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Using conventional decay or beta counting, sample sizes ranging from about 0.5 to 10 g of carbon are typical.
It is bounded and defined by the Carpathian Mountains to the east and south, and the Apuseni Mountains to the west.
As a diverse and relatively protected region, the area has always been rich in wildlife, and remains one of the more ecologically diverse areas in Europe.
The chronological frame of the Paleolithic coincides with that of the Pleistocene (the first period of the Quaternary), and is marked by four great glaciations, as established in the Alps (Günz, Mindel, Riss and, Würm).
While an ever-increasing amount of data has become available on the evolution of the climate, fauna and vegetation of present-day Romania, there is very little in the fossil record to give researchers an idea of what Paleolithic man in Romania looked like.
This “great summer” effect was the chief reason the Earth had emerged from an ice age, because hot northern summers had melted the great ice caps of North America and Eurasia, exposing darker land and sea to absorb more sunlight and warm the whole planet.
The effect was huge: about an extra 50 watts per square metre 80 degrees north in June.
C) dating is an isotopic or nuclear decay method of inferring age for organic materials.
The technique provides a common chronometric time scale of worldwide applicability on a routine basis in the age range from about 300 calender years to between 40,000 and 50,000 years.
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