摘要 : Culture experiments with living planktic foraminifers reveal that the ratio of boron to calcium (B/Ca) in Orbulina universa increases from 56 to 92μmolmol~(-1) when pH is raised from 7.61+/-0.02 to 8.67+/-0.03 (total scale). Acros... 展开 Culture experiments with living planktic foraminifers reveal that the ratio of boron to calcium (B/Ca) in Orbulina universa increases from 56 to 92μmolmol~(-1) when pH is raised from 7.61+/-0.02 to 8.67+/-0.03 (total scale). Across this pH range, the abundances of carbonate, bicarbonate, and borate ions also change (+530, -500, and +170μmolkg~(-1), respectively). Thus specific carbonate system control(s) on B/Ca remain unclear, complicating interpretation of paleorecords. B/Ca in cultured O. universa also increases with salinity (55-72μmolmol~(-1) from 29.9-35.4‰) and seawater boron concentration (62-899μmolmol~(-1) from 4-40ppm B), suggesting that these parameters may need to be taken into account for paleorecords spanning large salinity changes (~ 2‰) and for samples grown in seawater whose boron concentration ([B]_(SW)) differs from modern by more than 0.25ppm. While our results are consistent with the predominant incorporation of the charged borate species BOH4-into foraminiferal calcite, the behavior of the partition coefficient K_D (defined as [B/Ca]_(calcite)/BOH4-/HCO3-_(seawater)) cannot be explained by borate incorporation alone, and suggests the involvement of other pH-sensitive ions such as CO_3~(2-) For a given increase in seawater B(OH)_(4-), the corresponding increase in B/Ca is stronger when B(OH)_(4-) is raised by increasing [B]_(SW) than when it is raised by increasing pH. These results suggest that B incorporation controls should be reconsidered. Additional insight is gained from laser-ablation ICP-MS profiles, which reveal variable B/Ca distributions within individual shells. 收起