[S-GL22] 年代層序単元境界の研究最前線

[SGL22-P08] 根室層群の白亜系-古第三系境界堆積物の磁気特性

*星 博幸¹、高橋 亮貴¹、高嶋 礼詩²、林 圭一³ (1.愛知教育大学、2.東北大学、3.北海道立総合研究機構)

キーワード：根室層群、白糠丘陵、K–Pg境界、岩石磁気、帯磁率

Previous and ongoing studies have suggested that a Cretaceous–Paleogene (K–Pg) boundary is present in a muddy sequence of the Nemuro Group in the Shiranuka Hill area in eastern Hokkaido. An interdisciplinary approach, including detailed mapping, radiometric dating, geochemical analyses, and biostratigraphic and magnetostratigraphic investigations, is needed to locate a K–Pg horizon in the group. For this purpose, we have investigated stratigraphic variations in rock magnetic properties of marine sediments across the probable K–Pg boundary. Samples were collected along a tributary of the Kawaruppu River, where a muddy sequence of the upper Kawaruppu Formation is exposed, and the presence of the K–Pg boundary is suggested from a preliminary geochemical investigation. The S-ratio, which is a measure of the relative contribution of high- and low-coercivities to the saturation isothermal remanent magnetization (SIRM), and the ‘hard’ IRM (HIRM), which is a measure of the absolute contribution of high-coercivity minerals to the remanent magnetization, both imply a broadly coarsening-upward trend across the probable K–Pg boundary. On the other hand, the pattern of the stratigraphic variation in the low-field magnetic susceptibility (MS) appears to be different between the upper and lower parts across the probable K–Pg boundary; the MS data show a cyclic variation of 50–60-m wavelength below and a steady decrease above. This change's cause is unclear, but this change may be related to paleoenvironmental changes at the K–Pg boundary.