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Neoproterozoic Ediacaran References

 

 

Ediacaran (Vendian) References

References

Aitken, JD (1988), First appearance of trace fossils in Mackenzie Mountains, northwest Canada, in relation to the highest glacial deposits and lowest small shelly fossils, in E Landing, GM Narbonne & P Myrow [eds.],Trace Fossils, Small Shelly Fossils and the Precambrian-Cambrian Boundary. N.Y. State Mus. Bull. No. 463: 8.

Anderson, MM (1978), Ediacaran fauna, in DN Lapedes (ed.), Yearbook of science and technology.  McGraw-Hill, p. 146–149.

Aitken, JD (1989), Uppermost Proterozoic formations in central Mackenzie Mountains, Northwest Territories. Geol. Survey Can. Bull. No. 368. 

Ayala, FJ, A Rzhetsky & FJ Ayala (1998), Origins of the metazoan phyla: molecular clocks confirm paleontological estimates Proc. Natl. Acad. (USA) 95: 606-611

Benus, AP (1988), Sedimentological context of a deep-water Ediacaran fauna (Mistaken Point, Avalon Zone, eastern Newfoundland), in E Landing, GM Narbonne & P Myrow  [eds.], Trace fossils, small shelly fossils and the Precambrian-Cambrian boundary: N.Y. State Mus. Bull. No. 463: 8-9.

Bergström, J (1990), Precambrian trace fossils and the rise of bilaterian animalsIchnos, 1: 3-13.

Bowring, SA & DH Erwin (1998), A new look at evolutionary rates in deep time: Uniting paleontogy and high-precision geochronologyGSA Today 8:1-8.

Brasier, MD (1992), Introduction. Background to the Cambrian ExplosionJ. Geol. Soc. Lond. 149: 585-587.

Brasier, M, O Green & G Shields (1997), Ediacaran sponge spicule clusters from southwestern Mongolia and the origins of the Cambrian faunaGeology 25: 303-306

Briggs, DEG, DH Erwin & FJ Collier (1994), The Fossils of the Burgess Shale.  Smithsonian Inst. Press, 238 pp. 

Clarkson, ENK (1993), Invertebrate Palaeontology and Evolution [4th ed.]. Chapman & Hall, 434 pp. 

Conway Morris, S (1998), The Crucible of Creation. Oxford Univ. Press. 

Cowie, JW & MD Brasier [eds.] (1989), The Precambrian-Cambrian Boundary. Clarendon Press. 

Crimes, TP & D McIlroy (1999), A biota of Ediacaran aspect from lower Cambrian strata on the Digermul Peninsula, Arctic NorwayGeol. Mag. 136: 633-642. 

Crimes, TP A Insole & BJP Williams (1995) A rigid bodied ediacaran biota from Upper Cambrian strata in Co. Wexford, Eire.  Geol. J. 30: 89-109. 

Dzik, J & AY Ivantsov (1999), An asymmetric segmented organism from the Ediacaran of Russia and the status of the DipleurozoaHist. Biol. 13: 255-268. 

Erwin, DH & EH Davidson (2002), The last common bilaterian ancestorDevelopment, 129, 3021-3032.  

Farmer, J, G Vidal, M Modeczydłowska, H Strauss, P Ahlberg & A Siedlecka (1992), Ediacaran fossils from the Innerelv Member (late Proterozoic) of the Tanafjorden area, northeastern FinnmarkGeol. Mag. 129: 181-195.  (Modeczydlowska) 

Fedonkin, MA & BM Waggoner (1997), The Late Precambrian fossil Kimberella is a mollusc-like bilaterian organismNature 388: 868-871.

Gehling, JG (1987), Earliest known echinoderm -- a new Ediacaran fossil from the Pound Subgroup of South AustraliaAlcheringa 11: 337-345. 

Gehling, JG (1991), The case for Ediacaran fossil roots to the metazoan treeMem Geol. Soc. India 20: 181-223. 

Gehling, JG (2001), Evolution, environment and provinces of the Ediacara biota: Toward a subdivision of the terminal Proterozoic. Geol. Assoc. Can. Min. Assoc. Can. Abstr. 26: 50.

Gehling, JG & JK Rigby (1996) Long expected sponges from the Neoproterozoic Ediacara fauna of South Australia. J. Paleontol., 2: 185-195.

Gehling, JG, GM Narbonne & MM Anderson (2000) The First Named Ediacaran Body Fossil, Aspidella terranovicaPalaeontology 43: 427-456.

Glaessner, MF (1961), Pre-Cambrian animals, in The Fossil Record and Evolution: Readings from Scientic American. WH Freeman & Co., pp. 63-69.

Glaessner, MF & M Wade (1966), The Late Precambrian fossils from Ediacara, South AustraliaPalaeontology 9: 599-628.

Grotzinger, JP, SA Bowring, BZ Saylor & AJ Kaufman (1995), Biostratigraphic and geochronologic constraints on early animal evolutionScience, 270: 598-604.

Grotzinger, JP, W Watters, AH Knoll & O Smith (1998), Diverse Calcareous Fossils from the Ediacaran-Age Nama Group, Namibia.  Abstracts with Programs, Geol. Soc. Amer. 20:  A-147.

Gürich, G (1933), Die kuibis fossilen der Nama-Formation von Sudwestafrika. Paläontol. Zeit. 15: 137-154. 

Hagadorn, JW (1998), Restriction of a Late Neoproterozoic Biotype. Unpub. PhD diss., Univ. Southern Calif., Los Angeles.

Hagadorn, JW, CM Fedo & BM Waggoner (2000), Early Cambrian Ediacaran-type fossils from CaliforniaJ. Paleont. 74: 731-740. 

Hahn, G, R Hahn, OH Leonardos, HD Pflug, & DHG Walde (1982), Körperlich erhaltene Scyphozoen- Reste aus dem Jungpräkambrium BrasiliensGeol. Palaeont. 16: 1- 18.

Hofmann, HJ, GM Narbonne & JD Aitken, JD (1990) Ediacaran remains from intertillite beds in northwestern Canada. Geology 18: 1199–1202.

Hoffman, HS, J Hill & AF King (1979), Late Precambrian microfossils, southeast Newfoundland, in Curr. Res. Pt. B, Geol Surv. Can. 79-1B: 83-98.

Ivantsov, AY (2001) [Иванцов, АЮ], Vendia and other Precambrian "Arthropods" [Vendia и другие докембрийские "Артроподы"].  Paleont. Zh. [Палеонтол. журн] № 4. С. 3-10.

Jenkins, RJF (1981), The concept of an ‘Ediacaran Period’ and its stratigraphic significance in Australia Trans. R. Soc. S. Aus. 105: 179-194.

Jensen, S, JG Gehling & ML Droser (1998) Ediacara-type fossils in Cambrian sedimentsNature 393: 567–569.

Kerr, RA (2002), A trigger for the Cambrian Explosion?  Science 298: 1547.

King, AF (1980), The birth of the Caledonides: Late Precambrian rocks of the Avalon Peninsula, Newfoundland and their correlatives in the Appalachian - Caledonian Orogen [in DR Wones (ed.), The Caledonides in the U.S.A.] Dept. Geol. Sci, Va. Polytech. Univ. Mem. 2: 3-8.

Knoll, AH & SB Carroll (1999), Early animal evolution: Emerging views from comparative biology and geologyScience 284: 2129-2137.  

Knoll, AH, M Walter, G Narbonne & N Christie-Blick, (2000), The Ediacaran Period: A New Addition to the Geologic Time Scale., Unpubl. Report of the Terminal Proterozoic Subcommission of the International Commission on Stratigraphy.  35 pp. (including dissenting comments) WWW (accessed 050831).    

Kouchinsky, A & S Bengston (2002), The tube wall of Cambrian anabaritidsActa Pal. Pol. 47: 431–444.

Langille, GB (1974), Earliest Cambrian - Latest Proterozoic ichnofossils and problematic fossils from Inyo County, California. Unpub. Ph.D. thesis. State University of New York, Binghamton, 194 pp. 

Li, C-W, J-Y Chen, & T-E Hua (1998), Precambrian sponges with cellular structuresScience 279: 879 - 882.

Martin, MW, DV Grazhdankin, SA Bowring, DAD Evans, MA Fedonkin, & JL Kirschvink (2000), Age of Neoproterozoic bilaterian body and trace fossils, White Sea, Russia: Implications for metazoan evolutionScience 288: 841-845.

McMenamin, MAS (1986), The Garden of Ediacara. Palaios 1: 178-182.

McMenamin, MAS (1996), Ediacaran biota from Sonora, MexicoProc. Nat. Acad. Sci USA 93: 4990-4993.  

McMenamin, MAS (1998)The Garden of Ediacara.. Columbia Univ. Press. 

Moczydlowska M & TP Crimes (1995), Late Cambrian acritarchs and their age constraints on an Ediacaran-type fauna from the Booley Bay Formation, Co. Wexford (Eire)Geol.. J., 30:  111-128.

Mooi, R (2001), Not all written in stone: Interdisciplinary syntheses in echinoderm paleontologyCan. J. Zool. 79: 1209-1231.

Narbonne, GM & JG Gehling (2003), Life after snowball: The oldest complex Ediacaran fossils. Geology, 31: 27-30.

Nielsen, C (2001), Animal Evolution: Interrelationships of the Living Phyla [2nd ed.], Oxford Univ. Press.  568 pp.

Peterson, KJ & EH Davidson (2000), Regulatory evolution and the origins of the bilaterians. Proc. Nat. Acad. Sci USA 97: 4430-4433.

Peterson, KJ, B Waggoner & JW Hagadorn (2003), A fungal analog for Newfoundland Ediacaran fossils?  Integr. Comp. Biol., 43: 127–136.  

Pflug, HD (1972), Zur fauna der Nama-Schichten in Sadwest-Afrika, III. Erniettomorpha, Bau und systematische Zugehorigkeit. Palaeontographica A 139: 134-170.

Runnegar, B (1992), Evolution of the earliest animals in JW Schopf (ed.) Major Events in the History of Life.  Jones & Bartlett.

Runnegar, B (2000), Loophole for Snowball EarthNature 405: 403-404.

Runnegar, B & MA Fedonkin (1992), Proterozoic metazoan body fossils,. in JW Schopf & C Klein (eds.), The Proterozoic biosphere: A Multidisciplinary Study. Cambridge, 1: 369-388.

Seilacher, A (1984), Late Precambrian and Early Cambrian Metazoa: preservational or real Extinctions? in HD Holland & AF Trendall [eds.], Patterns of Change in Earth Evolution.  Springer Verlag, pp. 159-168. 

Seilacher, A (1989), Vendozoa: organismic constructions in the Proterozoic biosphereLethaia, 22: 229-239.

Seilacher, A (1992), Vendobionta and Psammocorallia: lost construction of Precambrian evolution. J. Geol. Soc. 149: 607-613.

Seilacher, A, M Meschede, EW Bolton & H Luginsland (2000), Precambrian "fossil" Vermiforma is a tectographGeology 28: 235 - 238.

Sokolov, BS (1952), [On the age of the old sedimentary cover of the Russian Platform] Izvest. Akad. Nauk SSSR, Ser. Geol. 5: 21-31.

Sokolov, BS & Fedonkin, MA (1984) The Vendian as the terminal system of the PrecambrianEpisodes 7: 12-19.  

Valentine, JW (1995), Late Precambrian bilaterians: Grades and clades, in WM Fitch & FJ Ayala [eds.], Tempo and Mode in Evolution: Genetics and Paleontology 50 Years After Simpson. Nat. Acad. Sci. 87-107. 

Walker, G (2003), Snowball Earth. Crown Group: 269 pp.

Walter, MR, R Elphinstone & GR Heys (1989), Proterozoic and Early Cambrian trace fossils from the Amadeus and Georgina Basins, central AustraliaAlcheringa, 13: 209-256.

Wray, GA, JS Levinton & LH Shapiro (1996), Molecular evidence for deep Precambrian divergences among metazoan phylaScience 274: 568 - 573.

Notes

[1] Ask any Texan, even your normally urbane and cosmopolitan host, about the Middle East.  We will be happy to share our knowledge of the fabled realms of Eye-Rak, Gutter (Qatar), Sow-Dee, Jawd'n (1 syllable), and Iz-rul.  

[2]  This requires a little explanation.  Refer to the figure in Knoll et al. (2000).  As we hinted, there is a separate glaciation event which shows up in some exposures and dates to between 600 and 580 My.  Some of the Twitya trace fossils apparantly occur below the tillite associated with this Ice Age, which some call the Marinoan.  So far as we are aware, no one claims to have found metazoans from a level below the Ediacaran GSSP.  


 

page uploaded 15 May 2002
unless otherwise indicated, content © Chris Clowes 2002 (last updated: 3 Mar 2002)
checked ATW051008, edited RFVS111126