Incremental growth of the Patagonian Torres del Paine laccolith over 90 k.y.

The Miocene Paine Granite in the Torres del Paine Intrusive Complex, southern Chile, is an extraordinary example of an upper crustal mafic and granitic intrusion. The granite intruded as a series of three sheets, each one underplating the previous sheet along the top of the basal Paine Mafic Complex. High-precision U/Pb geochronology on single zircons using isotope dilution-thermal ionization mass spectrometry yields distinct ages of 12.59 +/- 0.02 Ma and 12.50 +/- 0.02 Ma, respectively, for the first and last sheet of the laccolith. This age relationship is consistent with field observations. The zircon ages define a time frame of 90 +/- 40 k.y. for the emplacement of a >2000-m-thick granite laccollith. These precise U-Pb zircon ages permit identification of the pulses in a 20 k.y. range. The data obtained for the Paine Granite fill the gap between 100 k.y. and 100-1000 yr pulses described in the literature for crustal magma chambers.

El mosaico de peces de La Pineda (Tarragona)

En el Museo Arqueológico Provincial de Tarragona se halla una interesante obra de la musivaria tarraconense, datada en el siglo III después de J. C. Este mosaico policromo, que en la primavera de 1960 fue trasladado del lugar en que se encontró e instalado en el Museo, ha sido poco divulgado. Está situado actualmente en la pared del final de las escaleras que conducen a los pisos altos, lo que dificulta su es tuda ; de todos modos, hemos procurado salvar este inconveniente con los medios a nuestro alcance.

Bandelettes de momies inscrites du Livre des Morts. Egyptien 90

Contient : Fragment a ; fragment b ; Fragment d ; Fragment c

Anàlisi multivariada craniomètrica de les poblacions catalano-balears del passat

S'ha portat a terme una analisi estadística de les dades craniometriques de les principals poblacions catalano-balears del passat, des de J'Edat del Bronze fins a l'Edat Mitjana, i posteriorment s'han integrat les poblacions en un context peninsular més ampli. S'han analitzalles relacions entre poblacions per mitja d'un analisi d'agrupament (cluster), emprant els algoritmes UPGMA i del "veí més proper" i la distancia euclídea al quadrat. Així mateix, s'ha realitzat un re-mostreig (bootstrap) per comprovar la robustes de les agrupacions obtingudes i un test de Mantel per comprovar el grau de concordan~a entre les poblacions femenines i masculines. Els resultats mostren que, a nivell peninsular, els Bascos són la població més diferenciada de la resta des d'un punt de vista morfologic, la qual cosa pot estar relacionada amb una major antiguitat d'aquesta població, potser present des de temps pre-neolítics. La segona font de variació peninsular la constitueixen dues poblacions amb possibles influencies foranies d'origen africa: jueus i musulmans. La resta de poblacions, incloent-hi les de Mallorca, són notablement homogenies a pesar de la seva heterogene'itat cultural, temporal i geogràtfica. Finalment, es conclou que no hi ha cap analisi estadística que objectivament recolzi I'existencia deIs tipus racials tradicionalmcnt descrits a la Península Iberica, i que responen a una visió tipologica i estatica de la diversitat humana.

Les restes humanes del jaciment epipaleolític de la Balma de Guilanyà (Navés, Solsonès)

Les restes humanes deIs períodes epipaleolític i mesolític estan pobrament representades a la Península Iberica, tot i que existeixen dos jaciments mesolítics excepcional s a Muge, Portugal (Moita do Sebastiao i Cabe~o da Arruda), amb uns 67 individus, i un altre de recentment excavat a Oliva (El Collado, Valencia), on s'han trobat uns 15 individus. EIs primers estan datats entre 7.240 i 6.300 a.P. (Ferreira 1994: 664-674), mentre que el darrer té una datació de 7.640-7.570 a.P (Aparicio 1989). Ambdós jaciments es troben en zones properes a estuaris de rius o a la costa, la qual cosa permetia 1'explotació intensiva de recursos marins molt variats. Aquest tipus d' economia condicionava un tipus de vida força sedentaria i a més a més, va permetre un increment en la densitat de població, que hauria tingut lloc probablement entre el 8.000-7.000 a.e. (Ferreira 1994: 664-674). A Catalunya, s'han excavat fins ara pocs jaciments importants d'aquests periodes (Martín y Vaquer 1995: 35-73), tots d'ells en zones d'interior i corresponents presumiblement a grups petits de caçadors-recol·lectors, força diferents dels posteriors assentaments humans més grans com Muge i Oliva. De tots aquests jaciments, només a la Balma de Guilanya (Naves, Solsones) s'han trobat restes humanes que es puguin atribuir sense cap mena de dubte als nivells epipaleolítics.

Frecuencias de trepanación en la Edad del Bronce

En un estudio osteológico de los restos humanos de la Edad del Bronce de Cataluña se ha puesto de manifiesto la existencia, en esta época, de un suave y gradual proceso de difusión racial a lo largo del litoral noroeste del Mediterráneo, así como las influencias que éste ha tenido en el área catalana, donde aparece un elemento foráneo, de origen centroeuropeo, minoritario, localizado fundamentalmente en Solsona y de modo particular en tres yacimientos muy cercanos entre sí: los megalitos de El Collet, Clara y la cueva sepulcral de AigüesVives (fig. 1). Este aporte foráneo, relacionado sin duda con las prospecciones de metal y objetos de origen transpirenaico como la cerámica de apéndice de botón, aparece asentado en la zona reutilizando los sepulcros y mezclado con la población indígena, según muestran las abundantes formas de tránsito (Turbón, 1977, págs. 132, 340, 418 Y 326).

Friday Facts, February 25, 2011, Vol. 90

Bureau of Nutrition and Health Promotion part of the Iowa Department of Public Health produces of weekly newsletter about the Iowa WIC Program for the State of Iowa citizen.

Follicular lymphoma at relapse after rituximab containing regimens: comparison of time to event intervals prior to and after (90) Y-ibritumomab-tiuxetan.

Radioimmunotherapies with Zevalin® (RIT-Z) showed encouraging results in patients with relapsed/refractory follicular lymphoma (FL), leading frequently to failure-free intervals longer than those achieved by the last previous therapy. We compared time-to-event variables obtained before and after RIT-Z in patients with relapsed FL, previously exposed to rituximab. All patients with relapsed non-transformed, non-refractory, non-rituximab-naïve FL who have been treated with RIT-Z in two different centres in Europe were included. Staging and response were assessed by contrast-enhanced CT in all patients; PET/CT was performed according to local availability. Event-free survival (EFS) and time to next treatment (TTNT) following the last previous therapy and after RIT-Z were compared. Pre-therapy characteristics were tested in univariate analyses for prediction of outcomes. A description of the patterns of relapse was also provided. Among 70 patients treated, only 16 fulfilled the inclusion criteria. They were treated with a median of 3 prior lines of chemo-immunotherapies, including a median of 2 rituximab-containing regimens; 6 patients had undergone myeloablative chemotherapy with autologous stem cell rescue (ASCT). Overall response rates were 10 (62%) CR/CRu, 3 (19%) PR and 3 (19%) PD; response rates were similar in patients with prior ASCT. After RIT-Z only few patients obtained EFS and TTNT longer than after the last previous therapy. All four patients receiving rituximab maintenance were without progression 12 months after RIT-Z. Relapses occurred in both previously and newly involved sites; a significant association was found between the number of pathologic sites involved prior to RIT-Z and subsequent TTNT. Despite the excellent response rate, the duration of response was shorter than the previous one confirming the known trend of relapses to occur earlier after subsequent treatments. Rituximab maintenance after RIT-Z showed encouraging results in terms of prolonging EFS, warranting further studies. Copyright © 2010 John Wiley & Sons, Ltd.

Dating human skeletal remains using a radiometric method: Biogenic versus diagenetic (90)Sr and (210)Pb in vertebrae.

In forensic science, there is a strong interest in determining the post-mortem interval (PMI) of human skeletal remains up to 50 years after death. Currently, there are no reliable methods to resolve PMI, the determination of which relies almost exclusively on the experience of the investigating expert. Here we measured (90)Sr and (210)Pb ((210)Po) incorporated into bones through a biogenic process as indicators of the time elapsed since death. We hypothesised that the activity of radionuclides incorporated into trabecular bone will more accurately match the activity in the environment and the food chain at the time of death than the activity in cortical bone because of a higher remodelling rate. We found that determining (90)Sr can yield reliable PMI estimates as long as a calibration curve exists for (90)Sr covering the studied area and the last 50 years. We also found that adding the activity of (210)Po, a proxy for naturally occurring (210)Pb incorporated through ingestion, to the (90)Sr dating increases the reliability of the PMI value. Our results also show that trabecular bone is subject to both (90)Sr and (210)Po diagenesis. Accordingly, we used a solubility profile method to determine the biogenic radionuclide only, and we are proposing a new method of bone decontamination to be used prior to (90)Sr and (210)Pb dating.