Studie Milady Jonášové se zabývá využitím jmenované kantáty italského hudebního skladatele Benedetta Marcella operním impresáriem Antoniem Denziem v pasticciu "Sansone", provedeným v roce 1729 na scéně pražského divadla v paláci hraběte Františka Antonína Sporcka., Milada Jonášová., Rubrika: Studie, and České resumé na s. 51, anglický abstrakt na s. 5.
Studie Marie Škarpové se zabývá literárními prameny a okruhy duchovních písní, které byly inspirací pro repertoár kancionálu "Jesličky, staré a nové písničky", jehož autorem byl přední český barokní básník a duchovní Fridrich Bridelius., This study deals with that portion of the repertoire of the Czech Advent and Christmas songbook Jesličky (Prague, 1658) by Fridrich Bridelius, which newly appeared in Czech hymnography thanks to this song book, and it summarizes the various results of the search for textual sources from other languages for these “new” songs in Jesličky. It points out their ties to contemporary German written hymnography (of both German and Bohemian provenience) and to Latin hymnography, i.e. to contemporary Latin songs. The text is thus not only a contribution towards discovering the ways that Czech hymnographers of the 17th century became familiar with the new, i.e. baroque, poetic language, but also, above all, an attempt to stimulate further hymnological research on baroque hymnographic works in the early modern history of Central Europe and the interconnections and relationships between them., Marie Škarpová., Rubrika: Studie, and České resumé na s. 397, anglický abstrakt na s. 377.
Klíšťata sají obrovské množství krve, která je jejich jediným zdrojem živin a energie. Přesný enzymatický mechanismus zpracování krve ve střevě klíšťat však kupodivu nebyl donedávna vůbec znám. Náš komplexní molekulární model trávení hostitelského hemoglobinu u klíštěte obecného (Ixodes ricinus) poprvé odhalil analogii enzymatického aparátu s krevsajícími ploštěnci a hlísticemi, a zároveň tato znalost představuje zásadní poznatek pro účinný boj s klíšťaty a jimi přenášenými patogeny., Ticks (in this case Ixodidae and Argasidae) feed on enormous amounts of host blood, which provides their ultimate source of energy and nutrients. There has been only limited evidence on the exact molecular mechanisms of blood digestion in ticks. For the first time, our complex enzymatic model of proteolytic digestion in the Common Tick (Ixodes ricinus) reveals the analogy of tick intestinal proteolysis with bloodfeeding platyhelminthes and nematodes and presents a future application potential in tick or tick-borne pathogen interventions., and Daniel Sojka.
The 14-3-3 proteins are a family of acidicr egulatory molecules found in all eukaryotes. 14-3-3 proteins function as molecular scaffolds by modulating the conformation of their binding partners. Through the functional modulation of a wide range of binding partners, 14-3-3 proteins are involved in many processes including cell cycle regulation, metabolism control, apoptosis, and control of gene transcription. This minireview includes a short overview of 14-3-3 proteins and then focuses on their role in the regulation of two important binding partners: FOXO forkhead transcription factors and an enzyme tyrosine hydroxylase., V. Obšilová, J. Šilhan, E. Bouřa, J. Teisinger, T. Obšil., and Obsahuje bibliografii a bibliografické odkazy
Speleothems in 6 sandstone caves in the Bohemian Paradise (Český ráj) were dated by means of 14C and U-series methods. Stable isotopes of C and O, FAAS, IR, XRD, XRF and SEM were used to characterize the carbonate material and its source. Stable isotopes (C and O) composition of speleothems in two caves corresponds to values characteristic for cave speleothems in Central Europe. In other caves they indicate evaporation and fast carbon dioxide escape during carbonate precipitation. The speleothems from the Krtola Cave were deposited between 8 and 13 kyr BP. Speleothems were deposited 5-8 kyr BP in the Sintrová, Mrtvé Údolí and U Studánky caves. Calcite coatings on smooth sandstone surfaces in studied caves demonstrate that cave walls did not retreat even a few mm in the last 5-8 kyr since speleothem deposition and are thus not evolving under recent climatic conditions. Most of the cave ceilings and walls are at present time indurated by hardened surfaces, which protect the sandstone from erosion. Sandstone caves probably intensively evolved either during or at the end of the Last Glacial period. There are two different erosion mechanisms which might have formed/reshaped the caves at that time: A) In the case of permafrost conditions: Repeated freeze/melt cycles affecting sandstone pore space followed by the transport of fallen sand grains by minor temporary trickles. We expect that heat was transmitted by air circulating between the cave and the surface; B) Seepage erosion of sandstone during the melting of permafrost, prior forming of case hardening., Jiří Bruthans, Jana Schweigstillová, Petr Jenč, Zdeňka Churáčková and Petr Bezdička., and Obsahuje bibliografii