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Paleoenvironmental evolution of the coastal plain of Southern Brazil: palynological data from a Holocene core in Santa Catarina State

机译:巴西南部沿海平原的古环境演变:圣达塔琳娜州全新世核心的宫颈数据

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摘要

This paper presents a paleoenvironmental reconstruction from palynological analyses of a sedimentary core of Holocene age, drilled at municipality of Garopaba (Santa Catarina), Southern Brazil. A total of 46 samples was collected for palynological analyses in the 450 cm-long core PCSC-3, as also three samples for radiocarbon dating and granulometric analyses. The palynological content includes 84 taxa related to pollen grains of angiosperms (38) and gimnosperm (3), spores of pteridophyta (16) and bryophyta (2), spores of fungi (8), algae (3), acritarchs (3), dinoflagellate cysts (2) and microforaminiferal linings (1). Three specimens of acritarchs are described and illustrated in detail. Three palynological phases were defined based on changes in assemblages: Phase I, Phase II and Phase III. The Phase I is characterized as a lagoonal paleoenvironment with marine influence from the beginning of the sedimentation (5390 cal yr BP), based on occurrences of acritarchs, dinoflagellate cysts and microforaminiferal linings. The Phase II (3032 yr BP until 858 cal yr BP) also is characterized by a lagoonal paleoenvironment, however, presented decrease in percentage of marine elements and increase in freshwater algae record, suggesting less marine influence in the lagoonal body. In Phase III (last 856 years), underwater sedimentation prevailed, under swamp-like conditions.
机译:本文介绍了全新世时代沉积核心沉积核心的古环境重建,在巴西南部Garopaba(Santa Catarina)的沉积核心钻探。在450cm-Long核心PCSC-3中收集共有46个样品,用于450cm-Long核心PCSC-3,也是Radiocarbon Datering和粒度分析的三个样品。腭核含量包括84个与花粉颗粒有关的Angiosperms(38)和Gimnosperm(3),蕨类植物孢子(16)和苔藓藻(2),孢子(8),藻类(3),Acritarchs(3), Dinoflagellate囊肿(2)和微多氧化物衬里(1)。详细描述和说明了三种Antritarchs标​​本。基于组装的变化定义了三个腭相关:II,II期和III期。该阶段I的特征是,基于沉积物(5390 Cal Yr BP)的沉积物的开始,基于Acritarchs,Dinoflageate囊肿和微食物衬里的发生,该阶段是遗传古环境。 II期(3032 YR BP直到858只CAL YR BP)还具有泻湖古环境,然而,近期海洋元素的百分比减少,淡水藻类的增加,表明LAGOONAL体内的海洋影响更少。在沼泽状条件下,在第三阶段(过去856岁)中,水下沉降普遍存在。

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  • 作者单位

    Univ Fed Rio Grande do Sul Programa Posgrad Geociencias Inst Geociencias Lab Palinol Marleni Marques Toigo Dept Paleontol Av Bento Goncalves 9500 BR-91540000 Porto Alegre RS Brazil;

    Univ Fed Rio Grande do Sul Programa Posgrad Geociencias Inst Geociencias Lab Palinol Marleni Marques Toigo Dept Paleontol Av Bento Goncalves 9500 BR-91540000 Porto Alegre RS Brazil;

    Univ Fed Rio Grande do Sul Programa Posgrad Geociencias Inst Geociencias Lab Palinol Marleni Marques Toigo Dept Paleontol Av Bento Goncalves 9500 BR-91540000 Porto Alegre RS Brazil;

    Univ Fed Rio Grande do Sul Programa Posgrad Geociencias Inst Geociencias Lab Palinol Marleni Marques Toigo Dept Paleontol Av Bento Goncalves 9500 BR-91540000 Porto Alegre RS Brazil;

    Univ Fed Rio Grande do Sul Programa Posgrad Geociencias Inst Geociencias Lab Palinol Marleni Marques Toigo Dept Paleontol Av Bento Goncalves 9500 BR-91540000 Porto Alegre RS Brazil;

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  • 原文格式 PDF
  • 正文语种 eng
  • 中图分类 自然科学总论;
  • 关键词

    coastal plain; environmental evolution; Holocene; palynology; Santa Catarina;

    机译:沿海平原;环境进化;全新世;Palynology;圣卡塔琳娜;

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