567 resultados para Tibetan Mastiff


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This study reports on the occurrence of Molossus coibensis J. A. Allen, 1904, in the Brazilian Amazon and the second record of this species from Brazil. It also presents a comparative analysis with other two small-bodied Molossus species that occur in Brazil: M. molossus (Pallas, 1766) and M. aztecus Saussure, 1860. The report is based on 8 females captured in urban areas of the city of Bragança, in the northern Brazilian state of Pará. Morphometric data and the qualitative comparison of morphological features permitted the identification of the specimens as M. coibensis, hitherto known only in Tapirapoan, in the southwestern state of Mato Grosso, west-central Brazil. © SAREM, 2013.

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Within a community, species may germinate at different times so as to mitigate competition and to take advantage of different aspects of the seasonal environment (temporal niche differentiation). We illustrated a hypothesis of the combined effects of abiotic and biotic competitive factors on germination timing and the subsequent upscale effects on community assembly. We estimated the germination timing (GT) for 476 angiosperm species of the eastern Tibetan Plateau grasslands under two light treatments in the field: high (i.e. natural) light and low light. We also measured the shift in germination timing (SGT) across treatments for all species. Furthermore, we used phylogenetic comparative methods to test if GT and SGT were associated with seed mass, an important factor in competitive interactions. We found a significant positive correlation between GT and seed mass in both light treatments. Additionally, small seeds (early germinating seeds) tended to germinate later and large seeds (late germinating seeds) tended to germinate earlier under low light vs high light conditions. Low light availability can reduce temporal niche differentiation by increasing the overlap in germination time between small and large seeds. In turn, reduced temporal niche differentiation may increase competition in the process of community assembly.

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Curved mountain belts have always fascinated geologists and geophysicists because of their peculiar structural setting and geodynamic mechanisms of formation. The need of studying orogenic bends arises from the numerous questions to which geologists and geophysicists have tried to answer to during the last two decades, such as: what are the mechanisms governing orogenic bends formation? Why do they form? Do they develop in particular geological conditions? And if so, what are the most favorable conditions? What are their relationships with the deformational history of the belt? Why is the shape of arcuate orogens in many parts of the Earth so different? What are the factors controlling the shape of orogenic bends? Paleomagnetism demonstrated to be one of the most effective techniques in order to document the deformation of a curved belt through the determination of vertical axis rotations. In fact, the pattern of rotations within a curved belt can reveal the occurrence of a bending, and its timing. Nevertheless, paleomagnetic data alone are not sufficient to constrain the tectonic evolution of a curved belt. Usually, structural analysis integrates paleomagnetic data, in defining the kinematics of a belt through kinematic indicators on brittle fault planes (i.e., slickensides, mineral fibers growth, SC-structures). My research program has been focused on the study of curved mountain belts through paleomagnetism, in order to define their kinematics, timing, and mechanisms of formation. Structural analysis, performed only in some regions, supported and integrated paleomagnetic data. In particular, three arcuate orogenic systems have been investigated: the Western Alpine Arc (NW Italy), the Bolivian Orocline (Central Andes, NW Argentina), and the Patagonian Orocline (Tierra del Fuego, southern Argentina). The bending of the Western Alpine Arc has been investigated so far using different approaches, though few based on reliable paleomagnetic data. Results from our paleomagnetic study carried out in the Tertiary Piedmont Basin, located on top of Alpine nappes, indicate that the Western Alpine Arc is a primary bend that has been subsequently tightened by further ~50° during Aquitanian-Serravallian times (23-12 Ma). This mid-Miocene oroclinal bending, superimposing onto a pre-existing Eocene nonrotational arc, is the result of a composite geodynamic mechanism, where slab rollback, mantle flows, and rotating thrust emplacement are intimately linked. Relying on our paleomagnetic and structural evidence, the Bolivian Orocline can be considered as a progressive bend, whose formation has been driven by the along-strike gradient of crustal shortening. The documented clockwise rotations up to 45° are compatible with a secondary-bending type mechanism occurring after Eocene-Oligocene times (30-40 Ma), and their nature is probably related to the widespread shearing taking place between zones of differential shortening. Since ~15 Ma ago, the activity of N-S left-lateral strike-slip faults in the Eastern Cordillera at the border with the Altiplano-Puna plateau induced up to ~40° counterclockwise rotations along the fault zone, locally annulling the regional clockwise rotation. We proposed that mid-Miocene strike-slip activity developed in response of a compressive stress (related to body forces) at the plateau margins, caused by the progressive lateral (southward) growth of the Altiplano-Puna plateau, laterally spreading from the overthickened crustal region of the salient apex. The growth of plateaux by lateral spreading seems to be a mechanism common to other major plateaux in the Earth (i.e., Tibetan plateau). Results from the Patagonian Orocline represent the first reliable constraint to the timing of bending in the southern tip of South America. They indicate that the Patagonian Orocline did not undergo any significant rotation since early Eocene times (~50 Ma), implying that it may be considered either a primary bend, or an orocline formed during the late Cretaceous-early Eocene deformation phase. This result has important implications on the opening of the Drake Passage at ~32 Ma, since it is definitely not related to the formation of the Patagonian orocline, but the sole consequence of the Scotia plate spreading. Finally, relying on the results and implications from the study of the Western Alpine Arc, the Bolivian Orocline, and the Patagonian Orocline, general conclusions on curved mountain belt formation have been inferred.

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Als paläoklimatische Archive können unter anderem Stalagmiten und Klappen von Ostrakoden herangezogen werden. Bisher gab es noch keine veröffentlichten Ergebnisse räumlich hochaufgelöster Spurenelementverteilungen in einzelnen Ostrakodenklappen. Das gleiche gilt für die Bestimmung radiogener Blei-Isotope in Stalagmiten. Um klimatische Prozesse vergangener Zeiten zu untersuchen, wurde eine neue LA-ICP-MS (Laserablations – Massenspektrometrie mit induktiv gekoppeltem Plasma) Technik für hochaufgelöste in-situ Messungen von Spurenelementen und Bleiisotopen entwickelt. rnrnZunächst wurden geeignete Materialien für die Kalibrierung der Technik untersucht; als Proben dienten die Silikatreferenzgläser BAM-S005-A und BAM-S005B der Bundesanstalt für Materialforschung und –prüfung (BAM). Die Homogenität dieser Referenzgläser wurde mit LA-ICP-MS und den anderen mikroanalytischen Methoden EPMA (Elektronenmikrosonde) und SIMS (Ionensonde) überprüft. Die Ergebnisse zeigten, dass alle Haupt- und die meisten Spurenelemente in beiden Gläsern selbst im Mikrometerbereich homogen verteilt sind. Ausnahmen sind einige Spurenelemente, wie Cs, Cl, Cr, Mo und Ni, die heterogen in den Gläsern verteilt sind. Die Hauptelementzusammensetzung von BAM-S005-A und BAM-S005-B wurde mit Hilfe der EPMA bestimmt, wobei die Ergebnisse die Referenzwerte des BAM-Zertifikats bestätigten. Mit Ausnahme von Sr, Ba, Ce und Pb, stimmten die LA-ICP-MS-Spurenelementwerte mit den zertifizierten Werten innerhalb der angegebenen Fehlergrenzen überein. Gründe für die Diskrepanz der vier oben erwähnten Elemente sind noch unklar, aber sind möglicherweise durch fehlerhafte Referenzwerte zu erklären. Zusätzlich wurden 22 Spurenelemente gemessen, deren Gehalte von BAM nicht zertifiziert wurden. Aufgrund dieser Untersuchungen konnte festgestellt werden, dass beide BAM-Gläser für mikroanalytische Anwendungen geeignet sind.rnrnUm neuartige paläoklimatische Proxies im Calcit von Ostrakoden aus tibetanischen Seesedimenten zu untersuchen, wurde die Spurenelementvariabilität in einzelnen Ostrakodenklappen durch eine neue LA-ICP-MS-Technik bestimmt. Klappen von Ostrakoden der drei Arten (Leucocytherella sinensis Huang, 1982, ?Leucocythere dorsotuberosa Huang, 1982 und ?L. dorsotuberosa f. postilirata sensu Pang, 1985) wurden aus zwei Sedimentkernen des Nam Co Sees auf dem Hochplateau von Tibet gewonnen. Zwei LA-ICP-MS-Varianten, Spot- bzw. Linienanalyse, wurden verwendet, um die Elementkonzentrationen der Spurenelemente Mg, Sr, Ba, U und die der Seltenen Erdelemente (SEE) in den Klappen einzelner Ostrakoden zu bestimmen. Die Ergebnisse zeigten, dass die Linienanalyse präzisere Daten als die Spotanalyse liefert und sie wurde daher vorgezogen. Signifikante Unterschiede in der Spurenelementzusammensetzung zwischen den verschiedenen Arten der Ostrakoden wurden nicht gefunden. Variationen der Elementverhältnisse Mg/Ca und Sr/Ca in den Klappen stimmen mit veröffentlichten Seenspiegelschwankungen während des Holozäns überein, was zeigt, dass Mg- und Sr-Messungen in den Ostrakoden zur Untersuchung paläohydrochemischer Prozesse in diesem Gebiet herangezogen werden kann. Die gute Korrelation, die in dieser Arbeit zwischen Ba/Ca und Sr/Ca gefunden wurde, ist ein Hinweis darauf, dass der Einbau von Ba und Sr in die Klappen durch den gleichen Mechanismus erfolgte. Eine mögliche Beziehung zwischen dem U/Ca-Verhältnis in den Ostrakoden und den Redoxbedingungen auf dem Boden des Sees in der Vergangenheit wird diskutiert. Relativ geringe und konstante La/Ca-Verhältnisse wurden festgestellt, deren Ursache möglicherweise entweder auf der SEE-Charakteristik des Seewassers, auf biologischen Prozessen in den Ostrakoden oder auf Kontamination von Fe-Mn und/oder organischen Substanzen beruhen. Weitere Untersuchungen an Proben aus diesem Gebiet, speziell Klappen von lebenden Ostrakoden, sind notwendig, um den Gehalt von Ba, U und den SEE in Ostrakoden als paläoklimatische Proxies von Umweltbedingungen zu verwenden.

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This article focuses on several key philosophical themes in the criticism of Sakaguchi Ango (1906–1955), one of postwar Japan’s most influential and controversial writers. Associated with the underground Kasutori culture as well as the Burai-ha of Tamura Taijirō (1911–1983), Oda Sakunosuke (1913–1947) and Dazai Osamu (1909–1948), Ango gained fame for two provocative essays on the theme of daraku or “decadence”—Darakuron and Zoku darakuron—pubished in 1946, in the wake of Japan’s traumatic defeat and the beginnings of the Allied Occupation. Less well-known is the fact that Ango spent his student years studying classical Buddhist texts in Sanskrit, Pali and Tibetan, and that he at at one time aspired to the priesthood. The article analyses the concept of daraku in the two essays noted above, particularly as it relates to Ango’s vision of a refashioned morality based on an interpretation of human subjectivity vis-à-vis the themes of illusion and disillusion. It argues that, despite the radical and modernist flavor of Ango’s essays, his “decadence” is best understood in terms of Mahāyāna and Zen Buddhist concepts. Moreover, when the two essays on decadence are read in tandem with Ango’s wartime essay on Japanese culture (Nihon bunka shikan, 1942), they form the foundation for a “postmetaphysical Buddhist critique of culture,” one that is pragmatic, humanistic, and non-reductively physicalist.

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Region-specific empirically based ground-truth (EBGT) criteria used to estimate the epicentral-location accuracy of seismic events have been developed for the Main Ethiopian Rift and the Tibetan plateau. Explosions recorded during the Ethiopia-Afar Geoscientific Lithospheric Experiment (EAGLE), the International Deep Profiling of Tibet, and the Himalaya (INDEPTH III) experiment provided the necessary GT0 reference events. In each case, the local crustal structure is well known and handpicked arrival times were available, facilitating the establishment of the location accuracy criteria through the stochastic forward modeling of arrival times for epicentral locations. In the vicinity of the Main Ethiopian Rift, a seismic event is required to be recorded on at least 8 stations within the local Pg/Pn crossover distance and to yield a network-quality metric of less than 0.43 in order to be classified as EBGT5(95%) (GT5 with 95% confidence). These criteria were subsequently used to identify 10 new GT5 events with magnitudes greater than 2.1 recorded on the Ethiopian Broadband Seismic Experiment (EBSE) network and 24 events with magnitudes greater than 2.4 recorded on the EAGLE broadband network. The criteria for the Tibetan plateau are similar to the Ethiopia criteria, yet slightly less restrictive as the network-quality metric needs to be less than 0.45. Twenty-seven seismic events with magnitudes greater than 2.5 recorded on the INDEPTH III network were identified as GT5 based on the derived criteria. When considered in conjunction with criteria developed previously for the Kaapvaal craton in southern Africa, it is apparent that increasing restrictions on the network-quality metric mirror increases in the complexity of geologic structure from craton to plateau to rift. Accession Number: WOS:000322569200012

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This thesis provides a critique of Western media articles concerning self-immolation in Tibet. I begin by illustrating how the Western media provides reductionist accounts of Tibetan self-immolation by depicting the act solely as a form of political protest in response to Chinese occupation. I argue that these limited portrayals of self-immolation can be attributed to the Shangri-La imagery that characterizes much of the Western conceptions of Tibet. Through Shangri-La imagery, both Tibetans and their Buddhist religion are portrayed as utopic, peaceful, and able to provide the antidote to solving Western problems relating to modernization and consumerism. After illustrating the ways in which Shangri-La imagery influences Western media portrayals of Tibetan self-immolation, this thesis explores the commonly disregarded Buddhist dimensions of the act. Looking to Buddhist doctrine, scripture, and history, this thesis establishes a clear relationship between self-immolation and Buddhism, which situates the act as being more complicated than mere political protest. I argue that these limited portrayals given by the Western media are problematic because they overlook a fundamental aspect of self-immolation, thus potentially misrepresenting Tibetans. This thesis explores the Buddhist dimensions of self-immolation as a possible way to further understand what has led more than one hundred Tibetans to perform this act during the time of political crisis.

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BACKGROUND: The neuronal ceroid lipofuscinoses (NCL) are a heterogenous group of inherited progressive neurodegenerative diseases in different mammalian species. Tibetan Terrier and Polish Owczarek Nizinny (PON) dogs show rare late-onset NCL variants with autosomal recessive inheritance, which can not be explained by mutations of known human NCL genes. These dog breeds represent animal models for human late-onset NCL. In mice the chloride channel 3 gene (Clcn3) encoding an intracellular chloride channel was described to cause a phenotype similar to NCL. RESULTS: Two full-length cDNA splice variants of the canine CLCN3 gene are reported. The current canine whole genome sequence assembly was used for gene structure analyses and revealed 13 coding CLCN3 exons in 52 kb of genomic sequence. Sequence analysis of the coding exons and flanking intron regions of CLCN3 using six NCL-affected Tibetan terrier dogs and an NCL-affected Polish Owczarek Nizinny (PON) dog, as well as eight healthy Tibetan terrier dogs revealed 13 SNPs. No consistent CLCN3 haplotype was associated with NCL. CONCLUSION: For the examined animals we excluded the complete coding region and adjacent intronic regions of canine CLCN3 to harbor disease-causing mutations. Therefore it seems to be unlikely that a mutation in this gene is responsible for the late-onset NCL phenotype in these two dog breeds.

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Higgins School of the Humanities/Difficult Dialogues: Video Recording from 09/27/2011 event featuring John Makransky and Alan Lightman titled "Effective Priactice" Event Description: At Clark, we have chosen to focus on the concept of effective practice as we rethink our curriculum. What is the nature of practice? What makes something a practice? Does practice serve our intentions, or open unexpected pathways? What does it mean if we also ask it to be effective? And what forms of practice do the humanities cultivate? Our guests for a conversation about practice are John Makransky, Professor of Buddhism and comparative theology at Boston College and a teacher in the Dzogchen tradition of Tibetan Buddhism, and Alan Lightman, physicist, writer and activist, and adjunct faculty member at MIT. They both have lives profoundly rooted in questions of practice.

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Alveolar echinococcosis (AE)--caused by the cestode Echinococcus multilocularis--is a severe zoonotic disease found in temperate and arctic regions of the northern hemisphere. Even though the transmission patterns observed in different geographical areas are heterogeneous, the nuclear and mitochondrial targets usually used for the genotyping of E. multilocularis have shown only a marked genetic homogeneity in this species. We used microsatellite sequences, because of their high typing resolution, to explore the genetic diversity of E. multilocularis. Four microsatellite targets (EmsJ, EmsK, and EmsB, which were designed in our laboratory, and NAK1, selected from the literature) were tested on a panel of 76 E. multilocularis samples (larval and adult stages) obtained from Alaska, Canada, Europe, and Asia. Genetic diversity for each target was assessed by size polymorphism analysis. With the EmsJ and EmsK targets, two alleles were found for each locus, yielding two and three genotypes, respectively, discriminating European isolates from the other groups. With NAK1, five alleles were found, yielding seven genotypes, including those specific to Tibetan and Alaskan isolates. The EmsB target, a tandem repeated multilocus microsatellite, found 17 alleles showing a complex pattern. Hierarchical clustering analyses were performed with the EmsB findings, and 29 genotypes were identified. Due to its higher genetic polymorphism, EmsB exhibited a higher discriminatory power than the other targets. The complex EmsB pattern was able to discriminate isolates on a regional and sectoral level, while avoiding overdistinction. EmsB will be used to assess the putative emergence of E. multilocularis in Europe.