1,744,491 research outputs found
Efficacy of BIBF 1120 or BIBF 1120 plus chemotherapy on nasopharyngeal carcinoma in vitro and in vivo
No full textCong Xue,1 Ying Tian,2 Jing Zhang,3 Yuanyuan Zhao,1 Jianhua Zhan,2 Wenfeng Fang,1 Li Zhang1 1Department of Medical Oncology, 2Department of Research, Sun Yat-Sen University Cancer Center, State Key Laboratory of Oncology in South China, Collaborative Innovation Center of Cancer Medicine, 3Department of Medical Oncology, The First Affiliated Hospital of Guangzhou Traditional Chinese Medicine University, Guangzhou, People’s Republic of China Purpose: BIBF 1120 is a potent triple angiokinase inhibitor now being evaluated in many types of tumors. We examine the antitumor effects of BIBF 1120 on nasopharyngeal carcinoma (NPC) in vitro and in vivo. Materials and methods: The effect of BIBF 1120 on NPC cell proliferation was evaluated using the Cell Counting Kit 8 assay. The activities of BIBF 1120 as a single agent and in combination with cisplatin (DDP) in NPC tumor xenografts were evaluated by measuring microvessel density and expression of vascular endothelial growth factor signaling. Results: BIBF 1120 exhibited limited inhibition of the growth of three NPC cell lines. Concurrent administration of BIBF 1120 and DDP provided greater antitumor effects compared to that observed with the use of either inhibitor as a single agent in the NPC xenograft model. Microvessel density and expression of vascular endothelial growth factor signaling were significantly reduced. Conclusion: BIBF 1120, either as a single agent or in combination with DDP, demonstrates significant antitumor and antiangiogenic effects in the NPC xenograft model. Our results indicate that BIBF 1120 administered in conjunction with chemotherapy might provide an effective treatment method for NPC. Keywords: BIBF 1120, nasopharyngeal carcinoma, antiangiogenesis, microvessel densit
Artists' earnings and copyright: a review of British and German music industry data in the context of digital technologies
Get PDFDigital technologies are often said (1) to enable a qualitatively new engagement with already
existing cultural materials (for example through sampling and adaptation), and (2) to offer a
new disintermediated distribution channel to the creator. From a review of secondary data on
music artists’ earnings and seven in-depth interviews, it appears that both ambitions have
remained, until now, largely unfulfilled. The paper discusses to what extent the structure of
copyright law is to blame, and sets out a research agenda
3rd Floor: Staff Enjoying Snacks at University Author Reception
No full texthttps://digitalcommons.pittstate.edu/unihistoryphotos/1120/thumbnail.jp
Appendix A Table SD1. CaCO3, δ¹⁸O, δ¹³C and Sr isotopes from ODP Site 181-1120
No full textAn integrated chemostratigraphic (87Sr/86Sr, d13C and 18O) study of benthic foraminifera is presented for a 210 m-thick, intermediate depth (upper/middle bathyal transition), Miocene nannofossil ooze section of Ocean Drilling Program Site 1120, Campbell Plateau off New Zealand. Our results indicate that new 87Sr/86Sr, d13C and d18O profiles are wholly consistent with their respective Miocene reference curves. These observations facilitate identification of a total of five reliable chemostratigraphic datums, which are based on the fundamental structural changes in the 87Sr/86Sr curve and paired simultaneous d13C and d18O events. The resultant age-depth relationship clearly shows that the Miocene (20-5 Ma) biopelagic sedimentation on the Campbell Plateau was essentially continuous at a moderate to high, linear sedimentation rate (17.5 m/m.y. with an exception of the uppermost 13 m). Our findings do not support the shipboard biostratigraphic age model, which assumes that the critical early-middle Miocene transition was interrupted by a major hiatus (<~3 m.y.). Because of its unique bathymetric setting at a paleowater-depth of ~ 600 m, which is among the shallowest of the coeval isotopically studied deep-sea sections in the South Pacific/Southern Ocean, Site 1120 will serve as a reference section for surveying the evolution of intermediate-water paleoceanography in the Southern Hemisphere across the middle Miocene climatic transition
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