Anshuman Swain

3 weeks ago | analyticalsciencejournals.onlinelibrary.wiley.com | Paul Jacobs |Anshuman Swain |Neil Wilson |Wyger M. Brink

APT amide proton transfer BM4D four-dimensional Bloch matching CEST chemical exchange saturation transfer DS direct saturation MT magnetization transfer NOE nuclear Overhauser effect NOEMTR nuclear Overhauser effect magnetization transfer ratio PCB printed circuit board rNOE relayed nuclear Overhauser effect RF radiofrequency RMSE root mean squared error ROI region of interest SAR specific absorption rate SPM12 statistical parametric mapping 12 WASSR water saturation shift referencing 1...

Sep 8, 2024 | nature.com | Richard J. Knecht |Jacob S. Benner |Anshuman Swain |Lauren Azevedo-Schmidt |Michael S. Engel |Paul Selden | +2 more

AbstractMuch of what we know about terrestrial life during the Carboniferous Period comes from Middle Pennsylvanian (~315–307 Mya) Coal Measures deposited in low-lying wetland environments1,2,3,4,5. We know relatively little about terrestrial ecosystems from the Early Pennsylvanian, which was a critical interval for the diversification of insects, arachnids, tetrapods, and seed plants6,7,8,9,10.