Knowledge Resource Center for Ecological Environment in Arid Area
DOI | 10.1016/j.polar.2021.100636 |
How strong was pedogenesis in Schirmacher Oasis during the Late Quaternary? | |
Warrier, Anish Kumar; Mahesh, B. S.; Sebastian, Joju George; Mohan, Rahul | |
通讯作者 | Warrier, AK (corresponding author), Manipal Acad Higher Educ, Manipal Inst Technol, Dept Civil Engn, Manipal 576104, Karnataka, India. |
来源期刊 | POLAR SCIENCE
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ISSN | 1873-9652 |
EISSN | 1876-4428 |
出版年 | 2021 |
卷号 | 30 |
英文摘要 | We compare the sediment magnetic properties of two lakes in Schirmacher Oasis, East Antarctica and discuss the intensity of pedogenesis during the Late Quaternary. The magnetic minerals are land-derived with no obliteration of the signal due to bacterial or anthropogenic sources. The magnetic grains of Lake L-49 are much smaller in size compared to Lake Sandy's (low ratio values of IRM20mT/ARM and S-20). The iron oxide minerals in Lake Sandy's sediments are coarse stable single domain (SSD) and multi-domain (MD) grains with the SSD concentration increasing during the Holocene. Percentage frequency-dependent susceptibility, a marker for pedogenic iron oxide minerals shows a similar trend for Lake Sandy, with the values remaining low during the Last Glacial Stage (LGS) and increasing towards the Holocene. Such a pattern is not observed in the sediments of Lake L-49. Principal Component Analysis reveals a relatively stronger intensity of pedogenesis in the Lake Sandy catchment during the deglaciation. From the data, we observe that even though pedogenesis is active, the intensity is not strong enough to form superparamagnetic (SP) grains. The peaks in chi(fd) for both the lakes show a direct relationship with Antarctic Isotope Maximum events recorded in an ice-core data suggesting that chi(fd) can be used as a proxy for paleo-pedogenesis in Antarctica. |
英文关键词 | Iron oxides Magnetic grain size Pedogenesis Environmental magnetism Schirmacher oasis East Antarctica |
类型 | Article |
语种 | 英语 |
收录类别 | SCI-E |
WOS记录号 | WOS:000729935500004 |
WOS关键词 | PRINCIPAL-COMPONENTS-ANALYSIS ; MAGNETIC-PROPERTIES ; EAST ANTARCTICA ; LAKE ; SOIL ; SEDIMENTS ; CLIMATE ; SURFACE ; VARIABILITY ; CALIBRATION |
WOS类目 | Ecology ; Geosciences, Multidisciplinary |
WOS研究方向 | Environmental Sciences & Ecology ; Geology |
资源类型 | 期刊论文 |
条目标识符 | http://119.78.100.177/qdio/handle/2XILL650/374000 |
作者单位 | [Warrier, Anish Kumar; Sebastian, Joju George] Manipal Acad Higher Educ, Manipal Inst Technol, Dept Civil Engn, Manipal 576104, Karnataka, India; [Warrier, Anish Kumar] Manipal Acad Higher Educ, Ctr Climate Studies, Manipal 576104, Karnataka, India; [Mahesh, B. S.; Mohan, Rahul] Minist Earth Sci, Natl Ctr Polar & Ocean Res, Vasco Da Gama 403804, Goa, India |
推荐引用方式 GB/T 7714 | Warrier, Anish Kumar,Mahesh, B. S.,Sebastian, Joju George,et al. How strong was pedogenesis in Schirmacher Oasis during the Late Quaternary?[J],2021,30. |
APA | Warrier, Anish Kumar,Mahesh, B. S.,Sebastian, Joju George,&Mohan, Rahul.(2021).How strong was pedogenesis in Schirmacher Oasis during the Late Quaternary?.POLAR SCIENCE,30. |
MLA | Warrier, Anish Kumar,et al."How strong was pedogenesis in Schirmacher Oasis during the Late Quaternary?".POLAR SCIENCE 30(2021). |
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