日本地球惑星科学連合2014年大会

講演情報

インターナショナルセッション(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-PT02_1AM1] Biocalcification and the Geochemistry of Proxies

2014年5月1日(木) 09:00 〜 10:45 421 (4F)

コンビーナ:*豊福 高志(独立行政法人海洋研究開発機構)、北里 洋(独立行政法人海洋研究開発機構海洋・極限環境生物圏領域)、Bijma Jelle(アルフレッドウェゲナー極域海洋研究所)、座長:北里 洋(独立行政法人海洋研究開発機構海洋・極限環境生物圏領域)

10:30 〜 10:45

[BPT02-P01_PG] 造礁性サンゴ骨格の結晶組織が示すaragoniteとhaliteの共沈

ポスター講演3分口頭発表枠

*甕 聡子1永井 隆哉1川野 潤2渡邊 剛1 (1.北海道大学大学院理学院、2.北海道大学創成研究機構)

キーワード:reef-building coral, calcification, biomineral, aragonite

In the last JpGU Meeting, we reported halite grains in coral skeleton through the observation of massive coral skeleton of Porites lobata by Analysis Transmission Electron Microscope (ATEM). Each halite grain typically shows a square shape and its grain size is around 80 nm. The spatial distribution of halite grains is inhomogeneous and seems to be independent on the arrangement of growth lines.
We observed new evidence that the halite grains in coral skeleton could precipitate during coral calcification. The electron diffraction patterns from some selected areas including both an aragonite and a halite grain show that there are special crystallographic orientation relationships between them. In consideration of misfit ratios between some selective bond lengths of halite and those of aragonite, crystallographic orientations of halite and aragonite seem to be a kind of hetero-epitaxial relationship.
This is the first observation for a primary precipitated mineral phase other than aragonite in coral skeletons. The halite phase in coral skeleton will provide a new perception for understanding the process of coral calcification.