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Monte Tuttavista

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Geographical location of Monte Tuttavista and age span of Sardolagus obscurus n. gen. n. sp. Legend of lithology: (1) Quaternary deposits; (2) Pliocene within-plate basalts; (3) Permian to early Eocene volcano-sedimentary rocks; (4) late Variscan magmatic complex; (5) Variscan metamorphic basement (modified from Carmignani et al., 2016).

Geographical location of Monte Tuttavista and age span of Sardolagus obscu... Available to Purchase

Published: 01 May 2018
Figure 1 Geographical location of Monte Tuttavista and age span of Sardolagus obscurus n. gen. n. sp. Legend of lithology: ( 1 ) Quaternary deposits; ( 2 ) Pliocene within-plate basalts; ( 3 ) Permian to early Eocene volcano-sedimentary rocks; ( 4 ) late Variscan magmatic complex; ( 5
Journal Article

Systematics and paleobiogeography of Sardolagus obscurus n. gen. n. sp. (Leporidae, Lagomorpha) from the early Pleistocene of Sardinia Available to Purchase

Chiara Angelone, Stanislav Čermák, Blanca Moncunill-Solé, Josep Quintana, Caterinella Tuveri, Marisa Arca, Tassos Kotsakis
Published: 01 May 2018
Journal of Paleontology (2018) 92 (3): 506–522.
DOI: https://doi.org/10.1017/jpa.2017.144
...Figure 1 Geographical location of Monte Tuttavista and age span of Sardolagus obscurus n. gen. n. sp. Legend of lithology: ( 1 ) Quaternary deposits; ( 2 ) Pliocene within-plate basalts; ( 3 ) Permian to early Eocene volcano-sedimentary rocks; ( 4 ) late Variscan magmatic complex; ( 5...
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Reverse fault (white mark) of the positive flower structure related to the Cedrino Fault, leading to superposition of massive Kimmeridgian limestones on stratified, less competent, dragfolded Tithonian-Berriasian limestones, at Punta Fraigada (northern slope of Monte Tuttavista, near Orosei).

Reverse fault (white mark) of the positive flower structure related to the ... Available to Purchase

Published: 01 January 2008
F ig . 13. – Reverse fault (white mark) of the positive flower structure related to the Cedrino Fault, leading to superposition of massive Kimmeridgian limestones on stratified, less competent, dragfolded Tithonian-Berriasian limestones, at Punta Fraigada (northern slope of Monte Tuttavista
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 Figure8—Scatterplots illustrating the high discriminant potential of the measurements of PH/AA (1, 2, 3, 4) and TH/AA (5, 6) of P4. Different species that may coexist in the same fossil site (due to sympatry as P. oeningensis and P. tobieni or to taphonomic mixing as P. sardus and P. figaro) appear well separated (8.1, 8.2, 8.5, 8.6), as well as populations of the same species (P. sardus, 8.3); these measurements can give additional support to specific differences (Italian Mio–Pliocene species, 8.4) and allow hints about phylogenetic relationships. FI:P. figaro, Monte Tuttavista X-4, Sardinia, Italy (Angelone, 2005); IT:P. italicus, Torre di Picchio, central Italy (Angelone, in press); MIcc:P. michauxi, Ciabòt Cagna, northwestern Italy (Angelone, 2007); MIse:P. michauxi, Sète, southern France (data courtesy N. López Martínez); MIar:P. michauxi, El Arquillo, central Spain (data courtesy Prof. N. López Martínez); OE:P. oeningensis, Escobosa; SA:P. sardus, Monte Tuttavista VI-6, Sardinia, Italy (Angelone et al., 2008); sa:P. sardus, Monte Tuttavista IV-5, Sardinia, Italy (Angelone et al., 2008); SO:P. sorbinii, Brisighella 25, central Italy (Angelone, 2007); SV:P. savagei, Arondelli, north-western Italy (Berzi, 1967); TO:P. tobieni, Escobosa

Figure 8 —Scatterplots illustrating the high discriminant potential of the... Available to Purchase

Published: 01 January 2009
, El Arquillo, central Spain (data courtesy Prof. N. López Martínez); OE: P. oeningensis , Escobosa; SA: P. sardus , Monte Tuttavista VI-6, Sardinia, Italy ( Angelone et al., 2008 ); sa: P. sardus , Monte Tuttavista IV-5, Sardinia, Italy ( Angelone et al., 2008 ); SO: P. sorbinii
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Geologic sections (A-A’ and B-B’; traces in fig. 1) across the Monte Tuttavista (west of Orosei), showing the positive flower structure related to the Cedrino Fault. 1– Recent continental deposits. 2– Limestones and sandy limestones with nummulites and alveolinas (Cuisian). 3– Monte Bardia Limestone: massive and stratified white limestones (Berriasian-Kimmeridgian). 4– S’Adde Limestone: stratified ligh-brown micritic limestones with ammonites (Callovian to Oxfordian). 5– Dorgali Dolostone: brown dolostones (Bathonian). 6– Rhyolites, red sandstones and quartz conglomerates (Permian). 7– Granite (Upper Palaeozoic). 8– Quartz phyllites (Palaeozoic).

Geologic sections (A-A’ and B-B’; traces in fig. 1 ) across the Monte Tutta... Available to Purchase

Published: 01 January 2008
F ig . 12. – Geologic sections (A-A’ and B-B’; traces in fig. 1 ) across the Monte Tuttavista (west of Orosei), showing the positive flower structure related to the Cedrino Fault. 1– Recent continental deposits. 2– Limestones and sandy limestones with nummulites and alveolinas (Cuisian). 3
Journal Article

New Characters for Species Discrimination within the Genus Prolagus (Ochotonidae, Lagomorpha, Mammalia) Available to Purchase

Chiara Angelone, Carmen Sesé
Published: 01 January 2009
Journal of Paleontology (2009) 83 (1): 80–88.
DOI: https://doi.org/10.1666/07-067R2.1
... , El Arquillo, central Spain (data courtesy Prof. N. López Martínez); OE: P. oeningensis , Escobosa; SA: P. sardus , Monte Tuttavista VI-6, Sardinia, Italy ( Angelone et al., 2008 ); sa: P. sardus , Monte Tuttavista IV-5, Sardinia, Italy ( Angelone et al., 2008 ); SO: P. sorbinii...
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Age, depositional environment and stratigraphic value of the Cuccuru ’e Flores Conglomerate: insight into the Palaeogene to Early Miocene geodynamic evolution of Sardinia Available to Purchase

Iginio Dieni, Francesco Massari, Jacques Médus
Published: 01 January 2008
Bulletin de la Société Géologique de France (2008) 179 (1): 51–72.
DOI: https://doi.org/10.2113/gssgfbull.179.1.51
...F ig . 13. – Reverse fault (white mark) of the positive flower structure related to the Cedrino Fault, leading to superposition of massive Kimmeridgian limestones on stratified, less competent, dragfolded Tithonian-Berriasian limestones, at Punta Fraigada (northern slope of Monte Tuttavista...
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View PDF for article title, Age, depositional environment and stratigraphic value of the Cuccuru ’e Flores Conglomerate: insight into the Palaeogene to Early Miocene geodynamic evolution of Sardinia
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A new species of Myotragus Bate, 1909 (Artiodactyla, Caprinae) from the Early Pliocene of Mallorca (Balearic Islands, western Mediterranean) Available to Purchase

PERE BOVER, JOSEP QUINTANA, JOSEP ANTONI ALCOVER
Published: 23 April 2010
Geological Magazine (2010) 147 (6): 871–885.
DOI: https://doi.org/10.1017/S0016756810000336
... obtained at Capo Figari (northeastern Sardinia). Remains of this caprine have been recovered from other deposits on the island, such as Capo Mannu (western central Sardinia: Van der Made, 1999 ), Monte Tuttavista (eastern Sardinia: Abbazzi et al . 2004 ) and from an unknown locality at Campidano...
View PDF for article title, A new species of Myotragus Bate, 1909 (Artiodactyla, Caprinae) from the Early Pliocene of Mallorca (Balearic Islands, western Mediterranean)
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Discussion on «The Sardinia-Corsica microplate and its role in the Northern Apennine Geodynamics: new insights from the Tertiary intraplate strike-slip tectonics of Sardinia» by G. Oggiano, A. Funedda, L. Carmignani & S. Pasci (2009) Available to Purchase

Iginio Dieni, Francesco Massari
Published: 01 February 2011
Italian Journal of Geosciences (2011) 130 (1): 136–138.
DOI: https://doi.org/10.3301/IJG.2010.28
... alii , 1998 ), indicating the middle Ilerdianlate Cuisian interval. This clearly demonstrates that the assemblage results from processes of reworking and mixing. C habrier (1970) later attributed a Cuisian-early Lutetian age to the rudites in the area NW of Monte Corallinu (Dorgali), without however...
View PDF for article title, Discussion on «The Sardinia-Corsica microplate and its role in the Northern Apennine Geodynamics: new insights from the Tertiary intraplate strike-slip tectonics of Sardinia» by G. Oggiano, A. Funedda, L. Carmignani & S. Pasci (2009)
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Reply to: Discussion on «The Sardinia-Corsica microplate and its role in the Northern Apennine Geodynamics: new insights from the Tertiary intraplate strike-slip tectonics of Sardinia» by Igino Dieni & Francesco Massari Available to Purchase

Giacomo Oggiano, Antonio Funedda, Luigi Carmignani, Sandro Pasci
Published: 01 February 2011
Italian Journal of Geosciences (2011) 130 (1): 139–143.
DOI: https://doi.org/10.3301/IJG.2010.26
... vulcano-sedimentaria della Sardegna centro-settentrionale . Boll. Soc. Geol. It. , 121 , 3 – 10 . Chabrier G. ( 1967 ) - Le Synclinal Crétacé de Gorropu (Sardaigne) . C.R. Soc. Géol. France , 7 , 321 – 322 . Chabrier G. ( 1969 ) - Sur la stratigraphie et la tectonique des monts...
View PDF for article title, Reply to: Discussion on «The Sardinia-Corsica microplate and its role in the Northern Apennine Geodynamics: new insights from the Tertiary intraplate strike-slip tectonics of Sardinia» by Igino Dieni & Francesco Massari
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The Sardinia-Corsica microplate and its role in the Northern Apennine Geodynamics: new insights from the Tertiary intraplate strike-slip tectonics of Sardinia Available to Purchase

Giacomo Oggiano, Antonio Funedda, Luigi Carmignani, Sandro Pasci
Published: 01 June 2009
Italian Journal of Geosciences (2009) 128 (2): 527–539.
DOI: https://doi.org/10.3301/IJG.2009.128.2.527
..., south of the Monte Albo, where the Variscan basement and the Mesozoic to Eocene cover are once again involved in Tertiary strike-slip faults. The structural framework includes: dextral E-W trending transcurrent faults with related thrusts and folds (e.g. Monte Tuttavista, Punta Cusidore) ( C habrier...
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First occurrence of the ‘hunting hyena’ Chasmaporthetes in the Late Miocene fossil bearing localities of Toros Menalla, Chad (Africa) Available to Purchase

Louis de Bonis, Stephane Peigne, Andossa Likius, Hassane T. Makaye, Michel Brunet, Patrick Vignaud
Published: 01 July 2007
Bulletin de la Société Géologique de France (2007) 178 (4): 317–326.
DOI: https://doi.org/10.2113/gssgfbull.178.4.317
.... ( 2004 ). “ Chasmaporthetes melei n.sp., an endemic hyaenid (Carnivora, Mammalia) from the Monte Tuttavista fissure fillings (late Pliocene to early Pleistocene, Sardinia, Italy) .” Riv. Ital. Pal. Strat ., 110 ( 3 ), 707 – 714 . Schaub S. ( 1941 ). “ Ein neues hyaenidengenus von der...
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View PDF for article title, First occurrence of the ‘hunting hyena’ Chasmaporthetes in the Late Miocene fossil bearing localities of Toros Menalla, Chad (Africa)
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The Upper Valdarno Plio-Pleistocene vertebrate record: an historical overview, with notes on palaeobiology and stratigraphic significance of some important taxa Available to Purchase

Rook Lorenzo, Croitor Roman, Delfino Massimo, Marco P. Ferretti, Gallai Gianni, Pavia Marco
Published: 01 February 2013
Italian Journal of Geosciences (2013) 132 (1): 104–125.
DOI: https://doi.org/10.3301/IJG.2012.16
... of the Upper Valdarno Basin . Ital. J. Geosci. , 132 , 98 - 103 . doi: 10.3301/IJG.2012.27 . Rook L. Ferretti M.P. Arca M. Tuveri C. ( 2004 ) - Chasmaporthetes melei n.sp., an endemic Hyaenid (Carnivora, Mammalia) from the Monte Tuttavista fissure fillings (Late Pliocene to Early...
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View PDF for article title, The Upper Valdarno Plio-Pleistocene vertebrate record: an historical overview, with notes on palaeobiology and stratigraphic significance of some important taxa
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