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Frozen in time: concepts of 'global glaciation' from 1837 (die Eiszeit) to 1998 (the Snowball Earth).

INTRODUCTION

A completely ice-bound Earth, where life is arrested by extreme cold, is not a story out of science fiction but has been proposed to explain Neoproterozoic paleobiology and climates. The Snowball Earth hypothesis is the subject of considerable media interest on a par with global warming. The basic premise was originally outlined in 1837 by Louis Agassiz in his famous Discours de Neuchatel, in which he set out the case for die Eiszeit, a geologically recent Great Ice Age that had smothered the tropics and wiped out all life. A divine creator then introduced new species. Following widespread dismissal of Agassiz's controversial claim to have discovered glacial deposits in the Amazon in 1866, the idea fell out of favour. The concept of ancient 'globally-engulfing glaciations' was given new life in the early 1930s by T. Gevers as the geology of the continents was mapped and the intercontinental distribution of Permo-Carboniferous and Precambrian glacial tillites became evident. To 'permanentists' such as the Toronto glacialist A.P. Coleman, who rejected Wegener's drifting continents explanation for widespread Permo-Carboniferous glacial deposits, the presence of tillites in the steamy heat of the tropics necessitated equatorial ice sheets when 'a world found itself in the grip of the fiercest ... of the ice ages'. Similarly, in reference to the late Precambrian record, D. Mawson referred to the 'world-wide nature of the Earth's greatest glaciation' in 1949. After a brief intermission, when the glacial origin and climatic significance of many deposits was questioned, the ideal of low-latitude glaciation was resurrected in 1964 as the 'great infra-cambrian glaciation' of W.B. Harland. In the early 1970s, L.J.G. Schermerhorn countered by showing that many alleged 'tillites' were the result of submarine mass flow in tectonically active basins. Notwithstanding these findings, fears of 'nuclear winter' arising from nuclear conflagration reawakened interest in an ice-bound Earth in the late 1980s. This culminated in P. Hoffman's and J.L. Kirschvink's Neoproterozoic Snowball Earth model of severe, ten million-year-long global refrigerations when temperatures plummeted to -50[degrees]C, the world's oceans froze and all planetary biological activity was arrested only to be revived during short, brutal interglacials. These so-called 'freeze-fry' episodes are thought to have been a precursor to the Cambrian 'explosion'.

In this paper I expand on the historical development of the idea over the past 160 years and show that the current 'Snowball' version is based on several premises of 'permanentist' thinking that arose in opposition to Wegener in the 1920s and that have survived the advent of plate tectonics and sedimentology largely intact.

INTRODUCTION

Une Terre complement enserree dans la glace, off la vie a ete suspendue par le froid, ce n'est pas une idee de science fiction, mais une idde qui a deja ete proposee pour expliquer la paleobiologie et les climats du Neoproterozoique. L'hypothese d'une Terre boule de neige fait l'objet d'autant d'attention des medias que l'idee d'un rechauffement de la planete. La premisse de base en a ete decrite en 1837 par Louis Agassiz dans son fameux Discours de Neuchatel, document off il plaidait pour die Eiszeit (temps de glace), un grand age glaciaire gdologiquement recent qui aurait envahi les tropiques et elimine toute vie. Un createur divin aurait depuis cree de nouvelles especes. Puis, avec le rejet generalise de la pretention d'Agassiz d'avoir decouvert des depots glaciaires en Amazonie en 1866, l'idde a ete oubliee. Au debut des annees 1930, T. Gevers a redonne vie au concept d'anciennes glaciations planetaires a la faveur de la cartographie gdologique des continents, alors qu'a ete mis en dvidence l'existence de tillites glaciaires permo-carboniferes et prdcambriennes. Du point de vue des fixistes comme le glacielliste de Toronto A. P. Coleman, lequel rejetait l'idde de derive des continents de Wegener pour expliquer la distribution permo-carbonifere des depots glaciaires, l'existence de tillites dans les zones tropicales chaudes et humides impliquaient obligatoirement l'existence de lentilles glaciaires equatoriales, alors (traduction) ... que le monde s'est trouve aux prises avec de terribles ages glaciaires. De meme, se referant a des depots de la fin du Precambrien, D. Mawson en 1949, evoquait (traduction) la nature globale de l'etendue de la plus grande glaciation de la Terre. Ensuite, apres un bref intermede, alors que l'origine et la nature glaciaire de nombreux depots etait remise en question, l'idee de glaciation a de basses latitudes a ete ressuscitee en 1964 par W. B. Harland (traduction) la grande glaciation infracambrienne. Au debut des annees 1970, L. J. G. Schermeerhorn a contreattaque en montrant que nombre de ces presumees tillites n'etaient que la resultante de coulees sedimentaires sousmarines dans des bassins techniquement actifs. Malgre ces decouvertes, vers la fin des annees 1980, la peur d'un hiver nucleaire resultant d'une conflagration nucleaire a vu renaitre l'interet pour l'idee d'une Terre englacee. Ce dernier episode a connu son apogee avec le modele de P. Hoffman et de J. L. Kirschivink d'une Terre boule de neige au Neoproteozoique, soit un periode frigorifique de dix millions d'anndes, la temperature chutant a -50[degrees]C, les oceans etant geles et ou toute activite biologique etait stoppee, sauf pour quelques periodes interglaciaires brutales de courtes dures. Ces episodes d'alternance chaud-froid auraient ete a l'origine de l'explosion Cambrienne. Dans le present article j'explique l'dvolution historique de cette idee au cours des derniers 160 ans, et je demontre que l'actuel concept de boule de neige repose sur plusieurs premisses de la mouvance fixiste qui s'est fait jour en opposition a Wegener dans les annees 1920, laquelle a survecue sans etre vraiment affectee par les developpements de la tectonique des plaques et de la sedimentologie.

THE FIRST SNOWBALL (1837-76): THE PLEISTOCENE "EISZEIT"

Louis Agassiz (1807-1873: Fig. 1, 2) was the first formal proponent of global glaciation, which he called 'die Eiszeit' (a name borrowed from his friend Karl Schimper's famous poem; 'Ice of the past! of an age when frost in its stern clasp held the lands of the south') in his 1837 Discours of Neuchatel (Carozzi, 1966, 1967). Intending to speak on his speciality (fossil fish) he gave a hastily written lecture in which he set out an audacious theory of a catastrophic Great Ice Age. His theory had two parts: the first, built on earlier observations by many others, proposed that present-day glaciers had been much more extensive in the past. With some exceptions, this was readily accepted both in Europe and North America (North, 1943; Carozzi, 1974; Hallam, 1989). The second part of Agassiz's theory however, was highly controversial and was based on his mentor Georges Cuvier's hypothesis that an ice age had wiped out all life. Cuvier (1769-1832) was the leading catastrophist of his age and had noticed in mapping the Paris Basin with his colleague Alexandre Brongniart that many fossil groups appeared to die out at unconformities. He resorted to 'ancient revolutions' to account for these abrupt breaks in geological successions and fauna. Cuvier was entranced by the preservation of complete Siberian mammoths in permafrost and saw this as evidence of a great cataclysm. In 1812, in his Discours sur les Revolutions de la Surface du Globe he wrote: 'It also left in northern countries the bodies of great quadrupeds encased in ice and preserved with their skin, hair and flesh down to our times ... The animals were killed therefore at the same instant when glacial conditions overwhelmed the countries they inhabited. Cuvier mistook these migratory animals adapted to a cold environment for tropical animals suddenly overtaken by cold.

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Agassiz was greatly impressed by the ice-entombed Siberian mammoth s and argued that 'a sudden intense winter, that was also to last for ages, fell upon the globe', 'the development of these huge ice sheets must have led to the destruction of all organic life at the Earth's surface' (Fig. 1). He regarded the ice age as divinely inspired severing any genetic relationship between past and present life forms ('death enveloped all nature in a shroud). Species were generated anew after each ice age. Glacial landforms were seen as the product of 'God's great plough'. The reaction of the audience after his lecture at Neuchatel was such that 'some observers feared the introduction of fisticuffs' (Bolles, 1999, p. 87). The wider public and scientists alike were outraged at his notion that a 'Siberian winter established itself for a while on ground previously covered by rich vegetation and inhabited by great mammals'. Driven by an unyielding belief in catastrophism and a fundamental opposition to Darwin's theory of evolution, Agassiz was unsettled by the notion that life may have survived ice ages unscathed in tropical oases. Agassiz was undeterred by the 1863 publication of Lyell's book on The Geological Evidences of the Antiquity of Man that marshalled evidence that during ice ages, pre-ice age species including humans, had simply moved south. J. Lubbock introduced the term 'prehistory' in 1865, recognizing that glaciation had simply interrupted organisms, not wiped them out. Between 1865 and 1866 Agassiz explored the Brazilian Amazon and found red-coloured clays with pebbles and large boulders which he called "Pleistocene Amazonian drift" (Fig. 2b). This he argued was evidence of a series of physical events extending over the whole globe ... if the geological winter existed ... it must have been cosmic'. To some, Agassiz's 1866 paper on "Traces of Glaciers under the Tropics' delivered in Washington D.C., arguing for equatorial glaciation, was a 'new and fundamental phase of the Ice-Age theory' (Agassiz and Coutinho, 1868). Agassiz pressed on and wrote of a 'geological winter' extending over the whole globe (Agassiz, 1876). He dared the scientific community to 'imagine, if you can, floating ice under the equator, such as now exists on the coasts of Greenland (Agassiz, 1886). In hindsight, it was a complete blunder (Carozzi, 1974). The bouldery clay 'drift' was the not the product of a tropical ice sheet but deep weathering of igneous rocks and exfoliation of core stones (Branner, 1893; Fig. 2b). In 1872, one of Canada's leading geologists, Sir William Dawson (a virulent opponent of continental glaciation; O'Brien, 1971), took the opportunity to poke fun at Agassiz in his book Notes on the Post-Pliocene Geology of Canada. He wrote the glacier theory had grown until 'like the imaginary glaciers themselves, it overspread the earth', even 'to Brazil and employed to excavate the valley of the Amazon. But this was its last feat and it has recently been melting away under the warmth of discussion until it is now but a shadow of its former self. By 1870 Agassiz's notion of a worldwide cosmic winter was moribund. It was to be resurrected once more as the record of pre-Pleistocene glaciations began to be discovered.

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THE SECOND SNOWBALL (C. 1926): 'WORLD WIDE REFRIGERATION'

The study of pre-Pleistocene glacial deposits begins with A.E. Ramsay's 1855 glacial interpretation of Permian breccias in central England. Later proved to be wrong, Ramsay's work spurred others to look for evidence of ancient glaciations. Results soon appeared, such as W.T. Blandford's discovery of Permo-Carboniferous glacial deposits at Talchir in India, and that by A.R.C. Selwyn at Hallet's Cove in Australia, both in 1859. The first description of Precambrian glacial rocks was made by H.P. Woodward in the Flinders Ranges of Australia in 1889; others soon followed, such as ancient 'moraines' in Scandinavia (Reusch, 1891). Already, the presence of ancient glacial rocks in central India was interpreted as the product of 'a more extensive and severe glaciation than that of the glacial period of Pleistocene times' and its explanation was seen as 'a tough nut to crack' (Geikie, 1894, p. 825). The Earth's oldest glacial rocks (mid-Proterozoic) were reported from Gowganda in northern Ontario (Coleman, 1907) and in 1906 Albrecht Penck introduced the term tillite for ancient lithified tills. Today, it is easy to underestimate the huge public interest that these discoveries created because they revealed great changes in ancient climates when many scientists believed the Earth's surface had simply been hotter in the past and was 'advancing toward an icy old age' (Coleman, 1941, p. 7). The then young (23) Winston S. Churchill commented on this gloomy picture in his novel Savrola, which he wrote in 1898; 'the cooling process would continue; the perfect development of life would end in death, the whole universe itself would one day be cold and lifeless as a burnt-out firework.' To Coleman, his finding of very old glacial deposits 'banished this gloomy foreboding' such that "mankind may proceed ... free from the haunting dread of an approaching extinction of the race.'

By the early years of the twentieth century, as the geology of the continents began to be better known, it was realized that Permian and Precambrian glacial deposits occur virtually on all continents and at low latitudes. Moreover, many striated surfaces show that ice had moved north away from the tropics, requiring ice covers whose dimensions made the sheets of the Pleistocene seem insignificant. A.P. Coleman's influential paper of 1908 and his book Ice Ages Recent and Ancient (1926) reviewed what was known of Earth's ancient glacial record. Emphasising the extensive presence of glacial rocks at low latitudes, he declared that 'the Permo-Carboniferous ice was the most terrible known in the world's history' (Coleman, 1939). In his review of Pleistocene ice ages, published two years after his death in 1939, Coleman (1941, p. 6) was careful to stress that the Permo-Carboniferous glaciation 'when ice reached the tropics' ... had the better right to be called The Ice Age'. The geomorphologist W.M. Davis, who accompanied Coleman on field trips in South Africa and Australia, declared that 'the Permian glacial climate is one of the most remarkable problems disclosed by geology today'. He firmly rejected the pre-Wegener hypothesis of 'an Antarctic continent of which Australia, South Africa and a part of South America were possibly but lobes' as an explanation for Permo-Carboniferous tillites in the tropics (Davis, 1908). To Coleman, explaining why the 'world ... found itself in the grip of the fercest and longest winter of the ages' was 'one of the most thrilling problems in all of geology' (Coleman, 1916). Sayles (1919) reviewed what was known of Pleistocene glaciolacustrine varves and used this model to explain the presence of banded and laminated slates commonly found with Permian and Precambrian glacials. He declared with particular reference to the Permian glacials present in the tropics of India and Africa, that 'it will now be necessary to explain not only the former presence of the great ice sheet in the tropics but marked alternations of seasons too.' Any theory of glaciation, Coleman wrote in 1926, 'must account for a world-wide refrigeration affecting all zones of both hemispheres at the same time' (p. 282). The idea of worldwide glaciation found support in the Precambrian record too. In his influential Textbook of Geology published in 1920, A.W. Grabau wrote (p. 206) of Precambrian 'glaciers extending from the poles to South Australia and South Africa' requiring 'extremes of refrigeration far beyond those known today'. After discovering widely distributed and very thick late Precambrian tillites in southwest Africa, Gevers (1931)invoked 'globally-engulfing glaciations'. He wrote 'there appear to have been glacial periods of world-wide extent'. Of course, none of these conclusions could have been reached without all these workers rejecting the idea of continental drift.

To the 'permanentists' who believed in an Earth where continents and oceans remain static, the global scattering of glacial rocks required enormous ice sheets expanding into low latitudes (Grabau, 1920; Coleman, 1926, 1932, 1939). The presence of ancient glacial rocks in the steamy tropical heat of low latitudes was nothing less than 'astonishing', rousing 'incredulity among the geologists of Europe and America' (Coleman, 1926, p. 97). Travelling through 'rank jungle growth.., the noon sun was very hot and yet we stood on a smoothly glaciated and striated floor ... the tillite might well have been boulder clay by the shore of a Canadian river.... the contrast of the present with the past was astounding' (Coleman, 1926, p. 106-7). He wrote of 'being laughed at by country people while I chipped striated clasts from tillite well within the tropics not far from plantations of bananas' (Coleman, 1939, p. 450); the words 'incredible' pepper his many publications. Refusing to believe that the continents had shifted, the only other explanation was to have ice at low latitudes (Coleman, 1932). ' The dry wilting sun glare and perspiration made the thought of an ice sheet at that very spot most incredible but alluring' (Coleman, 1926, p. 123).

Wegener and the Great 'Southern Glaciation'

Alfred Wegener saw the global scattering of tillites in a very different light; here was clear evidence that continents were previously clustered together and had since been moved apart (Wegener, 1912, 1924). The wide distribution of Permo-Carboniferous tillites across the southern continents was a key to his reconstruction of the supercontinent Pangea and its climate belts. Despite support from the southern hemisphere where the evidence is clearest (e.g., Du Toit, 1921), Wegener's message largely fell on deaf ears. His theory of 'continental drift' as an explanation for tropical tillites was regarded as 'incredible' (Coleman, 1926, p. 263), a 'fairy tale' (Willis, 1944) and 'purely fantastic' (Flint, 1957, p. 503). Their objections are today seen as ironic because to many other geologists, Wegener's reconstruction of the southern ice sheet blanketing the polar and sub-polar regions of Pangea was the most convincing argument for continental drift (LeGrand, 1988). That the loudest opposition to Wegener came from leading North American geologists was not surprising. First, Wegener's famous map showing the supposed arrangement of land during the geologically recent Pleistocene where the outer terminal moraines of the ice sheets in Europe and North America 'join up smoothly' was patently incorrect and quickly rejected. Unfortunately, the entire thesis of continental drift was also thrown out. Second, Wegener had indirectly questioned the combined weight of their expertise by daring to question the supposed glacial origin of the famous 'Squantum Tillite' found near Boston. This was seen as a classic Permo-Carboniferous glacial deposit (it met 14 out of 15 criteria for being glacial as identified by Sayles, 1914, 1919) but Wegener's reconstruction of Pangea placed the Boston area near the equator. He warned that not all poorly sorted rocks were true glacial tillites (Fig. 3) and thus were unreliable indicators of past climate and continental positioning (Wegener, 1928). He argued that the Squantum was marine in origin and not deposited directly by an ice sheet (and in this was later proven correct; Crowell, 1957; Dott, 1961; see below) and, as we now know, is of Late Neoproterozoic age (Thompson and Bowring, 2000).

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In 1932, Coleman wrote that 'enough has been noted to show that inadequate to account for known facts in regard to the greatest times of glaciation'. To the permanentists, glaciations were seen as 'catastrophic events in the world's history'. Cotton (1942) referred to glaciation as a 'climatic accident' and Pauly (1957) referred to 'world-wide abnormal climates" Such events were regarded as being superimposed on static continents where deep glacial erosion and deposition of coarse bouldery sediments such as tills simply interrupted an otherwise orderly Davisian cycle of landscape and sediment evolution from youth to maturity. As a result, ancient glaciations were seen as highly unusual events ('slow motion catastrophes'; Bolles, 1999) and as such were of chronostratigraphic value because such events could be precisely correlated from one continent to another (e.g., Chumakov, 1981). Clearly, because these deposits are found on all continents and can be precisely correlated, then truly global glaciations must have occurred, a circular argument still thriving in the modern literature (see below).

THE THIRD SNOWBALL (C. 1949): 'THE WORLD'S GREATEST ICE AGE'

The work of Mawson (1949) on the Sturtian Tillites of South Australia ('the greatest thing of the kind recorded anywhere in the world; Mawson, 1958) is a good example of the classical approach to interpretation of sedimentary strata containing poorly sorted, laminated and banded rocks. The depositional model then available was that of continental glacial deposition where tills, glaciolacustrine and outwash deposits record the climatically driven waxing and waning of ice sheets. Ironically, Mawson's earlier visits to Antarctica, the first as a member of Ernest Shackleton's British Antarctic Expedition of 1907-1909, had been spurred by his desire to seek 'first hand knowledge of the conditions of sedimentation during an ice age'; Mawson, 1958, p. xxvii). He was, however, greatly disappointed because 'the products of glacial erosion are almost entirely dumped on the floor of the surrounding ocean and thus not available for investigation' (Mawson, 1949, p. 52). Obliquely, he had touched on a major finding, that Earth's glacial record is selectively preserved in glacially influenced marine facies. Inspired by reports of late Precambrian tillites from equatorial Africa and their broad global distribution elsewhere, Mawson (1949) invoked a massive 'world-wide' glaciation 'where glaciation is evidenced even to the equator'. Echoing Coleman's early comment on the late Paleozoic ice ages, he concluded that the late Precambrian glaciation had been the most 'severe of all in earth history; in fact, no less than 'the world's greatest ice age'.

The Growth of Sedimentology

With the development of the discipline of sedimentology in the 1950s, attention quickly focussed on submarine processes such as debris flows and turbidity currents. It was soon appreciated that not all poorly sorted rocks are glacial tillites deposited below glaciers on elevated continental surfaces; many are non-glacial deep-marine mass-flow deposits interbedded with turbidites (Fig. 3, 4). Such rocks are a common component of non-glacial submarine fan successions. Pettijohn (1984, p. 128) remarked that the now classic paper of Kuenen and Migliorini (1950) 'unlocked the secret' by revealing that graded, fine-grained and rhythmically laminated facies were deposited by turbidites and were not axiomatically 'varvites' hitherto a favourite criterion among those looking for evidence of cold climates (e.g, Sayles, 1914, 1919). Pettijohn (1984, p. 131) recounted the 1952 Geological Society of America field trip to the so-called Squantum Tillite near Boston, the focus of earlier debate between Coleman and Wegener in the 1920s. One of the participants was J.C. Crowell 'who had seen many of such deposits in California and had never considered any of them tillites. Indeed they were pebbly mudstones, probably products of submarine slump'. Near Squantum Head were graded slates, 'interpreted as deposits in glacial lakes ... the case for glacial origin was suspect if not downright wrong. Imagine our dismay at seeing the Squantum for the first time, a classical deposit long cited as evidence of Permian glaciation in America.' Crowell (1957) explained many ancient pebbly mudstone deposits as debris flows produced by the mixing of fine and coarse-grained sediment during slumping. Ironically, the supposed glacial origin of the Squantum had been the reason why an earlier generation of geologists had rejected of the entire notion of 'continental drift' (see above). The work of Crowell (1957), Dott (1961) and Winterer (1963) led to the introduction of purely descriptive terms for poorly sorted and laminated facies that avoided any preconceived notion of a glacial origin (e.g., diamict, mixtite, symmictite, tilloid, rhythmite; see Schermerhorn, 1966). Opposition and resentment to this reappraisal of Earth's glacial record is evident in the reference to 'this bleak period of disappointment' by Harland and Herod (1975, p. 190).

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THE FOURTH SNOWBALL (1964): THE 'INFRACAMBRIAN GLACIATION'

The proponents of 'big glaciation' counterattacked with novel geophysical evidence in support of low-latitude glaciation. Harland and Bidgood (1959) reported magnetic data purporting to record equatorial paleolatitudes for Neoproterozoic glacials, and invoked a huge 'infracambrian glaciation' of global extent involving 'near synchronous worldwide tillites' (Harland, 1964, Harland and Herod, 1975, p. 201). That tillites were found closely associated with carbonates was cited as additional evidence of huge fluctuations in global climates. Paleomagnetic data were subsequently shown to be a result of later, postdepositional metamorphism and remagnetization, but a large body of paleomagnetic data has evolved in support of low-latitude glaciation (see below). It was also demonstrated that the common association of 'tillites and carbonates' was the product of active tectonic settings in which non-glacial marine mass flows were interbedded with olistostromes, debris flows and turbidites composed of detrital, reworked carbonate (Schermerhorn, 1974).

At the same time that sedimentology was leading to a reassessment of the sedimentary record of 'big glaciation', a second front opened with the replacement of 'continental drift' by 'plate tectonics' in the 1960s (McKenzie and Parker, 1967). Schermerhorn (1974) led the charge in re-examining ancient 'glacial' deposits in the light of their tectonic and basinal setting. Building on the work of Crowell (1957) and others, he argued that many supposed Neoproterozoic 'tillites' are non-glacial debris flows of unknown climatic significance, deposited in tectonically active marine basins marginal to uplifted source areas. Their worldwide distribution that had impressed so many others simply reflected their former close proximity within an earlier supercontinent and a long history of subsequent plate movements. He identified the importance of tectonic uplift in generating regional ice covers and also stressed the poor dating control on most deposits. Others followed, such as Martin et al.'s (1985) detailed and lengthy refutation of the glacial origin of the Namibian Neoproterozoic diamictites (Fig. 5) recently proposed as key evidence of a Snowball Earth (Hoffman et al., 1998).

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Hambrey and Harland's (1981) very impressive Earth's Pre-Pleistocene Glacial Record compiled the known rock record but perhaps missed the opportunity to place it in the context of plate tectonics and emerging paleogeographic reconstructions. This is ironic given that Harland was one of the earliest converts to plate tectonics (LeGrand, 1988). In the early 1980s, as knowledge of glaciomarine environments rapidly expanded based on shipborne studies in the Arctic and Antarctic margins, so it became clear that the record of ancient glacial climates is preferentially stored in rocks of marine origin (Anderson, 1983). Work by Young and Gostin (1989, 1991) has confirmed the glacially influenced marine origin of the classic Sturtian 'Tillites' of Australia that had been the cornerstone of Mawson's worldwide glaciation. Eyles (1993) reviewed the record in the context of broader knowledge of depositional systems and basin evolution. He confirmed Schermerhorn's thesis that a 'glacial' origin cannot be demonstrated for many ancient deposits and that most of the demonstrably glacially influenced strata had been selectively deposited in rift basins. The genetic association between glacially influenced strata deposited offshore, and uplift of elevated source areas on rift flanks was clear. If the precise causative linkages are still a little fuzzy, it is evident that the ancient glacial deposits cannot be studied in the absence of discussion of plate tectonic and basinal setting (Crowell, 1999). Similarly, such approaches are key to the discrimination of glacial from nonglacial successions containing diamictites.

THE FIFTH SNOWBALL (C. 1998): "SNOWBALL EARTH"

The Snowball Earth of Hoffman et al. (1998) is a bold reworking of the global glaciation models of earlier workers and incorporates much new geochemical and paleomagnetic data. The model owes much to Cold War concepts of a 'nuclear winter' where dust veils thrown up by nuclear explosions lower global albedo resulting in "complete glaciation of the world" (Budyko, 1982, p. 269; Kirschvink et al., 2000). Based on work principally in Namibia (Fig. 5) Hoffman et al. (1998) and Hoffman and Schrag (2000) propose a runaway albedo mechanism for initiating Snowball glaciation, where extreme cold and thick sea ice shut down all hydrological activity and chemical weathering such that marine autotrophic activity and organic carbon burial would cease. This, it was argued, would drive the ocean carbon isotope composition to near-mantle values. After some 10 million years, sufficient volcanically emitted C[O.sub.2] would accumulate to produce global temperatures of +50 [degrees]C starting the catastrophic meltdown of ice and precipitation of cap carbonates deposits.

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Eyles and Januszczak (2004) reviewed the Snowball Earth model at length and showed that the model retains much of the classical thinking of the 'permanentists' of the 1920s. First, the Snowball model is based on stratigraphic analyses, which, to borrow Harland and Herod's (1975) phrase are 'sedimentologically unsophisticated" Old, and by now very shop-worn assumptions that poorly sorted diamictite facies must be continental tillites deposited below ice sheets, and any fine-grained, rhythmically laminated facies are glaciolacustrine varvites, can still be found in the Snowball literature (Hoffman et al., 1998; p. 1342). One is hard pressed to find detailed sedimentological descriptions of strata held to record key global events (e.g., Hoffman and Schrag, 2002). This is decades after sedimentologists began to highlight the simplistic interpretation of ancient 'glacial' strata and the need for comprehensive facies and basin analysis studies.

Second, the model is based on the circular argument that because the deposits are tillites that are of a wide global extent, then they must record an unusual catastrophic event such as global glaciation. This assumption was first made in the 1920s and was recycled by Harland and Herod (1975) and Chumakov (1981). It is now repeated uncritically by adherents of the Snowball model such as Tojo et al. (1999) for whom 'the global distribution of glacial deposits of Neoproterozoic age suggests that the ice sheet of the time developed even to the equatorial area'. This argument has even been exported farther back in time, where according to Bekker et al. (1999) 'evidence of three glaciations in the early Paleoproterozoic ... of North America ... and at least one on three other continents suggests that these ice ages were of global extent'. Proterozoic glaciations must have been unlike any subsequent glaciations of the Phanerozoic 'because they can be found on every continent.... unlike the more a really limited distribution of Pleistocene glacial deposits' (Sohl et al., 1999, p. 1121) suggesting 'climatic extremes unrivalled in Earth history' (Kennedy et al., 2001a, p. 1135), and ice ages 'unlike any in Phanerozoic Earth history because oft heir great severity' (Sohl et al., 1999, p. 1120). It can be appreciated that these quotes closely resemble the writings of the permanentists of the 1920s such as A.P. Coleman. Available age dates do not support the contention that 'glacial' diamictites were deposited during synchronous global glaciations (Evans, 1999); in response, Snowballers spawn new snowball events to fit each new age result (e.g., Table 1 in Hoffman and Schrag, 2002).

Third, the Snowball model overemphasizes the apparent paradox in the ancient rock record, where 'glacial' diamictites are interbedded with carbonates and some times have distinct 'cap carbonates'. The juxtaposition is argued to record brutally hot greenhouse conditions, but as detailed sedimentological data accrue, such strata are revealed to be not primary chemical precipitates but are detrital in origin, principally the deposits of turbidites reworking old carbonate deposits, and comprise an integral part of very thick marine successions containing poorly sorted mass flows misidentified as tillites. These successions reach many kilometres in thickness and were deposited on newly formed continental margins as Rodinia broke apart and huge volumes of detrital carbonate were reworked (see below). Where present, primary and stromatolitic carbonates are separated from underlying diamictite units by unconformities or many tens and sometimes hundreds of metres of marine strata, thereby questioning any supposed immediate 'cap' relationship (e.g., Hoffman et al., 1998).

Fourth, snowballers suggest that evolutionary stress imposed by extreme cold, when organisms survived glaciation only by living around hydrothermal vents, played a causal role in triggering the Cambrian 'Explosion'. In contrast, what is known of Neoproterozoic Ediacarian biotas indicate they were environmentally sensitive lichen-like organisms living in shallow euphotic settings (Narbonne, 1998). The acritarch record of Australia indicates that pre- and post-Snowball populations are identical and do not indicate repopulation of marine areas by extremophiles that survived both catastrophic glaciation in hot springs and the brutal greenhouse conditions which followed (Grey et al., 2003).

Fifth, much emphasis has been placed on paleomagnetic data indicating low depositional paleolatitudes (Evans, 1999). Eyles and Januszczak (2004) concluded that precisely how magnetic characteristics were acquired, when, and even the origin of many of the strata being sampled remain major unresolved issues. These limitations are echoed by Meert and Torsvik (2004).

Sixth, the reappearance of banded iron formations in the late Neoproterozoic has been genetically linked to global glaciation; the assumption is that anoxic seawaters form below a global cover of thick sea ice thereby enabling ferrous iron to remain in solution (Hoffman et al., 1998; Hoffman and Schrag, 2002). In fact, banded iron deposits are not uniquely associated with Neoproterozoic diamictite deposits and often occur stratigraphically below such deposits, are absent outright, or are demonstrably postdepositional (Young, 2003). The reappearance of banded iron is more likely related to episodes of continental rifting in the Neoproterozoic and deposition in enclosed or restricted rift basins close to hydrothermal vents along incipient mid-ocean ridges.

Seventh, the Snowball earth model relies heavily on the assumption that glaciation is inherently linked to fluctuations in carbon isotope trends derived from carbonate rocks. The model predicts positive [sup.13]C values prior to the onset of glaciation, due to preferential incorporation of [sup.12]C in ocean waters as a result of biological activity. As environmental conditions deteriorate prior to each Snowball event and organisms die off, the burial of organic carbon reintroduces [sup.12]C into the world oceans giving negative [sup.13]C values that persist until the postglacial re-establishment of biological activity. Whereas there is good evidence for systematic isotope fluctuations, the controls on such changes cannot simply be related to global glaciation. For example, snowball events have been identified, not from any direct geological record, but from geochemical data alone (e.g., Kennedy et al., 1998). How environmental changes held to be without parallel in the history of the planet left no direct stratigraphic record is difficult to understand. Additional factors that need to be considered include the exposure and weathering of older carbonate and enhanced vertical gradients in seawater [sup.13]C due to redox stratification of ocean waters and accelerated burial of organic carbon in rapidly subsiding rift basins. Isotopic excursions may be regional in scope resulting from the formation of restricted basins during the rifting of Rodinia where waters in enclosed or semi-restricted basins are in disequilibrium with global surface oceans (Shields et al., 2002). Some carbon isotope values from carbonate interbeds and clasts within supposedly 'glacial' diamictites show positive trends (Kennedy et al., 2001a). Strontium isotope data also fail to support hydrological cycle shutdown during Snowball glaciation and enhanced continental weathering in the aftermath (Kennedy et al., 2001b). Neither is the Snowball model supported by climate modellers (Hyde et al., 2000; Baum and Crowley, 2001) who identify an ice free equator (Peltier, 2004).

Eyles and Januszczak (2004) propose an opposing uniformitarian model to the extreme catastrophic snowball view of Neoproterozoic glaciation. The global context of glaciation in the Neoproterozoic is the massive first-order reorganization of the planet's geography, climate and ocean systems resulting from the breakup and dispersal of the supercontinent Rodinia. Commencing about 750 Ma and lasting for at least 150 million years, global rifting was the overriding control on sedimentary basin formation, basin-fill stratigraphies and glaciation. A first phase of rifting occurred after 750 Ma along the paleo-Pacific margin of Laurentia, and the second phase of rifting occurred at about 600 Ma along its paleo-Atlantic Iapetan margin (Young, 1992; Li and Powell, 2001). It cannot simply be coincidental that these two rift phases are directly linked to the two principle episodes of glaciation of the Neoproterozoic: the first phase that of the Sturtian (c. 750 Ma) and equivalent Rapitan glacials, the second that of the Marinoan and Vendian glacial deposits (c. 600 Ma). The total length of rifted margin was more than 25,000 km, suggesting a staggered climatic response to uplift as rifting progressed diachronously, somewhat like a zipper. The stratigraphic record is dominated by thick submarine slope and fan deposits reflecting rift basin formation and influxes of large volumes of clastic sediment, including carbonate debris, from uplifted rift shoulders. Such successions are dominated by turbidites, olistostromes and debris-flow facies; some, where uplift or latitude was appropriate, are glacially influenced, but many are not (Schermerhorn, 1974, 1975; Eyles, 1993). Within tectonically active basins, the effects of glacioeustatic sea level are difficult to identify because of the control on relative water depths resulting from varying subsidence rates. Very thick coarsening-upward successions, hundreds of metres (sometimes kilometres) thick that can be traced globally and hitherto ascribed to 'glacioeustatic' fluctuations in sea level (Young, 1992) are more likely tectonically controlled. In short, rather than the product of global climatic catastrophes, the deposits of Neoproterozoic glaciers are seen as similar in scale and type to those of the Pleistocene (Eyles and Januszczak, 2004a).

DISCUSSION

At the conclusion of his lengthy review of Neoproterozoic glacial deposits, Schermerhorn commented on the myth-like nature of the concept of global glaciation. Interestingly enough, ancient tales of catastrophic glaciation followed by renewal are a fixture of several northern cultures and reflect a universal creation motif where a divine creator, disgusted with early humanity, decides to wipe the slate clean (Leeming and Leeming, 1994). In the Norse story of Ragnarok the world is brought to a dreadful end by the terrible Fimbulvinter. This story was written in 1220 A.D., as part of the epic poem Edda by the Icelander Snorris Sturluson. Other Norse creation myths tell of the evil Ice Giant Ymir, who is clearly based on folk memories of the last glaciation, 'from whose body the world was made. Ymir turned his body into the earth and his blood into the seas. His bones became mountains and his teeth became rocks'. Any geologist who has spent time working on modern glaciers will instantly recognise the imagery of a glacier slowly melting and retreating. Here in Canada, First Nation legends talk of the turtle (the land) being weighed down by a giant white toad that gobbled up all the fresh water; clearly a reference to the last ice sheet along whose margins Paleo Indians followed into what is now central Canada some 12,000 years ago. As the toad died, so the turtle was able to stand erect and the waters disappeared; we call this today 'glacioisostatic rebound'.

The forensic climatologist H. Lamb (1978) recounts folk legends from Asia and Iran where a golden age is destroyed by intense cold. Recently, writers of science fiction have taken up the theme. Louis Agassiz was clearly tapping into a universal fear when he proposed his devastating Eiszeit in 1837. More recently, the science fiction writer Aldiss (1985) writes in his Helliconia trilogy of the catastrophic nature of a global glaciation when 'cold gripped the favoured lands of the equator' and the planet 'lay in a chill catalepsy' 'wiping the Earth clear of festering civilizations', Many will clearly remember the effects that a few years of bad North American winters in the late 1970s with 'killer blizzards', combined with a slight dip in global temperatures, had on the media and the popular press (e.g., 'the Ice Age comes'; Halacy, 1978). The theme of killer blizzards reemerges in the recent Hollywood blockbuster The Day After Tomorrow.

In summary, the notion of globally widespread glaciation is one of the most enduring ideas in geology and has surviving from Agassiz's Eiszeit and the catastrophist school of Cuvier to reemerge in a different iteration as Snowball Earth in the late 1990s. Many of the assumptions behind the current model were first made in the 1920s by those who dismissed continental drift, and these notions have survived the plate tectonics revolution completely unscathed. The wide geographic distribution of rocks that are liberally interpreted as 'tillites' is still one of the planks of the Snowball Earth model despite advances in understanding of plate tectonics, crustal history and sedimentology. It may well be that late Neoproterozoic glaciation was regional in scope and tectonically preconditioned as a result of the breakup of Rodinia. Much fieldwork remains to be done on Earth's ancient glacial climates using well-tried uniformitarian principles embodied in sedimentary basin analysis.

ACKNOWLEDGEMENTS

The research on which this article is based was funded by the Natural Science and Engineering Research Council of Canada. I thank many individuals, principally Nicole Januszczak, Carolyn Eyles, Andrew Miall and John Crowell for many very helpful discussions. Alan Morgan and Grant Young reviewed the manuscript and I am grateful for their comments. The views cited herein are entirely those of the author.

REFERENCES

Agassiz, E.C., 1886, Louis Agassiz, his life and correspondence: Boston, Houghton, Mifflin and Co., v. 11, p. 639.

Agassiz, L., 1876, Geological Sketches: 2nd series, Boston, J.R. Osgood and Co., p. 153-229.

Agassiz, L. and Coutinho, J.M. da Silva, 1868, Sur la geologie de L'Amazone: C.R. Acad. Sciences, Paris, v. 64, p. 1269-1271.

Aldiss, B., 1985, Helliconia Winter: Jonathan Cape, London. 392 p.

Anderson, J.B., 1983, Ancient glacial-marine deposits: their spatial and temporal distribution, in Glacial-Marine Sedimentation: B.F. Molnia, Plenum Press, New York, p. 3-92.

Baum, S.K. and Crowley, T.J., 2001, GCM Response to Late Precambrian (-590 Ma) Ice-Covered Continents: Geophysical Research Letters, v. 28, p. 583-586.

Bekker, A., Eriksson, K.A., Kaufman, A.J., Karhu, J.A., and Beukes, N.J., 1999, Paleoproterozoic record of biogeochemical events and ice ages: Geological Society of America Abstracts with Programs, v. 31, p. 487.

Bolles, E.B., 1999, The Ice Finders: Counterpoint, Washington, D.C., 257 p.

Branner, J.C., 1893, The supposed glaciation of Brazil: Journal of Geology, v. 1, p. 753-772.

Budyko, M.I., 1982, The Earth's Climate: Past and Future: Academic Press, 307 p.

Carozzi, A.V., 1966, Agassiz's amazing geological speculation; The Ice Age: Studies in Romanticism, v. 2, p. 57-83.

Carozzi, A.V., 1967, Studies on Glaciers. Translated and edited by A.V. Carozzi, Hafner Publishing New York, 213 p.

Carozzi, A.V., 1974, Agassiz's influence on geological thinking in the Americas: Archives des Sciences: Societe de physique et d'histoire naturelle de Geneve, v. 27, p. 5-38.

Chumakov, N.M., 1981, Upper Proterozoic glaciogenic rocks and their stratigraphic significance: Precambrian Research, v. 15, p. 373-395.

Coleman, A.P., 1907, A lower Huronian ice age: American Journal of Science, v. 23, p. 187-203.

Coleman, A.P., 1908, Glacial periods and their bearing on geological theories: Geological Society of America, Bulletin, v. 19, p. 347-366.

Coleman, A.P., 1916, Dry land in geology: Geological Society of America, Bulletin, v. 27, p. 175-192.

Coleman, A.P., 1926, Ice Ages. Recent and Ancient: The MacMillan Company, 296 p.

Coleman, A.P., 1932, Glaciation and continental drift. Geographical Journal, v. LXXIX, p. 252-255.

Coleman, A.P., 1939, Ice ages in the geological column: Geological Society of America, Bulletin, v. 50, p. 449-452.

Coleman, A.P., 1941, The Last Million Years: AMS Press, New York, 216 p.

Cotton, C.A., 1942, Climatic Accidents in the Landscape: Whitcombe & Tombs, New Zealand, 354 p.

Crowell, J.C., 1957, Origin of pebbly mudstone: Geological Society of America, Bulletin, v. 68, p. 993-101.

Crowell, J.C., 1999, Pre-Mesozoic Ice Ages: Their Bearing on Understanding the Climate System. Geological Society of America, Memoir, v. 192, 106 p.

Davis, G.M., 1908, Causes of Permo-Carboniferous glaciation: Journal of Geology, v. 16, p. 79-82.

Dott, R.H., 1961, Squantum "Tillite", Massachusetts; evidence of glaciation or subaqueous mass movements?: Geological Society of America, Bulletin, v. 72, p. 1289-1306.

DuToit, A.L., 1921, Land connections between the other continents and South Africa in the past: South African Journal of Science, v. 18, p. 120-40.

Evans, D.A.D., 1999, A Proterozoic palaeoclimatic paradox persists: Tectonics Special Research Center, Annual Report, p. 63-64.

Eyles, N., 1993, Earth's glacial record and its tectonic setting: Earth Science Reviews, v. 35, p. 1-248.

Eyles, N. and Januszczak, 2004a, Interpreting the Neoproterozoic glacial record: The importance of tectonics, in G.S. Jenkins, M.A. McMenamin, C. McKay and L. Sohl, eds., The Extreme Proterozoic: Geology, Geochemistry and climate: American Geophysical Union, Geophysical Monography 146, p. 125-144.

Eyles, N. and Januszczak, 2004b, Zipper rift: A tectonic model for Neoproterozoic glaciations during the breakup of Rodinia after 750 Ma.: Earth Science Reviews, v. 65, p. 1-73.

Flint, R.F., 1957, Glacial Geology and the Pleistocene Epoch: John Wiley, New York, 589 p.

Geikie, J., 1894, The Great Ice Age: Third Edition, Spottiswoode and Co., London. 850 p.

Gevers, T.W, 1931, An ancient tillite in South West Africa: Transactions of the Geological Society of South Africa, v. 34, p. 1-17.

Grabau, A.W., 1920, A Textbook of Geology: D.C. Heath and Co., Boston, 976 p.

Grey, K., Walter, M.R., and Calver, C.R., 2003, Neoproterozoic biotic diversification: Snowball Earth or aftermath of the Acraman impact?: Geology, v. 31, p. 459-462.

Halacy, D.C., 1978, Ice or Fire? Surviving Climatic Change: Harper and Row, 212 p.

Hallam, A., 1989, Great Geological Controversies: Oxford Science Publications, 244 p.

Hambrey, M.J. and Harland, W.B., (eds.), 1981. Earth's Pre-Pleistocene Glacial Record: Cambridge University Press.

Harland, W.B., 1964, Critical evidence for a great infra-Cambrian glaciation: Geol. Rundsch., v. 54, p. 45-61.

Harland, W.B. and Bidgood, D.E.T., 1959, Palaeomagnetism in some Norwegian Sparagmites and the Late pre-Cambrian Ice Age: Nature, v. 184, p. 1860-1862.

Harland, W.B. and Herod, K.N., 1975, Glaciations through time, in Wright, A.E. and Moseley, F. (eds.), Ice Ages: Ancient and Modern, Seel House Press, Liverpool, p. 189-216.

Hoffman, P.F. and Schrag, D.P., 2000, Snowball Earth: Scientific American, January, p. 69-75.

Hoffman, P.F. and Schrag, D.P., 2002, The snowball Earth hypothesis: testing the limits of global change: Terra Nova, v. 14, p. 129-155.

Hoffman, P.F., Kaufman, A.J., Halverson, G.P., and Schrag, D.P., 1998, A Neoproterozoic Snowball Earth: Science, v. 281, p. 1342-1346.

Hyde, W.T., Crowley, T.J., Baum, S.K., and Peltier, W.R., 2000, Neoproterozoic 'snowball Earth' simulations with a coupled climate/ice-sheet model: Nature, v. 405, p. 425-429.

Kennedy, M.J., Christie-Blick, N., and Prave, A.R., 2001a, Carbon isotopic composition of Neoproterozoic glacial carbonates as a test of paleoceanographic models for snowball Earth phenomena: Geology, v. 29, p. 1135-1138.

Kennedy, M.J., Christie-Blick, N., and Sohl, L.E., 2001b, Are Proterozoic cap carbonates and isotopic excursions a record of gas hydrate destabilization following Earth's coldest intervals?: Geology, v. 29, p. 443-446.

Kennedy, M.J., Runnegar, B., Prave, A.R., Hoffman, K.-H. and Arthur, M.A., 1998, Two or four Neoproterozoic glaciations?: Geology, v. 26, p. 1059-1063.

Kirschvink, J.L., Giados, E.J., Betrani, E., Beukes, N., Gutzmer, J., Maepa, L.N., and Steinberger, R.E., 2000, Paleoproterozoic Snowball Earth; extreme climatic and geochemical global change and its biological consequences: Proceedings National Academy of Sciences 97, p. 1400-1405.

Kuenen, P.H. and Migliorini, C.I., 1950, Turbidity currents as a cause of graded bedding: Journal of Geology, v. 58, p. 91-127.

Lamb, H., 1978, Climatic history and the Future: Princeton University Press, 835 p.

LeGrand, H.E., 1988, Drifting Continents and Shifting Theories: Cambridge University Press, New York, 313 p.

Leeming, D. and Leeming, M., 1994, A Dictionary of Creation Myths: Oxford University Press, 330 p.

Li, Z.X. and Powell, C.M., 2001, An outline of the palaeogeographic evolution of the Australasian region since the beginning of the Neoproterozoic: Earth Science Reviews, v. 53, p. 237-277.

Martin, H., Porada, H. and Walliser, O.H., 1985, Mixtite deposits of the Damara sequence, Namibia: Problem of interpretation. Palaeogeography, Palaeoclimatology, Palaeoecology, v. 51, p. 159-196.

Mawson, D., 1949, The late Precambrian ice-age and glacial record of the Bibliando Dome: Journal and Proceedings of the Royal Society of New South Wales, v. 82, p. 150-174.

Mawson, D., 1958, Letter to Sir Raymond Priestley, in F. Jacka, and E. Jacka (eds.), Mawson's Antarctic Diaries: 1988, Unwin, 414p.

McKenzie, D.P. and Parker, R.L., 1967, The north Pacific: An example of tectonics on a sphere: Nature, v. 216, p. 1276-1280.

Meert, J.G. and Torscik, T.H., 2004, Paleomagnetic constraints on Neoproterozoic 'Snowball Earth' continental reconstructions, in G.S. Jenkins, M.A. McMenamin, C. McKay and L. Sohl, eds., The Extreme Proterozoic: Geology, Geochemistry and climate: American Geophysical Union, Geophysical Monography 146, p. 5-12.

Narbonne, G.M., 1998, The Ediacara biota: a terminal Neoproterozoic experiment in the evolution of life: GSA Today, v. 8, p. 1-6.

North, F.J., 1943, Centenary of the Glacial Theory: Proceedings of the Geologists' Association, LIV, p. 1-28.

O'Brien, C.F., 1971, Sir William Dawson. A Life in Science and Religion: American Philosophical Society, Philadelphia, 207 p.

Pauly, K.A., 1957, The Cause of the Great Ice Ages: Privately printed, 60 p.

Peltier, W.R., Tarasov, L., Vetoretti, G., and Solheim, L.P., 2004, Climate dynamics in deep time: Modeling the "Snowball Bifurcation" and assessing the plausibility of its occurrence, in G.S. Jenkins, M.A. McMenamin, C. McKay and L. Sohl, eds., The Extreme Proterozoic: Geology, Geochemistry and climate: American Geophysical Union, Geophysical Monography 146,, p. 107-124.

Pettijohn, 1984, Diary of an Unrepentant Field Geologist: University of Chicago Press, Chicago, 260 p.

Reusch, H., 1891, Skruinsmerker og moraenegrus eftervist i finmarken fra en period megetaeldre end "istiden": Nor. Geol. Unders., v. 1, p. 97-100.

Sayles, R.W., 1914, The Squantum Tillite: Memoirs of the Museum of Comparative Zoology at Harvard College. v. X.

Sayles, R.W., 1919, Seasonal deposition in aqueoglacial sediments: Memoirs of the Museum of Comparative Zoology at Harvard College. v. XLVII.

Schermerhorn, L.J.G., 1966, Terminology of mixed coarse-fine sediments: Journal of Sedimentary Petrology, v. 36, p. 831-836.

Schermerhorn, L.J.G., 1974, Late Precambrian mixtites: Glacial and/or nonglacial?: American Journal of Science, v. 274, p. 673-824.

Schermerhorn, L.J.G., 1975, Tectonic framework of Late Precambrian supposed glacials: in A.E. Wright and F. Moseley, eds., Ice Ages: Ancient and Modern: Geological Journal Special Publication, p. 241-274.

Shields, G.A., Brasier, M.D., Stille, P., and Dorjnamjaa, D., 2002, Factors contributing to high [sup.13]C values in Cryogenian limestones of western Mongolia: Earth and Planetary Science Letters, v. 196, p. 99-111.

Sohl, L.E., Christie-Blick, N., and Kent, D.V., 1999, Paleomagnetic polarity reversals in the Marinoan (ca. 600 Ma) glacial deposits of Australia: Implications for the duration of low-latitude glaciation in Neoproterozoic time: Geological Society of America, Bulletin, v. 111, p. 1120-1139.

Thompson, M.D. and Bowring, S.A., 2000, Age of the Squantum "tillite", Boston Basin, Massachusetts: U-Pb zircon constraints on terminal Neoproterozoic glaciation: American Journal of Science, v. 300, p. 630-655.

Tojo, B. et al., 1999, Cyclicities in Earth-warming episode recorded in the Rasthof cap carbonate overlying the Neoproterozoic Chuos diamictite in Namibia: Geological Society of America Abstracts with Programs, v. 31, p. 486-487.

Wegener, A.L., 1912, Die entstehung der kontinente: Geologische Rundschau, v. 3, p. 276-292.

Wegener, A.L., 1924, The Origin of Continents and Oceans: Translation J.G.A. Skerl of 3rd German ed., Methuen & Co. Ltd., London.

Wegener, A.L., 1928, Two notes concerning my theory of continental drift, in van der Gracht, W.AJ.M. van Waterschoot, ed., Theory of Continental Drift: A Symposium: American Association of Petroleum Geologists, Tulsa, p. 97-103.

Willis, B., 1944, Continental Drift: Ein marchen: American Journal of Science, v. 242, p. 509-513.

Winterer, E.L., 1963, Late Precambrian pebbly mudstone in Normandy, France, in A.E.M. Nairn, ed., Problems in Paleoclimatology, Interscience, London, p. 159-178.

Young, G.M., 1992, Late Proterozoic stratigraphy and the Canada-Australia connection: Geology, v. 20, p. 215-218.

Young, G.M., 2003, Stratigraphic and tectonic settings of Proterozoic glaciogenic rocks and banded iron-formations: relevance to the Snowball Earth debate: Journal of African Earth Sciences, v. 35, p. 451-466.

Young, G.M. and Gostin, V.A., 1989, An exceptionally thick upper Proterozoic (Sturtian) glacial succession in the Mount Painter area, South Australia: Geological Society of America, Bulletin, v. 101, p. 834-845.

Young, G.M. and Gostin, V.A., 1991, Late Proterozoic (Sturtian) succession of the North Flinders Basin, South Australia: an example of temperate glaciation in an active rift setting, in J.B. Anderson and G.M. Ashley, eds., Glacial Marine Sedimentation: Paleoclimatic Significance, Geological Society of America Special Paper, p. 207-223.

Nicholas Eyles

Environmental Earth Sciences

University of Toronto at Scarborough

Scarborough ON M1C 1A4 Canada

eyles@utsc.utoronto.ca

Accepted as revised 17 September 2004
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