AH
About
Hi there! I am Abdul Hameed, and I am all about digging into the past to understand how our Earth used to be. I have got a Ph.D. in Paleopedology, which means I study ancient soils to figure out what the environment was like way back when they formed. My work helps us to learn about how the Earth has changed over time and what that means for us today. I am passionate about uncovering these stories from the ground and sharing them with others.
Employment
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State University of Campinas (UNICAMP) Postdoctoral Fellow (FAPESP)2025 - 2028
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University of Delhi Ph. D.2017 - 2023
Education
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University of Delhi M. Sc.2013 - 2015
Projects & Funding
Projects & funding information is unavailable.
Publications (11)
- Micromorphology and clay mineralogy of the palaeosols in the Lower Siwalik Sub-Group, Kangra sub-basin, NW Himalaya: a response to Himalayan orogeny and climate change Save
- Palaeopedogenesis and weathering in overbank sediments of the Siwalik Group: Link to Himalayan uplift and climate change during late Miocene Save
- Holocene climate variability deciphered from Chilika Lagoon sediments: Implication for anthropogenic activity or paleocyclones? Save
- Soil-geochemistry of the Ganga basin along a 2000 km transect: Implications for chemical weathering during pedogenesis influenced by source, climate, and neotectonics Save
- PALEOPEDOGENESIS IN OVERBANK SEDIMENTS OF SIWALIK GROUP, NW HIMALAYA: WEATHERING AND CLIMATE CHANGE DURING 12 TO 5 MA Save
- Major, trace and rare earth element geochemistry of Archaean carbonate sediments of Tanwan group rocks of the Bhilwara supergroup, India: implications for seawater geochemistry and depositional environment Save
- Clay mineralogical evidence of near-equatorial Palaeocene–Eocene Thermal Maximum in Barmer Basin, India Save
- Paleopedological evolution of Siwalik succession from Kangra sub-Basin, NW Himalayan: Implications for climate change and weathering conditions Save
- Paleopedology of Siwalik Paleosols of Kangra Sub-Basin, NW Himalaya: Implication for Weathering and Climate change 11 Ma to 6 Ma Save
- Micromorphology and clay mineralogy of lower siwalik paleosols: Implications for landscape stability and climatic fluctuations of 2.5 ka to 10 ka intervals at 12 ma in the Himalayan foreland basin Save