[M-IS26] 生物地球化学

[MIS26-02] 海水と鉱物とのリアルな反応連繋：　サンゴ礁の生態

*市川 和彦¹、服田 昌之² (1.前院地球環境科学院、北大、2.理学部生物学、お茶の水大学)

キーワード：石灰化, 海の生き物, リアルな反応連繋, プロトンダイナミクス, 物質収支

We need to elucidate which marine calcifying organisms can carry out the actual fixation of atmospheric carbon dioxide or not. The carbon dioxide species dissolved into seawaters are starting material of reversible reaction between calcification and decalcification. In our bottom-up research the real enhanced skeleton formation was actually observed from individual primary corals to each tubular colony. The proton transfer in coral reef-building seawaters controls all reversible acid/base dissociation reactions (Chem. Eur. J. 2014, 20, 13656-13661*). After the true real reactions among different chemical species in seawaters were identified on the basis of material energetics and biology of marine calcifying organisms, a reasonable overall reaction should be estimated as material balance. From our data of base/acid titration (Chem. Eur. J. 2007, 13, 10176-10181**), light microscope observation and culture experiment*) it was become clear that the enhanced skeleton production of each coral polyp skeleton and each colony is controlled by reversible reaction between calcification and decalcification, Ca²⁺ + HCO₃^- U CaCO₃ + H⁺. Here solubility product [Ca²⁺][HCO₃^-] is much larger than [Ca²⁺][CO₃^2-] for reversible equation Ca²⁺ + CO₃^2- U CaCO₃. Our idea*) of proton dynamics demonstrated the increase of [Ca²⁺], and the decrease of major [HCO₃^-] and minor [CO₃^2-] with decreasing pH at a given P_CO2 and 〜7.8 < pH < 〜8.4. Thus stable variation of seawater pH over geological and laboratory timescales is actually real in reef-building seawaters under no anthropogenic influence on atmospheric carbon dioxide. *) Suwa, Hatta and Ichikawa. **) Ichikawa.