The Bentzen-Kaufmann Cave Site 48 SH 301

Abstract

A small cave in northeastern Wyoming yielded a number of bone fragments and artifacts representing an intermittent cultural deposition since the Early Period. A radiocarbon age of 6975 ± 275 years was obtained for one of the oldest components in the site.     

The cave bear’s hibernation: reconstructing the physiology and behaviour of an extinct animal

Abstract

When studying an extinct species such as the cave bear (Ursus spelaeus ROSENMÜLLER 1794), it is possible to apply a variety of molecular biology techniques such as the study of stable isotopes or mitochondrial DNA (mDNA) to infer patterns of behaviour or physiology that would otherwise remain concealed. Throughout Europe and along time, differences in the isotopic values (δ¹³C and δ¹⁵N) of cave bears arise from environmental differences and the Pleistocene climatic evolution. The climate determines the hibernation length, during which the cave bears undergo a particular physiology that can be related to an increase in δ¹⁵N during climate cooling. In order to verify whether hibernation affected the isotopic values, we compared cave bears in different ontogenetic stages. The results show that perinatal values reflect the values for mothers during hibernation, while juveniles show differences in maternal investment. A previous study in the literature based on complete mitochondrial DNA sequences of several individuals collected from closely situated caves showed that each cave housed, almost exclusively, a single lineage of haplotypes. This pattern suggests extreme fidelity to the birth site, or homing behaviour, and that cave bears formed stable maternal social groups, at least for the purpose of hibernation. Studies of this type offer unexpected data on the palaeobiology of this extinct animal.     

Evidence of homing following translocation of long‐tailed bats (Chalinolobus tuberculatus) at Grand Canyon Cave,New Zealand

Abstract

Homing behaviour in the New Zealand long‐tailed bat (Chalinolobus tuberculatus), a temperate insectivorous species, was investigated at Grand Canyon Cave, central North Island. A pilot study of nine adult male bats was conducted to determine whether use of the cave was regular enough for a homing study. Eight bats returned to the cave over the 3‐week monitoring period, six on the night following release. Nine additional bats carrying radio transmitters were then released at three sites (three at each site) c. 5, 10 and 20 km due east of the cave; sites estimated to be located within, on the border of, and outside the population's known familiar area respectively. All but one of these nine bats were subsequently detected at the cave. Results suggest that adult long‐tailed bats are able to return home following displacement both inside and outside their familiar area. Implications of these findings for translocations of bats and the possession of a potential long‐distance navigation system by this species are discussed.     

Extinction pattern of Alpine cave bears - new data and climatological interpretation

ABSTRACT

Cave bears have disappeared from the Alps from different altitudes at different times. The temporal progression of the HDEL (Height Dependent Extinction Line) – a compilation of the geologically most recent radiocarbon dates per altitude level – is not consistent with the general cooling of the temperatures from about 45 ka BP. The cave bear sites of the Northern Alps with the most recent radiocarbon ages are not situated in the lowlands but in caves in altitudes of 1,500 m to 1,700 m above sea level (a.s.l.).

Cave bears fed almost exclusively on herbs and leaves. It was assumed that with the general cooling in the OIS 3 since about 45 ka BP also the migration of the alpine elements into the lowlands took place. It could be recognized that the populations in the lower situated cave bear site became earlier extinct than the cave bear population in the higher altitudes.

With new radiocarbon dates, done at the Curt-Engelhorn-Center Archaeometry at the Reiss-Engelhorn-Museen in Mannheim (Germany), the HDEL can be determined much more precisely and the causes of gradual extinction are also better understood.     

Descriptions of the first semi-aphenopsian troglobiotic Patrobini and of a new anophthalmic cave-dwelling Trechini from central Sichuan,China (Coleoptera: Caraboidea)

Summary

The first known troglobiotic species belonging to the ground beetle tribe Patrobini is reported from a limestone cave called Lianhua Dong in Pengzhou, a suburb county-level city in northern Chengdu, Sichuan Province, China. Troglopatrobus zhouchaoi n. gen., n. sp., is an eyeless and large-sized patrobine beetle with extremely elongated body (esp. head and elytra) and appendages. Duvalioblemus (Shublemus) liyuani n. subgen., n. sp., a minute anophthalmic trechine species, is also discovered from the same cave. It is the first cave-dwelling species belonging to this genus already known as endogean from Sichuan and Yunnan provinces.     

Isotopic insights on cave bear palaeodiet

Abstract

More than 300 cave bear bones from all over Europe have carbon and nitrogen isotopic composition that match overwhelmingly a diet based on plants, except for samples from two caves in Romania, for which high nitrogen-15 amounts have been interpreted as reflecting an omnivorous diet. This paper aims at deciphering the various factors influencing the carbon and nitrogen isotopic composition of a potential omnivorous species like cave bear, those linked to trophic levels and variations among plants and those caused by physiological factors. The comparison of European cave bears with coeval Late Pleistocene large mammals with different diets clearly shows that all the cave bear populations, including those from Romania, present isotopic values overlapping with herbivores, not with carnivores. Therefore omnivory is very unlikely for cave bears. Consumption of plants with high δ¹⁵N values, such as graminoids, forbs and possibly fungi, could explain in part the observed isotopic pattern. In addition, the variations in δ¹⁵N values through ontogeny support the hypothesis of a different hibernation pattern for the Romanian cave bears with high δ¹⁵N values. Future investigations using new isotopic approaches, especially nitrogen isotopic composition of collagen amino acids, should contribute to decipher the paleoecology of these Romanian cave bears.     

Diet reconstruction in cave bears from craniodental morphology: past evidences,new results and future directions

ABSTRACT

The diet of the cave bear (Ursus spelaeus) is a controversial topic, as different paleobiological approaches (e.g. dental wear, isotopic biochemistry, skull morphometrics) result in different dietary inferences for the cave bear, ranging from carnivory to pure herbivory. Here, we review the main results obtained from these approaches, with special emphasis on those obtained from the morphometric analyses of the cave bear craniodental skeleton. Then, we compute a between-group Principal Components Analysis from a set of 3D-landmarks digitized on 103 mandibles of living bears and extinct cave bears and using a phylomorphospace approach. Moreover, we also reconstructed the evolutionary trajectory of the cave bear mandible from the hypothetical shape of its inferred ancestor. Our results indicate that the mandible of the cave bear possess specific traits indicative of a highly-herbivorous diet or, at least, more herbivorous than their closest living relative, the brown bear (Ursus arctos). Moreover, we also propose new directions for future research to obtain more detailed inferences on the potential food resources consumed by the cave bear being crucial to understand the ‘life and death’ of this vanished animal.     

Phenotypic plasticity in the greater mouse-eared bat in extremely different roost conditions

Bats use various roost types with a wide spectrum of ecological features. The greater mouse-eared bat Myotis myotis (Borkhausen, 1797), creates nurseries in attics and caves in Central Europe. The stable low temperature and high humidity cave microclimate contrasts that of attics, which may alter species adaptations and life strategies. We analysed population characteristics (composition, body condition, parasite load, and immune response) and genetic relatedness of two proximal M. myotis populations. Age, sexual and parasite species composition were similar between the cave and attic sites. However, a significantly higher parasite load and body condition was detected in the post-partum females and juveniles of the cave colony (n = 263 bats from the cave, 231 from the attic), with the cave colony females having a significantly stronger immune response (n = 2 caves and 2 attics, 20 females per site). There was no evidence for genetic divergence between cave and attic populations (n = 3 caves and 3 attics, 24 females per site), indicating that different population characteristics are not genetically based and that M. myotis is an example of a species with rather unique phenotypic plasticity.     

Un nuovo ascomicete entomogeno rinvenuto in grotta: Cordyceps riverae

Abstract

A new entomogenous Ascomycete found in cave: Cordyceps riverae.—A new species of entomogenous Cordyceps, belonging to Subgenus Racemella (Ces.) Sacc., found on an adult Lepidotteron in a cave near L'Aquila (Abruzzo, Italy) is described. The characters of this species, named Cordyceps riverae, are compared with those of other similar species of Cordyceps.     

Three new species of the aphaenopsian trechine genus Pilosaphaenops Deuve & Tian, 2008 from South China Karst (Coleoptera: Carabidae: Trechinae)

Summary

Three new trechine species of the genus Pilosaphaenops Deuve & Tian, 2008, P. qianzhii n. sp. from cave Lubian Dong in Pingtang County, southern Guizhou Province, P. mengzhenae n. sp. and P. weiguofui n. sp. from cave Xia Dong in Nandan County, and cave Shenlong Gong in Huanjiang County respectively, northern Guangxi Zhuang Autonomous Region, are described and illustrated. A key to all known species of this genus is also provided.

http://www.zoobank.org/urn:lsid:zoobank.org:pub:170C467F-5421-49AD-B1B1-091D8BD58B88     

From a molecules’ perspective – contributions of ancient DNA research to understanding cave bear biology

Abstract

Few members of the Pleistocene megafauna have been as extensively studied as cave bears. Multidisciplinary research into cave bears has provided insights into their morphology, ecology, and evolution. Genetic studies have profited from the availability of large numbers of well-preserved remains. As a result, ‘ancient DNA (aDNA)’ from cave bears has provided significant insights into cave bear ecology, phylogeography and even potential causes of their extinction. Here I review the contributions that genetic research has made to our understanding of cave bear biology and evaluate the potential that new, genomic tools provide to shed further light onto how these iconic representatives of the Pleistocene megafauna lived and died.     

贵州兴义喀斯特洞穴可培养放线菌多样性及抗菌活性初筛

【目的】进一步了解兴义喀斯特洞穴可培养放线菌资源及产活性代谢产物的能力。【方法】选取多种分离培养基,利用稀释直接涂布平板法对贵州黔西南兴义市多个喀斯特洞穴的土壤和岩石进行可培养放线菌资源分离;利用三种发酵培养基对相关放线菌进行生物产物初筛。【结果】根据16S rRNA基因序列的比对分析,将分离得到的251株放线菌分别归类到44个属,其中链霉菌属(Streptomyces)占分离菌株的比例为24.30%,小单孢菌属(Micromonospora)占比11.95%,红球菌属(Rhodococcus)占比9.16%,微杆菌属(Microbacterium)占比7.17%,诺卡氏菌属(Nocardia)占比6.37%,该五类放线菌为该地区可培养放线菌的优势菌群。对70株细菌进行活性次级代谢产物筛选,其中35株放线菌对指示菌具有抑制活性,且主要类群为链霉菌属和小单孢菌属。【结论】贵州兴义喀斯特洞穴中存在丰富多样的放线菌类群,且蕴藏大量具有产生活性次级代谢产物能力的菌株,为医药产业提供潜力菌株资源,极具进一步发掘和研究的价值。     

Palaeoecology of cave bears as evidenced by dental wear analysis: a review of methods and recent findings

Abstract

The study of dental wear was first used years ago to infer the palaeoecology of fossil mammals and in particular their diet. Results depend predominantly on the scale of the analysis used. Analyses of dental macrowear, mesowear or microwear do not provide the same type of dietary information, be it about the seasonal, annual or lifetime diet. This contribution focuses on emblematic species, cave bears (Ursidae), in particular Ursus spelaeus spelaeus. Methods used by previous researchers to infer their dietary preferences and thus their palaeoecology are reviewed and compared. This review is complemented by an analysis of several specimens of cave bears from the Goyet cave in Belgium, using dental microwear texture analysis (DMTA), a methodology widely applied for reconstructing palaeodiets. Three main conclusions are drawn here: (1) DMTA is the method that provides the most precise palaeobiological inferences; (2) during the pre-dormancy period, cave bears show dietary flexibility; (3) dental wear alone might be not sufficient to provide a complete reconstruction of the cave bear palaeodiet.     

Was the European cave bear an occasional scavenger?

Rabal‐Garcés, R., Cuenca‐Bescós, G., Canudo, J.I. & de Torres, T. 2011: Was the European cave bear an occasional scavenger? Lethaia, Vol. 45, pp. 96–108. The cave bear Ursus spelaeus fossils remains are quite abundant in the Late Pleistocene site of Coro Tracito (Huesca, Spain). The site constitutes the highest mountain record of cave bears in the Iberian Peninsula. Being a monospecific locality, it permits the study of the biology and dietary habits of this species. The study of the limb bones established first, the mortality pattern of this population of Ursus spelaeus and, second, the alteration pattern due to carnivore tooth‐marks. Some authors have performed similar analyses in the same kind of skeletal elements in other cave bear localities all over Europe and, therefore it has been possible to compare our results with those from other sites. The tooth‐marks found in the bones of cave bears, especially in monospecific sites, have been attributed to a scavenging behaviour. In agreement with the authors, our analysis presented here supports the hypothesis of scavenging behaviour for cave bears. □Behaviour, Late Pleistocene, Spain, taphonomy, tooth‐marks, Ursus spelaeus.     

Late Pleistocene leopards as a bone accumulator: taphonomic results from S’Espasa cave and other Iberian key sites

Abstract

The Pleistocene faunal accumulations documented in caves have commonly been attributed to the activity of humans or carnivores. According to the palaeontological and archaeological literature, cave hyena (Crocuta spelaea) was the main known bone accumulator in karstic environments. However, in recent times, the role of leopards as bone accumulators has been revealed, and recent research has identified this behaviour in the Iberian Pleistocene. Moreover, there are other caves where leopard could have been claimed as an accumulator such as S’Espasa. In this work we present its taphonomic study. This cave was compared with the actualistic studies of leopards. Besides, the site of S’Espasa was compared with the other leopard dens in the Iberian Peninsula. These sites present faunal assemblages composed mainly by leopard (Panthera pardus) and Iberian wild goat (Capra pyrenaica), the bones of this ungulate present a similar pattern of bone modification by carnivores, skeletal survival rate, and bone breakage. These features indicate that goats could have been accumulated by leopards. With the data from this work and the previous ones, we try to establish a pattern that will help in the future to identify other accumulations created by this big cat.     

Carnivore involvement in bone assemblages based on taphonomic and zooarchaeological analyses of Cova del Coll Verdaguer site (Barcelona,Iberian Peninsula)

Abstract

Carnivores are the main biological agents identified in the Upper Pleistocene assemblage of Cova del Coll Verdaguer (NE Iberian Peninsula). At the site, ungulate bones were primarily accumulated and modified by hyenas, as shown by partly digested bones, coprolites and the pattern of damage on bones. However, other small- to medium-sized carnivores seemed to be involved in the accumulation, owing primarily to the presence of their bones and coprolites. Finally, other carnivores, including the brown bear, used the cave to hibernate and for birthing cubs. The combination of zooarchaeological and taphonomic studies, together with previous coprogenic analyses, at the site indicates that it is only by using these combined approaches that it is possible to identify the majority of the agents involved in an accumulation.     

A three-dimensional analysis of tooth-root morphology in living bears and implications for feeding behaviour in the extinct cave bear

ABSTRACT

The morphology of both crowns and tooth-roots reflects dietary specialisation in mammalian carnivores. In this article, we analyse the tooth-root morphology of maxillary teeth from CT scans of living bears (Ursus arctos, Ursus americanus, Ursus maritimus, Ursus thibetanus, Melursus ursinus, Helarctos malayanus, Tremarctos ornatus and Ailuropoda melanoleuca) in order to make inferences about the diet and feeding behaviour of the extinct cave bear (Ursus spelaeus sensu lato). Specifically, we investigate two major mitochondrial clades of extinct cave bears recognized by previous authors: Ursus ingressus and Ursus spelaeus (U. spelaeus spelaeus, U. spelaeus ladinicus, U. spelaeus eremus). Our results indicate a close association between tooth-root surface area and feeding behaviour in all living bear species. Tooth-root surface area values of cave bears suggest that they relied more on vegetative matter than living brown bears (Ursus arctos) but subtle differences between these species/subspecies could also indicate different feeding strategies among the members of cave bear complex.     

Craniodental remains ofPapio angusticeps from the haasgat cave site,South Africa

Haasgat is a fossil-bearing cave site that has yielded 83 craniodental fossils of early Papio.All of the Haasgat cave baboon fossil collection may be identified as Papio angusticeps.The Haasgat fossils of P. angusticepsextend the previously known size range of the species as identified at other sites. The concordance of this and other fauna with that of Kromdraai suggest that Haasgat probably dates to the terminal Pliocene. We hypothesize that the Haasgat baboons and associated fauna were accumulated by versatile predators operating in a cave in a montane forest environment with savannah or open woodland nearby.     

What happens to dead birds left in a cave and its vicinity for a quarter of a century? A taphonomic experiment

Abstract

This paper describes a bird carcass-monitoring experiment carried out in a limestone cave and its immediate vicinity in southern Poland for almost a quarter of a century. Some specimens deposited outside the cave were preserved almost intact, others were only a little weathered. Soft tissues and remnants of feathers were preserved in some of the samples inside the cave. Stages of bone modifications that can occur in a cave have been distinguished and illustrated for the first time. Also, bird bones from owl pellets have been used in a carcass-monitoring experiment for the first time. Bone modifications in the form of wrinkling, bending and/or collapsing of the bone surface were recorded only on the bones of birds that decomposed inside the cave, and not on bones that had been isolated from owl pellets prior to their deposition in the cave. Therefore, it is postulated that avian – and possibly also small mammal – bones that have been defleshed, either by people or animals, have a greater chance to survive and fossilize than bones deposited as complete carcasses in a cave. This agrees with the generally accepted notion that larger assemblages of small vertebrates in caves are usually the result of predator accumulation.