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机译:欧洲黄土带南端的晚更新世Belotinac剖面(塞尔维亚南部):利用粒度和稳定的C和N同位素进行环境和气候重建
Laboratory for Paleoenvironmental Reconstruction, Faculty of Sciences, University of Novi Sad, 21000 Novi Sad, Serbia;
Chair of Geomorphology, University of Bayreuth, 95440 Bayreuth, Germany,Department of Geography, Justus-Liebig University Giessen, Senckenbergstr. 1, 35390 Giessen, Germany;
Department of Geography, Memorial University of Newfoundland, St. John's, A1B 3X9 Canada;
Laboratory for Paleoenvironmental Reconstruction, Faculty of Sciences, University of Novi Sad, 21000 Novi Sad, Serbia;
Soilbiogeochemistry Group, Martin Luther University Halle-Wittenberg, von Seckendorff-Platz 3, 06120 Halle, Germany;
Laboratory of Mineralogy and Petrology (Luminescence Research Group), Department of Geology and Soil Science, Ghent University, Krijgslaan 281 (S8),B-9000 Gent, Belgium;
Chair of Geomorphology, University of Bayreuth, 95440 Bayreuth, Germany;
Laboratory for Paleoenvironmental Reconstruction, Faculty of Sciences, University of Novi Sad, 21000 Novi Sad, Serbia;
Department of Geography, RWTH Aachen University, Germany;
Laboratory for Paleoenvironmental Reconstruction, Faculty of Sciences, University of Novi Sad, 21000 Novi Sad, Serbia;
Laboratory for Paleoenvironmental Reconstruction, Faculty of Sciences, University of Novi Sad, 21000 Novi Sad, Serbia;
Chair of Geography, Faculty of Philosophy, University of Eastern Sarajevo, Alekse Santica 1, 71420 Pale, Republic of Srpska, Bosnia and Herzegovina;
机译:欧洲黄土带最南端的贝洛蒂纳克断面(塞尔维亚南部):初步结果
机译:黄土 - 古溶液序列对南黄土高原颗粒尺寸成分对南黄土高原季度气候的影响
机译:来自南部莱索托的更新世晚期至全新世早期气候变化的稳定碳同位素证据
机译:古环境重建(植被和气候)在近期优先岛和全新世碳同位素的土壤后期龙底烯及全新世
机译:利用微量元素和稳定同位素特征进行的气候重建,保存在美国西维吉尼亚州南部阿巴拉契亚山脉的七叶树溪洞的晚更新世石笋早期。
机译:锶同位素揭示了中国南部红土盖层的风化过程对古地理重建具有重要意义
机译:基于发光的新的年代学框架将最后两个冰川周期定格在斯塔拉奇(塞尔维亚)欧洲更新世黄土的南端