Climate Change Data Portal
DOI | https://doi.org/10.1594/PANGAEA.875711 |
Major elemental concentrations from NGRIP ice core across the interstadial period GI-21.2 | |
Della Lunga; Damiano; Müller; Wolfgang; Rasmussen; Sune Olander; Svensson; Anders M; Vallelonga; Paul T | |
发布日期 | 2017-05-28 |
数据集类型 | dataset |
英文简介 | Several abrupt shifts from periods of extreme cold (Greenland stadials, GS) to relatively warmer conditions (Greenland interstadials, GI) called Dansgaard-Oeschger events are recorded in the Greenland ice cores. Using cryo-cell UV-laser-ablation inductively-coupled-plasma mass spectrometry (UV-LA-ICPMS), we analysed a 2.85 m NGRIP ice core section (~ 250 years; 2691.50–2688.65 m depth) across the transitions of GI-21.2, a short-lived interstadial prior to interstadial GI-21.1 (GI-21.2: 84.87–85.09 ka b2k). GI-21.2 is a ~100-year-long period with d18O values 3–4 per mil higher than the following ~200 years of stadial conditions (GS-21.2), which precede the major GI-21.1 warming. We report concentrations of "major" elements indicative of dust and/or sea salt (Na, Fe, Al, Ca, Mg) at a spatial resolution of ~ 200 µm, while maintaining detection limits in the low-ppb range, thereby achieving sub-annual time resolution even in deep NGRIP ice. We present an improved external calibration and quantification procedure using a set of five ice standards made from aqueous (international) standard solutions. Our results show that element concentrations decrease drastically (more than tenfold) at the warming onset of GI-21.2 at the scale of a single year, followed by relatively low concentrations characterizing the interstadial part before gradually reaching again typical stadial values. |
空间范围 | Latitude: 75.100000 * Longitude: -42.320000 |
时间范围 | 1996-07-01T00:00:00 - 1996-07-01T00:00:00 |
语种 | 英语 |
国家 | 国际 |
学科大类 | 气候变化 |
学科子类 | 冰冻圈 |
文献类型 | 数据集 |
条目标识符 | http://gcip.llas.ac.cn/handle/2XKMVOVA/213748 |
推荐引用方式 GB/T 7714 | Della Lunga,Damiano,Müller,et al. Major elemental concentrations from NGRIP ice core across the interstadial period GI-21.2.2017-05-28.https://doi.org/10.1594/PANGAEA.875711. |
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