Abstract
The intensified monsoon increases summer rainfall and creates wet conditions in the Asian summer monsoon region during the early Holocene. Along with millennial-scale changes of the monsoon intensity, it is still unclear whether the boundary of the monsoon region changes according to monsoon variability. Investigations into the early Holocene environment in monsoon marginal zones are crucial for understanding the monsoon boundary changes. Zhuye Lake is located at the northwest edge of the Asian summer monsoon, the northern Qilian Mountains, which are less affected by modern summer monsoon water vapor. Previous studies have reached different conclusions regarding the early Holocene climatic and environmental changes based on different dating methods (14C and OSL (optically stimulated luminescence)) and materials (shells, carbonate, pollen concentrates and bulk organic carbon). In this study, we synthesized 102 14C dates and 35 OSL dates from ten Holocene sedimentary sections and ten paleo-shorelines in the lake basin. A comparison between ages from different dating methods and materials generally shows that carbon reservoir effects are relatively slight in Zhuye Lake while the disordered chronologies are mainly related to the erosion processes and reworking effects. In addition, proxy data, including lithology, pollen, total organic carbon and carbonate, were collected from different sites of Zhuye Lake. According to the new synthesis, the early Holocene environment was relatively humid, associated with high runoff and lake water levels. The result indicates that the monsoon boundary moves to the north during the period of the intensified monsoon. A typical arid-area lake was formed during the mid-Holocene when carbonate accumulation and high organic matter contents were the main features of this period. The lake retreated strongly during the late Holocene, showing a drought trend. Overall, the lake evolution is generally consistent with the Holocene Asian summer monsoon change, showing the monsoon influence to monsoon marginal zones.
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References
Aguado E, Burt J E. 2004. Understanding Weather and Climate (3rd ed.). New Jersey: Prentice Hall.
An Z S, Porter S C, Kutzbach J E, et al. 2000. Asynchronous Holocene optimum of the East Asian monsoon. Quaternary Science Reviews, 19: 743–762.
Barry R G, Chorley R J, Yokoi N J. 2004. Atmosphere, Weather, and Climate (8th ed.). London: Routledge.
Cai Y J, Tan L C, Cheng H, et al. 2010. The variation of summer monsoon precipitation in central China since the last deglaciation. Earth and Planetary Science Letters, 291: 21–31.
Chen C T A, Lan H C, Lou J Y, et al. 2003. The Dry Holocene megathermal in Inner Mongolia. Palaeogeography, Palaeoclimatology, Palaeoecology, 193: 181–200.
Chen F H, Shi Q, Wang J M. 1999. Environmental changes documented by sedimentation of Lake Yiema in arid China since the Late Glaciation. Journal of Paleolimnology, 22: 159–169.
Chen F H, Zhu Y, Li J J. 2001. Abrupt Holocene changes of the Asian monsoon at millennial-and centennial-scales: Evidence from lake sediment document in Minqin Basin, NW China. Chinese Science Bulletin, 46: 1942–1947.
Chen F H, Wu W, Holmes J A, et al. 2003. A mid-Holocene drought interval as evidenced by lake desiccation in the Alashan Plateau, Inner Mongolia, China. Chinese Science Bulletin, 48: 1–10.
Chen F H, Cheng B, Zhao Y, et al. 2006. Holocene environmental change inferred from a high-resolution pollen record, Lake Zhuyeze, arid China. The Holocene, 16: 675–684.
Chen F H, Yu Z C, Yang M L, et al. 2008. Holocene moisture evolution in arid central Asia and its out-of-phase relationship with Asian monsoon history. Quaternary Science Reviews, 27: 351–364.
Chen L H, Qu Y G. 1992. Water-land Resources and Reasonable Development and Utilization in the Hexi Region. Beijing: Science Press.
Ding Y H, Chan J C L. 2005. The East Asian summer monsoon: an overview. Meteorology and Atmospheric Physics, 89: 117–142.
Dykoski C A, Edwards R L, Cheng H, et al. 2005. A high-resolution, absolute-dated Holocene and deglacial Asian monsoon record from Dongge Cave, China. Earth and Planetary Science Letters, 233: 71–86.
Fleitmann D, Burns S J, Mudelsee M, et al. 2003. Holocene forcing of the Indian monsoon recorded in a stalagmite from Southern Oman. Science, 300: 1737–1739.
Hartmann K, Wünnemann B. 2008. Hydrological changes and Holocene climate variations in NW China, inferred from lake sediments of Juyanze palaeolake by factor analyses. Quaternary International, 194: 28–44.
He Y, Theakstone W H, Zhang Z L, et al. 2004. Asynchronous Holocene climate change across China. Quaternary Research, 61: 52–63.
Herzschuh U. 2006. Palaeo-moisture evolution in monsoonal Central Asia during the last 50,000 years. Quaternary Science Reviews, 25: 163–178.
Holmes J A, Zhang J W, Chen F H, et al. 2007. Paleoclimatic implications of an 850-year oxygen-isotope record from the northern Tibetan Plateau. Geophysical Research Letters, 34: L23403.
Hong Y T, Hong B, Lin Q H, et al. 2005. Inverse phase oscillations between the East Asian and Indian Ocean summer monsoons during the last 12000 years and paleo-El Niño. Earth and Planetary Science Letters, 231: 337–346.
Huang D S. 1997. Gansu Vegetation. Lanzhou: Gansu Science and Technology Press.
Jin L Y, Chen F H, Morrill C, et al. 2012. Causes of early Holocene desertification in arid central Asia. Climate Dynamics, 38: 1577–1591.
Li Y, Wang N A, Cheng H Y, et al. 2009a. Holocene environmental change in the marginal area of the Asian monsoon: a record from Zhuye Lake, NW China. Boreas, 38: 349–361.
Li Y, Wang N A, Morrill C, et al. 2009b. Environmental change implied by the relationship between pollen assemblages and grain-size in N.W. Chinese lake sediments since the Late Glacial. Review of Palaeobotany and Palynology, 154: 54–64.
Li Y, Morrill C. 2010. Multiple factors causing Holocene lake-level change in monsoonal and arid central Asia as identified by model experiments. Climate Dynamics, 35: 1119–1132.
Li Y, Wang N A, Li Z L, et al. 2011. Holocene palynological records and their responses to the controversies of climate system in the Shiyang River drainage basin. Chinese Science Bulletin, 56: 535–546.
Li Y, Wang N A, Chen H B, et al. 2012a. Tracking millennial-scale climate change by analysis of the modern summer precipitation in the marginal regions of the Asian monsoon. Journal of Asian Earth Sciences, 58: 78–87.
Li Y, Wang N A, Carrie M, et al. 2012b. Millennial-scale erosion rates in three inland drainage basins and their controlling factors since the Last Deglaciation, arid China. Palaeogeography, Palaeoclimatology, Palaeoecology, 365–366: 263–275.
Li Y, Wang N A, Li Z L, et al. 2012c. Reworking effects in the Holocene Zhuye Lake sediments: A case study by pollen concentrates AMS 14C dating. Science China: Earth Sciences, 55: 1669–1678.
Li Y, Morrill C. 2013. Lake levels in Asia at the Last Glacial Maximum as indicators of hydrologic sensitivity to greenhouse gas concentrations. Quaternary Science Reviews, 60: 1–12.
Liu H Y, Cui H T, Pott R, et al. 1999. The surface pollen of the woodland-steppe ecotone in southeastern Inner Mongolia, China. Review of Palaeobotany and Palynology, 105: 237–250.
Long H, Lai Z P, Wang N A, et al. 2010. Holocene climate variations from Zhuyeze terminal lake records in East Asian monsoon margin in arid northern China. Quaternary Research, 74: 46–56.
Long H, Lai Z P, Wang N A, et al. 2011. A combined luminescence and radiocarbon dating study of Holocene lacustrine sediments from arid northern China. Quaternary Geochronology, 6: 1–9.
Long H, Lai Z P, Fuchs M, et al. 2012. Timing of Late Quaternary palaeolake evolution in Tengger Desert of northern China and its possible forcing mechanisms. Global and Planetary Change, 92–93: 119–129.
Ma Y Z, Zhang H C, Pachur H J, et al. 2003. Late Glacial and Holocene vegetation history and paleoclimate of the Tengger Desert, northwestern China. Chinese Science Bulletin, 48: 1457–1463.
Mischke S, Kramer M, Zhang C J, et al. 2008. Reduced early Holocene moisture availability in the Bayan Har Mountains, northeastern Tibetan Plateau, inferred from a multi-proxy lake record. Palaeogeography, Palaeoclimatology, Palaeoecology, 267: 59–76.
Morrill C, Overpeck J T, Cole J E. 2003. A synthesis of abrupt changes in the Asian summer monsoon since the last deglaciation. The Holocene, 13: 465–476.
Morrill C, Overpeck J T, Cole J E, et al. 2006. Holocene variations in the Asian monsoon inferred from the geochemistry of lake sediments in central Tibet. Quaternary Research, 65: 232–243.
Pachur H J, Wünnemann B, Zhang H C. 1995. Lake evolution in the Tengger Desert, northwestern China, during the last 40,000 years. Quaternary Research, 44: 171–180.
Reimer P J, Baillie M G L, Bard E, et al. 2009. IntCal09 and Marine09 radiocarbon age calibration curves, 0–50,000 years cal BP. Radiocarbon, 51: 1111–1150.
Shen J, Liu X Q, Wang S M, et al. 2005. Palaeoclimatic changes in the Qinghai Lake area during the last 18,000 years. Quaternary International, 136: 131–140.
Sugita S. 1993. A modern pollen source area from an entire lake surface. Quaternary Research, 39: 239–244.
Wang B, Lin H. 2002. Rainy season of the Asian-Pacific summer monsoon. Journal of Climate, 15: 386–396.
WANG F N, LI B S, WANG J L, et al. 2012. Pleniglacial millennium-scale climate variations in northern China based on records from the Salawusu River Valley. Journal of Arid Land, 4(3): 231–240.
Wang K L, Jiang H, Zhao H Y. 2005. Atmospheric water vapor transport from westerly and monsoon over the Northwest China. Advances in Water Science, 16: 432–438.
Wang Y B, Liu X Q, Herzschuh U. 2010. Asynchronous evolution of the Indian and East Asian Summer Monsoon indicated by Holocene moisture patterns in monsoonal central Asia. Earth-Science Reviews, 103: 135–153.
Yancheva G, Nowaczyk N R, Mingram J, et al. 2007. Influence of the intertropical convergence zone on the East Asian monsoon. Nature, 445: 74–77.
Zhang H C, Ma Y Z, Li J J, et al. 2001. Palaeolake evolution and abrupt climate changes during last glacial period in NW China. Geophysical Research Letters, 28: 3203–3206.
Zhang H C, Wünnemann B, Ma Y Z, et al. 2002. Lake level and climate changes between 42,000 and 18,000 C-14 yr BP in the Tengger Desert, Northwestern China. Quaternary Research, 58: 62–72.
Zhang H C, Peng J L, Ma Y, et al. 2004. Late quaternary palaeolake levels in Tengger Desert, NW China. Palaeogeography, Palaeoclimatology, Palaeoecology, 211: 45–58.
Zhang H C, Ming Q Z, Lei G L, et al. 2006. Dilemma of dating on lacustrine deposits in a hyperarid inland basin of NW China. Radiocarbon, 48: 219–226.
Zhang J C, Lin Z G. 1992. Climate of China. New York: Wiley.
Zhao S Q. 1983. A new scheme for comprehensive physical regionalization in China. Acta Geographica Sinica, 38: 1–10.
Zhao Y, Yu Z, Chen F, et al. 2008. Holocene vegetation and climate change from a lake sediment record in the Tengger Sandy Desert, northwest China. Journal of Arid Environments, 72: 2054–2064.
Zhu Y, Xie Y W, Cheng B, et al. 2003. Pollen transport in the Shiyang River drainage, arid China. Chinese Science Bulletin, 48: 1499–1506.
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Li, Y., Wang, N., Zhang, C. et al. Early Holocene environment at a key location of the northwest boundary of the Asian summer monsoon: a synthesis on chronologies of Zhuye Lake, Northwest China. J. Arid Land 6, 511–528 (2014). https://doi.org/10.1007/s40333-014-0064-y
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DOI: https://doi.org/10.1007/s40333-014-0064-y