Synthèse biostratigraphique du plio-pléistocène de Guadix-Baza (Province de Granada,Sud-Est de l'Espagne)

In the Guadix-Baza basin, a continental sequence 0214 ranging from the Upper Miocene (Upper Turolian) to the Middle Pleistocene (Cromerian) has been established. An essay of biozonation by means of the Rodent succession is proposed, based on the following biozones: Trilophomys castroi, Mimomys occitanus, Mimomys cappetai, Mimomys cf. reidi, Mimomys ostramosensis, Allophaiomys pliocaenicus, Mimomys savini and Arvicola cantiana.     

中国的(亻莫)鼠(Mimomys)化石

本文详细综述了中国的 Mimomys 属材料.分布青海共和、甘肃合水、河北阳原及辽宁林西的 M. (Villanyia) chinensis Kormos、在甘肃合水与 M. gansunicus Zheng 共生,其时代为泥河湾期(或晚维拉方期,相当于 MN 18); 分布陕西渭南、山西平陆、榆社及河北阳原的 M. orientalis Young 和欧洲种 M. stehlini Kormos、分布渭南的 M. youhenicus 和欧洲种 M. kretzoii Fejfar 分别处于大致相同的进化阶段并和一个与 M. banchiaonicus 相似的种类共生, 其时代均为游河期(或早维拉方期,相当于 MN 16); 山西襄汾的 M. peii sp. nov. 的时代为大柴期(或中维拉方期,相当于 MN 17); 山西离石的 M. cf. intermedius (Newton) 的时代为泥河湾期;山西屯留的 Mimomys sp. 的时代可能偏早,为西村期(可能相当于路西南期或 MN 15).     

On the fallacy of using orthogenetic models of rectilinear change in arvicolid teeth for estimating the age of the first human settlements in Western Europe

Lozano-Fernández et al. (Lozano-Fernández I, Blain HA, López-García JM, Agustí J. 2014. Biochronology of the first hominid remains in Europe using the vole Mimomys savini: Fuente Nueva 3 and Barranco León D, Guadix-Baza Basin, south-eastern Spain. Hist Biol: Int J Paleobiol. doi:10.1080/08912963.2014.920015) recently published age estimates for two Late Villafranchian sites of Orce (Guadix-Baza basin, SE Spain), BL-D and FN-3, which provide some of the earliest evidence of human presence in Western Europe. The estimates were obtained from mean Lm1 values of the water vole Mimomys savini preserved in the sites and a couple of rectilinear equations derived in the Atapuerca TD section for site age on tooth length. However, this chronometric tool has problems that discourage its use in biostratigraphy, including: (1) the assumption of an orthogenetic trend of Lm1 increase during the evolution of the M. savini/Arvicola lineage; (2) the use of a chronology for the TD section not supported by original ESR data; (3) the discrepancies between the mean Lm1 values published for the TD levels and (4) the chronological ranges predicted when the standard deviations are used, which are exceedingly large as to be of value for biostratigraphic purposes. As a result, the pseudo numerical ages estimated for the Orce sites only add noise to the timing of the first human dispersal in Europe, which is based on a combination of results from well-established techniques such as palaeomagnetism, biostratigraphy and ESR.     

Studies on Porochlamydia buthi g. n., sp. n., an intracellular pathogen of the scorpion Buthus occitanus

An endemic disease caused by an intracellular microorganism related to the Chlamydiales, Porochlamydia buthi g. n., sp. n., exists in populations of the scorpion Buthus occitanus of Languedoc in southern France. The pathogen's developmental cycle occurs in the hepatopancreatic cells and progressively brings about the destruction of this organ. The microorganism is spread mostly through dejecta which contain the infectious forms during nearly the entire period of illness.     

The mammal fauna from the late Early Biharian site of Castagnone (Northern Monferrato, Piedmont, NW Italy)

Small and large mammals associated in Early Pleistocene floodplain sediments outcropping near Castagnone (Cerrina Valley, northern Monferrato Hills, Piedmont, NW Italy) are here examined, with particular emphasis on the voles. The micromammal assemblage includes Talpa sp., Sciurus cf. S. warthae, Mimomys savini, Mimomys pusillus, Microtus (Allophaiomys) cf. M. (A.) nutiensis, Ungaromys cf. U. nanus, Apodemus mystacinus, Leporidaeindert. and the associated macrofauna lists the following generic Galerian components: Stephanorhinus cf. S. hundsheimensis, Sus sp., Hippopotamus sp., Capreolus sp. and other Cervidae indet. (a fallow-deer and a megacerine), Bison sp. and Elephantidae indet. Due to the co-occurrence of U. nanus and an evolutionary advanced form of Allophaiomys with the normal paleomagnetic polarity of the embedding sediments, this faunal assemblage can be biochronologically dated to the late Early Biharian within the Jaramillo subchron.     

The late Neogene rodent succession of the Guadix–Baza Basin (south‐eastern Spain) and its magnetostratigraphic correlation

In this paper a magnetostratigraphically calibrated biozonation of the Miocene–Pliocene continental record of the Guadix–Baza Basin (south‐eastern Spain) is presented. This biozonation is based on a rodent succession which ranges from the latest Miocene (c. 6 Ma) to the latest Pliocene (c. 2.6 Ma). A total of nine biozones have been defined for the late Miocene and Pliocene, all of them based on the range or concurrent‐range of rodent species: Apodemus gudrunae – Apocricetus alberti Zone, Apocricetus barrierei Zone, Paraethomys aff. abaigari Zone, Trilophomys Zone, Mimomys davakosi Zone, Dolomys adroveri Zone, Mimomys hassiacus Zone, Mimomys polonicus Zone and Kislangia ischus Zone. A magnetobiostratigraphical correlation has been established between these biozones and the standard ATNTS scale, on the basis of the palaeomagnetic analysis carried out on the sections of Negratín, Botardo‐1 and Gorafe. The correlation has been completed with previous palaeomagnetic analysis in the sections of Galera and Zújar. The magnetobiostratigraphical correlation here established indicates a late Messinian age for the Apodemus gudrunae – Apocricetus alberti Zone, a Zanclean age for the Apocricetus barrierei, Paraethomys aff. abaigari, Trilophomys and Mimomys davakosi zones and a Piazencian age for the Mimomys hassiacus, Mimomys polonicus and Kislangia ischus zones. The Dolomys adroveri Zone is mostly Zanclean in age, but its uppermost part belongs to the Piazencian. Therefore, unit MN13 is correlated with the late Messinian, MN14 is correlated with the early Zanclean, most of MN15 is correlated with the late Zanclean, while the uppermost part of MN15 and MN16 are correlated with the Piazencian.     

Fine structure of scorpion trichobothria (Arachnida,Scorpiones)

Summary The fine structure of trichobothria in the scorpions Buthus occitanus (Amoureux, 1789) and Euscorpius carpathicus (Linné, 1767) was investigated by electron microscopy. In both species, cuticular and cellular characteristics are very similar. The articulation of the hair corresponds to that of other arachnid hair sensilla. The receptor endings are excentrically attached to the hair base. They consist of an enveloped S-shaped bundle of seven dendrites in B. occitanus and four in E. carpathicus. Neighbouring outer dendritic segments differ a great deal in diameter and ciliary modification. In B. occitanus, three enveloping cells and several additional secretory cells surround the inner dendritic segments. Structural characteristics are compared to those of other arachnid sensilla and their possible functional significance is discussed.     

Revision of the fossil vole assemblage (Mammalia,Rodentia, Arvicolidae) from Pleistocene deposits at Kisláng,Hungary

Abstract: The species‐rich fossil vertebrate assemblage from Pleistocene sedimentary deposits at Kisláng, Hungary, was originally described as containing eight species of arvicolids, six of which were considered new. Re‐examination of the material in the collection of the Hungarian Geological Institute, consisting of most of the previously described material, including the six name‐bearing types and also further undescribed specimens, indicates that the taxa Kislangia rex, Mimomys cf. hassiacus, Mimomys coelodus, Mimomys pusillus, Mimomys tornensis, Pitymimomys sp., Borsodia newtoni, Lagurodon arankae and Allophaiomys deucalion are present. Most of these species are compatible with Early Pleistocene age close to the boundary between the Villányian and Biharian regional stages (MQR10, MQ1, c. 1.6–2.0 Ma). However, the specimen of Mimomys cf. hassiacus is of approximately mid‐Pliocene age (MN15 c. 3.6–4.0 Ma), and one of the Pitymimomys specimens is referable to P. stenokorys, described from the earliest Pleistocene (MNR2–MNR3, MN17 c. 2.3–2.4 Ma). The assemblage is therefore interpreted as derived from at least three different geological periods and because of reworking of material is considered unusable to characterize any particular stratigraphic level. These conclusions are placed in the context of historical and current biostratigraphies.     

Étude de l'action deBacillus thuringiensis chez le scorpionButhus occitanus

Le scorpionButhus occitanus (Amoreux) infectéper os élimineBacillus thuringiensis (Berliner) dans ses déjections d'une manière progressive et en relation avec la prise de nourriture. Après inoculation dans l'hémocoele les germes peuvent persister longtemps dans l'hémolymphe sans que les animaux présentent des symptômes pathologiques. Seules les doses très élevécs conduisent à une septicémie. La DL 50, supérieure à 2,5 millions de bactéries, montre la très grande résistance de ces Arachnides à cette infection bactérienne.     

Walk the line: 600000 years of molar evolution constrained by allometry in the fossil rodent Mimomys savini

The allometric-constraint hypothesis states that evolutionary divergence of morphological traits is restricted by integrated growth regulation. In this study, we test this hypothesis on a time-calibrated and well-documented palaeontological sequence of dental measurements on the Pleistocene arvicoline rodent species Mimomys savini from the Iberian Peninsula. Based on 507 specimens representing nine populations regularly spaced over 600 000 years, we compare static (within-population) and evolutionary (among-population) allometric slopes between the width and the length of the first lower molar. We find that the static allometric slope remains evolutionary stable and predicts the evolutionary allometry quite well. These results support the hypothesis that the macroevolutionary divergence of molar traits is constrained by static allometric relationships.     

A distinct large vole lineage from the Late Pliocene - Early Pleistocene of China

A distinct large vole lineage involving three species from the Late Pliocene - Early Pleistocene of China is morphologically and quantitatively delineated. A special sinuous line (linea sinuosa) pattern, not previously recognized, diagnoses the new lineage, and distinguishes the species in the lineage from all other vole genera known either from China or elsewhere. At present, only two morphologically discrete evolutionary stages can be recognized in the lineage. The primitive stage is represented by rooted Mimomys peii and M. banchiaonicus, and the advanced stage is represented by the newly described rootless Heteromimomys zhengi nov. gen., nov. sp. from the Paleolithic site of Renzidong Cave in Anhui Province. The schmelzmuster of M. peii and Heteromimomys zhengi nov. gen., nov. sp. is also examined to provide more details about the lineage. This lineage diverged from Mimomys by the Late Pliocene within North China. The comparison between the arvicoline species co-existing with Heteromimomys zhengi nov. gen., nov. sp. and those from Haiyan Formation in the Yushe Basin, Shanxi Province, suggests the age of Heteromimomys zhengi nov. gen., nov. sp. can be correlated to or predate the Haiyan Formation, which is in reversely magnetized sediment identified as Chron 2r. The loss of roots in the lineage corresponds with a cooling event at the beginning of the Pleistocene, and seems to characterize the Nihewanian age of the Chinese Land Mammal ages from the perspective of arvicoline biochronology.     

Primary Structure of a Short Toxin from the Venom of a Vietnamese Scorpion (Buthus sp.)

The complete amino acid sequence of an important toxin (toxin 14) from the venom of a Vietnamese scorpion (Buthus occitanus sp.) has been determined, which includes 35 amino acid residues and three disulfide bridges (molecular weight, 3843 Da). The comparison of the sequence with known sequences of short scorpion toxins led to the conclusion that toxin 14 belongs to a novel group of toxins affecting the excitability of myelinated nerves.     

Biochronology of the first hominid remains in Europe using the vole Mimomys savini: Fuente Nueva 3 and Barranco León D,Guadix-Baza Basin,south-eastern Spain

The sites of Barranco León D (BL-D) and Fuente Nueva 3 (FN-3) in the Guadix-Baza Basin (Granada, Spain), together with the site of Sima del Elefante in the Sierra de Atapuerca (Burgos, Spain), constitute one of the oldest records of the earliest hominid population in the European continent west of Dmanisi (Georgia, Lesser Caucasus). In the Guadix-Baza Basin, evidence of human occupation has been found to date in the form of lithic industry (Mode 1) and cut marks in large-mammal fossil remains (mainly of hippopotamuses and elephants), and recently a human tooth considered as the oldest in Europe has been discovered. Although in the case of Sima del Elefante there is unanimity among the scientific community regarding the chronology of the unit in which the hominid remains were found (Unit TE9c, 1.22 Ma), there is continuing debate on the chronology of the sites of the Guadix-Baza Basin (FN-3 and BL-D). This applies especially to BL-D, as the numerical datings published for this site have a very high error range (1.4 ± 0.38 Ma). In this paper, the chronology of these two sites is determined using as a marker the morphological and morphometric changes undergone by Mimomys savini in its first lower molar (m1) over the course of its evolutionary history. It has been possible to confirm that the oldest human presence in the Guadix-Baza Basin and at Sima del Elefante (Atapuerca) share a similar chronology, dated to between 1.1 and 1.4 Ma. Apparently, the oldest site with human remains in Europe is seen to be BL-D, dated to 1.26 ± 0.13 Ma, followed by Level TE9c, dated to 1.22 ± 0.16 Ma, and FN-3, dated to 1.20 ± 0.12 Ma.     

The Atapuerca sites and the ibeas hominids

The Atapuerca railway Trench and Ibeas sites near Burgos, Spain, are cave fillings that include a series of deposits ranging from below the Matuyama/Bruhnes reversal up to the end of Middle Pleistocene. The lowest fossil-bearing bed in the Trench contains an assemblage of large and small Mammals includingMimomys savini, Pitymys gregaloides, Pliomys episcopalis, Crocuta crocuta, Dama sp. and Megacerini; the uppermost assemblage includesCanis lupus, Lynx spelaea, Panthera (Leo) fossilis, Felis sylvestris, Equus caballus steinbeimensis, E.c. germanicus, Pitymys subterraneus, Microtus arvalis agrestis, Pliomys lenki, and alsoPanthera toscana, Dicerorbinus hemitoechus, Bison schoetensacki, which are equally present in the lowest level. The biostratigraphic correlation and dates of the sites are briefly discussed, as are the paleoclimatic interpretation of the Trench sequences. Stone artifacts are found in several layers; the earliest occurrences correspond to the upper beds containingMimomys savini. A set of preserved human occupation floors has been excavated in the top fossil-bearing beds. The stone-tool assemblages of the upper levels are of upper-medial Acheulean to Charentian tradition. The rich bone breccia SH, in the Cueva Mayor-Cueva del Silo, Ibeas de Juarros, is a derived deposit, due to a mud flow that dispersed and carried the skeletons of many carnivores and humans. The taxa represented are:Ursus deningeri (largely dominant),Panthera (Leo) fossilis, Vulpes vulpes, Homo sapiens var. Several traits of both mandibular and cranial remains are summarized. Preliminary attempts at dating suggest that the Ibeas fossil man is older than the Last Interglacial, or oxygen-isotope stage 5.     

Isolation and Partial Characterization of Lectin from the Venom of Vietnamese Scorpion Buthus occitanussp.

A lectin was isolated from the venom of scorpion Buthus occitanussp. by means of Sephadex G-50 gel filtration and CM-cellulose ion exchange chromatography. The homogeneous lectin preparation consisted of homodimeric molecules with a subunit M _rof 9.3 kDa. Glycine, alanine, and serine dominated in the lectin amino acid composition. The lectin was a glycoprotein containing 20% carbohydrates (predominantly mannose and glucose). Trypsin-treated murine erythrocytes agglutinated at a lectin concentration of 32 g/ml. Hemagglutination was inhibited by carbohydrates (L-fucose > D-glucose > L-rhamnose > D-xylose). The lectin revealed no phospholipase or hyaluronidase, nor toxic activity.     

云南省迪庆州更新世早期哺乳类化石的发现

本文简述横断山脉中段中甸尼西的哺乳类化石九种,能鉴定到种一级的只有1/3,其中(亻莫)鼠是新种.     

河北阳原—蔚县晚上新世小哺乳动物化石

1984年于泥河湾组下段下部发现小哺乳动物化石标本1800余件,经初步鉴定,它们代表了食虫目、啮齿目和兔形目的26个种,其中的 Paenelimnoecus, Pliopentalagus, Germanomys 为我国首次发现.估计动物群的时代为游河期早期,相当于欧洲的维拉方早期 (MN 16).     

Fine structure of scorpion spermatozoa (Buthus occitanus; buthidae,scorpiones)

The mature spermatozoa of Buthus occitanus are threadlike in shape and divided into sperm head, middle piece, and end piece. The sperm head is corkscrew shaped anteriorly and in this region bears an unusual acrosomal complex consisting of a ring-shaped acrosomal vacuole associated with a subacrosomal filament and a perinuclear amorphous component. The subacrosomal filament extends posteriorly into a tube-like invagination of the elongated nucleus. The middle piece is characterized by elongated mitochondria which spiral around the anterior part of the flagellum in an extended collar separated from the flagellum by an extracellular cleft, termed the central flagellar tunnel. In addition to the usual 9 × 2 + 2 axonemal pattern in flagella, 9 × 2 + 1 and 9 × 2 + 3 patterns also were observed. The end piece is represented by the free flagellum. Similarities and diversities of scorpionid spermatozoa are discussed with respect to systematic relationships.     

Burrow decorations as antipredatory devices

Animal decorations are normally interpreted as signals of quality.In spiders, however, decorations may have different functions,including the attraction of prey to the web or making the spidercryptic to predators. To date, there is scant evidence for thelatter hypothesis. Here we use the burrow-decorating wolf spiderLycosa tarantula to test whether turrets around the burrow serveto prevent burrow invasion and predation from the Occitan scorpionButhus occitanus. We located spiders and scorpions in fieldenclosures and manipulated the presence or absence of decorationsor turrets. We found that the presence of the turret decreasesthe rate of burrow invasion and improves spider survival, possiblybecause the turret makes the burrow cryptic to scorpions. Inaddition, a field survey showed that burrows with larger decorationshad a lower chance of being invaded by scorpions. These resultsprovide evidence that the decoration has an antipredatory functionin nature.