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Ajab Singh

Biographic Data

ID6396111
NAMEAjab Singh
GIVEN NAMESAjab
FAMILY NAMESingh
SIGNATURESINGH A
AFFILIATIONSUniversity of Malaya
ORCID0000-0002-1936-1426
VERIFIEDYes
TOTAL WORKS3
TOTAL CITATIONS0
AUTHOR COUNT3
EDITOR COUNT0
FIRST PUBLICATION YEAR2019
LATEST PUBLICATION YEAR2024
H-INDEX0
  • Open paleoenvironment and dry climate in south India immediately before the Youngest Toba Tuff eruption (~75 ka) are suggested by Vondrichnus structures at the Jwalapuram locality, Jurreru valley

    Open Access•Ajab Singh•ARTICLE•Quaternary Research•2024

    The Younger Toba Tuff (YTT) eruption is regarded as one of the largest of its time and possibly responsible for changing past climate and vegetation from C 3 to C 4 in the Indian subcontinent. A paleosol constituting a Toba pre-tephra horizon at the Jwalapuram locality, exhibits the preservation of biogenic structures identified as Vondrichnus planoglobus and Vondrichnus obovatus. This study investigated their paleoecological and paleoenvironment…

  • A Review Study on Youngest Toba Tuff Ash, Artifacts and Vertebrate Remains Preserved in the Quaternary Alluvial Sediments of India and Their Significances in Climate and Paleoenvironment Interpretatio…

    Open Access•Ajab Singh, Ashok K Srivastava et al.•CHAPTER•Science, Policies and Conflicts…•2022

  • YTT ash from Quaternary sediments of Kapileshwar area, Purna alluvial basin, Central India

    Open Access•Ashok K Srivastava, Ajab Singh•ARTICLE•Quaternary International•2019

No prominent works on this page.

  • YTT ash from Quaternary sediments of Kapileshwar area, Purna alluvial basin, Central India

    Open Access•Ashok K Srivastava, Ajab Singh•ARTICLE•Quaternary International•2019

  • A Review Study on Youngest Toba Tuff Ash, Artifacts and Vertebrate Remains Preserved in the Quaternary Alluvial Sediments of India and Their Significances in Climate and Paleoenvironment Interpretatio…

    Open Access•Ajab Singh, Ashok K Srivastava et al.•CHAPTER•Science, Policies and Conflicts…•2022

  • Open paleoenvironment and dry climate in south India immediately before the Youngest Toba Tuff eruption (~75 ka) are suggested by Vondrichnus structures at the Jwalapuram locality, Jurreru valley

    Open Access•Ajab Singh•ARTICLE•Quaternary Research•2024

    The Younger Toba Tuff (YTT) eruption is regarded as one of the largest of its time and possibly responsible for changing past climate and vegetation from C 3 to C 4 in the Indian subcontinent. A paleosol constituting a Toba pre-tephra horizon at the Jwalapuram locality, exhibits the preservation of biogenic structures identified as Vondrichnus planoglobus and Vondrichnus obovatus. This study investigated their paleoecological and paleoenvironment…

Alluvium (2 works) · Geochemistry (2 works) · Geological and Geochemical Analysis (2 works) · Geology (2 works) · Geology and Paleoclimatology Research (2 works) · Geomorphology (2 works) · Paleontology (2 works) · Pleistocene-Era Hominins and Archaeology (2 works) · Quaternary (2 works) · Tephra (2 works)

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