宁夏水洞沟遗址第2地点发掘报告

水洞沟第2地点是水洞沟遗址群的重要遗址之一, 自2003年来共进行了4次发掘, 揭露面积约100m2, 发现7个文化层, 包含用火遗迹、石制品、动物化石、串珠装饰品和磨制骨针等。本文观察和研究的石制品1万余件, 总体上显示中国北方石片石器工业的技术特征, 但最下部第7文化层出土1件具有水洞沟第1地点特征的石叶石核。动物化石比较破碎, 集中分布于火塘内部或周围, 反映了古人类围绕火塘进行肉类资源利用的行为。综合水洞沟第2地点的AMS14C及光释光测年数据,该地点主要文化层年龄集中在距今41ka-20ka BP之间。     

Late Famennian gastropoda from south-west England

The gastropod fauna of the Upper Devonian Baggy and Pilton formations in south‐west England is revised and includes some 30 taxa. The topmost part of the Upper Famennian succession in Devon is represented by clastic near‐shore and shallow shelf sediments, indicating a short‐term transgressive phase (‘Strunian Transgression’). The sequence yields a highly diverse fauna dominated by brachiopods and ostracodes, locally supplemented by crinoids, bryozoans, trilobites and molluscs. The taxa ‘Patellostium’britannicum sp. nov., Angyomphalus (Angyomphalus) junius sp. nov. and Dictyotomaria eurocapillaria sp. nov. are erected; a junior homonym is replaced by Macrochilina? piltonensis nom. nov. The gastropod fauna displays an independent character, where latest Devonian faunal elements overlap with Late Palaeozoic taxa expressing a transition similar to that of the bivalves, brachiopods, echinoderms and corals, without a sharp faunal break at the Devonian/Carboniferous boundary. Apart from the Caenogastropoda, all subclasses of gastropods are represented. Members of the bellerophontoids, pleurotomarioids and loxonematoids are most abundant, followed by murchisonioids, naticimorphs, euomphalomorphs and platyceratoids. The various gastropod groups represent different ecological demands and trophic categories, and together with the accompanying fauna indicate that nearly all habitats and niches were occupied in the shallow South Laurussian Shelf.     

Upper Pleistocene Panthera leo spelaea (Goldfuss, 1810) remains from the Bilstein Caves (Sauerland Karst) and contribution to the steppe lion taphonomy,palaeobiology and sexual dimorphism

Remains of the steppe lion Panthera leo spelaea (Goldfuss) from historical digs in the Bilstein Caves of Warstein (Sauerland, NW Germany) are described. Their age seems to be from the Early Weichselian periods (Upper Pleistocene). Whereas the Bilstein cave was inhabited by cave bears at that time only a few hyena prey remains, were most likely imported into the cave entrance by hyenas. Bite and crush marks on a few bones of Bison priscus, Bos primigenius, Cervus elaphus, a rhinoceros Coelodonta antiquitatis vertebra and even several chewed cave bear bones prove the hyena presence which is similar to other caves in the Sauerland hyena den cave rich region. Additionally some larger wolves subspecies Canis lupusspelaeus bones were found, but only few Crocuta crocuta spelaea remains are present. After taphonomic comparisons to six other hyena and cave bear den caves of northern Germany, this cave can be classified as a cave bear den, which was briefly used by hyenas only for food storage or commuting or cave bear predation site in one part of the Cave. The lion material refers at least to one young adult lioness, one more adult female and two male lions; therefore, at minimum, the remains of four adult individuals are represented. The absence of juvenile lion material, in contrast to cave bear cub remains in the Bilstein Caves, proves that P. leo spelaea did not use this and all other caves in the region to raise their cubs. The bone material from the Bilstein Caves would prove the same hyena-lion antagonism conflict being recently proven for the Perick Caves, Balve Cave or Martins Cave well. Other situations in caves such as the Keppler Cave and the Bilstein Cave initially show the more complex taphonomic situation of lion remains in European caves, especially in cave bear dens, where they seem to have hunted periodically cave bears, such as it is already proven for hyenas in the Sauerland Karst and other caves of Europe.     

周口店田园洞古人类化石点的无颈鬃豪猪(Hystrix subcristata)

周口店田园洞位于北京猿人遗址西南6km处,是新发现的晚期智人化石地点。该地点是迄今我国北方地区第四纪化石地点中含豪猪材料最丰富的。从头骨、牙齿、头后骨骼的形态特征及大小判断,田园洞的豪猪应归入我国现生无颈鬃豪猪(Hystrixsubcristata)。14C测年表明,含豪猪化石的地层时代为3.05～0.467万年,为更新世末期到全新世中期,是目前所知豪猪化石在我国北方地区的最晚记录。     

丹江库区晚新生代三种兔形类化石

记述了丹江库区周围发现的三种兔形类化石：产在丹江二级阶地基座岩层中的淅川跳兔（新种）Alloptoxxichuanwnsissp．nov．个体小,形态较早中新世中期的A．minor原始,其时代可能是早中新世早期,同时详细讨论了Alloptox的进化和分类;发现于台子山林场裂隙堆积物中的进步上新五褶兔（新种）Pliopentalagusprogressivussp.nov.个体为该属已知各种中最大者,形态较已知种更接近于现生的Pentalagus,它的时代可能为上新世末或更新世初;产于郧县曲远河口汉水Ⅳ级阶地的复齿拟鼠兔Ochotonoidescomplicidens与蓝田金丝猴发现于同一阶地,推测其时代为早更新世晚期。     

选择性支气管动脉插管转铁蛋白受体单克隆抗体灌注治疗中晚期肺癌(附68例临床报告)

本文对68例中晚期肺癌进行选择性支气管动脉插管采用转铁蛋白受体单克隆抗体与表阿霉素、顺伯等药物制成偶联物灌注。结果显示,肿瘤明显消退24例(35.2％),部分消退36例(52.5％),无变化8例(12.3％),总有效率为87.7％。通过对支气管动脉插管,导向灌注疗法结果显示,本疗法优于周围静脉供药,且无严重并发症,副作用轻,不失为一种可供选择的治疗方法。     

Dinocrocuta gigantea头骨的发现

本文记述了甘肃和政县晚中新世地层中发现的一个完整的巨鬣狗头骨;讨论了它的分类地位,修正了 Schlosser 1903年建种时的一些鉴定错误.巨鬣狗是鬣狗科中一个十分特化的成员,应代表一个独立的属.根据命名规则,我们采用 N. schmidt-Kittler 1976年所创的 Dinocrocuta. 因此,这个种应订正为 Dinocrocuta gigantea (schlosser, 1903).     

山西蒲县薛关细石器

本文记述了采自山西蒲县薛关的一批细石器。这批石器属于以楔状石核为特征的典型细石器技术传统。它的发现,对探索旧石器时代晚期人类在吕梁山一带劳动、生息状况,对进一步探讨我国华北地区各细石器文化之间的相互关系,都有一定的意义。     

妊娠晚期阴道B族链球菌的感染对肠道菌群和妊娠结局的影响

目的探究妊娠晚期阴道B族链球菌(group B Streptococcus,GBS)的感染对肠道菌群和妊娠结局的影响。方法选取2018年3月至2019年11月大连市中心医院孕检并分娩的妊娠妇女744人为对象,调查并统计B族链球菌的感染率;筛选有和没有B族链球菌感染妊娠妇女各47人,调查不良妊娠结局的发生率;选取信息匹配的妊娠晚期阴道B族链球菌感染和未感染的妊娠妇女,采集粪便样本,提取菌群DNA,用16S rDNA方法分析菌群变化。结果744名妊娠妇女中B族链球菌检出49例,感染率为6.59%;B族链球菌感染组总的不良妊娠发生比例为76.6%,正常组发生比例为27.7%(χ^2=5.491,P<0.05)。B族链球菌感染组妊娠妇女胎膜早破(χ^2=16.177,P<0.01)、难产(χ^2=21.134,P<0.01)和羊水异常(χ^2=22.989,P<0.05)的发生率与未感染组比较显著增高。B族链球菌感染组妊娠妇女肠道菌群发生显著变化。结论妊娠晚期阴道B族链球菌的感染可能引起肠道菌群紊乱,增加不良妊娠结局。     

Enigmatic tubes associated with microbial crusts from the Late Jurassic of the Northern Calcareous Alps (Austria): a mutualistic sponge–epibiont consortium?

Irregular tube-shaped microfossils incertae sedis are a typical constituent of Late Jurassic shallow-water reefal carbonates of the Northern Calcareous Alps of Austria and are described in open nomenclature. The enigmatic, polymorphous spar-filled tubes with neither observable external nor internal skeletal elements occur either free within peloidal sediments or mostly fixed to skeletal substrates embedded in microbial crusts including the genera Labes Eliášová, Crescentiella Senowbari-Daryan et al . or Isnella Senowbari-Daryan. The tubes are varied in shape and closely resemble different taxa of sponges. As the microbial crusts preferentially occur associated with these tubiform microfossils, this association is suggested to be non-parasitic and mutualistic. Without the surrounding crusts, the existence of these animals would have been masked or perhaps even totally lost in the fossil record expressing the importance of these findings as a characteristic element in the inventory of Late Jurassic reefal biocoenoses.