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| 1 | Slumping in the Upper Jurassic Baisakhi Formation of the Jaisalmer Basin, western India: Sign of synsedimentary tectonics?显示文摘A spectacularly exposed slump is described from a 120-m-long road cut between the villages of Kanod and Deva in the northeastern Jaisalmer Basin of Rajasthan,India.The Upper Jurassic part of the sediments at the outcrop was formed in a near-shore setting and belongs to the Ludharwa Member of the Baisakhi Formation.The 3-m-thick unit shows a number of asymmetric folds and thrust faults leading to an imbrication of partly lithified sandstone beds.The deformation structures allow the reconstruction of a movement towards the northwest.This agrees well with the basin configuration that shows a deepening into this direction.Although the determination of a specific trigger mechanism is difficult for soft-sediment deformation structures,an earthquake caused by synsedimentary tectonics in the basin seems to be the most likely explanation. | Matthias Alberti Dhirendra K.Pandey Jitendra K.Sharma Narendra K.Swami Alfred Uchman | 2017 | Journal of Palaeogeography2017，6，4： | 2 |
| 2 | Taxonomy and palaeocology of flysch trace fossils: the Marnosoarenacea formation and asso- ciated facies (Miocene, Northern Apennines, Italy ) 显示文摘 | UCHMAN A | 1995 | Beringeria1995，15，： | 1 |
| 3 | Vasoactive intestinal peptide (VIP) and pituitary adenylate cycla- se activating polypeptide (PACAP) in humans with multiple scle- rosis显示文摘 | BARANOWSKA BIK A KOCHANOWSKI J UCHMAN D | 2013 | J Neuroimmunol2013，263，12： | 1 |
| 4 | Superporous organice-inorganic poly(N-isopropylacrylamide)-based hydrogel with a very fast temperature response显示文摘 | Strachotova B Strachota A Uchman M | 2007 | Polymer2007，48，6： | 1 |
| 5 | Early Devonian trace fossils in marine to non-marine redbeds in Podolia,Ukraine:palaeoenvironmental implications显示文摘 | Uchman A Drygant D Paszkowski M etal | 2004 | Palaeogeography Palaeoclimatology Palaeoecology2004，214，12： | 1 |
| 6 | Large microbial- foraminiferal oncoids from condensed lower-middle Jurrassic deposits: A case study from the Tatra Mountains, Poland 显示文摘 | Gradzinski M Tyszka J Alfred Uchman A | 2004 | Palaeogeography Palaeoclimatology Palaeoecology2004，213，： | 1 |
| 7 | Super porous organic-inorganic poly (N-isopropylacrylamide)-based hydrogel with a very fast temperature response 显示文摘 | Strachotov B Strachota A Uchman M | 2007 | Poly- mer2007，48，6： | 1 |
| 8 | Ichnology of the rhenodanubian flysh (Lower Cretaceous-Eocene)in Austria and Germany 显示文摘 | UCHMAN A | 1999 | Beringeria1999，25，： | 1 |
| 9 | Ichnology of eocene flysh de- posits of the Istria Peninsula, Croatia and Slovenia 显示文摘 | TUNIS G UCHMAN A | 1996 | Ichnos1996，5，： | 1 |
| 10 | Taxonomy and palaeoecology of flysh trace fossils:The Marnoso-arenacea Formation and as- sociated facies 显示文摘 | UCHMAN A | 1995 | Beringgeria1995，15，： | 1 |
| 11 | Trends in diversitry frequency and com- plexity of graphoglyptid trace fossils:evolutionary and palaeoeoenvironmental aspects 显示文摘 | UCHMAN A | 2003 | Palaeo2003，192，： | 1 |
| 12 | The oldest deep-sea Ophiomorpha and Scolicia and associated trace fossils from the Upper Jurassic - Lower Cretaceous deep-water turbidite deposits of SW Bulgaria 显示文摘 | TCHOUMATCHENCO P UCHMAN A | 2001 | Palaeogeography Palaeoclimatology Palaeoecology2001，169，12： | 1 |
| 13 | A zoophycos group trace fossil from miocene flysch in Southern Turkey: Evidence for a U-shaped causative burrow显示文摘 | Alfred Uchman Huriye Demircan | 1999 | Ichnos1999，，4： | 1 |
| 14 | Super porous organic-inorganic poly (N-isopropylacrylamide)-based hydrogel with a very fast temperature response显示文摘 | Strachotova B Strachota A Uchman M | 2007 | Polymer2007，48，： | 1 |
| 15 | Super porous organic-inorganic poly (N-isopropylacrylamide)-based hydrogel with a very fast temperature response显示文摘 | Strachotová B Strachota A Uchman M | 2007 | Polymer2007，48，6： | 1 |
| 16 | Cellulose-based graft copolymers with controlled architecture prepared in a homogeneous phase显示文摘 | RAUS V STEPANEK M UCHMAN M | 2011 | Journal of Polymer Science Part A:Polymer Chemistry2011，49，： | 1 |
| 17 | Revision of the Ichnogenus Sabellarifex Richter, 1921 and its relationship to Sko- lithos Haldeman, 1840 and Polykladichnus Ftirsich, 1981 显示文摘 | SCHLIRF M UCHMAN A | 2005 | Journal of Systematic Palaeontology2005，，3： | 1 |
| 18 | Trace fossils of an amalgamated storm-bed succession from the Jurassic of the Kachchh Basin,India:The significance of time-averaging in ichnology显示文摘The uppermost part of the Upper Bathonian Sponge Limestone member, Patcham Formation, of the Jhura Dome of Kachchh Mainland is a thickening-and shallowing-upward succession topped by medium-to thick-bedded hummocky cross-stratified grainstones deposited by storm waves. Occasionally, thin, commonly lenticular, intraclastic-bioclastic silty marl intercalations between the grainstones are highly bioturbated, in contrast to the grainstones, in which, for the most part, trace fossils occur scattered. Large exposures of bedding planes of the grainstones allow the detailed investigation of ichnological features, whereas the high density of traces in the soft marls precludes the identification of any ichnotaxa. Eighteen ichnotaxa have been recorded including Ophiomorpha, Thalassinoides, Taenidium, Gyrophyllites, Chondrites, Dactyloidites, Teichichnus, Bolonia, and Ancorichnus. Except for Ophiomorpha nodosa and Thalassinoides, which generally indicate moderate to high energy conditions and are the dwelling burrows of suspension-feeding to omnivorous crustaceans, the ichnotaxa represent a deposit-feeding behaviour of their producers and thus are characteristic of low-energy environments. The trace fossils form three ichnoassemblages characterized by(1) Ophiomorpha nodosa and Thalassinoides suevicus,(2)?Thalassinoides isp. A, Taenidium, and Bolonia lata,and(3) Ancorichnus. The dominance of traces of deposit-feeders in rocks indicative of high-energy events is counterintuitive and points to their non-contemporaneity. The sediments were deposited during brief highenergy events, whereas the trace fossils were produced when, after waning of storms low-energy conditions prevailed. This time-averaging is particularly pronounced in trace fossils that extend vertically downwards and may reach strata deposited under distinctly different conditions. Thus, environmental interpretations based on trace fossils should refer to colonisation surfaces rather than to the sediment surrounding the trace fossils. In the latter case, interpretations may be erroneous, especially when erosion subsequently destroyed sedimentary evidence of their original environment. | Franz To Fürsich Alfred Uchman Matthias Alberti Dhirendra K.Pandey | 2018 | Journal of Palaeogeography2018，7，1： | 1 |
| 19 | 显示文摘 | Strachotova B Strachota A Uchman M | 2007 | Polymer2007，48，6： | 1 |
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