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Palaeolimnological evidence of environmental change over the last 400 years in the Rwenzori Mountains of Uganda

机译:乌干达Rwenzori山区近400年环境变化的古生物学证据

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Tropical alpine areas may be highly sensitive to climate change. Yet, because high-resolution palaeoenvironmental studies in these regions are scant, patterns of environmental change over the last few centuries, and linkages with regional changes, remain poorly resolved. This article presents a 400-year palaeolimnological record from Lower Kitandara Lake (3,989 m above m.a.s.l.), located in the Rwenzori Mountains of Uganda, where marked glacial recession has been recorded over much of the twentieth century. An age model is produced for a 57.5 cm sediment core based on Pb-210 and C-14 dating, suggesting a basal date of approximately 1600 AD. Diatom and organic geochemistry (%TOC, C/N ratios, delta C-13) analyses are carried out at an approximately decadal resolution. Twentieth-century glacial recession does not appear to have significantly impacted either the diatom or geochemical records. However, large ecological changes have occurred during the past 400 years, particularly shown by the diatom fluxes and geochemical data. Throughout the core, the diatom record reveals only minor changes in assemblage composition, which may be related to the dominance of Staurosira construens var. venter in the lake's diatom flora, a tychoplanktonic taxon which is highly adaptive to environmental change. Geochemical analyses, however, reveal a marked change at around the end of the eighteenth century, when C/N ratios suggest an increase in the dominance of algal aquatic sources to lacustrine organic matter, concomitant with a stabilisation of catchment inputs and increased diatom productivity, which may have been caused by reduced glacial inputs. The relationship between these changes at Lower Kitandara Lake and wider regional climate change that occurred at the end of the eighteenth century is not well understood, but this study highlights the need for additional research to link drivers of alpine ecosystem change with those operating at low altitudes.
机译:热带高山地区可能对气候变化高度敏感。但是,由于这些地区的高分辨率古环境研究很少,因此过去几个世纪以来环境变化的模式以及与区域变化的联系仍然难以解决。本文介绍了位于乌干达Rwenzori山脉的Lower Kitandara湖(高于a.s.l.的3,989 m)的400年古孢子学记录,在整个20世纪的大部分时间里都记录到明显的冰川衰退。根据Pb-210和C-14测年建立了一个57.5 cm沉积物芯的年龄模型,表明基础日期约为1600 AD。硅藻和有机地球化学(%TOC,C / N比,C-13增量)分析的分辨率约为十年。二十世纪的冰川衰退似乎并未对硅藻或地球化学记录产生重大影响。但是,在过去的400年中,发生了巨大的生态变化,硅藻通量和地球化学数据尤其表明了这一点。在整个岩心中,硅藻记录仅显示出组合物组成中的细微变化,这可能与恒星Staurosira construens var的优势有关。湖泊的硅藻区系中的通风器,是一种对环境变化具有高度适应性的梯形浮游生物分类群。然而,地球化学分析显示,在18世纪末,当C / N比值表明藻类水生源对湖相有机物的优势度增加时,伴随着集水量输入的稳定和硅藻生产率的提高,这可能是由于冰川输入减少所致。较低的Kitandara湖的这些变化与18世纪末发生的更广泛的区域气候变化之间的关系尚未得到很好的了解,但这项研究强调了需要进行更多研究,以将高山生态系统变化的驱动因素与在低海拔地区运行的那些因素联系起来。

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