Kirschvink J.Late Proterozoic low-latitude global glaciation: the snowball earth[A].In: SchopfJ W,Klein C(eds).The Proterozoic Biosphere[C].Cambridge University Press,1992.51~52.
[2]
Hoffiman P,Schrag.The snowball earth hypothesis: testing the limits of global change[J].Terra Nova,2002,14: 129~155.
[3]
Barfod G H.New Lu-Hf and Pb-Pb age constraints on the earliest animal fossils[J].Earth Plauet.Sci.Lett.,2002,201: 203~212.
[4]
Zhang Q,Piper J D A.Paleomagnetic study of Neoproterozoic glacial rocks of the Yangzi block: Paleolatitude and configuration of South China in the late Proterozoic Supercontinent [J].Precamb.Res.,1997,85: 173~199.
[5]
Macouin M,Besse J,Ader M,et al.Combined paleomagnetic and isotopic data from the Doushantuo carbonate,South China: implication for the "Snowball Earth" hypothesis[J].Earth Planetary Science Letters,2004,in press.
[6]
Zhou C,Tucker R,Xiao S,et al.New constraints on the ages of Neoproterozoic glaciations in south China[J].Geology,2004,32(5):437~440.
[7]
Sohl L E,Christie-Blick,Kent D.Paleomagnetic polarity reversals in Marinoan (ca.600Ma) glacial deposits of Australia: implications for the duration of low-latitude glaciation in Neoproterozoic time[J].Geological Society of America Bulletin,1999,111:1120~1139.
[8]
Evans D A D.Stratigraphic,geochronological,and paleomagnetic constraints upon the Neoproterozoic climatic paradox[J].American Journal of Science,2000,300: 347~433.
[9]
Yang Z,Sun Z,Yang T,et al.A long connection (750-380Ma) between South China and Australia: paleomagnetic constraints[J].Earth Planetary Science Letters,2004,220: 423~434.
[10]
Yin C,Liu D,Gao L,et al.Lower boundary age of the Nanhua System and the Gucheng glacial stage: Evidence from SHRIMPII dating[J].Chinese Science Bulletin,2003,48: 1657~ 1662.