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Upper Pliocene alluvial deposits outcropping at Grad, Northeastern Slovenia, contain bone fragments which very possibly belong to a mastodont. The bones are altered to apatite with outstanding abundance of As, Sr, Be, U, Y and Hg. Normalised REE abundance shows a consistent decrease of LREE to Eu, and then an increase of HREE, with almost equal normalised LaN and YbN values. Kratka vsebina Zgornjepliocenski re~ni sedimenti pri Gradu vsebujejo odlomke kosti, ki najverjetneje pripadajo mastodontu in so spremenjene v apatit. V kemi~ni sestavi mo~no izstopajo

Chemical composition of a Pliocene large mammal (mastodont ?) bone fragment from alluvial deposits at Grad, Northeastern Slovenia