The taxonomic status and biochronological implications of new finds ofOreopithecus from Baccinello (Tuscany, Italy)
Identifieur interne : 001007 ( Istex/Curation ); précédent : 001006; suivant : 001008The taxonomic status and biochronological implications of new finds ofOreopithecus from Baccinello (Tuscany, Italy)
Auteurs : L. Rook [Italie] ; T. Harrison [États-Unis] ; B. Engesser [Suisse]Source :
- Journal of Human Evolution [ 0047-2484 ] ; 1996.
Descripteurs français
- Wicri :
- topic : Toscane.
English descriptors
- KwdEn :
- Academic press, Anterior root, Anterior view, Anthracomys, Anthracomys majori, Baccinello, Baccinello area, Bamboli, Bambolii, Biostratigraphically equivalent sites, Bovidae, Bovidae indet, Broad cingular shelf, Buccal, Buccal side, Casteani, Cheek teeth, Cingulum, Clayey silts, Crocina, Dentine, Dentine exposure, Direct comparisons, Distal margin, Distally, Distobuccal margin, Enamel, Enamel surface, Engesser, Entoconid, Etruria, Etruscus, Eumaiochoerus etruscus, Evolutionary change, Fauna, Faunal, Faunal horizons, Fossil, Freshwater molluscs, Geol, Gracillimus, Great trasubbie outcrop, Grosseto, High level, Hypoconid, Hypoconulid, Indet, Ital, Large area, Large sample, Largest specimen, Late miocene, Lateral, Lorenz, Lorenzi, Main cusps, Majori, Malar, Malar fragment, Mammal, Mammalia, Mandible, Mandibular, Mandibular corpus, Maremma, Maremma region, Maremmia, Maremmia lorenzi, Mesial, Mesial margin, Metaconid, Midline, Miocene, Molariform, Monte bamboli, More molariform, Morphological change, Naturhistorisches museum, Occlusal, Occlusal surface, Oreopithecus, Oreopithecus bambolii, Oreopithecus material, Oreopithecus specimens, Oreopithecus table, Other localities, Other oreopithecus specimens, Other specimens, Outcrop, Paludotona, Partial mandible, Patella, Pavolona, Podere, Protocone, Protoconid, Right mandibular fragment, Right side, Rook, Several species, Silt, Single depositional basin, Small sample, Southern tuscany, Stratigraphic, Stratigraphic section, Taxonomic, Time interval, Trasubbie, Trasubbie river valley, Tuscany, Type material, Tyrrhenotragus, Tyrrhenotragus gracillimus, dentition, fauna, late Miocene, mandible, stratigraphy.
- Teeft :
- Academic press, Anterior root, Anterior view, Anthracomys, Anthracomys majori, Baccinello, Baccinello area, Bamboli, Bambolii, Biostratigraphically equivalent sites, Bovidae, Bovidae indet, Broad cingular shelf, Buccal, Buccal side, Casteani, Cheek teeth, Cingulum, Clayey silts, Crocina, Dentine, Dentine exposure, Direct comparisons, Distal margin, Distally, Distobuccal margin, Enamel, Enamel surface, Engesser, Entoconid, Etruria, Etruscus, Eumaiochoerus etruscus, Evolutionary change, Fauna, Faunal, Faunal horizons, Fossil, Freshwater molluscs, Geol, Gracillimus, Great trasubbie outcrop, Grosseto, High level, Hypoconid, Hypoconulid, Indet, Ital, Large area, Large sample, Largest specimen, Late miocene, Lateral, Lorenz, Lorenzi, Main cusps, Majori, Malar, Malar fragment, Mammal, Mammalia, Mandible, Mandibular, Mandibular corpus, Maremma, Maremma region, Maremmia, Maremmia lorenzi, Mesial, Mesial margin, Metaconid, Midline, Miocene, Molariform, Monte bamboli, More molariform, Morphological change, Naturhistorisches museum, Occlusal, Occlusal surface, Oreopithecus, Oreopithecus bambolii, Oreopithecus material, Oreopithecus specimens, Oreopithecus table, Other localities, Other oreopithecus specimens, Other specimens, Outcrop, Paludotona, Partial mandible, Patella, Pavolona, Podere, Protocone, Protoconid, Right mandibular fragment, Right side, Rook, Several species, Silt, Single depositional basin, Small sample, Southern tuscany, Stratigraphic, Stratigraphic section, Taxonomic, Time interval, Trasubbie, Trasubbie river valley, Tuscany, Type material, Tyrrhenotragus, Tyrrhenotragus gracillimus.
Abstract
Abstract: Several species of mammals endemic to the late Miocene faunas of the Maremma region of Tuscany in Italy are known to have undergone a significant degree of morphological change during the time interval between the deposition of V-1 and V-2 horizons at Baccinello. This raises the interesting question of whether or notOreopithecus, which occurs in association with both V-1 and V-2 faunas, exhibits corresponding morphological change or taxonomic differentiation through time. Detailed comparisons of theOreopithecussample from Baccinello V-1 (and from the biostratigraphically equivalent sites of Ribolla, Casteani and Montemassi) with the type material ofO. bamboliifrom the site of Monte Bamboli, tentatively correlated with Baccinello V-2, indicate that there are no morphological or metrical differences by which to distinguish them. The recovery of a small sample ofOreopithecusspecimens from the Trasubbie River valley near Baccinello, derived from horizons stratigraphically above those yielding a V-1 fauna, allows, for the first time, direct comparisons of material from different strata within a single depositional basin. The material consists of a newly discovered partial mandible (IGF 4883V) from the F1 horizon, and four isolated teeth, a malar fragment, and a patella from the V-2 horizon. IGF 4883V is very similar toOreopithecusspecimens from Baccinello V-1, although it differs in having a more molariform P3and relatively larger cheek teeth. However, given the extent of variation inOreopithecus, and the fact that the mandible almost certainly belonged to a male individual, these minor differences do not seem to be significant, and are best interpreted as being due to intraspecific variation. This conclusion is further supported by comparisons with Baccinello V-2 specimens, which appear to be indistinguishable from the large sample of specimens from Baccinello V-1. Although the sample ofOreopithecusspecimens from horizons located above V-1 remains small, there is sufficient material to conclude that there is no evidence of morphological change or taxonomic differentiation inOreopithecusduring the time interval of about 2Ma between Baccinello V-1 and V-2.
Url:
DOI: 10.1006/jhev.1996.0002
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<term>Stratigraphic section</term>
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<term>Time interval</term>
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<term>Type material</term>
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<term>Bamboli</term>
<term>Bambolii</term>
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<term>Bovidae indet</term>
<term>Broad cingular shelf</term>
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<term>Clayey silts</term>
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<term>Distally</term>
<term>Distobuccal margin</term>
<term>Enamel</term>
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<term>Miocene</term>
<term>Molariform</term>
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<term>Silt</term>
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<term>Time interval</term>
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<front><div type="abstract" xml:lang="en">Abstract: Several species of mammals endemic to the late Miocene faunas of the Maremma region of Tuscany in Italy are known to have undergone a significant degree of morphological change during the time interval between the deposition of V-1 and V-2 horizons at Baccinello. This raises the interesting question of whether or notOreopithecus, which occurs in association with both V-1 and V-2 faunas, exhibits corresponding morphological change or taxonomic differentiation through time. Detailed comparisons of theOreopithecussample from Baccinello V-1 (and from the biostratigraphically equivalent sites of Ribolla, Casteani and Montemassi) with the type material ofO. bamboliifrom the site of Monte Bamboli, tentatively correlated with Baccinello V-2, indicate that there are no morphological or metrical differences by which to distinguish them. The recovery of a small sample ofOreopithecusspecimens from the Trasubbie River valley near Baccinello, derived from horizons stratigraphically above those yielding a V-1 fauna, allows, for the first time, direct comparisons of material from different strata within a single depositional basin. The material consists of a newly discovered partial mandible (IGF 4883V) from the F1 horizon, and four isolated teeth, a malar fragment, and a patella from the V-2 horizon. IGF 4883V is very similar toOreopithecusspecimens from Baccinello V-1, although it differs in having a more molariform P3and relatively larger cheek teeth. However, given the extent of variation inOreopithecus, and the fact that the mandible almost certainly belonged to a male individual, these minor differences do not seem to be significant, and are best interpreted as being due to intraspecific variation. This conclusion is further supported by comparisons with Baccinello V-2 specimens, which appear to be indistinguishable from the large sample of specimens from Baccinello V-1. Although the sample ofOreopithecusspecimens from horizons located above V-1 remains small, there is sufficient material to conclude that there is no evidence of morphological change or taxonomic differentiation inOreopithecusduring the time interval of about 2Ma between Baccinello V-1 and V-2.</div>
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