Arid
DOI10.1007/s10933-017-0007-7
Geochemical imprints of coupled paleoenvironmental and provenance change in the lacustrine sequence of Orog Nuur, Gobi Desert of Mongolia
Yu, Kaifeng1,3,4; Lehmkuhl, Frank1; Diekmann, Bernhard2; Zeeden, Christian1; Nottebaum, Veit1; Stauch, Georg1
通讯作者Yu, Kaifeng
来源期刊JOURNAL OF PALEOLIMNOLOGY
ISSN0921-2728
EISSN1573-0417
出版年2017
卷号58期号:4页码:511-532
英文摘要

In the arid environment, due to the scarcity of a continuous terrestrial archive, lacustrine sequences are often employed as a paleoenvironmental repository. However, numerous spatial and temporal heterogeneities exist concerning previously studied sites in arid central Asia. Furthermore, surveys using a XRF core scanning technique on lacustrine sequences retrieved in hyperarid desert settings are largely rare. Hence, two parallel sediment cores (ONW I; ONW II) were retrieved from Orog Nuur, in the Gobi Desert of Mongolia. Continuous, high-resolution elemental abundances at a 1-cm scanning step size were examined in core ONW II using XRF core scanning. To constrain the data quality, elements with high error margins relative to measured peak areas and those elements/proxies below the significance level during the multivariate statistics are excluded for environmental/provenance implications. Based on multivariate statistical evaluation, the bulk-geochemistry of the core sediments are governed by (1) grain-size composition, (2) authigenic productivity (Ca, Cl, CaCO3) in an alkaline environment, (3) allochthonous organic material (TOC and C/N-atomic), and (4) terrigenous input via fluvial inflows, as well as quasi-constant aeolian input through the late Quaternary (Al, Si, K, Ti, and Fe). Disparate source lithotypes, as well as authigenic productivity of the lake system existed before and after Termination I. The Holocene was dominated by a distinct high productivity alkaline environment with more felsic and alkaline input relative to the late Pleistocene. This might be attributed to an increased hydrodynamic strength of riverine inflow and/or intensified erosion and weathering of felsic source rocks in the upper catchment of the Orog Nuur. Therefore, in order to gain a better understanding of the bulk-geochemistry of lake sediments, the coupled provenance and environmental signatures, as well as land surface processes in the catchment need to be systematically discerned. Thus, the XRF core scanning data obtained in this study would have practical and complimentary merit for other lacustrine studies focused on the desert realm across the globe.


英文关键词XRF core scanning Orog Nuur Provenance Grain size Late Quaternary Gobi Desert
类型Article
语种英语
国家Germany ; Peoples R China
收录类别SCI-E
WOS记录号WOS:000414421600006
WOS关键词RADIOCARBON AGE CALIBRATION ; MOISTURE EVOLUTION ; CENTRAL-ASIA ; NW CHINA ; MU-XRF ; SEDIMENTS ; CORE ; HOLOCENE ; BASIN ; FLUCTUATIONS
WOS类目Environmental Sciences ; Geosciences, Multidisciplinary ; Limnology
WOS研究方向Environmental Sciences & Ecology ; Geology ; Marine & Freshwater Biology
资源类型期刊论文
条目标识符http://119.78.100.177/qdio/handle/2XILL650/200711
作者单位1.Rhein Westfal TH Aachen, Dept Geog, Templergraben 55, D-52056 Aachen, Germany;
2.Helmholtz Ctr Polar & Marine Res, Alfred Wegener Inst, Telegrafenberg A43, D-14473 Potsdam, Germany;
3.Global Energy Interconnect Dev & Cooperat Org, Energy & Climate Change Div, 8 Inner Xuanwumen Str, Beijing 100031, Peoples R China;
4.Chinese Acad Sci, Nanjing Inst Geog & Limnol, State Key Lab Lake Sci & Environm, 73 East Beijing Rd, Nanjing 210008, Jiangsu, Peoples R China
推荐引用方式
GB/T 7714
Yu, Kaifeng,Lehmkuhl, Frank,Diekmann, Bernhard,et al. Geochemical imprints of coupled paleoenvironmental and provenance change in the lacustrine sequence of Orog Nuur, Gobi Desert of Mongolia[J],2017,58(4):511-532.
APA Yu, Kaifeng,Lehmkuhl, Frank,Diekmann, Bernhard,Zeeden, Christian,Nottebaum, Veit,&Stauch, Georg.(2017).Geochemical imprints of coupled paleoenvironmental and provenance change in the lacustrine sequence of Orog Nuur, Gobi Desert of Mongolia.JOURNAL OF PALEOLIMNOLOGY,58(4),511-532.
MLA Yu, Kaifeng,et al."Geochemical imprints of coupled paleoenvironmental and provenance change in the lacustrine sequence of Orog Nuur, Gobi Desert of Mongolia".JOURNAL OF PALEOLIMNOLOGY 58.4(2017):511-532.
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