"These boots were made for walking": the isotopic analysis of a C(4) Roman inhumation from Gravesend, Kent, UK

As part of the road widening scheme between London and Dover, Oxford Archaeology South uncovered a large boundary ditch of Iron Age origin that contained Iron Age and Roman inhumations, adjacent to which was a small mid-late Roman cemetery, interpreted as a rural cemetery for Romano-British farmers. Grave goods in the cemetery were restricted to a few individuals with hobnailed boots. Bulk bone collagen isotopic analysis of 11 skeletons of Iron Age and Roman date gave a typical C(3) terrestrial signal (average δ(13) C = -19.8‰, δ(15) N = 9.3‰), but also revealed one (SK12671) with a diet which included a substantial C(4) component (δ(13) C = -15.2‰, δ(15) N = 11.2‰). This is only the second such diet reported in Roman Britain. Subsequent δ(18) O(c) and (87) Sr/(86) Sr measurements on the dental enamel in this individual were, however, consistent with a "local" origin, indicating that either C(4) protein was consumed in Late Roman Britain, or that he came from somewhere else, but where conditions gave rise to similar isotopic values. If we accept the latter, then it indicates that using oxygen and strontium isotopes alone to identify "incomers" may be problematic. The provision of hobnailed boots for the dead appears to have had a strong symbolic element in Late Roman Britain. We suggest that in this case the boots may be significant, in that he was being equipped for the long march home.     

Missing link in Late Antiquity? A critical examination of Hollstein’s Central European Oak Chronology

In 1980 Ernst Hollstein published his Central European Oak Chronology, which covers a period from 724 BCE to 1974 CE. Besides a later correction of the end date of the sampling site chronologies Kirnsulzbach (Germany) and Gustavsburg (Germany) this master chronology has since not been changed and still remains one of the most important bases for dendrochronological dating in western Germany. It stands out in so far as it provides comprehensive graphical findspot series for each individual sampled site and year to year growth values for eight regional sub-chronologies in addition to the combined Central European reference curve.Particularly due to the fact of Hollstein’s chronology being publicly available, it has frequently been criticized for its insufficient data to bridge the Late Antiquity between 350 and 400 CE with only three sampling sites (tomb near Beerlegem, Belgium; tomb inside of Cologne Cathedral, Germany; subfossil trees near Broichweiden, Germany) and that these site chronologies cover those decades with inadequate correlation coefficients. With regard to recent statistical threshold values for crossdating, Hollstein’s Late Antiquity bridging needs to be reconsidered.Therefore, in a combined effort, the dendrochronological laboratories at Rheinisches Landesmuseum Trier (RLM), the University of Cologne and Albert-Ludwigs-University Freiburg re-evaluated Hollstein’s findings for Late Antiquity by including the respective dendrochronological examinations conducted in Rhineland-Palatinate, North Rhine-Westphalia and north-eastern France during the past 40 years. A total of 62 site chronologies were compiled to establish a new Late Antiquity chronology. Thirteen of these site chronologies could be used to support Hollstein’s original bridging series between 350 and 400 CE while the mean series for Broichweiden had to be corrected from end date 365 to 503 CE. Furthermore, this new bridging chronology could be validated by comparing it to an independent chronology from southern Germany. This study thus proves that the integrity of Hollstein’s Central European Oak Chronology is not compromised by a flawed Late Antiquity bridging and that therefore dating based on the Roman part of this chronology can still be considered as absolute.     

Uniform diet in a diverse society. Revealing new dietary evidence of the Danish Roman Iron Age based on stable isotope analysis

A systematic dietary investigation during Danish Roman Iron Age (1‐375AD) is conducted by analyzing stable isotope ratios of carbon (δ¹³C) and nitrogen (δ¹⁵N) in the collagen of human and animal bone. The human sample comprises 77 individuals from 10 burial sites. In addition 31 samples of mammals and fish were analyzed from same geographical area. The investigation characterizes the human diet among different social groupings and analyses dietary differences present between sex, age, and site phase groups. Diachronically, the study investigates the Roman influences that had an effect on social structure and subsistence economy in both the Early and Late Period. Geographically the locations are both inland and coastal. The isotopic data indicate extremely uniform diet both between and within population groups from Early and Late Roman periods and the data are consistent throughout the Roman Iron Age. Protein consumption was dominated by terrestrial animals with no differences among social status, age, sex, or time period, while terrestrial plant protein only seems to have contributed little in the diet. Furthermore, the consumption of marine or aquatic resources does not seem to have been important, even among the individuals living next to the coast. Am J Phys Anthropol, 2010. © 2010 Wiley‐Liss, Inc.     

Condiments before Claudius: new plant foods at the Late Iron Age oppidum at Silchester,UK

Our understanding of the introduction and adoption of new plant foods in Roman Britain is currently limited by a lack of data from a group of Late Iron Age settlements commonly referred to as oppida (large pre-Roman towns). This paper presents the first evidence of several imported plant foods from Late Iron Age Britain in the form of waterlogged plant remains from the oppidum at Silchester. These were recovered from the basal contexts of two wells, dated to the early first century a.d. One olive stone and several seeds of celery, coriander and dill were identified. The results are compared to archaeobotanical data from elsewhere in Britain and northwestern Europe, demonstrating that Silchester is part of the wider phenomenon of the adoption of new flavourings and fruits in Late Iron Age Europe.     

Bone traumas in late antique populations from Croatia

We present the results of the analyses of traumatic bone injuries in two Late Antique (3r to 5th century AD) skeletal samples from Croatia: Zadar--located on the eastern Adriatic coast, and a composite skeletal series from continental Croatia consisting of skeletons from Osijek, Vinkovci, Strbinci, and Zmajevac. The osteological series from continental Croatia are related to settlements located on, or near the Danubian military border, while Zadar--350 km to the west, is located deep in the territory of the Roman Empire. Numerous historical sources describe barbaric incursions, as well as large battles related to civil wars during the Late Antique period in continental Croatia. Conversely, there is no mention of similar events in the Zadar region. In accordance with these data our analysis tests the hypothesis that the inhabitants of continental Croatia were exposed to greater levels of violence than those living in Zadar. Analysis of bone traumas in the two series shows a similar, relatively high prevalence of long bone fractures in both samples, with a slightly higher frequency recorded in Zadar. Both series exhibit a high frequency of cranial injuries with, once again, higher frequencies recorded in the Zadar series. Additionally, two perimortem cranial fractures (one caused by a sword, the other by a blunt object) were observed in Zadar. Some of the recorded traumas in both samples resulted from accidents, but a number of injuries clearly resulted from intentional violence of lesser intensity. Further multidisciplinary research incorporating osteological, archaeological, and historical analyses is necessary to confirm the results obtained from these samples.     

On the Late Pleistocene and Holocene history of vegetation and human impact in the Ücker valley, north-eastern Germany

A high-resolution Late Pleistocene and Middle to Late Holocene pollen profile of regional significance is presented. The coring site is located in a mire between two lakes. Ober- and Unter-ückersee, in Brandenburg, north-eastern Germany. The study was carried out in an archaeological context. It provides information about the history of vegetation, climate and human impact in the ücker river valley and the surrounding hills, the Uckerm?rker Hügelland. Hence, it is an important contribution for the reconstruction of the past vegetation of this area of Brandenburg. Seven AMS ¹⁴C-dates based on pollen concentrates provide a chronology for the middle Holocene part of the profile. Phases of intensive human activity can be shown from the middle Neolithic times until the Roman Iron Age. Received February 1, 2000 / Accepted January 18, 2001     

Arthritis in Roman Britain.

The pattern of arthritis in Roman Britain was investigated by examining the skeletons of 416 adults from the Roman cemetery at Poundbury Camp near Dorchester, Dorset. The mean height of the people was not much less than that of the current British population, and the prevalence of right handedness was similar to our own. There was a high prevalence of osteoarthritis for such a relatively young community, with particularly severe changes in the vertebral column. The pattern of joints affected by osteoarthritis was different from that seen now, but the prevalence of vertebral ankylosing hyperostosis was much the same. Rheumatoid arthritis was seen as often as the expected rat would indicate, given that the population died young, but it was rare. Other forms of arthritis, including gout and ankylosing spondylitis, were not seen.     

A First Case of Human Trichuriasis from a Roman Lead Coffin in France

A paleoparasitological study was carried out on 2 lead coffins recovered from the Roman site of Jaunay-Clan (near Poitiers, France). For the first time, this particular type of burial gave positive parasitological results, and eggs of the whipworm Trichuris trichiura were identified in 1 individual. In the present case, thanatomorphose associated with funerary practices may explain the scarcity of the recovered eggs. However, human whipworm has now been observed in 9 individuals dated to the Roman period. The very high frequency of Trichuris sp. eggs in Roman archaeological sites (up to 80%) suggests that fecal peril, hygiene, and waste management were problematic during this period. Finally, due to the fact that very few analyses have been conducted on human bodies dated to the Roman period, more analyses must be performed in the future to provide further information about diseases in the Roman world.     

A giant rhinocerotoid (Mammalia, Perissodactyla) from the Late Oligocene of north-central Anatolia (Turkey)

A giant rhinocerotoid is described for the first time south of the Black Sea, in Turkey. The single specimen, a fragmentary radius referred to Paraceratherium sp., originates from conglomerates nearby at Gözükizilli, in the Çankiri–Çorum Tertiary basin. These layers correspond to the Lower member of the Kizilirmak Formation. The same locality (Gözükizilli-2) yields also the small rhinocerotid Protaceratherium sp., cf. P. albigense (Roman, 1912). Three other mammal localities (Gözükizilli-1, in the Lower Member of the formation, with several rodent species; Tepe 641 and Kizilirmak, in the Upper Member, with a diversified micro- and macro-mammal fauna) allow us to refer the Kizilirmak Formation as a whole to the Late Oligocene. All the observed taxa have strong Asian and/or European affinities, which precludes any geographical insulation for this part of Anatolia during the Late Oligocene.  © 2008 The Linnean Society of London, Zoological Journal of the Linnean Society, 2008, 152 , 581–592.     

Late Celtic and early Roman plant remains from the oppidum of Bibracte, Mont Beuvray (Burgundy, France)

Two single assemblages of cereals and chaff from the oppidum Bibracte, (Burgundy, France), give evidence of cereal trade, food supply and crop processing in late Celtic and early Roman times. The first deposit consists mainly of Triticum dicoccon chaff which was buried in a wooden box near the sanctuary of La Terrasse. The second assemblage was a store of different wheats and barley excavated in a Roman cellar at the Pature du Couvent. The analyses of these finds are presented, and recent archaeobotanical research at Mont Beuvray is summarized.     

Biocorrosion and biodeterioration of antique and medieval glass

Over the past few years we have examined various antique and medieval glasses with regard to general biogenic damage, biopitting (crater erosion), bio‐crusts, and opalescent and white biogenic films. Experiments were carried out on pieces from Roman glass bottles excavated near Abu Tor, Sinai, some pieces of green and blue glass from Cologne Cathedral, some pieces from a little church in Evreux, glass samples from the fortress of the former Dukedom of Delmenhorst near Oldenburg, and some neolithic flint tools from the Negev Desert, Israel. Modern glass from a pigsty (19th century) additionally has been used for laboratory experiments on the attack of glass surfaces by fungi and bacteria. Some of the bacteria used in these experiments were isolated from the ancient pieces of glass. Biopitting with structures very similar to the biopitting of marble and limestone was found on almost all specimens. Lichens were not identified directly, but fungi and algae were observed in the pits as well as under the thin layers exfoliating from the Roman glass bottles. Initial steps of colonization and the potential for heavy‐metal accumulation by the isolated bacteria have been shown in laboratory experiments. A fractal dimension of diffusion‐limited disaggregation (DLD) is suggested as one possible explanation for the characteristic form and structure of the microbially induced and shaped biopitting patterns. A biopitting classification is suggested.     

Osteochondroma of the phalanx: A late Roman case

Accounting for 20–50% of all benign forms, solitary osteochondromae are the most common kind of bone tumour. The long bones of the lower extremity are the most frequently affected; the small bones of the hands and feet, the pelvis, the scapula, and the spine are less usual locations. This paper describes an osteochondroma in a proximal phalanx of the hand of a female aged between 17 and 25 years buried in a Late Roman necropolis from SE Spain. The bone displayed a solitary osteochondroma, which was confirmed by macroscopic and radiographic examination. This is the first palaeopathological example of a solitary sessile osteochondroma of the hand.     

安徽淮南晚新生代鬣狗类化石(英文)

记述了安徽淮南地区晚新生代洞穴、裂隙堆积中发现的鬣狗化行。材料系2003年至2006年间由本文作者之一(金昌柱)等在淮南市八公山区进行地层古生物调查时,于大居山老洞、西裂隙及大顶山裂隙的堆积物中采集到的。与鬣狗伴生的其他哺乳动物属种多样,并具有一定的地质断代意义。大居山老洞有Pliopentalagus huainanensis、Kowalskia sp.、Nan- nocricetus mongolicus等,西裂隙有Sericolagus sp.、Mimomys sp.、Equus sanmeniensis等,大顶山裂隙则有Lepus sp.、Ailuropoda sp.、Homotherium ultima等。所发现的鬣狗化石包括Adcrocuta extmta、Chasmaporthetes lunensis和Crocuta crocuta三种其中Crocuta crocuta至少包括三个个体;其他两种则只有一个个体。淮南的鬣狗种类跨越了晚中新世至晚更新世。Adcrocuta eximia为欧亚大陆晚中新世的特有种,为鬣狗科中朝食骨方向演化的类群;体型和前臼齿主尖与晚中新世较原始的属种(如Hyaenictitherium)相比,都有壮大的趋势。Chasmaporthetes地理分布最广,除欧亚大陆有多处化石记录外,还出现于北美洲的晚上新世至中更新世动物群中。修长的肢骨与尖利的颊齿表明了其擅长奔跑的能力和主动猎食的习性。该属在淮南的出现突出反映了一种相对开阔的古地理环境。Crocuta crocuta在大居山西裂隙与大顶山裂隙中都有发现。斑鬣狗分布于中国多处的中-晚更新世地点,包括台湾的澎湖列岛。在前臼齿的形态上,C.crocuta与Pachycrocuta相似,比A.eximia的宽大,具有更为进步的特征。这说明在早更新世晚期至中更新世早期,Crocuta极可能完全取代了Pachycrocuta。迄今在安徽Pachycrocuta仅发现于和县与繁昌的洞穴堆积中,由于目前确定高分辨率的洞、裂隙堆积物的地层年代较为困难,安徽的有关动物群足否记录了这个替代事件有待于进一步工作。淮南的鬣狗化石至少涉及了两个不同时期的动物群:一为Adcrocuta eximia所代表的晚中新世动物群,二为Crocuta所代表的晚上新世-更新世动物群。Chasma- porthetes lunensis的出现对于年代的确定并无太大帮助,但具有草原习性的Chasmaporthetes却为动物群的古生态环境分析和重建提供了一些证据。     

Human impact as registered in the pollen record: some results from the western Lake Constance region,Southern Germany

Pollen analytical results from a littoral profile taken in Lake Constance compared with pollen profiles from small kettle holes nearby form the basis for conclusions concerning human population density, the economy and environment from the Neolithic period to the Middle Ages. Early Neolithic human impact is implicated in a lime decline and also the expansion of beech. The late Neolithic lakeshore settlements caused a decline of elm, beech and lime and, by shifting cultivation, considerably changed the forest cover. The settlements were abandoned after less than 100 years. There were long periods without distinct human impact in the middle and towards the end of the late Neolithic period. Since at least the Late Bronze Age there has been permanent habitation in the region. Human impact was greatest in the High Medieval period and later, and was also substantial in the late La Tène and Roman periods. Distinct declines in human impact can be observed between the La Tène and Roman periods and in the Migration and Merovingian periods. In these intervals, open land and grazed oak forest were replaced by birch and later on by beech forests. The decreases in human impact are not of the same intensity in all diagrams.     

泥河湾盆地上新世生物地层序列与环境

总结了泥河湾盆地晚上新世生物地层,讨论了12个剖面含哺乳动物化石层位的相互关系,以稻地老窝沟剖面的地层顺序为基础排列出约3.7～2.6Ma时段内的9个代表性的生物地层单位。哺乳动物以Paenelimnoecus chinensis、Lunanosorex cf.L.lii、Trischizolagus、Pliopentalagus nihewanicus、Ungaromys、Mimomys sp.、Chardina truncatus、Mesosiphneus praetingi、M, paratingi、Plio- siphneus lyratus、Pseudomeriones complicidens、Castor anderssoni、Huaxiamys downsi、Chardinomys yusheensis、C.nihowanicus、Hipparion houfenense和Gazella blacki组合为特征。动物群在时代上与榆社麻则沟动物组合、静乐红土动物群、灵台雷家河剖面V带及任家沟静乐红粘土动物组合、宁县水磨沟动物组合、游河动物群及沂南棋盘山洞穴动物组合相当。动物群所反映的是温带草原为主、间有树林和干草原的稀树草原环境。     

Expected trends and surprises in the Lateglacial and Holocene vegetation history of the Iberian Peninsula and Balearic Islands

Recent, high-resolution palaeoecological records are changing the traditional picture of post-glacial vegetation succession in the Iberian Peninsula. In addition to the influence of Lateglacial and Early Holocene climatic changes, other factors are critical in the course of vegetation development and we observe strong regional differences. The floristic composition, location and structure of glacial tree populations and communities may have been primary causes of vegetation development. Refugial populations in the Baetic cordilleras would have been a source, but not the only one, for the early Lateglacial oak expansions. From Mid to Late Holocene, inertial, resilient, and rapid responses of vegetation to climatic change are described, and regional differences in the response are stressed. The role of fire, pastoralism, agriculture, and other anthropogenic disturbances (such as mining), during the Copper, Bronze, Iberian, and Roman times, is analysed. The implications of ecological transitions in cultural changes, especially when they occur as societal collapses, are discussed.     

我国部分地区E1^3—E2^1孢粉属种演变的古气候意义

通过对我国部分地区古新世晚期一始新世早期孢粉植物群演化发展规律的分析研究,结合国内外地层学研究的新进展,提出我国古新世晚期气候以暖湿为特征,且暖期的结束与始新世/古新世界限相吻合或接近,因此可以本次暖期的结束作为古新世的顶界。     

FIRST REPORT OF THE FERTILE PLANT GENUS UMKOMASIA FROM LATE PERMIAN BEDS IN INDIA AND ITS BIOSTRATIGRAPHIC SIGNIFICANCE

Abstract:  The genus Umkomasia Thomas, a female fructification of Dicroidium , is reported from Late Permian beds exposed in the Behra Rivulet near the village of Karaonda in the Tatapani-Ramkola Coalfield, Chhattisgarh, India. This is the first record of this genus from the Late Permian, and from Indian Gondwana. Two species have been recognized: Umkomasia polycarpa Holmes and U. uniramia Axsmith, Taylor, Taylor and Cuneo. The find suggests that the genus Dicroidium appeared in the Late Permian before reaching its acme in the Middle–Upper Triassic.     

Late Quaternary human settlement patterning in the Jebel Gharbi

This paper presents the latest results of geoarchaeological research on the Upper Pleistocene sequence in the Jebel Gharbi (previously called Jebel Nafusah), a mountain range located in Tripolitania, northwestern Libya. Numerous archaeological sites are found adjacent to springs that formed as a consequence of tectonic activities. The springs originated when Upper Pleistocene earthquakes produced ground displacements that created water outlets, some of which are still active. Springs are spread all along the massif and at the foot of the mountains in Jebel Gharbi. We suggest that they offered attractive resources to populations coming from drier parts of North Africa or the near-by Sahara. The earliest sites associated with the springs include Aterian lithic techno-complexes that have been dated between 80,000 and 40,000 BP. Since then, these springs have attracted many populations, as documented here by settlements belonging to the Later Stone Age (Upper Palaeolithic), Iberomaurusian (Late Upper Palaeolithic or Epipalaeolithic), Neolithic, Roman period, and present time.