Younger Dryas-Holocene sedimentary plant-wax hydrogen isotopes from the southern European Alps

We present a Younger Dryas-Holocene record of the hydrogen isotopic composition of sedimentary plant waxes (dDwax) from the southern European Alps (Lake Ghirla, N-Italy) to investigate its sensitivity to climatic forcing variations in this mid-latitude region (45°N). A modern altitudinal transect of dD values of river water and leaf waxes in the Lake Ghirla catchment is used to test present-day climate sensitivity of dDwax. While we find that altitudinal effects on dDwax are minor at our study site, temperature, precipitation amount, and evapotranspiration all appear to influence dDwax to varying extents. In the lake-sediment record, dDwax values vary between -134 and -180 per mil over the past 13 kyr. The long-term Holocene pattern of dDwax parallels the trend of decreasing temperature and is thus likely forced by the decline of northern hemisphere summer insolation. Shorter-term fluctuations, in contrast, may reflect both temperature and moisture-source changes. During the cool Younger Dryas and Little Ice Age (LIA) periods we observe unexpectedly high dDwax values relative to those before and after. We suggest that a change towards a more D-enriched moisture source is required during these intervals. In fact, a shift from northern N-Atlantic to southern N-Atlantic/western Mediterranean Sea sources would be consistent with a southward migration of the Westerlies with climate cooling. Prominent dDwax fluctuations in the early and middle Holocene are negative and potentially associated with temperature declines. In the late Holocene (<4 kyr BP), excursions are partly positive (as for the LIA) suggesting a stronger influence of moisture-source changes on dDwax variation. In addition to isotopic fractionations of the hydrological cycle, changes in vegetation composition, in the length of the growing season, and in snowfall amount provide additional potential sources of variability, although we cannot yet quantitatively assess these in the paleo-record. We conclude that while our dDwax record from the Alps does contain climatic information, it is a complicated record that would require additional constraints to be robustly interpreted. This also has important implications for other water-isotope-based proxy records of precipitation and hydro-climate from this region, such as cave speleothems.

Market reforms and privatisation in the English National Health Service

The article examines developments in the marketisation and privatisation of the English National Health Service, primarily since 1997. It explores the use of competition and contracting out in ancillary services and the levering into public services of private finance for capital developments through the Private Finance Initiative. A substantial part of the article examines the repeated restructuring of the health service as a market in clinical services, initially as an internal market but subsequently as a market increasing opened up to private sector involvement. Some of the implications of market processes for NHS staff and for increased privatisation are discussed. The article examines one episode of popular resistance to these developments, namely the movement of opposition to the 2011 health and social care legislative proposals. The article concludes with a discussion of the implications of these system reforms for the founding principles of the NHS and the sustainability of the service.

GIS technologies and spatial organization patterns among hunter-gatherers: an archaeological case study from Southern Patagonia (southern South America)

This paper discusses some aspects of hunter-gatherer spatial organization in southern South Patagonia, in later times to 10,000 cal yr BP. Various methods of spatial analysis, elaborated with a Geographic Information System (GIS) were applied to the distributional pattern of archaeological sites with radiocarbon dates. The shift in the distributional pattern of chronological information was assessed in conjunction with other lines of evidence within a biogeographic framework. Accordingly, the varying degrees of occupation and integration of coastal and interior spaces in human spatial organization are explained in association with the adaptive strategies hunter-gatherers have used over time. Both are part of the same human response to changes in risk and uncertainty variability in the region in terms of resource availability and environmental dynamics.

Espaço e sentidos: uma topoanálise de “vila dos confins”

vol. 19, n. 2, p. 211-223, jul./dez. 2015.

Rifiuti prodotti nel settore marmifero: applicazioni e recupero.

Con il presente elaborato, si vuole fornire un contributo alla conoscenza sul riutilizzo degli scarti derivanti dall’estrazione e lavorazione nelle cave di marmo, per aggiungere un’ulteriore tassello per arriva ad un’economia circolare anche in questo settore. Viene descritta la realtà del comprensorio apuo-versiliese, le cave e le tecnologie utilizzate per l’estrazione e le lavorazioni. Successivamente, viene presentata la regolamentazione europea e regionale sulla gestione e lo smaltimento dei rifiuti di cava, definiti rifiuti speciali. È stata presentata una breve sintesi delle regolamentazioni europee e regionali riguardanti l’attività estrattiva, con particolare riguardo alla problematica del trattamento dei rifiuti speciali dal punto di vista legislativo. Attraverso il caso della Cooperativa Apuana Vagli, si prende in esame uno studio reale dove analizzare le problematiche legate allo smaltimento dei rifiuti generati dall’attività estrattiva. Il materiale prodotto dai tagli dei blocchi in cava è stato campionato e sottoposto ad analisi granulometriche di laboratorio. Dai risultati è stato possibile ottenere le proprietà fisiche del materiale analizzato, grazie alle quali sono stati ipotizzati i possibili riutilizzi.

Avaliação das condições de iluminância das actividades de espeleólogos em ambiente de gruta

O objectivo deste estudo foi avaliar as condições de iluminância das actividades desenvolvidas por espeleólogos expostos a ambiente de grutas. Foi realizado um estudo descritivo transversal. Foram avaliados os níveis de iluminância das actividades desenvolvidas por 16 espeleólogos, em duas duas grutas desprovidas de iluminação natural. A idade média dos trabalhadores foi de 40,65 (±10,93) anos. No ambiente de gruta a maioria dos trabalhadores utilizava uma lanterna instalada no capacete (451,0±305,7lux). Não foram detectados sinais e sintomas de patologias visuais ligados à exposição do ambiente gruta. Os sinais de iluminância são adequados para a maioria das actividades realizadas.

The lives, acts, and martyrdoms, of the apostles of Our Saviour. To which are added lives of the evangelists, Mark and Luke.

Originally published (London, 1675) as Antiquitates apostolicae ... as a continuation of Antiquitates christianae by Jeremy Taylor. Later editions published with numerous variations in title.

Die cromerzeitlichen Bären aus der Einhornhöhle bei Scharzfeld

Up to now the bear remains from the "Einhornhöhle,, Cave near Scharzfeld at the foot of the Harz Mountains have been aseribed to the species "Ursus spelaeus" without undertaking comprehensive studies. Owing to an erroneous Classification of the gravel deposits covering part of the cave floor into the Middle Terrace of the Oder Rivulet, the fossil-bearing strata have been assigned to the Eemian Interglacial. RODE, who included a part of the Scharzfeld teeth in his treatise on teeth of the bears, has stated arctoidal features in their formation apart from certain specializations. He arrived at the conclusion that the Scharzfeld Bear differs more pronouncedly from all Central European Cave Bears he had investigated than the same differ from each other, and he named the Scharzfeld Bear: "Ursus spelaeus var. hercynica". The geological exploration of the Einhornhöhle Cave and of its environs carried out by DUPHORN in 196? resulted in the aforesaid gravels pertaining to a terrace of a Pre-Elster- Glaciation age; according to DUPHORN the fossil-bearing Sediments were deposited in a Pre-Elster-Glaciation ffarm- Climate Period. The very sparse aceompanying fauna does not contain any Stratigraphie key form; arctic elements and members of an interglacial forest fauna are missing. Its composition teils in favour of a dry, yet not too cool period of the Pleistocene, which is younger than the Villa- franchium. Consequently the cave must have been taken pos- session of for settling in the Cromerian Interglacial. The investigation of the bear remains has led to the result that, in all systematically .important teeth and skeleton characteristics, the Scharzfeld Bear shows either concor- dance with Ursus deningeri or greater analogy to the same than to Ursus spelaeus; in a few properties it even appears somewhat more primitive than Ursus deningeri. Therefore the bears of the Einhornhöhle Cave belong to the species "Ursus deningeri v. REICHENAU 1906". In the frontal teeth certain specializations occur. However, in view to the great varia- bility of the deningeri-"rassenkreis" there does not seem to be a justification for establishing a subspecies of its own. Whereas up to now nothing had been known in respect of the hibernation habits of Ursus deningeri, there has for the first time been furnished proof that an Ursus deningeri population had oecologically become "cave" bears. Consequently this specialization, as the onset and cause of which the Elster Glaciation was up to now considered, must already be originating in older cold epochs.

Pempheris vanicolensis (Cuvier, 1831)

Pempheris vanicolensis has reported for the first time from Persian Gulf (Kish Island). Various aspects of the biology of P. vanicolensis Cuvier & Valenciennes, a recent Lessepsian (Suez Canal) immigrant into the Mediterranean, are given. Red Sea and Mediterranean populations were compared, and the results indicate that the spawning season is shortened in the Mediterranean, continuing from April to September, as opposed to year-round in the Red Sea. Descriptions of a ripe ovary and post-larva from the Mediterranean are given. Individuals reach a mean size of 10.8 cm in their first year, and 14.4 cm in the second year. Little change has occurred in the diet of the immigrant population, and both populations feed nocturnally, chiefly on larval and adult stages of planktonic crustaceans. Direct underwater observations on the diurnal behavior of the species show that the fish leave their daytime cave shelter at sunset, congregate at a nearby site and then migrate inshore and disperse into small groups to feed. Before dawn, they reassemble at the cave's entrance, and finally enter it at sunrise, after the school has built up. Observations on Persian Gulf sweepers show that the fish are segregated into size groups, ranging 15–18 cm adults at depths of 3 m.

Achados arqueológicos : ossadas e restos cerâmicos

No ano de 1998, foi o signatário solicitado a dar parecer, no âmbito das funções atribuídas, a nível municipal, ao centro de Estudos Arqueológicos do Concelho de Oeiras/Câmara Municipal de Oeiras, sobre a descoberta fortuita de ossos supostamente humanos, aparecidos no decurso de obras de beneficiação na cave do edifício onde se encontra instalada a Biblioteca Operária Oeirense.

Vestígios paleontológicos do Algar da Manga Larga

O Algar da Manga Larga tem-se revelado uma das mais importantes cavidades verticais em Portugal e, apesar de ser já conhecido pelos espeleólogos desde há mais de trinta anos, continua a fornecer dados com relevante significado científico. No decurso de uma acção de pesquisa espeleológica promovida pela AESDA no referido Algar foi fotografado um conjunto de ossos de carnívoro, jacentes numa galeria a cerca de 95 metros abaixo da entrada da cavidade. As respectivas características morfológicas e biométricas indicavam tratar-se de um grande felídeo, remetendo para espécie actualmente extinta na Europa, nomeadamente o leopardo, Panthera pardus (L., 1758). A evidente importância paleontológica dos testemunhos ósseos levou a que se desencadeasse um conjunto de procedimentos com o objectivo de os salvaguardar adequadamente e de promover o seu estudo. Para esse efeito, realizaram-se os contactos necessários e procedeu-se ao registo e à recolha das peças em apreço atribuindo especial atenção à sua integridade e conservação. Seguiram-se as tarefas ligadas ao estudo biométrico comparativo dos restos osteológicos. A presença deste e outros vestígios faunísticos, nomeadamente de gato-bravo, em zonas profundas e de difícil acesso desta gruta, indiciam a existência de condutas que estão ou estiveram em contacto com o meio exterior, as quais não foram ainda referenciadas. Deste modo, para além do evidente interesse paleontológico da descoberta, é possível serem extrapoladas interpretações com aplicação no âmbito da exegese da própria cavidade, situação que levou já à descoberta de uma galeria não registada. Este trabalho tem vindo a ser amplamente divulgado junto da comunidade espeleológica nacional e internacional, inclusivamente no 14º Congresso Internacional de Espeleologia que se realizou em 2005 na Grécia. O estudo paleontológico está concluído e a aguardar publicação em revista da especialidade (CARDOSO & REGALA, no prelo).

O belo antro e a grande oliveira : recepções da alegoria da caverna na tradição neoplatônica

Desde a Magna Grécia de Pitágoras, Empédocles e Parmênides, passando pelas relações “perigosas” entre a sabedoria nascente e as tradições órfico-dionisíacas, em nítida continuidade com a mitologia arcaica e as narrativas teogônicas, dialogando com as práticas médicas asclepíades, a filosofia antiga visita cavernas. A caverna da República, uma das mais poderosas e fecundas alegorias do pensamento ocidental, é simultaneamente herdeira e ponto de fuga da longa trajetória dessa metáfora. Não se pretende aqui, no entanto, compreender a imagem platônica como a consumação de uma velha tradição filosófica que “pensa em cavernas”; procura-se, antes, iluminar essa alegoria com a interpretação oferecida pela filosofia acadêmica posterior. No Antro das Ninfas, Porfírio parte de 11 versos de Homero (Od. XIII, 102-112) para habilmente desenhar uma exegese inspirada na teoria platônica da alma. A lectio porfiriana permite sugerir que a imagem da caverna revela algo mais que uma simples alegoria literária. Ela dá prova da existência de relações dialógicas e circulares entre a filosofia platônica e o imaginário religioso popular do mundo antigo. _______________________________________________________________________________ ABSTRACT

Changes in the storage and sink of carbon dioxide in subsurface atmospheres controlled by climate-driven processes: the case of the Ojo Guareña karst system

A comprehensive environmental monitoring program was conducted in the Ojo Guareña cave system (Spain), one of the longest cave systems in Europe, to assess the magnitude of the spatiotemporal changes in carbon dioxide gas (CO2) in the cave–soil–atmosphere profile. The key climate-driven processes involved in gas exchange, primarily gas diffusion and cave ventilation due to advective forces, were characterized. The spatial distributions of both processes were described through measurements of CO2 and its carbon isotopic signal (δ13C[CO2]) from exterior, soil and cave air samples analyzed by cavity ring-down spectroscopy (CRDS). The trigger mechanisms of air advection (temperature or air density differences or barometric imbalances) were controlled by continuous logging systems. Radon monitoring was also used to characterize the changing airflow that results in a predictable seasonal or daily pattern of CO2 concentrations and its carbon isotopic signal. Large daily oscillations of CO2 levels, ranging from 680 to 1900 ppm day−1 on average, were registered during the daily oscillations of the exterior air temperature around the cave air temperature. These daily variations in CO2 concentration were unobservable once the outside air temperature was continuously below the cave temperature and a prevailing advective-renewal of cave air was established, such that the daily-averaged concentrations of CO2 reached minimum values close to atmospheric background. The daily pulses of CO2 and other tracer gases such as radon (222Rn) were smoothed in the inner cave locations, where fluctuation of both gases was primarily correlated with medium-term changes in air pressure. A pooled analysis of these data provided evidence that atmospheric air that is inhaled into dynamically ventilated caves can then return to the lower troposphere as CO2-rich cave air.