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首页> 外文期刊>Acta Botanica Brasilica >Plant succession in a forest on the Lower Northeast Slope of Serra Geral, Rio Grande do Sul, and Holocene palaeoenvironments, Southern Brazil
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Plant succession in a forest on the Lower Northeast Slope of Serra Geral, Rio Grande do Sul, and Holocene palaeoenvironments, Southern Brazil

机译:巴西南部南里奥格兰德州和全新世古环境的东北下坡森林中的植物演替

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The study of plant succession provides information on vegetation dynamics of a region and, therefore, improves our understanding of the natural trends of present ecosystems. With this objective, plant succession based on palynology of a sediment profile in a swamp forest was studied on the Lower Northeast Slope of Serra Geral, Rio Grande do Sul. Samples were treated with HCl, HF, KOH and acetolysis; slides were mounted in glycerol-jelly. For each sample a minimum of 500 grains of pollen + pteridophyte and bryophyte spores was counted and other palynomorphs were counted in parallel. Tilia and Tilia Graph software were used to construct percentage and concentration diagrams, with three 14C datings. The results show a local water reservoir in the beginning of the Holocene (± 9800 yrs. BP), creating a herbaceous plant marsh by hydrosere. The initial colonization of the marsh by trees occurred about 8800 yrs. BP, with tropical species from the Coastal Plain migrating in an east-west direction. Afterwards, there was a dry phase between 7000-5000 yrs. BP. The second appearance of regional tree species began at about 5000 yrs. BP, resulting in the present forest and in the west-east migration of tropical species from interior lowlands, like this one, to re-colonize the coast after the last marine regression.
机译:对植物演替的研究提供了有关某个地区植被动态的信息,因此提高了我们对当前生态系统自然趋势的理解。为此目的,在南里奥格兰德州塞拉杰拉尔的东北下坡上研究了基于沼泽沉积物的孢粉学的植物演替。样品用HCl,HF,KOH和乙解处理;将载玻片固定在甘油冻中。对于每个样品,至少计数了500粒花粉+蕨类植物和苔藓植物孢子,并同时计数了其他孢粉。使用Tilia和Tilia Graph软件构建带有三个14C日期的百分比和浓度图表。结果表明,在全新世初期(±9800 yrs。BP),当地有一个水库,通过水耕形成了草本植物沼泽。树木最初在沼泽中定植的时间约为8800年。 BP,沿海平原的热带物种向东西方向迁移。之后,在7000-5000年之间出现了干燥阶段。 BP。区域树种的第二次出现始于大约5000年。 BP,导致了目前的森林和热带内陆低地热带物种的西迁,如上图所示,在上次海洋退化之后重新定居了海岸。

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