日本地球惑星科学連合2021年大会

講演情報

[J] 口頭発表

セッション記号 M (領域外・複数領域) » M-IS ジョイント

[M-IS16] 古気候・古海洋変動

2021年6月5日(土) 09:00 〜 10:30 Ch.26 (Zoom会場26)

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(九州大学大学院理学研究院)、山本 彬友(国立研究開発法人 海洋研究開発機構)、座長:山本 彬友(国立研究開発法人 海洋研究開発機構)

10:00 〜 10:15

[MIS16-15] Reconstruction of Early Pleistocene sea-surface temperature in the Northwestern Pacific Ocean based on calcareous microfossils

*桑野 太輔1、土屋 祐貴2、大浦 佑馬1、林 広樹3、久保田 好美4、万徳 佳菜子5、亀尾 浩司1 (1.千葉大学、2.名古屋大学、3.島根大学、4.国立科学博物館、5.国立環境研究所)


キーワード:石灰質ナノ化石、浮遊性有孔虫化石、モダンアナログ、古海洋学、更新世、上総層群

Planktonic foraminifera and calcareous nannofossils have been used to clarify past marine environments based on relationships between distributions of living taxa and sea-water conditions (e.g., Takemoto and Oda, 1997; Aizawa et al., 2004). In this study, we reconstruct the sea surface temperature (SST) based on the Modern Analog Technique (MAT) of calcareous microfossil assemblages. The MAT is a useful method for reconstructing SST by comparing the similarity between fossil and modern assemblages (e.g., Pflaumann et al., 1996). Around the Pacific coast of Japanese islands, many surface sediments have been obtained by grab sampler and piston corer, and the modern microfossil assemblages of those have been studied (e.g., Tanaka, 1991). We apply the MAT to 27 samples of the upper part of the Kiwada Formation, Kazusa Group, obtained by Kuwano et al. (in press). We estimated the SST by calculating the squared chord distance (SCD) between fossil and modern assemblages, subsequently taking the weighted temperature average of the top five samples with the highest similarity. The modern foraminiferal and nannofossil assemblage dataset were obtained from Takemoto and Oda (1997) and Tanaka (1991), respectively. The modern SST dataset was used in July from the Japan Oceanographic Data Center (2004).
The reconstructed SST tends to be high during interglacial, and the summer SST ranged between 23.4 and 27.7 ℃. On the other hand, during the glacial Marine Isotope Stage (MIS) 38, the SSTs temporarily dropped by 1–2 ℃. This sea-surface variation is similar to that of planktonic foraminiferal δ18O change although the nannofossil SSTs were sharp declines rather than planktonic δ18O changes in some horizons.

[Reference]
Aizawa et al., 2004, Marine Micropaleontology, 52, 277–297.
Japan Oceanographic Data Center, 2004, https://jdoss1.jodc.go.jp/vpage/bts_j.html
Kuwano et al., in press, Stratigraphy.
Pflaumann et al., 1996, Paleoceanography, 11, 15–35.
Takemoto and Oda, 1997, Paleontological research, 1, 291–310.
Tanaka, 1991, Sci. Rep., Tohoku Univ., 2nd ser. (Geol.), 61, 127-198.