TY - JOUR A1 - Scheller, Frieder W. A1 - Schmid, Rolf T1 - A tribute to Isao Karube (1942-2020) and his influence on sensor science JF - Analytical and bioanalytical chemistry : a merger of Fresenius' journal of analytical chemistry, Analusis and Quimica analitica KW - Karube KW - Japan KW - biosensors KW - lifetime achievements Y1 - 2020 U6 - https://doi.org/10.1007/s00216-020-02946-5 SN - 1618-2642 SN - 1618-2650 VL - 412 IS - 28 SP - 7709 EP - 7711 PB - Springer CY - Berlin ER - TY - JOUR A1 - Bents, Dominik A1 - Groth, Detlef A1 - Satake, Takashi T1 - The secular trend and network effects on height of male Japanese students from 1955 to 2015 JF - Journal of biological and clinical anthropology JF - Anthropologischer Anzeiger ; Mitteilungsorgan der Gesellschaft für Anthropologie N2 - Introduction: Body height is influenced by biological factors such as genetics, nutrition and health, but also by the social network, and environmental and economical factors. During centuries, the Japanese society has developed on islands. This setting provides ideal natural conditions for studying the influence of social networks on human height. Material and methods: We investigated body height of male Japanese students aged 17.5 years obtained in 47 prefectures, from the Japanese school health survey of the years 1955, 1975, 1995, and 2015. Results: Japanese students increased in height from 163.23 cm in 1955 to 170.84 cm in 1995, with no further increase thereafter (170.63 cm in 2015). Students living in neighboring prefectures were similar in height. The correlation of height between neighboring prefectures ranged between r = 0.79 and r = 0.49 among first degree neighbors, between r = 0.49 and r = 0.21 among second degree neighbors and dropped to insignificance among third degree neighbors indicating psychosocial effects of the community on body height. Tall stature and short stature prefectures did not remain tall or short throughout history. Autocorrelations of height within the same prefectures decreased from the 20 years periods of 1955-1975, 1975-1995 and 1995-2015 (r = 0.52, r = 0.61, r = 0.63, respectively) to the 40 years periods of 1955-1995 and 1975-2015 (r = 0.49, r = 0.52), down to the 60 years period of 1955-2015 (r = 0.27), indicating significant volatility of height. Conclusion: Body height of 17.5 years old Japanese students increased since 1955. Body height depended on height of the neighboring prefecture, but was volatile with decreasing autocorrelation during a period of 60 years. KW - body height KW - community effect KW - neighbor correlation KW - Japan Y1 - 2018 U6 - https://doi.org/10.1127/anthranz/2018/0838 SN - 0003-5548 VL - 74 IS - 5 SP - 423 EP - 429 PB - Schweizerbart CY - Stuttgart ER - TY - JOUR A1 - Ganghof, Steffen T1 - A new political system model BT - Semi-parliamentary government JF - European Journal for Political Research N2 - Semi-parliamentary government is a distinct executive-legislative system that mirrors semi-presidentialism. It exists when the legislature is divided into two equally legitimate parts, only one of which can dismiss the prime minister in a no-confidence vote. This system has distinct advantages over pure parliamentary and presidential systems: it establishes a branch-based separation of powers and can balance the ‘majoritarian’ and ‘proportional’ visions of democracy without concentrating executive power in a single individual. This article analyses bicameral versions of semi-parliamentary government in Australia and Japan, and compares empirical patterns of democracy in the Australian Commonwealth as well as New South Wales to 20 advanced parliamentary and semi-presidential systems. It discusses new semi-parliamentary designs, some of which do not require formal bicameralism, and pays special attention to semi-parliamentary options for democratising the European Union. KW - semi-parliamentarism KW - bicameralism KW - Australia KW - New South Wales KW - Japan Y1 - 2018 U6 - https://doi.org/10.1111/1475-6765.12224 SN - 0304-4130 SN - 1475-6765 VL - 57 IS - 2 SP - 261 EP - 281 PB - Wiley CY - Hoboken ER - TY - JOUR A1 - Korup, Oliver A1 - Hayakawa, Yuichi A1 - Codilean, Alexandru T. A1 - Matsushi, Yuki A1 - Saito, Hitoshi A1 - Oguchi, Takashi A1 - Matsuzaki, Hiroyuki T1 - Japan's sediment flux to the Pacific Ocean revisited JF - Earth science reviews : the international geological journal bridging the gap between research articles and textbooks N2 - Quantifying volumes and rates of delivery of terrestrial sediment from island arcs to subduction zones is indispensable for refining estimates of the thickness of trench fills that may eventually control the location and timing of submarine landslides and tsunami-generating mega-earthquakes. Despite these motivating insights, knowledge about the rates of erosion and sediment export from the Japanese islands to their Pacific subduction zones remains patchy regardless of the increasing availability of highly resolved data on surface deformation, climate, geology, and topography. Traditionally, natural erosion rates across the island arc have been estimated from regression of topographic catchment metrics and reservoir sedimentation rates that were recorded over several years to decades. We review current research in this context, correct for a systematic bias in one of the most widely used predictions, and present new estimates of decadal to millennial-scale erosion rates of Japan's terrestrial inner forearc. We draw on several independent and unprecedented inventories of mass wasting, reservoir sedimentation, and concentrations of cosmogenic Be-10 in river sands. We find that natural Be-10-derived denudation rates of several mm yr(-1) in the Japanese Alps have been sustained over several centuries to millennia, and are, within error, roughly consistent with sediment yields inferred from artificial reservoir sedimentation. Local exceptions may likely result from release of sediment storage or regional landsliding episodes that trigger transient sediment pulses. Our synopsis further reveals that catchments draining Japan's eastern seaboard differ distinctly in their tectonic, lithological, topographic, and climatic characteristics between the Tohoku, Japanese Alps, and Nankai inner forearc segments, which is underscored by a marked asymmetric pattern of erosion rates along the island arc. Erosion rates are highest (up to at least 3 mm yr(-1)) in the Japanese Alps that mark the collision of two subduction zones, where high topographic relief, hillslope and bedrock-channel steepness foster rapid denudation by mass wasting. Comparable, if slightly lower, erosion rates characterise the Nankai inner forearc in southwest Japan, most likely due to higher typhoon-driven rainfall totals and variability rather than its high topographic relief. In contrast, our estimated erosion and flux rates are lowest in the Tohoku inner forearc catchments that feed sediment into the Japan Trench. We conclude that collisional mountain building of the Japanese Alps drives some of the highest erosion rates in the island arc despite similar uplift and precipitation controls in southwest Japan. We infer that, prior to extensive river damming, reservoir construction, and coastal works, the gross of Japan's total sediment export to the Pacific Ocean entered the accretionary margin of the Nankai Trough as opposed to the comparatively sediment-starved Japan Trench. Compared to documented contemporary rates of sediment flux from mountainous catchments elsewhere in the Pacific, the rivers draining Japan's inner forearc take an intermediate position despite high relief, steep slopes, very high seismicity, and frequent rainstorms. However, the average rates of millennial-scale denudation in the Japanese Alps particularly are amongst the highest reported worldwide. Local mismatches between these late Holocene and modern rates emphasise the anthropogenic fingerprint on sediment retention that may have significantly reduced the island arc's mass flux to its subduction zones, as is the case elsewhere in east and southeast Asia. (C) 2014 Elsevier B.V. All rights reserved. KW - Erosion KW - Japan KW - Subduction zone KW - Landslides KW - Cosmogenic nuclides KW - Sediment budget Y1 - 2014 U6 - https://doi.org/10.1016/j.earscirev.2014.03.004 SN - 0012-8252 SN - 1872-6828 VL - 135 SP - 1 EP - 16 PB - Elsevier CY - Amsterdam ER -