Zhn-sheng Ji, Jin-xin Yo, Gui-chun Wu,*, Qin Sun, Qiu-yun Shi, Ho Li, Ji-fu He,Sho-wen Zhng

a Chinese Academy of Geological Science, CAGS, Beijing 100037, China

b Institute of Geology, CAGS, Beijing 100037, China

1. Objectives

The western Gangdese in Tibet during Triassic was previously considered to be a part of the Gangdese Oldland(Zhao ZZ et al., 2001; Fig. 1). If the Gangdese Oldland did exist, it means no prospect of petroleum exploration of the Triassic strata in western Gangdese area. Fortunately, the recent biostratigraphic progresses don’t support the existence of the Gangdese Oldland. This paper aims to briefly introduce the new paleogeographic interpretation and the reason that the western Gangdese in the Triassic was marine instead of terrigenous on the basis of the recent conodont data.

2. Methods

The logic link of denying such a vast land as the Gangdese Oldland by discovering such tiny fossils as conodonts is based on the following geological principles. The first is the paleogeographic principle that the existence of an ancient land is interpreted by the absence of strata. The second is the sedimentologic principle that limestone or dolomite containing marine fossils were accumulated in an environment of carbonate platform or slope. The third is the stratigraphic principle that the existence of a certain-age strata is determined by the existence of its index fossils.

Conodonts, the index fossils for the marine strata from Middle Cambrian up to Late Triassic, played a critical role in the denying of the Gangdese Oldland. The conception of the Gangdese Oldland was established on the stratigraphic cognition that the Triassic strata did not deposit. If the above stratigraphic understanding is true, there is no chance to find Triassic conodonts. On the contrary, if Triassic conodonts were discovered, it suggests the existence of the Triassic marine strata. If the Triassic marine strata are found anywhere in the scope of the Gangdese Oldland, the conception of the Gangdese Oldland will be proved to be incorrect.Furthermore, the paleoenvironment of the related area of the Gangdese Oldland should be reinterpreted by the lithologic facies of the strata yielding Triassic conodonts.

3. Results

The conception of the Gangdese Oldland was first questioned by the discovery of the typical Late Triassic Norian conodont Epigondolella specimens in the so-called Middle Permian Xiala Formation at the Dibu Co section which is located in the middle west of the Gangdese Oldland by Ji ZS et al. in 2006. The above conodont data suggest the existence of the Late Triassic Norian carbonate sediments over there. The carbonate sediments suggest its environment probably was carbonate platform or slope, but never land as thought before. It is the first evidence to collapse the conception of the Gangdese Oldland. More conodont samples were collected and checked in the so-called Middle Permian Xiala Formation limestone nearby the Dibu Co section to verify its reliability. Inspiringly, not only Late Triassic conodonts are found repeatedly but also abundant Early and Middle Triassic conodonts were found (Fig. 2). Neogondolella carinata zone, Neospathodus triangularis - N. homeri zone, Chiosella timorensis zone, Paragondolella inclinata -P. polygnathiformis zone and Epigondolella zone, ranging from the Early Triassic to Late Triassic, could be recognized in ascending order.

術(shù)后第6天，轉(zhuǎn)至我院治療，患者神志模糊，GCS評分 12分（E4V3M5），伴發(fā)熱（38.4℃），專科查體見右外耳道、乳突術(shù)腔干潔，留置紗條1條，無膿性分泌物，耳后傷口干潔。當天腦部CT提示右乳突呈術(shù)后改變；當天血常規(guī)示白細胞升高（10.9×109）;腦脊液示白細胞記數(shù)（35×106/L），紅細胞數(shù)(－)，總蛋白（1.07g/L），葡萄糖（7.14mmol/L）。

Fig. 1.Sections producing Triassic conodonts in the“Gangdese land”(after Zhao ZZ et al., 2001 and references therein).

Fig. 2.Typical conodont specimens found at the Dibucuo section, Coqen County, Tibet. 1-Neospathodus homeri (Bender); 2-Neospathodus triangularis (Bender); 3-Chiosella timorensis (Nogami); 4-Neospathodus conservativus Muller; 5-Neospathodus dieneri Sweet; 6-Neospathodus cristagalli (Huckriede); 7, 8-Neospathodus waageni Sweet; 9–12-Neogondolella carinata (Clark); 13-Budurovignathus sp.; 14, 15-Neogondolella cf. szaboi (Kovacs); 16, 17-Paragondolella inclinata (Mosher); 18-Paragondolella polygnathiformis (Budurov and Stefanov);19-Gladigondolella tethydis (Huckriede); 20-transitional form from Paragondolella inclinata to Paragondolella polygnathiformis; 21,22-Neogondolella bulgarica (Budurov and Stefanov); 23-Paragondolella inclinata (Mosher); 24-Cratognathodus sp.; 25a, 25b-Epigondolella cf. englandi; 26a, 26b-Epigondolella sp.; 27a, 27b-the evolved Epigongdolella serruta Orchard. Scale bar is 400 μm for figures 1-8 and 600 μm for figures 9-30.

In addition, Early Triassic conodonts were discovered at the Mopanshan section and the Zishisang section in the Southern Qiangtang. The Southern Qiangtang has been considered to be the northward extending part of the Gangdese Oldland during Early and Middle Triassic. The Early Triassic conodonts were found in samples taken from the so-called Permian limestone by the geologists of the Guizou Institute of Geological Survey and Jilin Institute of Geological Survey respectively. These data indicate that the marine Triassic deposition spread widely in the so-called Gangdese Oldland.

我國外籍員工招聘主要集中在東部沿海的發(fā)達地區(qū)，其中北京招聘崗位為1 054個；廣東有899個；上海為894個，江蘇595個，浙江500個，排名前五的省市招聘數(shù)量約占全國總量的60%。其中廣東省招聘外籍員工的需求主要聚集在深圳和廣州這兩個國際化都市，兩市占全省招聘數(shù)量的70%。

主動脈瓣狹窄：可見明顯加快的主動脈瓣向速度，患者收縮期最大開放幅度低于16毫米；主動脈瓣關(guān)閉不全：舒張期可見主動脈瓣下返流信號，關(guān)閉間隙不小于2毫米；瓣環(huán)及二尖瓣鈣化：可見明顯增強瓣環(huán)以及二尖瓣回聲，厚度不低于3毫米；主動脈瓣鈣化：主動脈瓣葉僵硬，增厚幅度不小于3毫米，活動明顯受限[3]。

卓時Premier系列Precious月相功能腕表的鑲鉆表耳重現(xiàn)海瑞溫斯頓紐約第五大道旗艦店的拱門造型，令人過目難忘，表圈與表耳共鑲嵌57顆圓形明亮式切工鉆石。 時、分指示及月相功能通過優(yōu)質(zhì)瑞士自動上鏈機械機心驅(qū)動，其動力儲存長達68小時。腕表配備藍色或棕色鱷魚皮表帶，搭配鑲嵌17顆圓形明亮式切工鉆石的白18K金或玫瑰18K金材質(zhì)針扣。

Judging from one site of the Dibu Co area, the authors deduced that there was a vast carbonate platform or slope in the scope of the so-called Gangdese Oldland from Early Triassic to Late Triassic Norian. If this deduction is correct,more locations of the Triassic carbonate sediments could be found in the Gangdese Oldland elsewhere. Checking conodonts in the so-called Middle Permian Xiala formation elsewhere was inspired by the study of the Dibu Co section.

Then more conodont investigations were carried out in other locations to testify the existences of Triassic marine deposition. Inspiring and expectant results were obtained in the following works. Early Triassic conodonts were found at the Langjiu section of the Shiquanhe area in the westmost Gangdese Oldland by Ji ZS et al. in 2007. Late Triassic conodonts were found at the Yawa section by Ji ZS et al. in 2010. Early Triassic conodonts were found at the Wenbudangsang section in the northwest Gangdese Oldland by Wu GC et al. in 2014. Early Triassic conodonts were found both at the Namtso section by Wu GC et al. in 2017 and at the Renduo section by Wu GC et al. in 2018.

In a similar way, the Early and Middle Triassic conodonts indicate that the existence of the Lower and Middle Triassic carbonate sediments and furtherly means its environment in this area was probably carbonate platform or slope in the Early and Middle Triassic too.

4. Conclusions

The newly-discovered conodonts reveal the existence of Triassic carbonate in several outcrops in the western Gangdese region and the southern Qiangtang region. The conception of the Gangdese Oldland should be eliminated for the investigation of conodonts which are typical marine microfossils. These scattered outcrops nowadays suggest the existence of a vast and continuous carbonate platform or slope environment during the Triassic.

For a more detailed discussion and mentioned references in this paper, refer to the summary papers (Ji ZS et al., 2008,2018).

Acknowledgment

This study was supported by National Natural Science Foundation of China (41472030), Basic Research Project of Ministry of Science and Technology of China(2015FY310100), China Geological Survey (DD20160120-02, DD20160120-04 and DD20160126), and Central Publicinterest Scientific Institution Basal Research Fund (J1607).