1 Pol ish Geo log i cal In sti tute -Na tional Re search In sti tute, Rakowiecka 4, 00-975 Warszawa, Po land Brañski, P., Mikulski, S.Z., 2016. Rare earth el e ments dis tri bu tion in fine-grained de pos its from the up per most Tri as sic and Lower Ju ras sic of the Pol ish Ba sin: prov e nance and weath er ing in the source area. Geo log i cal Quar terly, 60 (2): 441-450, doi: 10.7306/gq.1288Nine teen sam ples of up per most Tri as sic and Lower Ju ras sic claystones and mudstones, which were formed in the epicontinental Pol ish Ba sin, were ana lysed by in duc tively cou pled plasma mass spec trom e try (ICP-MS) for rare earth el ements (REE) and other se lected trace el e ments (Sc, Y, Th, Zr and U). The re sults in di cate that the source of most of the claystones and mudstones stud ied were sed i men tary rocks of the up per con ti nen tal crust of old cratonic ar eas, where the protolith had a mainly fel sic char ac ter. How ever, in the lat est Tri as sic a char ac ter is tic layer formed, im ply ing sig nif i cant in put from mafic vol ca nic protolith. It was also found that mod er ately in tense chem i cal weath er ing usu ally fa voured in creased concen tra tion of the rare earths. Ex tremely strong hy dro ly sis, re lated to ep i sodes of very hot and hu mid cli mate (green house events), caused con spic u ous im pov er ish ment in REE in re sid ual clays. Weath er ing and re cy cling pro cesses mod i fied the com po si tion of REE to some ex tent, but gen er ally did not oblit er ate the orig i nal char ac ter is tics of the protolith. In some samples, en rich ment in rare earth el e ments was ob served, caused by ad mix tures of ac ces sory min er als (be ing a main car rier of REE) and/or in creased sort ing dur ing re cy cling. Key words: rare earth el e ments, prov e nance, palaeo-weath er ing, up per most Tri as sic and Lower Ju ras sic, Pol ish Ba sin.