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| 1 | In- fluence of plant growth hormones on the growth of Mucorrouxii and chitosan production显示文摘 | Chatterjee Sandipan Chatterjee Sudipta Chatterjee B P | 2009 | Microbiological Research2009，164，3： | 1 |
| 2 | Enhancement of growth and chitosan production by Rhizopusoryzae in whey medium by plant growth hormones显示文摘 | Chatterjee Sudipta Chatterjee Sandipan Chatterjee B P | 2008 | Interna- tional Journal of Biological Macromolecules2008，42，2： | 1 |
| 3 | Clarification of fruit juice with chitosan显示文摘 | Sandipan Chatterjee Sudipta Chatterjeed | 2004 | Process Biochemistry2004，，39： | 1 |
| 4 | Clarification of fruit juice with chitosan显示文摘 | Sandipan Chatterjee Sudipta Chatterjee Bishnu P Chatterjee | 2004 | Process Biochem- istry2004，，39： | 1 |
| 5 | Clarification of fnfit juice with chitosan显示文摘 | Sandipan Chatteriee Sudipta Chatterjee Bishnu P Chatterjee | 2004 | Process biochemistry2004，39，12： | 1 |
| 6 | Adsorption of a model anionic dye, eosin Y, from aqueous solution by chitosan hydrobeads 显示文摘 | Sudipta Chatterjee Sandipan Chatterjee Bishnu P Chatterjee | 2005 | Journal of Colloid and Interface Science2005，288，1： | 1 |
| 7 | Clarification of fruit juice with chitosan显示文摘 | SANDIPAN CHATTERJEE SUDIPTA CHATTERJEE BISHNU P CHATTERJEE | 2004 | Process Biochemistry2004，39，12： | 1 |
| 8 | Clarification of fruit juice with chitosan显示文摘 | Sndipan Chatterjee Sudipta Chatterjee Bishnu P Chatterjee | 2004 | Process Bio- chemistry2004，39，12： | 1 |
| 9 | Adsorption of arsenite and arsenate onto muscovite and biotite mica显示文摘 | Sudipta Chakraborty Mariette Wolthers Debashis Chatterjee Laurent Charlet | 2006 | Colloid and Interface Science2006，5，： | 1 |
| 10 | Clarification of fruit juice with chitosan显示文摘 | Sandipan Chatterjee Sudipta Chatterjee Bishnu P. Chatterjee Arun K. Guha | 2003 | Process Biochemistry2003，，12： | 1 |
| 11 | Clarification of fruit juice with chitosan显示文摘 | CHATTERJEE Sandipan CHATTERJEE Sudipta CHATTERJEE B | 2004 | Process Biochemistry2004，39，12： | 1 |
| 12 | A new type of chitosan hydrogel sorbent generated by anionic surfactant gelation显示文摘 | Sudipta Chatterjee Tania Chtterjee Seung H Woo | 2010 | Bioresource Technology2010，101，： | 1 |
| 13 | Trace fossil evidences of an Early Miocene paleoseismic event and depositional regime change from the Kutch(Kachchh) Basin显示文摘Unconsolidated siliciclastic sediments can undergo post-burial deformation, which leads to the formation of distinctive sedimentary structures, known as soft-sediment deformation structures(SSDS). The presence of a series of sand volcanoes confined to a particular lithostratigraphic horizon can represent a paleoseismic activity and, thereby, exemplifies the concept of “seismite”. The Kutch Basin has been a tectonically active region since the initiation of eastern Gondwana rifting followed by a tectonic inversion during the Cenozoic due to the collision of the Indian and Eurasian plates. A stratum-bound series of sand volcanoes belonging to the Khari Nadi Formation(KNF) is exposed along the banks of Khari River. They separate the shallow marine deposits below and non-marine deposits above with their characteristic marine and paleosol trace fossil suites, respectively. Although a seismogenic origin has been much debated for the SSDS,the ichnofabric analysis of the sand-volcano-bearing stratum unequivocally points toward such an origin under a shallow seafloor condition. In addition to the sedimentary regime change from an open shallow-marine setting to a continental depositional environment concomitant with basinal uplift, the behavior of the burrowing crustaceans testifies to a syn-depositional development of a fault network associated with the fluidization, sand volcanism, and the resilience of the trace-producers in surviving those processes until the sedimentary regime change in the overlying strata. Although the ichno-sedimentological evidence apparently differs from the previous works that proposed a continuous base-level rise from the beginning of deposition of the Khari Nadi Formation up to the middle part of the overlying Chhasra Formation, the paleoseismic activity,its ichnologic signature, and the depositional regime change refer to a higher-resolution(i.e., lower-order)sequence-stratigraphic change causing a short-duration regression within a longer-duration cycle of base-level rise. | Ayush Srivastava Sudipta Dasgupta Krishanu Chatterjee Mohuli Das | 2024 | Journal of Palaeogeography2024，13，1： | 0 |
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