496 research outputs found

    Single-beam phase retrieval with partially coherent light illumination

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    A single-beam phase retrieval method with partially coherent illumination is proposed. By using an obverse and reverse iterative (ORI) algorithm, objects can be reconstructed within less time by recording a sequence of diffraction patterns at different axial planes under partially coherent light illumination. Partially coherent light illumination reduces coherent noise and the number of diffraction patterns needed for reconstruction. Thus, the whole process is fast and has high immunity to external perturbation due to the reference-less configuration. Both simulation and experimental results are presented to demonstrate the feasibility of the proposed approach

    MCSD 1.0 - Multimodal Chinese Sarcasm Dataset

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    This repository includes full text file of Multimodal Chinese Sarcasm Dataset (MCSD), a curated dataset for research on multimodal sarcasm detection in Mandarin Chinese publicly broadcasted stand-up comedy. The corpus is structured as follows: unique utterance ID for each transcribed segment. manually verified transcription of the spoken utterance (in Mandarin). pseudonymized speaker ID. annotated label (sarcastic / not sarcastic) for each transcription. aligned start and end timestamps. reference to the original publicly available video. For full dataset description and annotation guidelines, please see: Link Contributors and roles Xiyuan Gao (University of Groningen) – PhD researcher. Responsible for dataset design, transcription processing, annotation guideline. Dr. Bruce Xiao Wang (Hong Kong Polytechnic University) – Collaborator and linguistic expert. Contributed to the research framework, research methodology design, and Mandarin discourse insights. Meiling Zhang, Shuming Zhang, and Zhu Li – Carried out manual labeling of sarcasm in the transcribed data based on developed annotation protocols. Dr. Matt Coler & Dr. Shekhar Nayak (University of Groningen) – Supervisors. Provided research supervision and guidance on ethical compliance.</li

    Role of Sprouty2 in prostate carcinogenesis

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    Prostate cancer (PC) is the most common cancer in men. In the UK alone, there are over 30,000 men diagnosed with PC every year. Loss of SPRY2 and activation of receptor tyrosine kinases are common events in PC. However, the molecular basis of their interaction and clinical impact remains to be fully examined. SPRY2 loss may functionally synergise with aberrant cellular signalling to drive PC and to promote treatment resistant disease. Using a combination of in vitro, pre-clinical in vivo models and clinical PC, this thesis shows the impact of SPRY2 loss upon activation of the ErbB signalling system via a positive feedback regulation of the ErbB-PI3K/AKT cascade. Loss of SPRY2 resulted in hyper-activation of PI3K/AKT signalling to drive proliferation and invasion by enhanced internalisation of EGFR/HER2 and their sustained localisation and signalling at the early endosome in a PTEN-dependent manner. This involves activation of p38 MAPK by PI3K to facilitate clathrin-mediated ErbB receptor endocytosis. Furthermore, this thesis suggests a critical role of PI3K/AKT in PC whereby in vitro and in vivo inhibition of PI3K suppresses proliferation and invasion, supporting PI3K/AKT as a target for therapy particularly in patients with PTEN-haploinsufficiency, low SPRY2 and ErbB expressing tumours. In conclusion, SPRY2 is an important tumour suppressor in PC; its loss drives the PI3K/AKT pathway via functional interaction with the ErbB system

    Phylogenetic relationships and estimation of divergence times among Sisoridae catfishes

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    Nineteen taxa representing 10 genera of Sisoridae were subjected to phylogenetic analyses of sequence data for the nuclear genes Plagl2 and ADNP and the mitochondrial gene cytochrome . The three data sets were analyzed separately and combined into a single data set to reconstruct phylogenetic relationships among Chinese sisorids. Both Chinese Sisoridae as a whole and the glyptosternoid taxa formed monophyletic groups. The genus is likely to be the earliest diverging extant genus among the Chinese Sisoridae. The four species included in the study formed a monophyletic group. was indicated to be earliest diverging glyptosternoid, followed by and . Our data supported the conclusion that and both formed a monophyletic group. On the basis of the fossil record and the results of a molecular dating analysis, we estimated that the Sisoridae diverged in the late Miocene about 12.2 Mya. The glyptosternoid clade was indicated to have diverged, also in the late Miocene, about 10.7 Mya, and the more specialized glyptosternoid genera, such as , originated in the Pleistocene (within 1.9 Mya). The speciation of glyptosternoid fishes is hypothesized to be closely related with the uplift of the Qinghai-Tibet Plateau.Nineteen taxa representing 10 genera of Sisoridae were subjected to phylogenetic analyses of sequence data for the nuclear genes Plagl2 and ADNP and the mitochondrial gene cytochrome . The three data sets were analyzed separately and combined into a single data set to reconstruct phylogenetic relationships among Chinese sisorids. Both Chinese Sisoridae as a whole and the glyptosternoid taxa formed monophyletic groups. The genus is likely to be the earliest diverging extant genus among the Chinese Sisoridae. The four species included in the study formed a monophyletic group. was indicated to be earliest diverging glyptosternoid, followed by and . Our data supported the conclusion that and both formed a monophyletic group. On the basis of the fossil record and the results of a molecular dating analysis, we estimated that the Sisoridae diverged in the late Miocene about 12.2 Mya. The glyptosternoid clade was indicated to have diverged, also in the late Miocene, about 10.7 Mya, and the more specialized glyptosternoid genera, such as , originated in the Pleistocene (within 1.9 Mya). The speciation of glyptosternoid fishes is hypothesized to be closely related with the uplift of the Qinghai-Tibet Plateau

    Re-Os dating of chalcopyrite from selected mineral deposits in the Kalatag district in the eastern Tianshan Orogen, China

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    The Kalatag Cu-Zn-Au district contains a number of economically important Cu deposits in eastern Tianshan in Xinjiang, NW China. Due to the lack of precise mineralization ages, the metallogenesis of this area has long been a matter of debate. In this study, chalcopyrite Re-Os isotope methods are used to date the South Meiling Cu-Zn and Hongshi Cu deposits in the eastern part of Kalatag area. The South Meiling Cu-Zn deposit is hosted in volcanic-sedimentary rocks of the Late Ordovician to Early Silurian Daliugou Formation. The deposit consists of two parts: a concordant massive sulfide ores and discordant vein-type ores located in the footwall strata. The principal ore minerals are pyrite, chalcopyrite, sphalerite, minor tetrahedrite, galena and pyrrhotite. Gangue minerals include quartz, sericite and barite, and minor chlorite, plagioclase and carbonate minerals. The Hongshi Cu deposit represents a hydrothermal vein system hosted in the mafic volcanic rocks of Daliugou Formation. The orebodies are associated with quartz veins and controlled by subsidiary faults of the Kalatag fault. The ore-forming process can be divided into the early, middle and late stages and is characterized by quartz-pyrite, quartz-chalcopyrite-pyrite and quartz-carbonate-gypsum veins, respectively. Re-Os analyses of chalcopyrite from the South Meiling Cu-Zn deposit yield an isochron age of 434.2 +/- 3.9 Ma and initial Os-187/Os-188 ratio of 0.647 +/- 0.098 (MSWD = 0.59). Re-Os analyses of chalcopyrite from the Hongshi Cu deposit yield an isochron age of 431.8 +/- 2.7 Ma and initial Os-187/Os-188 ratio of -0.165 +/- 0.075 (MSWD = 0.77). Since chalcopyrite is the primary copper mineral, we interpret these isochron ages as the timing of Cu mineralization, based on field geology and petrographic evidence. These results suggest that the Re-Os ages presented here provide, for the first time, a direct constraint on an early Paleozoic Cu mineralization event of the eastern Tianshan Orogen. The high initial Os-187/Os-188 ratios (0.647 +/- 0.098) ratio of similar to 434 Ma chalcopyrite from the South Meiling deposit suggest that the metal was sourced from a two end-member mixing of crust and mantle materials. Moreover, we propose that the VMS mineral system and hydrothermal vein system of the Kalatag district were related to the south-dipping subduction of the Kalamaili oceanic plate during the Late Ordovician-Silurian. (C) 2016 Elsevier B.V. All rights reserved.973 Project [2014CB440803]; National Nature Science Foundation of China [41572077, U1139301, 41202064, 41203037]; China Geological Survey Bureau [1212011140056, 12120114081701]SCI(E)[email protected]; [email protected]
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