Knowledge Resource Center for Ecological Environment in Arid Area
DOI | 10.1007/978-3-030-01599-2_13 |
The Thar Desert Calcretes: A Proxy for Understanding Late Quaternary Paleoclimate Shifts | |
Achyuthan, Hema | |
通讯作者 | Achyuthan, H (corresponding author), Anna Univ, Inst Ocean Management, Chennai 600025, Tamil Nadu, India. |
会议名称 | 1st Springer Conference of the Arabian-Journal-of-Geosciences (CAJG) |
会议日期 | NOV 12-15, 2018 |
会议地点 | Hammamet, TUNISIA |
英文摘要 | In the Thar Desert, India, calcretes occur in several geomorphic environments and have been classified based on their form, induration, chemistry and associations with parent material. These calcretes have been dated from late Neogene-Early Pleistocene (hardpan calcretes) to 5 ka (nodular calcretes). The calcretes consist of CaCO3 (40-75%) with SiO2, Al2O3 and Fe2O3 content in decreasing amounts. Integration of multiple data including textural, chemistry and soil micromorphology indicate that the calcrete nodules formed within the dunes are pedogenic in origin while those occurring in the interdunal depressions are largely groundwater formations. Hardpan calcretes formed on various types of bedrocks are geosols and complex in origin. Stable isotope data for the pedogenic calcretes of C and O vary from -3.8 to -0.2 parts per thousand, and between -6.1 and -1.5% for O-18 PDB values, groundwater calcretes (delta C-13 -2.0 and 2.5 parts per thousand, and between -5 and -1 parts per thousand for delta O-18) and hardpan calcretes yield slightly higher delta O-18 values (-5.9 to -1.3 parts per thousand) than the eolian pedogenic carbonates indicating that the calcretes in the desert margin of the Thar Desert was formed near the surface supporting a thin veneer of soil column. The carbon isotope values signify both C3 and C4 vegetation, with increasing C4 vegetation since the late Quaternary period. |
英文关键词 | Late Quaternary Calcrete Pedogenic Groundwater Geosols Semi-arid to arid conditions |
来源出版物 | PATTERNS AND MECHANISMS OF CLIMATE, PALEOCLIMATE AND PALEOENVIRONMENTAL CHANGES FROM LOW-LATITUDE REGIONS |
ISSN | 2522-8714 |
EISSN | 2522-8722 |
出版年 | 2019 |
页码 | 53-57 |
ISBN | 978-3-030-01599-2; 978-3-030-01598-5 |
出版者 | SPRINGER INTERNATIONAL PUBLISHING AG |
类型 | Proceedings Paper |
语种 | 英语 |
收录类别 | CPCI-S |
WOS记录号 | WOS:000623519900013 |
WOS关键词 | GEOCHEMISTRY ; CARBONATES ; RAJASTHAN |
WOS类目 | Environmental Sciences ; Meteorology & Atmospheric Sciences ; Oceanography |
WOS研究方向 | Environmental Sciences & Ecology ; Meteorology & Atmospheric Sciences ; Oceanography |
资源类型 | 会议论文 |
条目标识符 | http://119.78.100.177/qdio/handle/2XILL650/370228 |
作者单位 | [Achyuthan, Hema] Anna Univ, Inst Ocean Management, Chennai 600025, Tamil Nadu, India |
推荐引用方式 GB/T 7714 | Achyuthan, Hema. The Thar Desert Calcretes: A Proxy for Understanding Late Quaternary Paleoclimate Shifts[C]:SPRINGER INTERNATIONAL PUBLISHING AG,2019:53-57. |
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