Hostname: page-component-586b7cd67f-t7fkt Total loading time: 0 Render date: 2024-11-27T17:43:13.277Z Has data issue: false hasContentIssue false
  • English
  • Français

Palynological records of Holocene monsoon change from the Gulf of Tonkin (Beibuwan), northwestern South China Sea

Published online by Cambridge University Press:  20 January 2017

Zhen Li ,
Yulan Zhang ,
Yongxiang Li  and
Jing Zhao
Zhen Li*
Affiliation:
State Key Laboratory of Estuarine and Coastal Research, East China Normal University, Shanghai, 200062, China
Yulan Zhang
Affiliation:
School of Ocean & Earth Science, Tongji University, Shanghai, 200092, China
Yongxiang Li
Affiliation:
Department of Earth and Environmental Sciences, Tulane University, LA 70118, USA School of Earth Science and Engineering, Nanjing University, Nanjing, 210093, China
Jing Zhao
Affiliation:
School of Ocean & Earth Science, Tongji University, Shanghai, 200092, China
*
⁎Corresponding author. E-mail addresses:[email protected][email protected] (Z. Li).
Get access Rights & Permissions [Opens in a new window]

Abstract

Palynological records in cores C4 and B106 from the Gulf of Tonkin reveal signals of paleo-monsoon and paleoenvironmental change during the late Pleistocene and Holocene. Before ∼ 13.4 cal kyr BP, the Gulf of Tonkin was exposed to the atmosphere and covered by grassland. Starting at ∼ 11.7 cal kyr BP, the Gulf of Tonkin was inundated by brackish water, indicated by the appearance of the brackish algae Cleistosphaeridium, Sentusidinium and Spiniferites, a decrease of herb content, and an increase of Pinus. After Hainan Island was completely separated from the Leizhou Peninsula by Qiongzhou Strait at ∼ 8.5 cal kyr BP, a continuous marine sedimentary environment was found. The current patterns were similar to those of the present, with a general trend of current homogenization reflected by gradually decreasing quantities of Quercus pollen and a narrowing gap between the palynological concentrations of the southern and northern parts of the region. The data suggest that three short periods of strengthened winter monsoons and currents were centered at ∼ 6.0 cal kyr BP, ∼ 2.7 cal kyr BP and ∼ 0.2 cal kyr BP and that two short periods of strengthened summer monsoons and currents were centered at ∼ 7.5 cal kyr BP and ∼ 3.4 cal kyr BP.

Keywords

PalynologyHolocene monsoon changePaleoenvironmentGulf of TonkinThe South China Sea
Type
Short Paper
Information
Quaternary Research , Volume 74 , Issue 1 , July 2010 , pp. 8 - 14
Copyright
University of Washington

Access options

Get access to the full version of this content by using one of the access options below. (Log in options will check for institutional or personal access. Content may require purchase if you do not have access.)

References

An, Z.S. The history and variability of the East Asian palaeomonsoon climate. Quaternary Science Reviews 19, (2000). 171–187.Google Scholar
Banerjee, S.K. Chasing the paleomonsoon over China: its magnetic record. GSA Today 5, (1995). 93–97.Google Scholar
Beaudouin, C., Suc, J.P., Escarguel, G., Arnaud, M., and Charmasson, S. The significance of pollen signal in present-day marine terrigenous sediments: The example of the Gulf of Lions (western Mediterranean Sea). Geobios 40, (2007). 159–172.Google Scholar
Birks, H.J.B., and Line, J.M. The use of rarefaction analysis for estimating palynological richness from Quaternary pollen-analytical data. The Holocene 2, (1992). 1–10.Google Scholar
Bush, M.B. Deriving response matrices from central American modern pollen rain. Quaternary Research (2000). 132–143.CrossRefGoogle Scholar
Chen, X., and Fan, S. Late Quaternary deposition and environment in the sea area Northwest of Hainan Island. Tropical Oceanology 7, 1 (1988). 39–47. (Chinese with English abstract) Google Scholar
Duplessy, J.C., Ivanova, E., Murdmaa, I., Peterne, M., and Labeyrie, L. Holocene paleoceanography of the Northern Barents Sea and variations of the northward heat transport by Atlantic Ocean. Boreas 30, (2001). 2–16.Google Scholar
Faegri, K., and Iversen, J. Textbook of pollen analysis. 4th ed (1992). Alden Press, London. 78–83.Google Scholar
Fan, F., Lin, M., Jiang, R., and ZHuang, J. The submarine buried paleo-delta in the east outer continental shelf of Hainan Island. Ocean Science 6, (1999). 55–58. (Chinese with English abstract) Google Scholar
First Institute of Oceanography, SOA Report of Sedimentary Characteristics of China Sea. (2001). Google Scholar
Florin, R. The distribution of conifer and taxad genera in time and space. Acta Horti Bergiani 20, (1963). 121–312.Google Scholar
Guangdong Institute of Botany Guangdong Vegetation. (1976). Science Press, Beijing. (in Chinese) Google Scholar
Hammer, Q., Harper, D.A.T., and Ryan, P.D. PAST: paleontological statistics software package for education and data analysis. Palaeontologia Electronica 4, 1 (2001). 9 Google Scholar
Heusser, L.E. Pollen distribution in marine sediments on the continental margin off northern California. Marine Geology 80, (1988). 131–147.Google Scholar
Huang, Z., Zhang, W., Chai, F., and Xu, Q. On the lowest sea level during the culmination of the latest glacial period in south China. Acta Geographica Sinica 50, 5 (1995). 385–393.Google Scholar
Hurlbert, S.H. The non-concept of species diversity: a critique and alternative parameters. Ecology 52, (1971). 577–586.CrossRefGoogle Scholar
Kou, Y., and Du, D. Sedimentary features of shallow ancient river channels on the northern shelf of the South China Sea. Acta Geologica Sinica 68, 3 (1994). 268–277.Google Scholar
Kudrass, H.R., Erlenkueser, H., Vollbrecht, R., and Weiss, W. Global nature of the Younger Dryas cooling event inferred from oxygen isotope data from Sulu Sea cores. Nature 349, (1991). 406–409.Google Scholar
Li, F., Dong, T., Jiang, X., Zhuang, J., Yu, J., and Du, Q. Buried paleo-channel system and change of sea level on the continental shelf in Yinggehai Basin. Oceanologia et Limnologia Sinica 21, 4 (1990). 356–363. (Chinese with English abstract) Google Scholar
Li, Z., Saito, Y., Matsumoto, E., Wang, Y., Tanabe, S., and Vue, Q.L. Climate change and human impact on the Song Hong (Red River) Delta, Vietnam, during the Holocene. Quaternary International 144, (2006). 4–28.Google Scholar
Li, Z., Saito, Y., Matsumoto, E., Wang, Y., Haruyama, S., Hori, K., and Doanh, L.Q. Palynological record of climate change during the last deglaciation from the Song Hong (Red River) delta, Vietnam. Palaeogeography, Palaeoclimatology, Palaeoecology 235, (2006). 406–430.Google Scholar
Li, Z., Zhang, Z., Li, J., Li, Z., Liu, L., Fan, H., and Li, G. Pollen distribution in surface sediments of a mangrove system, Yingluo Bay, Guangxi, China. Review of Palaeobotany and Palynology 152, (2008). 21–31.Google Scholar
Li, Z., Li, Z., Zhang, W., Li, J., Meng, X., and Liu, L. Pollen assemblage and sedimentary environment evolution in the coastal zone in Qinzhou Bay, Guangxi Province. Quaternary Sciences 30, 3 (2010). 1–11. (Chinese with English abstract) Google Scholar
Lin, M. Submarine geomorphology of the eastern continental shelf of the Hainan Island. Marine Geology & Quaternary Geology 15, 4 (1995). 37–46. (Chinese with English abstract) Google Scholar
Lin, D., Liu, C., Fang, T., Tsai, C., Murayama, M., and Chen, M. Millennial-scale changes in terrestrial sediment input and Holocene surface hydrography in the northern South China Sea (IMAGES MD972146). Palaeogeography, Palaeoclimatology, Palaeoecology 236, (2006). 56–73.Google Scholar
Maxwell, A.L. Holocene monsoon changes inferred from lake sediment pollen and carbonate records, northeastern Cambodia. Quaternary Research 56, (2001). 390–400.Google Scholar
Morton, B., and Blackmore, G. South China Sea. Marine Pollution Bulletin 42, (2001). 1236–1263.Google Scholar
Moss, P.T., Kershaw, A.P., and Grindrod, J. Pollen transport and deposition in riverine and marine environments within the humid tropics of northeastern Australia. Review of Palaeobotany and Palynology 134, (2005). 55–69.Google Scholar
Patrick, T., Moss, A., Kershaw, P., and Grindrod, J. Pollen transport and deposition in riverine and marine environments within the humid tropics of northeastern Australia. Review of Palaeobotany and Palynology 134, (2005). 55–69.Google Scholar
Penny, D. The Holocene history and development of the Tonle Sap, Cambodia. Quaternary Science Reviews 25, (2006). 310–322.Google Scholar
Peros, M.C., and Gajewski, K. Testing the reliability of pollen-based diversity estimates. Journal of Paleolimnology 40, (2008). 357–368.Google Scholar
Porter, S.C., and An, Z. Correlation between climate events in the North Atlantic and China during the last glaciation. Nature 375, (1995). 305–308.Google Scholar
Romagnoli, S., Cai, G., and Cresti, M. Kinesin-like proteins and transport of pollen tube organelles. Cell Biology International 27, (2003). 255–256.Google Scholar
Southon, J., Kashgarian, M., Fontugne, M., Metivier, B., and Yim, W.W.-S. Marine reservoir corrections for the Indian Ocean and Southeast Asia. Radiocarbon 44, (2002). 167–180.Google Scholar
Su, D., Chen, H., Chen, X., and Li, Z. Evolution of Asian monsoon variability revealed by oxygen isotopic record of middle Holocene massive coral in the northern South China Sea. Quaternary International 213, (2010). 56–68.Google Scholar
Sun, X., Li, X., and Beug, H.J. Pollen distribution in hemipelagic surface sediments of the South China Sea and its relation to modern vegetation distribution. Marine Geology 156, (1999). 211–226.Google Scholar
Sun, D., Gagan, M.K., Cheng, H., Scott-Gagan, H., Dykoski, C.A., Lawrence Edwards, R., and Su, R. Seasonal and interannual variability of the Mid-Holocene East Asian monsoon in coral δ18O records from the South China Sea. Earth and Planetary Science Letters 237, (2005). 69–84.Google Scholar
Tanabe, S., Hori, K., Saito, Y., Haruyama, S., Vu, V.P., and Kitamura, A. Song Hong (Red River) delta evolution related to millennium-scale Holocene sea-level changes. Quaternary Science Reviews 22, (2003). 2345–2361.CrossRefGoogle Scholar
Tang, D., Kawamura, H., Lee, M.-A., and Dien, T.V. Seasonal and spatial distribution of chlorophyll-α concentrations and water conditions in the Gulf of Tonkin, South China Sea. Remote Sensing of Environment 85, (2003). 475–483.Google Scholar
Tchernia, P. Descriptive regional oceanography. Marine Series vol. 3, (1980). Pergamon Press, 235 Google Scholar
Thin, N.N. The Fansipan flora in relation to the Sino-Japanese Floristic Region. The University Museum and the University of Tokyo, Bulletin No. 37. (1998). Google Scholar
van der Knaap, W.O. Estimating pollen diversity from pollen accumulation rates: a method to assess taxonomic richness in the landscape. The Holocene 19, (2009). 159–163.Google Scholar
Wang, P. Response of Western Pacific marginal seas to glacial cycles: paleoceanographic and sedimentological features. Marine Geology 156, (1999). 5–39.Google Scholar
Wang, K., Jiang, H., and Zhang, Y. Quaternary pollen, spore and algae distribution and environment in South China Sea and its coastal area. (1990). Tongji Press, Shanghai.Google Scholar
Wang, L., Sarnthein, M., Erlenkeuser, H., Grimalt, J., Grootes, P., Heilig, S., Ivanova, E., Kienast, M., Pelejero, C., and Pflaumann, U. East Asian monsoon climate during the Late Pleistocene: high-resolution sediment records from the South China Sea. Marine Geology 156, (1999). 245–284.Google Scholar
Wang, Y., Cheng, H., Edwards, R.L., He, Y., Kong, X., An, Z., Wu, J., Kelly, M.J., Dykoski, C.A., and Li, X. The Holocene Asian Monsoon: Links to Solar Changes and North Atlantic Climate. Science 308, (2005). 854–857.Google Scholar
Wu, Z.Y. Vegetation of China. (1980). Science Press, Beijing. (in Chinese) Google Scholar
Wu, Z., Fen, W., Liao, B., and Jin, Z. Papeogeographic study in the continental shelf of the northern South China Sea during the last stage of the Late Pleistocene. Acta Geographica Sinica 48, 6 (1993). 491–496. (Chinese with English abstract) Google Scholar
Xia, Z., Ma, S., Liang, K., and Shi, Y. The characteristics analysis of sea bottom deposit in Lingdingyang Bay of the Pearl River estuary. Marine Geology & Quaternary Geology 28, 2 (2008). 7–13. (Chinese with English abstract) Google Scholar
Xie, X., Müller, R.D., Ren, J., Jiang, T., and Zhang, C. Stratigraphic architecture and evolution of the continental slope system in offshore Hainan, northern South China Sea. Marine Geology 247, (2008). 129–144.Google Scholar
Xu, Q., Li, Y., Yang, X., Xiao, Y., Liang, W., and Peng, Y. Source and distribution of pollen in the surface sediment of Daihai Lake, inner Mongolia. Quaternary International 136, (2005). 33–45.Google Scholar
Yancheva, G., Nowaczyk, N.R., Mingram, J., Dulski, P., Schettler, G., Negendank, J., Liu, J., Sigman, D.M., Peterson, L.C., and Haug, G.H. Influence of the intertropical convergence zone on the East Asian monsoon. Nature 445, (2007). 74–77.Google Scholar
Yao, Y., Harff, J., Meyer, M., and Zhan, W. Reconstruction of paleo-shoreline in the northwest of South China Sea since the last glacial maximum. Science in China Series D: Earth Sciences 39, 6 (2009). 753–762.Google Scholar
Yu, K., Zhao, J., Wei, G., Chen, X., and Wang, P. Mid–late Holocene monsoon climate retrieved from seasonal Sr/Ca and δ18O records of Porites lutea corals at Leizhou Peninsula, northern coast of South China Sea. Global and Planetary Change 47, (2005). 301–316.Google Scholar
Zhang, Y., and Long, J. Sporopollen and algae research of core B106 in the northern South China Sea and its paleoenvironmental evolution. Frontiers of Earth Science in China 2, 2 (2008). 157–161.Google Scholar
Zhang, W., Wang, K., and Li, Z. Sporo-pollen assemblages in beach sediments in Guangxi and Guangdong and its significance. Marine Science Bulletin 18, 1 (1999). 36–42. (in Chinese with English abstract) Google Scholar
Zhang, Y., Zhang, W., and Wang, K. Studies on the relationship between sporo-pollen of surface sediments and vegetation of the continental margin in the northeastern South China Sea. Marine Science Bulletin 21, 4 (2002). 26–36. (in Chinese with English abstract) Google Scholar
Zhao, H., Zhang, Q., Song, C., Qiu, Z., Lin, X., and Yuan, J. Geomorphology and Environment of the South China Coast and the South China Sea Islands. (1999). China Science Press, Beijing. 119–121.Google Scholar
Zhao, H., Wang, L., and Yuan, J. Origin and time of Qiongzhou Strait. Marine Geology & Quaternary Geology 27, 2 (2007). 33–41. (Chinese with English abstract) Google Scholar
Zheng, Z., and Li, Q. Vegetation, climate, and sea level in the past 55, 000 years, Hanjiang delta, Southeastern China. Quaternary Research 53, (2000). 330–340.Google Scholar
Zong, Y. Mid-Holocene sea-level highstand along the Southeast Coast of China. Quaternary International 117, (2004). 55–67.Google Scholar