Abstract
Previous studies on the amplitude of East Asian summer monsoon (EASM) changes mainly focused on northern China (represented by the Loess Plateau). However, a rare investigation centered on the subtropical zone of southern China, where the important route for EASM moved northward or southward, especially addressing a lack of the research on mammals. The Ailuropoda-Stegodon fauna is a representative mammal fauna in southern China since the late Pleistocene. It indicates the southern mid-subtropical-tropical forest environment with tropical climate characteristics, and its southward or northward movements in the subtropical zone imply the changes of EASM intensity. Based on previous research, combined with the species characteristics and distribution range of the Ailuropoda-Stegodon fauna with tropical animals during the marine isotope stage 5 (MIS5), MIS3, MIS2, and MIS1 Megathermal periods, this paper mainly investigates its evolution and the fluctuations of EASM. The conclusions include: (1) The distribution geometric centers in the MIS5, MIS3, MIS2, and MIS1 Megathermal periods are (26°14′N, 111°22′E), (24°35′N, 107°30′E), (22°48′N, 112°01′E), and (26°19′N, 112°25′E), respectively. (2) Compared with the MIS5 period, the EASM of the MIS3 and MIS2 moved 180 km and 380 km southwards, and that of the MIS1 Megathermal period moved about 10 km northwards. The EASM movement indicated by the fauna migration happened synchronous with the climate records of stalagmites in subtropical China, the sporopollen from eastern China, and oxygen isotopes from Sulu Sea. They also correspond to the peaks and valleys of the total solar radiation at 35°N in the winter half-year. This suggests that the migrations of the Ailuropoda-Stegodon fauna are consistent with the changes of the global climate, and the driving force is mainly from the changes of total solar radiation at 35°N in the winter half-year.
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14C Laboratory of Archaeology, Department of History in Peking University, 14C Laboratory of the Institute of Archaeology in CASS (1982) Reliability of radiocarbon dates of samples collected from limestone regions and the age of the Zengpiyan and Xianrendong prehistoric sites. Acta Archaeol Sin (2): 243–250. (In Chinese)
An ZS (2000) The history and variability of the East Asian paleomonsoon climate. Quaternary Sci Rev 19(1–5): 171–187. https://doi.org/10.1016/S0277-3791(99)00060-8
An ZS, Kukla G, Porter SC, et al. (1991) Magnetic susceptibility evidence of monsoon variation on the Loess Plateau of central China during the last 130 000 years. Quaternary Res 36(1): 29–36. https://doi.org/10.1016/0033-5894(91)90015-W
An ZS, Liu TS, Lu YC, et al. (1990) The long term paleomonsoon variation recorded by the loess-paleosol sequence in central China. Quatern Int 7–8: 91–95. https://doi.org/10.1016/1040-6182(90)90042-3
Cai BQ (1999) Late Pleistocene mammalian fossils and paleogeographic environment in the Taiwan Strait. J Xiamen Univ(Arts & Soc Sci) (4): 29–33. (In Chinese)
Cao KQ (1982) Vertebrate fossils in Shanghai. Shanghai Geology (2): 50–55. (In Chinese)
Chen DZ, Qi GQ (1978) Hominid fossil and its symbiotic mammals remains from Xichou, Yunnan province. Vertebr Palasiat 16(1): 34–46. (In Chinese)
Chen SX, Wang JK, Zhong YM, et al. (1995) Study on the amino acid ages of fossils teeth and mixed-deposition phenomenon in some caves. Acta Sci Nat Univ Sunyatseni 7(3): 89–94. (In Chinese)
Cheng H, Edwards RL, Sinha A, et al. (2016) The Asian monsoon over the past 640 000 years and ice age terminations. Nature 534(7609): 640–646. https://doi.org/10.1038/nature18591
Chinese natural geographical editorial board of the CAS (1979) Chinese natural geography-animal geography. Science Press. pp 51–70. (In Chinese)
Dansgaard W, Johnsen SJ, Clausen HB, et al. (1993) Evidence for general instability of past climate from a 250-kyr ice-core record. Nature 364: 218–220. https://doi.org/10.1038/364218a0
Fan XC, Zheng GZ (2006) Archaeological finding and research of Quaternary mammal fossils in Fujian. Science Press. pp 1–200. (In Chinese)
Foose TJ, Strien NV (1997) Asian Rhinos-Status survey and conservation action plan. Gland, Switzerland, and Cambridge, UK: IUCN, 1–40.
Geheyan Archaeological Team of Qingjiang in Hubei Province, The Hubei Provincial Institute of Cultural Relics and Archaeology (2004) Qingjiang Archaeology, Science Press, Beijing, China. pp 6–24. ISBN: 9787030141521. (In Chinese)
Grant KM, Rohling M, Matthews MB, et al. (2012) Rapid coupling between ice volume and polar temperature over the past 150000 years, Nature 491: 744–747. https://doi.org/10.1038/nature11593
Han DF, Zhang SS (1978) A canine fossil found in Jiande and new evidence of Quaternary mammal fossils in Zhejiang. Vertebr Palasiat 16(4): 255–263. (In Chinese)
Zong GF, Huang XS (1985) Remains of Early Holocene Cultural Relics and Mammals in Pupiao, Baoshan, Yunnan. Prehistory (4): 46–50. (In Chinese)
Huang JF (2009) A brief history of the evolution of Chinese Rhinoceros, Ph.D Thesis. Shanxi Normal University, Xi’an, China. (In Chinese)
Huang WB (1963) Notes on the cave and cave-deposits in Kaoyao, Loting and Fengkai district, Kwangtung. Vertebr Palasiat 3(1): 79–83. (In Chinese)
Huang WB (1979) The nature and ages for the South China cave fauna. Vertebr Palasiat 17(4): 327–343. (In Chinese)
Huang WB (2000) Cave deposit and fissure—filling sequence of China. Quat Sci 3(2): 155–164. (In Chinese)
Huang WB, Ji HX (1963) Note on Holocene Hsienjen Cave deposit of Wannian, Kiangsi. Vertebr Palasiat 7(3): 263–272. (In Chinese)
Huang ZG, Zhang WQ (2000) The shift of tropical zone during the Last Glacial Maximum in China. Acta Geogr Sin 55(5): 587–595. (In Chinese)
Huang ZG, Zhang WQ (2006) The Quaternary Faunas and climatic fluctuation in tropical China. Trop Geogr 2(1): 5–11. (In Chinese)
Huang ZG, Zhang WQ, Jiang LM (2003) Climatic characteristics in tropic areas of China during MIS3. Quat Sci 23(1): 77–82. (In Chinese)
Janis C (1984) Tapirs as living fossils. In: Eldredge N, Stanley SV(eds.), Living Fossils. New York: Springer-Verlag. pp 80–86.
Ji HX (1982) The living environment of the quteranary mammalian faunas in South China. VertebrPalasiat 20(2): 147–154. (In Chinese)
Jiang XY, Chen G (1985) 14C age of cave sediments in Guilin. In: The Geographical Society of China(ed.), Karst Landforms and Caves. pp 130–141. Science Press, Beijing ISBN: 130312797. (In Chinese)
Jiang YJ (1992) A study on mammalia fauna of late Pleistocene in the Karst Caves of Guangxi. Carsol Sin 3(1): 38–42. (In Chinese)
Jin CZ, Pan WS, Zhang YQ, et al. (2009) The Homo sapiensCave hominin site of Mulan Mountain, Jiangzhou District, Chongzuo, Guangxi with emphasis on its age. Chin Sci Bull 54(19): 2848–2856. (In Chinese)
Jin DS, Zheng F (1993) Palaeoclimate in the coastal area of central Fujian in 120 000 years BP. Geol of Fujian 12(3): 218–226. (In Chinese)
Jin JH, Wang YY, Zhang ZH (2004) The quaternary Ailuropoda-Stegodon fauna of Lechang, Guangdong. Acta Sci Nat Univ Sunyatseni 7(4): 95–101. (In Chinese)
Li BS, Bian GG, Zhang W, et al. (2007) New discovery of the Late Pleistocene mammal fossils in Dongjiang River Valley, South of Nanling Range, China. Acta Geol Sin 9(9): 1195–1199. (In Chinese)
Li BS, Wen XH, Zhang DD, et al. (2008) Paleoclimate change recorded in the red earth and brown-yellow sediment of Late Quaternary for northeastern part of Guangdong Province, south to the Nanling Mountains, China. Chin Sci Bull 53(24): 3866–3875. https://doi.org/10.1007/s11434-008-0421-3
Li WM, Zhang ZF, Gu YM, et al. (1982) A fauna from Lianhua Cave, Dantu, Jiangsu. Acta Anthropol Sin 1(2): 169–179. (In Chinese)
Li YH, Wu ML, Peng SL, et al. (1984) The unearthed human teeth fossils and contemporary mammalian fauna in Tubo of Liujiang, Guangxi province. Acta Anthropol Sin 3(4): 322–329. (In Chinese)
Li YX, Lei CY (1980) Fossil mammals from Lishui, Jiangsu. Vertebr Palasiat 18(1): 59–64. (In Chinese)
Li ZW, Li BS, Sun L, et al. (2015) Paleontologicl evidence for the north movement of Mid-subtropical during the OIS 5e period in southern China. Quat Sci 35(3): 712–720. (In Chinese)
Liang ZT, Li YX (1959) The investigations for the Maba Man site and preliminary observation for human fossil skulls. Acta Sci Nat Univ Sunyatseni (1–2): 136–146. (In Chinese)
Linsley BK (1996) Oxygen-isotope record of sea level and climate variations in the Sulu Sea over the past 150000 years. Nature 38: 234–237. https://doi.org/10.1038/380234a0
Liu ZY (2003) The origin of rice farming in China from the comparative analysis of Yuchanyan and Niulan cave. Agric Archaeol (1): 76–88. (In Chinese)
Liuzhou Museum, Guangxi Cultural Relics Working Group (1983) Neolithic shell mound site of liyuzui in Dalongtan, Liuzhou City. Archaeol (9): 769–774. (In Chinese)
Mitchell A (2005) The ESRI Guide to GIS Analysis, Volume 2. ESRI Press.
Pan YJ, Shen GJ, Fang YS (2002) U-series dating of fossil teeth from lianhua cave in Zhenjiang, Jiangsu Province. Acta Anthropol Sin 21(2): 155–157. (In Chinese)
Peng PX, Li BS, Bian GG, et al. (2011) Re-study of mammal fossils of the Bishou Cave in Dongjiang River Valley, Southern Nanling Mountains, China. Acta Geol Sin 85(11): 2031–2038. (In Chinese)
Qi GQ, He CK (1999) Quaternary fauna of Penghu trench in Taiwan and its paleogeographic environment. Quat Sci (2): 71. (In Chinese)
Qiu LC, Song FY, Wang LH (1982) Excavation of Neolithic artifacts in dushizai cave site, Yangchun, Guangdong. Archaeol (5): 456–459. (In Chinese)
Reimer PJ, Baillie MGL, Bard E, et al. (2009) IntCal09 and Marine09 radiocarbon age calibration curves, 0–50,000 years cal BP. Radiocarbon 51: 1111–1150. https://doi.org/10.2458/azu_js_rc.55.16947
Shen GJ, Wang W, Wan Q, et al. (2001) U-series dating of hominid site ganqian cave at Tubo, Liujiang, Guangxi in South China. Acta Anthropol Sin 20(3): 238–244. (In Chinese)
Shreshta VP (2007) A Concise Geography of Nepal. Climate. Kathmandu: Mandal Publications.
Shi YF, Kong ZC, Wang SM, et al. (1992) The characteristics of climate and environment during Holocene mega warm period in China. In: Shi YF, Kong ZC (eds.), Climate and Environment of Holocene Megawarm Period in China. pp1–18. Ocean Press, Beijing ISBN 7502729720. (In Chinese)
Song FY, Zhang ZH, Deng ZK, et al. (1992) Excavation brief of Huangyuan Cave of Fengkai in 1989 and 1990, Guangdong. Southeast Cult 1: 148–156. (In Chinese)
Sun G, Xu Q, Jin K, et al. (1998) The historical withdrawal of Wild Elephas maximus in China and its relationship with human population pressure. J Northeast For Univ 26(4): 47–50. (In Chinese)
Tang LY, Shen CM (1992) Vegetation and climate during the Holocene high temperature in northern Jiangsu. In: Shi YF, Kong ZC(Eds.), Climate and Environment of Holocene Megawarm Period in China. pp 80–93. Ocean Press, Beijing ISBN: 7502729720. (In Chinese)
Tong HW (2007) Warm likes animals and their paleoenvironmental significance occurred in northern China since the Quaternary. Sci China Ser D 37(7): 922–933. (In Chinese)
Tong HW (2013) The southward migration of Quaternary mammalian fauna in China. In: Proceedings of the 11th National Congress and 27th Annual Meeting of the Palaeontological Society of China. pp 246. University of Chinese Academy of Sciences, Beijing. (In Chinese)
Training Class of Cultural Relics and Archaeology in Guangxi, Guangxi Cultural Relics Working Group (1975) Neolithic shell mound sites in Nanning, Guangxi. Archaeol 5: 295–301. (In Chinese)
Wang JK, Chen JJ, Chen Q, et al. (1990) The discovery and exploitation of the resources of animal fossils in Panlongdong Cave, Yunfu County, Guangdong Province. Trop Geogr 10(4): 333–339. (In Chinese)
Wang LH, Peng SL, Chen YZ (1982) On the human fossils and stone arthfacts found in Baojiyan Cave, Guilin. Acta Anthropol Sin 1(1): 30–35. (In Chinese)
Wang PX, Min QB, Bian YH, et al. (1986) Planktonic foraminifera in the continental slope of the northern South China Sea during the last 130000 years and their paleo-oceanographic implications. Acta Geol Sin 62(3): 215–225. (In Chinese)
Wang W, Mo JY (2004) Human fossil teeth newly discovered in Nanzhan Cave of Fusui, Guangxi. Acta Anthropol Sin 5(2): 130–137. (In Chinese)
Wang Y, Qin DG, Jin CZ (2017) New elephas remains from the Zhiren cave of Mulan Mountain, Chongzuo, Guangxi with discussion on quaternary proboscidean evolution in southern China. Quat Sci 37(4): 854–859. (In Chinese)
Wang YJ, Cheng H, Edwards RL, et al. (2008) Millennial- and orbital-scal changes in the East Asian monsoon over the past 224 000 years. Nature 451(28): 1090–1093.
Wang YX (2003) China’s mammal species and subspecies classification catalogues and their distributions. pp 60–137. China Forestry Press, Beijing ISBN: 9787503831317. (In Chinese)
Wang ZT, Xu F, Sun G (1997) A preliminary analysis of the relationship between the extinction of Rhinoceros and Human population pressure in China. Acta Ecol Sin 17(6): 640–644. (In Chinese)
Wei F, Wu WT, Zhang MH (1990) Neolithic animal fauna of Hemudu Site, Yuyao, Zhejiang. pp 1–117. Ocean Press, Beijing ISBN9787502704209. (In Chinese)
Wen HR, Wen RS (1996) Climate change of winter half year during historical period in China. pp 1–169. Science Press, Beijing ISBN: 9787030051240. (In Chinese)
Wu ML, Wang LH, Zhang YY, et al. (1975) The Paleoanthropoids fossils and cultural relics in Tongzi, Guizhou. Vertebr Palasiat 13(1): 14–23. (In Chinese)
Xie GM (1991) Human cultural relics and animal fossils of Badu Mountain, Du’an, Guangxi. Acta Anthropol Sin 10(3): 264–267. (In Chinese)
Xu QQ (1980) The relationship between earth orbit and climate change. Chin Sci Bull (4): 180–182. (In Chinese)
Xu QQ (2000) The biological “mass extinction” of 11 000 years ago. Fossil (4): 16+19–20. (In Chinese)
Yan XH (1992) Discussion on Tanshishan Culture from Animal Archaeology. Archaeology and Cultural Relics (1): 102–109. (In Chinese)
Yang SL, Ding ZL (2008) Advance-retreat history of the East-Asian summer monsoon rainfall belt over northern China during the last two glacial-interglacial cysles. Earth and Planet Sc Lett 274: 499–510. https://doi.org/10.1016/j.epsl.2008.08.001
Yang SL, Ding ZL, Li YY, et al. (2015) Warming-induced northwestward migration of the East Asian monsoon rain belt from the Last Glacial Maximum to the mid-Holocene. P Nati Acad Sci USA 112(43): 13178–13183. https://doi.org/10.1073/pnas.1504688112
Yang ST, Chen ZJ (1981) The important discovery of Hedang site in Foshan. Collection of Cultural Relics 3: 24–27. (In Chinese)
Yuan FL (1993) Multilayered landforms in Nanling Mountain range and their related theoretical problems. Quat Sci 13(4): 361–363. (In Chinese)
Yuan SX (1993) Puzzlement caused by the 14C age data of early Neolithic Age in South China and its real age. Archaeol 4: 367–375. (In Chinese)
Yuan SX, Chen TM, Gao SJ (1986) Uranium series chronological sequence of some palaeolithic sites in South China. Acta Anthropol Sin 5(2): 179–190. (In Chinese)
Zhang MH (1981) Fauna of Luojiajiao site. In: the Relics and Archaeology Institution of Zhejiang Province (ed.), Journal of the Relics and Archaeology Institution of Zhejiang Province. pp 43–51. Cultural Relics Press, Beijing ISBN: 9787030257291. (In Chinese)
Zhang XF, Ji XP, Shen GJ (2004) U-series dating on fossil teeth from Xianren Cave in Xichou, Yunnan Province. Acta Anthropol Sin 23(1): 88–92. (In Chinese)
Zhang XY (1987) Quaternary mammal fossils and their fauna division in Yunnan Province. In: The Glaciers and Frozen Society of China(Ed.), The symposium of Quaternary Glacier and Quaternary Geology Papers(3 rd). pp 303–314. Geological Publishing House, Beijing. (In Chinese)
Zhang ZH (1996) Introduction to the Cenozoic Mammalian. Guangdong people’s publishing house, Guangzhou, pp246–275. ISBN:9787218023243. (In Chinese)
Zhang ZH, Zhang F, Chen QS (1994) Preliminary report on the excavation of Luoshanyan site in Fengkai, Guangdong. Acta Anthropol Sin 11(4): 300–308. (In Chinese)
Zhou GX (1982) Bailian Cave Site in Liuzhou, Guangxi, China — Exploration on the transition from late paleolithic culture to early neolithic culture in South China. Southeast Cult (2): 8–13. (In Chinese)
Zong GF, Huang XS (1985) Note on some mammalian fossils from the latest Pleistocene of Xialatuo, Luhuo, Sichuan. Vertebr Palasiat 10(4): 287–294. (In Chinese)
Acknowledgements
This study was financially supported by the National Natural Science Foundation of China (Grant No. 41571007, 41201006), the Strategic Priority Research Program of the Chinese Academy of Sciences (Category B, Grant No. XDB 26000000), the Open Fund Project of the State Key Laboratory of Nuclear Resources and Environment (Grant No. NRE1507).
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Li, Zw., Sun, L., Li, Bs. et al. East Asian summer monsoon changes in subtropical China since late Pleistocene: Evidence from the Ailuropoda-Stegodon fauna. J. Mt. Sci. 19, 418–432 (2022). https://doi.org/10.1007/s11629-021-6985-y
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DOI: https://doi.org/10.1007/s11629-021-6985-y