JpGU-AGU Joint Meeting 2020

講演情報

[E] 口頭発表

セッション記号 B (地球生命科学) » B-PT 古生物学・古生態学

[B-PT04] Biomineralization and Geochemistry of Proxies

コンビーナ:豊福 高志(国立研究開発法人海洋研究開発機構)、Jelle Bijma(アルフレッドウェゲナー極域海洋研究所)、北里 洋(国立大学法人東京海洋大学)、廣瀬 孝太郎(早稲田大学  大学院創造理工学研究科 地球・環境資源理工学専攻)

[BPT04-03] Effects of larger benthic foraminifers from global warming analysed by Micro-X-ray CT

*木下 峻一1黒柳 あずみ2西 弘嗣2佐々木 理2藤田 和彦3鈴木 淳4川幡 穂高5 (1.東北大学大学院理学研究科、2.東北大学総合学術博物館、3.琉球大学、4.産業技術総合研究所、5.東京大学)

キーワード:大型底生有孔虫、マイクロCT、有孔虫殻、飼育実験、地球温暖化

Studying calcification organisms are essential for understanding environmental changes in the tropical to subtropical seas. Although symbiont-bearing larger benthic foraminifers (LBF) is one of important calcification organism with complex calcium carbonate shells living in coral reefs. They produce plentiful calcium carbonate following to reef corals and calcareous algae in coral reef area. However, the relationships between foraminiferal shell calcification and SST are not cleared yet because it was difficult to measure and calculate foraminiferal shell volume accurately, due to the tiny size and complexity of their shell form. Thus, this study tried to analyze responses of the symbiont-bearing LBF to global warming by culturing experiment in laboratory with means of Micro-X-ray CT investigations.

In this study, we cultured asexually reproduced individuals of Sorites orbiculus under six different temperature conditions to examine the effects of SST on calcium carbonate producing of LBF. Experimental results with 12 weeks culturing indicated that increasing rates of shell weight, shell volume and the number of chambers added were generally increase with temperature increasing from 19 °C to 27 °C. On the other hand, calculated shell density is in constant in whole range of experiment temperature. Due to these results, it was suggested that shell weight was most closely dependent upon their shell volume. Their increasing rates of shell weight and shell volume were reversed their trends and decreasing at 29 °C, despite their growth rate of number of chambers added was still in constant from 27 °C to 29 °C. Therefore, the optimum temperatures for their chamber growth rate and calcification rate might be showed some deviation. This deviation might be caused by deviation of optimum temperatures of LBF and their photosynthesis symbionts. Finally, in future predicted global warming will be disturbed LBF calcification.