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Analysis of historical trend of carotenoid concentrations in sediment cores from Lake Shinji, Japan

机译:日本新治湖沉积岩心中类胡萝卜素浓度的历史趋势分析

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The historical trend of the concentrations of carotenoids originating from phytoplankton in sediment cores collected at two sites in Lake Shinji, a eutrophic oligohaline lake was investigated to clarify the changes in phytoplankton community structures in the lake over the last 100 years. Eight kinds of carotenoids were detected in the sediments, i.e., astaxanthin and lutein from chlorophytes, alloxanthin from cryptophytes, canthaxanthin, echinenone and zeaxanthin from cyanobacteria, diatoxanthin from diatoms, and β-carotene from unspecified algal groups. On the basis of the stoichiometric relation between total organic carbon (TOC) and total sulfur (TS), the historical changes in the TOC concentration of sediment cores since circa 1970 have been attributable to the decomposition of organic matter by sulfate reduction, confirming the importance of diagenetic processes in Lake Shinji sediments. It was found that labile chlorophyll a is transformed diagenetically to more stable pheophytin a and pyropheophytin a within the upper 5 cm of the cores. Similarly, the concentrations (μg g~(-1) TOC) of carotenoids, other than diatoxanthin, in the cores decreased rapidly within this zone, and in the cores lower than 5 cm below lake floor, their concentrations showed a decreasing or fixed trend with depth. This suggests that these carotenoids have been degraded in sediments depending on their stabilities. Among the diatoxanthin, lutein and zeaxanthin of which the stability is similar, the relative abundance of lutein (chlorophytes) has increased since circa 1970, and, conversely, the relative abundance of diatoxanthin (diatoms) has decreased. Diatoms are likely a staple food for the shellfish Corbicula japonica in Lake Shinji, because they are rich in lipids, which are needed for the growth and survival of C. japonica. Hence, the relative decrease in the number of diatoms may have some effect on the decrease in the population of C. japonica since the 1970s in the lake.
机译:研究了富营养化的盐卤湖新治湖两个地点收集的沉积物核心中浮游植物中类胡萝卜素浓度的历史趋势,以阐明过去100年该湖中浮游植物群落结构的变化。在沉积物中检测到八种类胡萝卜素,即绿藻类植物中的虾青素和叶黄素,隐藻类植物中的Alloxanthin,蓝藻中的角黄素,海胆烯酮和玉米黄质,硅藻中的重钙黄素和未指明的藻类中的β-胡萝卜素。根据总有机碳(TOC)与总硫(TS)的化学计量关系,自1970年左右以来沉积物核心TOC浓度的历史变化可归因于硫酸盐还原法分解的有机物,这证实了其重要性济湖沉积物中的成岩作用过程已经发现,不稳定的叶绿素a在核心的上部5 cm内通过双电导转化为更稳定的脱镁叶绿素a和焦脱镁叶绿素a。同样,在该区域内,岩心中除地黄素外的类胡萝卜素浓度(μgg〜(-1)TOC)迅速下降,在湖床以下5 cm以下的岩心中,其浓度呈下降或固定趋势。与深度。这表明这些类胡萝卜素已根据其稳定性在沉积物中降解。在稳定性相似的地黄质黄素,叶黄素和玉米黄质中,叶黄素(绿藻类)的相对丰度自1970年左右以来有所增加,反之,地黄质的相对丰度(硅藻类)却有所降低。硅藻可能是Shinji湖贝类Corbicula japonica的主食,因为它们富含脂质,这是C. japonica的生长和生存所必需的。因此,自1970年代以来,硅藻数量的相对减少可能对日本锦葵的种群减少有一定影响。

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