||June 21, 2001
GSA Release No. 01-31
Snowball Fight In Edinburgh
The Snowball Earth theory has been gaining momentum since 1992 when Joseph L. Kirschvink of the California Institute of Technology coined the term. Kirschvink's initial model of an ice-covered Earth was just a beginning. When Paul Hoffman of Harvard University and other colleagues picked up the hypothesis, packed in more evidence, and tossed it to the science community again, it really started to stick.
"This session brings together advocates, antagonists, and undecideds who are experts in geology, atmospheric science, marine geochemistry, and evolutionary biology," explained Paul Hoffman, the session chair. "They'll bring a mix of new discoveries and contrasting perspectives on a highly controversial Snowball Earth theory."
One debated issue concerns the role of methane in the snowball cycle.
Dan Schrag from Harvard University will propose a new, counterintuitive model for the initiation of a snowball Earth. The model involves a slow leak of methane from organic-rich sediments into an atmosphere that was less destructive of methane (i.e. less oxidizing) than the present atmosphere. Because methane is a very potent greenhouse gas (60x more powerful than CO2, mole per mole), atmospheric CO2 levels would adjust downward to compensate for a rise in methane. This is unstable, however, because any interruption of the methane leak would result in rapid loss of methane through oxidation, plunging the Earth into a global glaciation. The evidence such a scenario comes from carbon isotopic records immediately prior to glaciation. This methane 'trigger' for snowball events would be deactivated by a rise of oxygen (a slow leak could not cause methane to build up because it would be destroyed too rapidly). The advent of macro-animals is commonly attributed to a rise in oxygen (which is needed both for their construction and operation), which might explain why snowball events ceased after animals appeared.
Martin Kennedy from the University of California, Riverside, will take a different stand in his address, "The Snowball Earth: Myth or Methane?" Kennedy will present physical, geochemical, and theoretical evidence for an alternative model in which massive destabilization of ice-like methane gas hydrates coincided with postglacial warming. Gas hydrates are an enormous and highly unstable reservoir of potential greenhouse gasses (carbon dioxide and methane) and are increasingly believed by paleoclimatologists to play a critical role in Earth's climate system. Their deposition is favored by cold climatic conditions and would have been at a maximum during the extremely severe Neoproterozoic ice ages. In contrast to the snowball Earth hypothesis, the model is based on a "conventional" modern climate system, but scaled to the colder conditions implied by evidence for low latitude glaciation. The deposition of cap carbonates and with unusual isotopic values is an expected outcome of a large-scale methane release.
Another argument concerns a 'Slushball' Earth-an idea that predated the Snowball Earth. One of the questions it now raises is: Did the tropical seas remain open during Snowball Earth?
Simple climate models imply that ice-albedo feedback makes a partially ice-covered planet unstable if ice cover exceeds ~50% surface area. The instability results in total ice cover (i.e. so-called 'hard' snowball Earth). Recently, more complex climate models suggest that a partially ice covered planet may be stable (although simulation times do not exceed a few decades) with up to 40% open water in the tropics. This so-called 'soft' snowball, or 'slushball' Earth appeals to many biologists, who are concerned for the survivability of eukaryotic algae and early micro-animals if any existed. Bruce Runnegar from UCLA will make this argument at the session. In fact, Joe Kirschvink's original snowball Earth hypothesis allowed for patches of open water in the tropics, shifting back and forth across the equator with the seasons.
The counter-arguments are the following: (i) the long-term stability of 'slushball' Earth solutions has not been demonstrated; (ii) ice lines will rapidly recede as CO2 builds up due to complete continental ice cover (eliminating crustal rock weathering which normally consumes CO2). Thus, a 'slushball' Earth will not be long-lived (as indicated by paleomagnetic evidence), and would not produce iron-formations or cap carbonates, as observed in the rock record; (iii) Sea ice in the tropics would be <20 m thick, permitting algae to grow and micro-animals to feed even if no open water were present.
The hydrological cycle on a Snowball Earth is another area of disagreement.
Geological evidence implies that mobile (i.e. thick, wet-based) glaciers existed at least locally during Neoproterozoic ice ages. If the oceans were ice covered, where would the moisture come from to allow glaciers to grow? The presence of thick accumulations of glacial debris, it is argued, negates a frozen ocean. Jim Walker (University of Michigan) has basically reached the same conclusion, but not on the basis of geological evidence. His arguments are based on climate theory and he will examine what the weather would have been like on Snowball Earth. On theoretical grounds, he has come to the conclusion that the surface of the ice would have melted during the summer, providing a moist environment.
The counter argument is that ablation of sea ice in the tropics will provide sufficient moisture for glaciers to slowly grow along elevated sea coasts because of the lapse rate (decrease in air temperature, hence moisture-holding capacity, with elevation). Because a Snowball Earth will be long-lived (millions of years), even a very slow rate of glacier growth (10 cm annually) will make a ice 1000 m thick in 10,000 years. Modeling results were presented at the recent American Geophysical Union meeting in Boston supporting the buildup of thick glaciers on a Snowball Earth. Moreover, as atmospheric CO2 builds up from volcanic outgassing, the Snowball Earth will become warmer and warmer, increasing the sea ice ablation rates and the glacier accumulation rates.
Another point of Snowball contention concerns the evidence for high orbital obliquity.
Certain structures like ice or sand wedges are common in permafrost soils and are normally attributed to large seasonal temperature fluctuations. In South Australia, these structures occur in an area believed to have been close to the equator when it was glaciated. Seasonal temperature fluctuations are normally small near the equator (and diurnal fluctuations are too rapid to produce the observed structures). The structures have been interpreted (principally by George Williams at Adelaide University) as indicating that the Earth had a high orbital obliquity during the pre-Cambrian (i.e. a large angle between the equatorial and ecliptic planes).
With very high obliquity (over 54 degrees), the tropics would be colder on a mean annual basis than the polar regions, thus favoring low-latitude glaciation. Grant Young (University of Western Ontario) will make this argument in his presentation, "Is the Snowball a "No-ball"?: The Case against the Snowball Earth Hypothesis."
"The occurrence of glaciers and highly variable seasonal temperatures in the tropics is perhaps better explained by an Earth that was radically different--for example, the Earth's rotational axis may have been inclined at a much higher angle than today's, throwing traditional latitude-related seasonality into a spin," Young said. "Another possibility is that the Earth's magnetic field was different in the geologic past--instead of the familiar two magnetic poles, the Earth's field may have had four or more, so that the magnetic evidence of tropical glaciations may be spurious. There is no doubt that the Earth underwent climatic convulsions twice in its long history but we are far from understanding their causes or the physical parameters that existed on Earth when they took place."
The arguments against high obliquity are as follows: (i) it results in hot summers at all latitudes, which makes it difficult to for glaciers to grow; (ii) widely observed sedimentary features (e.g. iron-formations, cap carbonates, large stable isotope shifts) are not explained; (iii) there is no credible mechanism to lower the obliquity at the end of the pre-Cambrian; (iv) there may be other means of producing ice/sand wedges without strong seasonality (e.g. surge-type glaciers). The latter point, at least, will be brought up by Paul Hoffman for discussion during the Snowball Earth workshop that immediately follows the session.
This is a sampling of a few of the arguments and different perspectives of the Snowball Earth session that will take place in Edinburgh. While Paul Hoffman 'promises' to keep silent as he fulfills his role as session chair, that "hat" comes off when he enters the workshop when the real debates begin. Weather forecast? Stormy and unpredictable.
During the Earth System Processes meeting, June 25-28, contact the GSA/GSL Newsroom at the Edinburgh International Conference Centre for assistance and to arrange for interviews: +44 (0) 131 519 4134
Ted Nield, GSL Science and Communications Officer
Ann Cairns, GSA Director of Communications
The abstract for this presentation is available at: http://gsa.confex.com/gsa/2001ESP/finalprogram/abstract_186.htm
Post-meeting contact information:
Earth and Planetary Science
20 Oxford St.
Cambridge, MA 02138,
Office Phone: +01 617 496 6380
Geological Society of London
+44 (0) 20 7434 9944
Geological Society of America
+01 303 447 2020 ext. 1156
To view other Earth System Processes press releases, see