globalchange  > 过去全球变化的重建
DOI: 10.1016/j.palaeo.2016.05.011
论文题名:
Reply to the comment on “Geochemistry of buried river sediments from Ghaggar Plains, NW India: Multi-proxy records of variations in provenance, paleoclimate, and paleovegetation patterns in the Late Quaternary” by Singh et al. (2016), Palaeogeography, Palaeoclimatology, Palaeoecology 449 (2016) 85–100
作者: Singh A.; Paul D.; Sinha R.; Thomsen K.J.; Gupta S.
刊名: Palaeogeography, Palaeoclimatology, Palaeoecology
ISSN: 0031-0182
出版年: 2016
卷: 455
起始页码: 68
结束页码: 70
语种: 英语
英文关键词: Buried sediment ; Ghaggar river ; Isotopic composition ; Paleoclimate ; Provenance
英文摘要: In the comment on our paper (this issue), Clift et al. (2016) compared our recently reported radiogenic Nd-isotopic record in two drill cores (Singh et al., 2016) with those from the Hakra floodplain sediments and Indus Delta sediments. While they agree with the concept of erosion patterns in the western Himalayan sources being climatically modulated, they offer an alternative interpretation for our reported variability in the radiogenic Nd-isotopic values. Here, we show that the Nd-isotopic values for the Holocene succession instead can be explained by the bedrock geology of the source region of these sediments. Moreover, we note that whereas our paper considers a ~ 75 ka fluvial depositional record, their comment is only based on the post-Last Glacial Maximum (LGM) record. When considering the longer record, their arguments do not negate the main conclusions of our original paper. © 2016 Elsevier B.V.
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资源类型: 期刊论文
标识符: http://119.78.100.158/handle/2HF3EXSE/68379
Appears in Collections:过去全球变化的重建

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作者单位: Department of Earth Sciences, Indian Institute of Technology Kanpur, India; Centre for Nuclear Technologies, Technical University of Denmark, Roskilde, Denmark; Imperial College London, London, United Kingdom

Recommended Citation:
Singh A.,Paul D.,Sinha R.,et al. Reply to the comment on “Geochemistry of buried river sediments from Ghaggar Plains, NW India: Multi-proxy records of variations in provenance, paleoclimate, and paleovegetation patterns in the Late Quaternary” by Singh et al. (2016), Palaeogeography, Palaeoclimatology, Palaeoecology 449 (2016) 85–100[J]. Palaeogeography, Palaeoclimatology, Palaeoecology,2016-01-01,455
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