Core solidification and the Cambrian explosion: did one begat the other?

Let's face it, we all find it easier to live our lives with the help of patterns. Whether it's a daily routine or consultation of an astrology column (insert expletive of choice here) - or even us amateur astronomers guiding our telescopes via the constellations - our continued existence relies on patterns. After all, if we didn't innately recognise our mother's face or differentiate harmless creatures from the shape of a predator, we wouldn't last long. So it shouldn't be any surprise that scientists also rely on patterns to investigate the complexities of creation.

Richard Feynman once said that a scientific hypothesis starts with a guess, which should perhaps be taken with a pinch of salt. But nonetheless scientists like to use patterns when considering explanations for phenomena; at a first glance, this technique matches the principle of parsimony, or Occam's Razor, i.e. the simplest explanation is usually the correct one - excluding quantum mechanics, of course!

An example in which a potential pattern was widely publicised prior to confirmation via hard data was that of periodic mass extinction, the idea being that a single cause might be behind the five greatest extinction events. Four years after Luis Alvarez's team's suggestion that the 66 million year-old Chicxulub impactor could have caused the Cretaceous-Paleogene extinction, paleontologists David Raup and Jack Sepkoski published a 1984 paper hypothesising extinctions at regular intervals due to extraterrestrial impacts.

This necessitated the existance of an object that could cause a periodic gravitational perturbation, in order for asteroids and comets to be diverted into the inner solar system. The new hypothesis was that we live in binary star system, with a dwarf companion star in an highly elliptical, 26 million-year orbit. This would be responsible for the perturbation when it was at perihelion (i.e. closest approach to the sun).

What's interesting is that despite the lack of evidence, the hypothesis was widely publicised in popular science media, with the death-dealing star being appropriately named Nemesis after the Greek goddess of retribution. After all, the diversification of mammals was a direct result of the K-T extinction and so of no small importance to our species.

Unfortunately, further research has shown that mass extinctions don't fall into a neat 26 million-year cycle. In addition, orbiting and ground-based telescopes now have the ability to detect Nemesis and yet have failed to do so. It appears that the hypothesis has reached a dead end; our local corner of the universe probably just isn't as tidy as we would like it to be.

Now another hypothesis has appeared that might appear to belong in a similar category of neat pattern matching taking precedence over solid evidence. Bearing in mind the importance of the subject under scrutiny - the origin of complex life - are researchers jumping the gun in order to gain kudos if proven correct? A report on 565 million year-old minerals from Quebec, Canada, suggests that at that time the Earth's magnetic field was less than ten percent of what it is today. This is considerably lower than earlier estimate of forty percent. Also, the magnetic poles appear to have reversed far more frequently during this period than they have since.

As this is directly related to the composition of the Earth's core, it has led to speculation that the inner core was then in the final stage of solidification. This would have caused increased movement in the outer liquid, iron-rich core, and thus to the rapid generation of a much higher magnetic field. In turn, the larger the magnetic field dipole intensity, the lower the amount of high energy particles that reach the Earth's surface, both cosmic rays and from our own sun. What is particularly interesting about this time is that it is just (i.e. about twenty million years) prior to the so-called Cambrian explosion, following three billion years or so of only microbial life. So were these geophysical changes responsible for a paradigm shift in evolution? To confirm, we would need to confirm the accuracy of this apparently neat match.

It's well known that some forms of bacteria can survive in much higher radiation environments than us larger scale life forms; extremophiles such as Deinococcus radiodurans have even been found thriving inside nuclear reactors. Therefore it would seem obvious that more complex organisms couldn't evolve until the magnetic field was fairly high. But until circa 430 million years ago there was no life on land (there is now evidence that fungi may have been the first organisms to survive in this harsh environment). If all life was therefore in the sea, wouldn't the deep ocean have provided the necessary radiation protection for early plants and animals?

By 600 million years ago the atmospheric oxygen content was only about ten percent of today's value; clearly, those conditions would not have been much use to pretty much any air-breathing animals we know to have ever existed. In addition, the Ediacaran assemblage, albeit somewhat different from most subsequent higher animals, arose no later than this time - with chemical evidence suggesting their development stretched back a further 100 million years. Therefore the Canadian magnetic mineral evidence seems to be too late for the core solidification/higher magnetic field generation to have given the kick start to a more sophisticated biota.

In addition, we shouldn't forget that it is the ozone layer that acts as an ultraviolet shield; UVB is just as dangerous to many organisms, including near-surface marine life, as cosmic rays and high-energy solar particles. High-altitude ozone is thought to have reached current density by 600 million years ago, with blue-green algae as its primary source. O2 levels also increased at this time, perhaps driven by climate change at the end of a global glaciation.

Although the "Snowball Earth" hypothesis - that at least half of all ocean water was frozen solid during three or four periods of glaciation - is still controversial, there is something of a correlation in time between the geophysical evidence and the emergence of the Ediacaran fauna. As to the cause of this glacial period, it is thought to have been a concatenation of circumstances, with emergent plate tectonics as a primary factor.

How to conclude? Well, we would all like to find neat, obvious solutions, especially to key questions about our own origin. Unfortunately, the hypothesis based on the magnetic mineral evidence appears to selectively ignore the evolution of the Ediacaran life forms and the development of the ozone layer. The correlation between the end of "Snowball Earth" and the Ediacaran biota evolution is on slightly firmer ground, but the period is so long ago that even dating deposits cannot be accurate except to the nearest million years or so.

It's certainly a fascinating topic, so let's hope that one day the evidence will be solid enough for us to finally understand how and when life took on the complexity we take for granted. Meanwhile, I would take any speculation based on new evidence with a Feynman-esque pinch of salt; the universe frequently fails to match the nice, neat, parcels of explanations we would like it to. Isn't that one of the factors that makes science so interesting in the first place?

Valuing the velvet worm: noticing the most inconspicuous of species

Most of the recent television documentaries or books I've encountered that discuss extra-terrestrial life include some description of the weirder species we share our own planet with. Lumped together under the term 'extremophiles' these organisms appear to thrive in environments hostile to most other life forms, from the coolant ponds of nuclear reactors to the boiling volcanic vents of the deep ocean floor.

Although this has rightly gained attention for these often wonderfully-named species (from snottites to tardigrades) there are numerous other lifeforms scarcely noticed by anyone other than a few specialists, quietly going about their unassuming business. However, they may provide a few useful lessons for all of us, including that we should acknowledge there may be unrecognised problems generated when we make rapid yet radical modifications to local environments.

There is a small, unassuming type of creature alive today that differs little from a marine animal present in the Middle Cambrian period around five hundred million years ago. I first read about onychophorans in Stephen Jay Gould's 1989 exposition on the Burgess Shale, Wonderful Life, and although those fossil marine lobopodians are not definitively onychophorans they are presumed to be ancestral. More commonly known by one genus, peripatus, or even more colloquially as velvet worms, there are at least several hundred species around today, possibly many more. The velvet component of their name is due to their texture, but they bear more resemblance to caterpillars than to worms. They are often described as the ‘missing link' between arthropods and worms but as is usually the case this is a wildly inappropriate term in this context of biological classification. The key difference to the Burgess Shale specimens is that today's velvet worms are fully terrestrial: there are no known marine or freshwater species.

Primarily resident in the southern hemisphere, the largely nocturnal peripatus shun bright light and requiring humid conditions to survive. Although there are about thirty species here in New Zealand, a combination of their small size (under 60mm long) and loss of habitat means they are rarely seen. The introduction of predators such as hedgehogs - who of course never meet peripatus in their northern hemisphere home territory - means that New Zealand's species have even more to contend with. Although I frequently (very carefully) look under leaf litter and inside damp logs on bush walks in regions known to contain the genus Peripatoides - and indeed where others have told me they have seen them - I have yet to encounter a single specimen.

There appears to be quite limited research, with less than a third of New Zealand species fully described. However, enough is known about two species to identify their population status as 'vulnerable'. One forest in the South Island has been labelled an 'Area of Significant Conservation Value' thanks to its population of peripatus, with the Department of Conservation relocating specimens prior to road development. Clearly, they had better luck locating velvet worms than I have had! It isn't just the New Zealand that lacks knowledge of home-grown onychophorans either: in the past two decades Australian researchers have increased the number of their known species from just seven to about sixty.

Their uncanny resemblance to the Burgess Shale specimens, despite their transition from marine to terrestrial environments, has led velvet worms to be described by another well-worn phrase, 'living fossils'. However, is this short-hand in any way useful, or is it a lazy and largely inaccurate term? The recent growth in sophisticated DNA analysis suggests that even when outward anatomy may be change little, the genome itself may vary widely. Obviously DNA doesn't preserve in fossils and so any such changes cannot be tracked from the Cambrian specimens, but the genetic variation found in other types of organisms sharing a similar appearance shows that reliance on just external anatomy can be deceptive.

Due to lack of funding, basic taxonomic research, the bedrock for cladistics, is sadly lacking. In the case of New Zealand, some of the shortfall has been made up for by dedicated amateurs, but there are few new taxonomists learning the skills to continue this work - which is often seen as dull and plodding compared to the excitement of, for example, genetics. Most people might say so what interest could there be in such tiny, insignificant creatures as peripatus? After all, how likely would you be to move an ant's nest in your garden before undertaking some re-landscaping? But as shown by the changing terminology from 'food chains' to 'food webs', in most cases we still don't understand how the removal of one species might generate a domino effect on a local ecosystem.

I've previously discussed the over-reliance on 'poster' species such as giant pandas for environmental campaigns, but mere aesthetics don't equate to importance, either for us or ecology as a whole. It is becoming increasingly clear that by weight the majority of our planet's biomass is microbial. Then come the insects, with the beetles prominent both by number of species and individuals. Us large mammals are really just the icing on the cake and certainly when it comes to Homo sapiens, the rest of the biosphere would probably be far better off without us, domesticated species aside.

It would be nice to value organisms for themselves, but unfortunately our market economies require the smell of profit before they will lift a finger. Therefore if their usefulness could be ascertained, it might help generate greater financial incentive to support the wider environment. Onychophorans may seem dull, but there are several aspects to them that is both interesting in itself and might also provide something fruitful for us humans.

Firstly, they have an unusual weapon in the form of a mechanism that shoots adhesive slime at prey. Like spider silk, is it possible that this might prove an interesting line of research in the materials or pharmaceutical industries? After all, it was the prickly burrs of certain plants that inspired the development of Velcro, whilst current studies of tardigrades (the tiny 'water bears' living amongst the mosses) are investigating their near indestructability. If even a single, tiny species becomes extinct, that genome is generally lost forever: who knows what insights it might have led to? Although museum collections can be useful, DNA does decay and contamination leads to immense complexities in unravelling the original organism's genome. All in all, it's much better to have a living population to work on than rely on what can be pieced together post-extinction.

In addition, for such tiny creatures, velvet worms have developed complex social structures; is it possible that analysis of their brains might be useful in computing or artificial intelligence? Of course it is unlikely - and extinction is nothing if not natural - but the current rate is far greater than it has been outside of mass extinctions. Losing a large and obvious species such as the Yangtze River dolphin (and that was despite it being labelled a ‘national treasure') is one thing, but how many small, barely-known plants and animals are going the same way without anyone noticing? Could it be that right now some minute, unassuming critter is dying out and that we will only find out too late that it was a vital predator of crop-eating pests like snails or disease vectors such as cockroaches?

It has been said that ignorance is bliss, but with so many humans needing to be fed, watered and treated for illness, now more than ever we need as much help as we can get. Having access to the complex ready-made biochemistry of a unique genome is surely easier than attempting to synthesise one from scratch or recover it from a long-dead preserved specimen? By paying minimal attention to the smallest organisms that lie all around us, we could be losing so much more than just an unobtrusive plant, animal or fungus.

We can't save every species on the current endangered list but more attention could be given to the myriad of life forms that get side-lined by the cute and cuddly flagship species, usually large animals. Most of us would be upset by the disappearance of the eighteen hundred or so giant pandas still left in the wild, but somehow I doubt their loss would have as great an impact on the surrounding ecosystem than that of some far less well known flora or fauna. If you think that's nonsense, then consider the vital roles that bees and dung beetles play in helping human agriculture.

Although the decimation of native New Zealand wildlife has led to protective legislation for all our vertebrates and a few famous invertebrates such as giant weta, the vast majority of other species are still left to their own devices. That's not to say that the ecosystems in most other countries are given far less support, of course. But without funding for basic description and taxonomy, who knows what is even out there, never mind whether it might be important to humanity? Could it be that here is a new field for citizen scientists to move into?

Needless to say, the drier climes brought on by rising temperatures will not do peripatus any favours, thanks to its need to remain in damp conditions. Whether by widespread use of the poison 1080 (in the bid to create a pest-free New Zealand by 2050) or the accidental importation of a non-native fungus such as those decimating amphibians worldwide and causing kauri dieback in New Zealand, there are plenty of ways that humans could unwittingly wipe out velvet worms, etal. So next time you watch a documentary on the demise of large, familiar mammals, why not spare a thought for all those wee critters hiding in the bush, going about their business and trying to avoid all the pitfalls us humans have unthinkingly laid for them?