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机译:台湾亚高山撤退湖湖相沉积物芯的多代理方法追踪的全新世季风气候变化
Department of Palynology and Climate Dynamics, Albrecht-von-Haller Institute for Plant Sciences, University of Goettingen, Goettingen 37073, Germany;
Department of Palynology and Climate Dynamics, Albrecht-von-Haller Institute for Plant Sciences, University of Goettingen, Goettingen 37073, Germany;
Department of Geosciences, National Taiwan University, Taipei 106, Taiwan;
Department of Oceanography, National Sun Yat-sen University, Kaohsiung 804, Taiwan;
Department of Oceanography, National Sun Yat-sen University, Kaohsiung 804, Taiwan;
Department of Marine Science, R.O.C. Naval Academy, Kaohsiung 813, Taiwan;
Department of Oceanography, National Sun Yat-sen University, Kaohsiung 804, Taiwan;
Department of Geosciences, National Taiwan University, Taipei 106, Taiwan;
机译:南极东部席尔马赫绿洲地区湖泊沉积物中心的全新世气候变化:多代理方法
机译:泥灰岩和湖泊沉积物有机物的碳同位素反映了冰川晚期和全新世早期(公元16800至5,540 cal B.P.)期间的陆地景观变化:一项关于西爱尔兰拉奇因基昆湖沉积物的多代理研究
机译:泥灰岩和湖泊沉积物有机物的碳同位素反映了冰川晚期和全新世早期(16,800至5,540 cal yr BP)期间的陆地景观变化:一项关于西爱尔兰因基昆湖湖沉积物的多代理研究
机译:Grinnell湖沉积物核心,冰川国家公园,蒙大拿州的古古镇变化持续延迟全新型
机译:马加迪湖和苏打湖循环:现代碳酸钠以及晚更新世和全新世湖相湖泊沉积物的研究
机译:北极湖沉积物中的微生物群落结构反映了全新世气候条件的变化