Proterozoic snowball periods
-1000 —
–
-950 —
–
-900 —
–
-850 —
–
-800 —
–
-750 —
–
-700 —
–
-650 —
–
-600 —
–
-550 —
A recent estimate of the timing and duration of Proterozoic glacial periods. Note that great uncertainty surrounds the dating of pre-
Gaskiers glaciations. The status of the Kaigas is not clear; its dating is very insecure and many workers do not recognise it as a glaciation. From Smith 2009.
[1] An earlier and longer possible snowball phase, the
Huronian glaciation, is not shown here.
The
Snowball Earth hypothesis posits that the
Earth's surface became entirely or nearly entirely frozen at least once, some time earlier than 650
Mya (million years ago). Proponents of the hypothesis argue that it best explains
sedimentary deposits generally regarded as of
glacial origin at
tropical paleolatitudes, and other otherwise enigmatic features in the
geological record. Opponents of the hypothesis contest the implications of the geological evidence for global glaciation, the
geophysical feasibility of an
ice- or
slush-covered ocean,
[2][3] and the difficulty of escaping an all-frozen condition. There are a number of unanswered questions, including whether the Earth was a full snowball, or a "slushball" with a thin equatorial band of open (or seasonally open) water.
The geological time frames under consideration come before the sudden appearance of multicellular life forms on Earth known as the
Cambrian explosion, and the most recent snowball episode may have triggered the evolution of multi-cellular life on Earth. Another, much earlier and longer, snowball episode, the
Huronian glaciation, which occurred 2400 to 2100 Ma may have been triggered by the first appearance of oxygen in the atmosphere, the "
Great Oxygenation Event."
History
Sir
Douglas Mawson (1882–1958), an Australian geologist and Antarctic explorer, spent much of his career studying the
Neoproterozoic stratigraphy of South Australia where he identified thick and extensive glacial sediments and late in his career speculated about the possibility of global glaciation.
[4]
Mawson's ideas of global glaciation, however, were based on the mistaken assumption that the geographic position of Australia, and that of other continents where low-latitude glacial deposits are found, has remained constant through time. With the advancement of the
continental drift hypothesis, and eventually
plate tectonic theory, came an easier explanation for the glaciogenic sediments—they were deposited at a point in time when the continents were at higher latitudes.
In 1964, the idea of global-scale glaciation reemerged when
W. Brian Harland published a paper in which he presented
palaeomagnetic data showing that glacial
tillites in
Svalbard and
Greenland were deposited at tropical latitudes.
[5] From this palaeomagnetic data, and the sedimentological evidence that the glacial sediments interrupt successions of rocks commonly associated with tropical to temperate latitudes, he argued for an ice age that was so extreme that it resulted in the deposition of marine glacial rocks in the tropics.
In the 1960s,
Mikhail Budyko, a Russian climatologist, developed a simple energy-balance climate model to investigate the effect of ice cover on global
climate. Using this model, Budyko found that if ice sheets advanced far enough out of the polar regions, a feedback loop ensued where the increased reflectiveness (
albedo) of the ice led to further cooling and the formation of more ice, until the entire Earth was covered in ice and stabilized in a new ice-covered equilibrium.
[6] While Budyko's model showed that this ice-albedo
stability could happen, he concluded that it had never happened, because his model offered no way to escape from such a scenario.
The term "snowball Earth" was coined by
Joseph Kirschvink in a short paper published in 1992 within a lengthy volume concerning the biology of the
Proterozoic eon.
[7] The major contributions from this work were: (1) the recognition that the presence of
banded iron formations is consistent with such a glacial episode and (2) the introduction of a mechanism with which to escape from an ice-covered Earth—the accumulation of
CO
2 from volcanic outgassing leading to an ultra-greenhouse effect.
Franklyn Van Houten's discovery of a consistent geological pattern in which lake levels rose and fell is now known as the "Van Houten cycle." His studies of phosphorus deposits and
banded iron formations in sedimentary rocks made him an early adherent of the "snowball Earth" hypothesis postulating that the planet's surface froze more than 650 million years ago.
[8]
Interest in the snowball Earth increased dramatically after
Paul F. Hoffman applied Kirschvink's ideas to a succession of Neoproterozoic sedimentary rocks in
Namibia and elaborated upon the hypothesis by incorporating such observations as the occurrence of
cap carbonates in the journal
Science in 1998.
[9]
In 2010, Francis MacDonald reported evidence that Pangaea was at equatorial latitude during the
Cryogenian with glacial ice at or below sea level and the associated
Sturtian glaciation was global.
[10][11]
Evidence
The snowball Earth hypothesis was originally devised to explain the apparent presence of glaciers at tropical latitudes.
[12] Modeling suggested that once glaciers spread to within 30° of the equator, an
ice-albedo feedback would result in the ice rapidly advancing to the equator
[13] (further modelling shows that ice can in fact get as close as 25° or closer to the equator without initiating total glaciation
[14]). Therefore, the presence of glacial deposits seemingly within the tropics appeared to point to global ice cover.
Critical to an assessment of the validity of the theory, therefore, is an understanding of the reliability and significance of the evidence that led to the belief that ice ever reached the tropics. This evidence must prove two things:
- that a bed contains sedimentary structures that could have been created only by glacial activity;
- that the bed lay within the tropics when it was deposited.
During a period of global glaciation, it must also be demonstrated that glaciers were active at different global locations at the same time, and that no other deposits of the same age are in existence.
This last point is very difficult to prove. Before the
Ediacaran, the biostratigraphic markers usually used to correlate rocks are absent; therefore there is no way to prove that rocks in different places across the globe were deposited at the same time. The best that can be done is to estimate the age of the rocks using radiometric methods, which are rarely accurate to better than a million years or so.
[15]
The first two points are often the source of contention on a case-to-case basis. Many glacial features can also be created by non-glacial means, and estimating the latitude of landmasses even as little as
200 million years ago can be riddled with difficulties.
[16]
Palaeomagnetism
The snowball Earth hypothesis was first posited in order to explain what were then considered to be glacial deposits near the equator. Since tectonic plates move in time, ascertaining their position at a given point in history is not easy. In addition to considerations of how the recognisable landmasses could have fit together, the latitude at which a rock was deposited can be constrained by palaeomagnetism.
When
sedimentary rocks form, magnetic minerals within them tend to align themselves with the Earth's magnetic field. Through the precise measurement of this
palaeomagnetism, it is possible to estimate the
latitude (but not the
longitude) where the rock matrix was deposited. Paleomagnetic measurements have indicated that some sediments of glacial origin in the
Neoproterozoic rock record were deposited within 10 degrees of the equator,
[17] although the accuracy of this reconstruction is in question.
[15] This palaeomagnetic location of apparently glacial sediments (such as
dropstones) has been taken to suggest that glaciers extended to sea-level in the tropical latitudes. It is not clear whether this can be taken to imply a global glaciation, or the existence of localised, possibly land-locked, glacial regimes.
[18] Others have even suggested that most data do not constrain any glacial deposits to within 25° of the equator.
[19]
Skeptics suggest that the palaeomagnetic data could be corrupted if the Earth's magnetic field was substantially different from today's. Depending on the rate of cooling of the Earth's core, it is possible that during the Proterozoic, its
magnetic field did not approximate a
dipolar distribution, with a North and South pole roughly aligning with the planet's axis as they do today. Instead, a hotter core may have circulated more vigorously and given rise to 4, 8 or more poles. Paleomagnetic data would then have to be re-interpreted as particles could align pointing to a 'West Pole' rather than the North Pole. Alternatively, the Earth's dipolar field could have oriented such that the poles were close to the equator. This hypothesis has been posited to explain the extraordinarily rapid motion of the magnetic poles implied by the Ediacaran palaeomagnetic record; the alleged motion of the north pole would occur around the same time as the Gaskiers glaciation.
[20]
Another weakness of reliance on palaeomagnetic data is the difficulty in determining whether the magnetic signal recorded is original, or whether it has been reset by later activity. For example, a mountain-building
orogeny releases hot water as a by-product of metamorphic reactions; this water can circulate to rocks thousands of kilometers away and reset their magnetic signature. This makes the authenticity of rocks older than a few million years difficult to determine without painstaking mineralogical observations.
[14] Moreover, further evidence is accumulating that large-scale remagnetization events have taken place, that may require revision of the position of the paleomagnetic poles.
[21][22]
There is currently only one deposit, the Elatina deposit of Australia, that was indubitably deposited at low latitudes; its depositional date is well constrained, and the signal is demonstrably original.
[23]
Low-latitude glacial deposits
Sedimentary rocks that are deposited by glaciers have distinctive features that enable their identification. Long before the advent of the
snowball Earth hypothesis many
Neoproterozoic sediments had been interpreted as having a glacial origin, including some apparently at tropical latitudes at the time of their deposition. However, it is worth remembering that many sedimentary features traditionally associated with glaciers can also be formed by other means.
[24] Thus the glacial origin of many of the key occurrences for snowball Earth has been contested.
[15] As of 2007, there was only one "very reliable" – still challenged
[15] – datum point identifying tropical
tillites,
[17] which makes statements of equatorial ice cover somewhat presumptuous. However evidence of sea-level glaciation in the tropics during the
Sturtian is accumulating.
[25] Evidence of possible glacial origin of sediment includes:
- Dropstones (stones dropped into marine sediments), which can be deposited by glaciers or other phenomena.[26]
- Varves (annual sediment layers in periglacial lakes), which can form at higher temperatures.[27]
- Glacial striations (formed by embedded rocks scraped against bedrock): similar striations are from time to time formed by mudflows or tectonic movements.[28]
- Diamictites (poorly sorted conglomerates). Originally described as glacial till, most were in fact formed by debris flows.[15]
Open-water deposits
It appears that some deposits formed during the snowball period could only have been formed in the presence of an active hydrological cycle. Bands of glacial deposits up to 5,500 meters thick, separated by small (meters) bands of non-glacial sediments, demonstrate that glaciers were melting and re-forming repeatedly for tens of millions of years; solid oceans would not permit this scale of deposition.
[29] It is considered possible that
ice streams such as seen in
Antarctica today could be responsible for these sequences. Further, sedimentary features that could only form in open water, for example
wave-formed ripples, far-traveled
ice-rafted debris and indicators of photosynthetic activity, can be found throughout sediments dating from the snowball Earth periods. While these may represent 'oases' of
meltwater on a completely frozen Earth,
[30] computer modelling suggests that large areas of the ocean must have remained ice free arguing that a "hard" snowball is not plausible in terms of energy balance and general circulation models.
[31]
Carbon isotope ratios
There are two stable
isotopes of carbon in
sea water:
carbon-12 (
12C) and the rare
carbon-13 (
13C), which makes up about 1.109 percent of carbon atoms.
Biochemical processes, of which
photosynthesis is one, tend to preferentially incorporate the lighter
12C isotope. Thus ocean-dwelling photosynthesizers, both
protists and
algae, tend to be very slightly depleted in
13C, relative to the abundance found in the primary
volcanic sources of the Earth's carbon. Therefore, an ocean with photosynthetic life will have a lower
13C/
12C ratio within organic remains, and a lower ratio in corresponding ocean water. The organic component of the lithified sediments will forever remain very slightly, but measurably, depleted in
13C.
During the proposed episode of snowball Earth, there are rapid and extreme negative excursions in the ratio of
13C to
12C.
[32] This is consistent with a deep freeze that killed off most or nearly all photosynthetic life – although other mechanisms, such as
clathrate release, can also cause such perturbations. Close analysis of the timing of
13C 'spikes' in deposits across the globe allows the recognition of four, possibly five, glacial events in the late Neoproterozoic.
[33]
Banded iron formations
2.1 billion year old rock with black-band ironstone
Banded iron formations (BIF) are sedimentary rocks of layered
iron oxide and iron-poor
chert. In the presence of oxygen,
iron naturally rusts and becomes insoluble in water. The banded iron formations are commonly very old and their deposition is often related to the oxidation of the Earth's atmosphere during the
Paleoproterozoic era, when dissolved iron in the ocean came in contact with photosynthetically produced oxygen and precipitated out as iron oxide.
The bands were produced at the
tipping point between an
anoxic and an oxygenated ocean. Since today's atmosphere is
oxygen rich (nearly 21 percent by volume) and in contact with the oceans, it is not possible to accumulate enough iron oxide to deposit a banded formation. The only extensive iron formations that were deposited after the Paleoproterozoic (after 1.8 billion years ago) are associated with
Cryogenian glacial deposits.
For such iron-rich rocks to be deposited there would have to be anoxia in the ocean, so that much dissolved iron (as
ferrous oxide) could accumulate before it met an oxidant that would precipitate it as
ferric oxide. For the ocean to become anoxic it must have limited gas exchange with the oxygenated atmosphere. Proponents of the hypothesis argue that the reappearance of BIF in the sedimentary record is a result of limited oxygen levels in an ocean sealed by sea ice,
[7] while opponents suggest that the rarity of the BIF deposits may indicate that they formed in inland seas.
Being isolated from the oceans, such lakes may have been stagnant and anoxic at depth, much like today's
Black Sea; a sufficient input of iron could provide the necessary conditions for BIF formation.
[15] A further difficulty in suggesting that BIFs marked the end of the glaciation is that they are found interbedded with glacial sediments.
[18] BIFs are also strikingly absent during the
Marinoan glaciation.
[citation needed]
Cap carbonate rocks
Volcanoes may have had a role in replenishing
CO
2, possibly ending the global ice age that was the snowball Earth during the
Cryogenian Period.
Around the top of
Neoproterozoic glacial deposits there is commonly a sharp transition into a chemically precipitated sedimentary
limestone or
dolostone metres to tens of metres thick.
[34] These cap carbonates sometimes occur in sedimentary successions that have no other carbonate rocks, suggesting that their deposition is result of a profound aberration in ocean chemistry.
[35]
These cap carbonates have unusual chemical composition, as well as strange sedimentary structures that are often interpreted as large ripples.
[36] The formation of such sedimentary rocks could be caused by a large influx of positively charged
ions, as would be produced by rapid weathering during the extreme greenhouse following a snowball Earth event. The
δ13C isotopic signature of the cap carbonates is near −5 ‰, consistent with the value of the mantle — such a low value is usually/could be taken to signify an absence of life, since photosynthesis usually acts to raise the value; alternatively the release of methane deposits could have lowered it from a higher value, and counterbalance the effects of photosynthesis.
The precise mechanism involved in the formation of cap carbonates is not clear, but the most cited explanation suggests that at the melting of a snowball Earth, water would dissolve the abundant
CO
2 from the
atmosphere to form
carbonic acid, which would fall as
acid rain. This would weather exposed
silicate and
carbonate rock (including readily attacked glacial debris), releasing large amounts of
calcium, which when washed into the ocean would form distinctively textured layers of carbonate sedimentary rock. Such an
abiotic "
cap carbonate" sediment can be found on top of the glacial till that gave rise to the snowball Earth hypothesis.
However, there are some problems with the designation of a glacial origin to cap carbonates. Firstly, the high carbon dioxide concentration in the atmosphere would cause the oceans to become acidic, and dissolve any carbonates contained within — starkly at odds with the deposition of cap carbonates. Further, the thickness of some cap carbonates is far above what could reasonably be produced in the relatively quick deglaciations. The cause is further weakened by the lack of cap carbonates above many sequences of clear glacial origin at a similar time and the occurrence of similar carbonates within the sequences of proposed glacial origin.
[15] An alternative mechanism, which may have produced the
Doushantuo cap carbonate at least, is the rapid, widespread release of methane. This accounts for incredibly low — as low as −48 ‰ —
δ13C values — as well as unusual sedimentary features which appear to have been formed by the flow of gas through the sediments.
[37]
Changing acidity
Isotopes of the element
boron suggest that the
pH of the oceans dropped dramatically before and after the
Marinoan glaciation.
[38] This may indicate a buildup of
carbon dioxide in the atmosphere, some of which would dissolve into the oceans to form
carbonic acid. Although the boron variations may be evidence of extreme climate change, they need not imply a global glaciation.
Space dust
The Earth's surface is very depleted in the element
iridium, which primarily resides in the
Earth's core. The only significant source of the element at the surface is
cosmic particles that reach Earth.
During a snowball Earth, iridium would accumulate on the ice sheets, and when the ice melted the resulting layer of sediment would be rich in iridium. An
iridium anomaly has been discovered at the base of the cap carbonate formations, and has been used to suggest that the glacial episode lasted for at least 3 million years,
[39] but this does not necessarily imply a
global extent to the glaciation; indeed, a similar anomaly could be explained by the impact of a large
meteorite.
[40]
Cyclic climate fluctuations
Using the ratio of mobile
cations to those that remain in soils during
chemical weathering (the chemical index of alteration), it has been shown that chemical weathering varied in a cyclic fashion within a glacial succession, increasing during interglacial periods and decreasing during cold and arid glacial periods.
[41] This pattern, if a true reflection of events, suggests that the "snowball Earths" bore a stronger resemblance to
Pleistocene ice age cycles than to a completely frozen Earth.
What's more, glacial sediments of the
Portaskaig formation in Scotland clearly show interbedded cycles of glacial and shallow marine sediments.
[42] The significance of these deposits is highly reliant upon their dating. Glacial sediments are difficult to date, and the closest dated bed to the Portaskaig group is 8 km stratigraphically above the beds of interest. Its dating to 600 Ma means the beds can be tentatively correlated to the Sturtian glaciation, but they may represent the advance or retreat of a snowball Earth.
Mechanisms
One computer simulation of conditions during a snowball Earth period
[43]
The initiation of a snowball Earth event would involve some initial cooling mechanism, which would result in an increase in the Earth's coverage of snow and ice. The increase in Earth's coverage of snow and ice would in turn increase the Earth's
albedo, which would result in
positive feedback for cooling. If enough snow and ice accumulates, runaway cooling would result. This positive feedback is facilitated by an equatorial continental distribution, which would allow ice to accumulate in the regions closer to the equator, where
solar radiation is most direct.
Many possible triggering mechanisms could account for the beginning of a snowball Earth, such as the eruption of a
supervolcano, a reduction in the atmospheric concentration of
greenhouse gases such as
methane and/or
carbon dioxide, changes in
solar energy output, or perturbations of the
Earth's orbit. Regardless of the trigger, initial cooling results in an increase in the area of the Earth's surface covered by ice and snow, and the additional ice and snow reflects more solar energy back to space, further cooling the Earth and further increasing the area of the Earth's surface covered by ice and snow. This positive feedback loop could eventually produce a frozen
equator as cold as modern-day
Antarctica.
Global warming associated with large accumulations of carbon dioxide in the atmosphere over millions of years, emitted primarily by volcanic activity, is the proposed trigger for melting a snowball Earth. Due to positive feedback for melting, the eventual melting of the snow and ice covering most of the Earth's surface would require as little as 1,000 years.
Continental distribution
A tropical distribution of the continents is, perhaps counter-intuitively, necessary to allow the initiation of a snowball Earth.
[44] Firstly, tropical continents are more reflective than open ocean, and so absorb less of the Sun's heat: most absorption of solar energy on Earth today occurs in tropical oceans.
[45]
Further, tropical continents are subject to more rainfall, which leads to increased river discharge — and erosion. When exposed to air,
silicate rocks undergo weathering reactions which remove carbon dioxide from the atmosphere. These reactions proceed in the general form: Rock-forming mineral + CO
2 + H
2O → cations + bicarbonate + SiO
2. An example of such a reaction is the weathering of
wollastonite:
- CaSiO3 + 2CO2 + H2O → Ca2+ + SiO2 + 2HCO3−
The released
calcium cations react with the dissolved
bicarbonate in the ocean to form
calcium carbonate as a chemically precipitated
sedimentary rock. This transfers
carbon dioxide, a greenhouse gas, from the air into the
geosphere, and, in steady-state on geologic time scales, offsets the carbon dioxide emitted from
volcanoes into the atmosphere.
A paucity of suitable sediments for analysis makes precise continental distribution during the Neoproterozoic difficult to establish.
[46] Some reconstructions point towards polar continents — which have been a feature of all other major glaciations, providing a point upon which ice can nucleate. Changes in ocean circulation patterns may then have provided the trigger of snowball Earth.
[47]
Additional factors that may have contributed to the onset of the Neoproterozoic snowball include the introduction of atmospheric free oxygen, which may have reached sufficient quantities to react with
methane in the atmosphere, oxidizing it to carbon dioxide, a much weaker greenhouse gas,
[48] and a younger — thus fainter — Sun, which would have emitted 6 percent less radiation in the Neoproterozoic.
[15]
Normally, as the Earth gets colder due to natural climatic fluctuations and changes in incoming solar radiation, the cooling slows these weathering reactions. As a result, less carbon dioxide is removed from the atmosphere and the Earth warms as this greenhouse gas accumulates — this '
negative feedback' process limits the magnitude of cooling. During the
Cryogenian period, however, the Earth's continents were all at
tropical latitudes, which made this moderating process less effective, as high weathering rates continued on land even as the Earth cooled. This let ice advance beyond the polar regions. Once ice advanced to within 30° of the equator,
[49] a positive feedback could ensue such that the increased reflectiveness (
albedo) of the ice led to further cooling and the formation of more ice, until the whole Earth is ice covered.
Polar continents, due to low rates of
evaporation, are too dry to allow substantial carbon deposition — restricting the amount of atmospheric carbon dioxide that can be removed from the
Carbon cycle. A gradual rise of the proportion of the
isotope carbon-13 relative to carbon-12 in sediments pre-dating "global" glaciation indicates that
CO
2 draw-down before snowball Earths was a slow and continuous process.
[50]
The start of snowball Earths are always marked by a sharp downturn in the δ
13C value of sediments,
[51] a hallmark that may be attributed to a crash in biological productivity as a result of the cold temperatures and ice-covered oceans.
During the frozen period
Global ice sheets may have delayed or prevented the establishment of multicellular life.
[citation needed]
Global temperature fell so low that the equator was as cold as modern-day
Antarctica.
[52] This low temperature was maintained by the high albedo of the ice sheets, which reflected most incoming solar energy into space. A lack of heat-retaining clouds, caused by water vapor freezing out of the atmosphere, amplified this effect.
Breaking out of global glaciation
The
carbon dioxide levels necessary to unfreeze the Earth have been estimated as being 350 times what they are today, about 13% of the atmosphere.
[53] Since the Earth was almost completely covered with ice, carbon dioxide could not be withdrawn from the atmosphere by release of alkaline metal ions weathering out of
siliceous rocks. Over 4 to 30 million years, enough
CO
2 and
methane, mainly emitted by
volcanoes, would accumulate to finally cause enough greenhouse effect to make surface ice melt in the tropics until a band of permanently ice-free land and water developed;
[54] this would be darker than the ice, and thus absorb more energy from the Sun — initiating a "
positive feedback".
On the continents, the melting of
glaciers would release massive amounts of glacial deposit, which would erode and weather. The resulting sediments supplied to the ocean would be high in nutrients such as
phosphorus, which combined with the abundance of
CO
2 would trigger a
cyanobacteria population explosion, which would cause a relatively rapid reoxygenation of the atmosphere, which may have contributed to the rise of the
Ediacaran biota and the subsequent
Cambrian explosion — a higher oxygen concentration allowing large multicellular lifeforms to develop. This
positive feedback loop would melt the ice in geological short order, perhaps less than 1,000 years; replenishment of atmospheric oxygen and depletion of the
CO
2 levels would take further
millennia.
Destabilization of substantial deposits of
methane hydrates locked up in low-latitude
permafrost may also have acted as a trigger and/or strong positive feedback for deglaciation and warming.
[55]
It is possible that carbon dioxide levels fell enough for Earth to freeze again; this cycle may have repeated until the
continents had drifted to more polar latitudes.
[56]
More recent evidence suggests that with colder oceanic temperatures, the resulting higher ability of the oceans to dissolve gases led to the carbon content of sea water being more quickly oxidized to carbon dioxide. This leads directly to an increase of atmospheric carbon dioxide, enhanced greenhouse warming of the surface of the Earth, and the prevention of a total snowball state.
[57]
Slushball Earth hypothesis
While the presence of glaciers is not disputed, the idea that the entire planet was covered in ice is more contentious, leading some scientists to posit a "slushball Earth", in which a band of ice-free, or ice-thin, waters remains around the
equator, allowing for a continued
hydrologic cycle.
This hypothesis appeals to scientists who observe certain features of the sedimentary record that can only be formed under open water, or rapidly moving ice (which would require somewhere ice-free to move to). Recent research observed geochemical cyclicity in
clastic rocks, showing that the "snowball" periods were punctuated by warm spells, similar to
ice age cycles in recent Earth history. Attempts to construct computer models of a snowball Earth have also struggled to accommodate global ice cover without fundamental changes in the laws and constants which govern the planet.
A less extreme snowball earth hypothesis involves continually evolving continental configurations and changes in ocean circulation.
[58] Synthesised evidence has produced models indicating a "slushball Earth",
[59] where the stratigraphic record does not permit postulating complete global glaciations.
[58] Kirschivink's original hypothesis
[7] had recognised that warm tropical puddles would be expected to exist in a snowball earth.
The snowball Earth hypothesis does not explain the alternation of glacial and interglacial events, nor the oscillation of glacial sheet margins.
[60]
Scientific dispute
The argument against the hypothesis is evidence of fluctuation in ice cover and melting during "snowball Earth" deposits. Evidence for such melting comes from evidence of glacial dropstones,
[29] geochemical evidence of climate cyclicity,
[41] and interbedded glacial and shallow marine sediments.
[42] A longer record from Oman, constrained to 13°N, covers the period from 712 to 545 million years ago — a time span containing the
Sturtian and Marinoan glaciations — and shows both glacial and ice-free deposition.
[61]
There have been difficulties in recreating a snowball Earth with
global climate models. Simple GCMs with mixed-layer oceans can be made to freeze to the equator; a more sophisticated model with a full dynamic ocean (though only a primitive sea ice model) failed to form sea ice to the equator.
[62] In addition, the levels of
CO
2 necessary to melt a global ice cover have been calculated to be 130,000 ppm,
[53] which is considered by some
[who?] to be unreasonably large.
Strontium isotopic data have been found to be at odds with proposed snowball Earth models of silicate weathering shutdown during glaciation and rapid rates immediately post-glaciation.
Therefore, methane release from permafrost during
marine transgression was proposed to be the source of the large measured carbon excursion in the time immediately after glaciation.
[63]
"Zipper rift" hypothesis
Nick Eyles suggest that the Neoproterozoic Snowball Earth was in fact no different from any other glaciation in Earth's history, and that efforts to find a single cause are likely to end in failure.
[15] The "Zipper rift" hypothesis proposes two pulses of continental "unzipping" — first, the breakup of the supercontinent
Rodinia, forming the proto-Pacific ocean; then the splitting of the continent
Baltica from
Laurentia, forming the proto-Atlantic — coincided with the glaciated periods. The associated tectonic uplift would form high plateaus, just as the
East African Rift is responsible for high topography; this high ground could then host glaciers.
Banded iron formations have been taken as unavoidable evidence for global ice cover, since they require dissolved iron ions and anoxic waters to form; however, the limited extent of the Neoproterozoic banded iron deposits means that they may not have formed in frozen oceans, but instead in inland seas. Such seas can experience a wide range of chemistries; high rates of evaporation could concentrate iron ions, and a periodic lack of circulation could allow anoxic bottom water to form.
Continental rifting, with associated subsidence, tends to produce such landlocked water bodies. This rifting, and associated subsidence, would produce the space for the fast deposition of sediments, negating the need for an immense and rapid melting to raise the global sea levels.
High-obliquity hypothesis
A competing hypothesis to explain the presence of ice on the equatorial continents was that the Earth's
axial tilt was quite high, in the vicinity of 60°, which would place the Earth's land in high "latitudes", although supporting evidence is scarce.
[64] A less extreme possibility would be that it was merely the Earth's
magnetic pole that wandered to this inclination, as the magnetic readings which suggested ice-filled continents depends on the magnetic and rotational poles being relatively similar.
In either of these two situations, the freeze would be limited to relatively small areas, as is the case today; severe changes to the Earth's climate are not necessary.
Inertial interchange true polar wander
The evidence for low latitude glacial deposits during the supposed snowball Earth episodes has been reinterpreted via the concept of inertial interchange
true polar wander (IITPW).
[65][66] This hypothesis, created to explain palaeomagnetic data, suggests that the Earth's axis of rotation shifted one or more times during the general timeframe attributed to snowball Earth. This could feasibly produce the same distribution of glacial deposits without requiring any of them to have been deposited at equatorial latitude.
[67] While the physics behind the proposition is sound, the removal of one flawed data point from the original study rendered the application of the concept in these circumstances unwarranted.
[68]
Several alternative explanations for the evidence have been proposed.
Survival of life through frozen periods
A tremendous glaciation would curtail photosynthetic life on Earth, thus letting the atmospheric oxygen be drastically depleted and perhaps even disappear, and thus allow non-oxidized iron-rich rocks to form.
Detractors argue that this kind of glaciation would have made life extinct entirely. However, microfossils such as
stromatolites and
oncolites prove that, in shallow marine environments at least, life did not suffer any perturbation. Instead life developed a trophic complexity and survived the cold period unscathed.
[69] Proponents counter that it may have been possible for life to survive in these ways:
- In reservoirs of anaerobic and low-oxygen life powered by chemicals in deep oceanic hydrothermal vents surviving in Earth's deep oceans and crust; but photosynthesis would not have been possible there.
- As eggs and dormant cells and spores deep-frozen into ice right through the most severe phases of the frozen period.
- Under the ice layer, in chemolithotrophic (mineral-metabolizing) ecosystems theoretically resembling those in existence in modern glacier beds, high-alpine and Arctic talus permafrost, and basal glacial ice. This is especially plausible in areas of volcanism or geothermal activity.[70]
- In deep ocean regions far from the supercontinent Rodinia or its remnants as it broke apart and drifted on the tectonic plates, which may have allowed for some small regions of open water preserving small quantities of life with access to light and CO
2 for photosynthesizers (not multicellular plants, which did not yet exist) to generate traces of oxygen that were enough to sustain some oxygen-dependent organisms. This would happen even if the sea froze over completely, if small parts of the ice were thin enough to admit light.
- In nunatak areas in the tropics, where daytime tropical sun or volcanic heat heated bare rock sheltered from cold wind and made small temporary melt pools, which would freeze at sunset.
- In pockets of liquid water within and under the ice caps, similar to Lake Vostok in Antarctica. In theory, this system may resemble microbial communities living in the perennially frozen lakes of the Antarctic dry valleys. Photosynthesis can occur under ice up to 100 m thick, and at the temperatures predicted by models equatorial sublimation would prevent equatorial ice thickness from exceeding 10 m.[71]
- In small oases of liquid water, as would be found near geothermal hotspots resembling Iceland today.[72]
However, organisms and ecosystems, as far as it can be determined by the fossil record, do not appear to have undergone the significant change that would be expected by a
mass extinction. With the advent of more precise dating, a phytoplankton extinction event which had been associated with snowball Earth was shown to precede glaciations by 16 million years.
[73] Even if life were to cling on in all the ecological refuges listed above, a whole-Earth glaciation would result in a biota with a noticeably different diversity and composition. This change in diversity and composition has not yet been observed
[74]– in fact, the organisms which should be most susceptible to climatic variation emerge unscathed from the snowball Earth.
[40]
Implications
A snowball Earth has profound implications in the history of
life on Earth. While many
refugia have been postulated, global ice cover would certainly have ravaged
ecosystems dependent on sunlight.
Geochemical evidence from rocks associated with low-latitude glacial deposits have been interpreted to show a crash in oceanic life during the glacials.
The melting of the ice may have presented many new opportunities for diversification, and may indeed have driven the rapid evolution which took place at the end of the
Cryogenian period.
Effect on early evolution
The
Neoproterozoic was a time of remarkable diversification of multicellular organisms, including animals. Organism size and complexity increased considerably after the end of the snowball glaciations. This development of multicellular organisms may have been the result of increased evolutionary pressures resulting from multiple
icehouse-hothouse cycles; in this sense, snowball Earth episodes may have "pumped" evolution. Alternatively, fluctuating nutrient levels and rising oxygen may have played a part. Interestingly, another major glacial episode may have ended just a few million years before the
Cambrian explosion.
Mechanistically, the impact of snowball Earth (in particular the later glaciations) on complex life is likely to have occurred through the process of
kin selection. Organ-scale differentiation, in particular the terminal (irreversible) differentiation present in animals, requires the individual cell (and the genes contained within it) to "sacrifice" their ability to reproduce, so that the colony is not disrupted. From the short-term perspective of the gene, more offspring will be gained by causing the cell in which it is contained to ignore any signals received from the colony, and to reproduce at the maximum rate, regardless of the implications for the wider group. Today, this incentive explains the formation of tumours in animals and plants.
It has been argued
[75] that because snowball Earth would undoubtedly have decimated the population size of any given species, the extremely small populations that resulted would all have been descended from a small number of individuals (see
founder effect), and consequently the average relatedness between any two individuals (in this case individual cells) would have been exceptionally high as a result of glaciations. Altruism is known to increase from rarity when relatedness (R) exceeds the ratio of the cost (C) to the altruist (in this case, the cell giving up its own reproduction by differentiating), to the benefit (B) to the recipient of altruism (the germ line of the colony, that reproduces as a result of the differentiation), i.e. R > C/B (see
Hamilton's rule). The evolutionary pressure of the high relatedness in the context of a post-glaciation population boom may have been sufficient to overcome the reproductive cost of forming a complex animal, for the first time in Earth's history.
There is also a rival hypothesis which has been gaining currency in recent years: that early snowball Earths did not so much
affect the evolution of life on Earth as result from it. In fact the two hypotheses are not mutually exclusive. The idea is that Earth's life forms affect the global carbon cycle and so major evolutionary events alter the carbon cycle, redistributing carbon within various reservoirs within the biosphere system and in the process temporarily lowering the atmospheric (greenhouse) carbon reservoir until the revised biosphere system settled into a new state. The Snowball I episode (of the
Huronian glaciation 2.4 to 2.1 billion years) and Snowball II (of the Precambrian's Cryogenian between 580 – 850 million years and which itself had a number of distinct episodes) are respectively thought to be caused by the evolution of
oxygenic photosynthesis and then the rise of more advanced multicellular animal life and life's colonization of the land.
[76][77]
Effects on ocean circulation
Global ice cover, if it existed, may – in concert with geothermal heating – have led to a lively, well mixed ocean with great vertical convective circulation.
[78]
Occurrence and timing of snowball Earths
Neoproterozoic
There are three or four significant ice ages during the late
Neoproterozoic. Of these, the Marinoan was the most significant, and the Sturtian glaciations were also truly widespread.
[79] Even the leading snowball proponent Hoffman agrees that the ~million year long Gaskiers glaciation did not lead to global glaciation,
[44] although it was probably as intense as the
late Ordovician glaciation. The status of the Kaigas "glaciation" or "cooling event" is currently unclear; some workers do not recognise it as a glacial, others suspect that it may reflect poorly dated strata of Sturtian association, and others believe it may indeed be a third ice age.
[80] It was certainly less significant than the
Sturtian or
Marinoan glaciations, and probably not global in extent. Emerging evidence suggests that the Earth underwent a number of glaciations during the Neoproterozoic, which would stand strongly at odds with the snowball hypothesis.
[3]
Paleoproterozoic
The snowball Earth hypothesis has been invoked to explain glacial deposits in the
Huronian Supergroup of Canada, though the palaeomagnetic evidence that suggests ice sheets at low latitudes is contested.
[81][82] The glacial sediments of the Makganyene formation of South Africa are slightly younger than the Huronian glacial deposits (~2.25 billion years old) and were deposited at tropical latitudes.
[83] It has been proposed that rise of free oxygen that occurred during the
Great Oxygenation Event removed methane in the atmosphere through oxidation. As the
Sun was notably weaker at the time, the Earth's climate may have relied on methane, a powerful greenhouse gas, to maintain surface temperatures above freezing.
In the absence of this methane greenhouse, temperatures plunged and a snowball event could have occurred.
[82]
Karoo Ice Age
Before the theory of continental drift, glacial deposits in
Carboniferous strata in tropical continents areas such as India and South America led to speculation that the
Karoo Ice Age glaciation reached into the tropics. However, a continental reconstruction shows that ice was in fact constrained to the polar parts of the
supercontinent Gondwana.
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