Paleontological Evidence for a Northward Shift of the Climate Zone During the Qin and Han Dynasties—A Case of Paleontology from Lake Deposits in the Salawusu River Basin, Mu Us Desert, China

The lacustrine horizon (thickness of 8.75 cm thick) of the Qin and Han dynasties (221 BC–220 AD) was determined based on AMS-14C analysis conducted by the Beta Analytic Radiocarbon Dating Laboratory on the Dishaogouwan section (37°43′ N, 108°31′ E) in the Salawusu River Basin, Mu Us Desert, located in the temperate zone of China. The identification results of the ostracod and charophyta fossils from the four samples at this horizon show the following results: 1. All the samples contain 458 ostracod fossil valves, belonging to six genera and eight species. Their quantity (valves) and percentage, in descending order of abundance, are Candoniella albicans (Brady), 255/55.68%, Ilyocypris bradyi Sars, 73/15.94%, Eucypris inflata Sars, 46/10.04%, Cyclocypris serena Koch, 26/5.68%, Candona kirgizica Mandelstam, 18/3.93%, Ilyocypris biplicata (Koch), 17/3.71%, Candoniella mirabilis Schneider14/3.06% and Leucocytherella sinensis Huang, 6/1.31%. 2. All the samples contain 99 fossil charophyte gyrogonites, belonging to one genera and four species. In terms of quantity/percentage, the Chara sp. is the most abundant, with 41 pieces (41.41%), followed by Chara braunii Gemlin, with 26 pieces (26.26%); Chara leptosperma Braun and Chara canescens Loiseleur account for 19 pieces (19.19%) and 13 pieces (13.13%), respectively. Based on the analysis of the ecological environment of the existing species of these ostracods and charophytes, combined with the fossilized Ilyocypris brady, Ilyocypris biplicata, and Gyraulus convexiusculus Hutton found in all the samples—which indicate very warm, even subtropical climates then—it can be concluded that during the Qin and Han Dynasties, the Salawusu River Basin was primarily characterized by a freshwater lake environment under a warm climate, with the average annual temperature and precipitation in this area approximately 2.1 °C and 100 mm higher than they are currently. The prevailing East Asian summer monsoon pushed the warm temperate climate at least 110 km northwestward from this basin. During this period, there were at least four episodes of brief subtropical climate fluctuations, occurring approximately every 110 years.