This book presents the study of limnogeomorphology, in which past proxy data such as lacustrine sediments with information on landform development can be linked to modern observed data acquired by instruments, including hydro-geomorphological and sedimentary data. Traditionally, in the field of earth sciences, it has been thought that geophysical studies dealing mainly with the present process were not smoothly linked to geological studies that originated from historical studies. Although such earth-surface process studies are closely related to those on historical landform development in the field of geomorphology, they have been studied separately. Those two geomorphology studies correspond to process geomorphology (dynamic geomorphology) and historical geomorphology. There have been some attempts to combine them; however, they lacked past quantitative records available for further analyses. In the study of limnogeomorphology, proxy data can be converted to quantitative information to be utilized in future environmental discussions. This book also covers information not only on large lake-catchment systems, but on small systems. Those include long-term and short-term and large-scale and small-scale environmental changes in east Eurasia such as Lake Baikal, Lake Khuvsgul, Lake Biwa, and small lakes in Japan, Mongolia, China, and Korea.
Kenji Kashiwaya Knihy


Long continental records from lake Baikal
- 370 stránek
- 13 hodin čtení
Lake Baikal in eastern Siberia is a crucial site for detecting long-term global changes, owing to its high sensitivity to climatic oscillation and its extraordinarily long history. Because lacustrine sediments have an advantage in providing high-resolution information, the sediments in Lake Baikal contain excellent continuous records of past conditions including paleoclimates, evolution, and specification of organisms. Based on the study by the Baikal Drilling Project, this book provides information on global climatic and environmental changes for as much as 12 million years. The book also includes discussions of comparatively short-term changes such as glacial and interglacial transitions that directly link to the present and future environment. Long Continental Records from Lake Baikal summarizes the latest knowledge on the paleoenvironment and provides a foundation for further studies in global environmental changes.