Genus Micrina (small shelly fossils) from the Lower Cambrian of South Australia: Morphology, microstructures, and possible relation to halkieriids

Paleontological Journal

Volumn 36, Issue 1, 2002, Pages 9-19

  Ushatinskaya, G T ^a  

^a PALEONTOLOGICAL INSTITUTE   (Russian Federation)

Author keywords

[No Author keywords available]

Indexed keywords

MICRINA;

EID: 4344691839     PISSN: 00310301     EISSN: None     Source Type: Journal    
DOI: None     Document Type: Article

References (22)

1. Bengtson, S., The Lower Cambrian Fossil Tommotia, Lethaia, 1970, vol. 3, pp. 363-392.
2. Bengtson, S., Aspects of Problematic Fossils in the Early Palaeozoic, Acta Univ. Upsaliensis, 1977, no. 415, pp. 1-71.
3. Bengtson, S., The Cap-Shaped Cambrian Fossil Maikhanella and the Relationship between Coeloscleritophorans and Molluscs, Lethaia, 1992, vol. 25, pp. 401-420.
4. Bischoff, G.C.O., Dailyatia, a New Genus of the Tommotiidae from Cambrian Strata of SE Australia (Crustacea, Cirripedia), Senckenberg. lethaea, 1976, vol. 57, no. 1, pp. 1-33.
5. Conway Morris, S., Enigmatic Shells, Possibly Halkieriid, from the Middle Cambrian Burgess Shale, British Columbia, Neues Jahrb. für Geologie und Paläontologie Abhandl., 1995, no. 195, pp. 319-331.
6. Convvay Morris, S. and Chapman, A.J., Lower Cambrian (Ninella, Siphogonuchites) from Xinjiang and Shaanxi, China, Geol. Mag., 1996, vol. 133, no. 1, pp. 33-51.
7. Conway Morris, S. and Chapman, A.J., Lower Cambrian Halkieriids and Other Coeloscleritophorans from Aksu-Wushi, Xihjiang, China, J. Paleontol., 1997, vol. 71, no. I, pp. 6-22.
8. Conway Morris, S. and Peel, J.S., Articulated Halkieriids from the Lower Cambrian of North Greenland, Nature, 1990, vol. 345, pp. 802-805.
9. Conway Morris, S. and Peel, J.S., Articulated Halkieriids from the Lower Cambrian of North Greenland and Their Role in Early Protostome Evolution, Phil. Trans. R. Soc. London Ser. B, 1995, vol. 347B, pp. 305-358.
10. Daily, B., The Cambrian in South Australia, in: El sistema Cámbrico su Paleogeografia y el problema de su base 2, Proc. 20th Congr. Geol. Intern. Mexico, 1956, pp. 91-147.
11. Daily, B., The Base of the Cambrian and the First Cambrian Faunas, in: Stratigraphic Problems of the Later Precambrian and Early Cambrian, Centre for Precambrian Research Spec. Pap., 1972, no. 1.pp. 13-42.
12. Demidenko, Yu.E., Skeletal Problematic Fossils from the Lower Cambrian of South Australia, Cand. Sci. (GeoI.-Mineral.) Dissertation, Moscow: Paleontol. Inst. Ros. Akad. Nauk, 1999.
13. Esakova, N.V. and Zhegallo, E.A., Biostratigraphy and Fauna of the Lower Cambrian of Mongolia, Tr. Sovm. Ross.Mongol'. Eksp., 1996, issue 46, pp. 1-214.
14. Fonin, V.D. and Smirnova, T.N., A New Group of Problematic Early Cambrian Organisms and Some Methods of Their Preparing, Paleontol. Zh., 1967, no. 2, pp. 15-27.
15. Laurie, J.R., Phosphatic Fauna of the Early Cambrian Todd River Dolomite, Amadeus Basin, Central Australia, Alcheringa, 1986, vol. 10, pp. 431-454.
16. Qian Yi and Bengtson, S., Palaeontology and Biostratigraphy of the Early Cambrian Meishucunian Stage in Yunnan Province, South China, Fossils and Strata, 1989, no. 24, pp. 1-156.
17. Tate, R., The Cambrian Fossils of South Australia, Trans. Proc. R. Soc. S. Australia, 1892, vol. 15, no. 2, pp. 183-189.
18. Ushatinskaya, G.T., Drevneishye lingulyaty (The Earliest Lingulata), Moscow: Nauka, 1995.
19. Ushatinskaya, G.T., Tannuolinids, in The Cambrian Biostratigraphy of the Stansbury Basin, South Australia, Alexander, E.M., Jago, J.B., Rozanov, A.Yu., and Zhuravlev, A.Yu., Eds., Trans. Palaeontol. Inst., 2001, vol. 282, pp. 117-120.
20. Voronova, L.G., Drozdova, N.A., Esakova, N.V., et al., Iskopaemye nizhnego kembriya gor Makkenzi (Kanada) [Fossils of the Lower Cambrian of the Mackenzie Mountains (Canada)], Moscow: Nauka, 1987.
21. Walcott, C.D., Cambrian Brachiopoda, Monogr. US Geol. Surv., 1912, vol. 51, parts 1 and 2.
22. Williams, A. and Cussack, M., Evolution of a Rhythmic Lamination in the Organophosphatic Shells of Brachiopods, J. Struct. Biol., 1999, vol. 126, pp. 227-240.