanical material archaeologically dated to the Linear Pottery culture (LBK) (ca. 5400-5000 cal. B.C.) and the Lengyel culture (ca. 4400-4000 cal. B.C.). The composition of plant remains suggests that Stipa pennata s.l. played a certain role in the economy of the Neolithic settlers. The presence of this xerothermic grass is best explained by local gathering rather than distant transport or coming into the sediment by chance. The finding of Hierochlo? cf. australis grains represents the first identification of this plant in archaeobotanical material from Poland. This, now rare, plant contains coumarin and for this reason could have been useful in prehistory. Other plants such as Bromus spp., Chenopodium album type, Fallopia convolvulus and Galium spp. were found in large quantities, and although common weeds now, they could also have been collected by the Neolithic settlers. Plants such as Corylus avellana and Vaccinium vitis-idaea that are typically considered to be collected as foods are present in the studied material but in very small quantities. Received September 17, 2001 / Accepted March 13, 2002     

The presence of two-grained einkorn at the time of the Bandkeramik culture

At the end of the 6th millennium B. C. Triticum monococcum (einkorn) and Triticum dicoccum (emmer) were the main cereals of the early Neolithic Bandkeramik culture in central Europe. New archaeobotanical investigations at relevant Bandkeramik sites reveal the regular occurrence of morphologically two-grained einkorn. Some preliminary thoughts on the state of research and the possible origin of two-grained einkorn forms are presented here. Received January 7, 2002 / Accepted August 5, 2002 Correspondence to: Angela Kreuz     

Peptide growth factor phytosulfokine-α contributes to the pollen population effect

Density-dependent pollen germination and tube growth in vitro is a well-documented phenomenon, termed the pollen population effect, but far less is known about its molecular basis. We present evidence to support phytosulfokine-α [Y(SO₃H)IY(SO₃H)TQ; PSK-α] as a native bioactive factor contributing to this effect. Mature pollen grains of Nicotiana tabacum L. var.macrophylla were incubated in liquid medium for 2 h. Pollen germination frequency increased in a density-dependent manner from 625 to 46,000 grains/ml. Conditioned medium, obtained from the medium of pollen cultured at a density of 10,000 pollen grains/ml for 12 h, promoted the germination of pollen cultured at a low density (625 grains/ml). A rabbit antiserum against PSK-α specifically inhibited the promotive effect of conditioned medium. Quantification by enzyme-linked immunosorbent assay showed that the conditioned medium contained 0.4 nM of PSK-α. Exogenous PSK-α also stimulated pollen germination in the low-density culture. These results indicate that PSK-α is an important regulator involved in the pollen population effect. Received: 15 March 2000 / Accepted: 24 May 2000     

Biostratigraphy and <Superscript>14</Superscript>C dating of a lake sediment sequence on the north-west Estonian carbonaceous plateau,interpreted in terms of human impact in the surroundings

The sediment stratigraphy of a medium-sized mixotrophic lake (Ruila) situated below the highest shoreline of the Baltic Ice Lake in the West-Estonian Lowland is described. The lake is without natural inlets our outlets. The reconstruction of vegetation and land-use history based on pollen data, combined with available archaeological data and detailed ¹⁴C dating allows us to give a provisional reconstruction of the temporal and spatial pattern of natural and human induced environmental changes in north-west Estonia during the Holocene. Both radiocarbon dates derived from terrestrial macrofossil dating by accelerator mass spectrometry (AMS) and conventional dating of bulk lake sediment are discussed. The isolation of the lake basin from the Yoldia Sea took place ca. 9700 cal B. C. The Ancylus Lake transgression at ca. 8400 cal B. C. did not reach the basin, but caused a ground water rise, seen in the sediment stratigraphy of the lake. The first signs of human impact on the pollen record appear ca. 5400 cal B. C. (Late Mesolithic). The history of arable farming has been divided into three periods: 1) introduction of crop cultivation and animal husbandry (1500 cal B. C. – A. D. 500); 2) establishment of animal husbandry A. D. 500–1000) and 3) establishment of crop cultivation and intensive cattle breeding (A. D. 1000–today). Due to unfavourable eda-phic conditions the introduction of arable farming was delayed for more than 1000 years compared with elsewhere on the north coast of Esotnia, and intensity of land-use never reached the same proportion as in these areas. Received August 15, 2001 / Accepted August 5, 2002 Correspondence to: Leili Saarse     

Extensive forest grazing and hay-making on mires – vegetation changes in south-central Sweden due to land use since Medieval times

The influence of pre-industrial animal husbandry on the boreal forest in south-central Sweden has been studied by pollen and charcoal analyses of peat profiles from two mires in the vicinity of a shieling site. The impact of farming on the local vegetation development is demonstrated from cal. A. D. 1300–1500 in three ways: forest clearance and cultivation of cereals at the local shieling site; alterations of hydrology and vegetation, such as an increase in Cyperaceae, at mires used for hay production; changes in the composition in the surrounding forest, with decreasing proportions of Betula, Picea and boreo-nemoral broadleaved trees and a consequent increase in Pinus, due to grazing and a change of fire regime. Similar alterations to the forest vegetation are noted at other sites in central and northern Sweden during the last thousand years, when the system of using shielings became more widespread. Hence, early animal husbandry is demonstrated to have had a regional impact on the long-term boreal forest development, replacing the original mixed deciduous-coniferous forest with Pinus dominated forest. Received November 27, 2001 / Accepted June 20, 2002 Correspondence to: Marie Emanuelsson     

Roman plant remains from Veli Brijun (island of Brioni), Croatia

41 archaeobotanical samples were analysed, which had been collected from the seabed at uvula Verige (Verige bay) on the island of Veli Brijun, Croatia, the site of a Roman villa which was settled from the 1st to the 5th century A. D. From the analysis of plant macrofos-sils it is evident that the eu-Mediterranean evergreen woodland, today described as Quercion ilicis in the phyto-sociological system, already existed in the Roman period. During this period it became degraded as a result of human activities to other vegetation types such as maquis and garrigue scrub, and grassland. The remains of Vitis vinifera (grapevine), Olea europaea (olive), Ficus carica (fig), and Pinus pinea (stone pine) were most frequently recorded; they all derive from very important and characteristic Mediterranean foods. Prunus avium (sweet cherry) and P. persica (peach), some vegetables and spices were probably cultivated, too, as well as some cereals, most probably Panicum miliaceum (millet). Juglans regia (walnut), Castanea sativa (sweet chestnut), and Corylus avellana (hazel) were possibly cultivated on the island or imported from neighbouring Istia. The records of some fresh water plants show that there was fresh water in uvala Verige and its surroundings in Roman times, much more than today. Received February 29, 2000 / Accepted January 31, 2001     

Prehistory of plant growing and collecting in northern Italy, based on seed remains from the early Neolithic to the Chalcolithic (c. 5600–2100 cal b.c.)

The stages of the early Neolithic and the spread of agriculture in northern Italy are difficult to determine and basically still unclear, since this region was influenced by deeply different cultures coming from both the Mediterranean coasts and the Balkans. The complex interrelations due to the contributions from both cultures are reinterpreted here thanks to recent data, modifying a picture which 15 years ago was believed to be definite. According to radiocarbon chronology, the appearance of the earliest farming communities in northern Italy should be dated around 5600–5500 cal b.c. Early farmers cultivated several cereal and pulse taxa, of which the more important were Hordeum vulgare/distichum, Triticum dicoccum, T. monococcum, T. aestivum/durum/turgidum, Lens culinaris and Pisum sp. In addition they gathered many wild plants. The spread of agriculture was a rapid phenomenon and within a few centuries agriculture was established into the Alps. Little is known about the middle and late Neolithic, with the Square-mouthed pottery culture “Bocca Quadrata”, from c. 5100 cal b.c. onwards, since most of the archaeological features discovered up to the present have produced only a few plant remains. We demonstrate the introduction of poppy and a few other innovations like a slightly increased cultivation of free-threshing cereals and flax. Archaeobotanical analyses from Chalcolithic or Copper Age settlements, from c. 3500 cal b.c. onwards, are even scarcer and a comparison with the earlier Neolithic settlements does not yet seem possible.     

First archaeological evidence of banana cultivation in central Africa during the third millennium before present

Phytoliths recovered from refuse pits excavated in central Cameroon and dated to ca 2500 B.P. have been positively identified for the first time in Africa as derived from Musa the cultivated banana, after a comparative study of Musa and Ensete phytoliths. This discovery provides archaeologists with unequivocal proof of early agriculture in central Africa. Furthermore, the presence of banana in Cameroon much earlier than previously assumed could explain how agriculture spread through the rain forest. Lastly, as Musa is of Asian origin, this study provides the first concrete evidence of contacts across the Indian Ocean a millennium earlier than currently accepted. Received July 12, 1999 / Accepted May 4, 2000     

Stone Age to recent land-use history at Pegrema, northern Lake Onega, Russian Karelia

The village of Pegrema in Karelia may be regarded as a Stone Age innovation centre in the large Lake Onega area. Two pollen and plant macrofossil diagrams are presented which represent the first contribution to the study of human impact in the area using anthropogenic pollen indicators. A continuous but sporadic human presence from the Mesolithic onwards is demonstrated. While there is no archaeological evidence relating to the period 4200–3000 B.P., the pollen data suggest continuous, though rather sparse human presence. The data do not support any natural catastrophes in Pegrema as has been suggested elsewhere. Cerealia pollen is recorded earlier than expected (c. 5000 B.P.=. In the Bronce Age and Iron Age, the settlement of the Zaonezhye peninsula is reflected by a slight increase in herb pollen representation, sporadic Cerealia pollen and several periods of regression in Picea. The long introductory period of agriculture to the area, as well as the similarities and discrepancies between different sources of evidence (palaeoecological, archaeological and historical) are discussed at some length. The start of land clearance for permanent cultivation in the profile Pegrema S was dated to the late 13^th century. The beginning of more intensive field cultivation in the 15^th century is clearly seen in the pollen succession at both localities. The fluctuation in anthropogenic indicators can be related to population density based on historical data. The village of Pegrema was depopulated in 1956 which is reflected in a distinct decline in settlement indicators. Received February 17 / Accepted May 19, 2000     

Multi-disciplinary evidence of the Holocene history of a cultivated floodplain area in the wetlands of northern Colombia

An environmental reconstruction of the last 10,000 ¹⁴C years of a frequently flooded wetland ecosystem in the lower Magdalena valley in northern Colombia is presented, on the basis of a multi-disciplinary study of the sediments of the upper 15 m of the core from Boquillas (74°33'E, 9°7'N; 20 m a. s. l.). We used the following studies: pollen, lithology, organic structures, clay mineralogy, soil and sediment geochemistry, and δ¹³C values. The chronology is based on 13 AMS radiocarbon dates; the humic acid fractions were used in the case of seven samples. Pollen from local origin (swamps, open grass-rich vegetation, and gallery forest) show the development of the wetland area. River-transported pollen from a greater distance (dry forest, montane forest, Alnus) show changes in river activity and reflect large-scale changes of climatic conditions in the Momposina basin. From c. 10,010 to 9370 uncal B. P. (zone BQS-Ia) the river system was of high energy, as inferred by the lithological changes. The landscape was dominated by open grass-rich vegetation with gallery forest along the streams. A marked representation of Alnus and montane forest taxa indicate significant water transport and river dynamics. Climatic conditions were dry. From c. 9370-8430 uncal B. P. (zone BQS-Ib) wetlands were isolated from the main river system, and clayey sediments with kaolinite, smectite and illite as the main minerals accumulated in a lower-energy environment. Climatic conditions were dry and changes in the seasonal precipitation favoured the expansion of the gallery forest. From c. 8430 to 8040 uncal B. P. (zone BQS-Ic) low values of river-transported pollen indicate dry climatic conditions and open vegetation became more abundant. The flooding frequency of the Boquillas site diminished. From 8040 to 4900 uncal B. P. (zone BQS-Id) the Boquillas site was dominated by open vegetation with patches of gallery forest along the streams. Supply of river-transported allochthonous pollen (from many sources) was minimal. Clay minerals from the sediments suggest variable temperature and precipitation. From c. 4900 to 1550 uncal B. P. )zone BQS-II) the site was within the reach of the main river system as is the case today. Frequent flooding, coinciding with peaks of river-transported grains of Alnus and high sediment supply, point to high precipitation in the composite catchment area of the Magdalena, Cauca, San Jorge, and Cesár rivers. High values of phosphorous in the upper part of the core point to the presence of a pre-Hispanic civilization, approximately from 2000 uncal B. P. onward. Construction of an extensive drainage system allowed irrigation as well as drainage depending the annual cycle of precipitation. The landscape was significantly modified and allowed an extensive crop production on a system of raised fields. Received May 18, 2001 / Accepted June 15, 2001     

Continuity and changes in plant resources during the Neolithic period in western Switzerland

The Neolithic and Bronze Age (4400-1570 B.C.) pile dwellings of Concise-sous-Colachoz on the shore of Lake Neuchatel (Canton of Vaud, western Switzerland), known as an archaeological site for more than 140 years, were recently re-investigated due to rescue excavations. Plant macrofossil analyses were done for several Neolithic occupation phases (3868-2440 B.C. the Cortaillod classique, Cortaillod moyen, Cortaillod tardif and Auvernier periods) with a focus on cereal remains, and additionally, archaeological deposits dating to the Cortaillod moyen culture (3710-3677 B.C.) were studied in detail. The preliminary study of cereal macrofossil remains from all the mentioned Neolithic phases show that the most important cereals were Triticum aestivum/durum/turgidum (naked wheat), T. monococcum (einkorn) and Hordeum vulgare (barley). The preferences for specific crops did obviously not alter significantly through time, but, extraordinarily, significant amounts of einkorn continued to be grown for at least 1400 years during the Neolithic period. Other cultivated plants were Pisum sativum (pea), Linum usitatissimum (flax), and Papaver somniferum (opium poppy). Additionally to the seeds, capsule fragments of opium poppy were found in the Cortaillod moyen deposits. These represent the first finds of uncharred capsule fragments in Europe. Compared with other central European sites, opium poppy was very common during the 38th and 37th cent. B.C. and obviously less appreciated towards the end of the Neolithic in the western part of Switzerland. In central Switzerland the trends seem different: there opium poppy was mainly used during the Late Neolithic period. This may be due to cultural differences within contemporaneous human societies. Wild fruits which were collected as plant resources during the Cortaillod moyen period included Prunus spinosa (sloe), Cornus sanguinea (dogwood), Malus sylvestris (apple), Rubus idaeus/caesius/fruticosus (raspberry/dewberry/blackberry), Fragaria vesca (wild strawberry), Rosa sp. (hip), Quercus sp. (acorn), Corylus avellana (hazelnut), and Fagus sylvatica (beechnut), among others. Compared with other Neolithic sites in westem and central Switzerland the local population of Concise-sous-Colachoz used few sloes, while dogwood fruits were in use throughout the Neolithic period at Lake Neuchatel. Received September 4, 2001 / Accepted May 13, 2002     

Vegetation in the mountains of northwest Iberia during the last glacial-interglacial transition

A new core taken from a site in the Sierra de Courel range of mountains in the northwest Iberian peninsula, Spain, enables a palaeoenvironmental reconstruction to be made of the biological events resulting from climatic changes and human activities during the last 17,000 years in the area. The sequence begins with a phase characterised by the dominance of Gramineae (Poaceae) and Pinus. A markedly arid period with prevalence of Artemisia pollen occurred between 17,5000 and 15,500 uncal. B.P. Subsequently, a succession of woodlands with Betula, Pinus and other mesophilous and thermophilous trees was recognised during the period 15,500-13,500 uncal. B.P. Between 13,500 and 10,300 uncal. B.P. herbaceous vegetation formations indicating moister conditions dominated the pollen record, although a maximum of Gramineae has been dated during the period 11,300-10,300 uncal. B.P. Comparison with other pollen data from neighbouring mountains allows an interpretation of the vegetation changes during the glacial/interglacial transition in the mountains of northwest Iberia. The Holocene pollen record from the site does not differ markedly from other records in the area, tree expansion occurring before 10,000 uncal. B.P. and high values of deciduous Quercus mixed with other trees and shrubs persisting until 3500 uncal. B.P., when increased human activities are shown by a fall of the tree pollen percentages. Received July 7, 1999 / Accepted May 22, 2000     

The embalming of the ancestors of the Dutch royal family

During the restoration of the main church in Breda (the Netherlands), the city archaeologists rediscovered a tomb with remains of the ancestors of the Dutch royal family. Research was carried out prior to the reburial of the remains. The combination of historical, osteological, dendrochronological and ¹⁴C data provided names and dates for 7 of the 8 embalmed bodies. The tomb was in use between A.D. 1475 and 1526. Archaeobotanical results could be compared with several recipes for embalming from the same period. Strikingly many macroremains were found where mainly pollen was expected. This could mean the bodies were resting on a bed of herbs and spices, but it could also have been due to the lack of confidence of the embalmers; they may have used all the available aromatics to conceal the smell of the corpse. At least some of the species were imported from the Mediterranean and/or subtropical regions, but others were probably locally cultivated. Received August 27, 2001 / Accepted April 1, 2002     

Evidence for Mesolithic agriculture in and around central Europe?

A critical assessment of the data recently put forward in favour of a ‘Mesolithic agriculture’ for Central and Northern Europe is presented. The archaeobotanical record is quite clear: hundreds of excavations of early Neolithic sites, whether from Linearbandkeramik or Trichterbecher (funnel beaker) settlements have produced remains of cultivated plants in large numbers. In contrast to this, all Mesolithic sites excavated so far have not revealed even one macroscopic find of crop plants. The ‘Mesolithic agriculture’ as assumed by several authors, is based solely on single pre-Neolithic pollen grains of the Cerealia-type that occur in pollen diagrams. It is shown that absolute distinction of pollen from wild grasses and cereals is impossible. There is a certain overlapping of both types that must not be neglected. Because of the large pollen sums in modern pollen diagrams, even very scarce grains of Cerealia-type pollen are encountered. Most of these single pre-Neolithic grains must derive from native wild grasses, while others come by long-distance transport etc. Another important feature is the scattered occurrence of Cerealia-type pollen grains from the early Holocene (or even Pleistocene) to the start of the Neolithic. They do not occur in synchronous phases and even in neighbouring sites they do not agree in age. As long as there are no well-dated macro-remains of crop plants of pre-Neolithic age, there is no evidence of Mesolithic agriculture.     

Pollen morphology of selected crop plants from southern China and testing pollen morphological data in an archaeobotanical study

Identification of pollen grains of cultivated plants is essential in archaeobotanical studies. In this study, we investigated the pollen morphology of 30 species which are representatives of most of the crop plants in southern China, using a light microscope. Our results show that the pollen grains of these species or genera can generally be identified by their size, aperture(s) and exine sculpture. We found that: (1) some cultivated cereals can be distinguished from wild species of Poaceae according to their size frequency combined with their morphological features; (2) the lengths of the equatorial diameter (E), polar axis (P) and the greatest dimension of the lumina (the size of the network sculpturing) of the exine reticulum may be diagnostic features to distinguish some brassicaceous vegetables. There are significant differences between the E and P values among Brassica campestris (B. rapa, oilseed rape, Chinese cabbage), B. alboglabra (B. oleracea var. alboglabra, gai lan, Chinese kale), B. parachinensis (B. rapa var. parachinensis, choy sum, Chinese flowering cabbage) and B. chinensis (B. rapa ssp. chinensis, pak choi), but moderate differences in the longer axis length of the reticulum lumina, which provide potential for identifying species on the basis of pollen grains. We compared the P values and the longer axis length of the lumina of modern specimens of Brassicaceae pollen grains with those of fossil pollen extracted from the Ming-Qing cultural layer in the Fuqikou site at Chongqing, China, and found that the fossil pollen grains of Brassicaceae probably represent vegetable plants related to B. parachinensis. Moreover, we measured the diameters of rice pollen grains from modern paddy fields to assess the pollen size frequency and found that the size range from ~?34 to 38 µm is closely associated with rice pollen in southern China, which can be used to detect pollen signals of human activities in archaeobotanical investigations.     

A new archaeobotanical database program

The available quantity of archaeobotanical data derived from the identification of macroremains has expanded considerably over the last few decades. In order to obtain a supraregional or even regional overview for a particular period of time, or of the distribution of a single species, a database is needed. At the Archaeobotanical Department of the Institute of the "Kommission für Arch?ologische Landesforschung in Hessen e.V." (KAL) such a database has been developed in the last few years. It is suitable for the handling of large quantities of archaeobotanical results, including a whole range of background information comprising archaeological, ecological and other related data, and offers various possibilities for the evaluation of these data. Received January 8, 2001 / Accepted April 9, 2002