Trends in the occurrence of human and veterinary antibiotics in the sediments of the Yellow River, Hai River and Liao River in northern China

2011 ◽  
Vol 159 (7) ◽  
pp. 1877-1885 ◽  
Author(s):  
Li-Jun Zhou ◽  
Guang-Guo Ying ◽  
Jian-Liang Zhao ◽  
Ji-Feng Yang ◽  
Li Wang ◽  
...  
2017 ◽  
Vol 97 ◽  
pp. 19-30 ◽  
Author(s):  
Jing Fu ◽  
Hisashi Yokoyama ◽  
Baoshan Cui ◽  
Jin Zhou ◽  
Jiaguo Yan ◽  
...  

2016 ◽  
Vol 85 (2) ◽  
pp. 290-298 ◽  
Author(s):  
Shuzhen Peng ◽  
Qingzhen Hao ◽  
Luo Wang ◽  
Min Ding ◽  
Wei Zhang ◽  
...  

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.


The Holocene ◽  
2020 ◽  
pp. 095968362094114
Author(s):  
Liu Yang ◽  
Minmin Ma ◽  
Tingting Chen ◽  
Yifu Cui ◽  
Panpan Chen ◽  
...  

The introduction of wheat into China between ~4500 and 4000 cal. a BP is thought to have restructured the ancient Chinese agricultural system and contributed to the formation and development of Chinese civilization. However, the spatial variation in agricultural development before and after the introduction of exotic crops across the Yellow River valley has not yet been discussed in detail. Here, we report new archaeobotanical data and radiocarbon dates from 25 sites in Sanmenxia, Henan Province, which was a hub for human migration in the middle reach of the Yellow River. Integrating our data with those of other archaeobotanical studies in northern China confirms that spatial cropping patterns in the Yellow River valley changed significantly around 4000 cal. a BP in the context of trans-Eurasia exchanges. From 7000 to 4000 cal. a BP, millet crops in the upper and middle Yellow River valley dominated the agricultural system, while mixed millet and rice agriculture developed in the lower Yellow River valley. In the subsequent period (4000–2200 cal. a BP), the cropping system in the upper Yellow River valley changed predominantly to barley and wheat agriculture, supplemented with millets. The contemporaneous cropping system in the middle and lower Yellow River valley, however, was dominated by millets, supplemented with wheat and rice. We argue that technological innovation and its dissemination in the context of trans-Eurasian cultural exchanges provided the basis for changes in the agricultural systems in northern China during the Bronze Age. Additionally, the trajectory of agricultural development was influenced by the natural environment and social change in different regions of the Yellow River valley.


Sign in / Sign up

Export Citation Format

Share Document