throughout human evolution history, beauty has always been one of the necessary integral components of human need. as greer (2010) said, “one of the prehistoric human’s responses to the animal life around them was to etch and paint these animals on the walls of their caves. turning them into art and rendering them beautiful was a natural response - a way to help make sense of a hostile and conf...

anxiety comprises many clinical descriptions and phenotypes. a genetic predisposition to anxiety is undoubted; however, the nature and extent of that contribution is still unclear. extensive genetic studies of the serotonin (5-hydroxytryptamine, 5-ht) transporter (5-htt) gene have revealed how variation in gene expression can be correlated with anxiety phenotypes. complete genome-wide linkage s...

since last few decades, the rapid industrialization has led to the development of many new chemicals, namely of which different kind of pesticides are of the most important ones. it is now evident that almost every food, agricultural product, water, soil and human body etc. is contaminated with some sort of chemical or pesticide. in some highly industrialized countries, new ailments have been r...

Although the spatiotemporal oscillations of Greenland Ice Sheet (GrIS) during last millennia have played a prominent role in global environmental changes, its glacial response to natural variability still needs be better constrained. Here, we focused on reconstruction behavior and deglaciation process along Tyroler Valley (74° N, 22° E), within Northeast National Park. This NW-SE valley connect...

In southern South America, well-dated glacial geomorphological records constrain the last cycle across much of former Patagonian Ice Sheet, but its northeastern sector remains comparatively understudied and unconstrained. This knowledge gap inhibits our understanding timing maximum glacier extent, duration maximum, onset deglaciation, whether asynchronies exist in behaviour ice sheet with latit...

Abstract The modern, over 250-m-deep basin of Lake Constance represents the underfilled northern part an 400-m-deep, glacially overdeepened trough, which reaches well into Alps at its southern end. overdeepening was formed by repeated glacial advance-retreat cycles Rhine Glacier throughout Middle to Late Pleistocene. A seismic survey revealed a Quaternary sediment fill more than 150 m thickness...