Assessing the Scale and Pace of Large Shell-Bearing Site Occupation in the Prince Rupert Harbour Area,British Columbia

Methodological advancements in geoarchaeology and spatial and chronological modeling are opening new avenues to interpreting large coastal shell-bearing sites. We document the developmental histories of two such sites around Prince Rupert Harbour, Canada, using systematic percussion coring, intensive radiocarbon dating, and 3D surface mapping with Total Station and LiDAR. We also re-analyze a third site (Boardwalk/GbTo-31) excavated and radiocarbon dated in the 1960s, 1970s, and early 2000s using archival field notes, site maps, and stratigraphic profiles georectified using LiDAR. We map the natural landform beneath the sites and document the degree to which people physically modified landforms through the deposition of massive shell accumulations. We model site development through time and space and use accumulation rates and OxCal modeling to test for intentional deposition events. All three sites demonstrate complex and heterogeneous occupation histories. At each we identify instances of very rapid deposition that effectively terraced and extended parts of the natural landform to create places for constructing houses, though these episodes take place within longer histories of slower quotidian deposition. The anthropogenic modifications to the coastline in this area are the result of these mixed processes associated with long histories of occupation.     

Luminescence dating of anthropogenic deposits from Tall Zarʿa in the Jordan Valley

This study uses quartz-based optically stimulated luminescence dating to determine when a massive fortification wall (W11186) was constructed in the archaeological site of Tall Zarʿa in the Jordan Valley. A total of 11 samples of sediments were taken from a trench on the north side of the wall (extramuros). The extracted quartz grains had good luminescence characteristics and were identified as well bleached by comparison with feldspar infrared-stimulated luminescence (IRSL) ages. The optical ages showed that the deposition against the wall occurred in two different periods. The first was around 3.20 ± 0.07 ka ago (Iron Age), and the second was around 2.28 ± 0.08 ka (Hellenistic period). Human activity was evident because of the intermixing of cultural material with the presumed naturally deposited units.     

Prehistoric Human Impacts to Marine Mollusks and Intertidal Ecosystems in the Pacific Islands

From long-term stratigraphic records in Pacific Island archaeological sites, researchers have documented alterations to molluskan species richness and abundance, decreases or increases in mollusk shell size and, in rare cases, human foraging may have contributed to the extirpation of mollusk taxa. Mollusks perform critical ecosystem functions in tropical intertidal environments, including improving water quality through filtration, regulating algal cover, and increasing habitat and substratum complexity through ecosystem engineering. These critical ecosystem functions can be negatively affected by human foraging, possibly contributing to decreased resilience of coral reefs to climatic alterations. We review modern ecological research on human impacts to mollusks and intertidal ecosystems that illustrates the mechanisms and effects of human foraging. We then examine centuries to millennial scale archaeological records from the Pacific Islands to understand long-term, time-averaged trends in human impacts to intertidal ecosystems.     

The In Situ Preservation in the Unsaturated Zone: Results from Environmental Investigations at the ‘Schultz Gate’ Case Study in the Medieval Town of Trondheim,Norway

Medieval Trondheim is located on the eastern part of Nidarneset, a small peninsula formed by the river plain at the mouth of the River Nid on the southern shore of Trondheimsfjord. The topographic conditions for medieval Trondheim differ from those of the other Norwegian medieval towns (notably Bergen, Oslo, and Tønsberg), and the protected, historic part of Trondheim contains anthropogenic sediments which lie entirely within an unsaturated environment. A large proportion of these sediments contain wood and other types of organic material. The thickness of the anthropogenic sediments varies greatly from more than 4 m to less than 0.5 m, and they overlie well-drained alluvial sands and gravels. The Directorate for Cultural Heritage (Riksantikvaren) and the Norwegian Institute for Cultural Heritage Research (NIKU) have different roles in the management of cultural heritage sites. However, they cooperate in developing sustainable management and a scientific approach to research, as well as finding practical solutions aimed at securing stable preservation conditions for anthropogenic sediments that are vulnerable and sensitive to environmental changes, both chemical and mechanical. In this paper we present results from environmental investigations conducted in 2007 and 2012 at a location in the central part of medieval Trondheim where an in situ preservation project has been established on the site of new construction work. The project is cross-interdisciplinary, combining archaeological retrieval methods with the sampling and analysis of soil chemical parameters and the monitoring of present basic parameters such as temperature, moisture and redox potential. The monitoring has been ongoing since the beginning of 2013 and will continue until 2017.     

First Introduction and Early Exploitation of the Persian Fallow Deer on Cyprus (8000–6000 cal. bc)

The Persian fallow deer (Dama dama mesopotamica) is currently a threatened species. However, it played an important role in many Late Glacial and Early Holocene human societies in the Near and Middle East. This is especially true of the island of Cyprus, where it was introduced at the beginning of the Neolithic and held a predominant place in human subsistence throughout Cypriot prehistory until the Bronze Age. The earliest levels of the extensive Cypriot Pre‐Pottery Neolithic B site of Shillourokambos, occupied between 8400 and 7000 cal. bc , provided 3036 identified remains of this deer. It was possible to measure or determine the age‐at‐death for 1361 and 1444 remains, respectively. Analyses allow for discussions on when the fallow deer was introduced to the island of Cyprus, its origin and how populations were managed. These studies also lead to the reconstruction of acquisition and butchery techniques, as well as culinary practices, and the morphological evolution of males and females throughout time. The Persian fallow deer was introduced to Cyprus later than suids, dogs, cats, goats and cattle, and at nearly the same time as sheep, towards ca 8000 cal. bc . Despite the absence of any skeletal changes, this introduction may reflect an attempt to domesticate the fallow deer on the nearby continental mainland. However, after being introduced to the island, deer appear to have been released into the wild and hunted. Copyright © 2015 John Wiley & Sons, Ltd.     

Contemporary Sorted Patterned Ground in Low Altitude Areas of Tasmania

This paper summarises the distribution of patterned ground phenomena in Tasmania. It presents observations of low altitude sorted stone circles forming on glacial and alluvial deposits in the vicinity of Queenstown, Western Tasmania. Evidence suggests that freeze‐thaw derived patterned ground could develop in most inland valleys in Tasmania where cold air drainage causes sub‐zero ground temperatures in winter and permits the formation of ground and segregation ice to low elevations. Field observations suggest that patterned ground can only develop where freeze‐thaw processes are not inhibited by vegetation. The occurrence of patterned ground below altitudes of 900 m asl in Tasmania is largely a result of anthropogenic disturbance.     

朦胧的新旧易位:民国初年太炎弟子入职北大与“旧派”之动向——以朱希祖为中心

在民初北大的人事变动中,朱希祖作为正牌章太严弟子先于他人入职,颇充当了排头兵的角色。其入职并未引起旧派人士的强烈反应,旧派众人其后渐次离开北大,与朱希祖并无直接关系,原因亦各自不同,但均对校长何燏时主政下北大未来的趋向怀有背离之感。虽然后来更多太炎门生进入北大,代替桐城派等旧派人士居于核心地位,但以历史的眼光加以评判,此番新旧更替实有"以旧易旧"的意味。这说明在民初数年里,新旧世界虽已有移形换位之势,但"新"、"旧"之间的关系还有些朦胧,其清晰的标准尚在确立与制定之中。     

The Archaeological Record of Human Impacts on Animal Populations

Recent archaeological research has fundamentally altered our understanding of the scope of past human impacts on nondomesticated animal populations. Predictions derived from foraging theory concerning the abundance histories of high-return human prey and diet breadth have been met in many parts of the world. People are known to have introduced a broad variety of nondomesticated animals, from sponges to agoutis and rats, to a remarkably broad set of contexts, in turn causing a wide variety of secondary impacts. By increasing the incidence of fire, human colonists have in some cases transformed the nature of the vegetation on the colonized landscape, in turn dramatically affecting animal populations on those landscapes. In island settings, these triple threats--predation, biotic introductions, and vegetation alteration--routinely led to extinctions but there is no archaeological evidence that small-scale societies caused extinction by predation alone on islands or continents. Indeed, the recent history of this famous argument suggests that it is better seen as a statement of faith about the past rather than as an appeal to reason. Perhaps most importantly, our burgeoning knowledge of past human impacts on animals has important implications for the conservation biology of the future.     

Creating authentic ‘glacial’ landforms from waste materials: Two UK case studies

This paper describes two case studies of hills of waste material in the UK that have been specifically conceived to replicate glacial landforms. In one case a spent oil‐shale tip ('bing') and municipal waste dump in West Lothian has been remodelled and restored in the form of a local glacial crag‐and‐tail. In the other, a municipal waste disposal landraise hill in Lancashire has been designed to resemble the local drumlins. An assessment of the geomorphological authenticity of the landforms is made and it is concluded that the involvement of glacial geomorphologists in such projects is important if convincing and authentic outcomes are to be achieved. Adherence to landscape principles and attention to detail can pay dividends in winning public support, in achieving cost savings, and in securing successful after‐uses.     

Geothermal fluids circulation at Caldas do Moledo area, Northern Portugal: geochemical and isotopic signatures

A hydrogeological conceptual model of the Caldas do Moledo geothermal site is proposed that shows mixing between geothermal waters and local shallow groundwaters. Stable isotope values of Caldas do Moledo geothermal waters indicate recharge areas located at relatively high altitudes (850–1250 m a.s.l.). The NW–SE Vigo–Régua shear zone plays an important role in fluid recharge and circulation towards the NNE–SSW Régua–Verin fault system, forming a path for ascent of geothermal fluids. The apparent ¹⁴C age of geothermal fluids (15.66 ± 2.86 ka BP) was estimated in the total dissolved inorganic carbon (TDIC). Geothermometer calculations indicate that, assuming a conductive temperature gradient of 32°C per kilometer for northern Portugal, the maximum depth of circulation is roughly 1.8 ± 0.4 km. The K, Ca and SO₄ concentrations found in some Caldas do Moledo geothermal spring waters show mixing between deep geothermal and shallow groundwater systems. Local shallow groundwaters showing the highest SO₄ concentrations were found at low elevation areas, originating from fertilisers and pesticides applied to the Port wine vineyards in the Douro River valley. Geothermal waters from boreholes AC1 and AC2 do not show evidences of direct pollution from the spreading of such agrochemicals.