A reappraisal of the lost suids from the Late Miocene of Gravitelli (Sicily, Italy) and paleobiogeographical implications

IF 1.7 3区 地球科学 Q2 PALEONTOLOGY Palaeoworld Pub Date : 2024-04-01 DOI:10.1016/j.palwor.2023.02.001
Alessio Iannucci
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Abstract

The long-lost mammal fauna from Gravitelli (Messina, Sicily, Italy) represents one of the most important records for investigating faunal dynamics during the Late Miocene of the Mediterranean, although it is unfortunately only known from descriptions carried out in the early 1900s, as the original collection was lost during the Messina Earthquake of 1908. Gravitelli suids have been referred to Propotamochoerus sp. after the redescription of the casts of two specimens that survived to the present day. However, there is further material that has not been considered, which makes that of Gravitelli one of the most abundant samples of Late Miocene suids from Italy, with a minimum number of four individuals represented. A reappraisal of all Gravitelli suids allows to ascribe them to Propotamochoerus provincialis (Suinae, Dicoryphochoerini), following a comparison with related Late Miocene to Pliocene species from Eurasia. Moreover, the re-examination of the geological setting of the locality reveals that the mammal fauna of Gravitelli occurred well below the pre-evaporitic deposits of the Tripoli Formation, whose base is dated in Sicily at ∼7 Ma. Therefore, Gravitelli fauna either dates to the late Tortonian or, at most, to the earliest pre-evaporitic Messinian, corresponding to MN 11 or MN 12 in terms of mammal biochronology. This implies that the occurrence of P. provincialis at Gravitelli is the earliest in Italy and that emerged land masses connected Sicily with the European mainland earlier than 7 Ma. Available dates support a diachronous dispersal of Propotamochoerus in western Europe during the Turolian, being first known from the Balkans ∼8.3 Ma, then from Gravitelli prior to 7 Ma, and then from the Iberian Peninsula since ∼6.2 Ma. A similar pattern is known for Mesopithecus (Cercopithecidae). Although often discussed in light of its potential significance for Afro-Eurasian dispersals, only a fraction of the mammal fauna of Gravitelli has been reconsidered systematically. Notwithstanding the necessity of such dedicated studies, the faunal elements identified so far have an almost entirely European character and no species is shared with Cessaniti (Calabria), despite the two faunas have often been considered part of a paleobioprovince documenting a connection between southern Italy and northern Africa. At Gravitelli, the only species of African origin is the endemic hippo Hexaprotodon? siculus, but the extensive fossil record of insular hippopotamids testifies to their ability to colonize islands even in the absence of land bridges. Gravitelli hippos are nonetheless noteworthy, as the revised age of the site implies that they represent the earliest hippopotamids known outside Africa.

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对Gravitelli(意大利西西里岛)中新世晚期丢失的suids的重新评估及其古生物地理学意义
格拉维泰利(意大利西西里岛墨西拿)失落已久的哺乳动物动物群是研究地中海晚中新世动物动态的最重要记录之一,但遗憾的是,由于原始采集物在 1908 年墨西拿地震中遗失,人们只能通过 20 世纪早期的描述来了解该动物群。Gravitelli 麂在对两只存活至今的标本进行重新描述后,被归类为 Propotamochoerus sp.。然而,还有更多的材料未被考虑,这使得格拉维特利的样本成为意大利晚中新世麂类最丰富的样本之一,至少有四个个体具有代表性。通过与欧亚大陆晚中新世至上新世的相关物种进行比较,对所有 Gravitelli 麂的重新评估使我们可以将其归类为省氏麂(Propotamochoerus provincialis,麂科,Dicoryphochoerini)。此外,对该地区地质环境的重新研究表明,格拉维泰利的哺乳动物群发生在的黎波里地层的前蒸发沉积层之下,而西西里岛的地层基底年代为 7 Ma。因此,格拉维泰利动物群要么可以追溯到托尔托尼晚期,要么最多可以追溯到最早的梅西尼前蒸发沉积,从哺乳动物生物年代学的角度来看,相当于MN 11或MN 12。这意味着在格拉维泰利出现的P.provincialis是意大利最早的,而且早在7Ma之前就出现了连接西西里岛和欧洲大陆的陆块。现有的数据支持Propotamochoerus在图罗利安时期在西欧的非同步扩散,最早出现在巴尔干半岛,时间为8.3 Ma∼,然后在7 Ma之前出现在Gravitelli,然后从6.2 Ma∼开始出现在伊比利亚半岛。类似的模式也出现在Mesopithecus (Cercopithecidae)身上。尽管人们经常讨论格拉维特利哺乳动物群对非洲-欧亚大陆扩散的潜在意义,但只有一小部分哺乳动物群得到了系统的研究。尽管有必要进行此类专门研究,但迄今为止发现的动物群几乎完全具有欧洲特征,没有一个物种与塞萨尼提(卡拉布里亚)共享,尽管这两个动物群经常被认为是古生物区的一部分,记录了意大利南部与非洲北部之间的联系。在格拉维泰利,唯一源自非洲的物种是当地特有的河马 Hexaprotodon? siculus,但海岛河马的大量化石记录证明,即使在没有陆地桥梁的情况下,它们也有能力在岛屿上定居。尽管如此,格拉维特利河马还是值得注意的,因为该遗址的修正年龄意味着它们代表了非洲以外已知最早的河马。
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来源期刊
Palaeoworld
Palaeoworld PALEONTOLOGY-
CiteScore
4.00
自引率
5.90%
发文量
95
期刊介绍: Palaeoworld is a peer-reviewed quarterly journal dedicated to the study of past life and its environment. We encourage submission of original manuscripts on all aspects of palaeontology and stratigraphy, comparisons of regional and global data in time and space, and results generated by interdisciplinary investigations in related fields. Some issues will be devoted entirely to a special theme whereas others will be composed of contributed articles. Palaeoworld is dedicated to serving a broad spectrum of geoscientists and palaeobiologists as well as serving as a resource for students in fields as diverse as palaeobiology, evolutionary biology, taxonomy and phylogeny, geobiology, historical geology, and palaeoenvironment. Palaeoworld publishes original articles in the following areas: •Phylogeny and taxonomic studies of all fossil groups •Biostratigraphy, chemostratigraphy, chronostratigraphy •Palaeoecology, palaeoenvironment and global changes throughout Earth history •Tempo and mode of biological evolution •Biological events in Earth history (e.g., extinctions, radiations) •Ecosystem evolution •Geobiology and molecular palaeobiology •Palaeontological and stratigraphic methods •Interdisciplinary studies focusing on fossils and strata
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