The Environmental History of Tigray (Northern Ethiopia) in the Middle and Late Holocene: A Preliminary Outline

This paper outlines the environmental history of the Tigrean Plateau (northern Ethiopia) during the Holocene, based on the available geomorphological, palynological, archaeological, and historical evidence. At present, it seems that (1) the plateau experienced a more humid climate with a denser vegetation cover during the Early Holocene; (2) Soil erosion due to clearing vegetation began in the Middle Holocene; (3) agricultural activity was intensified in the Late Holocene, as a consequence of the rise of a state; (4) demographic pressure increased from the early first millennium BC to the mid–first millennium AD, causing soil erosion; (5) environmental degradation and demographic decline occurred in the late first millennium AD; (6) the vegetation cover was regenerated in the early second millennium AD; and (7) progressive vegetation clearance started again in the second half of the second millennium AD.Cet article trace l'histoire ambiante du Plateau Tigréen dans l'Holocène en utilisant les données géomorphologiques, palynologiques, archéologiques et historiques. Il semble que (1) dans l'Holocène ancien le plateau était caractérisé par une phase humide avec une dense végétation; (2) l'érosion causée par l'abbattage de la végétation commen¸a dans l'Holocène moyen; (3) l'activité agricole s'inténsifia à la fin de l'Holocène, par conséquence de l'essor d'un état; (4) la pression démographique augmenta de plus en plus du début du premier millénaire av. J.-Ch. à la moitié du premier millénaire ap. J.-Ch.; (5) la dégradation ambiante et la diminution démographique se vérifièrent à la fin du premier millénaire ap. J.-Ch.; (6) une régéneration de la vegetation se vérifia au début du seconde millénaire ap. J.-Ch.; et (7) l'abbatage de la végétation recommen¸a dans la seconde moitié du seconde millénaire ap. J.-Ch.     

Human occupation and geomorphological evolution of the Thessaloniki Plain (Greece) since mid Holocene

The plain of Thessaloniki is an important area from a historical standpoint. Numerous reigns and empires have occupied the area, leaving behind numerous archaeological remains. The literature and historical evidences show that the city of Pella was located near the sea and its harbor was the starting point of various conquests of famous kings such as Philip the 2nd and Alexander the Great. At present, the ancient capital is located 28 km inland the large fertile plain of Thessaloniki.     

Holocene hyrax dung deposits in the afroalpine belt of the Bale Mountains (Ethiopia) and their palaeoclimatic implication

Abstract

The results of pollen analysis and radiocarbon dating are presented for two hyrax dung deposits from rock shelters found in the Afroalpine zone of the Bale Mountains (South-Central Ethiopia). Deposits accumulated from about 15,000 to 1500 (cal) years BP and from 7000 (cal) years BP till nowadays, respectively. Pollen spectra of the initial stages of deposit development (up to 15,000 (cal) years BP) correlate with unfavourable conditions in the Late Glacial Maximum. The African Humid Period (AHP) (15,000–5000 (cal) years BP) is registered in this palaeoecological record as well as the Younger Dryas event (about 12,500 (cal) years BP). Upward shift of Afromontane forest belt and expansion of ericoid communities at high altitudes were characteristic of the Pleistocene/Holocene transition (about 10,000 (cal) years BP). The AHP which continues around 10,000 (cal) years BP after Younger Dryas, was interrupted by a dry episode around 8200 (cal) years BP. Principal aridisation trend during the last 5000 years was observed. Presumably the first traces of human activities in this area can be shown for up about 2500 (cal) years BP.     

Scottish landform examples 44: the Dirc Mhòr meltwater gorge

The Dirc Mhòr gorge in the central Grampian Highlands is 1.1 km long, ～250 m wide and up to 110 m deep, and is incised in granite bedrock. It is the largest of several bedrock gorges that are incised into spurs, cols or plateau margins in the area, and its present catchment area is negligible. The floor of the gorge is covered by coarse rockfall debris, and the sides of the gorge are mantled by talus accumulations; surface water flow is absent. The gorge is inferred to have evolved over several glacial-interglacial cycles, with subglacial meltwater erosion deepening the gorge under successive ice sheets, and paraglacial rockwall collapse widening the gorge during intervening interglacial periods. Subglacial erosion may also have contributed to gorge enlargement as it widened.     

Editorial I

Communication strategies emphasize concerns for content (what is said) and process (the way things are said). Scientists have a responsibility to communicate the findings of their research, enhancing prospects that their insights can meaningfully inform management practice. When used effectively, principles from geomorphology provide critical guidance for environmental management. Three key geomorphic messages are outlined here: Respect diversity through communicating spatial and temporal controls upon landscape character and behaviour; Work with nature in conveying the range of behaviour of any given system; and Be proactive by determining the trajectory of landscape change. Uptake of geomorphic understanding reflects, among many factors, our ability to communicate findings clearly. In communicating these messages, different approaches are likely to prove more effective when addressing differing audiences, whether school/university classes, stakeholders, managers, politicians, or the broader community. Collective approaches to learning through dialogue are encouraged as they promote deeper learning, prospectively enhancing the uptake of geomorphic understanding, thereby promoting healthier environmental futures.     

Palaeoecology and Archaeology of the Village of Uukuniemi,Eastern Finland

Abstract

In the present article, pollen analytical results from Lake Kirkkolampi are presented and compared with results provided by archaeological material. Pollen analysis is connected with the archaeological research project at Papinniemi in Uukuniemi. Papinniemi is one of the numerous Greek Orthodox settlements that existed in Karelia in the fourteenth to seventeenth centuries. Archaeological evidence of settlement preceding this period is very scarce, and in this respect Uukuniemi represents a typical area in eastern Finland. There is no archaeological evidence of permanent settlement in Uukuniemi from the Early Metal Period (c. 1800 bc–ad 400), the Middle Iron Age (c. ad 400–800) or from the Late Iron Age (c. ad 800–1300). Pollen analysis demonstrated the onset of cultivation c. cal ad 300. Marked intensification of agricultural activities and cultivation in permanent fields took place around cal ad 800. A shift in land-use practises, including a declining use of fire, is visible at cal ad 1520–1600. The discrepancy between archaeological and palaeoecological records raises several questions, and the problems of Early Metal Period and Iron Age populations, as well as settlement continuity, are discussed.     

Neolithic occupation and mid-Holocene soil formation at Encosta de Sant'Ana (Lisbon,Portugal): a geoarchaeological approach

Excavations at the archaeological site of Encosta de Sant'Ana (Lisbon, Portugal) uncovered a mid-Holocene buried alluvial soil associated with early Neolithic occupation layers. Routine laboratory analyses and micromorphological observations were undertaken on the soil material. Humic acids from its Ab horizon, as well as Neolithic ecofacts, were radiocarbon dated. The dates obtained indicate that soil was formed between c. 8.0 and 6.0 cal ka BP and that the pedological evidence fits the record of the North Atlantic Holocene IRD events (“Bond events”) and the so-called “Holocene climate optimum”. The geoarchaeological record reveals that Neolithic inhabitants settled upon a stable surface, still affected by soil formation that was suddenly interrupted by slope wasting, probably in correspondence to Bond event 4, at c. 6.0 cal ka BP.     

世界历史教学的挑战

当今,无论在研究领域还是教学领域,世界历史都成为最重要的议题之一。人们可以真切地感受到有关世界体系的历史研究取得了长足发展。这一新趋势削弱了传统的中、小学历史教学,传统历史教学建立在种族中心主义方法基础之上,被民族国家用于加强民族集体认同（通常与其他国家相对立）。与此相反,新的世界历史教学可以被视为一种开展不同文化间教育和加强世界主义的手段。这里建议世界历史课程计划以概念、空间和时间这三重框架为基础。概念框架集中于两个主题：人类社会的演进及其相互交往;空间框架可以持续利用与主题有关的球体投影图来展示;时间框架由基于9个时代的历史分期连接起来,另附一个时期论述未来前景。     

Innovative Trends in Women's and Gender Studies of the National Socialist Era

The text is less a review of the new literature than a reflectionon significant and innovative current trends in the historiographyon women and gender in the National Socialist era. The firstpart deals with various women's activities within milieus andprofessions, including their room for manoeuvre: midwives, socialworkers, female Nazi functionaries, and female auxiliary workersof the Nazi Wehrmacht. The second part of the article addressesspecific features of biopolitics, targeted not only againstJews but also against asocial women, homosexuals and prostitutes.It also looks at visual images of bodies. Although the Nazistried to create strongly determined binaries to categorize ‘we’and ‘the others’ in the arts and other propagandamaterial, there existed, in fact, a broad spectrum of body images,especially among media stars. A third trend in the history ofthe Third Reich deals not only with the politics of exclusionbut also of inclusion, as found in the concept of Volksgemeinschaft(national community), a concept that had many facets, such asthe Volksfamilie, comradeship and home front. And it was themedia that had the task of ‘translating’ this conceptto the people in many appealing ways. The fourth part considersthe gendering of memories after 1945 and the dominance of malenarratives and points of view. The four parts of the articleare intended to contribute to intersectional history and thehistory of social engineering.     

大学校史研究中的若干问题

学校的历史,是一个学校整体的历史。因其在教育史、文化史、社会史上的特殊地位,使得它的研究具有一般历史研究所不具备的特殊意义。但在中国特殊的国情下,一方面是大学离散聚合频繁,存亡继绝难测,从而加大了校史研究的复杂性;另一方面又因缺乏历史学者的参与,而使得大学校史的撰写存在诸多缺憾,校史的研究难成一门“显学”。     

Ancient Fife: Seen through its place‐names

Many publications have appeared dealing in whole or part with breeds of hij 1 cattle in Scotland, but none approach this subject from a geographical standpoint. This is perhaps surprising in view of the fact that the various breeds have long been an important element in the cultural landscape. Moreover, during the past thirty years their numbers have increased fivefold to some 380,000 and profound changes have taken place in the traditional breed structure. It is the purpose of this paper to fill in part this gap by describing and explaining, in a general way, the distribution of the main breeds and crosses.     

Fluvial sediments, correlations and palaeoenvironmental reconstruction: The development of robust radiocarbon chronologies

Multiple sequences of radiocarbon dates extracted from organic materials are increasingly being used to provide robust chronologies for landscape development, particularly the timing and correlation of significant climatic and ‘process’ events. Whilst the validity of using such frameworks in sedimentary environments such as lake basins and raised bogs has been the focus of much attention, such debates have not extended to fluvial systems. Using examples from three lowland, vertically accreting river valleys in East Anglia, UK, this paper assesses the robustness of their associated radiocarbon chronologies by assessing the contrasting age estimates that are obtained by dating different parts of the same organic sample (humic, humin and plant macrofossils) at a variety of stratigraphic levels. Overall, the humin and humic acid fraction results were statistically consistent, whilst the plant macrofossil remains were found to be of a slightly younger age. In these examples, it is argued that the younger ages appear to be the result of Phragmites (common reed) roots pushing plant macrossils through the sedimentary sequence or opening up voids for material to fall through, although studies in lacustrine and mire environments suggest alternative explanations may also be possible. Whichever explanation is preferred, this study demonstrates clearly that the complexity of valley floor stratigraphy and processes is such, that using single radiocarbon dates, whether AMS or bulk samples to reconstruct chronologies of ‘geomorphic system response’ may need to be refined and subjected to the same level of assessment that has been applied in other sedimentary systems.     

Court-day crowds in colonial Virginia

ABSTRACT

For a generation, legal historians investigating colonial Virginia have emphasized the dramaturgy of court day. According to the dramaturgical school of interpretation, administrative and judicial activities of county court officials amounted to theatrical performances that simultaneously enforced economic order and stabilized traditional social relationships. Such interpretations assume a large audience routinely attended county courts to observe legal dramas. Often, however, only a small number of persons can be documented as present during court day. The independence theorem from probability theory suggests that the number of documentable attendees is a useful and easily calculated estimate for actual total crowd size. If so, some Virginia court sessions were attended by hundreds of people, while others drew only a few participants. A variety of factors apparently inhibited court attendance in older Virginia counties. By contrast, in newer frontier counties, mid-eighteenth-century revisions of court calendars produced heavy attendance at court day. Regardless of the number of people in attendance, any Virginia county court could still effectively enforce credit contracts.     

An 8000-year history of landscape,climate, and copper exploitation in the Middle East: the Wadi Faynan and the Wadi Dana National Reserve in southern Jordan

Investigations of geomorphology, geoarchaeology, pollen, palynofacies, and charcoal indicate the comparative scales and significance of palaeoenvironmental changes throughout the Holocene at the junction between the hyper-arid hot Wadi 'Arabah desert and the front of the Mediterranean-belt Mountains of Edom in southern Jordan through a series of climatic changes and episodes of intense mining and smelting of copper ores. Early Holocene alluviation followed the impact of Neolithic grazers but climate drove fluvial geomorphic change in the Late Holocene, with a major arid episode corresponding chronologically with the ‘Little Ice Age’ causing widespread alluviation. The harvesting of wood for charcoal may have been sufficiently intense and widespread to affect the capacity of intensively harvested tree species to respond to a period of greater precipitation deduced for the Roman–Byzantine period – a property that affects both taphonomic and biogeographical bases for the interpretation of palynological evidence from arid-lands with substantial industrial histories. Studies of palynofacies have provided a record of human and climatic causes of soil erosion, and the changing intensity of the use of fire over time. The patterns of vegetational, climatic change and geomorphic changes are set out for this area for the last 8000 years.     

The spatial distribution of Palaeolithic human settlements and its influence on palaeoecological studies: a case from Northern Iberia

The aim of this study is to assess the influence of human site location choice on biogeographical and paleoecological studies based on archaeological remains, through a case study in north-western Spain. Data from an exhaustive literature survey and field trips were managed with GIS and subjected to statistical analyses. The results show that the influence of the different variables shifted through the Palaeolithic, although certain general preferences can be seen: low altitudes (median: 151 m a.s.l.), South-facing surfaces, generally gentle slopes (median: 13°) and moderate distances to water courses (median: 297 m). These choices were conditioned by geomorphological factors, with LGM glacier extent imposing an upper limit in the range of occupied altitudes and marine and fluvial terraces conditioning site location patterns. The results suggest that human site location patterns during the Palaeolithic were not random, conditioning the information available from archaeological remains. Our results allow us to identify some key areas where information on past faunal distributions, and more generally on biocoenoses, will be scarce or missing.     

A Forgotten Legacy: The Romanov Patronage of Finland’s Early Art Collections

The earliest art collections of Finland’s National Gallery came into being when, as the Grand Duchy of Finland, it was an autonomous part of imperial Russia (1809–1917). The prevailing view of Finnish museum studies, however, sees the Finnish Art Society, the precursor of the Finnish National Gallery, as being modelled on exclusively European cultural institutions. The history of the Society and its collections have thus been seen as resistant to any alien eastern influences, and as an attempt to differentiate Finnish culture from Russian art collecting practices. Drawing on the theoretical shift in cultural studies from the conception of stable, clearly demarcated cultural identities of nation states toward less rigidly defined identities, the aim of this essay is to reconstruct the hidden Russian presence in Finnish museum historiography. Based on original unpublished sources, my study shows that the earliest support of Finland’s cultural infrastructure was given by the Romanov patrons Nicholas I, Alexander II, and Alexander III. By exposing the absence and physical erasure of “imperial identity” in the official Finnish museum narrative, I reveal how museums can at once elevate particular discourses and practices while marginalizing other historical processes in a nation’s cultural past.     

政治-社会史:深化史学研究的新路径

自上世纪80年代社会史研究复兴以来,长期处于史学研究核心的政治史作为方法论的支配地位渐趋式微。但就政治与社会的密切关系、中国传统社会政治一体化的特征及社会史研究整体性目标的追求而言,“政治—社会史”的研究理应成为当前政治史研究的一个新路径。在坚持唯物史观、以历史学为本位的前提下,借鉴政治学、社会学与人类学等学科的理论与研究方法,由更广义的政治现象切入社会生活,考量政治与社会环境、社会结构、社会文化、社会治理等方面的互动关系及其影响,则可以深化传统的政治史的研究。     

DEEP GENETICS: UNIVERSAL HISTORY AND THE SPECIES

The popularity of books such as Yuval Noah Harari's Sapiens: A Brief History of Humankind suggests that universal history‐writing has a continuous not a broken past. Rather than “returning,” it is perhaps the most enduring genre of all. This review essay explores the deep‐history element of universal histories and the ongoing purchase of the stadial tradition for a new history of the species. Why are deep histories of the species so reliably appealing, and what do they mean in the twenty‐first century? Although the Anthropocene would seem to be the pertinent context for this ongoing historiography, this essay suggests that the new domain of genetic genealogy powerfully individualizes and commercializes deep history for neoliberal times.     

试析上古时期的历史记忆与历史记载

上古时期口耳相传的历史记忆是后世历史记载的源头.在相关的历史记载中还可以看到其某些影子.出现于早期历史记忆中的"人"多为"英雄"或"圣人",而非普通的人.逐渐剥落掉神的身影,而呈现出真正的"人"面貌,已经是野蛮与文明之际的事情.但是即使在这个时期,人--神之间仍然有着千丝万缕的联系.历史记忆是古代文明出现上升的阶梯.