海面下に着底した東南極氷床の安定性に関する研究

第一阶段：完成东南极洲阿德利盆地高分辨率样品制备，完成加速器质谱法铍同位素分析。详细介绍高分辨率数据集的手稿正在准备提交给科学期刊。第二阶段：利用加速器质谱仪对来自东南极洲萨布丽娜海岸地区的额外样品进行铍同位素分析。将其与附近较浅深度的地核进行比较，尽管地核位置接近，但数据中存在一些有趣的差异。研究结果正在与合著者进行讨论，这些数据以海报的形式在日本地球科学联合会会议和美国地质学会会议上发表。第三阶段：利用加速器质谱法对塔斯马尼亚西海岸Selina湖的样品进行了分析，涵盖了过去5个海洋同位素阶段（MIS 1-5）。随着样本数量的增加，看到比预期更强烈的气候信号是很有趣的。这项分析的结果在美国地质学会会议上作为口头报告提出，手稿已经完成，正在与合著者进行讨论。它将很快提交给一家科学杂志。

Phase 1: Preparation of the high resolution Adelie Basin, East Antarctica samples has been completed, and analysis of beryllium isotopes by accelerator mass spectrometry is finished. A manuscript detailing the high resolution dataset is being prepared for submission to a scientific journal.Phase 2: Additional samples from the Sabrina Coast region of East Antarctica have been analyzed by accelerator mass spectrometer for beryllium isotopes. Comparison to a nearby core at a shallower depth reveal some interesting differences in the data, despite the proximity of the core sites. The results are under discussion with coauthors, and the data was presented at the Japan Geosciences Union meeting and the Geological Society of America meeting in poster form.Phase 3: Samples from Lake Selina in the West Coast Range of Tasmania have been analyzed by accelerator mass spectrometry, covering the past five marine isotope stages (MIS 1-5). With a greater sample number, it has been interesting to see a stronger climate signal than expected. The results from this analysis were presented at the Geological Society of America meeting as an oral presentation, and the manuscript is complete and under discussion with coauthors. It will shortly be submitted to a scientific journal.