Publications:
Publications
Kumon, F., Kanamaru, K., Tawara, T., Noriko, K., Yamamoto, M., and Hayashi, H., 2005. Relashionship among weather factors, biological productivity, and TOC content of sediments in Lake Kizaki, central Japan. Jour. Geol. Soc. Japan.
http://www.jstage.jst.go.jp/article/geosoc/111/10/599/_pdf
Abstracts
Kanamaru, K., Francus, P., and Bradley, R., 2008. Establishment of reliable paleoclimatic proxies obtained from high-resolution x-ray fluorescence analysis performed on anoxic fjord sediment, Saanich Inlet, BC. Representing and Reducing Uncertainties in High-resolution Proxy Climate Data workshop, Trieste, Italy
Kanamaru, K., Francus, P., and Bradley, R., 2008. Early to mid Holocene sediment flux and seasonal provenance using x-ray fluorescence and backscattered electron microscopic studies from anoxic fjord, Saanich Inlet, BC, Canada. Twelfth Annual Continental Scientific Drilling Workshop. DOSECC.
Kanamaru, K., Francus, P., and Bradley, R., 2006. Holocene sedimentation recorded in varved sediments in Saanich Inlet, British Columbia, Eos Trans. AGU, 87(52), Fall Meet. Suppl., Abstract PP21C-1696.
Kanamaru, K., Francus, P., and Bradley, R., 2006. The behavior of major and minor metals using a high resolution XRF scanner on laminated Holocene sediment in Saanich Inlet, British Columbia: Mn and Ca spikes. Northeastern 41st Annual Meeting. The Geological Society of America.
Kanamaru, K., Kumon, F., Hayashi, H., 2002. Total organic carbon and nitrogen in lake sediment as paleoclimatic proxy. The 11th International Symposium on River and Lake Environments.
Kanamaru, K., Kumon, F., 2002. Relationship between climate and TOC and TN fluxes in the sediment of lake Kizaki, central Japan. Japan Earth and Planetary Science Joint Meeting.
Kanamaru, K., Kumon, F., 2001. Variability of TOC and TN in the sediment of Lake Kizaki, in relation to limnological and meteorological condition. Japan Earth and Planetary Science Joint Meeting.
Kumon, F., Adhikari, D.P., Kanamaru, K., 2001. Climatic variability during the last 1300 years as deduced from the lake sediments of the Nishina Three Lakes, central Japan. The Geological Society of Japan.