THE LATE PLEISTOCENE APENNINE CHAMOIS FROM GROTTA MORA CAVORSO (SIMBRUINI MOUNTAINS, CENTRAL ITALY)

This paperdescribes a sub-entire, partially articulated skeleton of chamois found togetherwith other vertebrate remainsina silty lens withlimestone clastsbetween the 104 and 105 SSUU of Grotta Mora Cavorso(Latium, Italy). Thissilty lensis chronologically correlatable to a temperate oscillation of MI...

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Main Authors: LEONARDO SALARI, MARIO F. ROLFO, CARMELO PETRONIO
Format: Article
Language:English
Published: Università degli Studi di Milano 2014-11-01
Series:Rivista Italiana di Paleontologia e Stratigrafia
Online Access:https://riviste.unimi.it/index.php/RIPS/article/view/6081
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spelling doaj-d86bb7b8929e4c00b0cbcfe76676f44f2020-11-24T23:28:06ZengUniversità degli Studi di MilanoRivista Italiana di Paleontologia e Stratigrafia0035-68832039-49422014-11-01120310.13130/2039-4942/60815396THE LATE PLEISTOCENE APENNINE CHAMOIS FROM GROTTA MORA CAVORSO (SIMBRUINI MOUNTAINS, CENTRAL ITALY)LEONARDO SALARIMARIO F. ROLFOCARMELO PETRONIOThis paperdescribes a sub-entire, partially articulated skeleton of chamois found togetherwith other vertebrate remainsina silty lens withlimestone clastsbetween the 104 and 105 SSUU of Grotta Mora Cavorso(Latium, Italy). Thissilty lensis chronologically correlatable to a temperate oscillation of MIS 3.The skull and post-cranial remains from Grotta Mora Cavorso were compared with the fossil remains of chamois from numerous Late Pleistocene and older Holocene sites of Italy and of Pyrenees and Iberian Peninsula. Additional comparisons were made with large samples of extant chamois, Rupicapra pyrenaica ornata , R. pyrenaica pyrenaica and R. rupicapra rupicapra .Morphological and morphometric features of the skull and the horn-core, as well as other characters of the metacarpus suggest to refer the fossil remainsfrom Grotta Mora Cavorsoto Apennine chamois, R. pyrenaica ornata . This is the earliest ascertained recordin Central-Southern Italyofthe ornata -like chamois, a subspeciesso far knownwith certaintyonly in the Holocene, orpossibly in the Lateglacial.https://riviste.unimi.it/index.php/RIPS/article/view/6081
collection DOAJ
language English
format Article
sources DOAJ
author LEONARDO SALARI
MARIO F. ROLFO
CARMELO PETRONIO
spellingShingle LEONARDO SALARI
MARIO F. ROLFO
CARMELO PETRONIO
THE LATE PLEISTOCENE APENNINE CHAMOIS FROM GROTTA MORA CAVORSO (SIMBRUINI MOUNTAINS, CENTRAL ITALY)
Rivista Italiana di Paleontologia e Stratigrafia
author_facet LEONARDO SALARI
MARIO F. ROLFO
CARMELO PETRONIO
author_sort LEONARDO SALARI
title THE LATE PLEISTOCENE APENNINE CHAMOIS FROM GROTTA MORA CAVORSO (SIMBRUINI MOUNTAINS, CENTRAL ITALY)
title_short THE LATE PLEISTOCENE APENNINE CHAMOIS FROM GROTTA MORA CAVORSO (SIMBRUINI MOUNTAINS, CENTRAL ITALY)
title_full THE LATE PLEISTOCENE APENNINE CHAMOIS FROM GROTTA MORA CAVORSO (SIMBRUINI MOUNTAINS, CENTRAL ITALY)
title_fullStr THE LATE PLEISTOCENE APENNINE CHAMOIS FROM GROTTA MORA CAVORSO (SIMBRUINI MOUNTAINS, CENTRAL ITALY)
title_full_unstemmed THE LATE PLEISTOCENE APENNINE CHAMOIS FROM GROTTA MORA CAVORSO (SIMBRUINI MOUNTAINS, CENTRAL ITALY)
title_sort late pleistocene apennine chamois from grotta mora cavorso (simbruini mountains, central italy)
publisher Università degli Studi di Milano
series Rivista Italiana di Paleontologia e Stratigrafia
issn 0035-6883
2039-4942
publishDate 2014-11-01
description This paperdescribes a sub-entire, partially articulated skeleton of chamois found togetherwith other vertebrate remainsina silty lens withlimestone clastsbetween the 104 and 105 SSUU of Grotta Mora Cavorso(Latium, Italy). Thissilty lensis chronologically correlatable to a temperate oscillation of MIS 3.The skull and post-cranial remains from Grotta Mora Cavorso were compared with the fossil remains of chamois from numerous Late Pleistocene and older Holocene sites of Italy and of Pyrenees and Iberian Peninsula. Additional comparisons were made with large samples of extant chamois, Rupicapra pyrenaica ornata , R. pyrenaica pyrenaica and R. rupicapra rupicapra .Morphological and morphometric features of the skull and the horn-core, as well as other characters of the metacarpus suggest to refer the fossil remainsfrom Grotta Mora Cavorsoto Apennine chamois, R. pyrenaica ornata . This is the earliest ascertained recordin Central-Southern Italyofthe ornata -like chamois, a subspeciesso far knownwith certaintyonly in the Holocene, orpossibly in the Lateglacial.
url https://riviste.unimi.it/index.php/RIPS/article/view/6081
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