Inhibition of nonhomologous end joining to increase the specificity of CRISPR/Cas9 genome editing

DNA repair, one of the fundamental processes occurring in a cell, safeguards the genome and maintains its integrity. Among various DNA lesions, double-strand breaks are considered to be the most deleterious, as they can lead to potential loss of genetic information, if not repaired. Non-homologous end joining (NHEJ) and homologous recombination are two major double-strand break repair pathways. SCR7, a DNA ligase IV inhibitor, was recently identified and characterized as a potential anticancer compound. Interestingly, SCR7 was shown to have several applications, owing to its unique property as an NHEJ inhibitor. Here, we focus on three main areas of research in which SCR7 is actively being used, and discuss one of the applications, i.e. genome editing via CRISPR/Cas, in detail. In the past year, different studies have shown that SCR7 significantly increases the efficiency of precise genome editing by inhibiting NHEJ, and favouring the error-free homologous recombination pathway, both in vitro and in vivo. Overall, we discuss the current applications of SCR7 to shed light on the unique property of the small molecule of having distinct applications in normal and cancer cells, when used at different cellular concentrations.

Isotopic disequilibrium in Globigerina bulloides and carbon isotope response to productivity increase in Southern Ocean

Oxygen and carbon isotope ratios in planktonic foraminifera Globigerina bulloides collected from tow samples along a transect from the equatorial Indian ocean to the Southern Ocean (45 degrees E and 80 degrees E and 10 degrees N to 53 degrees S) were analysed and compared with the equilibrium delta O-18 and delta C-13 values of calcite calculated using the temperature and isotopic composition of the water column. The results agree within similar to 0.25% for the region between 10 degrees N and 40 degrees S and 75-200 m water depth which is considered to be the habitat of Globigerina bulloides. Further south (from 40 degrees S to 55 degrees S), however, the measured delta O-18 and delta C-13 values are higher than the expected values by similar to 2% and similar to 1% respectively. These enrichments can be attributed to either a `vital effect' or a higher calcification rate. An interesting pattern of increase in the delta C-13(DIC) value of the surface water with latitude is observed between 35 degrees S and similar to 60 degrees S, with a peak at similar to 42 degrees S. This can be caused by increased organic matter production and associated removal. A simple model accounting for the increase in the delta C-13(DIC) values is proposed which fits well with the observed chlorophyll abundance as a function of latitude.