贵州毕节扒耳岩巨猿地点的偶蹄类

系统记述了自2001年以来从贵州省毕节扒耳岩洞穴堆积中出土的偶蹄目化石:最后"双齿尖河猪"("Dicoryphochoerus"ultimus)、麂(未定种)(Muntiacus sp.)、凤岐祖鹿(?)(Cervavitus?fenqii)、黑鹿(相似种)(Cervus(R.)cf C.(R.)unicolor)、羚牛(未定种)(Budorcas sp.)、山羊亚科(属种未定)(Caprinae gen.et sp.indet.)、羚羊(未定种)(Gazella sp.)、斯迈提丽牛(未定种)(Leptobos(Smertiobos)sp.)8个种类。毕节扒耳岩巨猿动物群中的偶蹄类与广西柳城巨猿洞和湖北建始龙骨洞的偶蹄类可比性最大。毕节偶蹄类含有较多的古老种类, 指示其地质时代为早更新世早期; 同时显示其生态环境为植被既有密集的丛林又有开阔的草地(或草坡), 局部镶嵌有半开阔树林,而附近分布有一定的水域, 气候温暖, 非常适合高等灵长类栖息。     

安徽繁昌早更新世人字洞古人类活动遗址及其哺乳动物群

1998年,在安徽繁昌县癞痢山发现了两处洞穴、裂隙堆积。在随后两年中对其中之一的人 字洞进行了系统发掘,采集到一定数量的石制品、骨制品和属种丰富、生态习性多样的大量脊 椎动物化石。人字洞发育于三叠纪灰岩中,洞穴堆积物厚约30米,可分为上下两个堆积单元, 脊椎动物化石和古人类遗物主要产于上堆积单元。经初步研究,人字洞动物群包含67种哺乳动 物,与我国南、北方第四纪早期的其它主要动物群相比,其绝灭属、种比例更高,动物群中主 要属种的形态特征更原始,然而该动物群中真马(Equus)的出现,表明其地质时代为早更新世 早期。这一动物群具有浓郁的北方色彩,显示出更新世初期我国境内有一次明显的降温事件,促 使北方动物大规模向南迁徒,在长江以南形成东洋界和古北界动物地理区系交错带的过渡区动 物群。人字洞动物群的发现为研究我国第四纪早期动物群的特征和动物地理区系演化及古气候 环境变迁提供了重要的信息。     

日本三宅岛火山土壤中硫代硫酸盐氧化菌的分离、生物学特性及鉴定

【目的】利用培养法从日本三宅岛火山土壤(堆积年限131年)中分离到一株能氧化分解硫代硫酸盐的细菌MU2A-22T。【方法】用培养法对该菌株MU2A-22T进行了生理生化性质以及分类学位置上的确定。【结果】菌株MU2A-22T为革兰氏阴性,短杆状或球状。理化性质表明该菌株能利用葡萄糖、L-阿拉伯糖、葡萄糖酸盐、己二酸酯、dL-苹果酸钠、硫代硫酸钠(最适浓度为2.5 mmol/L)为唯一碳源进行自养生长。最适生长温度为25°C 30°C,最适pH为6.0 8.0。菌株MU2A-22T的16S rRNA序列与菌株Paracoccus solventivorans 6637T亲缘关系最近,序列相似性为97%,编码核酮糖-1,5-二磷酸羧化酶/加氧酶(Rubisco)的基因也被确定。对Paracoccus属内几种近缘菌的脂肪酸分析,证明菌株MU2A-22T中含有Paracoccus属的特征氨基酸,其中含量大于10%的分别为C18:1(74.7%)和C18:0(12.1%)。DNA-DNA杂交实验表明,菌株MU2A-22T与Paracoccus solventivorans 6637TDNA的相似度为49.3%。MU2A-22T菌株G+C含量为66.5%66.7%。【结论】菌株MU2A-22T为Paracoccus属内的一新种菌(登录号GQ452286),命名为Paracoccus scorialis sp.nov.。     

中国古人类遗址年代学的研究进展与问题

我国丰富的古人类遗存为研究东亚乃至全球古人类起源、迁徙和演化提供了重要的基础材料与数据。对已发表的2000多处旧石器时代古人类遗址年代学数据的整理和统计分析发现,绝大多数遗址目前仍缺少基本的年代学数据,不足20%的遗址开展过测年,仅10%左右具有相对可靠的年代学数据,只有极少数开展了多种测年方法的交叉定年。对于80多处出土古人类化石的遗址,亦过半存在明显的年代学争议。我们对一些古人类遗址中的常见各种复杂的同沉积和沉积后改造现象进行了详细分析,探讨了我国测年平台和测年队伍建设、考古发掘以及年代学采样与测年方法学等方面存在的问题,及其对遗址年代学研究的可能影响。基于此,笔者提出改善我国古人类年代学研究现状的可能措施,希望可以抛砖引玉,引发对该研究领域更多的关注和思考。     

Clustered trilobite assemblages in the Middle Devonian Hamilton Group

Clusters of well-preserved trilobites occur throughout lower and middle Paleozoic strata. This phenomenon, however, remains poorly understood. Several thin, regionally persistent beds in the Middle Devonian (Givetian) Hamilton Group of New York State display taphonomic and sedimentary features which indicate rapid burial by storm-generated clouds of fine-grained sediment. Furthermore, components in these units display little or no post-mortem disturbance and, therefore, reflect in faunal associations. These beds contain two types of clustered assemblages of the trilobites Phacops (Green), Greenops boothi (Green) and Dechenella rowi (Green). Body clusters comprise dense assemblages of three or more complete trilobite corpses. Moult clusters , in contrast, are composed of three more moult ensembles; i.e., articulated thoracopygidia in close proximity to corresponding cephala. Clusters are species-segregated and contain only a small portion of the total size range exhibited by trilobite species. Moreover, body clusters and moult clusters are morphometrically undifferentiated indicating that these two cluster modes represent related phenomena. Analogy with modern marine arthropods suggests that trilobites assembled into monospecific, age-segregated clusters and moulted prior to en masse copulation.     

An integrative ichnological and taphonomic approach in a transgressive–regressive cycle: a case study from Devonian of Paraná Basin,Brazil

The palaeoenvironmental context of a section of the Devonian Ponta Grossa Formation (Paraná Basin) was examined using an integrated ichnological and taphonomic approach. Three taphofacies (T‐A, T‐B and T‐C) and six ichnofabrics are recognized. T‐A is mainly composed of disarticulated organisms and is associated with Chondrites, Planolites‐Palaeophycus, Asterosoma‐Zoophycos and Asterosoma‐Chondrites ichnofabrics, representing the Cruziana ichnofacies. The upward increase in diversity and abundance of body fossils for Taphofacies A can be explained by changes in sedimentation rates during aggradational to progradational phases. T‐B beds, represented by articulated brachiopods, occur in distal tempestites associated with the Skolithos ichnofabric (Skolithos ichnofacies) and represent higher hydrodynamic energy and oxygenation than in T‐A. Taphofacies C, characterized by a mix of articulated and disarticulated organisms, generally lacks bioturbation except for Chondrites ichnofabrics occurring only at the bed tops, suggesting low substrate oxygenation and low‐energy conditions. T‐C indicates the maximum transgression in the T‐R cycle, characterizing it as a good indicator of maximum flooding surfaces. The composite Asterosoma‐Teichichnus ichnofabric (bioturbation degree 5) occurs in layers without body fossils and represents suites of the Cruziana ichnofacies. This likely reflects intense intrastratal activity at all substrate levels, which facilitated the oxygenation of the substrate disallowing the preservation of organism remains. This observation indicates that the bioturbation is an important factor controlling the loss of taphonomic information within the TAZ, mainly when associated with detritus‐feeding trace fossils.     

Persistence of Halophylic Methanogens and Oil-Degrading Bacteria in an Offshore Oil-Producing Facility

Microbial communities in a high saline, Tetrakis-Hydroxymethyl Phosphonium Sulfate (THPS) and nitrate-treated Nigerian oil-producing facilities were investigated. Methanogens in produced water samples preferred methanol, while those in pig-run samples (oily wastes from pipelines) preferred H₂/CO₂, as substrates to produce methane and stimulate metal corrosion. The results coincide with the dominance of methylotrophic and hydrogenotrophic methanogens in the respective samples. The same microbial populations were also THPS and high salinity tolerant. The nitrate reducers and hydrocarbon degraders were also dominant in the reservoir. A more inclusive and effective mitigation strategy is therefore required to effectively tackle biocide resistant methanogens in biocide treated oilfield.     

Schistosoma japonicum: Immunopathology of nephritis in Macaca fascicularis

Macaca monkeys experimentally infected with Schistosoma japonicum developed a chronic progressive kidney lesion characterized by an increase of mesangial matrix, local glomerular hypercellularity, and local thickening of glomerular basement membrane. Immunofluorescence studies revealed the localization of IgG, IgM, IgA, and IgE immunoglobulins mostly in the mesangial area of the glomeruli accompanied by the deposition of Schistosoma antigens. By electron microscopy, in addition to the local thickening of the glomerular basement membrane, dense homogeneous deposits and those with moth-eaten appearance were detected in the mesangial matrix. These findings suggest that worms in the bloodstream continuously release antigenic materials that stimulate host's antibody response belonging to various immunoglobulin classes including IgE. The produced antibodies and antigens would form immune complexes that deposited in the glomeruli. The increased vascular permeability caused by antigen-IgE antibody interaction may play an important role in the deposition of immune complexes and in the rapid development of kidney injury.     

Pratiques funéraires et recrutement : reprise d’étude des collections osseuses issues des dolmens du Languedoc oriental et sud des Cévennes à la fin du Néolithique

Collective burials were the main and most widespread funerary practice at the end of the Neolithic, beginning of the Bronze Age in the south of France. Megalithic monuments required a huge investment of time and labor. According to ethnographic studies, these monumental tombs are generally built and managed collectively. One can therefore wonder who was buried inside these structures because several archaeological studies indicate that access to these tombs can sometimes be restricted to certain members of the population. Indeed, ethnography highlights that access to certain tombs can be structured by variables such as kinship, social status, etc. While previous studies have mainly focused on the architecture and function of these monuments, this article focuses on the process of deposition of human remains and the characterization of the population buried inside these monuments. Since 2012, a project has been undertaken on the dolmens of the south of France in order to discuss funerary practices and to compare them with data from other archaeosciences to rediscuss the funerary traditions in place at the end of the Neolithic, the beginning of the Bronze Age.