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In this study, we analyzed the influence of El Niño-Southern Oscillation (ENSO) on the spatio-temporal variability of droughts in Ecuador for a 48-year period (1965-2012). Droughts were quantified from 22 high-quality and homogenized time series of precipitation and air temperature by means of the Standardized Precipitation Evapotranspiration Index. In addition, the propagation of two different ENSO indices (El Niño 3.4 and El Niño 1 + 2 indices) and other atmospheric circulation processes (e.g., vertical velocity) on different time-scales of drought severity were investigated. The results showed a very complex influence of ENSO on drought behavior across Ecuador, with two regional patterns in the evolution of droughts: (1) the Andean chain with no changes in drought severity, and (2) the Western plains with less severe and frequent droughts. We also detected that drought variability in the Andes mountains is explained by the El Niño 3.4 index [sea surface temperature (SST) anomalies in the central Pacific], whereas the Western plains are much more driven by El Niño 1 + 2 index (SST anomalies in the eastern Pacific). Moreover, it was also observed that El Niño and La Niña phases enhance droughts in the Andes and Western plains regions, respectively. The results of this work could be crucial for predicting and monitoring drought variability and intensity in Ecuador. [ABSTRACT FROM AUTHOR]

HLA-G and HLA-A frequencies have been analysed in Amerindians from Ecuador. HLA-G allele frequencies are found to be closer to those of other Amerindians (Mayas from Guatemala and Uros from Peru) and closer to European ones than to Far East Asians groups, particularly, regarding to HLA-G*01:04 allele. HLA-G/-A haplotypes have been calculated for the first time in Amerindians. It is remarkable that HLA-G*01:05N "null" allele is found in a very low frequency (like in Amerindian Mayas and Uros) and is also found in haplotypes belonging to the HLA-A19 group of alleles (HLA-A*30, -A*31, -A*33). It was previously postulated that HLA-G*01:05N appeared in HLA-A*30/-B*13 haplotypes in Middle East Mediterraneans. It may be hypothesized that in Evolution, HLA-G*01:05N existed primarily in one of the HLA extant or extinct -A19 haplotype, whether this haplotype was placed in Middle East or other World areas, including America. However, the highest present day HLA-G*01:05N frequencies are found in Middle East Mediterraneans., (Copyright © 2017. Published by Elsevier Inc.)