Contacts in the last 90,000 years over the Strait of Gibraltar evidenced by genetic analysis of wild boar (Sus scrofa)

[EN] Contacts across the Strait of Gibraltar in the Pleistocene have been studied in different research papers, which have demonstrated that this apparent barrier has been permeable to human and fauna movements in both directions. Our study, based on the genetic analysis of wild boar (Sus scrofa), suggests that there has been contact between Africa and Europe through the Strait of Gibraltar in the Late Pleistocene (at least in the last 90,000 years), as shown by the partial analysis of mitochondrial DNA. Cytochrome b and the control region from North African wild boar indicate a close relationship with European wild boar, and even some specimens belong to a common haplotype in Europe. The analyses suggest the transformation of the wild boar phylogeography in North Africa by the emergence of a natural communication route in times when sea levels fell due to climatic changes, and possibly through human action, since contacts coincide with both the Last Glacial period and the increasing human dispersion via the strait.This study was supported by The Emirates Centre for Wildlife Propagation (Morocco). The funder had no role in study design, data collection and analysis, decision to publish, or preparation of the manuscript.Soria-Boix, C.; Donat-Torres, MP.; Urios, V. (2017). Contacts in the last 90,000 years over the Strait of Gibraltar evidenced by genetic analysis of wild boar (Sus scrofa). PLoS ONE. 12(7). doi:10.1371/journal.pone.0181929S12

Genome-wide analysis reveals the ancient and recent admixture history of East African Shorthorn Zebu from Western Kenya

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Arthrobacter D-xylose isomerase: partial proteolysis with thermolysin.

The pattern and kinetics of partial proteolysis of Arthrobacter D-xylose isomerase tetramer was studied in order to determine the flexibility of surface loops that may control its stability. It was completely resistant to trypsin, chymotrypsin and elastase at 37 degrees C, but thermolysin cleaved specifically and quantitatively at Thr-347-Leu-348 between helices 10 and 11 to remove 47 residues from the C-terminus of each 43.3 kDa subunit. At high temperatures, helices 9 and 10 were removed from each 38 kDa subunit to give a 36 kDa tetramer. The kinetics of nicking by thermolysin indicated that the Thr-347-Leu-348 loop is locked at low temperatures, but 'melts' at 25 degrees C and is fully flexible above 34 degrees C. The flexibility appears to be associated with binding of Ca2+ ions at the active site, since Co2+, Mg2+ and xylitol protect in proportion to their ability to displace Ca2+. The missing C-terminal helices make many intersubunit contacts that appear in the structure to stabilize the tetramer, but the properties of the purified nicked proteins are almost indistinguishable from the native enzyme. Both the 38 kDa tetramer and the 36 kDa tetramer are identically active and dissociate similarly in urea or SDS to fully active dimers, but the nicked dimers are slightly less stable to urea at 62 degrees C. In the Mg2+ form the thermostability of the 38 kDa tetramer is identical with that of the native enzyme, but the 36 kDa tetramer has a slightly lower 'melting point' (70 degrees C versus 80 degrees C), which may be due to unravelling from the end of helix 8. Since elimination of all the C-terminal helices and many intersubunit contacts has so little effect, one can conclude that the 'weak point' that controls the protein's thermostability lies within the N-terminal beta-barrel domain