Japan Geoscience Union Meeting 2024

Presentation information

[E] Poster

P (Space and Planetary Sciences ) » P-EM Solar-Terrestrial Sciences, Space Electromagnetism & Space Environment

[P-EM11] Space Weather and Space Climate

Mon. May 27, 2024 5:15 PM - 6:45 PM Poster Hall (Exhibition Hall 6, Makuhari Messe)

convener:Ryuho Kataoka(National Institute of Polar Research), Mary Aronne(NASA Goddard Space Flight Center), Yumi Bamba(National Institute of Information and Communications Technology), Antti Pulkkinen(NASA Goddard Space Flight Center)

5:15 PM - 6:45 PM

[PEM11-P16] Annual 10Be record in travertine covering 1510-1701: a new proxy for reconstructing annual solar activity

Hongyang Xu2, *Hiroko Miyahara1, Kazuho Horiuchi3, Hiroyuki Matsuzaki4, Xi Zhao2, Hailing Gan2, Weijun Luo5, Michael E. Meadows6, Xiangmin Zheng2, Limin Zhou2 (1.Musashino Art University, 2.East China Normal University, 3.Hirosaki University, 4.The University of Tokyo, 5.Chinese Academy of Sciences, 6.University of Cape Town)

Keywords:Travertine, Cosmogenic nuclide, Solar activity, Galactic cosmic rays, Beryllium-10

Previous research has revealed that the 10Be record in laminated travertine has significant potential for reconstructing past high-resolution solar activity. However, the depositional processes of atmospheric 10Be into travertine have not been fully resolved, and thus the methodology for extracting the production signal has not been established. In this study, we present an annually resolved 10Be record from Baishuitai travertine covering 1510-1701 CE, along with environmental proxies, discuss the potential influence of climatic/environmental variations on the travertine 10Be record, and propose an improved correction methodology for extracting the atmospheric 10Be production signal from the travertine. We show that 10Be deposition in travertines has two environmental impacts: the transport efficiency of atmospheric 10Be into travertine and the additional 10Be inflow from overland flow caused by rainfall. We demonstrate that these effects can be corrected based on iron and potassium contents and that the resulting corrected record reasonably agrees with ice-core and tree-ring data, indicating that 10Be in travertine can be a good proxy for probing the past annual solar activity.