Alba David M, Montoya Plini, Pina Marta, Rook Lorenzo, Abella Juan, Morales Jorge, Delson Eric
Institut Català de Paleontologia Miquel Crusafont, Universitat Autònoma de Barcelona, Edifici ICTA-ICP, Carrer de les Columnes s/n, Campus de la UAB, 08193 Cerdanyola del Vallès, Barcelona, Spain.
Àrea de Paleontologia, Departament de Geologia, Universitat de València, c/ Doctor Moliner 50, 46100 Burjassot, València, Spain.
J Hum Evol. 2015 Nov;88:1-14. doi: 10.1016/j.jhevol.2015.08.003. Epub 2015 Sep 11.
We report dental remains of the extinct colobine monkey Mesopithecus from the Turolian (MN13, Late Miocene, ca. 6.23 Ma) locality of Venta del Moro (Valencia, Spain). They include most of the deciduous dentition and the unerupted germs of the first molars of a single infantile individual, as well as two lower left lateral incisors from two additional individuals. On the basis of morphometric comparisons, mainly based on the M1s, these remains are attributed to the Late Miocene species Mesopithecus pentelicus. They represent a significant addition to the knowledge of the deciduous dentition of this taxon, much less well-known than the permanent dentition. Although this genus was widely distributed from the Late Miocene through the Pliocene across Europe, southwestern Asia, Pakistan, and China, until now its occurence in the Late Miocene of the Iberian Peninsula had not been documented conclusively. Hence, the reported remains considerably enlarge southwestwards the known geographic distribution of Mesopithecus. The presence of this genus at Venta del Moro must be understood within the framework of the significant faunal turnover that took place in European faunas during the latest Turolian (the second Messinian mammalian dispersal), which is further documented at this locality by the occurrence of other eastern immigrants. At the same time, the presence of M. pentelicus at this site agrees well with previous paleoenvironmental and sedimentological evidence, indicating a lacustrine depositional environment with strong hydrologic seasonality.
我们报告了来自西班牙巴伦西亚市文塔德尔莫罗的图洛阶(MN13,晚中新世,约623万年前)的已灭绝疣猴中猴的牙齿化石。这些化石包括一个幼年个体的大部分乳牙列以及第一恒磨牙的未萌出牙胚,还有来自另外两个个体的两颗左下侧切牙。基于形态测量比较,主要是基于第一恒磨牙,这些化石被归为晚中新世物种五棱中猴。它们为该分类群乳牙列的知识增添了重要内容,乳牙列远不如恒牙列为人所知。尽管该属从中新世晚期到上新世在欧洲、亚洲西南部、巴基斯坦和中国广泛分布,但到目前为止,其在伊比利亚半岛晚中新世的出现尚未得到确凿记录。因此,所报告的化石极大地向西南方向扩展了中猴已知的地理分布范围。在文塔德尔莫罗发现该属物种必须放在图洛阶晚期(第二次墨西拿哺乳动物扩散)欧洲动物群发生重大更替的背景下来理解,该地点其他东部移民的出现进一步证明了这一点。同时,该地点五棱中猴的存在与先前的古环境和沉积学证据相符,表明这里是一个水文季节性很强的湖泊沉积环境。