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作 者:Yi-Liang Li Wei-Dong Sun Yu-Fen Zhao 李一良;孙卫东;赵玉芬(Department of Earth Sciences,the University of Hong Kong,Hong Kong,China;Institute of Oceanology,Center of Ocean Mega-Science,Chinese Academy of Sciences,Qingdao 266071,China;The Institute of New Pharmaceutical Technology,Ningbo University,Ningbo 315832,China)
机构地区:[1]Department of Earth Sciences,the University of Hong Kong,Hong Kong,China [2]Institute of Oceanology,Center of Ocean Mega-Science,Chinese Academy of Sciences,Qingdao 266071,China [3]The Institute of New Pharmaceutical Technology,Ningbo University,Ningbo 315832,China
出 处:《Science Bulletin》2021年第12期1157-1159,M0003,共4页科学通报(英文版)
基 金:supported by the Strategic Priority Research Program of the Chinese Academy of Sciences(XDB41000000 and XDA22050100);Qian Xuesen Laboratory,China Academy of Space Technology。
摘 要:Zhang et al.[1]reported the first direct detection of the natural supercritical CO_(2)(scCO_(2);critical point:31.1℃and 72.9 atm)in a deep-sea hydrothermal system.In their study,they measured in situ the Raman bands of scCO_(2)bubbling from an approximately 95℃hydrothermal vent.The Raman spectra indicated that the scCO_(2)bubbles also trapped N2 and CH4 gases and unidentified organic carbons.This discovery suggests a scenario that a layer of scCO_(2)might have existed in the Hadean atmosphere between the young ocean and the gaseous CO_(2)-dominated upper layers.Such a layer of scCO_(2)in the atmosphere should have been highly active in trapping energetic small molecules and catalytic transition metals and polymerizing organic matters,thereby aiding the creation of a favorable planetary environment for prebiotic evolution toward life.
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