Landscape Agency and Evenki-Iakut Reindeer Husbandry Along the Zhuia River, Eastern Siberia

This article is dedicated to the memory of Vasilii Nikolaeich Maksimov who drowned with his son while crossing the Zhuia River in 2012. The field research and laboratory analysis for this article was sponsored mainly by a grant from the Research Council of Norway (NFR 179316) within the multinational research framework “BOREAS: Histories from the North” organized by the European Science Foundation EUROCORES programme. A portion of the laboratory work, and the time for writing an analysis was made possible by an Advanced Grant from the European Research Council (ERC AdG 295458). The research could not have been carried out without the in-kind support, equipment and expertise of the Irkutsk State Technological University and the logistical support of the mining enterprise ‘Svetlyi’ based in Bodaibo. We are grateful to Iurii Vasil’evich Zharkov of the goldmining company Vitim and his uncle Iurii Alekseevich Zharkov of Svetlyi Ltd for professionally and reliably arranging ground transport for us and our equipment to and from the banks of the Zhuia River. We are also grateful to Iurii Konstantinovich Polititsyn, a lifetime resident of Svetlyi, who gave advice on sites of previous Evenki occupation and whose family helped us to navigate the river and organise the fieldwork. For this article, DGA was the principal investigator of the two grants, participated in most of the fieldwork, and composed this English text consulting Russian-language drafts prepared by EMI and OPV. EMI organized the fieldwork, conducted the trench digging, and prepared preliminary versions of the maps. OPV participated in the fieldwork, collected botanical samples, and participated in the interpretation of the pollen diagrams. ML participated in the fieldwork and conducted the phosphate analysis. The arduous work of identifying and counting the pollen grains, fungal spores and charcoal fragments was done by NVK in her laboratory in Irkutsk. We are indebted to our colleagues Drs. Ed Schofield and Dmitryi Mauquoy of the School of Geosciences at the University of Aberdeen for drafting the pollen diagrams and constructing the age-depth model and to Paul Ledger and Ilse Kamerling, also of the University of Aberdeen, for helping draft the final versions of the maps and figures.Peer reviewedPostprin

Late Jurassic - Early Cretaceous paleoenvironmental evolution of the Transbaikal basins (SE Siberia): implications for the Mongol-Okhotsk orogeny

International audienceThe Late Jurassic - Early Cretaceous tectonic evolution of SE Siberia was marked by the closure of the Mongol-Okhotsk ocean. While this geodynamic event led to compressive deformation and denudation in a wide area encompassing the North-Altay, Sayan and Baikal Patom ranges, it was contemporaneous to widespread extension from the Transbaikal region situated immediately north of the suture zone to the Pacific plate, affecting eastern Mongolia and northeastern China. In this study we review the paleontological and sedimentological data available in the Russian literature and provide new macro-floral and palynological data from the Mesozoic sediments of three Transbaikal basins. These data are used to describe the paleoenvironmental and paleoclimatic evolution of the Transbaikal area in order to assess the topographic evolution of the region in relation with the closure of the Mongol-Okhotsk ocean. We establish that the Transbaikal basins evolved in a continuously extensional tectonic setting from at least the Early-Middle Jurassic to the Early Cretaceous. The associated sedimentary environments are characterized by retrogradation from alluvial fan –braided river dominated systems prevailing during the Early to Middle Jurassic initial opening of the basins to meandering river–lacustrine systems that developed during the Late Jurassic - Early Cretaceous interval. No evidence of high relief topography was found and we conclude that, while compression and denudation occurred in the North Altai, Sayan and Patom ranges, in the Transbaikal region, the docking of the Mongolia-North China continent to Siberia was a “soft collision” event, possibly involving a major strike-slip displacement that did not lead to an orogenic event implying strong compressive deformation, crustal thickening and topography building

Quantum dot lasers and relevant nanoheterostructures

Spectral and power characteristics of QD stripe lasers operating in two-state lasing regime have been studied in a wide range of operation conditions. It was demonstrated that neither self-heating nor increase of the homogeneous broadening are responsible for quenching of the ground-state lasing beyond the two-state lasing threshold. It was found that difference in electron and hole capture rates strongly affects light-current curve. Modulation p-type doping is shown to enhance the peak power of GS lasing transition. Microring and microdisk structures (D = 4-9 mu m) comprising 1.3 mu m InAs/InGaAs quantum dots have been fabricated and studied by mu-PL and NSOM. Ground-state lasing was achieved well above root temperature (up to 380 K). Effect of inner diameter on threshold characteristics was evaluated