The main types of biomorphic microstructures from black carbonate shales of the Sinsk formation (Lower Cambrian) of the Siberian platform are described. The possibility of the thin-layered part of the Sinsk formation being the vitally buried remains of cyanobacterial mat is discussed.
IOS Press, Inc.
6751 Tepper Drive
Clifton, VA 20124
Tel.: +1 703 830 6300
Fax: +1 703 830 2300 firstname.lastname@example.org
(Corporate matters and books only) IOS Press c/o Accucoms US, Inc.
For North America Sales and Customer Service
West Point Commons
Lansdale PA 19446
Tel.: +1 866 855 8967
Fax: +1 215 660 5042 email@example.com