COLLEMBOLAN COMMUNITIES (HEXAPODA: COLLEMBOLA) FROM THE BUZĂU LAND GEOPARK (BUZĂU MOUNTAINS, ROMANIA)

The authors present the Collembola species collected from the Buzău Land Geopark (Buzău Mountains, Romania). The uniqueness of the Buzău Land Geopark is illustrated by the presence of very rare collembolan species such as Friesea afurcata (Denis, 1926), Deutonura phlegraea (Caroli, 1910), Xenylla welchi Folsom, 1916, Desoria tigrina Nicolet, 1842, Tetracanthella transylvanica Cassagnau, 1959 and Neanura parva (Stach, 1951). We also mention here Orchesella maculosa Ionescu, 1915, an endemic species for the Carpathian Mountains (Romania and Ukraine)

Carnivore impact on cave bear bones and the analysis of their dispersion. Case study: UrŞilor cave (NW Romania)

In taphonomy, the study of carnivore modification of fossil bones and the analysis of their dispersion represent the best approach to assessing the extent of bone modification and displacement for a given bone assemblage. Here we analyze the excavated bone deposit from Urşilor Cave, a well-documented and fossil-rich Upper Pleistocene cave bear site from the Romanian Carpathian Mountains. More than 1400 limb bones or bone remains were analyzed (NISPleft and right = 1424) and 69 measurable puncture marks were identified, measured and morphologically analyzed. Moreover, for assessing the degree of bone scattering, almost 540 cave bear limb bones and mandibles were refitted and the Index of Skeletal Disjunction (ISD) was calculated for the entire bone assemblage. More than 30 % of the analyzed cave bear limb bones were affected by carnivores: the ulnae were the most affected (39.3 %) while the humeri and femora were less modified (24.7 % and 25.5 %, respectively). The range of variation in size of the puncture marks, the morphological features of various tooth marks and the faunal composition of the studied bone assemblage indicate that at least two carnivore taxa are responsible for the bone modifications. The results obtained for the ISD index indicate higher displacement for femora when compared to other bones (e.g. tibiae, mandibles, humeri). Our analyses of bone modifications caused by carnivores indicate a low level of the scattering of intensely modified (by in situ consumption) bones, and notable carnivore impact on the configuration of the bone assemblage.Key words: Ursus spelaeus, taphonomy, ISD, tooth marks, Urşilor Cave, Romanian Carpathians.Vpliv zveri na kosti jamskih medvedov iz jame UrŞilor (SZ Romunija) in analiza njihove razkropljenostiProučevanje sledov zveri na fosilnih kosteh in razkropljenosti kosti v prostoru je najboljše tafonomsko orodje za pridobivanje podatkov o obsegu takšnih pojavov znotraj posameznega paleontološkega zbira. V raziskavi obravnavamo kosti jamskega medveda iz jame Urşilor, dobro raziskanega mlajšepleistocenskega najdišča v Romunskih Karpatih. Analizirali smo več kot 1424 dolgih cevastih kosti okončin ali njihovih odlomkov in pri tem prepoznali, izmerili in morfološko analizirali 69 odtiskov zob. Poleg tega smo izračunali indeks razkropljenosti okostja (Index of Skeletal Disjunction, ISD) za celotni paleontološki zbir, zaradi česar smo sestavili skoraj 540 dolgih cevastih kosti okončin in spodnjih čeljustnic jamskega medveda. Sledove zveri smo prepoznali na več kot 30 % kosti okončin, najpogosteje na komolčnicah (39.3 %), nekoliko redkeje pa na nadlahtnicah in stegnenicah (24.7 % oz. 25.5 %). Variabilnost v velikosti odtiskov zob, njihovih morfoloških značilnostih in favnistični sestavi proučevanega paleontološkega zbira pričajo o tem, da sta ugotovljene spremembe medvedjih kosti povzročili vsaj dve različni zveri. Vrednosti indeksa razkropljenosti okostja kažejo na izrazitejšo razkropljenost stegnenic v primerjavi z drugimi kostmi (npr. golenicami, nadlahtnicami, spodnjimi čeljustnicami). Naša analiza kaže na skromno razkropljenost intenzivno obgrizenih kosti (zaradi hranjenja v sami jami) in znaten vpliv zveri na konfiguracijo paleontološkega zbira.Ključne besede: Ursus spelaeus, tafonomija, ISD, ugrizi, jama Urşilor, Romunski Karpati

CARNIVORA FROM THE EARLY PLEISTOCENE OF GRĂUNCEANU (OLTEŢ RIVER VALLEY, DACIAN BASIN, ROMANIA)

The Grăunceanu site in the Olteţ River Valley has yielded a rich carnivoran assemblage including at least 10, possibly 11 species: Vulpes alopecoides, Nyctereutes megamastoides, Ursus etruscus, Meles thorali, Lutraeximia sp., Pliocrocuta perrieri, Lynx issiodorensis, Puma pardoides, Megantereon cultridens, Homotherium latidens and possibly Pachycrocuta brevirostris. The faunal assemblage is compared with approximately coeval sites Europe and western Asia. This comparative analysis shows that the Grăunceanu assemblage shows the greatest similarities with sites to the west such as Senèze and, particularly, Saint-Vallier, rather than more easternly ones such as Liventsovka and Dmanisi. The relative abundance of the taxa at Grăunceanu was compared to that of Saint-Vallier and broad similarities were found, except for the absence of some cursorially adapted taxa present at Saint-Vallier but absent from Grăunceanu. The absence at Grăunceanu of taxa with a reconstructed cursorial hunting strategy, such as Chasmaporthetes and Acinonyx, may suggest less open habitat at Grăunceanu than indicated in previous paleoenvironmental reconstructions

Ancient DNA reveals interstadials as a driver of common vole population dynamics during the last glacial period

Aim Many species experienced population turnover and local extinction during the Late Pleistocene. In the case of megafauna, it remains challenging to disentangle climate change and the activities of Palaeolithic hunter-gatherers as the main cause. In contrast, the impact of humans on rodent populations is likely to be negligible. This study investigated which climatic and/or environmental factors affect the population dynamics of the common vole. This temperate rodent is widespread across Europe and was one of the most abundant small mammal species throughout the Late Pleistocene. Location Europe. Taxon Common vole (Microtus arvalis). Methods We generated a dataset comprised of 4.2 kb long fragment of mitochondrial DNA (mtDNA) from 148 ancient and 51 modern specimens sampled from multiple localities across Europe and covering the last 60 thousand years (ka). We used Bayesian inference to reconstruct their phylogenetic relationships and to estimate the age of the specimens that were not directly dated. Results We estimated the time to the most recent common ancestor of all last glacial and extant common vole lineages to be 90 ka ago and the divergence of the main mtDNA lineages present in extant populations to between 55 and 40 ka ago, which is earlier than most previous estimates. We detected several lineage turnovers in Europe during the period of high climate variability at the end of Marine Isotope Stage 3 (MIS 3; 57-29 ka ago) in addition to those found previously around the Pleistocene/Holocene transition. In contrast, data from the Western Carpathians suggest continuity throughout the Last Glacial Maximum (LGM) even at high latitudes. Main Conclusions The main factor affecting the common vole populations during the last glacial period was the decrease in open habitat during the interstadials, whereas climate deterioration during the LGM had little impact on population dynamics. This suggests that the rapid environmental change rather than other factors was the major force shaping the histories of the Late Pleistocene faunas.info:eu-repo/semantics/publishedVersio

Pliocene large mammals of Romania

Se presenta una revisión de los grandes mamíferos del Plioceno de la cuenca Dácica y la depresión Brasov, Rumania, y se indican las asociaciones faunísticas de los sitios fosilíferos más significativos. Las asociaciones de mamíferos del Plioceno inferior (Rusciniense, MN 14-15) y Plioceno superior (Villafranquiense medio/superior, MN17, MQ1) están bien representadas, mientras las del Plioceno medio (Villafranquiense inferior, MN 16) son aún poco conocidas.A review of the Pliocene large mammals of the Dacic Basin and the Brasov Depression, Romania, is presented and the faunal associations of the most significant fossiliferous sites are indicated. Early Pliocene (Ruscinian, MN 14-15) and late Pliocene (middle/late Villafranchian, MN 17, MQ1) mammalian assemblages are well represented, whereas those of the middle Pliocene (early Villafranchian, MN 16) are still poorly known

Carnivore impact on cave bear bones and the analysis of their dispersion. Case study: UrŞilor cave (NW Romania)

In taphonomy, the study of carnivore modification of fossil bones and the analysis of their dispersion represent the best approach to assessing the extent of bone modification and displacement for a given bone assemblage. Here we analyze the excavated bone deposit from Urşilor Cave, a well-documented and fossil-rich Upper Pleistocene cave bear site from the Romanian Carpathian Mountains. More than 1400 limb bones or bone remains were analyzed (NISPleft and right = 1424) and 69 measurable puncture marks were identified, measured and morphologically analyzed. Moreover, for assessing the degree of bone scattering, almost 540 cave bear limb bones and mandibles were refitted and the Index of Skeletal Disjunction (ISD) was calculated for the entire bone assemblage. More than 30 % of the analyzed cave bear limb bones were affected by carnivores: the ulnae were the most affected (39.3 %) while the humeri and femora were less modified (24.7 % and 25.5 %, respectively). The range of variation in size of the puncture marks, the morphological features of various tooth marks and the faunal composition of the studied bone assemblage indicate that at least two carnivore taxa are responsible for the bone modifications. The results obtained for the ISD index indicate higher displacement for femora when compared to other bones (e.g. tibiae, mandibles, humeri). Our analyses of bone modifications caused by carnivores indicate a low level of the scattering of intensely modified (by in situ consumption) bones, and notable carnivore impact on the configuration of the bone assemblage.Key words: Ursus spelaeus, taphonomy, ISD, tooth marks, Urşilor Cave, Romanian Carpathians.Vpliv zveri na kosti jamskih medvedov iz jame UrŞilor (SZ Romunija) in analiza njihove razkropljenostiProučevanje sledov zveri na fosilnih kosteh in razkropljenosti kosti v prostoru je najboljše tafonomsko orodje za pridobivanje podatkov o obsegu takšnih pojavov znotraj posameznega paleontološkega zbira. V raziskavi obravnavamo kosti jamskega medveda iz jame Urşilor, dobro raziskanega mlajšepleistocenskega najdišča v Romunskih Karpatih. Analizirali smo več kot 1424 dolgih cevastih kosti okončin ali njihovih odlomkov in pri tem prepoznali, izmerili in morfološko analizirali 69 odtiskov zob. Poleg tega smo izračunali indeks razkropljenosti okostja (Index of Skeletal Disjunction, ISD) za celotni paleontološki zbir, zaradi česar smo sestavili skoraj 540 dolgih cevastih kosti okončin in spodnjih čeljustnic jamskega medveda. Sledove zveri smo prepoznali na več kot 30 % kosti okončin, najpogosteje na komolčnicah (39.3 %), nekoliko redkeje pa na nadlahtnicah in stegnenicah (24.7 % oz. 25.5 %). Variabilnost v velikosti odtiskov zob, njihovih morfoloških značilnostih in favnistični sestavi proučevanega paleontološkega zbira pričajo o tem, da sta ugotovljene spremembe medvedjih kosti povzročili vsaj dve različni zveri. Vrednosti indeksa razkropljenosti okostja kažejo na izrazitejšo razkropljenost stegnenic v primerjavi z drugimi kostmi (npr. golenicami, nadlahtnicami, spodnjimi čeljustnicami). Naša analiza kaže na skromno razkropljenost intenzivno obgrizenih kosti (zaradi hranjenja v sami jami) in znaten vpliv zveri na konfiguracijo paleontološkega zbira.Ključne besede: Ursus spelaeus, tafonomija, ISD, ugrizi, jama Urşilor, Romunski Karpati

SIZE OF THE CAVE BEAR POPULATION AND SKELETAL DISTRIBUTION FROM URŞILOR CAVE, ROMANIA

Spatial distribution analyses of fossil bones are often used in cave taphonomy for i) assessing directly the size of a given fossil population and ii) indirectly, for palaeo-environmental reconstructions. Urşilor Cave from northwestern Romania hosts one of the richest MIS 3 cave bear bone assemblages of Europe, and as the nature of the bone deposition was not settled yet, the study of the size of cave bear population and the distribution of the skeletal element was needed. More than 11,500 cave bear skeletal elements (NISPtotal = 11, 511), derived from 105 individuals (MNIcanines = 105) were extracted from the palaeontological excavation (ca. 9 m2) from the lower level of the cave and documented (photographed, mapped, and topographically measured). Almost 58% of all analyzed bones and teeth are concentrated in three quadrants of the excavation (C1, D1 and E2); the bones’ density decreases in the D4 and A1 quadrants. Based on the obtained results on the spatial distribution of the cave bear bones, we assume that the studied bone assemblage should be now regarded as a consequence of a cave trap (deposition in situ) while the hypothesis of fluvial transport (previously assumed) becomes questionable

Nouvelles données sur la chronologie des sites paléolithiques en contexte lœssique du Nord-Est et du Sud-Est de la Roumanie (Périphérie orientale des Carpates)

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Monitoring Human Impact in Show Caves. A Study of Four Romanian Caves

(1) Background: Show caves are unique natural attractions and touristic traffic can trigger their degradation within a short time. There are no universal solutions to counter the effects of the touristic impact upon the cave environment and both protection protocols and management plans have to be established on a case-by-case basis. (2) Methods: The study includes four show caves from the Romanian Carpathians, where monitoring of the number of visitors, paralleled by the monitoring of the main physicochemical parameters of the air and water (CO2, temperature, humidity, drip rate, conductivity, and pH) was implemented. (3) Results and Conclusions: The results of the study have: established a set of basic principles to be enforced by the management of show caves and issued a set of preventive measures and instructions to be followed by the personnel and stakeholders of the caves