Mid-Holocene local vegetation dynamics and human impact at Los Castillejos,Andalusia, Spain: evidence from charcoal analysis

From the anthracological study of considerable quantities of charcoal recovered from the excavation of the settlement at Los Castillejos de Montefrío, a synthesis was made of the vegetation dynamics during Recent Prehistory of the area, from the middle of the sixth millennium bc to the beginning of the second millennium bc. The vegetation dynamics mark four anthracological phases over this sequence. From the Late Neolithic (end of the fifth millennium bc) the influence of different activities such as livestock raising, burning and agriculture become evident in the development of the natural vegetation, altering species composition and appearance frequency. The last anthracological phase, MF4, spanning the second half of the third millennium bc, saw the regeneration of the tree vegetation as certain former activities ceased, indicating the environmental singularity of this enclave within the context of the southern Iberian Peninsula.     

The beginnings of fruit tree cultivation in the Iberian Peninsula: plant remains from the city of Huelva (southern Spain)

The combination of an archaeobotanical analysis from two different sites in the city of Huelva (Spain) and the identification of vine fields in the same area suggests that different fruit tree species (grapevine, olive, almond and pomegranate) and vegetables such as melon were introduced into the Iberian peninsula in the transition from the 9th to the 8th century cal bc. These dates represent the earliest chronology for arboriculture within the Iberian Peninsula. The material has been preserved by waterlogging allowing the preservation of a wide variety of species which indicate the development of fruit tree cultivation. The archaeological context provides information on the connections between this innovation and the Phoenician communities that established in the region in search of metal resources. Fruit tree cultivation, and particularly wine production, had a great impact on the local agriculture which was traditionally based on the production of annual crops. The new crops soon became an essential agricultural element of the communities that lived in the south and east of the Iberian Peninsula. From the 8th century cal bc onwards, agricultural production would be mostly market oriented.     

Landscape use and fruit cultivation in Petra (Jordan) from Early Nabataean to Byzantine times (2nd century <Emphasis Type="SmallCaps">bc</Emphasis>–5th century <Emphasis Type="SmallCaps">ad</Emphasis>)

Archaeobotanical analyses of charred seeds, fruit and wood charcoal from the residential part of the ez-Zantur area at Petra, Jordan, provide new data on the agricultural economy and use of the landscape in this famous merchant Nabataean city from the middle of the 2nd century bc to the beginning of the 5th century ad. The study is based on analyses of 7,640 whole and fragmented seeds, pips and fruit stones and 624 charcoal fragments sampled from household deposits. The results show that the food supply was based on common Mediterranean cultivated taxa such as cereals (Hordeum vulgare, Triticum aestivum/durum), pulses (Lens culinaris) and fruit (Olea europaea, Ficus carica, Vitis vinifera), which were probably cultivated both in the city and its hinterland. The by-products from the processing of cereals and fruit trees played a significant role in fuel supply, supplementing woody wild plants obtained from rocky slopes and the desert valley. The variety of fuel resources shows a major capacity to manage complex supply networks and perhaps the rarity of natural woodland cover. The existence of orchards within the city centre and notably olive groves is indicated in the Early Nabataean period (mid 2nd century to mid 1st century bc) but they expanded during the Classical Nabataean period (mid 1st century bc to 1st century ad), probably reflecting specialised fruit growing. Unusual plant remains such as Prunus armeniaca (apricot), P. persica (peach) and Juglans regia (walnut) are considered to be social indicators of prosperity. These archaeobotanical results fit with others from this region and match with the urbanization and social dynamics of the city of Petra.     

Neolithic land use in the northern Boreal zone: high-resolution multiproxy analyses from Lake Huhdasjärvi,south-eastern Finland

Two high-resolution pollen and charcoal analyses were constructed from sediments obtained from a small bay in eastern Finland in order to gain information on human activity during the Neolithic Stone Age, 5200–1800 bc. We used measurements of loss on ignition (LOI), magnetic susceptibility and geochemical analyses to describe the sedimentological characteristics. Palaeomagnetic dating and measurements of ¹³⁷Cs-activity were supported by ¹⁴C-datings. The analyses revealed human activity between 4400 and 3200 bc, which is synchronous with archaeological cultures defined through different stages of Comb Ware pottery types and Middle Neolithic pottery types with asbestos as a primary temper. Direct evidence of Hordeum cultivation was dated to 4040–3930 cal bc. According to the pollen data, more significant effort was put into the production of fibres from hemp and lime than the actual cultivation of food.     

Seven Millennia of human impact as reflected in a high resolution pollen profile from the profundal sediments of Litzelsee,Lake Constance region,Germany

A profundal core from Litzelsee, a small cirque lake in the western Lake Constance region, was investigated by pollen analysis and dated radiometrically. The upper part of the core, chronologically between 5000 cal bc and 1850 ad, was sampled continuously, resulting in a total of 449 samples, each with a sum of 1,000 arboreal pollen grains. Also in this huge data set, rare taxa, normally lacking or very scarce in pollen profiles, were registered. The ecological evaluation of these, with a focus on anthropogenic indicators, sheds light on environmental and human impact history from the Neolithic to Modern times. Further, the results are put in a regional context, together with seven other mostly unpublished pollen profiles studied in the same way.     

From deciduous forest to open landscape: application of new approaches to help understand cultural landscape development in western Norway

Development of the cultural landscape in a village situated by the inner fjords of western Norway is investigated by pollen analysis and quantitative reconstruction methods. Pollen samples from lake sediments and a soil profile were analysed and represent different spatial scales. The Landscape Reconstruction Algorithm (LRA) is applied to a large and a small lake to convert pollen percentages from the small lake into estimated local vegetation cover in selected time periods starting from 2800 cal bc (Middle Neolithic A). This reconstruction shows that estimated forest cover has fluctuated through time, and changes in openness related to human impact are distinct from the Early Bronze Age (1800–1200 cal bc). Pollen analyses from the soil profile indicate forest clearances from the Late Neolithic (2300–1800 cal bc). Gradual intensification of farming is recognized in both pollen diagrams throughout the Bronze and Iron Ages with increasing openness and spatial differentiation in land-use practices. Presence of pollen of cereals and flax record the cultivation of these plants from the Iron Age, and intensification of land-use may have caused erosion and re-sedimentation in the lake in medieval times. To identify a possible landscape in the past, HUMPOL software has been used with the Late Neolithic as a case study. The LRA-based estimates of forest cover are supported by the HUMPOL simulations, but several solutions to the Late Neolithic landscape pattern exist. The results clearly demonstrate how implementation of LRA and HUMPOL improve the understanding of cultural landscape development.     

Determining the responses of vegetation to natural processes and human impacts in north-eastern Poland during the last millennium: combined pollen,geochemical and historical data

Pollen, charcoal and geochemical investigations were carried out on annually laminated sediments of Lake ?abińskie (54°07′54.5″N; 21°59′01.1″E) and the results were combined with historical and climate data to better understand the mechanism behind plant cover transformations. A millennium-long record of environmental history at 6-years time resolution permitted an assessment of vegetation responses to past human impact and climate fluctuations. Our results show that the history of the region with repeated periods of warfare, epidemics, famine and crop failures is well reflected by environmental proxies. Before the Teutonic Order crusade (ad 1230–1283), agricultural activities of the Prussian tribes were conducted at a distance from the studied lake and caused slight disturbances of local forests. A stronger human impact was registered after ca ad 1460. We confirm that co-domination of pine forests with spruce and oak-hornbeam forests on drier habitats as well as the presence of birch and alder woods on wet surfaces near the lake lasted until ad 1610. We identified a transition period of 20 years between ad 1590 and 1610, when forest cover was significantly reduced and the area was partly transformed into open land used for farming activities. The comparison of our data with other pollen datasets from the region confirms significant spatio-temporal differences in the initiation of large-scale woodland clearings in the Great Masurian Lake District. A strong increase in local cultivation was noted after ad 1750 and became even stronger in the period ad 1810–1940. The last 60 years experienced a succession from arable fields and open grasslands to more tree-covered habitats overgrown by birch and alder.     

Wild fruit use among early farmers in the Neolithic (5400–2300 cal <Emphasis Type="SmallCaps">bc</Emphasis>) in the north-east of the Iberian Peninsula: an intensive practice?

The archaeobotanical record of 24 sites from the Neolithic period (5400–2300 cal bc) in the north-east of the Iberian Peninsula is evaluated. Remarkable amounts of data have recently been obtained for the early and middle Neolithic phases. Most of the studied sites were dry and they only yielded charred plant material. Among dry sites, several types of context were evaluated: dwelling areas, hearths, roasting pits and byres. Material was also analysed from a waterlogged cultural layer of one early Neolithic lakeshore site, La Draga. Quercus sp. (acorns), Corylus avellana L. (hazelnuts), Pistacia lentiscus L. (mastic fruits) and Vitis vinifera L. var. sylvestris (wild grapes) were among the most frequently encountered fruits and seeds. Their presence in the archaeobotanical record clearly maps their past ecological distribution in the region. There are differences observed between the charred dry-land material and the waterlogged uncharred material. Wild fruits were mostly present in an uncharred state in La Draga. Therefore, their consumption could go unnoticed in dry sites when fruits were eaten raw or without roasting. Larger amounts of charred remains of certain wild fruits like acorns and hazelnuts found in mountain areas are highlighted as potential evidence of the regular practice of roasting, potentially indicating regional traditions. All in all, our results support an intensive wild plant use at least during the first 1,300 years of the Neolithic period. Evidence of wild plant food consumption becomes scanty towards the second phase of the middle and the late Neolithic (4th and 3rd millennium cal bc). This, however, might also be due to taphonomic reasons.     

Plant food subsistence in the human diet of the Bronze Age Caspian and Low Don steppe pastoralists: archaeobotanical,isotope and <Superscript>14</Superscript>C data

The paper presents the result of analysis of charred food on the interior part of the vessels from the graves of the East Manych and West Manych Catacomb archaeological cultures (2500–2350 cal bc). The phytolith and pollen analyses identified pollen of wild steppe plants and phytoliths of domesticated gramineous plants determined as barley phytoliths. Direct ¹⁴С dating of one of the samples demonstrates that barley spikelets and stems were used in funeral rites by local steppe communities. However, there are no data suggesting that steppe inhabitants of the Lower Don Region were engaged in agriculture in the mid-3000 bc. Supposedly, barley could have reached the steppes through seasonal migrations of mobile pastoralists to the south, use of North Caucasus grasslands in the economic system of seasonal moves and exchange with local people. Nevertheless, presence of carbonized barley seeds in the occupation layers at North Caucasus settlements of 4000–3000 bc requires confirmation by direct ¹⁴С dating of such samples.     

History of agriculture in Mikkeli Orijärvi,eastern Finland as reflected by palynological and archaeological data

The introduction and development of cultivation in eastern Finland was studied by pollen and charcoal analysis of a palaeomagnetically dated sediment profile from Lake Orijärvi, in the vicinity of permanent prehistoric fields. The earliest changes of possibly anthropogenic origin are visible in the pollen data from 1630 b.c. onwards and indications of human impact become more evident from 500 b.c. onwards. According to finds of cereal pollen and AMS-dating of charred cereal grains from the oldest field layer, the onset of cultivation can be dated to the Merovingian period around a.d. 600. To a significant extent the pollen data reflect only the cultivation of Secale during the first 600 years. The marked intensification of agricultural activities including cultivation in permanent fields only becomes evident in the pollen data from about a.d. 1050 to 1080 onwards and the most intensive land use phase dates to a.d. 1300–1965. Archaeological and palaeoecological material indicate that swidden cultivation and permanent field cultivation were in use simultaneously during the late Iron Age. The combination of these techniques together with animal husbandry and hunting formed a subsistence strategy in the climatic border-zone outside the centres of the agricultural core areas.     

Barley grain at Uppåkra,Sweden: evidence for selection in the Iron Age

A metric analysis on hulled barley grain from the Iron Age regional centre of Uppåkra and surrounding sites in southern Sweden has identified a variation in the size of the grain found on these archaeological sites. Large, high-quality grain was found more frequently at Uppåkra when compared to sites in the surrounding area, where smaller grain was more frequent. The observed large grain found at Uppåkra was, however, restricted to only a few house contexts, including hall-buildings, while other contexts on the site, such as areas dedicated to craft production, had barley assemblages containing smaller grain, similar to the size range found on the surrounding sites. The intra-site variation between different contexts at Uppåkra points to a degree of sorting for larger grain and that this variation between grain assemblages was the result of selection after the crop processing was completed. The distribution of grain size at Uppåkra shows a pattern that indicates that the high-quality barley grain was indented for specific individuals or households. The different contexts at Uppåkra have together produced a record spanning the first millennium ad, representing almost the whole existence of the site. The evidence for selection of larger grain can be seen in the hall-buildings throughout most of the first millennium ad, although less prominently during the Late Roman Iron Age (ad 200–400), while during the Migration Period (ad 400–550) several houses on the main site Uppåkra had assemblages of large grain size. The distribution of grain size at the regional centre Uppåkra shows a pattern that indicates that the handling of large high-quality barley grain was part of a spatial organization, and such organization is similar to other functions observed on the site. The long-term record of grain size patterns across time shows that a structure for handling grain was already in place during the early phase of the settlement and that it remained for centuries. This study indicates that the affluence otherwise seen at the regional centre Uppåkra from an abundance of high-status objects, could also include agricultural wealth, with extensive access to high-quality grain.     

An 800 year record of mangrove dynamics and human activities in the upper Gulf of Thailand

A multiproxy record comprising pollen, charcoal, loss on ignition and particle size analyses from two radiocarbon dated sediment cores from Klong Kone subdistrict on the western coast of the Gulf of Thailand provides insights on mangrove dynamics, environmental changes and human activities during the last 800 years. The mangroves were dominated by Rhizophora which indicates that the area has been influenced by the sea level from at least 820 cal bp until 720 cal bp. An intertidal area may have formed that supported mangrove development as part of an old shoreline during 820–720 cal bp. After 720 cal bp, mangroves decreased and were replaced by grasses, suggesting that a lower sea level caused the mangroves to grow closer to the sea until around 140 cal bp. Cereal pollen increased from 720 cal bp suggesting probable use of the shoreline for intensive cultivation. The mangroves were characterised by Avicennia, which increased toward the top of the 2 cores, suggesting that the mangroves then grew further inland, probably due to recent sea-level rise. Intensive human activity is recorded during the 20th century, as indicated by increased particle size, charcoal and carbonate content. At present, human activity in the area includes dams and construction as well as aquaculture.     

From the field to the hearth: plant remains from Neolithic Croatia (ca. 6000–4000 cal <Emphasis Type="SmallCaps">bc</Emphasis>)

Until recently the recovery of plant remains in Croatia was rare, resulting in few studies addressing the nature of Neolithic crop cultivation. This paper presents new archaeobotanical data from eleven Neolithic settlements in coastal and continental Croatia. Within continental Croatia, three sites dating to the Star?evo culture (early/middle Neolithic; ca. 6000–5300 cal bc) and six to the Sopot culture (late Neolithic; ca. 5300–4000 cal bc) are examined along with two Hvar culture sites (late Neolithic; ca. 4800–4000 cal bc) located along the coast. Different settlement types are included in the study: open air sites, tells and cave sites. From the data collected the most common crops identified were einkorn, emmer, barley, lentil, pea and flax, as well as the fruits Cornus mas (Cornelian cherry) and Physalis alkekengi (Chinese lantern), which were particularly dominant in the Sopot culture settlements. By examining formation processes, sieved crop processing products and by-products were identified at six of the sites, suggesting that cereals were processed on a day-to-day basis at the household level. In contrast, the remains from the late Neolithic coastal cave site of Turska Pe? suggest two distinct formation processes. At the eastern side of the cave the plant remains suggest that episodes of dung burning occurred, possibly to clear the cave of excess waste during seasonal habitation of the cave by herders and livestock. Towards the back of the cave, cereal remains and higher charcoal densities may suggest an area used for food preparation or cooking.     

Earliest evidence of a primitive cultivar of <Emphasis Type="Italic">Vitis vinifera</Emphasis> L. during the Bronze Age in Sardinia (Italy)

The discovery of the Nuragic culture settlement of Sa Osa, Cabras-Oristano, Sardinia, has made it possible to investigate the domestication status of waterlogged uncharred grape pips that were recovered from three wells dating from the Middle and Late Bronze Age (ca. 1350–1150 bc). Applying the stepwise linear discriminant analysis method, a morphological comparison of archaeological seeds and modern wild and cultivated Sardinian grapes pips was performed to determine the similarities between them. The results showed that the archaeological seeds from the Middle Bronze Age have intermediate morphological traits between modern wild and cultivated grape pips from Sardinia. In contrast, the analyses performed on the archaeological seeds from the Late Bronze Age showed a high degree of similarity with the modern cultivars in Sardinia. These results provide the first evidence of primitive cultivated Vitis vinifera in Sardinia during the Late Bronze Age (1286–1115 cal bc, 2σ). This evidence may support the hypothesis that Sardinia could have been a secondary domestication centre of the grapevine, due to the presence of ancient cultivars that still exhibit the phenotypic characteristics of wild grapes.     

Plant uses and storage in the 5th century <Emphasis Type="SmallCaps">bc</Emphasis> Etruscan quarter of the city of Lattara,France

An area between land and water was chosen in the 7th century bc by native Gauls and foreign Etruscan and Greek merchants to establish a commercial enclave. Then, in the early 5th century bc, this initial settlement at La Cougourlude with post-built houses on the banks of the small coastal river Lironde was relocated to the margins of a nearby lagoon along the Mediterranean coast, giving rise to the walled port city of Lattara. Archaeological excavations undertaken in the 2000s along the southern wall of Lattara in Quarter 27 revealed three houses which contained almost exclusively Etruscan pottery. The objective of this study is to analyse the archaeobotanical remains from these dwellings so as to identify the plant foods which were consumed and used by their inhabitants, as well as the methods of storage. The question arises whether anything particularly relating to Etruscan origins can be detected from the diet of the inhabitants. To study this aspect we have compared the data collected during the excavation with research undertaken at neighbouring settlements dating from periods either older, contemporary with or younger than Lattara, as well as research undertaken at sites in the Etruscan area of Italy.     

The Iron Age in the Mrągowo Lake District,Masuria, NE Poland: the Salęt settlement microregion as an example of long-lasting human impact on vegetation

Pollen, non-pollen palynomorphs, charcoal and geochemical analyses of sediments from Lake Sal?t (NE Poland) were used to reconstruct vegetation changes related to the activity of the West Balt tribes during the Iron Age, in the period between the second half of the 7th century bc and the beginning of the 10th century ad. We distinguished five phases of human impact on environment. Woodland clearing around the studied lake started at the end of the 7th century bc. The most characteristic feature of this area during the whole Iron Age was a very high representation of semi-natural Betula woodlands, which was probably linked to a shifting agriculture. This type of land use lasted for over 1,500 years, until the second half of the 9th century ad. The greatest reduction in Betula woodlands took place between cal. years 650 and 450 bc. Its regeneration took place after ca. ad 830 when human activity decreased.     

Boreal forest dynamics in north-eastern Sweden during the last 10,000 years based on pollen analysis

A pollen record obtained from a 2.2-m sediment succession deposited in a small lake in the province of Västerbotten, north-eastern Sweden, reveals the presence of continuous forest cover since 8,500 calendar years before present (cal b.p.). Forest with abundant Pinus (pine) and Betula (birch) initially colonized the area, followed by a dominance of deciduous trees, primarily Betula, from ca. 8,000 to ca. 3,200 cal b.p. Pollen accumulation rates of Quercus (oak), Ulmus (elm) and Tilia (linden) suggest the possible local presence of these thermophilous tree species during this period. The climate gradually became colder and moister around 3,500 cal b.p. and an increased abundance of Sphagnum spores indicates paludification. Picea (spruce) became established around 3,200 cal b.p. and less than 500 years later this was the dominant tree species around the lake. The fire frequency as inferred from charcoal particles exhibits a general increase from ca. 3,000 cal b.p. with subsequent charcoal accumulation maxima at around 2,800 cal b.p., 1,700 cal b.p. and in recent time. The human influence on vegetation was significant during the last 200–300 years. Soil erosion increased substantially and fern spores amount to ca. 55% of the total pollen assemblage in the uppermost samples. These results suggest an extensive anthropogenic impact on the local forest ecosystem, with abundant logging, burning and ditching in the vicinity of the lake. Independent evidence of sub-recent human-induced environmental change is provided by historical accounts. Complementary information on catchment soil development and aquatic nutrient status was provided by records of magnetic susceptibility and elemental carbon, and nitrogen contents obtained from the same sediment core.     

Studies in the taxonomy of the Polypores II

The following genera are redefined:Albatrellus S. F. Gray,Heterobasidion Bref.,Haploporus Bond. et Sing. ex Sing.,Fomitopsis P. Karst. andRigidoporus Murrill two new subgenera are described:Polyporus subgen.Dendropolyporus Pouz. (type:Polyporus umbellatus) andRigidoporus subgen.Neooxyporus Pouz. (type:Polyporus latemarginatus); the genusOxyporus (Bourd. etGalz.)Donk is classified as a subgenus of the genusRigidoporus,Murrill and the generaBjerkandera P. Karst. andLeptoporus quél. are classified as subgenera of the genusTyromyces P. Karst. The new subfamilyAlbatrelloideae Pouz. (genera:Albatrellus andGrifola) is described and 14 new specific combinations are made. The new genusIrpicodon Pouz. (type:Irpex pendulus) is proposed.     

Historic grazing in southern New England,USA, recorded by fungal spores in lake sediments

Decadal-scale analyses of fungal spores in a lake-sediment core from Ware Pond, located in the town of Marblehead in northeastern Massachusetts, test the potential of this approach for reconstructing past sheep and cattle grazing in southern New England, USA. The influx of spores of Sordaria and other coprophilous taxa increases at ad 1650, which corresponds with the beginning of European settlement, and subsequent peaks in these taxa at ad 1840 coincide with maximum abundances of weedy and agricultural taxa in the pollen record. Historical data from Marblehead and neighbouring towns indicate that maximum numbers of cattle and sheep occurred at this time. These findings suggest that fungal spores in New England lake sediments can be used to reconstruct changes in grazing pressure over time at the landscape scale.     

Palaeocladocerans as indicators of environmental, cultural and archaeological developments in Eifel maar lakes region (West Germany) during the Lateglacial and Holocene periods

The use of subfossil cladocerans is rare for understanding environmental, cultural and archaeological developments of lakes in Europe. In 2007, we collected a 12-m long sediment core from Lake Schalkenmehrener Maar (SMM), Germany for the analyses of subfossil cladocerans. Dating of core was based on tephrochronology, radiocarbon and pollen stratigraphy. Pollen-based chronostratigraphy indicated a decline of species richness and abundance of chydorids during the Lateglacial (ca.14500?cal?yr?bp) with dominant cold preferring taxa Acroperus harpae Baird and Alona affinis Leydig. During the early B?lling, the abundance of cladocerans increased commensurate with growth of birch (Betula L.) and pine (Pinus L.) trees. Except a spike of Bosmina coregoni Baird during the Younger Dryas, cladoceran assemblages remained stable from the B?lling to the mid-Atlantic period. During the Neolithic (ca. 4300?bc), the abundance of B. coregoni increased sharply with reciprocal decrease in Daphnia. However, as soon as Daphnia was dominant (ca. 4250?bc), a reciprocal decline in abundance of B. coregoni occurred. The mid-Holocene change in cladoceran abundance coincided with the use of hardwood forest. This situation ended at ca. 4000?bc and remained unchanged throughout the Neolithic and Bronze Age (ca. 3000?C1200?bc). Low Daphnia abundance indicated reduced water quality in the Hunsr??ck-Eifel culture (ca. 800?bc). A spike of B. coregoni at ca. ad 150 indicates construction of the Roman Villa Rustica and extensive farming. However, reoccurrence of Daphnia at ca. ad 470 indicates the retreat of the Romans from the Eifel region. From the early Frankish rule (ca. ad 500) to the Medieval period (ca. ad 1500), species richness reduced but abundance of B. coregoni increased indicating a switch in lake ecosystem. The loss of species richness and the lack of precise evidence of the human activity in the region in the past have impeded the restoration of the ecosystem of the Lake SMM.