On the Occurrence of Sublepidodendron,a Lepidodenroid Plant from the Wutung Formation

正 The recent finding of plant-remains in the Hsiashan series adds an important chapter to the Carboniferous stratigraphy in the province of Kiangsi. This formation is certainly very widely distributed in the central and southern parts of the province, and has been hitherto considered to be Devonian     

On the Type Species of Chusenella

正 DIAGNOSIS: Test fusiform, slightly rounded at the ends; about 11.2 mm. long, 3.7 mm. wide, giving an axial ratio of about 1:3; whorl 9 to 10, the first three or four volutions closely coiled thence gradually evolute; spiral wall increases in thickness as the test grows, being 0.016 mm. in the firs     

On two New Fossil Fishes from Southwestern China

Among many other important discoveries of vertebrate palacontology made inthe past few years,a few remains of fish afford special interest.In W Kunming,Yunnan,remains of Hybodus were found which represent the second knownshark in China.In Weiyuan,Szechuan,a dental plate of Ceratodus has beendiscovered,which is so far the only record of this interesting fish in China.Both are described in the following lines.     

On the Occurrence of Gigantopteris-Flora in Kwangsi

The geological and geographical distribution of the genus Gigantopteriswas first summarized by Yabe in 1917. Fourteen years later Yoh published alist of 20 localities distributed in different provinces in China known at that timenamely Hunan, Shansi, Liaoning, Kiangsi, Fukien, Chekiang, Anhui, Yunnan     

ber ein Vorkommen von Ullmannia aus dem Perm in Kwangsi

Die Seltenheit oder Abwesenheit der Conifer-Reste in dem Perm von Ostasienist nach wie vor bemerkenswert. In dem so reichhaltigen Material der ShihhotzcSerie in Shansi, ist noch keine Spur (Vgl. Halle 1927, S. 263, 264, 267) oder nurunsicherer Rest (Sze 1935, S. 575) davon gefunden worden. Erst in 1933 hatte ichin P. L. Yuan's Sammlung von Sinkiang einige schlecht erhaltene Conifer-Zweige     

ADDITIONAL DICYNODONTIA REMAINS FROM SINKIANG

Since my first publication on the remains of Dicynodontia dis-covered by Prof.Yuan in Sinkiang between 1927 and 1930~1 a few morespecimens,collected during the same period and in the same general area,have been kindly handed to me by Prof.Yuan for study (April 1937).     

ber einige mesozoische Flora von Hsiwan(Kwangsi)

Seit der Publikation der Arbeit von Dr.S.S.Yoh(1933 a.a.0.)wurdendie Kohlenf(o|¨)hrenden Schichten in Hsiwan~1 im allgemeinen als Unter-karbon oder Kulm angeh(o|¨)rig betrachtet.So hat auch der Verfasser vor     

UPPER CAMBRIAN OF KAIPING BASIN.

The Cambrian of China is developed in Yunnan, Shantung, Chihliand Manchuria. The first collection of Cambrian fossils was made by VonRichthofen and described by Dames and Kayser. Dames studied thetrilobites and Kayser described the brachiopods.     

STRATIGRAPHY AND PAL?EONTOLOGY OF THE SINIAN ROCKS OF NANKOU

INTRODUCTION The Sinian rocks in China as far as we know are most well developedin Chihli and Shansi provinces. In Chihli, they are usually restricted to theupper part, as in Ta Yang, Pei Yu, Hsia Ma Ling, Ching Pei Kou and other     

SOME CORRELATIONS BETWEEN THE GEOLOGY OF CHINA PROPER AND THE GEOLOGY OF MONGOLIA

During the summer of 1930 we had. thanks to the Central Asiatic Expedition led by Dr. R.C. Andrews, a splendid opportunity for studying the geological formations of SE. Gobi, along the Kalgan-Urga trail, South and