奥地利 Kohfidisch 中新世晚期(Turolian,MN11)的豪猪 Hystrix parvae (Kretzoi, 1951)

IF 1.4 4区 地球科学 Q3 BIODIVERSITY CONSERVATION Palaeobiodiversity and Palaeoenvironments Pub Date : 2024-08-03 DOI:10.1007/s12549-024-00616-3
Gudrun Daxner-Höck, Viola Winkler, Daniela C. Kalthoff
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引用次数: 0

摘要

本文对Hystrix parvae进行了升级,它是迄今为止Hystrix s.str.中最小和最古老的灭绝物种。新数据来自奥地利 Kohfidisch 地区异常丰富的新化石收藏,其中包括 100 多件化石。门牙的珐琅质显微结构分析以及部分头骨、上下颌骨和牙齿的 X 射线显微计算机图像(microCT)为详细描述提供了支持。牙齿的形态和大小显示出很大的差异,这取决于个体发育阶段、牙齿位置和磨损阶段。落牙 D4/d4 和恒牙下颌 p4-m3 被鉴定为低冠或 brachydont。m1/2的平均畸形指数为69%。恒牙上P4-M3为短冠至中冠。M1/2 的平均齿列不齐指数为 114%。科菲迪什的喀斯特洞穴和裂隙系统提供了理想的育儿环境,不同发育阶段的大量乳齿就是证明。该动物群的年龄为晚中新世(下图瓦卢统,MN11),距今约 860 万年。
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The porcupine Hystrix parvae (Kretzoi, 1951) from the Late Miocene (Turolian, MN11) of Kohfidisch in Austria

This paper provides an upgrade of Hystrix parvae, which so far is the smallest and oldest extinct species of Hystrix s. str. The new data derive from the exceptionally rich new fossil collection of the locality Kohfidisch in Austria, that comprises more than 100 fossils. The detailed descriptions are supported by enamel microstructure analysis of incisors, and x-ray microcomputed images (microCT) of the partial skull, upper and lower jaws and teeth. The tooth pattern and sizes show wide ranges, depending on the ontogenetic stage, tooth position and stage of wear. The deciduous D4/d4 and the permanent lower p4-m3 are identified as low crowned or brachydont. The mean hypsodonty index of m1/2 is 69%. The permanent upper P4-M3 are brachydont to mesodont. The mean hypsodonty index of M1/2 is 114%. The karstic cave and fissure system of Kohfidisch provided an ideal nursery environment as evidenced by numerous deciduous teeth in different ontogenetic stages. The age of the fauna is Late Miocene (lower Turolian, MN11), around 8.6 million years.

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来源期刊
Palaeobiodiversity and Palaeoenvironments
Palaeobiodiversity and Palaeoenvironments BIODIVERSITY CONSERVATIONPALEONTOLOGY -PALEONTOLOGY
CiteScore
3.90
自引率
14.30%
发文量
33
期刊介绍: Palaeobiodiversity and Palaeoenvironments is a peer-reviewed international journal for the publication of high-quality multidisciplinary studies in the fields of palaeobiodiversity, palaeoenvironments and palaeobiogeography. Key criteria for the acceptance of manuscripts are a global scope or implications of problems on a global scale significant not only for a single discipline, a focus on the diversity of fossil organisms and the causes and processes of change in Earth’s history. The topics covered include: Systematic studies of all fossil animal / plant groups with a special focus on palaeoenvironmental investigations, palaeoecosystems and climate changes in Earth’s history, environment-organism interaction, comparison of modern and ancient sedimentary environments, palaeoecology and palaeobiogeography.
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