New latest Coniacian to middle Campanian foraminiferal data from the lower Zongshan Formation in the Chaqiela section,Gamba, southern Tibet

A first and detailed foraminiferal biostratigraphic work on the lower part of the Zongshan Formation (Limestone I and Calcareous Marl I sequence) in the Chaqiela section, Gamba, southern Tibet, allows the recognition of three latest Coniacian to middle Campanian planktic foraminiferal biozones: Dicarinella asymetrica Total Range Zone, Globotruncanita elevata Partial-Range Zone, and Contusotruncana plummerae Interval Zone. The base and top of the Santonian Stage in the Chaqiela section were placed at the lowest occurrence (LO) of Globotruncana linneiana and the highest occurrence (HO) of Dicarinella asymetrica, respectively. The deposition of the latest Coniacian to middle Campanian sediments of the lower Zongshan Formation in the Chaqiela section seems to have been continuous or at least without any major gap based on the planktic foraminiferal biozones and events.     

Integrated Silurian Chitinozoan and Graptolite Biostratigraphy of the Banwy River Section, Wales

The succession of 38 upper Llandovery–lower Wenlock chitinozoan taxa from graptolitic horizons in the Banwy River section (Powys, Wales) is described. Five new species are named: Bursachitina nestorae Conochitina leviscapulae Conochitina mathrafalensis Belonechitina cavei Belonechitina meifodensis . A further ten taxa are described under open nomenclature. Seven chitinozoan biozones are recognized in the Banwy River section, three of which ( Cingulochitina bouniensis Conochitina acuminata Salopochitina bella ) are new. The base of each biozone is correlated with the graptolite biostratigraphical scheme as follows: Angochitina longicollis Biozone — upper spiralis Biozone; Conochitina acuminata Biozone — lowermost lapworthi Biozone; Margachitina banwyensis Biozone — upper lapworthi Biozone; Margachitina margaritana Biozone — lowermost insectus Biozone; Cingulochitina bouniensis Biozone — upper murchisoni Biozone; Salopochitina bella Biozone — upper firmus Biozone. The succession of chitinozoan biozones in the Banwy River section is compared with that in other sections which have graptolite biostratigraphical control. This has highlighted the following: (1) the correlation of the base of the dolioliformis Biozone with the graptolite biozonation is imprecise; (2) E. dolioliformis is recorded only from levels after the first A. longicollis in Sweden (although this may reflect previously unrecognized synonymies); (3) the longicollis Biozone may be diachronous, its base correlating with levels low in the Telychian in Sweden, Norway and Estonia and with the upper Telychian spiralis Biozone in Wales and the Prague Basin; (4) data herein and from the Prague Basin indicate that the base of the margaritana Biozone correlates with a level low in the insectus Biozone.     

A late Wenlock flora from Co. Tipperary, Ireland

An assemblage of macroplants preserved as highly coalified compressions which lack anatomy is described from a Wenlock locality in County Tipperary, Ireland. Most of the fertile specimens are assigned to Cooksonia Lang. The taxonomic status of this genus is discussed. Some poorly preserved palynomorphs, including miospores, acritarchs, chitinozoans and a variety of tubes, have been isolated from associated sediments, but the age of the flora is based on graptolites. Sedimentological and palaeontological studies of the region are summarized. They provide little direct evidence for the habitats of the plants which are considered to have been terrestrial. The relevance of this flora to the current debate on the colonization of the land is evaluated and it is concluded that these plants provide the earliest record of erect fertile land plants of possible pteridophyte affinity.     

Palaeoecology of Upper Pleistocene-Holocene bryozoan and foraminiferal assemblages from Ku?dili (Kadiköy, Istanbul, Turkey)

Bryozoan and foraminiferal assemblages from a core drilled in the Kusdili (Kadiköy, Istanbul) Upper Pleistocene-Holocene sequence were studied. Assemblages are absent from the very basal and top parts but they are well represented all along the middle part of the sequence. All the species found presently live in the Mediterranean. In the area sedimentation seemingly started about 13?000 years ago in very shallow near-shore environments with the deposition of pebbly sediments rapidly evolving to mud. Near the base, the presence of erosional surface allows to recognize three successive sedimentary cycles. Bryozoan and foraminiferal assemblages found in the middle part of the sequence testify to a shallow water, estuarine or lagoonal paleo-environment, in which effects of low salinity waters, more obvious toward the top, could be related to the reestablishment of a connection between the Marmara Sea and the Black Sea through the Bosphorus, about 7000 years BP.     

内镜黏膜下剥离术和挖除术治疗上消化道肿瘤的疗效及安全性分析

目的:分析内镜黏膜下剥离术(ESD)和黏膜下挖除术(ESE)治疗上消化道肿瘤的疗效及安全性。方法:回顾性分析2017年1月至2019年4月我院消化内科接受ESD或ESE治疗的68例上消化道肿瘤住院患者的临床资料,收集患者基础疾病、手术时间、病变部位大小、整块切除率、并发症等资料,同时采用Logistic回归分析对术中穿孔进行危险因素分析。结果:64例患者完整切除瘤体(94.12%),肿瘤平均直径(16.98±8.29)mm。食管病灶病理类型以高级别上皮内瘤变为主,有15例(22.06%);胃部病灶分布以胃体、胃底和胃窦居多,分别有18例(26.47%)、16例(23.53%)和12例(17.65%),病理类型以间质瘤最多,占36.76%;11例患者发生并发症(16.18%),4例患者出现术后出血(5.88%),经过内镜下止血后好转,8例患术中穿孔(11.76%),均行内镜下尼龙绳联合钛夹行荷包缝合,其中1例患者术中穿孔合并术后迟发性出血;病灶最大直径(≥25 mm,P=0.036)和病灶部位(胃底,P=0.015)是导致ESD或ESE术中穿孔的独立危险因素。结论:ESD和ESE治疗上消化道肿瘤安全有效,但需注意病灶大小和胃底病变,因其是导致术中穿孔的独立危险因素。     

内蒙古上白垩统二连组发现一新镰刀龙类(英文)

镰刀龙类化石主要分布于亚洲白垩纪地层 (RussellandDong ,1 993;Xuetal.,1 999a ;KirklandandWolfe ,2 0 0 1 )。最近发现于内蒙古上白垩统二连组的杨氏内蒙古龙(Neimongosaurusyangi)代表这一类群中较为原始的属种 (张晓虹等 ,2 0 0 1 )。通过研究产自同一化石地点的镰刀龙类新材料 ,我们鉴定出一个不同于杨氏内蒙古龙的新属种 ,美掌二连龙(Erliansaurusbellamanusgen .etsp .nov.)。依据以下特征将Erliansaurusbellamanus归入镰刀龙超科 :肩胛骨干远端狭窄、肱骨近端角状、肱骨有后转子、肱骨的尺骨髁和桡骨髁位于肱骨干前部、肠骨髋臼后支远端加厚、距骨髁小和腓骨近端后缘窄。Erliansaurusbellamanus的以下自近裔特征区别于其他镰刀龙类 :前部尾椎具加大的滋养孔、肱骨后转子嵴状、肱骨后转子内侧有一卵形凹陷、肠骨外侧面坐骨柄上方有一多皱的肿状突起、腓骨近端后缘明显高于前缘以及腓骨前转子大、位置靠远端。本文对镰刀龙类的系统关系进行了初步的分析 ,结论如下 :北票龙 (Beipiaosaurus)代表除Eshanosaurus外最原始的属种 ,它没有以下一些其他镰刀龙类的进步性状 :掌爪近端深、胫骨短于股骨、非常短的骨以及第一骨关连跗骨。Erliansaurus、Alxasaurus、Neimongosaurus和Nothronychus比Bei     

Vegetation of the Lago de Sanabria area (NW Iberia) since the end of the Pleistocene: a palaeoecological reconstruction on the basis of two new pollen sequences

Various pollen sequences from lacustrine deposits close to Lago de Sanabria (NW Iberia) have for several decades been a key source of information for palaeoenvironmental reconstructions of SW Europe, though their interpretation has been the subject of some controversy. Here we present two new pollen sequences obtained from this area, and a new palaeoenvironmental reconstruction of the region. The available pollen data reach back to before 18,000 b.p., a period of very harsh climate with seasonal (non continuous) sedimentation and a landscape characterised by herbaceous formations dominated by Gramineae and Artemisia, and scrub formations dominated by Ericaceae and Cistaceae. Subsequently sedimentation became continuous, and various regional forest expansions are apparent. At a local level, the first forest expansion began about 12,000 b.p., when Betula pollen reached 70% followed by peaks in Pinus sylvestris-type (>80%) and Quercus robur-type (40%). The Younger Dryas saw a retreat of woodland formations in the area around the lake, with broadleaved deciduous woodland (largely oak) retreating at mid and low altitudes, but with pine woodland persisting in more sheltered sites. The climatic improvement in the Early Holocene favoured re-expansion of woodland, dominated by Pinus sylvestris-type at higher and Quercus robur and Q. pyrenaica at lower altitudes, until anthropogenic deforestation commenced around 4,000 b.p. The disappearance of natural pine woodlands in this region is probably largely attributable to human interference.     

Early Silurian (Telychian) rugose coral fauna of Daguan area, northeast Yunnan province, China

Study on rugose coral fauna of the Sifengya Formation (early Telychian) and Daluzhai Formation (mid-late Telychian) in Daguan area, northeast Yunnan Province, China was carried out. Rugose coral fauna of the Sifengya Formation included 18 genera and 34 species, while Daluzhai Formation with nine genera, ten species. We described rugose coral fauna (12 genera, 19 species) including one new genus and five new species, i.e. Protoketophyllum daguanense gen. et sp. nov., Crassilasma huanggexiense sp. nov., Pseudophaulactis heae sp. nov., P. convolutus sp. nov., and Shensiphyllum minor sp. nov. The characteristics and geological significance of rugose coral fauna of Sifengya Formation and Daluzhai Formation were analyzed. Particularly, rugose coral fauna of the Sifengya Formation represent early Telychian rugosan fauna in the Upper Yangtze region and improve the sequences of early Silurian (Llandovery) rugose coral assemblages in Yangtze region. It is therefore very meaningful to further analyze radiation period of rugose coral fauna in such epoch. __________ Translated from Acta Palaeontologica Sinica, 2005, 44(2): 229–246 [译自: 古生物学报, 2005, 44(2): 229–246]     

Nitrogen transported to three Gorges Dam from agro-ecosystems during 1980–2000

To evaluate the effect of human activities on the amount of nitrogen (N) transported to the Three Gorges Dam (TGD), we have developed and applied a model to estimate the riverine N transport from watersheds draining into the upper Changjiang River basin. By using this model and a database of agricultural statistics, we study the temporal and spatial changes in N inputs to watersheds and surface waters. The total amount of N transported to the surface drainage waters from the agro-ecosystem in 2000 showed a 2.9-fold increase over that in 1980. Considering a constant (37%) loss rate from the river, the annual amount of N transported to the TGD from the agro-ecosystem of the Changjiang river upper basin was about 0.35 × 10⁶, 0.47 × 10⁶, 0.59 × 10⁶, 0.64 × 10⁶ and 1.01 × 10⁶ t in 1980, 1985, 1990, 1995, and 2000, respectively. Further, the transported amount of new anthropogenic reactive N approximately quadrupled in 2000, while the amount of riverine N due to rural human waste varied slightly. Of the total N transported to surface drainage waters in 10 watersheds in 2000, the Jialingjiang watershed accounted for 35%; the TGD region, 15%; and the Toujiang, Wujiang and Minjiang watersheds, 11% each. In 1980, the N sources were concentrated in the rural areas surrounding Chendu City and Chongqing City; however, these sources considerably expanded in the 1990s. The increased use of synthetic fertilizers and the decrease in the fertilizer N-use efficiency are implicated as major causal factors of increased riverine N transport; the calculated amount of N transported to the main tributaries agrees well with previously reported data.