Spatially variable provenance of the Chinese Loess Plateau

Loess sequences of the Chinese Loess Plateau (CLP) compose one of the most complete Neogene–Quaternary terrestrial paleoclimatic archives. Understanding the CLP’s sediment sources is critical to tracing Asian aridification, atmospheric circulation patterns, and Asian monsoon evolution. Commonly, the sediments that compose the Quaternary strata of the CLP are considered largely homogeneous, and thus numerous studies have applied a uniform source model when attempting to use CLP-derived proxies as paleoclimate indicators. Here we present large-n detrital zircon U-Pb geochronology data from the Quaternary CLP. These data support spatial variability in sediment provenance across the CLP. At least three distinct provenance zones are recognized for Quaternary loess strata: central western, eastern, and northeastern. These zones received sediment primarily from their neighboring river systems. This finding conflicts with the classic views that attribute the Quaternary loess principally to the deserts north and west of the CLP. We conclude that fluvial processes, and thus precipitation, played an important and previously underemphasized role in Quaternary dust production in northern China. Furthermore, nonuniformity in CLP Quaternary sediment provenance raises questions about the validity of using paleoclimate information archived in the CLP to make sweeping regional interpretations.

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Geochemical and grain-size evidence for the provenance of loess deposits in the Central Shandong Mountains region, northern China

Quaternary Research ◽

10.1016/j.yqres.2016.01.005 ◽

2016 ◽

Vol 85 (2) ◽

pp. 290-298 ◽

Cited By ~ 20

Author(s):

Shuzhen Peng ◽

Qingzhen Hao ◽

Luo Wang ◽

Min Ding ◽

Wei Zhang ◽

...

Keyword(s):

Grain Size ◽

Loess Plateau ◽

Major Element ◽

Yellow River ◽

Northern China ◽

Chinese Loess Plateau ◽

The Yellow River ◽

Chinese Loess ◽

Loess Deposits ◽

The Chinese Loess Plateau

Widespread loess deposits in the Central Shandong Mountains yield valuable paleoclimatic records for this currently semi-humid monsoonal region of northern China. The grain-size distribution and major element composition for bulk samples and two grain-size fractions (< 20 and 20–63 μm) for the loess in the Central Shandong Mountains were compared with loess from the Chinese Loess Plateau and sediment from the Yellow River to help determine its provenance. The presence of a significant percentage of medium- and coarse-silt, and the difference in relatively immobile major element ratios of TiO2/Al2O3 and K2O/Al2O3 for the < 20 and 20–63 μm fractions, suggests that sediment that forms the loess deposits in the Central Shandong Mountains was not blown directly from the northern deserts of China as is the case for the loess deposits of the Chinese Loess Plateau. Rather, this suggests that sediments exposed during glacial times on the North China fluvial plain, including the floodplain of the Yellow River, were the major dust source for the loess in the Central Shangong Mountains. In addition, the wide distribution of perimontane loess in the Central Shandong Mountains region indicates the occurrence of strengthened local aridification during glacial times since the middle Pleistocene.

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SPATIAL ANALYSIS AND COMPARISON OF TEMPERATURE AND PRECIPITATION IN THE AMERICAN MIDWEST, EUROPE, AND THE CHINESE LOESS PLATEAU USING CLUMPED ISOTOPE THERMOMETRY

10.1130/abs/2017am-308017 ◽

2017 ◽

Author(s):

Hayley Bricker ◽

◽

Jace Bricker ◽

Bryce A. Mitsunaga ◽

John Mering ◽

...

Keyword(s):

Spatial Analysis ◽

Loess Plateau ◽

Chinese Loess Plateau ◽

Chinese Loess ◽

American Midwest ◽

Temperature And Precipitation ◽

Clumped Isotope ◽

The Chinese Loess Plateau

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Changes in soil water holding capacity and water availability following vegetation restoration on the Chinese Loess Plateau

Scientific Reports ◽

10.1038/s41598-021-88914-0 ◽

2021 ◽

Vol 11 (1) ◽

Author(s):

Yong-wang Zhang ◽

Kai-bo Wang ◽

Jun Wang ◽

Changhai Liu ◽

Zhou-ping Shangguan

Keyword(s):

Land Use ◽

Soil Water ◽

Loess Plateau ◽

Soil Layer ◽

Soil Physical Properties ◽

Chinese Loess Plateau ◽

Land Use Type ◽

Chinese Loess ◽

Water Holding ◽

The Chinese Loess Plateau

AbstractChanges in land use type can lead to variations in soil water characteristics. The objective of this study was to identify the responses of soil water holding capacity (SWHC) and soil water availability (SWA) to land use type (grassland, shrubland and forestland). The soil water characteristic curve describes the relationship between gravimetric water content and soil suction. We measured the soil water characteristic parameters representing SWHC and SWA, which we derived from soil water characteristic curves, in the 0–50 cm soil layer at sites representing three land use types in the Ziwuling forest region, located in the central part of the Loess Plateau, China. Our results showed that the SWHC was higher at the woodland site than the grassland and shrubland, and there was no significant difference between the latter two sites, the trend of SWA was similar to the SWHC. From grassland to woodland, the soil physical properties in the 0–50 cm soil layer partially improved, BD was significantly higher at the grassland site than at the shrubland and woodland sites, the clay and silt contents decreased significantly from grassland to shrubland to woodland and sand content showed the opposite pattern, the soil porosity was higher in the shrubland and woodland than that in the grassland, the soil physical properties across the 0–50 cm soil layer improved. Soil texture, porosity and bulk density were the key factors affecting SWHC and SWA. The results of this study provide insight into the effects of vegetation restoration on local hydrological resources and can inform soil water management and land use planning on the Chinese Loess Plateau.

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