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For over 120 years, the shell middens of western Scotland and the series of open-air sites on Oronsay have been the focus of debate in European Mesolithic studies. This paper challenges the significance of Oronsay in light of results from the geophysical survey and test-excavation of a new limpet and periwinkle shell midden dated to the late 5th or start of the 4th millennium calbcat Port Lobh, Colonsay that offers fresh evidence to re-evaluate critically the role of Oronsay and coastal resources in island settlement models ahead of the Mesolithic–Neolithic transition. Test excavations recovered a marine molluscan assemblage dominated by limpet and periwinkle shells together with crab, sea urchin, a fishbone assemblage composed mainly of Gadidae, some identifiable bird and mammal bone, carbonised macroplant remains, and pumice as well as a bipolar lithic assemblage and coarse stone implements. Novel seasonality studies of saithe otolith thin-sections suggest wintertime tidal fishing practices. At least two activity events may be discerned, dating from the late 5th millennium calbc. The midden could represent a small number of rapidly deposited assemblages or maybe the result of stocastic events within a more extended timeframe. We argue that alternative research questions are needed to advance long-standing debates about seasonal inter-island mobility versus island sedentism that look beyond Oronsay to better understand later Mesolithic occupation patterns and the formation and date of Oronsay middens. We propose alternative methodological strategies to aid identification of contemporaneous sites using geophysical techniques and lithic technological signatures.

An open-access database has been set up to support the research project study- ing the ‘Response of Humans to Abrupt Environmental Transitions’ (RESET). The main methodology underlying this project was to use tephra layers to tie together and synchronise the chronologies of stratigraphic records at archaeological and envi- ronmental sites. The database has information on occurrences, and chemical compo- sitions, of glass shards from tephra and cryptotephra deposits found across Europe. The data includes both information from the RESET project itself and from the published literature. With over 12,000 major element analyses and over 3000 trace element analyses on glass shards, relevant to 80 late Quaternary eruptions, the RESET project has generated an important archive of data. When added to the published information, the database described here has a total of more than 22,000 major element analyses and nearly 4000 trace element analyses on glass from over 240 eruptions. In addition to the database and its associated data, new methods of data analysis for assessing correlations have been developed as part of the project. In particular an approach using multi-dimensional kernel density estimates to evaluate the likelihood of tephra compositions matching is described here and tested on data generated as part of the RESET project.

The discovery of a cryptotephra (nonvisible volcanic horizon) in a windblown sand archaeological site in Poland highlights how luminescence and tephrostratigraphy may combine to better refine the chronology of such sites. In this study we identify a cryptotephra horizon which on the basis of major and minor element geochemistry and an OSL age of 2.3 ± 0.1 ka is correlated to the Glen Garry tephra. The different methodological strengths of OSL and tephrostratigraphy may be harnessed to counter the limitations of a single approach to produce a more secure chronology. Although in this study the tephra deposition event is shown to post-date the archaeological activity, the methodological approach is clearly demonstrated. Further investigations will reveal if cryptotephra layers are commonly preserved in such environmental settings. If this is so then future applications of this approach may prove to be more widely applicable.

This paper presents the first late Quaternary locality in the present-day territories of Poland where multiple cryptotephra layers have been identified. Located near Wegliny in southwest Poland, study of the Lateglacial gyttja deposits reveals the presence of at least four non-visible tephra horizons. Electron microprobe and laser-ablation ICPMS analysis of glass shards suggests products from at least two Icelandic volcanic centres: Katla and Snaesfellsness. Of particular importance is the discovery of two eruptions believed to originate from the east Eifel volcanic field within the Allerod chronozone. One correlates with the well documented Laacher See Tephra (LST) but the second horizon, herein designated T642/T655 would appear to represent an earlier precursor eruption. The chemical composition of the LST and the precursor tephra both appear to match to the Upper Laacher See Tephra (ULST) phase, which previously was thought to have dispersed not to the northeast but in a southerly direction, towards the Alpine foreland. This indicates the eruption dynamics of the Laacher See are more complex than hitherto recognised.

Peat is notoriously difficult to radiocarbon date as it is composed of a heterogeneous mix of organic materials of different radiocarbon ages and at different stages of humification. Different chemical fractions (most frequently humin and humic acid) have been observed to yield significantly different radiocarbon ages from some peat deposits. Here we present humin and humic acid dates on a range of grain-size fractions of peat from the open-air archaeological site of Ahrenshoft LA 58 D, northern Germany, which were measured to confirm the identity of the source of cryptotephra found at the site. Both the humin and humic acid ages increased with increasing grain size, and for all but one sample the humic acid fraction was younger than the corresponding humin date. When calibrated the 6 dates from the horizon containing the cryptotephra spanned a time period of up to 1500 years, and are insufficiently conclusive to definitively resolve which eruption is responsible for the observed ash horizon.

Changing river courses and fluctuations of the water table were some of the most fundamental environmental changes that humans faced during the Late Glacial, particularly as these changes affected areas intensively used for settlement and resource exploitation. Unfortunately, only a few stratigraphies have been documented in the North European plain that show the interaction between river development, vegetation history, and occupation by Late Palaeolithic humans. Here, we present the results of detailed stratigraphical studies (pedology, archaeology, chrono-, tephra-, and palynostratigraphy) at the Federmesser site Grabow 15 located in the broad Elbe River valley. The research aimed to produce a model of site formation based on a multiproxy approach, relating the local evidence to the palaeoenvironmental and settlement history of the wider region. After deposition of fluvial sands during the Late Pleniglacial in a braided setting, the river course developed locally toward a meandering system at the transition from the Older Dryas to the Allerod, while periodic flooding led to the deposition of floodplain sediments during the early Allerod. The floodplain was settled by people of the earliest “Federmessergruppen,” who are believed to have chosen this open floodplain area along the river for collecting and processing amber of local origin. Their artifacts became embedded in the aggrading floodplain sediments. In the late Allerod, floodplain sedimentation ceased and a Fluvisol-type soil developed, indicating a trend toward geomorphic stability. The Fluvisol was then covered by silty floodplain sediments due to a rising water level during the late Younger Dryas resulting in the cessation of human occupation in the area. Subsequent organic-rich Late Glacial/Holocene sediments preserved the settlement remains to the present.

Surveys and excavations in 1980–1 confirmed Peak Camp as a Neolithic enclosure on a flat promontory of the Cotswold escarpment overlooking the Severn Valley just 1 km south of Crickley Hill. Although heavily eroded by quarrying the site can be reconstructed as having two concentric arcs of boundary earthworks forming an oval plan which was probably open to the north where a steep natural slope defined the edge of the site. A section through the outer boundary showed four main phases of ditch construction, at least one causewayed. An extensive series of radiocarbon dates shows construction began in the late 37th century calbcand probably continued through successive remodellings into the 33rd century calbcor beyond. An internal ditch or elongated pit situated in the area between the inner and outer boundary earthworks had a similar history. Where sampled, the ditch and internal feature were rich in material culture, including a substantial assemblage of plain bowl pottery; flint implements and working waste; animal remains dominated by cattle but including also the remains of a cat; human foot bones; slight traces of cereal production; a fragment of a Group VI axe; part of a sandstone disc; and a highly unusual shale arc pendant of continental type. It is suggested that the ditch fills represent selectively redeposited midden material from within the site that started to accumulate in the late 5th or early 4th millennium calbc. The construction and use of Peak Camp is contemporary with activity on Crickley Hill, and the two sites probably formed components of a single complex. Its use was also contemporary with the deposition of burials at local long barrows in the Cotswold-Severn tradition which are linked by common ceramic traditions and the selective deposition of human body parts.

This paper focuses on the chronology and environmental significance of a sediment sequence from an alluvial locality in the vicinity of the historic site of Dunadd, Scotland. It outlines the rationale and statistical validity of an age model derived for a sequence of floodplain sediments from which detailed pollen-stratigraphical and plant macrofossil records have been derived. A series of radiocarbon dates are calibrated using a Bayesian modelling approach, the results of which can be refined by incorporating two independent age estimates based on tephra layers of known age. Analysis of the entire floodplain sequence for volcanic glass shards revealed the presence of discrete but geochemically very similar tephra layers within the upper (late Holocene) part of the sequence. Comparison with published geochemical data obtained from Icelandic tephras of historical age indicates strong statistical correlations with the Hekla 1947 AD and Hekla 1510 AD. While the Hekla 1510 AD tephra has previously been reported from sites within Britain and Ireland, the Dunadd sequence affords the first record of the Hekla 1947 AD tephra layer within Scotland. When the ages and stratigraphic positions of both tephra layers are incorporated into the Bayesian age model, an overall centennial to decadal precision for the late Holocene is achieved, with archaeological and environmental transitions discriminated with highest-likelihood age uncertainty ranges of 20-50 years at 95% confidence. The local environmental record is assessed in the light of this new chronological framework: the data support previously reported proposals for two periods of significant climatic deterioration with increased wetness, the first during the early Medieval period and the second during the late 16th and 17th centuries AD. (C) 2009 Elsevier Ltd. All rights reserved.

In 1986 remains of an adult woolly mammoth, Mammuthus primigenius (Blumenbach), were discovered at Norton Farm Pit, Condover, south of Shrewsbury, UK. Preliminary stratigraphical investigations indicated that this individual dated to the Devensian Late-glacial Interstadial, then the first evidence for survival of mammoth in Britain following the Last Glacial Maximum. Initial radiocarbon analysis confirmed this interpretation. Subsequent excavations in 1987/1988 recovered the remains of a further three juvenile mammoth individuals. All of these remains were found in the spoil heaps of overburden (ex situ) and their true stratigraphical context had to be reconstructed from the remnants surviving in the Pit. The 1987/1988 excavations enabled stratigraphical investigation of the site and submission of samples for radiocarbon (14C) dating, including the use of ultrafiltration pretreatment for bone samples, with the aims of reconstructing the geological and palaeoenvironmental evolution of the site and the sedimentary context of the unstratified mammoth remains. These results are presented here. This investigation indicates that the woolly mammoth remains at Condover derive from a dead-ice landscape dominated by eskers, kames and kettle-hole basins, and that the sedimentary sequence in which the mammoth remains were found forms the infilling of a kettle-hole basin. The sedimentary infilling and formation of the kettle-hole basin through ice block melt-induced subsidence were syngenetic. 14C determinations indicate that basin infill was initiated prior to Greenland Interstadial 1, and probably in Greenland Stadial 2 i.e. before 14.7 ka BP and that it continued until the early Holocene, around 8 ka BP. The sedimentological and 14C data indicate that the unstratified mammoth remains can be attributed to a dark grey clayey sandy silt (Unit C1), which accumulated during the earlier part of Greenland Interstadial 1 (14 to 14.5 ka BP) within an actively subsiding slow-flowing, beaded, fluvial network characterized by channels and pools/lakes, and with relatively shallow marginal slopes. The sedimentary architecture indicates survival of the buried ice block into Greenland Interstadial 1 and final melting only towards the end of the Interstadial at ca. 12.65 ka BP. Copyright © 2009 John Wiley & Sons, Ltd.

Optically stimulated luminescence (OSL) dating of sand has been used to identify periods of enhanced aeolian activity at two coastal archaeological sites in Orkney that coincide with periods of Holocene climatic deterioration recorded elsewhere in both Scotland and W Europe. Areas of Tofts Ness, Sanday were settled from the Neolithic, abandoned in the late Neolithic/early Bronze Age, reoccupied and permanently abandoned in the Iron Age. Sand layers above the Neolithic soils have been OSL dated to about 4000 BP, correlating well with a period of increased aeolian activity elsewhere in W Europe. OSL dating of aeolian sands above midden deposits and a Bronze Age burial at Lopness on Sanday suggest dune development by 3000 BP, although both sites also contain sand that was deposited during the `Little Ice Age'. Several possible mechanisms may have contributed to an increase in aeolian activity during the Holocene that led to the abandonment of these sites. Although volcanic eruptions in Iceland cannot be discounted as a contributory factor, a more likely driver of change in sand dune systems is the enhanced N Atlantic storminess suggested by ice core records from Greenland. During periods of climatic deterioration the declining productivity of other agricultural land places enhanced demands on agriculturally marginal sand dunes, leading to further destabilization and the potential for enhanced sand transport events.

In contrast to the widely reported research into the wetland prehistory of the Somerset Moors and Levels, the wetland archaeology for the historic periods of this region of south west England has always been less well known, being reliant on mostly non-wetland sources of information, e.g. documentary evidence, cartographic studies and inferences made from dry land archaeological sites. This study attempts to correct this imbalance by outlining palynological and radiocarbon evidence obtained in the last fifteen years from Godney Moor that suggests that palaeoenvironmental evidence may survive in at least certain parts of the region. Furthermore, data from an earlier study made in the 1940–50s are highlighted that would indicate more palaeoenvironmental information can be discerned for the Post-Roman period in previous studies if these findings are re-examined in the light of recent advances in knowledge.

A luminescence-based approach to the rapid characterisation of sites in terms of their datability and sedimentary history is described (luminescence profiling), and contrasting results presented for three Palaeolithic archaeological sites in Russia. Three mineral/grain-size fractions (polymineral silt-sized, polymineral sand-sized, quartz-enriched sand-sized) were separated from each of many small samples taken through the sites’ stratigraphies. Luminescence signals from the different fractions were measured using infra-red light, blue light, and thermal stimulation. Patterns in luminescence sensitivity and equivalent dose values are used to indicate which sites, samples, fractions and/or signals may yield meaningful luminescence ages, and the experimental effort that may be required to obtain said ages. Case studies range from a site where a detailed chronostratigraphy might be produced using a limited number of full luminescence dates to tie in the profiling results, to a site where profiling indicates there is little chance of producing useful luminescence dates. These interpretations are based on dialogue between the luminescence profiling results and archaeological, palaeoenvironmental, and geomorphological evidence. Luminescence profiling is shown to be a useful tool for understanding sedimentological process at each site, independent of full luminescence dating.

Coring in the Lagoon of Venice mudflats along previously collected high-resolution subbottom seismic-reflection survey profile lines has enabled the collection of interlayered radiocarbon-datable terrestrial plant material. Along present and former meander bends, dipping laminated sandy channel-bank deposits rest in sharp lithostratigraphic and chronologic contrast to the adjacent and overlying mudflat deposits. Horizontal channel migration rates of roughly 10 to 20 meters per century are orders of magnitude faster than the minimum estimates of vertical mudflat silt accumulation, which range from 5 to 25 centimeters per century. Given the nearly 6000-year history since the late-Holocene marine transgression that produced the initial lagoon environments of deposition, it is no surprise that channel meander migration has left a prevalence of channel-bank deposits in the subsurface lithostratigraphy. Furthermore, regional subsidence and rising relative sea level continue to enhance the net accumulat...

It is well known that Venice has always had an intimate association with the sea. Despite the historical interest the origins of the city have, until relatively recently, remained cloaked in obscurity. Until the mid-1980s Venice remained one of the few major historical cities in Europe where urban archaeology had yet to uncover significant information. Over the last two decades the situation has changed as shown by fifteen sites with early levels. Despite the difficulties of working in a tidal lagoon at considerable depths, archaeology has begun to chart the earliest inhabitation. This paper outlines some of the findings and the methodological approach adopted.

Climate changes over the Holocene have directly impacted on both coastal processes and human use of coastal areas. This paper presents results from the dating of wind blown sand deposits collected from coastal and archaeological sites in Northern Scotland. Archaeological remains are frequently found interspersed with sand deposits and represent distinct periods of occupation of settlement sites within the local landscapes. In some cases storm events sufficiently inundate the sites with sand to result in periodic abandonment. Storm events can also have dramatic results on adjacent rock coastlines, with storm boulder ridges emplaced by large waves, burying sand deposits on cliff-top sites. Work has been undertaken using a quartz SAR protocol to date sand deposition at two archaeological sites in Orkney and a cliff-top site in Shetland. These dates provide chronological information, which help to construct regional chronologies of climatic instability and environmental change and allow the SAR-OSL method to be assessed as an accurate sediment dating tool in this context.

Luminescence dating of aeolian sands from archaeological sites has potential to contribute to regional chronologies for sediment deposition and to provide a greater understanding of climatic influences on early communities. The Northern and Western Isles of Scotland provide important opportunities for sampling archaeologically intercalated sands for these purposes, and to provide constrained samples for method validation. A wide range of modern beaches have been sampled in the Western and Orkney Isles of Scotland to examine regional variations in luminescence sensitivity, residuals and ease of bleaching. These modern sands have negligible residuals for infra-red stimulated luminescence (IRSL), small optically stimulated luminescence (OSL) residuals and significant thermoluminescence residuals. The relationship between these signals and laboratory bleaching results may indicate the initial depositional environment, and hence lead to a means of identifying well-bleached dating samples. Both sensitivities and residuals show regional differences, reflecting local geology. Preliminary ages obtained from aeolian sands associated with archaeological sites at Amble (Northumbria) and Tofts Ness (Sanday, Orkney) using regenerative blue OSL techniques on extracted quartz are broadly consistent with external age controls from the first and third millennium BC.

Around 1600 burnt mounds, comprising heaps of fire cracked stones, up to several metres across with characteristic forms, are listed in the National Monuments Records of Scotland, with a diverse distribution. Many more are known in other parts of Europe, notably in Ireland and Scandinavia. Traditionally, these monuments are thought to relate to cooking activities throughout the Bronze Age though in recent years alternative functions have been suggested. Here results are presented from Lady Glassery Wood, a recently excavated site in the Kilmartin Valley. Samples for luminescence dating were collected in 1998, together with field gamma spectrometry measurements. Associated charcoal has also been subjected to radiocarbon dating. Despite and unusually low internal radioactivity from the rock samples examined, and low luminescence sensitivities from separated minerals, it has been possible to obtain concordant luminescence ages from both quartz and feldspars, giving a mean date of 2800±300 BC. Radiocarbon dating produces a 2 sigma calibrated age range of approximately 2800–2400 cal BC, in agreement with the luminescence age, indicating a late Neolithic date for the mound, one of a growing number of early dates in Scotland.

The term “Protoclassic,” employed regularly but inexplicitly in the literature of lowland Maya archaeology, has become increasingly nebulous and ambiguous in both meaning and usage. This paper reviews the history and use of the term and presents a formal redefinition of the Protoclassic as a ceramic stage based explicitly and exclusively on ceramic criteria. Some suggestions regarding future use of the term also are offered. The paper further addresses and resolves a number of persisting questions regarding Protoclassic orange wares, including problems concerning the actual existence of the “Aguacate ceramic group.” and the relationships of Aguacate-group pottery to other emergent orange wares of the terminal Late Preclassic and initial Early Classic periods. The nature and significance of the “Holmul I Style,” the “Floral Park Ceramic Sphere.” and the relationships of the two to each other and the larger, redefined “protoclassic” ceramic stage also are examined. A spatial distribution for protoclassic ceramics considerably expanded over what has ever been reported previously is described, and Chronometric data are presented to support a revised chronology for the protoclassic ceramic stage. Finally, ceramic data are offered that suggest a real subdivision of the protoclassic ceramic stage into an early, emergent facet originating entirely within Late Preclassic lowland traditions, and a later, fully “Classic” facet corresponding to the early Tzakol (Tzakol 1) ceramic horizon.

This paper examines, through the use of Accelerator Mass Spectrometry dating, the database of Lateglacial cultures involved in the recolonisation of northern Europe. The aim is not only to determine the timing of that recolonisation, but also to propose a general model of hunter-gatherer colonisation at a sub-continental scale. The question is addressed of how long the period of abandonment of northern Europe during the Würm/Weichsel glaciation may have lasted, and when it both started and came to an end. A series of questions is asked concerning the processes and mechanics of recolonisation and the sequences for specific areas are examined. AMS radiocarbon dating shows that a two stage process was involved, which has important implications for our analysis of regional settlement patterns and the changing scale of Lateglacial hunting systems. Recolonisation was a dynamic process, integral to, and internally driven by, the social life of Lateglacial hunters. It may have been constrained by environmental and resource factors, which we have emphasised here, but ultimately it was an historical, social process and should be similarily regarded to that of the farmers. By measuring rates of expansion data are provided for use in other studies of hunter-gatherer colonisation.

Renewed excavations in Kebara cave (Mt Carmel) made it possible to obtain a series of radiocarbon dates from the Upper Paleolithic layers of the site. The various readings indicate the presence of early Ahmarian industries around 43 –36 ka bp while the Levantine Aurignacian is dated to 36 –32 ka bp . Combined with the previously published TL dates for the uppermost Mousterian layers it is suggested that during the transition from the Middle to the Upper Paleolithic, the cave was abandoned and that this cultural phase should be dated to c . 46 /45 –43 /42 ka bp .

Presentation de la 21e liste de datations par radiocarbone realisees au laboratoire d'Oxford et concernant : des echantillons fauniques, floraux et environnementaux provenant de Grande-Bretagne, des restes humains provenant de Grande-Bretagne et de Belgique, de sites paleolithiques de Pologne, Moldavie, Russie et Ukraine, de sites mesolithiques de Grande-Bretagne, de Belgique, d'Allemagne et de Suede, de sites neolithiques et plus recents de Grande-Bretagne et d'Irlande, et de sites de Mediterannee orientale, d'Asie centrale et du sud-est, d'Egypte, d'Afrique sub-saharienne et d'Amerique du sud

Three years ago, ANTIQUITY reported a first archaeological insight into the origins of Venice. The city's historical records, famously good and full for its flourishing, say very little about the beginnings. This second report includes direct evidence from Piazza San Marco, the heart of the city.

Presentation des dates radiocarbone realisees par l'Universite d'Oxford depuis 1993. Elles couvrent le domaine europeen (Paleolithique, Neolithique et plus recent) et quelques sites oceaniens

Presentation de la 19e liste de datations par radiocarbone publiee par Archaeometry, contenant principalement le materiel date depuis le debut de l'annee 1993

Les fouilles realisees par Charles Mc Burney et John Clegg au debut des annees 60 dans le grotte de Coygan (Laugharne, Sud du Pays de Galles) revelaient une sequence d'occupation mousterienne, dont les principales decouvertes etaient des haches a bout coupe, stratifiees pres de la base de l'accumulmation d'une taniere de hyene. L'occupation humaine devrait etre comprise dans une periode d'environ 64-38000 BP selon les temoins stratigraphiques, favorisant une datation pour la periode la plus ancienne, avant 50000 BP. Quant a la taniere, elle a probablement ete occupee de 40000 BP au moins (voire 60000 BP) jusqu'a environ 24000 BP

Cryptotephra of Icelandic origin from the open-air archaeological site of Ahrenshoft LA 58 D (Kr. Nordfriesland, Schleswig-Holstein), northern Germany overlies a Late-glacial Havelte lithic assemblage, hitherto dated by 14 C and biostratigraphy to the earliest part of the Late-glacial interstadial (GI-1e to GI-1c 3 ). Peaks in ash shards are observed in two profiles. Major and minor element geochemistry indicates volcanic ash originating in the Katla system. Precise correlation to previously described tephra is uncertain due to overlapping chemical characteristics. The Ahrenshoft 14 C determinations, litho- and bio-stratigraphy encompass a broad age-span for the cryptotephra bearing sediments, from the end of the Allerod to the Preboreal. The most plausible volcanic eruption correlates are the Vedde Ash (∼Younger Dryas), already known from the European mainland, tephra AF555 (late Younger Dryas) and the Suduroy tephra (∼Preboreal/Boreal), hitherto recorded only in the North Atlantic region. These three ash horizons have been dated to, respectively, 12,171 ± 57 yr b2k in the NGRIP ice-core, c.11,500 cal BP, in Scotland and c.8000 cal BP, by radiocarbon from the Faroe Isles. Ongoing research on deposits from the type sites for the tephra layers may in the future differentiate these markers leading to better discrimination of the chemistries and a resolution of this question.

Presentation de la 18° liste de datations par radiocarbone concernant la faune du Pleistocene, l'habitat, le mobilier et l'environnement du Paleolithique europeen, oriental et africain, du Mesolithique anglais, du Neolithique et de l'âge des metaux anglais, portugais, africain, et de la prehistoire sud-americaine.

Four separate finds of human skeletal remains from the Norfolk Fens have been 14C-dated to the Early Bronze Age. It is suggested that they are a facet of the far more extensive deposition of bodies and artefacts in wet places.

Despite the city's long and illustrious history, little is known about the urban origins of Venice from the archaeological record. Recent excavations at the church of San Lorenzo have produced radiocarbon dates that give direct evidence for human occupation in the late 6th and 7th centuries AD, lending support to the tradition of settlement by refugees from the Lombard occupation of the mainland.

SORGHUM and millets are among the world's most important food crops and, for the inhabitants of the semi-arid tropics, they are the main sources of protein and energy. Little is known about the history of these crops; their domestication is thought to have occurred in the African savannah, but the date and precise location are unknown1,2. Excavations at an early Holocene archaeological site in southernmost Egypt, 100 km west of Abu Simbel, have yielded hundreds of carbonized seeds of sorghum and millets, with consistent radiocarbon dates of 8,000 years before present (BP), thus providing the earliest evidence for the use of these plants. They are morphologically wild, but the lipid fraction of the sorghum grains shows a closer relationship to domesticated than to wild varieties. Whatever their domestic status, the use of these plants 8,000 years ago suggests that the African plant-food complex developed independently of the Levantine wheat and barley complex.

The main problem with dating pottery by radiocarbon is that many different carbon sources, of different radiocarbon age, may contribute to the potsherd carbon content. Also, the process of firing is liable to destroy information that might help separate possible sources. We describe several pottery dating projects in which we have dated separate fractions (such as humics, lipids and classes of residual carbon). Although in some cases consistency between results is sufficient to accept that this approach can give a credible date, in other cases, no date has been possible, and general conclusions are difficult to make.

This paper discusses a number of concepts common to “transitions” in the Later Palaeolithic, whether change should be multifaceted in nature involving more than one cultural or technological attribute to be accepted as a defining point in time; the extent to which rate of change is important, be it gradual, accelerated, punctuated or uniform, and whether duration of change is relevant to the “transitions” debate. The case for refining chronologies is discussed. The paper concludes by drawing on the other papers in this section of the sourcebook to make some general methodological points.

We have made oxygen and carbon isotope measurements on limestone samples of Albian to Eocene age recovered from the Bottaccione Gorge section in the Umbrian Apennines, central Italy. Additional measurements have been made on topmost Maastrichtian and Palaeocene sediments from the adjacent Contessa Highway section. Our data from the Bottaccione Gorge show 13C maxima at the Cenomanian/Turonian boundary and during the Palaeocene, as well as a pronounced 13C minimum 7 metres above the clay layer at the K/T boundary. Our data from the Contessa Highway show a 13C minimum 9 metres above the K/T boundary clay. These minima are probably diagenetic artifacts. In the Bottaccione Gorge there is evidence for a hiatus in the early Middle Eocene. The Palaeocene of the Bottaccione Gorge appears to have been affected by slumping or faulting (in addition to the diagenetic overprinting) giving a spurious δ13C recovery after the K/T boundary, the Contessa Highway section appears to be more complete. The Coniacian-Maastrictian is characterized by relatively stable 13C values. Our data indicate an increase in δ18O (and therefore possible cooling) across the Cretaceous/Tertiary boundary in both the Bottaccione and Contessa Highway sections.

Andrews and Hammond (1990) recently presented a reevaluation of the Preclassic sequence at the early Maya site of Cuello in northern Belize and reported a substantial number of radiocarbon dates. These dates supported two mutually incompatible chronologies: (1) the "long" chronology advanced by Hammond et al. (1976, 1977, 1979), in which the Swasey phase spanned the second millennium B.C. in radiocarbon years and began as early as 2500 cal B.C. in calendar years; (2) a "short" chronology consistent with, or even more compressed than, the time scale based on ceramic comparisons and suggested by Coe (1980:34-35) and Marcus (1984), in which the Swasey phase would begin in the early first millennium cal B.C. (Figure 1). Andrews and Hammond noted that since both chronologies were supported by a number of dates from at least two laboratories, neither could be given preference on purely internal radiocarbon-dating criteria, nor could the discrepancy between the two suites be explained in terms of excavation, processing, or laboratory procedures; nor could arguments of residuality or intrusion be applied consistently, though some individual dates might be thus explained. Andrews and Hammond opted eventually for a version of the "short" chronology in which Swasey, and the Cuello sequence, began around the end of the second millennium cal B.C., largely on the basis of the much larger number of detailed ceramic sequences now available in southern Mesoamerica with which the Cuello typology could be compared. We report here a fresh dating of the Cuello sequence, for the first time using accelerator mass spectrometry (AMS) on the organic ("collagen") fraction of human bone from burials, which suggests a resolution of the dispute compatible with both stratigraphy and ceramic chronology and also indicates the potential utility of AMS dating of human burials as a way of constructing site chronologies.

It is well known that14C dating of fossil bone with seriously depleted protein levels, or bone that has been consolidated with preservatives, can produce erroneous results. In the tropics, warm and moist soil conditions lead to constant reworking of organic matter and add to the danger of bone contamination. Because of this,14C dating of preservative-impregnated bone from such areas has rarely been successful. We report here a set of AMS dates on both unconsolidated animal bone and polyvinyl acetate/polyvinyl alcohol (PVA/PV-OH) impregnated human burials from the Maya site of Cuello, Belize. The steps needed to purify the samples are described, together with details on the use of qualitative infra-red (IR) spectra as a means of assessing sample purity.

The earliest pottery yet found in the Western Hemisphere has been excavated from a prehistoric shell midden near Santarem in the lower Amazon, Brazil. Calibrated accelerator radiocarbon dates on charcoal, shell, and pottery and a thermoluminescence date on pottery from the site fall from about 8000 to 7000 years before the present. The early fishing village is part of a long prehistoric trajectory that contradicts theories that resource poverty limited cultural evolution in the tropics.