Knowledge Resource Center for Ecological Environment in Arid Area
DOI | 10.1016/j.quaint.2019.11.030 |
Carbonate crusts of Paleolake Zhuyeze, Tengeri Desert, China: Formation mechanism and paleoenvironmental implications | |
Sun, Qingfeng1; Zamanian, Kazem2; Li, Yanrong3; Wang, Hong4,5; Colin, Christophe6; Sun, Haixia1 | |
通讯作者 | Sun, Qingfeng |
来源期刊 | QUATERNARY INTERNATIONAL
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ISSN | 1040-6182 |
EISSN | 1873-4553 |
出版年 | 2019 |
卷号 | 532页码:157-165 |
英文摘要 | Carbonate crusts with unusual morphologies are scattered on the Holocene sand surface, i.e., dunes, which cover the Paleolake Zhuyeze bed in the Tengeri Desert, China. Two types of the crusts were identified. The first type contained fossilized wrinkles of plant root cortex, while the second type consisted of hollow chambers without the wrinkle features. Optical microscopy, scanning electron microscopy and cathodoluminescence analyses were performed to investigate the mineralogy and geochemistry of the crusts. Fossilized cortex texture imprints on the first type of crusts suggested that the crusts formed around the deceased rhizomes of reeds (Phragmites communis) as the nuclei of encrustation. Weakly oxidizing soil-sediment with rhizome was a prerequisite, which was favorable for rhizome decomposition to produce sufficient CO2 and HCO3- and generate carbonate minerals of encrustation on rhizome surfaces, with lake water as the main Ca2+ supply. A conceptual formation mechanism of the encrustation was conjectured. Similar to the formation mechanism of the first type, another type of crusts with chambers and without fossilized imprints of the cortex textures formed around the spherical rhizomes of Scirpus maritimus. The crust characteristics and other evidence suggested that the lake water was fresh; water plants, such as P. communis and S. maritimus, and snails previously inhabited the water; and encrustation reflected a stable, slow-oxidizing soil-sediment environment. These desert crusts provided insights to study paleoecology, paleohydrology and water-soil/sediment interface environment in the paleolake. |
英文关键词 | Carbonate crusts Aquatic plant roots Soil and sediment Encrustation mechanism Paleoenvironment Paleolake |
类型 | Article |
语种 | 英语 |
国家 | Peoples R China ; Germany ; USA ; France |
收录类别 | SCI-E |
WOS记录号 | WOS:000502533000014 |
WOS关键词 | CALCRETE LAMINAR CRUSTS ; CALCAREOUS ROOT TUBES ; SHIYANG RIVER-BASIN ; TENGGER DESERT ; FERROMANGANESE NODULES ; ENVIRONMENTAL-CHANGES ; MAJOR CONTRIBUTOR ; SHELL CARBONATE ; ORGANIC-MATTER ; LAKE EVOLUTION |
WOS类目 | Geography, Physical ; Geosciences, Multidisciplinary |
WOS研究方向 | Physical Geography ; Geology |
EI主题词 | 2019-11-10 |
来源机构 | 北京师范大学 ; E17 |
资源类型 | 期刊论文 |
条目标识符 | http://119.78.100.177/qdio/handle/2XILL650/310805 |
作者单位 | 1.Northwest Normal Univ, Fac Geog, Lanzhou 730070, Gansu, Peoples R China; 2.Georg August Univ Goettingen, Dept Soil Sci Temperate Ecosyst, Buesgenweg 2, D-37077 Gottingen, Germany; 3.Taiyuan Univ Technol, Dept Earth Sci & Engn, Taiyuan 030024, Shanxi, Peoples R China; 4.Beijing Normal Univ, Interdisciplinary Res Ctr Earth Sci Frontier, Beijing 100875, Peoples R China; 5.Univ Illinois, Prairie Res Inst, Illinois State Geol Survey, Champaign, IL 61820 USA; 6.Univ Paris Sud, Univ Paris Saclay, Lab Geosci Paris Sud, CNRS,UMR 8148, Batiment 504, F-91405 Orsay, France |
推荐引用方式 GB/T 7714 | Sun, Qingfeng,Zamanian, Kazem,Li, Yanrong,et al. Carbonate crusts of Paleolake Zhuyeze, Tengeri Desert, China: Formation mechanism and paleoenvironmental implications[J]. 北京师范大学, E17,2019,532:157-165. |
APA | Sun, Qingfeng,Zamanian, Kazem,Li, Yanrong,Wang, Hong,Colin, Christophe,&Sun, Haixia.(2019).Carbonate crusts of Paleolake Zhuyeze, Tengeri Desert, China: Formation mechanism and paleoenvironmental implications.QUATERNARY INTERNATIONAL,532,157-165. |
MLA | Sun, Qingfeng,et al."Carbonate crusts of Paleolake Zhuyeze, Tengeri Desert, China: Formation mechanism and paleoenvironmental implications".QUATERNARY INTERNATIONAL 532(2019):157-165. |
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