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机译:青藏高原纳木错全新世湖水位变化的潜在强迫机制:从腹足动物基壳的稳定同位素组成推断
Chinese Acad Sci, Inst Tibetan Plateau Res, Key Lab Tibetan Environm Changes & Land Surface P, Beijing 100101, Peoples R China|Univ Chinese Acad Sci, Beijing, Peoples R China;
Chinese Acad Sci, Inst Tibetan Plateau Res, Key Lab Tibetan Environm Changes & Land Surface P, Beijing 100101, Peoples R China;
Chinese Acad Sci, Inst Tibetan Plateau Res, Key Lab Tibetan Environm Changes & Land Surface P, Beijing 100101, Peoples R China|Univ Chinese Acad Sci, Beijing, Peoples R China;
Chinese Acad Sci, Inst Tibetan Plateau Res, Key Lab Tibetan Environm Changes & Land Surface P, Beijing 100101, Peoples R China;
Chinese Acad Sci, Inst Tibetan Plateau Res, Key Lab Tibetan Environm Changes & Land Surface P, Beijing 100101, Peoples R China;
Chinese Acad Sci, Inst Tibetan Plateau Res, Key Lab Continental Collis & Plateau Uplift, Beijing, Peoples R China;
gastropoda; Holocene; lake-level changes; Nam Co lake; Radix; shell geochemistry; Tibetan Plateau;
机译:从陆生腹足动物的全壳和壳内稳定同位素组成推断阿根廷中部全新世(〜4.5-1.7cal。Kyr BP)古环境条件
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机译:从土耳其Çatalhöyük的Unio壳的稳定同位素组成推断出早全新世古地质