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DOI | https://doi.org/10.1594/PANGAEA.833377 |
Seasonal changes in sediment core PS1795-2 | |
Sprenk; Daniela; Weber; Michael E; Kuhn; Gerhard; Wennrich; Volker; Hartmann; Thomas; Seelos; Klemens | |
发布日期 | 2014-06-17 |
数据集类型 | dataset |
英文简介 | The Weddell Sea and the associated Filchner-Rønne Ice Shelf constitute key regions for global bottomwater production today. However, little is known about bottom-water production under different climate and icesheet conditions. Therefore, we studied core PS1795, which consists primarily of fine-grained siliciclastic varves that were deposited on contourite ridges in the southeastern Weddell Sea during the Last Glacial Maximum (LGM). We conducted high-resolution X-ray fluorescence (XRF) analysis and grain-size measurements with the RADIUS tool (Seelos and Sirocko, 2005, doi:10.1111/j.1365-3091.2005.00715.x) using thin sections to characterize the two seasonal components of the varves at sub-mm resolution to distinguish the seasonal components of the varves. |
空间范围 | Latitude: -74.500160 * Longitude: -28.188500 |
时间范围 | 1990-01-18T15:07:00 - 1990-01-18T15:07:00 |
语种 | 英语 |
国家 | 国际 |
学科大类 | 气候变化 |
学科子类 | 气候变化 |
文献类型 | 数据集 |
条目标识符 | http://gcip.llas.ac.cn/handle/2XKMVOVA/233545 |
推荐引用方式 GB/T 7714 | Sprenk,Daniela,Weber,et al. Seasonal changes in sediment core PS1795-2.2014-06-17.https://doi.org/10.1594/PANGAEA.833377. |
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