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Creators/Authors contains: "Chatterjee, Abhishek"

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  1. ; ; ; ; (, Journal of the American Chemical Society)
    Controlling the structure and reactivity of the chain-end group is a central objective in modern polymer chemistry. Here, we introduce 3,6-anhydrogalactal as a single-addition monomer that enables efficient and versatile chain-end functionalization of metathesis polymers. Readily synthesized from biomass-derived galactal, 3,6-anhydrogalactal exhibits excellent single-addition reactivity, allowing precise chain-end modifications even when introduced simultaneously with the propagating monomer. Theoretical calculations provide mechanistic insights into the unique reactivities governing its single-addition behavior. Its broad functional group compatibility facilitates diverse applications, including block copolymer synthesis, polymer-polymer coupling, and bioconjugation, demonstrating significant potential for advancing polymer materials and bioconjugation strategies. 
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    Free, publicly-accessible full text available May 21, 2026
  2. ; ; ; ; ; ; ; ; ; ; et al (, Nature Chemical Biology)
    Free, publicly-accessible full text available August 21, 2026
  3. ; (, GEN Biotechnology)
    Free, publicly-accessible full text available December 1, 2025
  4. ; ; ; ; ; ; ; ; ; (, Nature)
    Free, publicly-accessible full text available December 11, 2025
  5. ; ; ; ; ; ; ; ; (, Nature Chemistry)
    Full Text Available 
  6. ; ; ; ; ; (, Journal of the American Chemical Society)
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  7. ; ; ; ; ; ; ; ; ; ; et al (, Nature Reviews Earth & Environment)
    Free, publicly-accessible full text available November 1, 2025
  8. ; ; ; ; ; ; ; ; ; ; et al (, Journal of the American Chemical Society)
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  9. ; ; ; ; ; ; ; ; ; ; et al (, Nature Climate Change)
    Abstract The Arctic–Boreal Zone is rapidly warming, impacting its large soil carbon stocks. Here we use a new compilation of terrestrial ecosystem CO2fluxes, geospatial datasets and random forest models to show that although the Arctic–Boreal Zone was overall an increasing terrestrial CO2sink from 2001 to 2020 (mean ± standard deviation in net ecosystem exchange, −548 ± 140 Tg C yr−1; trend, −14 Tg C yr−1;P < 0.001), more than 30% of the region was a net CO2source. Tundra regions may have already started to function on average as CO2sources, demonstrating a shift in carbon dynamics. When fire emissions are factored in, the increasing Arctic–Boreal Zone sink is no longer statistically significant (budget, −319 ± 140 Tg C yr−1; trend, −9 Tg C yr−1), and the permafrost region becomes CO2neutral (budget, −24 ± 123 Tg C yr−1; trend, −3 Tg C yr−1), underscoring the importance of fire in this region. 
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    Free, publicly-accessible full text available February 1, 2026
  10. ; ; ; ; ; ; ; ; ; ; et al (, Nature Methods)
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