Nonmetric dental characteristics of the early modern population of Okinawa Island in Nansei Islands,Japan

Dental morphological characteristics of the early modern population (c. 17–19th century AD) of Okinawa Island, Nansei Islands, were investigated to clarify their genealogical characteristics. We observed and classified 25 nonmetric traits of tooth crowns and roots from human remains (106 individuals) excavated from tombs of the early modern period in Okuma, Ginowan City, Okinawa. The incidences of these traits were compared with the incidences in the populations of the other Nansei Islands, of Japan, and of Asia overall. Univariate analysis of each trait and multivariate biological distance analysis based on the frequencies of the traits showed that the Okinawa population in the early modern period more closely resembled the migrant Yayoi populations than it did the native Jomon populations. It is difficult to support the “Ainu‐Ryukyu common origin theory” with regard to the early modern population in Okinawa without some modification of the theory, as well as the modern populations in Tanegashima and Okinawa Island. The geographical cline in the modern period from the northern Kyushu to the Okinawa Island via Tanegashima was confirmed in this analysis. Considering the major temporal changes in northern Kyushu and Tanegashima in addition to the geographical cline, the southward gene flow of the migrant Yayoi elements from northern Kyushu to the central Nansei Islands via the northeast end of the Nansei Islands is suggested. In addition, this study detected some temporal changes from the early modern to the modern period in Okinawa Island. Although the minor temporal change may be attributed to some genetic drift, gene flow from the Japanese main islands or China might be considered one of the causes of the change. Copyright © 2010 John Wiley & Sons, Ltd.     

16th-Century Ship Graffiti on the Town Walls of Eivissa, Balearic Islands, Spain

Among the historical ship depictions in Eivissa (Balearic Islands, Spain), the graffiti of galleys on the Renaissance city walls are of particular interest. From archival documents the building sequences of this monument can be confirmed. Thus the galley graffiti on the eastern side of the bastion of Sant Bernat can be narrowed down chronologically to slightly after 1568. These graffiti are also interpreted from the social history point of view, in the light of ongoing corsair incursions during the 16th century.
© 2009 The Author     

Evidence for Differential Ancient DNA Survival in Human and Pig Bones from the Norse North Atlantic

Current models of DNA degradation and previous research on Icelandic human skeletons predict ancient DNA preservation in the Norse North Atlantic faunal remains to be excellent. In contrast, we found that DNA preservation in Viking‐Age pig remains was poor. We posit that this discrepancy in DNA survival between human and faunal remains is due to differing taphonomies. Our results highlight that DNA degradation is strongly dictated by micro‐environmental taphonomic processes even in regions where the climate is conducive to DNA survival. Due to these differences, DNA preservation in animal remains may not be suitable proxies for DNA preservation in associated human remains. Copyright © 2012 John Wiley & Sons, Ltd.     

Late Holocene Changes in Shellfishing Behaviors From the Gulf of Carpentaria,Northern Australia

ABSTRACT

Dramatic changes in shellfishing behaviors occur across northern Australia during the late Holocene, marked most conspicuously by the cessation of large shell mound construction in some areas, and the reorganization of shellfishing behaviors towards more intensive production in the last 1,000 years. Excavations reveal rapid and widespread changes within coastal sites, an increasing diversification in overall subsistence resources, and patterns of increase in site establishment and use. Some of these changes have been argued to be associated with increasing climate variability and a trend towards increasing aridity during the late Holocene, thought to have transformed coastal ecosystems and mollusc availability. However, when these hypotheses are tested at the local level, more nuanced patterns of human-environment interaction emerge, which call into question interpretations based on broad-scale climate records. We suggest that disjunctions in the timing of the cessation of shell mound construction noted between the west and east Gulf of Carpentaria may be related, at least in part, to the timing and intensity of external cultural contacts with Macassan seafarers, associated with reorganization of mobility and production strategies, rather than as yet undemonstrated environmental changes impacting on shellfish availability.     

Contested enclave metageographies: The offshore islands of Taiwan

The offshore islands of Taiwan (Republic of China) are dynamic examples of contested metageographies, island spaces caught in between competing and opposing interpretations of their identities, relativities, notions of sustainability and futures. Three cases – (1) population growth, land use conflict, a switch from a military to a tourism economy, and ever closer links between mainland China and Kinmen Island; (2) the rejection of a move to establish a casino economy on the Penghu archipelago; and (3) protests against the storage of spent nuclear waste on Orchid Island – are presented as illustrative of such changing topographies, themselves reflective of a transition to a more democratic and pluralist society in Taiwan. The paper hints at an evolving shift in both vertical (top/down) and horizontal (island-to-island) relations in the construction of development paths and futures for Taiwan's de facto archipelago. This re-territorialization offers a fresh, archipelagic repivoting of political geography for and beyond Taiwan.     

Starch analysis reveals prehistoric plant translocations and shell tool use,Marquesas Islands,Polynesia

Starch analysis is proving particularly useful in tropical regions like the central Pacific where crop inventories are often dominated by starchy fruits and tubers and recovery of macrobotanical remains is rare. Analysis of 23 shell tools from the Marquesas Islands provides direct evidence for translocation of five traditional crop plants. Four taxa derive from the western Pacific, including Artocarpus altilis (breadfruit), Piper methysticum (kava), Colocasia esculenta (taro), and one or more species of Dioscorea (yam). The fifth taxon, the South American Ipomoea batatas (sweet potato), dates from the 14th century AD onward and constitutes the earliest record of this cultigen in the archipelago. The occurrence of sweet potato starch suggests that this crop plant may have been more important than usually is assumed, while the limited recovery of breadfruit starch, the main Marquesan food plant at western contact, requires further investigation. The starch residues also inform on tool use, demonstrating that shell tools ethnographically associated with specific crops (e.g., “breadfruit peelers”) had more generalised functions. This study is a further demonstration of the potential of starch analysis to provide important information on the history of crop introductions, on-site activities, and artefact use.     

Modelling site formation dynamics: geoarchaeological,chronometric and statistical approaches to a stratified rockshelter sequence,Polynesia

Formation processes and chronology are central to many archaeological endeavours, and accuracy in the latter is dependent on control of the former. Here we consider how to integrate geoarchaeological and chronometric evidence to better understand the formational history, along with the timing and duration of cultural activities, at a regionally significant site in the southern Cook Islands (Polynesia) which dates from ∼12th century AD. Initially we model natural and cultural processes of deposition using geoarchaeological evidence. The results are integrated with 21 radiocarbon dates, including nine new AMS results on identified medium and short-lived materials. Sample outliers are identified manually and statistically and a Bayesian analysis helps to refine age estimates for the site's 12 stratigraphic zones. The timing and rate of sediment accumulation is further considered through an age–depth model. Finally, the chronology developed from these combined approaches is used to address three key processes: 1) initial site use, potentially relevant to human colonisation of this Polynesian island and archipelago; 2) on-site activities and patterns of resource use; and 3) major marine deposition events which disrupted cultural activities and may have palaeoclimatological significance. The approach developed here potentially has utility elsewhere, particularly where human activities are recurrent and of limited duration.     

Miocene molluscs and barnacles from Mont Rond,Kerguelen Islands

A sedimentary deposit discovered at Kerguelen Islands in 1988 is interbedded in the Cape MacLear cliffs, near Mont Rond (Ronarc'h Peninsula). The age of this oceanic deposit is considered to be lower to middle Miocene as indicated by isotopic dating of both the underlying and overlying basalts. This deposit yields a fauna essentially consisting of molluscs (bivalves, gastropods) and crustaceans (cirripedes). This fauna exhibits some similarities to Miocene to Recent austral faunas (New Zealand, Argentina) as a result of the establishment of the Antarctic Circumpolar Current. However, it has no species in common with the extant Kerguelen fauna. The Mont Rond fossil assemblage is best compared with either of two types of extant communities developed on a bare sandy sea floor where infaunal species are dominant, but most likely to an opportunistic one in depths from approximately 10 to 80 m.     

Palaeontology of the Chatham Islands,SW Pacific—a review

Despite their small area, the Chatham Islands host diverse and abundant fossils. Fossil assemblages of Permian to Late Cretaceous age preserved in terrestrial to shallow marine deposits represent the only record of plants and animals that once inhabited the eastern extension of Zealandia. Lower Cenozoic sediments have yielded a shallow marine fauna, including a rich molluscan assemblage linked to the oceanic inundation of this landmass. The late Cenozoic biota documents the re-emergence of the Chatham Islands and the establishment of major oceanic currents, which meet along the Chatham Rise. This review summarizes the fossil record of the Chatham Islands and the Chatham Rise, integrating data from published and unpublished sources.