Abdur Rahman

Publications

• Late Holocene fire and precipitation history of the Kashmir Himalaya: Inferences from black carbon in lake sediments
• Isotopic Evidence for Degradation of Particulate Black Carbon in the Ocean
• Non-Redfieldian C:N:P ratio in the inorganic and organic pools of the Bay of Bengal during the summer monsoon
• Report on Quantitative Reconstruction and Numerical Methods for Analysis of Past Climate Variability Using Diatoms
• Palaeoenvironment shifts during last ~ 500 years and eutrophic evolution of the Wular Lake, Kashmir Valley, India
• Paleo-biogeochemistry of the Central Himalayan region during late MIS 3 using stable isotopic composition of organic matter occluded in diatoms and lake sediments
• Isotopic exploration of eco-hydrological connectivity in the riparian zones of Southern Western Ghats, India
• Paleoenvironment of the Central Himalaya during late MIS 3 using stable isotopic compositions of lacustrine organic matter occluded in diatoms and sediments
• Hydrological characteristics of the Bay of Bengal water column using δ18O during the Indian summer monsoon
• Nitrous oxide in the central Bay of Bengal during the summer monsoon
• Signatures of natural to anthropogenic transition in lake sediments from the Central Himalaya using stable isotopes
• Late Holocene paleoclimate reconstruction of northern Taiwan using a multiproxy approach in the Dream Lake sediment core
• Transport pathways of black carbon to a high mountain Himalayan lake during late Holocene: Inferences from nitrogen isotopes of black carbon
• Lake desiccation drives carbon and nitrogen biogeochemistry of a sub-tropical hypersaline lake
• Carbon and nitrogen biogeochemistry of a high-altitude Himalayan lake sediment: Inferences for the late Holocene climate
• Wildfire-vegetation-climate-human interactions in the central Taiwan region during 17.3–2.0 cal kyr BP, inferred from sediments of Toushe Basin
• Primary production and dinitrogen fixation in a subtropical inland saline environment
• Wildfire, vegetation, and climate history of central Taiwan from the end of the last glaciation to the late Holocene
• Transition of a semi-arid lake from freshwater to saline system: significant change in biogeochemical process rates
• Climate-fire-human interactions and their impact on the limnology conditions of the Dongyuan Lake, Southern Taiwan during the last 1800 cal years BP