The Palaeo‐Environmental Contexts of Three Possible Phoenician Anchorages in Portugal

The 2002 Joint Expedition of the Institute of Nautical Archaeology and the Centro Nacional de Arqueologia Náutica e Subaquática examined Phoenician maritime involvement in Portugal, combining archaeological, geological and geophysical surveys of former coastal sites—Santa Olaia, Abul and Castro Marim—where previous excavations have uncovered Phoenician remains. Significant geomorphic evolution of bay‐head delta and estuarine settings masks the fact that Phoenician sites were situated at the head of marine embayments or on estuary margins, had easy access to the sea, and immediate access to at least one natural anchorage. All sites exhibited topographical criteria familiar from Phoenician trading‐stations and merchant outposts in the Mediterranean. © 2009 The Authors     

Tracking Hunter-Gatherer Impact on Vegetation in Last Interglacial and Holocene Europe: Proxies and Challenges

Journal of Archaeological Method and Theory - We review palaeoenvironmental proxies and combinations of these relevant for understanding hunter-gatherer niche construction activities in...     

Mapping feminist geographies in Spain

Abstract

Based on our experience of years of research, teaching and academic administration, this text gathers reflections on the past, present and future developments of feminist geography in Spain. We first show how a gendered perspective was introduced into geography in the late eighties. We then reflect on what we call ‘the stage of consolidation’ alongside territorial inequalities at the turn of the century. And we finally present some notes what the current situation is and identify future challenges. Despite the difficulties, we offer a positive vision of a long journey that has no turning back.     

Historic Barrel Vaults Undergoing Differential Settlements

ABSTRACT

A principal reason of damage in historic masonry vaults consists in relative displacements of the vaults’ abutments. Excluding the case of seismic-induced damage, cracks are often produced by differential settlements generated by the lateral wall instability or soil degradation (e.g., due to stress concentrations, non-uniform soil stratigraphy, flooding phenomena etc.). When dealing with historic vaults, the effects of long-term deformation processes cannot often be linked directly to causes, which may also be unknown. In this article, the effects of differential settlements on historic masonry barrel vaults are investigated. An efficient 3D contact-based model was developed to reproduce experiments on a scaled pointed barrel vault (representative of a typology of late-medieval barrel vaults in Scotland) under non-uniform differential settlement. First, the numerical model is used to simulate the experimental campaign, achieving good agreement in terms of crack pattern (longitudinal shear) and transverse-longitudinal deformation profiles. Then, further analyses are carried out to gain insight on the effects of several plausible uniform and non-uniform settlement patterns on representative historic barrel vaults. Various settlement configurations were analysed and complex failure patterns observed. This study could help analysts in understanding the nature of on-going deformation process in historic masonry vaults and engineers in the design of strengthening strategies.     

Oldest record of the scale-leaved clade of Podocarpaceae,early Paleocene of Patagonia,Argentina

A new podocarpaceous conifer is described from the early Danian Salamanca Formation (southern Chubut, Patagonia, Argentina) based on compressions of leafy branches with cuticular remains. Kirketapel salamanquensis gen. et sp. nov. has amphistomatic, scale-like leaves with marginal frills distinguishable at the apex; stomata oriented randomly in relation to the major axis of the leaf with four to five subsidiary cells and extremely reduced Florin rings; and irregularly shaped epidermal cells. We compare K. salamanquensis with extant and extinct members of the imbricate-leaved podocarps, among which it closely resembles Florin’s Dacrydium group C genera (i.e., Lagarostrobos, Manoao, Lepidothamnus and Halocarpus). Among these genera, only Lepidothamnus has a living representative in South America, the Chilean L. fonkii, whose leaf macro- and micromorphological characters are described in detail for comparison. Overall, the Patagonian fossil species is most similar to the extant and extinct members of Lagarostrobos in its cuticular micromorphology; however, macromorphological characters, such as the leaf size, apex curvature and mode of flattening, clearly differentiate it from all four genera of Dacrydium group C. We include Kirketapel salamanquensis in a combined molecular and morphological phylogenetic analysis conducted under the maximum parsimony criterion. The new, early Paleocene fossil taxon is confidently recovered as part of the scale-leaved clade as defined herein, which also includes Halocarpus, Phyllocladus, Lepidothamnus, Parasitaxus, Lagarostrobos and Manoao, and it constitutes the oldest record known for the group by at least 17 million years as well as its first fossil occurrence outside Australasia, establishing a widespread Gondwanan history. Furthermore, based on its oldest locality of occurrence, K. salamanquensis shows that the divergence of the total group of the scale-leaved podocarps occurred by at least 65 million years ago, adding to the growing systematic knowledge of earliest Cenozoic macrofloras in the Southern Hemisphere.

Ana Andruchow-Colombo [aandruchow@mef.org.ar] and Ignacio Escapa [iescapa@mef.org.ar] CONICET, Museo Paleontológico Egidio Feruglio Av. Fontana 140, Trelew 9100, Chubut, Argentina; Raymond J. Carpenter* [raymond.carpenter@adelaide.edu.au] School of Biological Sciences, University of Tasmania, Private Bag 55, Hobart, Tas. 7001, Australia; Robert S. Hill [bob.hill@adelaide.edu.au] School of Biological Sciences and Environment Institute, University of Adelaide, Adelaide, SA 5005, Australia; Ari Iglesias [ari_iglesias@yahoo.com.ar] CONICET, Instituto de Investigaciones en Biodiversidad y Medioambiente INIBIOMA-CONICET, Universidad Nacional del COMAHUE, Quintral 1250, San Carlos de Bariloche 8400, Río Negro, Argentina; Ana Abarzua [anaabarzua@uach.cl] Instituto de Ciencias de la Tierra, Facultad de Ciencias, Universidad Austral de Chile, Av. Rector Eduardo Morales Miranda 23, Valdivia 5090000, Región de los Ríos, Chile; Peter Wilf [pwilf@psu.edu] Department of Geosciences, Pennsylvania State University, University Park, PA 16802, USA. *Also affiliated with: School of Biological Sciences, University of Adelaide, Adelaide, SA 5005, Australia. Received 28.2.2018; revised 22.8.2018; accepted 24.8.2018.     

Architecture and Urbanism in the Fortified Settlement of Pech Maho (Sigean,France) in the Third Century BC: A Social and Economic Perspective

This paper offers a synthesis of the urbanism and architecture of Pech Maho (Sigean) from a social and economic point of view. Its aim is to highlight the specificities of this settlement in the context of the Late Iron Age between south France and north‐east Spain. During the third century BC, this small site had an impressive defensive system, as well as quite a complex urban framework. The constructed blocks excavated so far show a predominance of multicellular buildings that testify to a wide range of ground plans. Most of the spaces seem to have been devoted to specialized activities of a clear economic orientation, whilst other buildings or spaces have a strong symbolic nature. Rooms used exclusively for domestic tasks are in the minority, while a large dwelling in the central area appears to have been a private residential unit. All of this suggests that Pech Maho would have been an economic centre, as well as the residence of an elite that would have exerted control over the productive and trading activities, in a context that clearly evokes that of an emporion.     

The Emergence of Chariots and Riding in the South Caucasus

Summary.   The beginning of the Late Bronze Age, i.e. the late fifteenth–early fourteenth centuries BC, saw the emergence of chariots in Transcaucasia, where rich barrows of this period yielded bronze chariot models. The latter correspond to the type of chariots widespread in the western Near East in the late sixteenth–early thirteenth centuries BC. Hence it can be inferred that, regardless of the ultimate origin of Near Eastern chariots, Transcaucasian specimens belong to the Near Eastern tradition. However, in Transcaucasia, in contradistinction to the Near East, the chariot was merely a prestige marker. The growing role of the horse indicative of horseback riding is attested by some Transcaucasian funeral complexes of the late second millennium BC, which correspond to those of the steppes of south Russia. It seems likely that the builders of these barrows were related to the Iranian population of the Russian steppes.