The Microbial Factor of Travertine Deposition between Yellowstone National Park (YNP), USA and Huanglong Scenic, Sichuan

Abstract:

Yellow Stone National Park (YNP), USA, is well-known as its glorious travertine geomorphology as well as Huanglong National Scenic District in Sichuan, China. But there were some difference between them. The travertine deposition of YNP were formed from geothermal activity, meanwhile Huanglong Scenic District is located in high attitude and cold area and the travertine deposition appeared in the cold water. With the increasing attention to global carbon cycle, origin of life and the life action in the extreme environment, the geothermal travertine formation origin and mechanism were focused by the scientists from different field. The research plan was also a part of “the Mars project”. The reason was that the Mars’s surface environment is similar to that of the ancient Earth. This article reviewed the research results of the microbiology diversity, community structure and distribution, function gene and special microbial carbon metabolism passway in the hot spring of YNP. We also summarized the biological factor in the process of the travertine deposition of YNP. After comparing the research progress on the travertine deposition between YNP and Huanglong Scenic District, we put foreword the further strategy to understand the biological effect on the travertine deposition of Huanglong Scenic District.

• Periodical: Advanced Materials Research (Volumes 518-523)
• Pages: 136-139
• DOI: https://doi.org/10.4028/www.scientific.net/AMR.518-523.136
• Online since: May 2012
• Authors: Qiong Fang Li, Fa Qin Dong, Qun Wei Dai, Ting Ting Huo, De Jun An, Shu Tang
• Keywords: Biological Factor, Geological Microorganism, Huanglong Scenic, Travertine, Yellowstone National Park (YNP)

References

[1] LIAN Bin: Geology-Geochemistry,Vol.6 (1995), pp.71-75(in Chinese)

[2] WU Jian,DAI Guifu: Geology-Geochemistry, Vol.1 (1995), pp.15-18 (in Chinese)

[3] CHEN Jun, LIAN Bin, WANG Bin, et al: Earth Science Frontiers, Vol.13-6(2006),pp.199-207

[4] J. Malusa, S. T.Overby, R.A. Parnell: Applied Geochemistry, vol.18(2003), pp.1081-1093

DOI: 10.1016/s0883-2927(02)00241-x

[5] W.Stumm J.J. Morgan: Aquatic chemistry. John Wiley & Sons, New York.1981.

[6] A.Pentecost: J. Hydrol. Vol. 16( 1995), P. 263-278

[7] J.L. Dandurand, R. Gout, J. Hoefs, G. Menschel, J. Schott, E.Usdowski: Chem. Geol. Vol. 36 ( 1982).P. 299-315.

DOI: 10.1016/0009-2541(82)90053-5

[8] TD Brock: Life at high temperatures: Science. Vol.158-3804 (1967),P.1012-1019

[9] J. L. Bishop, E. M. Melissa, D. Lane, R. L. Mancinelli: ICARUS.Vol. 169 (2004) ,pp.311-323

[10] M.J. Hellman, M.S. Ramsey: J. Volcanology and Geothermal Res. Vol.135(2004), pp.195-219

[11] H.S. Chafetz, and S.A. Guidry: Can J Earth Sci Vol.40(2003),p.:1515-1529

[12] T.D. Brock, Life at High Temperatures. Yellowstone National Park, WY: Yellowstone Association for Natural Science, History & Education, Inc. (1994)

[13] D.M. Ward, and T. Papke:Species composition of hot spring cyanobacterial mats. 6th Symp. Chem. Evol. and the Origin of Life, NASA, Palo Alto, CA, November. ( 1997)

[14] T.D. Brock: Thermophilic microorganisms and life at high temperatures. New York: Springer-Verlag.(1978)

[15] B.W. Fouke, , J.D. Farmer, D.J. Des Marais, L. Pratt, N.C. Sturchio, P.C. Burns, and M.K. Discipulo: J Sediment Res.Vol.70(2000). pp.265-285

[16] N.Hamamura, S. H. Olson, D. M. Ward, and W.P. Inskeep: Appl Environ Microb. 2005, Vol. 71-10(2005), pp.5943-5950

[17] C.L. Zhang,, B.W. Fouke, G.T. Bonheyo, A.D. Peacock, D.C. White, Y. Huang, and C.S. Romanek: Geochim Cosmochim Acta 68(2004), pp.3157-3169

[18] CHEN Xian, ZHU Xuewen, ZHOU Xulun: Congress.Vol.176-1(1988), pp.233-240

[19] Kurt O. Konhauser, Brian Jones, Anna-Louise Reysenbach: Can. J. Earth Sci. Vlo. 40(2003), pp.1713-1724

[20] Weixin Guo: ournal of Mountain Research , Vol.01(1988), p.26

[21] Dehao Zhu: Discovery of Nature.Vol.02(1986), p.34