Trees Underground: New Insights into Trees and Woodmanship in South-east England c. AD 800–1300

Summary

Study of wood recovered from waterlogged archaeological sites in London reveals much about the trees that grew in the city's hinterland between about AD 800 and 1300. Tentative reconstructions of some specific types of trees and ‘treeland’ have been made by combining three-dimensional recording of the timbers and roundwood with examination of how the wood was used, tree-ring analysis, species identification and experimental work in ancient woodland. It has also been possible to gain some appreciation of general trends during the mediaeval period such as the intensification of woodland management and the disappearance of wildwood conditions.     

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     

Argyll oakwoods: Use and ecological change, 1000 to 2000 AD — a palynological-historical investigation

Summary

This paper explores the relationship between ecological change and human use in Atlantic oakwoods during the last millennium. Information on vegetation change derived from high resolution pollen analytical studies can sometimes be satisfactorily linked with localised documentary evidence of historical woodland management. Key findings based on this approach using case studies of individual woods in Lorn are presented. Relatively diverse woods, probably containing old-growth, were transformed in the medieval period into disturbed open stands used for pasturage and local domestic wood supply. Around or prior to 1700 AD commercial management began and modes of exploitation changed so that, for a period until the late 19th or early 20th century, stands were cropped intensively. In the most recent 100 years or so, use of the woods has been relatively minor except as a grazing resource. The consequences of this history for the development of the current condition and character of Atlantic oakwood resources are discussed with reference to elements of woodland biodiversity such as arboreal species composition and Atlantic bryophyte assemblages.     

Palaeodiet reconstruction in a woman with probable celiac disease: A stable isotope analysis of bone remains from the archaeological site of Cosa (Italy)

Stable isotope analysis in the reconstruction of human palaeodiets can yield clues to early human subsistence strategies, origins and history of farming and pastoralist societies, and intra‐ and intergroup social differentiation. In the last 10 years, the method has been extended to the pathological investigation. Stable isotope analysis to better understand a diet‐related disease: celiac disease in ancient human bones was carried out. To do this, we analyzed the nitrogen and carbon isotopic composition of human (n = 37) and faunal (n = 8) bone remains from the archaeological site of Cosa at Ansedonia, on the Tyrrhenian coast near Orbetello (Tuscany), including the skeletal remains of a young woman (late 1st century–early 2nd century Common Era [CE]) with morphological and genetic features suggestive of celiac disease. We compared the young woman's isotopic data with those of other individuals recovered at the same site but from two later time periods (6th century CE; 11–12th century CE) and with literature data from other Italian archaeological sites dating to the same period. Her collagen δ¹³C and δ¹⁵N values differed from those of the samples at the same site, and from most but not all of the contemporary sites. Although the woman's diet appears distinct, chronic malnutrition resulting from severe malabsorption of essential nutrients due to celiac disease may have affected the isotopic composition of her bone collagen. Am J Phys Anthropol 154:349–356, 2014. © 2014 Wiley Periodicals, Inc.     

Pleistocene Plant Fossils in and near La Selva Biological Station, Costa Rica1

Radiocarbon dating and ⁴⁰Ar/³⁹Ar analysis of overlying tephra indicate that plant fossil assemblages exposed by stream erosion and well construction in and near La Selva Biological Station in eastern lowland Costa Rica are Pleistocene in age. We identified plant taxa based on wood, leaves, fruits, seeds, pollen, and spores examined from three sites at ca 30 m elevation. Extrapolating from modern ranges and surface temperature lapse rates suggests paleotemperatures 2.5–3.1°C cooler than at present     

Detection of the impact of early Holocene hunter-gatherers on vegetation in the Czech Republic, using multivariate analysis of pollen data

Pollen data from the Czech Republic was used to detect the early Holocene impact of hunter-gatherers on vegetation based on a selection of 19 early Holocene pollen profiles, complemented with archaeological information regarding the intensity of local and regional Mesolithic human habitation. Archaeological evidence was assigned to simple categories reflecting the intensity of habitation and distance from pollen sites. Multivariate methods (PCA and RDA) were used to determine relationships between sites and possible anthropogenic pollen indicators and to test how these indicators relate to the archaeological evidence. In several profiles the pollen signal was influenced by local Mesolithic settlement. Specific pollen types (e.g. Calluna vulgaris, Plantago lanceolata, Solanum and Pteridium aquilinum) were found to be significantly correlated with human activity. The role of settlement proximity to the investigation site, the statistical significance of pollen indicators of human activity, as well as the early occurrence of Corylus avellana and its possible anthropogenic dispersal, are discussed.     

Stable isotope evidence for late medieval (14th-15th C) origins of the eastern Baltic cod (Gadus morhua) fishery

Although recent historical ecology studies have extended quantitative knowledge of eastern Baltic cod (Gadus morhua) exploitation back as far as the 16th century, the historical origin of the modern fishery remains obscure. Widespread archaeological evidence for cod consumption around the eastern Baltic littoral emerges around the 13th century, three centuries before systematic documentation, but it is not clear whether this represents (1) development of a substantial eastern Baltic cod fishery, or (2) large-scale importation of preserved cod from elsewhere. To distinguish between these hypotheses we use stable carbon and nitrogen isotope analysis to determine likely catch regions of 74 cod vertebrae and cleithra from 19 Baltic archaeological sites dated from the 8th to the 16th centuries. δ¹³C and δ¹⁵N signatures for six possible catch regions were established using a larger sample of archaeological cod cranial bones (n = 249). The data strongly support the second hypothesis, revealing widespread importation of cod during the 13th to 14th centuries, most of it probably from Arctic Norway. By the 15th century, however, eastern Baltic cod dominate within our sample, indicating the development of a substantial late medieval fishery. Potential human impact on cod stocks in the eastern Baltic must thus be taken into account for at least the last 600 years.     

Pollen from archaeological layers and cultural landscape reconstruction: Case studies from the Bradano valley (Basilicata,southern Italy)

Abstract

The article aims at presenting some aspects of environmental reconstruction through pollen analysis from archaeological contexts. The anthropogenic pollen transport into archaeological sites is regarded as an interesting tool to improve knowledge on flora and vegetation in the area of influence of sites. The zoophilous plants can be found more easily than in the regional airborne pollen rain where anemophilous pollen is generally overrepresented. Moreover, pollen from archaeological contexts is mainly a result of the cultural landscape shaped by human activities. Two case studies from the Bradano Valley (Basilicata, southern Italy), rich in archaeological sites dating altogether from the Middle Bronze Age to the Medieval age, are reported. Difesa San Biagio and its surroundings is one of the biggest settlements of the area, settled in early times by Enotrians. Altojanni is an extended area mainly frequented in Hellenistic, Roman late Imperial and Medieval times. A very open landscape, and clear signs of plant exploitation and cultivation, breeding and settlements were present in the two sites. Though samples are disturbed and preservation problems are sometimes observed, the main characters of pollen spectra are recurrent. High percentages of Poaceae and Cichorioideae, together with coprophilous fungal spores, strongly suggest a long tradition of pastoral activities. These case study examples suggest that human activities would have produced a fairly xeric environment.     

Moisture record of the Upper Volga catchment between AD 1430 and 1600 supported by a δ13C tree-ring chronology of archaeological pine timbers

Investigations of interactions between climate change and humans suffer from the lack of climate proxies directly linked to historical or archaeological datasets that describe past environmental conditions at a particular location and time. We present a new set of pine tree-ring records (Pinus sylvestris L.) developed from burial timbers excavated at the historical center of Yaroslavl city, Russia. A 171-year δ¹³C tree-ring chronology from AD 1430 to AD 1600 evidences mostly wet summers during the 15th century but exceptionally dry conditions of the 16th century at the Upper Volga catchment. According to the tree-ring record there were four major droughts (<−1.5σ) lasting from 9 to 26 years: 1501–1517, 1524–1533, 1542–1555 and 1570–1596, and major pluvials (>+1.5σ) lasting from 70 to 5 years: 1430–1500, 1518–1523, 1534–1541, and 1556–1564. We discuss a plausible contribution of these droughts to crop failures and city fires documented with historical chronicles for the Upper Volga catchment. The devastating drought regime of the 16th century corresponds to the loss of independence of the Yaroslavl principality to the Grand Duchy of Moscow and the formation of the centralized Russian State during the reign of Ivan the Terrible (1533–1584) underpinning the emergence of the Russian Empire. This study substantiates the value of archaeological timbers from the oldest Russian cities and inclusion of stable carbon isotope analysis for understanding hydroclimatic regimes across the mid latitudes of East European Plain, and their relationship to the history of Russia.     

Abandonment of farmland and vegetation succession following the Eurasian plague pandemic of ad 1347–52

Aim This paper reviews the available documentary, archaeological and palaeoecological evidence for the abandonment of agricultural land and consequent regeneration of the forest in Europe after the Black Death. Location Western and northern Europe. Methods This review is the result of an exhaustive search of the historical, archaeological and palaeoecological literature for evidence indicating agricultural decline and forest regeneration in Eurasia during the 14th century. The available evidence for landscape change can be divided into two categories: (1) documentary and archaeological sources, and (2) palaeoecological reconstructions of past vegetation. In the past few years, several pollen diagrams from north‐west Europe have been reported with precise chronologies (decadal and even annual scale) showing the abandonment of farmland and consequent ecological change in the late medieval period. Results and main conclusions There is strong evidence of agricultural continuity at several sites in Western Europe at the time of the Black Death. The effects of the Black Death on the European rural landscape varied geographically, with major factors probably including the impact of the plague on the local population, and soil quality. At two sites in western and northern Ireland, the late medieval decline in cereal agriculture was probably a direct result of population reduction following the Black Death. In contrast, the decline in cereal production began at sites in Britain and France before the Black Death pandemic of ad 1347–52, and was probably due to the crisis in the agricultural economy, exacerbated by political instability and climate deterioration. Much of the abandoned arable land was probably exploited for grazing during the period between the decline in cereal farming and the Black Death. In the aftermath of the Black Death, grazing pressure was greatly reduced owing to reductions in the grazing animal population and a shortage of farmers. Vegetation succession on the abandoned grazing land resulted in increased cover of woody tree species, particularly Betula and Corylus, by the late 14th century. The cover of woodland was greatest at c.ad 1400, before forest clearance and agriculture increased in intensity.     

The impact of mining on the woody vegetation of the southern Andes: a study of charcoal from the Andean Precordillera in central western Argentina in the 18th and 19th centuries

Mining has played an important role in the generation of economic wealth since colonial times in South America. However, the impact of historical mining on the environment has not been studied in detail. In view of this, and based on the analysis of archaeological and modern wood data, we discuss the impact of historical mining and human occupation on the woody vegetation of an arid region in the southern Andes. We present the results of the analysis of archaeobotanical charcoal remains recovered from the “Los Hornillos” mining site located in the Andean Precordillera, northwestern Mendoza Province, Argentina. The archaeobotanical materials date from the late 18th to the early 19th century. Based upon wood anatomy, 60% of charcoal fragments were associated with Adesmia cf. uspallatensis, a shrub widely distributed there. We assessed the impact and legacy of human occupation on local and regional plant communities based on charcoal evidence, archaeological data and the age of living A. uspallatensis shrubs growing around the mining site. This analysis allowed us to determine the rate of growth of this species (1.22 mm per year) and mean maximum ages of around 70 years. Therefore, the current development of woody communities in this area is thought to be representative of recovery after historical mining and occupation across the Andean Precordillera and suggests that obtaining firewood for mining activities constituted an important factor influencing past natural vegetation dynamics.

     

The effects of the Taupo Tephra eruption of c. 1718 bp on the vegetation of Mt Hauhungatahi, central North Island, New Zealand

Abstract. An altitudinal series of eleven fine resolution pollen diagrams were used to examine the role of volcanism in forest dynamics on Mt Hauhungatahi. Partial pollen diagrams from four of these sites, chosen to illustrate the major effects of the 1718 bp Taupo eruption, are presented. Following the eruption Libocedrus bidwillii expanded in all sites. Open sites created by the eruption may have facilitated an expansion already underway as a result of more variable climatic conditions since c. 3000 bp . Weinmannia racemosa invaded upper montane forest c. 650 bp . The current altitudinal sequence of forest types, with Libocedrus dominating the subalpine and Weinmannia the upper montane forests, has thus been synthesized only within the last 1800 years. This is interpreted as a consequence of individualistic species' responses to major disturbance by the eruption. The results support nonequilibrium theories of community composition.     

Human activity and climate change during the historical period in central upland Japan with reference to forest dynamics and the cultivation of Japanese horse chestnut (<Emphasis Type="Italic">Aesculus turbinata</Emphasis>)

Karikomi Lake is located in the border area between the Hida and Echizen regions (36° 04N, 135° 44E) at 1075 m a.s.l., in the Hakusan mountains. Several villages are located near the lake where hansaibai was practised in the past, i.e. horse-chestnut trees (Aesculus turbinata) were favoured for their nuts which were gathered and processed as an important food source. To understand how the forest was used for this purpose, a core was taken from Karikomi Lake and the past vegetation was reconstructed through pollen analysis of the lake sediment. Climate deterioration caused by the Little Ice Age impinged severely on the local population and seems to have played a key role in the development of hansaibai and reliance on horse chestnut as a major food source. The pollen analytical data suggest that hansaibai was associated with increased frequency of famine periods during the Little Ice Age in Japan, although human impact in the vicinity of the lake began much earlier, in the 8^th century A.D. Deforestation and economic development during the twentieth century have led to abandonment of the use of horse chestnut as a major food source and the replacement of Aesculus by Fagus in the local forest which lies within lands designated as a National Park.     

Farm development at the Arctic cereal limit in northern Norway—continuity and discontinuities

The vegetational development of two neighbouring farm sites at the Arctic cereal limit was investigated by pollen analysis and ¹⁴C-dates. One farm was small and one larger and both had a long habitation history according to archaeological data. Temporary cereal growing at the minor farm may have been introduced about 3100 cal b.p. and was discontinued before 2550 cal b.p. From 1700–1600 cal b.p. Hordeum was cultivated at both farms. At the larger farm there was continuous settlement from c. 2250 cal b.p., but no evidence of cereal growing during the first c. 600 years after the establishment of the farm. It is suggested that changes in the natural conditions, especially paludification, caused a low-activity/abandonment phase at the smaller farm from c. 2550 to c. 1700 cal b.p. A regional abandonment period about 1250 cal b.p. (in the 7th century a.d.) affected the smaller farm in particular.     

Dendrochronological analysis and dating of wooden artefacts from the prehistoric copper mine Kelchalm/Kitzbühel (Austria)

The potential of dendrochronological analysis of wood found in prehistoric and historic mining areas in Tyrol has remained unattended for a long time. For the first time, systematically analysed wooden artefacts from a prehistoric mining area in Tyrol (Kelchalm near Kitzbühel) can be presented here.The investigated artefacts, related to mining and everyday life, were found in the course of archaeological excavations, which were carried out between 1932 and 1953 by Richard Pittioni and Ernst Preuschen. Taking an adequate number of tree rings and well-preserved wood wane into account, 21 pieces of mining timber were pre-selected for a dendrochronological analysis. The identified wood species are spruce (Picea abies, n=18) and fir (Abies alba, n=3). The length of the established tree-ring series ranges from 13 to 145. We cross-dated the tree-ring series of seven wooden artefacts among each other, which resulted in a spruce-fir tree-ring record of 153 values (Kelchalm mean curve). The last tree ring measured of the Kelchalm spruce-fir mean curve dates back to 1237 BC. This accurate dendro-result dates the Bronze Age mining activities at the Kelchalm to about two centuries earlier than the long-lasting assumption proposed by Richard Pittioni. His assumption was based on the typology of ceramic and metal artefacts.The established dendro-date for the Bronze Age mine at the Kelchalm matches with available ¹⁴C results from other important copper-mining areas in the north-eastern Alps (NE Alps). The activities at these other sites are dated between the 17th and 6th century BC. Furthermore, the radiocarbon dating, as well as the dendro-result from the Kelchalm, suggests a transition from earlier mined copper-ore deposits in the eastern areas of the NE Alps, to the later mined ore deposits in the western section. This has led to both parallel and sequential mining activities in several ore districts during the last two millennia BC in the NE Alps.     

Characterization of wood components of Portuguese medieval dugout canoes with high-resolution solid-state NMR

High-resolution nuclear magnetic resonance of carbon 13 was employed to characterize archaeological wood samples from Portuguese medieval dugout canoes. Structural and chemical modifications were assessed by comparing the structural features of archaeological wood samples with modern wood. The main results concern the strong decrease of sugar moiety with a complete disappearance of hemicelluloses. During ageing in water environment, the β-O-4 inter-unit linkages of lignins have not been degraded. The features of the ¹³C NMR spectra clearly reveal that the products of degradation of the carbohydrates occurring during depletion of sugars were not recombined inside the lignocellulosic matrix. Finally, this article gives a clear illustration that although the water contents of archaeological wood can certainly be used as a good criterion concerning their state of degradation, solid-state ¹³C NMR lead to unambiguously data as far the structural properties of archaeological waterlogged woods are concerned.     

Vegetation change during the Bronze Age studied in a multi-proxy approach: use of wood linked to charcoal analysis

During recent archaeological excavations in the alpine valley of Montafon, western Austria, a Bronze and early Iron Age settlement cluster located at about 1,000 m a.s.l. was excavated. The human impact on the woodland resulting from these prehistoric settlement activities has been evaluated by the analysis of charred plant macro remains from cultural layers from a hilltop settlement site and two other close-by settlements, all of them encompassing the Early and Middle Bronze Age (19th to 15th century cal. b.c.) and early Iron Age (6th/5th century cal. b.c.). Charred seeds and fruits have provided information on the supply of foodstuff while charcoal (anthracological) analyses of firewood have revealed the use of wood and consequently the changes in local woods. The latter analyses suggest that the spruce-fir woodland (Piceeto-Abietetum) was gradually cleared from the Early Bronze Age. During the Middle Bronze Age large amounts of Pinus sylvestris (pine), Betula (birch), Corylus avellana (hazel) and Sorbus (rowan) with some Picea abies (spruce) characterized the woods, and early succession stages indicate clearings. These anthracological studies are corroborated by pollen studies disclosing clearings in the woods since the Early Bronze Age, which gradually expanded during the Middle Bronze Age. Furthermore, several charcoals from a Middle Bronze Age hearth seem to be of the same age, and the pattern of their annual growth-rings suggests the pollarding of broadleaved trees.     

Reconstruction of the vegetation at A.D. 915 at Ohse-yachi Mire, northern Japan, from pollen, present-day vegetation and tephra data

The Towada-a (To-a) Tephra from A.D. 915 allowed reconstruction of the local and regional vegetation at and near Ohse-yachi Mire from pollen samples taken just below the tephra. In earlier studies the tephra was dated from ¹⁴C data, stratigraphy at archaeological sites and a historical record. Twelve cores along two perpendicular transects yielded pollen from modern and pre-tephra samples. The modern pollen data were compared with the modern vegetation, and used to interpret the pollen data from A.D. 915. Ericaceae, Drosera, Sanguisorba, other Rosaceae, and Sphagnum were concluded to be local elements. Ohse-yachi Mire was a wet Sphagnum bog in A.D. 915, with Sphagnum dominating the central part of the mire. The present stand of scrub was not yet established, but there was a stand of Pinus pumila scrub. The bog subsequently became drier and changed to the present-day mixed Moliniopsis-Sphagnum bog.     

The ancient minoans of crete: A biodistance study

The study of cranial material is an important source of information for biological reconstruction of past human populations. Such cranial data used for solving prehistoric problems (Buikstra et al, 1990). Cranial samples from the prehistoric population of Crete were studied to try to answer an archaeological problem (the hypothesis of the Mycenean invasion in the island during Late Bronze Age period). Historical and archaeological evidence suggests that Myceneans invaded Crete after the destroy caused by the eruption of the Thera Volcano (15^th century b.C.). The samples were analysed by Discriminant Analysis, and classification factor was the Era. It is concluded that: a) It is not abvious an entry of another population during the transitional period between NL/MM, because there is a common morphometric pattern, and b) the entrance and installation of the Myceneans during the Late Minoan period is possible because a different morphometric pattern was found. This last conclusion is in accordance with the archaeological evidence.     

A palynological study of the Acheulian site of Gesher Benot Ya’aqov, Israel

The results are discussed of the palynological (pollen-analytical) examination of a sediment section in the Hula Valley of northern Israel, with evidence of Acheulian occupation dated to 700,000–800,000 b.p. In general there is a fair agreement between the palynological data and the wood remains identified from the site, but there are also discrepancies, some of which can be explained and others not. Although relatively well represented in the pollen record, Pinus (pine) most probably did not occur in the Hula area. Some pollen types are thought to have been carried in from hundreds of kilometres away (long-distance transport). Together the pollen and wood evidence suggests that Quercus ithaburensis–Pistacia atlantica (Tabor oak–Atlantic terebinth) woodland (open forest) was found in the Hula Valley (other than the lake and marshes) and on the lower reaches of the mountains flanking the valley on both sides. In addition to deciduous Tabor oak, evergreen Kermes oak (Quercus calliprinos) must have been an important component of this woodland. Wild olive (Olea europaea var. oleaster) may also have been quite common here. The suggestion of open forest, with fairly widely spaced trees, is based upon the high non-arboreal pollen frequencies and indicates fairly dry climatic conditions. Various stream-bank trees and shrubs are represented in the pollen and/or wood records, such as Fraxinus (ash), Ulmus (elm), Salix (willow) and Platanus (plane tree). During the period represented by the upper section of the pollen diagram, Cedrus (cedar) must have reached the Hula area, indicating increased humidity. In the steppe-like field layer (undergrowth of the woodland) grasses (Gramineae) must have played a prominent role in addition to a great number of other species. In particular Compositae and Umbelliferae include a large variety of species (many different pollen types). Two Chenopodiaceae maxima, coinciding with Gramineae minima, are thought to be indicative of periods of increased climatic dryness. The local lake and marsh vegetation is fairly well represented in the pollen record, but interpretation in terms of vegetation succession is only possible to some degree. Mention is made here of Trapa natans (water chestnut), the nuts of which were consumed by the Acheulian inhabitants. Sytze Bottema: Deceased in 2005.