Notas sobre la lengua guaymí en Costa Rica

Como aproximación panorámica al estudio actual del guaymí, una de las lenguas de la familia chibcha, es un análisis introductorio de los rasgos gramaticales y tipológicos generales de esa lengua. Previa información de índole antropológica e histórico-cultural, se exponen en forma analítica aspectos sintácticos, sobre la frase verbal, el morfema de negación, el de reflexivización, los sujetos dativos, los objetos directos. Señala algunas tareas pendientes, que suponen un estudio más pormenorizado y extendido.Providing a panoramic view of the present studies of the Guaymí language, one of the Chibchan languages, this is an introductory analysis of the general grammatical and typological features of that language. First, information is given on anthropological, historical and cultural aspects. Then syntactic features are described for the verb phrase, the morpheme for negation, reflexive forms, dative subjects and direct objects. Mention is made of pending tasks requiring a broader and more detailed study.

From the Humpata Plateau to Namibe Desert, SW Angola

After the Congress, a six-day field trip, will be held through three southwestern provinces of Angola (Huíla, Namibe and Cunene), every day starting and ending in the city of Lubango, for overnight stay in Lubango, with the purpose to observe some of the main sites of geological interest in this zone of Angola. The itinerary of this field trip presents the geologic history of Southwestern Angola and its evolution in the scope of the Congo Craton, through a trip that begins in the first excursion days by the oldest geologic formations and phenomena until the recent geologic formations and phenomena on the last excursion days. On the first and second excursion days, September 5th and September 6th, the field trip will go along the Kunene Anorthosite Complex of Angola (KAC), to observe some petrographic features of the KAC that are important to understand the emplacement of this huge igneous massif of the early Kibarean age. These days of the field trip allow the observation of Earthen Construction, because this region of Cunene is privileged to appreciate a kind of Eco-construction, made of raw earth and in wattle and daub, built with ancient techniques, which constitute a real GeoHeritage. On September 7th, in the morning, the destination will be Tundavala, to visit Tundavala Gap, a huge escarpment of more than 1,000 m high cutted in Neo-Archean and Paleo-Proterozoic igneous rocks, the Ruins of Tundavala (quartzite blocks with sedimentary structures) and Tundavala Waterfalls on a quartzitic scarp. After lunch, the field trip continues towards Humpata plateau to observe the panoramic view over Lubango city from the Statue of Cristo Rei, then the outcrops of dolomitic limestones with stromatolites and dolerites and finally the Leba passage, a huge escarpment and one of the most spectacular parts of the Serra da Chela, traversed by a mountain road built in the early 70s of the last century, that can be observed from the belvedere of the Serra da Chela. On September 8th, the destination is the carbonatite complexes of Tchivira and Bonga, belonging to the Mesozoic alkaline massifs of ultrabasic rocks, a rift valley system that occurs during the Early Cretaceous. In this forth excursion day, due to the huge dimensions of these two carbonatite structures it will be visited, only, the Complex of Bonga, namely the outcrops of the northern part of the structure and secondary deposits on the boundary on the southern part of the of the Complex. The last two excursion days, September 9th and September 10th, are to observe the Cretaceous Basin of Namibe. On September 9th, the northern part of Namibe Basin will be visited to observe the volcanic basic rocks of Namibe as well as the interesting paleontological site of Bentiaba. On September 10th, the destination is the southern and more recent part of Namibe Basin, where on the Namib Desert, the exotic plant Welwitschia mirabilis can be observed, as well as Arco, an oasis in the desert. This last excursion day, ends up at the dunes of Tombwa near the mouth of Curoca river and the beautiful bay of Tombwa, where can be observed heavy minerals in their beach sands.

Ecografia con mezzo di contrasto dalla ricerca alla pratica clinica: diagnosi di carcinoma epatocellulare con sistema CEUS LI-RADS e con software di quantificazione della perfusione tissutale

Il carcinoma epatocellulare (HCC) rappresenta il tumore epatico primitivo più comune con una incidenza fino all’85%. È uno dei tumori più frequenti al mondo ed è noto per l’elevata letalità soprattutto in stadio avanzato. La diagnosi precoce attraverso la sorveglianza ecografica è necessaria per migliorare la sopravvivenza dei pazienti a rischio. Il mezzo di contrasto ecografico migliora la sensibilità e la specificità diagnostica dell’ecografia convenzionale. L’ecografia con mezzo di contrasto (contrast-enhanced ultrasound, CEUS) è pertanto considerata una metodica valida per la diagnosi di HCC a livello globale per la sua ottima specificità anche a fronte di una sensibilità subottimale. L’aspetto contrastografico delle lesioni focali epatiche ha portato un team di esperti allo sviluppo del sistema Liver Imaging Reporting and Data System (LI-RADS) con l’obiettivo di standardizzare la raccolta dati e la refertazione delle metodiche di imaging per la diagnosi di HCC. La CEUS è una metodica operatore-dipendente e le discordanze diagnostiche con gli imaging panoramici lasciano spazio a nuove tecniche (Dynamic Contrast Enhanced UltraSound, DCE-US) volte a migliorare l’accuratezza diagnostica della metodica e in particolare la sensibilità. Un software di quantificazione della perfusione tissutale potrebbe essere di aiuto nella pratica clinica per individuare il wash-out non visibile anche all’occhio dell’operatore più esperto. Il nostro studio ha due obiettivi: 1) validare il sistema CEUS LI-RADS nella diagnosi di carcinoma epatocellulare in pazienti ad alto rischio di HCC usando come gold-standard l’istologia quando disponibile oppure metodiche di imaging radiologico accettate da tutte le linee guida (tomografia computerizzata o risonanza magnetica con aspetto tipico) eseguite entro quattro settimane dalla CEUS; 2) valutare l’efficacia di un software di quantificazione della perfusione tissutale nel riscontro di wash-out per la diagnosi di HCC in CEUS.