摘要 : The most commonly used paleoclimatic proxies in speleothem studies are the carbon and oxygen stable isotopes and the trace elements of calcite. However, assessing the incorporation of other components, such as organic matter, may ... 展开
作者 | Martinez-Pillado~ V. Yusta~ I. Iriarte~ E. Alvaro~ A. Ortega~ N. Aranburu~ A. Arsuaga~ J. L. |
---|---|
作者单位 | |
期刊名称 | 《Quaternary International》 |
页码/总页数 | 141-151 / 11 |
语种/中图分类号 | 英语 / P5 |
关键词 | Speleothem color Organic matter Spectroscopy Fluorescence |
DOI | 10.1016/j.quaint.2020.04.006 |
馆藏号 | P-102 |