id	author	title	date	pages	extension	mime	words	sentence	flesch	summary	cache	txt
amq-246	Rozzi, Roberto; Palombo, Maria Rita; Barbieri, Maurizio	THE ARGALI (OVIS AMMON ANTIQUA) FROM THE MAGLIANA AREA (ROME)	2010	7	.pdf	application/pdf	4819	178	54	Since the analysis of trace elements confirms the presence of volcanic minerals, such as micas, pyrossen and leucite at various stages of alteration in analcime or clay minerals, the skull of Ovis ammon antiqua found at La Magliana is at least younger than the beginning of the volcanic activity in the study area, even though we cannot confirm whether these particles are related to the “Pozzo- lane grigie” or not. Accordingly, since: the sequence boundary between the PG3 and PG4 is an unconformity surface related to a lowstand phase during MIS 14 (MILLI, 1997); the de- posits of PG4 sequence widely outcrops at the top of the hills in the Fosso della Magliana area, while out- crops of PG5 sequence are scantily or not present and Portis considered the skull of Ovis ammon antiqua as found at La Magliana in levels whose description is consistent with the lacustrine-lagoonal deposits of the TST/HST of the PG4 sequence, we could hypothesize that the study specimen settled in a period covering the ending of MIS 14 and the beginning of MIS 13.	cache/amq-246.pdf	txt/amq-246.txt