TY - JOUR N2 - Trace fossils Phymatoderma melvillensis isp. nov., Thalassinoides isp., ?Nereites isp. and Planolites isp. are reported from the glacio−marine sediments of the Cape Melville Formation (Lower Miocene) of King George Island, West Antarctica. Their occurrence and strong bioturbation of sediments point to an offshore or deeper (outer shelf or upper slope) en− vironment. Deep marine crab Antarctidromia inflata Förster, 1985, has been found in Thalassinoides isp. The tracemaker (?crustacean) of Phymatodermamelvillensis re−reworked pelletal sediments probably during times of food deficiency. L1 - http://journals.pan.pl/Content/108314/PDF-MASTER/article-p83.pdf L2 - http://journals.pan.pl/Content/108314 PY - 2010 IS - No 1 EP - 99 KW - Antarctica KW - King George Island KW - Cape Melville Formation KW - ichnofossils KW - Miocene KW - glacio−marine strata A1 - Uchman, Alfred A1 - Gaździcki, Andrzej PB - Polish Academy of Sciences PB - Committee on Polar Research DA - 2010 T1 - Phymatoderma melvillensis isp. nov. and other trace fossils from the Cape Melville Formation (Lower Miocene) of King George Island, Antarctica SP - 83 UR - http://journals.pan.pl/dlibra/publication/edition/108314 T2 - Polish Polar Research ER -