Uptake of alkaline earth metals in Alcyonarian spicules (Octocorallia)

详细信息	查看全文 | 推荐本文 |

• 作者：I. Taubner^a ; ^{itaubner@geomar.de} ; F. Bö ; hm^a ; A. Eisenhauer^a ; D. Garbe-Schö ; nberg^b ; J. Erez^c
• 刊名：Geochimica et Cosmochimica Acta
• 出版年：2012
• 期刊代码：27_00167037
• 类别：ear
• 出版时间：1 May, 2012
• 卷：84
• 期：Complete
• 页码：239-255
• 文件大小：1289 K

摘要

Alcyonarian corals (Octocorallia) living in shallow tropical seas produce spicules of high-Mg calcite with 鈭?3 mol%MgCO₃. We cultured the tropical alcyonarian coral Rhythisma fulvum in experiments varying temperature (19-32 掳C) and pH (8.15-8.44). Alkalinity depletion caused by spicule formation systematically varied in the temperature experiments increasing from 19 to 29 掳C. Spicules were investigated for their elemental ratios (Mg/Ca, Sr/Ca) using ICP-OES, 未^44/40Ca using TIMS, as well as 未¹⁸O and 未¹³C by IRMS. Mg/Ca increased with temperature from 146 to 164 mmol/mol, in good agreement with the range observed for marine inorganic calcite. Mg/Ca increased by 1.0 卤 0.4 mmol/mol/掳C, similar to the sensitivity of Miliolid foraminifera. The pH experiments revealed a linear relationship between Mg/Ca and carbonate ion concentration of +0.03 卤 0.02 mmol/mol/渭Mol. Sr/Ca ranges from 2.5 to 2.9 mmol/mol being in good agreement with other high-Mg calcites. Temperature and pH experiments showed linear dependencies of Sr/Ca matching inorganic calcite trends and pointing to a decoupling of crystal precipitation rate and calcification rate. Ca isotopes range between 0.7鈥?and 0.9鈥?in good agreement with aragonitic scleractinian corals and calcitic coccoliths. Presumably Ca isotopes are fractionated by a biological mechanism that may be independent of the skeletal mineralogy. We observe no temperature trend, but a significant decrease of 未^44/40Ca with increasing pH. This inverse correlation may characterise biologically controlled intracellular calcification. Oxygen isotope ratios are higher than expected for isotopic equilibrium with a temperature sensitivity of 鈭?.15 卤 0.03鈥?掳C. Carbon isotope ratios are significantly lower than expected for equilibrium and positively correlated with temperature with a slope of 0.20 卤 0.04鈥?掳C.

Many of our observations on trace element incorporation in R. fulvum may be explained by inorganic processes during crystal formation, which do not comply with the intracellular mode of calcification in Alcyonarian corals. The observed elemental and isotopic compositions, however, could be explained if the partitioning caused by biological mechanisms mimics the effects of inorganic processes.