Manuel Rodríguez-Almagro , Asier Gómez-Olivencia , Mónica Villalba de Alvarado , Juan Luis Arsuaga , Nohemi Sala
{"title":"对 El Polvorín 洞穴 Sima I(伊比利亚半岛北部)出土的洞熊(Ursus cf. deningeri 和 U. spelaeus)的岩石学研究","authors":"Manuel Rodríguez-Almagro , Asier Gómez-Olivencia , Mónica Villalba de Alvarado , Juan Luis Arsuaga , Nohemi Sala","doi":"10.1016/j.qsa.2024.100171","DOIUrl":null,"url":null,"abstract":"<div><p>Cave bears used caves for hibernation and giving birth. Caves maintain stable conditions of temperature and humidity, which facilitates the preservation of fossil accumulations. Causes of mortality in caves are related to starvation during hibernation, which affects mainly juveniles and old adults, predation and accidents, affecting bears of all ages. The Iberian Peninsula is located in one of the extremes of the geographical range of this species and has yielded an abundant cave bear fossil record, particularly in karstic systems in the northern fringe. The origin of the accumulation of bear fossil sites in Iberia has been investigated mostly based on selected paleobiological variables (sex-ratio and age-at-death profiles) and qualitative taphonomic assessment. The objective of this paper is to delve into the origin of a bear accumulation with a large proportion of hyaena remains, the Sima I of El Polvorín cave (Biscay, Northern Iberian fringe, Spain). For that end a combination of quantitative paleobiological (age-at-death and sex) and taphonomic (bone fracture patterns and surface modifications) data is used. This analysis has ruled out humans and hyenas as the origin of the accumulation but, due to the limited number of fossil remains available it is not possible to ascertain whether the bear accumulation was the result of a natural trap within the cave, natural mortality during hibernation, or a combination of both causes. This study underscores the necessity of integrated methodological approaches and the potential of old paleontological collections to provide new important paleobiological and taphonomic information under these approaches.</p></div>","PeriodicalId":34142,"journal":{"name":"Quaternary Science Advances","volume":null,"pages":null},"PeriodicalIF":2.9000,"publicationDate":"2024-01-01","publicationTypes":"Journal Article","fieldsOfStudy":null,"isOpenAccess":false,"openAccessPdf":"https://www.sciencedirect.com/science/article/pii/S2666033424000091/pdfft?md5=6ebee61e0da3e37d43bd1a17dcd527f8&pid=1-s2.0-S2666033424000091-main.pdf","citationCount":"0","resultStr":"{\"title\":\"Taphonomic study of the cave bears (Ursus cf. deningeri and U. spelaeus) from the Sima I of the El Polvorín cave (Northern Iberian Peninsula)\",\"authors\":\"Manuel Rodríguez-Almagro , Asier Gómez-Olivencia , Mónica Villalba de Alvarado , Juan Luis Arsuaga , Nohemi Sala\",\"doi\":\"10.1016/j.qsa.2024.100171\",\"DOIUrl\":null,\"url\":null,\"abstract\":\"<div><p>Cave bears used caves for hibernation and giving birth. Caves maintain stable conditions of temperature and humidity, which facilitates the preservation of fossil accumulations. Causes of mortality in caves are related to starvation during hibernation, which affects mainly juveniles and old adults, predation and accidents, affecting bears of all ages. The Iberian Peninsula is located in one of the extremes of the geographical range of this species and has yielded an abundant cave bear fossil record, particularly in karstic systems in the northern fringe. The origin of the accumulation of bear fossil sites in Iberia has been investigated mostly based on selected paleobiological variables (sex-ratio and age-at-death profiles) and qualitative taphonomic assessment. The objective of this paper is to delve into the origin of a bear accumulation with a large proportion of hyaena remains, the Sima I of El Polvorín cave (Biscay, Northern Iberian fringe, Spain). For that end a combination of quantitative paleobiological (age-at-death and sex) and taphonomic (bone fracture patterns and surface modifications) data is used. This analysis has ruled out humans and hyenas as the origin of the accumulation but, due to the limited number of fossil remains available it is not possible to ascertain whether the bear accumulation was the result of a natural trap within the cave, natural mortality during hibernation, or a combination of both causes. 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引用次数: 0
摘要
洞穴熊利用洞穴冬眠和分娩。洞穴保持着稳定的温度和湿度条件,这有利于保存化石的积累。洞穴中熊的死亡原因与冬眠期间的饥饿(主要影响幼熊和老熊)、捕食和意外事故有关,所有年龄段的熊都会受到影响。伊比利亚半岛位于该物种地理分布范围的一个极端,因此有丰富的洞穴熊化石记录,尤其是在北部边缘的喀斯特系统中。对伊比利亚熊化石地点积累的起源进行的调查主要基于选定的古生物学变量(性别比例和死亡年龄剖面)和定性的岩石学评估。本文的目的是深入研究一个含有大量鬣狗遗骸的熊化石群的起源,即 El Polvorín 洞穴(西班牙伊比利亚北部边缘比斯开省)的 Sima I。为此,研究人员综合利用了定量古生物学(死亡年龄和性别)和岩石学(骨骼断裂模式和表面修饰)数据。这项分析排除了人类和鬣狗是熊堆积的起源,但由于可获得的化石遗骸数量有限,因此无法确定熊堆积是洞穴内的自然陷阱、冬眠期间的自然死亡,还是这两种原因共同作用的结果。这项研究强调了采用综合方法的必要性,以及古老的古生物藏品在这些方法下提供新的重要古生物学和岩石学信息的潜力。
Taphonomic study of the cave bears (Ursus cf. deningeri and U. spelaeus) from the Sima I of the El Polvorín cave (Northern Iberian Peninsula)
Cave bears used caves for hibernation and giving birth. Caves maintain stable conditions of temperature and humidity, which facilitates the preservation of fossil accumulations. Causes of mortality in caves are related to starvation during hibernation, which affects mainly juveniles and old adults, predation and accidents, affecting bears of all ages. The Iberian Peninsula is located in one of the extremes of the geographical range of this species and has yielded an abundant cave bear fossil record, particularly in karstic systems in the northern fringe. The origin of the accumulation of bear fossil sites in Iberia has been investigated mostly based on selected paleobiological variables (sex-ratio and age-at-death profiles) and qualitative taphonomic assessment. The objective of this paper is to delve into the origin of a bear accumulation with a large proportion of hyaena remains, the Sima I of El Polvorín cave (Biscay, Northern Iberian fringe, Spain). For that end a combination of quantitative paleobiological (age-at-death and sex) and taphonomic (bone fracture patterns and surface modifications) data is used. This analysis has ruled out humans and hyenas as the origin of the accumulation but, due to the limited number of fossil remains available it is not possible to ascertain whether the bear accumulation was the result of a natural trap within the cave, natural mortality during hibernation, or a combination of both causes. This study underscores the necessity of integrated methodological approaches and the potential of old paleontological collections to provide new important paleobiological and taphonomic information under these approaches.