Geomorphic Response to Rapid Uplift in a Folded Structure: The Upper Tigris Case

Author(s):  
Sabri Karadoğan ◽  
Catherine Kuzucuoğlu
FEBS Letters ◽  
2004 ◽  
Vol 577 (3) ◽  
pp. 403-408 ◽  
Author(s):  
Sonia Melino ◽  
Daniel O. Cicero ◽  
Fabio Forlani ◽  
Silvia Pagani ◽  
Maurizio Paci

PLoS ONE ◽  
2017 ◽  
Vol 12 (5) ◽  
pp. e0176775 ◽  
Author(s):  
Maya K. ◽  
Vishnu Mohan S. ◽  
Ruta B. Limaye ◽  
Damodaran Padmalal ◽  
Navnith K. P. Kumaran

2014 ◽  
Vol 14 (23) ◽  
pp. 12745-12762 ◽  
Author(s):  
B. Vogel ◽  
G. Günther ◽  
R. Müller ◽  
J.-U. Grooß ◽  
P. Hoor ◽  
...  

Abstract. Enhanced tropospheric trace gases such as CO, CH4 and H2O and reduced stratospheric O3 were measured in situ in the lowermost stratosphere over northern Europe on 26 September 2012 during the TACTS aircraft campaign. The measurements indicate that these air masses clearly differ from the stratospheric background. The calculation of 40-day backward trajectories with the trajectory module of the CLaMS model shows that these air masses are affected by the Asian monsoon anticyclone. Some air masses originate from the boundary layer in Southeast Asia/West Pacific and are rapidly lifted (1–2 days) within a typhoon up to the outer edge of the Asian monsoon anticyclone. Afterwards, the air parcels are entrained by the anticyclonic circulation of the Asian monsoon. The subsequent long-range transport (8–14 days) of enhanced water vapour and pollutants to the lowermost stratosphere in northern Europe is driven by eastward transport of tropospheric air from the Asian monsoon anticyclone caused by an eddy shedding event. We found that the combination of rapid uplift by a typhoon and eastward eddy shedding from the Asian monsoon anticyclone is a novel fast transport pathway that may carry boundary emissions from Southeast Asia/West Pacific within approximately 5 weeks to the lowermost stratosphere in northern Europe.


2021 ◽  
Vol 12 ◽  
Author(s):  
Tohru Minamino ◽  
Yusuke V. Morimoto ◽  
Miki Kinoshita ◽  
Keiichi Namba

FlgN, FliS, and FliT are flagellar export chaperones specific for FlgK/FlgL, FliC, and FliD, respectively, which are essential component proteins for filament formation. These chaperones facilitate the docking of their cognate substrates to a transmembrane export gate protein, FlhA, to facilitate their subsequent unfolding and export by the flagellar type III secretion system (fT3SS). Dynamic interactions of the chaperones with FlhA are thought to determine the substrate export order. To clarify the role of flagellar chaperones in filament assembly, we constructed cells lacking FlgN, FliS, and/or FliT. Removal of either FlgN, FliS, or FliT resulted in leakage of a large amount of unassembled FliC monomers into the culture media, indicating that these chaperones contribute to robust and efficient filament formation. The ∆flgN ∆fliS ∆fliT (∆NST) cells produced short filaments similarly to the ∆fliS mutant. Suppressor mutations of the ∆NST cells, which lengthened the filament, were all found in FliC and destabilized the folded structure of FliC monomer. Deletion of FliS inhibited FliC export and filament elongation only after FliC synthesis was complete. We propose that FliS is not involved in the transport of FliC upon onset of filament formation, but FliS-assisted unfolding of FliC by the fT3SS becomes essential for its rapid and efficient export to form a long filament when FliC becomes fully expressed in the cytoplasm.


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