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Journal of the Geological Society Journal of the Geological Society Discussion on Ordovician palaeogeography of Siberia and adjacent continents Journal of the Geological Society 1996; v. 153; p. 329-330 doi: 10.1144/gsjgs.153.2.0329 Email alerting click here to receive free e-mail alerts when new articles cite this article service Permission click here to seek permission to re-use all or part of this article request Subscribe click here to subscribe to Journal of the Geological Society or the Lyell Collection Notes Downloaded by on January 24, 2012 © Geological Society of London 1996 Journal of the Geological Society, London, Vol. 153, 1996, pp. 329-330. Printed in Northern Ireland Discussion on Ordovician palaeogeography of Siberia and adjacent continents Journal, Vol. 152, 1995, pp. 279-287. Ian W. D. Dalziel & Luis H. Dalla Salda write: In their Ordovician times and the total absence of glaciogenic strata interesting paper on ‘Ordovician paleogeography of Siberia of that age from its craton, this indicates thatthe and adjacentcontinent’, Torsvik etal. (1995) comment on Precordilleran terrane was transferred to Gondwana during the hypothesis of possible Laurentia-Gondwana collision the Ordovician Period (Dalziel 1993; Dalziel et al. 1994) as during the Ordovicianput forward by DallaSalda et al. also concluded in arecent biostratigraphic analysis of the (1992a, b) and amplified by Dalziel et al. (1994). Torsvik Precordillera and the Appalachians (Astini et al. 1995). and his colleagues agree with us that the palaomagnetic data Finally, we would like to point out that the ‘alternative do permit our ‘alternativepalaogeographic approach’ of approach’ to Ordovician palaeogeography explains much juxtaposition and collision between the twocontinental about North American geology south of New England, and masses in mid-Ordovician times as well as their ‘archetypal’ about western South America, that the ‘archetypal scenario’ scenario with its 3000-4500 km of interveningoceanic doesnot even address. Here we refer inter alia tothe lithosphere (Torsvik et al. 1995, p. 284 and figs lld-f). We otherwise puzzling apparent truncation of the Taconic appreciate theirtaking time to analyse our approach, and orogen in Georgia and Alabama, the origin of the Ouachita would like to comment briefly on theirobjections toour embayment, the Laurentian fauna of the Precordillera, the model. nature andnorthward termination of theFamatinian (1) Our ‘tight fit’ of Laurentiaand Gondwanafor orogen, and the mid- to late Palaeozoic initiation of Andean mid-Ordovician times (Dalziel et al. 1994, fig. 3) is said to orogenesis. We submit that the new approach, springing indicate‘unabridged faunal exchange’ between the two from the hypothetical role of Laurentia as the ‘keystone’ of continents that is not supported by the marine faunal data the early to mid-NeoproterozoicRodinian supercontinent (Torsvik et al. 1995, p. 285). In fact we propose not just a (for review see Dalziel 1995), offers answers without tight fit, but Alpine-style continent-continent collision. The seriously violating the basic premises on which the more presence of latitudinala mountain range thousands of traditional one is based. kilometres long and of Alpineproportions, is hardly 10 July 1995 compatible with exchange of marinefaunas between the juxtaposed continents. (2) Faunas indicative of ‘deep margins’ in the early Ordovician are implied to contradict our model (p. 285). Yet T. H. Torsvik, J. Tait, V. M. Moralev, W. S. McKerrow, B. India and Asia were separated by deep water until just prior A. Sturt & D. Roberts reply: On theSouth American to their collision, and the presently colliding Australia and craton, the early Palaeozoic rocks show facies consistent Asia are still in part separated by the nearly 6000m deep with cold waterenvironments: generally clastic sediments North Australia Basin. with low diversity faunas. By contrast, the distribution of (3) The fact that the Taconic Orogeny in the Canadian the Palaeozoic rocks in theAndean orogen is clearly Maritimes and New England involved arc-continent complex; many different warm and cold water facies occur in collision in no way precludes the involvement of a second adjacent exposures suggesting that sequences, once depos- continentas stated (p. 285). A Laurentia-Gondwana ited far apart, are now adjacent (Ramos et al. 1986). Some collision would unquestionably have been as complicated as of the Andeanterranes have facies andfaunas closely the Alpine collision between Europeand Africa orthe comparably with North America, while others have affinities present Australia-Asia collision, with several arcs, back-arc with Gondwana (exactly analogous with the exotic Permian basins, aseismic ridges, and interveningmicrocontinental and Mesozoic facies of the far-travelledterranes in the fragments involved. Althoughnot apparent in fig. lle of Western Cordillera of North America). These facts do not Torsvik et al., the geometry of the suggested mid-Ordovician lead us to change the views expressed previously (Torsvik et collision (controlled by the Taconic and Famatinian piercing al. 1995). points) leaves Newfoundland and New England outside the It is important that this theme is fully discussed, and we immediate zone of continent-continent collision (Dalziel et are grateful to Dalziel andDalla Salda fortheir remarks. al. 1994, fig. 3). We have no reason totake issue with We respond to their four particular comments as follows. well-established models about the Taconic orogen, merely to (1) We do not find it reasonable to expect the faunas of place them in a possible ‘alternative’palaeogeographic Laurentia and Gondwana to be separated for much of the setting. Ordovician if the two continents are contiguous. A (4) Contrary to the suggestion that the Devonian Period mountain range produced by a collision might be expected would be the most likely time of transfer of a Laurentian to act as a barrier to faunal migration for a short time, but terraneto SouthAmerica (p. 285), is the fact thatthe not fortens of million of years. If thefaunas cannot Cambrian-LowerOrdovician platform carbonates of the circumnavigate the mountains, some breaks in continuity of Precordillera are stratigraphically overlain in part by Upper the range would surely develop with time. Ordovician strata of glacial origin (Peralta & Carter 1992). (2) While deep margins are certainly not restricted to Given the low paleolatitude of Laurentia duringlate ocean-facing margins, some correlation cannot be denied. 329 330 DISCUSSION (3) In the Taconic Orogeny of Laurentia, there is only DALZIEL,I.W.D. 1993. Tectonic tracers and the origin of the proto-Andean evidence foran arc-continent collision (McKerrow et al. margin. XII Congreso Geolbgico Argentino Mendoza, 111, 367-374. -1995. Earth Before Pangea. Scientific American, 272,58-63. 1991; van der Pluijm et al. 1995,); there is no indication of a -, DALLASALDA, L.H. & GAHAGAN,L.M. 1994. Paleozoic Laurentia- second continent being involved. Gondwanainteraction and the origin of theAppalachian-Andean (4) The first exchange of non-marinefaunas between mountain system. Geological Society of America Bulletin. 106, 243-252. Laurentia and Gondwana occurs in the Emsian (late Early MCKERROW.W.S., DEWEY,J.F. & SCOTESE,C.F. 1991. The Ordovician and Silurian development of theIapetus Ocean. Special Papers in Devonian), at the time of the Acadian Orogeny (Scotese & Palaeontology, 44, 165-178. McKerrow 1990; Young 1990). This still seems to us the PERALTA.S.H. & CARTER, C.H.1992. Late Ordovician Gondwana glaciation: most probable time for a transfer of terranes from North to Evidence in pebbly mudstones of the Precordillera. province of San Juan, South America. Argentina. Geological Society of America Abstracts with Programs, 24, A91. Finally, we would point that our differences with Dalziel TORSVIK,T.H.. TAT. J., MORALEV, V.M., MCKERROW,W.S.. STURT,B.A. & & DallaSalda areephemeral. They will nodoubt be ROBERTS,D. 1995. Ordovician paleogeography of Siberia and adjacent resolved with further research. continents. Journal of the Geological Society, London, 152, 279-287. RAMOS,V.A., JORDAN.T.E., ALLMENDINGER, R.W., MPODOZES,C., KAY, S.M., CORTES,J.M. & PALMA,M. 1988. Palaeozoic terranes of the central Argentine-Chilean Andes. Tectonics. 5,855-880. References SCOTESE.C.F. & MCKERROW,W.S. 1990. Revised world maps and introduction. In: MCKERROW,W.S. & SCOTESE,C.F. (eds) Palaeozoic ASTINI, R.A., BENEDETTO,J.L. & VACCARI,N.E. 1995. The earlyPaleozoic Palaeogeography and Biogeography. Geological Society, London, evolution of the Argentine Precordillera as a Laurentian rifted. drifted, Memoirs, 12, 1-21. and collided terrane:Ageodynamic model. Geological Society of VAN DER PLLIIJM,B.A.. VANDER Voo, R. & TORSVIK, T.H.1995. Convergence America Bulletin, 148, 253-273. atthe Ordovician margin of Laurentia. New Per.spectiue.rthein DALLA SALDA,L.H., CINGOLANI,C.A. & VARELA, R.1992a. Early Paleozoic Appalachian-Caledonian Orogen (Hank Williams Volume) GAC Special orogenic belt of theAndes in SouthAmerica: Result of Laurentia- Paper XXX. (in press). Gondwana collision? Geology, 20,616-620. YOUNG,G.C. 1990. Devonianvertebrate distribution patterns and cladistic -, DALZIEL,I.W.D., CINGOLANI,C.A. & VARELA,R. 1992b. Didthe analysis of palaeogeographichypotheses. In: MCKERROW,W.S. & TaconicAppalachians continue into South America? Geology, 20, SCOTESE,C.F. (eds) Palaeozolc Palaeogeography and Biogeography. 1059-1062. Geological Society, London, Memoirs, 12, 243-255. IANW. D. DALZIEL,Institute for
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