Genesis of self-organized zebra textures in burial dolomites: Displacive veins, induced stress, and dolomitization

The dolomite veins making up rhythmites common in burial dolomites are not cement infillings of supposed cavities, as in the prevailing view, but are instead displacive veins, veins that pushed aside the host dolostone as they grew. Evidence that the veins are displacive includes a) small transform-fault-like displacements that could not have taken place if the veins were passive cements, and b) stylolites in host rock that formed as the veins grew in order to compensate for the volume added by the veins. Each zebra vein consists of crystals that grow inward from both sides, and displaces its walls via the local induced stress generated by the crystal growth itself. The petrographic criterion used in recent literature to interpret zebra veins in dolomites as cements - namely, that euhedral crystals can grow only in a prior void - disregards evidence to the contrary. The idea that flat voids did form in dolostones is incompatible with the observed optical continuity between the saddle dolomite euhedra of a vein and the replacive dolomite crystals of the host. The induced stress is also the key to the self-organization of zebra veins: In a set of many incipient, randomly-spaced, parallel veins just starting to grow in a host dolostone, each vein¿s induced stress prevents too-close neighbor veins from nucleating, or redissolves them by pressure-solution. The veins that survive this triage are those just outside their neighbors¿s induced stress haloes, now forming a set of equidistant veins, as observed.

Self-accelerating dolomite-for-calcite replacement: Self-organized dynamics of burial dolomitization and associated mineralization

A new dynamic model of dolomitization predicts a multitude of textural, paragenetic, geochemical and other properties of burial dolomites. The model is based on two postulates, (1) that the dolomitizing brine is Mg-rich but under saturated with both calcite and dolomite, and (2) that the dolomite-for-calcite replacement happens not by dissolution-precipitation as usually assumed, but by dolomite-growth-driven pressure solution of the calcite host. Crucially, the dolomite-for-calcite replacement turns out to be self-accelerating via Ca2 : the Ca2 released by each replacement increment accelerates the rate of the next, and so on. As a result, both pore-fluid Ca2 and replacement rate grow exponentially.

Implications of burial alterations on luminescence dating of archaeological ceramics

Recent mineralogical studies on archaeological pottery samples report significant variations in alkali metal concentrations due to environmental alterations during burial. Here we examine the effects of potassium (K) leaching on luminescence dating. The effect on the estimation of the dose rate is studied by considering four models of leaching (exponential, linear, early and late) and their impact on fine- and coarse-grain dating are calculated. The modeling approaches are applied to two cases of pottery in which evidence for alteration was found. Additionally, TL dating performed on pottery of one of the studied cases, indicates the importance of leaching effects on absolute dating measurements.

Impacte visual aeri a Argentona

Treball de recerca realitzat per un alumne d'ensenyament secundari i guardonat amb un Premi CIRIT per fomentar l'esperit cientí­fic del Jovent l'any 2009. Aquest treball té com a finalitat millorar l'entorn aeri d'Argentona, un poble situat a la comarca del Maresme. Els elements que creen més impacte visual aeri són les antenes en desús i el cablejat no soterrat. S'han buscat propostes per canviar aquesta situació: la retirada de les antenes, aprofitant l'arribada de la TDT, i el soterrament del cablejat aeri. Donat que ambdues accions afectarien al municipi i a la seva població, s'ha considerat necessari incloure una enquesta, per a conèixer l'opinió dels argentonins, i dues entrevistes, a l'alcalde i a l'enginyer municipal, per conèixer la postura oficial.

Adéu, Guau!

Treball de recerca realitzat per alumnes d'ensenyament secundari i guardonat amb un Premi CIRIT per fomentar l'esperit científic del Jovent l'any 2009. Aquest treball és una creació d’un projecte empresarial, per tal d’analitzar la viabilitat, examinar els objectius i descobrir els inconvenients de la creació d’una empresa. En aquest cas es tracta de crear un cementiri i vetlla d’animals de tot tipus, simulant el comiat que es realitza a les persones estimades, però destinat a les nostres mascotes, amb un servei de qualitat, serietat, responsabilitat i adequat als usuaris i clients. Es tracta d’una empresa que s’encarregarà de la recollida de l’animal, l’acondicionament per a la vetlla, la cerimònia de comiat, la impressió dels panegírics, l’obtenció d’objectes per recordar-ho, les decoracions florals o similars, la venta de plaquetes, tombes, gerros... segons el tipus de mètode seleccionat per a l’enterrament, així com la prestació d altres serveis addicionals que s’adaptin a les necessitats específiques dels usuaris/clients per tal de cobrir la demanda actual al sector. Es tracta d’una iniciativa destinada a les persones que necessiten desprendre s de les restes de les seves mascotes, després de la seva defunció, que volen oferir un comiat proper i afectuós a les seves mascotes.

Magnetization reversal and magnetic anisotropies in epitaxial Fe/MgO and Fe/MgO/Fe heterostructures grown on Si(001)

Epitaxial Fe/MgO heterostructures have been grown on Si(001) by a combination of sputtering and laser ablation deposition techniques. The growth of MgO on Si(001) is mainly determined by the nature of the interface, with large lattice mismatch and the presence of an amorphous layer of unclear origin. Reflection high energy electron diffraction patterns of this MgO buffer layer are characteristic of an epitaxial, but disordered, structure. The structural quality of subsequent Fe and MgO layers continuously improves due to the better lattice match and the burial of defects. A weak uniaxial in-plane magnetic anisotropy is found superimposed on the expected cubic biaxial anisotropy. This additional anisotropy, of interfacial nature and often found in Fe/MgO and Fe/MgO/GaAs(001) systems, is less intense here due to the poorer MgO/Si interface quality compared with that of other systems. From the evolution of the anisotropy field with film thickness, magnetic anisotropy is also found to depend on the crystal quality. Kerr measurements of a Fe/MgO multilayered structure grown on Si show two different switching fields, suggesting magnetic coupling of two of the three Fe layers. Nevertheless, due to the little sensitivity to the bottom Fe film, independent switching of the three layers cannot be ruled out.

A contribution to the study of post-depositional alterations of pottery using TL dating analysis

In luminescence dating, the potassium concentration significantly contributes to the dose rate value in the age estimation. Within this study, fine-grain thermoluminescence dating has been applied on sherds of calcareous pottery of known age, excavated at a Roman site in Mallorca, Spain. For those of the samples that showed signs of severe potassium leaching, according to chemical and mineralogical examination, the thermoluminescence analysis provided overestimated dates. By using the known archaeological age of the samples, a corrected dose rate value can be estimated which provides the potassium concentration averaged for the burial period. Finally, a step-like model can then be used to estimate the fraction of the burial period after which most of the alteration effects took place.

Coastal salina evaporites of the Triassic-Liassic boundary in the Iberian Peninsula: the Alacón borehole

The evaporite unit (the Lécera Formation), which was formed at the Triassic¿Liassic boundary in the Aragonian Branch of the Iberian Chain, was studied at the 01 Alacón borehole (Alacón village, Teruel province), where it is mainly constituted by a thick (>e and reflect deeper water settings, whereas in the upper part they correspond to shallower water settings. The evaporite sedimentation mainly occurred in a subsiding coastal basin of the salina or lagoon type. In this setting, the subaqueous precipitation of the carbonate and gypsum lithofacies was followed, in each cycle, by the interstitial growth of anhydrite in exposed conditions. As a whole, the evaporite succession reflects an infilling process. The conversion into anhydrite of the selenitic gypsum -probably also of the rest of depositional gypsum lithofaciesstarted under synsedimentary conditions and followed during shallow to moderate burial diagenesis.

Large gypsum nodules in the Paleogene and Neogene evaporites of Spain: distribution and palaeogeographic significance

Sabkha and deep burial set tings are the most com mon sites where diagenetic anhydrite forms. In a sabkha setting, displacive facies (iso lated nodules, bed ded nodules, enterolithic levels) of early diagenetic or primary anhydrite are generated (Shearman, 1966; Hardie, 1967). These anhydrite facies are commonly foundat the top of shoal ing cycles representing the evolution from subaqueous depositional conditions at the base (carbonates, lutites) to exposure conditions at the top where in ter stitially-grown gypsum/anhydrite de velops ( sabkha cy cles). In a deep burial setting, gypsum transforms to tally to anhydrite with in creas ing temperature and lithostatic pressure (Murray, 1964). Al though this mineral transformation usually preserves the depositional gypsum facies, a significant textural change is in volved in other cases, resulting in replacive anhydrite with a nodular-mosaic or"chicken-wire" fabric (Warren, 2006). In the two settings, how ever, the size of the individual anhydrite nodules is relatively small, rarely reaching some tens of centimetres across. More over, bedding is preserved or little disturbed, al though minor de formation is caused by the displacive sabkha nodules.

Las necrópolis protohistóricas tumulares de Cataluña meridional: el ejemplo de Sebes (Flix, Tarragona)

Se presentan los resultados de las recientes intervenciones arqueológicas realizadas en la necrópolis del Hierro I de Sebes (Flix, Tarragona). Se ha precisado la extensión de la necrópolis, su duración, los rituales funerarios y la estructura social de la población mediante técnicas y métodos de carácter interdisciplinar (antropología, carbono 14, prospecciones geofísicas…). Se ha constatado la coexistencia de túmulos y urnas y la agrupación de las estructuras en dos áreas. Sobre esta base se pretende mejorar el conocimiento de las necrópolis de cremación en un territorio de contacto entre diferentes tradiciones de enterramiento. Se dan a conocer datos inéditos procedentes del estudio antropológico de los huesos cremados de Sebes y de las dataciones radiocarbónicas de algunos de ellos. Estos datos, considerados en conjunto con los del resto de la necrópolis, permiten relacionarla más con las necrópolis tumulares leridanas que con las del Bajo Aragón - Terra Alta.

Novedades sobre el mundo funerario en la Ribera d’Ebre

La excavación de las necrópolis de incineración de Santa Madrona (Riba-roja d’Ebre) y Sebes (Flix) aportan nuevos datos sobre el estudio del mundo funerario en esta zona. Ambas presentan una fase de utilización durante la Primera Edad del Hierro (siglos vii-vi a.C.), caracterizada por un predominio de estructuras tumulares, junto a las que se documentan otras variantes (urnas funerarias sin túmulo, deposiciones de huesos sin urna, ofrendas funerarias, estructuras empedradas sin urna, etc.). En ambas necrópolis, los estudios antropológicos muestran que todos los grupos de edad estaban representados. Los materiales cerámicos y ajuares presentan gran similitud entre las diferentes sepulturas, lo que sugiere una cierta igualdad en el tratamiento de los difuntos. La existencia, en ambos casos, de dos áreas diferenciadas, podría indicar una separación en función de grupos familiares.

La necròpolis protohistòrica de Sebes (Flix, Ribera d'Ebre)

The archaeological research carried out between 2005 and 2008 at the site of Sebes (Flix, Tarragona) has identified an habitat of the early Iron Age and a contemporary burial site. In general the interrements are secondary cremations buried under circular tumuli. We focus on the first results of these interventions, as well as on the paleoanthropological analyses, the radiocarbon datings and the geophysical surveys.

Detection of Body Dump Sites and Clandestine Burials: a GIS-Based Landscape Approach

Forensic archaeology has been of inestimable help in the location and excavation of clandestine burials (Hunter 1996a:16-17, 1996b; Killam 2004; Levine et al. 1984). Landscape archaeology techniques have been adapted and widely applied for such purposes. In this article, an adaptation of one of the most common applications of archaeological GIS, that is predictive site location, is applied to the detection of body dump sites and clandestine burial sites, bringing together in the process the fields of landscape archaeology, forensic sciences, and GIS.

Modelling leaf development in Oxalis latifolia

This study was carried to develop functions that could explain the growth of Oxalis latifolia, in both early stages and throughout the season, contributing to the improvement of its cultural control. Bulbs of the Cornwall form of O. latifolia were buried at 1 and 8 cm in March 1999 and 2000. Samples were destructive at fixed times, and at each time the corresponding BBCH scale codes as well as the absolute number of growing and adult leaves were noted. Using the absolute number of adult leaves (transformed to percentages), a Gaussian curve of three parameters that explains the growth during the season (R2=0.9355) was developed. The BBCH scale permitted the fit of two regression lines that were accurately adjusted for each burial depth (R2=0.9969 and R2=0.9930 respectively for 1 and 8 cm). The best moment for an early defoliation in Northern Spain could be calculated with these regression lines, and was found to be the second week of May. In addition, it was observed that a burial depth of 8 cm does not affect the growing pattern of the weed, but it affects the number of leaves they produce, which decreases to less than a half of those produced at 1 cm.

El ritual funerari a la necròpolis del Coll del Moro, Gandesa (Terra Alta)

One of the five burials excavated in 1984 at the necropolis of Coll del Moro in Gandesa (Terra Alta-Tarragona) bore evidence of primary cremations. The tomb, a tumulus, yielded a cremation burial with a pottery urn and other vessels as funerary offerings. The chamber of the grave also contained bronze jewellery, basically bracelets. It is interesting to notice that the dead were cremated in the same place where the tomb was built. The complexity of the burial rite and the magnitude of some of the tumuli indicated a social structure consolidated with different grades of authority. We date these burials in the late Hallstatt but there is already evidence of commercial trade with punic people who arrived at the east coast in the second half of the seventh century BC and, from there, reached inland sites on the Ebro river and its afluents.