日本地球惑星科学連合2023年大会

講演情報

[J] オンラインポスター発表

セッション記号 M (領域外・複数領域) » M-IS ジョイント

[M-IS15] 古気候・古海洋変動

2023年5月25日(木) 10:45 〜 12:15 オンラインポスターZoom会場 (22) (オンラインポスター)

コンビーナ:岡崎 裕典(九州大学大学院理学研究院地球惑星科学部門)、長谷川 精(高知大学理工学部)、山崎 敦子(名古屋大学大学院環境学研究科)、小長谷 貴志(東京大学大気海洋研究所)

現地ポスター発表開催日時 (2023/5/23 17:15-18:45)

10:45 〜 12:15

[MIS15-P20] Establishment of Highly Accurate Age Model Using Radiocarbon Dating of Fossil Pollen Automatically Extracted from Lake Motosu Sediments

★Invited Papers

*太田 耕輔1,2横山 祐典1,2,3,4,5宮入 陽介1オブラクタ スティーブン6山本 真也7、Hubert-Ferrari A.8、V.M.A. Heyvaert9,10、M. De Batist10藤原 治11 (1.東京大学大気海洋研究所、2.東京大学理学系研究科地球惑星科学専攻、3.東京大学大学院総合文化研究科環境科学専攻、4.海洋研究開発機構、5.オーストラリア国立大学物理学研究科、6.秋田大学大学院国際資源科学研究科、7.山梨県富士山科学研究所、8.リエージュ大学地理学科、9.ベルギー王立自然科学研究所地質調査所、10.ゲント大学地質学部、11.産業技術総合研究所地質調査総合センター)

キーワード:放射性炭素、湖底堆積物、花粉

Lacustrine sediments record continuous paleoenvironmental changes, and depending on the location, may also record instantaneous event such as volcanic eruptions. Lakes are also often well-suited to provide highly accurate geochronological information, making them key archives for paleoclimate research. In the absence of annually laminated sediments, terrestrial macrofossils, such as leaves and plant fragments, are often relied upon for radiocarbon dating because they are deposited quickly after fixing atmospheric carbon dioxide. Therefore, unlike bulk sediments, no corrections of the carbon reservoir effect are necessary. However, deposition is sporadic, and leaves may be sparse. In addition, in oxidative benthic environments, leaves and plant fragments may decompose quickly after deposition. Pollen, on the other hand, offer a unique solution because they are composed of sporopollenin, a persistent molecule that is typically universally present in lacustrine sediments. The drawback is that the number of needed grains (~50,000) for radiocarbon dating in prohibitively high for manual extraction.
Here we present a novel solution to this problem by using a cell sorter with a newly designed pretreatment method and an improved extraction method to extract pollen fossils. This enables us to extract large pollen fossils (~150 µm) than what was previously possible. These are then measured using a single-stage accelerator mass spectrometer (AMS) at the Atmosphere and Ocean Research Institute, University of Tokyo.
We then apply this method to sediments recovered from Lake Motosu, which already has a very robust chronology, to evaluate the new method. Results indicate that the method is both successful and increases the accuracy of the Lake Motosu chronology by a factor between 1.5 and 3.5. Results also better clarify variations in the reservoir age of the lake, which were previously estimated from the ages of known widespread tephra deposited in the lake.