Fauna,environment and human presence during MIS5 in the North of Spain: The new site of Valdavara 3

Valdavara 3 is a new early late Pleistocene paleontological and archeological cave site in northwestern Iberia. Over 1400 fossils have been collected, representing about 40 species. The fauna is of interglacial aspect and is in accordance with the OSL dates from the fossiliferous layer, which indicate an age of 103–113 ka. The great taxonomical diversity indicates a varied landscape. A small collection of lithic artifacts was found associated with the fossils, demostrating presence of humans and suggesting short non-residential visits to the cave. The fossiliferous site was predominantly formed by natural processes. Many fossil localities have short or biased faunal lists, but the fossil fauna recovered from Valdavara 3 is remarkably diverse and may reflect the fauna which once lived there.     

Hickmania Troglodytes, the Tasmanian Cave Spider, and its Potential Role in Cave Management

Cave faunas – which often contain a high representation of spiders – are subject to increasing pressure from the effects of epigean habitat degradation and recreational caving activities. Hickmania troglodytes is a prominent member of the Tasmanian cave fauna, a spider of phylogenetic, zoogeographic and ecological importance, but about which little has previously been known. Long-term monitoring has revealed many unusual life-cycle characteristics in this species, most of which occur over long periods of time and are dependent upon environmental stability. The species presents a potentially useful tool in the management and monitoring of cave fauna and karst, as it is large, conspicuous, numerous, ubiquitous, sedentary, functionally significant and potentially sensitive to various sources of disturbance. H. troglodytes may provide a visible and obvious measure of disturbance in and around cave entrances, and may also prove useful in detecting broader scale impacts affecting the entire cave. Many promising developments are being made in terms of cave management in Tasmania, but other issues are less well addressed and still need to be resolved. With further research, the use of indicator or sentinel species may prove to be well suited to the less complex and often sparsely populated subterranean environment, and may play an important role within larger management strategies for cave fauna and karst.     

Subterranean phylogeography of freshwater crayfishes shows extensive gene flow and surprisingly large population sizes

Subterranean animals are currently viewed as highly imperiled, precariously avoiding extinction in an extreme environment of darkness. This assumption is based on a hypothesis that the reduction in visual systems and morphology common in cave faunas reflects a genetic inability to adapt and persist coupled with the perception of a habitat that is limited, disconnected, and fragile. Accordingly, 95% of cave fauna in the United States are presumed endangered due to surface environmental degradation and limited geographic distributions. Our study explores the subterranean phylogeography of stygobitic crayfishes in the southeastern United States, a global hotspot of groundwater biodiversity, using extensive geographic sampling and molecular data. Despite their endangered status, our results show that subterranean crayfish species have attained moderate to high levels of genetic diversity over their evolutionary histories with large population sizes and extensive gene flow among karst systems. We then compare the subterranean population histories to those of common surface stream-dwelling crayfishes. Our results show recent drastic declines in genetic variability in the surface crayfish and suggest that these species also warrant conservation attention.     

陕西蓝田地区第四纪哺乳动物群的划分

<正> 陕西蓝田地区的新生代地层保存得非常完好,各个时代的地层,几乎都有其代表,并发现了丰富的哺乳动物化石。在第四纪地层中,特别具有意义的是公王岭及陈家窝分别发现了蓝田人头盖骨及下颌骨,一些地区还发现了旧石器,更进一步证实这一地区在第四     

How might sea level change affect arthropod biodiversity in anchialine caves: a comparison of Remipedia and Atyidae taxa (Arthropoda: Altocrustacea)

Sea level change influences biodiversity of endemic cave fauna to varying degrees. In anchialine systems, a marine layer flows under less saline layers, each with differing associated fauna. We assess the role of present and historic (last glacial maximum – 18,000 years ago) distance from the ocean in determining species richness and phylogenetic diversity patterns for two groups of anchialine crustaceans: the marine-restricted Remipedia and a subset of groundwater-inhabiting atyid shrimp with greater tolerance for salinity variation. We calculated species richness and phylogenetic diversity per cave based on records of remipede and atyid diversity at 137 locations in the Yucatán Peninsula, Caribbean, Australia, and the Canary Islands. After calculating the distance of each cave’s surface opening from the past and present shoreline, we evaluated how species richness and phylogenetic diversity change with distance from the present and historic ocean. Remipede species richness and phylogenetic diversity declined rapidly with distance from the ocean. Ninety-five percent of the remipedes surveyed were located within 7 km of the present ocean and 18 km of the historic ocean. Atyid species richness and phylogenetic diversity declined more slowly with distance from the ocean than that of remipedes. Atyid shrimp were also distributed over a broader range: 95 % were located within 100 km of the present ocean and 240 km of the historic ocean. Our findings indicate that coastal geomorphology and salinity tolerance influence a clade’s distribution with respect to its distance from the ocean. We also report a possible latent response to sea level change.     

Sampling adequacy in an extreme environment: species richness patterns in Slovenian caves

Caves harbor a rich fauna unique to subterranean environments. Although extensive records of cave animals are available, only a small fraction of known caves in any region have been biologically assessed. We investigated the impact of incomplete sampling using one of the richest, best documented cave faunas in the world – that of the Dinaric karst of Slovenia. We utilized time snapshots (1940, 1970, and 2000) of the caves and cave fauna to analyze stability of hotspots, spatial pattern, and relationship between number of species and number of caves. Using data aggregated into 100km² hexagons, the location of hotspots, black–white joins, Moran's I, and spatial autocorrelation all remained constant, at least from 1970 on. The linear regression coefficient of the relationship between number of caves and number of species declined with time. Most hexagons had been sampled, but there was no indication that any hexagon had been sampled intensively enough for the accumulation curve of number of caves versus number of species within a hexagon to reach an asymptote. This appeared to be the result of a highly skewed distribution of species richness among caves. Number and position of hotspots can be predicted from information on these few high diversity caves.     

Regional species richness in an obligate subterranean dwelling fauna – epikarst copepods

Aim  The diversity of the obligate cave-dwelling fauna has proved difficult to measure because of the highly localized distributions of most species. We investigated: (1) the local and regional diversity patterns of a major component of the obligate cave-dwelling fauna living in the epikarst zone, the karst layer closest to the surface; (2) variations in local and regional patterns of species richness; and (3) sampling sufficiency at multiple scales.
Location  Caves in the Dinaric Mountains of Slovenia.
Methods  We sampled continuously the abundance of 37 species of copepods dislodged from the epikarst from 35 ceiling drips in six caves for a period of one year. Copepods were collected in a specially designed net that allowed continuous collection.
Results  Based on species accumulation curves and Chao estimates of total diversity, we determined that 3–4 months of continuous sampling were sufficient to find 90% of the species in a drip, that five drips were sufficient to find 90% of the species in a cave, and that five caves were sufficient to find 90% of the species in a region.
Main conclusions  The epikarst copepod fauna is a significant part of the aquatic cave fauna, contributing about 20% at the regional level. Because of the scale of variation, much of which occurs within a cave, and because of the availability of continuous sampling devices, the epikarst component of subterranean diversity seems to be more thoroughly and accurately measured than do other components.     

Kotumsar Cave biodiversity: a review of cavernicoles and their troglobiotic traits

The evolutionary adaptations of the organisms which inhabit the unusual and fragile ecosystems within caves are of inherent interest to both biologists and laymen. Cave organisms generally develop a high degree of physiological and behavioural adaptation for survival in the subterranean environment. The Kotumsar Cave is biologically the best known cave in India and has attracted interest from researchers from all over the world. This paper assesses the ecological community and overall habitat of the cave. This is based on long-term field observations and the review of the extensive literature on Kotumsar. For each species, features indicative of evolutionary adaptation to the cave environment are noted and conclusions drawn regarding the status of the species as a cavernicole. Several species of this cave are yet to get a proper study for correct taxonomic position although they have apparent troglomorphic dispositions. Several species which are highly endemic to this cave are probably in verge of its extinction. A serious measure to conserve the whole biodiversity has been suggested.     

北京凤凰山化石地点发掘简报

北京凤凰山地点位于周口店北京猿人遗址以北8km处, 是一处含哺乳动物化石与灰烬的洞穴-裂隙堆积。该地点包括两个化石层,上层为洞外的冲积物, 由棕红色黏土组成, 靠下部发现有零星的、破碎的化石, 可鉴定出似鸡骨山狐(Vulpes cf.chikushanensis)和羚羊(Antelopinae)两种类型; 下层含有灰烬层, 出土了较为丰富的哺乳动物化石, 可鉴定的哺乳动物化石包括鬣狗(Hyaenidae)、三门马(Equus sameniensis)、犀(Rhinocerotidae)、李氏野猪(Sus lydekkeri)、肿骨大角鹿(Megaloceros pachyosteus)、葛氏斑鹿(Cervus(Sika)grayi)、水牛(Bubalus sp.), 共7种。动物群与周口店第一地点和南京人化石地点的动物群相似, 指示该地点化石层的时代可能为中更新世。部分骨骼表面痕迹与灰烬层的发现显示该地点可能不排除有古人类活动痕迹的存在。     

The Pleistocene deer hunter of Sardinia

The Pleistocene mammalian fauna of Sardinia isendemic and consists of only a few taxa, indicating island conditions at the time.A sharp faunal break in the Middle Pleistocene separates an older fauna with Nesogoral from a younger one (Middle/Upper Pleistocene) which contains mainly deer (Megaceros cazioti), and ochotonid (Prolagus sardus), a small canid (Cynotherium sardous), and Tyrrhenicola.Commonly paleoecological conditions on islands have led to the development of faunas with dwarfed species, showing a low gear locomotion due to lack of large carnivores. In this aspect the younger Pleistocene fauna of Sardinia is different. A deer with the proportion of mainland species and a small canid were found. This is suggestive of the presence of a large predator. Indeed, together with this fauna a human temporal bone, showing some distinctive characters, was found in Grotta di Corbeddu, Oliena, Sardinia.These findings gave rise to further excavations in the same cave. A paleolithic settlement was discovered and two types of bone artefact could be distinguished. ¹⁴C dating revealed an age of 13590±140 yrs. B.P.These results suggest the development of an endemichuman culture, adapted to the restricted island environment and to the monotonous prey of deer and ochotonids, different from any known culture of that age.     

与南京汤山直立人伴生的偶蹄类及其古环境浅析

在汤山葫芦洞大洞发现的偶蹄类化石共有 4个科、 5个属种 ,其中化石毛冠鹿为首次在华东地区发现。除德氏水牛相似种以外 ,其它属种与周口店第 1地点的标本相比具有个体较大(如李氏野猪、葛氏斑鹿和肿骨鹿 )或形态较进步 (如李氏野猪、似德氏水牛 )。这些动物所反映的古环境为植被丰富 ,并以阔叶乔木和灌木为主 ,间有局部开阔草地。当时的年平均气温与现在相似 ,但冬季偏冷。     

Cave Fauna of Bermuda

Sea-level pools are found in most of Bermuda's known caves. Although the terrestrial fauna of the caves is sparse, a rich aquatic fauna inhabits the pools. While many of the marine cave animals are more or less regular immigrants from open littoral habitats, a number of new species have been discovered, including blind and probably subterranean ones. Zoogeographical connections exist between Bermuda's cave fauna and those of the West Indies and the Mediterranean.     

吉林安图人化石

<正> 1963年末,安图县石灰场工人在石门山采石中发现了一批哺乳动物化石。吉林省博物馆,延边朝鲜族自治州博物馆闻讯后,曾于1964年初先后派人前往现场调查。从化石的种类和堆积的残存现状判断,这是一处晚更新世洞穴堆积。同年五月,吉林省地质局区测大队、东北地理研究所和吉林省博物馆等单位联合组织了一个发掘小组,对残留的洞穴堆积进行了清理。从中获得了一枚古人类牙齿化石。     

Cultivable microscopic fungi from an underground chemosynthesis-based ecosystem: a preliminary study

Movile Cave, a unique groundwater ecosystem in southern Romania, was discovered in 1986. This chemoautotrophic cave contains an abundant and diverse fauna with terrestrial and aquatic invertebrate communities, including 33 endemic species. Since its discovery, studies have focused mainly on cave chemoautotrophic bacteria, while the microfungal community has been largely neglected. In this study, we determined the microfungal species living on various substrates in Movile Cave and compared this spectrum with the mycobiota detected outside the cave (outside air-borne and soil-borne microfungi). To investigate all of the niches, we collected samples for two consecutive years from the dry part of the cave (cave air and sediment, corroded limestone walls, isopod feces, and isopod and spider cadavers) and from the post-siphon part of the cave, i.e., Airbell II (sediment and floating microbial mat). A total of 123 microfungal species were identified from among several hundred isolates. Of these, 96 species were only detected in the cave environment and not outside of the cave, while 90 species were from the dry part of the cave and 28 were from Airbell II. The most diverse genera were Penicillium (at least 18 species) and Aspergillus (14 species), followed by Cladosporium (9 species). Surprisingly, high CFU counts of air-borne microfungi were found inside the cave; they were even higher than outside the cave during the first year of investigation.     

Molar microwear and dietary reconstructions of fossil cercopithecoidea from the Plio-Pleistocene deposits of South Africa

The South African Plio-Pleistocene cave deposits have yielded a diverse cercopithecoid fauna. In this study, the possible dietary proclivities of these extinct species are examined using details of molar microwear. Although sample sizes are often small, wear patterns suggest possible temporal changes in the diets of Parapapio jonesi from Makapansgat to Sterkfontein, of Papio robinsoni from Sterkfontein to Swartkrans, and Cercopithecoides williamsi from Makapansgat to Sterkfontein to Swartkrans. However, there does not appear to have been a significant change in the dietary habits of Parapapio broomi over time. The microwear patterns of the two temporally successive congeners, Theropithecus darti and T. oswaldi show no significant differences from one another. The sympatric congeners, Parapapio broomi and Pp. jonesi, have microwear signatures that differ significantly at Makapansgat (Members 3 and 4) but not at Sterkfontein (Member 4). Finally, the microwear analyses suggest that the extinct cercopithecoid species did not necessarily have diets similar to those of their closest living relatives.     

Evidence for reproductive isolation between cave bear populations

The European cave bear (Ursus spelaeus), which became extinct around 15,000 years ago, had several morphologically different forms. Most conspicuous of these were small Alpine cave bears found at elevations of 1,600 to 2,800 m. Whereas some paleontologists have considered these bears a distinct form, or even a distinct species, others have disputed this. By a combination of morphological and genetic methods, we have analyzed a population of small cave bears from Ramesch Cave (2,000 m altitude) and one of larger cave bears from Gamssulzen Cave (1,300 m), situated approximately 10 km apart in the Austrian Alps (Figure 1A). We find no evidence of mitochondrial gene flow between these caves during the 15,000 years when they were both occupied by cave bears, although mitochondrial DNA sequences identical to those from Gamssulzen Cave could be recovered from a site located about 200 km to the south in Croatia. We also find no evidence that the morphology of the bears in the two caves changed to become more similar over time. We suggest that the two cave bear forms may have represented two reproductively isolated subspecies or species.     

The hypogean invertebrate fauna of Georgia (Caucasus)

Information about the cave invertebrates of Georgia, Caucasus, is summarised, resulting in 43 troglo- and 43 stygobiont taxa reported from 64 caves. Species distribution analyses were conducted for 61 caves harbouring 58 invertebrate taxa, with the majority of caves (39) located in Apkhazeti (north-western Georgia). In 22 caves from central-west Georgia (Samegrelo, Imereti and Racha-Lechkhumi regions of west Georgia) 31 taxa are reported. Composition of cave fauna differed strongly between the caves in Apkhazeti and the central-west of Georgia. Only two taxa of the total 86 were shared, resulting in negligible similarity (Sørensen-Dice coefficient S_s=4.8%). Rarefaction indicated an increase in number of species with additional sampling could increase species richness from 58 to 76 for caves in Apkhazeti and from 31 to 69 for caves in central-west Georgia. These findings suggest that the low invertebrate species richness observed in caves of western Georgia is the result of insufficient sampling. A pairwise approach to analysing species co-occurrence showed ten positive spatial associations in 7 out of 86 cave species, all from Kveda Shakurani and Tsebelda caves. The species co-occurring in the same microhabitat require further study to understand their relationships.