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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:来自圣卡塔琳娜州的全新世岩心的孢粉学数据

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ABSTRACT 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:摘要本文通过对巴西南部加罗帕巴(圣卡塔琳娜州)市的全新世时代沉积岩芯的孢粉学分析,提出了古环境重建。在450厘米长的PCSC-3岩心中,总共收集了46个样品用于孢粉分析,另外还有3个样品用于放射性碳年代测定和粒度分析。孢粉的组成包括84个与被子植物的花粉粒(38)和裸子植物(3),蕨类植物的孢子(16)和苔藓植物的孢子(2),真菌的孢子(8),藻类(3),雌性植物(3),鞭毛藻囊肿(2)和有孔虫壁(1)。描述并详细说明了三位头像专家。根据组合的变化定义了三个孢粉学阶段:第一阶段,第二阶段和第三阶段。 I期的特征是从沉积开始(5390 cal yr BP)开始就有海洋影响的泻湖古环境,其基础是尖锐湿疣,鞭毛藻囊肿和有孔虫的衬里。 II期(3032年BP到858 cal BP)也具有泻湖古环境的特征,但是,海洋元素的百分比减少,淡水藻类记录增加,表明海洋对泻湖体的影响较小。在第三阶段(过去856年)中,在类似沼泽的条件下普遍存在水下沉积。

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