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The M17 leucine aminopeptidase of the malaria parasite Plasmodium falciparum : importance of active site metal ions in the binding of substrates and inhibitors
The M17 leucine aminopeptidase of the intraerythrocytic stages of the malaria parasite Plasmodium falciparum (PfLAP) plays a role in releasing amino acids from host hemoglobin that are used for parasite protein synthesis, growth, and development. This enzyme represents a target at which new antimalarials could be designed since metalloaminopeptidase inhibitors prevent the growth of the parasites i
Novel APC-cleavage sites in FVa providing insights into mechanisms of action of APC and its cofactor protein S.
A comparison of autumn migratnion strategies in robins erithacus rubecula at a coastal and an inland site in southern Sweden
Coverage- and temperature-dependent site occupancy of carbon monoxide on Rh(111) studied by high-resolution core-level photoemission
Adsorption sites in coadsorption systems determined by photoemission spectroscopy : K and CO coadsorbed on Rh(111)
IEA-HIA Task 23 Small Scale Reformers for On-site Hydrogen Supply
NMR structure determination of proteins supplemented by quantum chemical calculations: Detailed structure of the Ca2+ sites in the EGF34 fragment of protein S
Comparison of horizontal and vertical advective CO2 fluxes at three forest sites
Developing A Proactive Safety Performance Measurement Tool (SPMT) For Construction Sites
Azaflavones compared to flavones as ligands to the benzodiazepine binding site of brain GABA(A) receptors.
Localization of phosphatidylserine binding sites to structural domains of factor X-a
An exploratory study of Middle Stone Age and Later Stone Age site locations in Kenya’s Central Rift Valley using landscape analysis : a GIS approach
The Kenyan central rift has witnessed dramatic climatic changes over relatively short periods of time in response to global climatic changes, with the water levels of the lakes within the rift rising and falling with these changing conditions. There is considerable evidence showing extreme wet and dry phases throughout their existence. These wet and dry phases also influenced the vegetation cover,
