The Laterosensory Canal System in Epigean and Subterranean Ituglanis (Siluriformes: Trichomycteridae), With Comments About Troglomorphism and the Phylogeny of the Genus

The laterosensory system is a mechanosensory modality involved in many aspects of fish biology and behavior. Laterosensory perception may be crucial for individual survival, especially in habitats where other sensory modalities are generally useless, such as the permanently aphotic subterranean environment. In the present study, we describe the laterosensory canal system of epigean and subterranean species of the genus Ituglanis (Siluriformes: Trichomycteridae). With seven independent colonizations of the subterranean environment in a limited geographical range coupled with a high diversity of epigean forms, the genus is an excellent model for the study of morphological specialization to hypogean life. The comparison between epigean and subterranean species reveals a trend toward reduction of the laterosensory canal system in the subterranean species, coupled with higher intraspecific variability and asymmetry. This trend is mirrored in other subterranean fishes and in species living in different confined spaces, like the interstitial environment. Therefore, we propose that the reduction of the laterosensory canal system should be regarded as a troglomorphic (= cave‐related) character for subterranean fishes. We also comment about the patterns of the laterosensory canal system in trichomycterids and use the diversity of this system among species of Ituglanis to infer phylogenetic relationships within the genus. J. Morphol. 278:4–28, 2017. ©© 2016 Wiley Periodicals,Inc.     

皮氏菊头蝠(Rhinolophus pearsoni)的栖息生态特征

皮氏菊头蝠(Rhinolophus pearsoni)是我国南方典型的洞栖食虫性蝙蝠,具有重要的生态意义。近年于湘西州及张家界市的25个溶洞中共记录到该蝠450只次,对其栖息生态特征(空间分布、姿势、体温、栖点温度和栖点安全性等)进行了较为系统的观测。结果表明:该蝠的栖点主要集中分布于离洞口440 m之内的洞段(占99.3%),栖点高度通常介于2—10 m之间(84%),主要采取双足倒挂的姿势栖息于洞顶壁或侧壁,但单足倒挂的栖息姿势也较为常见(36.2%)。体温介于10.7—25.2℃,体温总是稍高于栖点温度,但两者之间无显著性差异(P0.05),且两者呈线性正相关。约64%的栖点"安全性高",而"安全性低"和"安全性中"的栖点分别占17.6%和18.4%。减少对洞穴的人为干扰是保护该物种的有效途径。     

A general view of the lower Palaeolithic of Turkey

Turkey is one of the rich countries in terms of the Lower Palaeolithic period. The favourable climatic and environmental conditions and quality stone raw material resources in the Pleistocene period caused the country to be heavily occupied by the people of the Lower Palaeolithic. Turkey has biface and flake industries of the Lower Palaeolithic period. Biface industries are more common in open-air sites and are often linked to the Acheulean. Biface tools are only found in the deposits of Karain Cave. The eastern and south-eastern parts of Turkey are the densest regions in terms of biface industries. This density decreases towards the west. However, this general appearance may have resulted from the insufficient level of excavations and surveys of Palaeolithic archaeology throughout the country. In this article, we try to draw a general framework of the Lower Palaeolithic period in Turkey, based on the important Lower Palaeolithic settlements in the country.     

Review of the millipede genus Eutrichodesmus Silvestri, 1910, in China,with descriptions of new cavernicolous species (Diplopoda,Polydesmida, Haplodesmidae)

The Eutrichodesmus fauna of mainland China, by far the largest genus in the Indo-Australian family Haplodesmidae, is reviewed and shown to encompass 23 species (of a total of 45), all keyed. The following nine new species, all presumed troglobites, are described: Eutrichodesmus triangularis sp. n., from Sichuan, Eutrichodesmus lipsae sp. n., from Guangxi, Eutrichodesmus tenuis sp. n., Eutrichodesmus trontelji sp. n., Eutrichodesmus latellai sp. n., Eutrichodesmus obliteratus sp. n. and Eutrichodesmus troglobius sp. n., all from Guizhou, Eutrichodesmus sketi sp. n., from Hunan, and Eutrichodesmus apicalis sp. n., from Hubei.     

Geometric morphometrics throws light on evolution of the subterranean catfish Rhamdiopsis krugi (Teleostei: Siluriformes: Heptapteridae) in eastern Brazil

Rhamdiopsis krugi is a highly specialized troglobitic (exclusively subterranean) catfish from phreatic water bodies of caves located within two separated metasedimentary basins in the region of Chapada Diamantina, Bahia state, Brazil. In order to test the hypothesis of isolation with differentiation of the groups from the Una‐Utinga and Irecê metasedimentary basins, we compared five populations among themselves and with an epigean species of Rhamdiopsis. This was accomplished using geometric morphometrics, a powerful tool for detecting differences in body shape at population and species levels. All studied samples differed significantly from each other, the epigean sample being the most distinct and the Una Basin populations clustering together. Geological and hydrological barriers explain the differences among the subterranean populations. We discuss our results together with the autapomorphies found in R. krugi, which validate its monophyly. These results imply an old age for the R. krugi clade, more than 10 Myr; alternative hypotheses are also presented. We propose a two‐step vertical colonization model of the subterranean habitat through the hyporheic zone by an epigean ancestral, with a progressive acquisition of the autapomorphies characterizing R. krugi. For conservation purposes, the two differentiated sets of populations should be considered and referred to as R. krugi ‘Una morphotype’ and R. krugi ‘Irecê morphotype’. © 2014 The Linnean Society of London, Biological Journal of the Linnean Society, 2014, 114 , 136–151.     

Reduction in the metabolic levels due to phenotypic plasticity in the Pyrenean newt,Calotriton asper,during cave colonization

According to theories on cave adaptation, cave organisms are expected to develop a lower metabolic rate compared to surface organisms as an adaptation to food scarcity in the subterranean environments. To test this hypothesis, we compared the oxygen consumption rates of the surface and subterranean populations of a surface‐dwelling species, the newt Calotriton asper, occasionally found in caves. In this study, we designed a new experimental setup in which animals with free movement were monitored for several days in a respirometer. First, we measured the metabolic rates of individuals from the surface and subterranean populations, both maintained for eight years in captivity in a natural cave. We then tested individuals from these populations immediately after they were caught and one year later while being maintained in the cave. We found that the surface individuals that acclimated to the cave significantly reduced their oxygen consumption, whereas individuals from the subterranean population maintained in the cave under a light/dark cycle did not significantly modify their metabolic rates. Second, we compared these metabolic rates to those of an obligate subterranean salamander (Proteus anguinus), a surface aquatic Urodel (Ambystoma mexicanum), and a fish species (Gobio occitaniae) as references for surface organisms from different phyla. As predicted, we found differences between the subterranean and surface species, and the metabolic rates of surface and subterranean C. asper populations were between those of the obligate subterranean and surface species. These results suggest that the plasticity of the metabolism observed in surface C. asper was neither directly due to food availability in our experiments nor the light/dark conditions, but due to static temperatures. Moreover, we suggest that this adjustment of the metabolic level at a temperature close to the thermal optimum may further allow individual species to cope with the food limitations of the subterranean environment.     

织金洞钟乳石沉积物表面可培养细菌多样性和网络分析

【背景】洞穴环境中蕴含丰富而独特的细菌资源,对洞穴环境中细菌的分离培养有助于了解洞穴细菌多样性及细菌资源的挖掘和利用。【目的】利用不同培养基分离细菌,探究钟乳石表面可培养细菌的多样性及其种间互作关系。【方法】通过11种培养基对织金洞内钟乳石沉积物表面的细菌进行分离纯化,并利用16S rRNA基因序列分析初步确定分离菌株的分类地位。在R软件下,通过Bipartite包分析可培养细菌属间的相互作用。【结果】从钟乳石沉积物表面共分离出206株细菌,它们隶属于4门25属45种,香农(Shannon)指数为4.78,辛普森(Simpson)指数为0.95。变形菌门(Proteobacteria)和芽孢杆菌属(Bacillus)分别为样品中可培养细菌的优势门(47.09%)和优势属(29.61%)。无机寡营养培养基有助于洞穴钟乳石沉积物细菌的分离。属水平-采样点网络分析表明,可培养细菌分布具有非随机、显著的嵌套性。芽孢杆菌属(Bacillus)、德沃斯氏菌属(Devosia)、产碱杆菌属(Alcaligenes)、节杆菌属(Arthrobacter)和短杆菌属(Brevibacterium)在细菌群落中存在较多的有效合作值(Effective Partners)和亲密度(Closeness),被其他细菌所依赖程度(Species Strength)较高,是该群落中的重要组成类群。【结论】织金洞内钟乳石沉积物表面存在丰富的细菌资源,分析细菌类群在群落中的作用应结合细菌相对丰度和网络分析。     

Hunting,disturbance and roost persistence of bats in caves at Ankarana,northern Madagascar

Surveys and monitoring of 37 caves in and around the Ankarana Special Reserve, northern Madagascar, yielded evidence of hunting of bats and potential disturbance of bats by miners and tourists, and colony counts for several bat species of potential conservation concern. Colony size decreased by 95% and 14% for a colony of Hipposideros commersoni and a colony of Eidolon dupreanum, respectively, when recent evidence of hunting occurred at those colonies and those declines are probably attributable to hunting. Evidence of hunting occurred commonly at the roosts of those species and most commonly at the roosts of Rousettus madagascariensis. Hunting of pteropodids was associated with high vulnerability of roosts to hunters, little forest buffer between the cave and open savannah and the absence of tombs in the cave. Roost sites of the hunted species persisted for at least several years and this regularity may facilitate hunting. This work supports the ranking of E. dupreanum, R. madagascariensis and H. commersoni as species of conservation concern. Managers should consider the impact of tourist visits on bats and of increasing access to caves for tourism. Conservation efforts for the hunted species should also seek to protect vulnerable and unprotected cave roosts.     

贵州洞穴淡水、陆生贝类区系及新种记述

首次报道了贵州省安龙县、贵阳市、独山县、荔波县、安顺市、开阳县、息烽县、盘县、兴义市、大方县、普定县等39个洞穴内不同生境的淡水、陆生贝类,经鉴定得淡水、陆生螺类共计71种,分隶于15科,36属,其中淡水螺类3科4属5种;陆生螺类66种,12科32属;1新种,即荔波双边凹螺Chamalycaeus libonensis sp.nov.附有种类名录,栖息环境及地理分布,并对洞穴中的淡水、陆生贝类区系组成进行了讨论,对新种进行了详细的描述,与近似种进行了比较。     

盘县大洞古人类遗址的地层和古气候研究

贵州盘县大洞的堆积物,自上而下可以分为3层。大洞主体堆积物为角砾堆积,来源于洞顶灰岩的崩塌,另外有人类遗物以及洞外片流作用带入的泥砂。人类化石、旧石器和哺乳动物化石主要分布在第2层角砾堆积中。堆积物在洞厅各部位均有相应分布,属同一沉积序列。已知的早期人类活动时间大约从260ka．B．P．开始,到142ka．B．P．前后结束,对应于深海氧同位素的第6、7阶段。角砾层下段,发育一套遭强烈溶蚀和风化的堆积物,地球化学分析结果显示其湿热的沉积环境,时间大约在260—180ka B．P．期间,对应于深海氧同位素第7阶段;大洞堆积物在气候变化周期上与黄土、青藏高原冰期序列可以对比。