Japan Geoscience Union Meeting 2021

Presentation information

[J] Poster

M (Multidisciplinary and Interdisciplinary) » M-IS Intersection

[M-IS16] Paleoclimatology and paleoceanography

Sat. Jun 5, 2021 5:15 PM - 6:30 PM Ch.23

convener:Yusuke Okazaki(Department of Earth and Planetary Sciences, Graduate School of Science, Kyushu University), Hitoshi Hasegawa(Faculty of Science and Technology, Kochi University), Atsuko Yamazaki(Faculty of Science, Kyushu University), Akitomo Yamamoto(Japan Agency for Marine-Earth Science and TechnologyAtmosphere and Ocean Research Institute)

5:15 PM - 6:30 PM

[MIS16-P27] Millennial-scale cyclicities recorded in the Cretaceous lacustrine core using Monte Carlo approach

*Hitoshi Hasegawa1, Hirofumi Asahi2 (1.Faculty of Science and Technology, Kochi University, 2.Center for Advanced Marine Core Research, Kochi University)

Keywords:Varve, Millennial-scale cyclicity, Age uncertainty, Monte Carlo approach

Detail paleoclimatic records under exceptionally warm “hothouse” condition provide crucial insights toward future climate predictions. However, climatic variations in millennial-scale at such deep-time archives commonly faces difficulties owing to the large uncertainties of absolute age at more than hundred kyr-scale. Annually laminated lacustrine deposits of Early Aptian (ca. 123–119 Ma) in southeast Mongolia firstly enable to obtain millennial- and shorter time-scale climate variability at such immemorial period. By combining μm-scale analysis of fluorescence microscopy images (seasonal resolution) and ultra-high-resolution elemental XRF scanning techniques (~1–5 year resolution), we were able to generate a continental climate record of unrivalled temporal resolution. Age model of the subject core was established at annual- to decadal time-scale, taking account a casual relation of ITRAX elemental composition and (annually formed) varve thickness. FFT power spectrum of high temporal resolution and long duration ITRAX record, with consideration of maximum age uncertainties (Monte-Carlo approach), exhibit partial presences of millennial-scale extreme drought events during the mid-Cretaceous ‘hothouse’ periods.