[M-IS10] 古気候・古海洋変動

[MIS10-30] Application of ramped pyrolysis ¹⁴C method to postglacial sediment in the Chukchi-Alaskan margin, western Arctic Ocean.

*鈴木 健太¹、山本 正伸^1,2、Rosenheim Brad³、大森 貴之⁴、Polyak Leonid⁵、南 承一⁶ (1.北海道大学大学院環境科学院、2.北海道大学大学院地球科学研究院、3.南フロリダ大学海洋科学大学、4.東京大学総合研究博物館、5.オハイオ州立大学バード極地研究所、6.韓国極地研究所)

The Arctic Ocean underwent dramatic climate changes in the past. Changes in sea-ice extent and ocean currents in the Arctic Ocean cause changes in surface albedo and deep water formation, which drove global climatic changes. However, Arctic paleoceanographic studies have been limited compared to the other oceans due to chronostratigraphic difficulties. One of the reasons for this is absence of material suitable for ¹⁴C dating in the Arctic Ocean sediments deposited since the last glacial maximum. To enable improved age constraints for sediments impoverished in datable material, we apply ramped pyrolysis ¹⁴C method (Rosenheim et al., 2008) to sedimentary records from the Chukchi-Alaska margin recovering Holocene to late-glacial deposits. Samples were divided into five fraction products by gradual heating sedimentary organic carbon from ambient room temperature to 900°C. The thermographs show a trimodal pattern of organic matter decomposition over temperature, and we consider that CO₂ generated at the lowest temperature range was derived from autochthonous organic carbon contemporaneous with sediment deposition, similar to studies in the Antarctic margin and elsewhere. For verification of results, some of the samples treated for ramped pyrolysis ¹⁴C were taken from intervals dated earlier by AMS ¹⁴C using bivalve shells. The ages of lowest temperature split showed older ages than the radiocarbon ages derived from bivalve shells indicating that those splits were still mixtures and not pure autochthonous organic matter. The relationship between radiocarbon ages of generated gas and pyrolysis temperature is linear. We used this empirical relationship to determine the optimal temperature yielding pure marine organic carbon and estimated age of horizons by sampling at those temperatures. We compare these ages to mixing model ages decoupling the simpler mixtures represented by our original low-temperature splits, which were consistent with the bivalve ages.