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首页> 外文期刊>Quaternary International >An exploratory Early and Middle Holocene sedimentary record with palynoforms and diatoms from Faiyum lake, Egypt
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An exploratory Early and Middle Holocene sedimentary record with palynoforms and diatoms from Faiyum lake, Egypt

机译:探索性的全新世早期和中期沉积记录,其中有埃及Faiyum湖的粉状和硅藻

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We report on the sedimentology, pollen and diatom records in a 26 m long core of Holocene sediments from the Tersa area, near the centre of the Faiyum Depression (Egypt). Two radiocarbon and one OSL dates have been obtained for the core, dates range from 9545 +/- 60 Cal. BP to c. 4040 BP. These correspond respectively with the Terminal Palaeolithic (Qarunian) and Neolithic Faiyum A (Faiyumian) cultures. The core is subdivided into 3 sedimentological units: unit 1 (21-26 m) is very thinly laminated, calcareous silt deposited in a deep water lake; unit 2 (9.5-21 m) is finely laminated sand, silt and carbonates formed as a lacustrine fan delta; unit 3 (9.5 m to the core top), is formed of massive silt, sandy silt and very fine grained flood plain sands. Planktonic diatom taxa, mainly Cyclostephanos, Aulacoseira, Cyclotella and Stephanodiscus spp. were abundant in units 1 & 2-a, indicating deep, open lake conditions. Magnetic minerals increased from the base of unit 2 indicating an increasing contribution of Nile alluvium. Benthic taxa such as Fragilaria, Cocconeis, Amphora and Navicula tended to increase towards the core top, from unit 2-b; 3-a to 3-b, indicative of lake shallowing and periods of low Nile floods. Unit 3-c is barren of diatoms and is compatible with terrestrial flood plain conditions. Vegetation was mainly represented by herbaceous pollen throughout most of the core and in the topmost sediment, pollen was scarce but pteridophyte (Osmundaceae) spores increased. Arboreal vegetation had low percentages in most of the record but increased in the middle section of the core (unit 2). A depositional deltaic environment was indicated throughout most of the core (sub-units 2-a & 3-a), where high abundances of Poaceae, Cyperaceae, Chenopodiaceae, Amaranthaceae, Polypodiaceae and Osmundaceae were recorded, indicating high Nile floods and fluctuating rainfall. (C) 2015 Elsevier Ltd and INQUA. All rights reserved.
机译:我们报告了在Faiyum凹陷(埃及)中心附近的Tersa地区26 m长的全新世沉积岩心中的沉积学,花粉和硅藻记录。岩心已获得两个放射性碳和一个OSL数据,数据范围为9545 +/- 60 Cal。 BP到C。 4040 BP。这些分别对应于旧石器时代的末代(Qarunian)和新石器时代的Faiyum A(Faiyumian)文化。岩心分为3个沉积学单元:第1单元(21-26 m)是非常薄的层状钙质粉砂沉积在深水湖中。 2号机组(9.5-21 m)是由细沙,粉砂和碳酸盐组成的精细层压而成的湖扇形三角洲。 3号单元(距岩心顶部9.5 m)由块状粉砂,沙质粉砂和细粒洪泛平原砂形成。浮游硅藻类群,主要是Cyclostephanos,Aulacoseira,Cyclotella和Stephanodiscus spp。 1和2-a单元中的水含量很高,表明湖水处于深水,开放的状态。磁性矿物从单元2的底部开始增加,表明尼罗河冲积层的贡献增加。底栖类群,例如Fragilaria,Cocconeis,Amphora和Navicula倾向于从2-b单元向核心顶部增加。 3-a至3-b,表示湖泊变浅和尼罗河洪水泛滥的时期。 3-c单元贫瘠的硅藻,与陆地洪水平原条件兼容。植被的主要特征是在整个岩心的大部分区域都具有草本花粉,在最顶层的沉积物中,花粉稀少,而蕨类植物(Osmundaceae)的孢子却增加了。在大部分记录中,乔木植被的百分比较低,但在核心的中部(单元2)有所增加。在整个核心区域(2-a和3-a子单元)的大部分区域均显示出沉积三角洲环境,记录下禾本科,莎草科,藜科,A菜科,Poly科和O科的丰度很高,这表明尼罗河洪水泛滥且降雨波动。 (C)2015 Elsevier Ltd和INQUA。版权所有。

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