Dr. Li, Yiliang

Cover
Profile Pic

Dr. Li, YiLiang

Associate Professor

My two recent research interests are in the general field of Astrobiology. One is the mineral records of the origin and evolution of the early biospheres. We use electron microscopic and spectroscopic methods to characterize biogenic minerals from the early Precambrian sedimentary rocks. Another one is the evaluation of Qaidam Basin on the north of Tibetan Plateau as a potential Martian analogue. Western Qaidam Basin is characterized by its vast distribution of dried salt lakes, thick deposition of clay and various salts and hyperarid climate. The understanding of the dynamic evolution of this area can provide comparative data for interpreting mysterious Martian geology and providing references for designing Martian land rovers.

Email:
Tel:
Fax:
Location:
Website:
Link:
yiliang@hku.hk
2859 8021
2517 6912
JL304
http://scholar.google.com/citations?user=WQGmJWYAAAAJ
www.astrobiology.hk
 

Teaching

EASC1406   An introduction to the Earth-Life System
EASC4403   Biogeochemical cycles
ENVM8010  Earth science and environmental  management
CCST9043   Time’s Arrow

Selected Publications

  1. A. Angles, Y.L. Li (2017) Similar ring structures on Mars and Tibetan Plateau confirm recent tectonism on Martian Northern polar region. International Journal of Astrobiology, 16, 355-359.
  2. Lv K., Norman L., Y.L. Li (2017) Oxygen-free biochemistry: the putative CHN foundation for exotic life in a hydrocarbon world? Astrobiology, 17, 1173-1181.
  3. K.P. Lv, L. Norman, Y.L. Li (2016) Restriction on the production of multi-wall carbon nanotubes and nanofibers by Gallionella sp. Geomicrobiology Journal, 33, 709-715.
  4. X.L. Hao, Y.L. Li (2015) Hexagonal plate-like magnetite nanocrystals produced in komatiite-H2O-CO2 reaction system at 450°C. International Journal of Astrobiology, 14, 547-553.
  5. Y.L. Li (2012) Hexagonal platelet-like magnetite as biosignature of thermophilic iron-reducing bacteria and its applications to the exploration of the modern deep, hot biosphere and the emergence of iron-reducing bacteria in early Precambrian oceans. Astrobiology, 12, 1100-1108.