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| 1 | 内脏脂肪组织通过产生骨桥蛋白调控成纤维细胞衰老促进心脏衰老显示文摘老化通过增加包括骨桥蛋白(osteopontin,OPN)在内的细胞外基质(extracellular matrix,ECM)蛋白的沉积引起心脏结构和功能改变进而导致进行性间质纤维化。虽然已知OPN参与各种病理状况,但其在心肌衰老中的作用仍不清楚。 | Sawaki D Czibik G Pini M Ternacle J Suffee N Mercedes R Marcelin G Surenaud M Marcos E Gual P Clément K Hue S Adnot S Hatem SN Tsuchimochi I Yoshimitsu T Hénégar C Derumeaux G 刘青 叶鹏 | 2018 | 中华高血压杂志2018，26，3： | 14 |
| 2 | Chronic intestinal pseudo-obstruction in patients with systemic lupus erythematosus: report of four cases显示文摘 | Federico Ceccato Adrián Salas Vanina Góngora Santiago Ruta Susana Roverano Juan Carlos Marcos Mercedes Garcìa Sergio Paira | 2008 | Clinical Rheumatology2008，，3： | 2 |
| 3 | Chiral codendrimers derived from poly (propyleneimine) dendrimers (DAB)显示文摘 | Jose Luis Serrano Mercedes Marcos Rafael Martin | 2003 | Chem Mater2003，15，20： | 1 |
| 4 | Melanocortin 1 receptor is expressed by uveal malignant melanoma and can be considered a new target for diagnosis and immunotherapy 显示文摘 | MERCEDES N L CRISTIAN P MARCOS R | 2007 | Invest Ophthalmol- VisSci2007，48，3： | 1 |
| 5 | Bis(salicylaldiminate) copper(II) and palladium(II) complexes: towards columnar mesophases显示文摘 | Joaquin Barbera Raquel Gimenez Nelida Gimeno Mercedes Marcos Maria Del Carmen Pina Jose Luis Serrano | 2003 | Liquid Crystals2003，，6： | 1 |
| 6 | SARS-CoV-2 infection in children requiring hospitalization: the experience of Navarra, Spain显示文摘Background Coronavirus disease 2019 in children,or pediatric COVID-19,initially was described as an acute respiratory syndrome similar to the adult presentation but with less severe manifestations.Methods We describe the clinical characteristics,disease presentation,treatments and outcomes of all pediatric cases with COVID-19 admitted to the reference hospitals in Navarra,Spain during the first wave of the COVID-19 outbreak(February-May 2020).Results We found a low number of hospitalized cases in infants and children compared to adults with a hospitalization ratio of 1:180.Most of these hospitalized cases did not suffer from severe disease.Over 80%of infections reported household contacts,and the mother was the known-contact in 83%of these cases.72%of hospitalized cases were previously healthy children.We describe how symptoms in pediatric cases are nonspecific and how COVID-19 can be presented with a wide range and variety of symptoms.Respiratory symptoms are not always present,and severe neurological and cardiac features can occur in previously healthy children.Conclusion Epidemiological description and case reports will be key to a better recognition and to adequate treatment of pediatric patients with COVID-19. | Laura Moreno-Galarraga Maria Urretavizcaya-Martinez Josune Alegria Echauri Marcos Garcia Howard Eva Ruperez Garcia Sergio Aguilera-Albesa Valentin Alzina de Aguilar Mercedes Herranz Aguirre | 2020 | World Journal of Pediatrics2020，16，6： | 1 |
| 7 | The Puesto Piris Formation: Evidence of basin-development in the North Patagonian Massif during crustal extension associated with Gondwana breakup显示文摘The Marifil Volcanic Complex, exposed in the eastern North Patagonian Massif, Argentina, includes up to 550 m of red conglomerates, sandstones, black siltstones, limestones, and reworked tuff of the Puesto Piris Formation. The basal part of this unit, which was deposited in high-gradient topographic relief, is composed of conglomerates and sandstones with thin layers of reworked tuffs. The lithofacies associations of the basal part indicate that the depositional mechanisms were mantled and gravitational flows.The middle part of the unit consists of fine sandstones, limestones, and black siltstones that were deposited in low-energy fluvial and lacustrine environments. The outcrops are located along the NEe SW direction and the major thickest units represented by limestones and siltstones, occur near the southeastern border of this NEeS W depocenter. Since the rhyolitic and trachytic lava flows and tuffs of the Marifil Volcanic Complex are interbedded with the sedimentary sequences of the Puesto Piris Formation,both units are coeval. Zircon Ue Pb age was obtained for a trachytic lava flow(193.4 ±3.1 Ma) suggesting that sedimentation and volcanism are Sinemurian. This extensional episode was recorded in the eastern,western, and southwestern sectors of the North Patagonian Massif, and is possibly associated with the Gondwana supercontinent breakup. | Leonardo Strazzere Daniel A.Gregori Leonardo Benedini Paulo Marcos Mercedes V.Barros Mauro C.Geraldes Cecilia Pavon Pivetta | 2019 | Geoscience Frontiers2019，10，1： | 1 |
| 8 | Pennsylvanian glacimarine sedimentation in the Cushamen Formation,western North Patagonian Massif显示文摘The metasedimentary sequence of the Cushamen Formation in the western North Patagonian Massif is540 m thick and comprises six sedimentary lithofacies associations related to a glacimarine environment.Four of these lithofacies represent distal glacimarine environments, whereas another one was deposited in proximal glacimarine environments, and the last includes subglacial environments. The organization and configuration of these lithofacies associations represent the advance and retreat of the glacier masses. The maximum glacial advance is correlatable with the G2 glacial interval of the Pennsylvanian Pampa de Tepuel, Las Salinas and Valley Chico, formations of the Extraandean Chubut, and the southern part of Neuquen Cordillera. Contemporaneously, in southern Chile there are marine and glacimarine sediments. The chronostratigraphic relationships between the Silurian to Permian units allow five paleogeographic stages to be distinguished. The middle Silurian-late Devonian igneous rocks represent the first magmatic stage. The second stage, which is transitional to the first, is represented by a marine basin that includes the late Devonian-early Carboniferous Esquel and Rio Pescado formations and the Llanquihue Complex. The third stage(early-late Carboniferous) includes granitoids of the second magmatic event that partially overlapped the first magmatic igneous belt. The fourth stage belongs to the late Carboniferous sedimentation of the Cushamen and equivalent formations. The extended early Permian magmatism was the last Paleozoic event in the studied area. | Paulo Marcos Daniel A.Gregori Leonardo Benedini Mercedes Barros Leonardo Strazzere Cecilia Pavón Pivetta | 2018 | Geoscience Frontiers2018，9，2： | 0 |
| 9 | 重叠——2020年阿根廷Hello Wood建造节显示文摘在阿根廷举办的2020年Hello Wood国际夏季建造节已圆满落幕。Hello Wood是一个以建筑搭建为主题的活动,在过去的几年中,已赢得了一系列国际著名建筑事务所的关注,如来自苏黎世的Urban Think-Tank和日本的隈研吾建筑都市设计事务所等。至此,该活动位于布达佩斯的主办方终于可以自豪地宣布,这个夏季大学生实体搭建活动及其教学理念已经在全球传播开来。四年以来,Hello Wood的阿根廷主办方MANDARINA和TACADI事务所沿袭匈牙利的模式,多次组织了Hello Wood Argentina的活动。 | Bea Palacio Mercedes Palacio Jeronimo Fanelli Marcos Llerena Andras Huszar Peter Pozsar David Raday Krisztian Toth Pedro Scarpaci(摄影) 范嘉苑(编译) | 2020 | 现代装饰2020，，8： | 0 |
| 10 | Characterization of Arroyo Verde Epithermal Deposit:Paragenesis,Mineral Geochemistry,Geochronology and Fluid Inclusions in Lower Chon Aike Volcanism,Argentina显示文摘Arroyo Verde epithermal deposit,in the North Patagonia region of Argentina,is located within the Lower Chon Aike volcanism and is developed between 192.6±2.5 Ma(mineralization host rock)and 189.5±2.6 Ma(overlying lava).Marifil volcanic complex is the host rock for these veins,veinlets and breccias.This particular small deposit has developed low to intermediate sulphidation characteristics,with gangue mineral textures associated with several ore minerals.Electron probe microanalysis determines electrum,silver minerals such as acanthite,and tetrahedrite,related Ag-Cu minerals like jalpaite,mckinstryite,stromeyerite,and base metals like chalcopyrite,sphalerite,galena and pyrite.Fluid inclusions in quartz of two out of five events indicate that these Low Jurassic veins were formed due to subtle boiling and dilution mechanisms and by low-salinity(3.4 wt.%to 6.7 wt.%NaCl Eq)magmatic-hydrothermal fluid at 225 to 310℃.The fluid inclusion measurements that indicate boiling(Event 3)were plotted,and based on this data,we interpret that the Arroyo Verde deposit has been eroded between 550 and 700 m.This particular character has not been previously recorded for other sectors of the eastern north Patagonian region. | Cecilia Pavón Pivetta Leonardo Benedini Paulo Marcos Ma.Agustina Cócola Mercedes Virginia Barros Daniel Gregori Leonardo Strazzere Anderson Costa dos Santos Mauro C.Geraldes | 2024 | Journal of Earth Science2024，35，1： | 0 |
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