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Titlebook: Earth Surface Processes and Environmental Changes in East Asia; Records From Lake-ca Kenji Kashiwaya,Ji Shen,Ju Yong Kim Book 2015 Springer

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Abschnitt Die Spaltung der Welt,ion (δ.N.), total organic carbon (TOC), total nitrogen (TN), carbon-to-nitrogen ratio (C/N) and redness analyses was conducted on a 269-cm long sediment core collected from Lake Xingkai to reconstruct the palaeoclimate and palaeoenvironment evolution of Northeast China since 28 ka BP. The analysis r
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Ein Zeichen sind wir, deutungslosunderstood and still under controversy. In this study, we obtained a 12.72-m-long sediment core (JP-C) from Jingpo Lake in south Heilongjiang Province, northeast China, and used AMS radiocarbon dating of terrestrial plant macrofossils to provide a robust chronology. This study will focus on the sedi
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https://doi.org/10.1007/978-1-4020-8229-0gistered landscape site (Yang GS, Jungwon Munhwa 14:1–38, 2010). Since the late Bronze Age, its water has been used for agricultural irrigation. The lake was initially formed at the mouth of a fanglomerate where Jurassic granites blocked the main course of a stream channel at about 305 m above sea l
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Theoretical Frameworks and School Context,ho, and Lake Soonpogaeho) in the Yeongdong region on the east coast of Korea. They deserve close examination as they clearly show the transition towards an agricultural society and local land-use changes during the late Holocene. Bongpo marsh began to develop ca. 650 BC as a coastal lagoon was rapid
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A Background to Engineering Designuminescence in sediment by surface exposure (bleaching) before burial. The time needed for bleaching is known to vary among the signals used in three methods: optically stimulated luminescence (OSL), infrared stimulated luminescence (IRSL), and post-infrared IRSL (pIRIR). A comparison of luminescenc
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