V51B:
Geochemistry of Sediments and Sediment Recycling and Implications for Crust and Mantle Evolution over Earth History II Posters


Session ID#: 10934

Session Description:
Sedimentary rocks record information on diverse topics such as environmental conditions from the distant past, the average composition of the continents, and the redox state of the oceans and atmosphere.  Although much of the Earth’s sedimentary record has been removed from our view by subduction processes, a long term consequence may be that the mantle “sees” and is influenced by Earth surface conditions.  We seek a broad range of contributions that deal with the record of continental evolution and the rise of oxygen, seen both in the sedimentary record and also potentially in igneous systems as a result of sediment recycling over Earth history.
Primary Convener:  Richard M Gaschnig, University of Massachusetts Lowell, Environmental, Earth and Atmospheric Sciences, Lowell, MA, United States
Conveners:  Xiao-Ming Liu, Carnegie Institution of Washington, Geophysical Laboratory, Washington, DC, United States and Elizabeth A Bell, University of California Los Angeles, Earth, Planetary, and Space Sciences, Los Angeles, CA, United States
Chairs:  Richard M Gaschnig, University of Massachusetts Lowell, Lowell, MA, United States and Elizabeth A Bell, University of California Los Angeles, Earth, Planetary, and Space Sciences, Los Angeles, CA, United States
OSPA Liaison:  Elizabeth A Bell, University of California Los Angeles, Earth, Planetary, and Space Sciences, Los Angeles, CA, United States

Cross-Listed:
  • EP - Earth and Planetary Surface Processes
  • PP - Paleoceanography and Paleoclimatology
  • T - Tectonophysics
Index Terms:

Abstracts Submitted to this Session:

Dustin Trail, University of Rochester, Rochester, NY, United States
Vanessa Markwitz, University of Western Australia, Crawley, WA, Australia and Christopher Kirkland, Curtin University, Dept of Applied Geology, Perth, WA, Australia
XiangDong Wang1, Laishi Zhao2, Zhong-Qiang Chen1, Derong Ma2, Pingan Yan2, Fei Guo1, Fu Wang2, QingXiang Wan1 and XiaoQing Han1, (1)China University of Geosciences, Wuhan, China, (2)China University of Geosciences Wuhan, Wuhan, China
Emmanuel JEMINIYI Ajidahun, University of Benin, Benin City, Nigeria
Kai Deng1, Shouye Yang2, Chao Li3, Lei Bi1 and Yuan-Pin Chang4, (1)State Key Laboratory of Marine Geology, Tongji University, Shanghai 200092, China, (2)Tongji University, State Key Laboratory of Marine Geology, Shanghai, China, (3)Tongji University, Shanghai, China, (4)National Sun Yat-sen University, Department of Oceanography, Kaohsiung, Taiwan
Zhenning Yang and Kunguang Yang, China University of Geosciences Wuhan, Wuhan, China
Change Cai1,2 and Nansheng Qiu2,3, (1)Research Center for Basin and Reservoir, China University of Petroleum, Beijing, China, (2)State Key Laboratory of Petroleum Resource and Prospecting, China University of Petroleum, Beijing, China, (3)1 State Key Laboratory of Petroleum Resources and Prospecting, China University of Petroleum, Beijing ,China 2 College of Geosciences, China University of Petroleum, Beijing , China, Beijing, China
Feng Cheng1, Hanlie Hong1,2, Chaoran Li1, Han Ye3 and Huan Yang1,2, (1)China University of Geosciences Wuhan, Faculty of Earth Sciences, Wuhan, China, (2)State Key Laboratory of Biogeology and Environmental Geology, Wuhan, China, (3)Zhejiang Institute of Geology and Mineral Resource, Hangzhou, China