Hyun Jung-Ho
Department of Environmental Marine Sciences, Hanyang University, 1271 Sa-1 dong, Ansan, Gyeonggi-do 426-791, South Korea.
Microb Ecol. 2006 Aug;52(2):244-52. doi: 10.1007/s00248-006-9012-5. Epub 2006 Aug 5.
Shipboard enrichment incubation experiments were performed to elucidate the limiting resources for heterotrophic prokaryotic production and to discuss the potential impact of bottom water and sediment discharges in relation to manganese (Mn) nodule exploitation on the heterotrophic prokaryotes in the oligotrophic northeast equatorial Pacific. Compared to an unamended control, the production of heterotrophic prokaryotes increased 25-fold in water samples supplemented with amino acids (i.e., organic carbon plus nitrogen), whereas the production increased five and two times, respectively, in samples supplemented with either glucose or ammonium alone. These results indicate that heterotrophic prokaryote production in the northeast equatorial Pacific was co-limited by the availability of dissolved organic carbon and inorganic nitrogen. In samples from the nutrient-depleted surface mixed layer (10-m depth), the addition of a slurry of bottom water and sediment doubled heterotrophic prokaryote production compared to an unamended control, whereas sonicating the slurry prior to addition quadrupled the production rate. However, little difference was observed between an unamended control and slurry-amended samples in the subsurface chlorophyll a (Chl a) maximum (SCM) layer. Thus, the impact of slurry discharge is more significant at the nutrient-depleted surface mixed layer than at the high-nutrient SCM layer. The greatly enhanced prokaryote production resulting from the addition of sonicated slurry further suggests that dissociated organic carbon may directly stimulate heterotrophic prokaryote production in the surface mixed layer. Overall, the results suggest that the surface discharge of bottom water and sediments during manganese nodule exploitation could have a significant environmental impact on the production of heterotrophic prokaryotes that are currently resource limited.
开展了船上富集培养实验,以阐明异养原核生物生产的限制资源,并探讨与锰结核开采相关的底层水和沉积物排放对贫营养的东北赤道太平洋异养原核生物的潜在影响。与未添加营养物的对照相比,添加氨基酸(即有机碳加氮)的水样中异养原核生物的产量增加了25倍,而仅添加葡萄糖或铵的样品中产量分别增加了5倍和2倍。这些结果表明,东北赤道太平洋异养原核生物的生产受到溶解有机碳和无机氮可用性的共同限制。在营养耗尽的表层混合层(10米深度)的样品中,添加底层水和沉积物的泥浆后,与未添加营养物的对照相比,异养原核生物的产量增加了一倍,而在添加前对泥浆进行超声处理使产量增加了四倍。然而,在次表层叶绿素a(Chl a)最大值(SCM)层中,未添加营养物的对照样品和添加泥浆的样品之间几乎没有差异。因此,泥浆排放对营养耗尽的表层混合层的影响比对高营养SCM层的影响更大。添加经超声处理的泥浆后原核生物产量大幅提高,这进一步表明解离的有机碳可能直接刺激表层混合层中异养原核生物的生产。总体而言,结果表明,锰结核开采过程中底层水和沉积物的表层排放可能会对目前资源有限的异养原核生物的生产产生重大环境影响。