珠穆朗玛峰北坡二叠纪动物化石的新资料

在无产阶级文化大革命的推动下,中国科学院西藏科学考察队通过三年(1966-1968)的调查研究,提出了我国西藏珠穆朗玛峰地区的地层系统。他们对该区南部的二叠系合称为色龙群,认为采到的化石属于早二叠世茅口期,可能包括部分晚二叠世龙潭期。同时指出:“至今没有在剖面上发现Gangamopteris植物群”;“对(该区)相当我国南方栖霞期的沉积和相当喜马拉雅西段的Talchir冰碛层,还不清楚”。     

焦作市解放区9家矿山企业全部关停

6月3日,随着老牛河宏丰建材厂、上白作建材厂两家持证到期矿山企业被关停,为焦作市解放区辖区内的持证矿山企业关停工作画上了完美的句号。     

EFFECTS OF DCMU ON CHLOROPHYLL FLUORESCENCE RATIO F685/F735 IN MARINE RED,BROWN AND GREEN ALGAE

The chorophyll fluorescence ratio F685/F735 in vivo can be a useful indicator for stress detection inhigher plants and seaweed. DCMU [3 - (3, 4 - dichlorophenyl ) - 1, 1 - dimethylurea] treatment influencesthis ratio. Th effects of DCMU on F685/F735 of marine red, brown and green algae under excitationlight of different wavelengths were investigted. In the brown algae, Laminaria japonica and Undariapinnatifida,DCMU did not increase this ratio under blue light excitation but increased the ratio slightlyunder excitation by green light. For the red algea, Halymenia sinensis, DCMU increased the ratiomarkedly under both blue and green ligh excitation. The percentage increase could reach 50% (undergreen light excitation) and was due to unequal enhancement at the two emission maxima by DCMU. Afraction of chlorophyll which contributed to fluorescence in the 735 nm region was less sensitive toDCMU and was likely from photosystem I of red algae. In the green alga, Ulva pertusa, DCMU causeda slight increase in F685     

全球上二叠统的年代对比

上二叠统记录着地质历史上最大的生物灭绝事件和最深刻的环境变化。长期以来由于世界各主要沉积区晚二叠世地层的同期性未能确定 ,对这一事件及其过程难以全面了解。随着乐平统成为全球上二叠统的标准 ,我们选用若干生物地层、磁性地层和层序地层等的联接点 ,提出乐平世地层世界对比的试用方案