| [1] |
(1)Маслов,В.П.,1973,Атлас породовразуюших организмов (Известквы х и Кре-мневых) Издательство 《Нзука》 Москва. Р9-14. (2)Лучинина, В. А., 1975,Лалеоальгическая характеристнка ранне го Кем-брия Сибирской платформы. Издательство 《Наука》Сибирское отде ление р14-16 (3)Wray，J .L.，1977, Calcareous algae .In Develop menbs in Palaeontology and Stratigraphy 4.Elsevier Scientific Publishing Company，Amsterdam，P 40-42. (4)Johnson, J.H.，1966, A review of the Cambrian algae.Q uarterly of the C olo- rado school of Mines, V.61, No.1. (5)Riding，R.and Toomey，D.F.，1972, The sedimentological role of Epaphyton and Rtenaaei in Lower Ordovician mounds, Southern Oklahoma.J.Palent，V. 46, M o.4, P509-519. (6)KopAs.K.s.，1975, Bouopocnx KeM6pxa.H3uaxenacrao 《Hayka》Mocxsa. (7)Lees, A.，1975, Possibe influence of salinity and to m perature on m odern shelf carbonate sedimentation.Marine Geology, V.19, No.3, P 159-198. (8)Seslavinskiy, K.B.，1979, Ordovician and Silurian climates and global climat- is belts. International geology revie w，V.21, No. 2, P 140-152. |