Showing posts with label Zealandia. Show all posts
Showing posts with label Zealandia. Show all posts

Monday 30 July 2018

Biophilic cities: why green is the new black

I've previously discussed the notion that children who spend more time outside in natural surroundings are more likely to have improved mental and physical health compared to their indoors, gadget-centred peers, but does the same hold true for adults as well? After all, there have been many claims that the likes of the fractal geometry of natural objects, the sensual stimulation, the random behaviour of animals, even feeling breezes or better air quality can have a positive or 'wellness' (horrific term though it is) effect.

It is pretty much a given that the larger the percentage of nature existing within conurbations, the greater the improvement to the local environment. This begins at the practical level, with vegetation mitigating extremes of heat while its roots helps reduce flooding. In addition, fauna and flora gain more room to live in, with a greater number of species able to survive than just the usual urban adaptees such as rats and pigeons. What about the less tangible benefits to humans, culminating in a better quality of life? Science isn't wishful thinking, so what about the evidence for more nature-filled urban environments improving life for all its citizens, not just children?

Studies suggest that having window views of trees can increase concentration and wellbeing in the workplace, while for hospital patients there is a clear correlation between types of view and both the length of recovery periods and painkiller usage. Therefore it seems that even the appearance of close-at-hand nature can have an effect, without the necessity of immersion. Having said that, there are clear advantages to having a public green space, since it allows a wide range of activities such as flying kites, playing ball games, jogging and boot camps, or just having a picnic.

Our largely sedentary, over-caloried lives necessitate as much physical activity as we can get, but there is apparently something greater than just physical exercise behind nature as a promoter of wellbeing. Investigation appears to show that spaces with trees and the hint of wilderness are far more beneficial than the unnatural and restricted geometries of manicured lawns and neatly maintained flower beds. It seems that we are still very much beholden to the call of the wild. If this is a fundamental component of our highly civilised lives, are urban planners aware of this and do they incorporate such elements into our artificial environments?

The concept of integrating nature into our towns and cities certainly isn't a new one. As a child, I occasionally visited Letchworth Garden City, a town just north of London. As the name suggests, it was an early form of 'Green Belt' planning, created at the start of the Twentieth century and divided into sectors for residential, industrial and agricultural usage. In its first half century it tried to live up to its intention to be self-sufficient in food, water and power generation, but this later proved impractical. I don't recall it being anything special, but then its heyday as a mecca for the health conscious (at a time when the likes of exercise and vegetarianism were associated with far left-wing politics) has long since passed. As to whether the inhabitants have ever been mentally - or even physically - advantaged compared to the older conurbations elsewhere in the UK, I cannot find any evidence.

Across the Atlantic, the great American architect Frank Lloyd-Wright conceived of something similar but on a far larger scale. His Broadacre City concept was first published in 1932, with the key idea that every family would live on an acre-sized plot. However, Lloyd-Wright's concept - apart from being economically prohibitive - relied on private cars (later updated to aerator, a form of personal helicopter) for most transportation; sidewalks were largely absent from his drawings and models. Incidentally, some US cities today have partially adopted the sidewalk-free model but without Lloyd-Wright's green-oriented features. For example, there are suburbs in oil-centric Houston that are only reachable by car; you have to drive even to reach shopping malls you can see from your own home, with high pedestrian mortality rates proving the dangers of attempting to walk anywhere. Back to Lloyd-Wright: like many of his schemes, his own predilections and aesthetic sensibilities seem to have influenced his design rather more than any evidence-based insight into social engineering.

In recent years the term 'biophilic cities' has been used to describe conurbations attempting to increase their ratio of nature to artifice, often due to a combination of public campaigning and far-sighted local governments. Although these schemes cover much wider ground than just human wellbeing (prominent issues being reduction in power usage and waste, greater recycling and ecological diversity, etc), one of the side effects of the improvements is to quality of life. Thirteen cities joined the Biophilic Cities project in 2013, but others are just as committed in the long-term to offsetting the downsides of urban living. Here are three cities I have visited that are dedicated to improving their environment:

  1. Singapore. Despite the abundance of tower blocks, especially in its southern half, this city that is also a nation has a half-century history of planting vegetation in order to live up to the motto ‘Singapore - City in a Garden’. Despite its large-scale adoption of high-tech, high-rise architecture, Singapore has preserved an equivalent area of green space and now ranks top of the Green View Index. Even the maximal artificiality of the main highways is tempered by continuous rows of tall, closedly-packed trees while building regulations dictate replacement of ground-level vegetation lost to development. A new 280-metre tall office, retail and residential building, due for completion in 2021, is set to incorporate overtly green elements such as a rainforest plaza. It could be argued that it's easy for Singapore to undertake such green initiatives considering that much of city didn't exist before the late Twentieth century and what did has been subject to wide-scale demolition. However, it seems that Singapore's Government has a long-term strategy to incorporate nature into the city, with the resulting improvements in the mental and physical wellbeing of its inhabitants.
  2. Toronto. Although not as ecologically renowned as Vancouver, the local government and University of Toronto are engaged in a comprehensive series of plans to improve the quality of life for both humans and the rest of nature. From the green roof bylaw and eco-friendly building subsidies to Live Green Toronto Program, there is a set of strategies to aid the local environment and planet in general. It is already paying dividends in a large reduction of air pollution-related medical cases, while quality of life improvements are shown by the substantial bicycle-biased infrastructure and increase in safe swimming days. There's still plenty to do in order to achieve their long term goals, particularly around traffic-related issues, but the city and its inhabitants are clearly aiming high.
  3. Wellington. New Zealand's capital has wooded parks and tree-filled valleys that the council promotes as part of the city's quality of life. The recreated wetlands at Waitangi Park and the Zealandia (formerly Karori) predator-proof wildlife sanctuary are key components in the integration of large-scale nature into the urban environment. Indeed, the latter is proving so successful that rare native birds such as the kaka are being increasingly found in neighbourhood gardens. Both the city and regional councils are committed to improving both the quality of life for citizens as well as for the environment in general, from storm water filtering in Waitangi Park to the wind turbines on the hilltops of what may be the world's windiest city.

These cities are just the tip of the iceberg when it comes to conurbations around the world seeking to make amends for the appalling environmental and psychological consequences of cramming immense numbers of humans into a small region that cannot possibly supply all their needs. In some respects these biophilic cities appear too good to be true, as their schemes reduce pollution and greenhouse gas emissions, improve the local ecosystem, and at the same time appear to aid the physical and mental wellbeing of their inhabitants. Yet it shouldn't be surprising really; cities are a recent invention and before that a nomadic lifestyle embedded us in landscapes that were mostly devoid of human intervention. If we are to achieve any sort of comfortable equilibrium in these hectic times, then surely covering bare concrete with greenery is the key? You don't have to be a hippy tree hugger to appreciate what nature can bring to our lives.

Thursday 12 October 2017

The zeal in Zealandia: revealing a lost continent

From an outsider's standpoint, geology appears to be a highly conservative science. As I have mentioned on numerous occasions, it seems astonishing that it took over four decades for Alfred Wegener's continental drift hypothesis to be formalised - via the paradigm-shifting discovery of sea floor spreading - into the theory of plate tectonics. I suppose that like evolution by natural selection, the mechanism, once stated, seems blindingly obvious in hindsight.

Regardless, the geological establishment appears to have been stubbornly opposed to the ideas of an outsider (Wegener was a meteorologist) who was unable to provide proof of an exact mechanism. This was despite the fact that the primary alternative, hypothetical submerged (but extremely convenient) land bridges, appear even more far-fetched.

Over the past few decades geophysical data has been accumulating that should generate rewrites of texts from the most basic level upwards. Namely, that the islands making up New Zealand are merely the tip of the iceberg, accounting for just six per cent of a mostly submerged 'lost' continent. Once part of the Southern Hemisphere's Gondwana, in 1995 the newly discovered continent was given the name Zealandia. Approximately five million square kilometres in size, it broke away from the Australasian region of Gondwana around 70-80 million years ago.

After a decade or two of fairly lacklustre reporting, 2017 seems to be the year in which Zealandia is taking-off in the public domain. First, the Geological Society of America published a paper in February. stating that Zealandia should be officially declared as a continent. Then in July the drill ship Joides Resolution began the two month long Expedition 371, a research trip under the International Ocean Discovery Programme (IODP). Scientists from twelve countries undertook deep sea drilling, gaining data on plate tectonics, palaeontology and climate history as well as research directly relevant to understanding the geology of the newest continent.

It is surprising then to learn that geologists first mooted the idea as early as the 1960s but that apart from some marine core samples collected in 1971, no-one undertook the necessary ocean-based research until very recently. Earth resources satellites have helped somewhat, but nothing could replace the evidence that emerged with deep drilling of the seabed. Therefore I wonder what has sparked the sudden interest in an idea that has been around for so long?

One possibility is the large amount of data that the international geological community required to prove the theory beyond doubt, coupled with the fact that this sort of research has little in the way of an obvious immediate practical benefit. It is extremely expensive to undertake deep sea drilling and few vessels are equipped for the purpose. Joides Resolution itself will be forty years old next year, having undergone several years' of refit to keep it going. Those areas of sea bed with potential oil or gas deposits may gain high-fidelity surveying, but compared to fossil fuels, fossil biota and sea bed strata research are very much at the whim of international project funding. In the case of the IODP, governments are cutting budgets on what are deemed non-essential projects, so it remains to be seen whether the intended follow-up trips will occur.

It would be disappointing if there was no further research as despite the acceptance of Zealandia, there is still a great deal of disagreement about what is known as the Oligocene Drowning. I first came across the notion of an eighth continent in the excellent 2007 book In Search of Ancient New Zealand, written by geologist / palaeontologist Hamish Campbell and natural history writer Gerard Hutching. The reason that over ninety per cent of Zealandia is underwater is due to the lack of thickness of its continental land mass - only 20-30km - making it far less buoyant than other continents.

But has this submerged percentage varied during the past eighty million years? There are some very divided opinions about this, with palaeontologists, geneticists and other disciplines taking sides with different camps of geologists. These can be roughly summarised as Moa's Ark versus the Oligocene Drowning, or to be more precise, what percentage, if any, of New Zealand's unique plants and animals are locally-derived Gondwanan survivors and how many have arrived by sea or air within the past twenty or so million years?

The arguments are many and varied, with each side claiming that the other has misinterpreted limited or inaccurate data. If Zealandia has at any time been entirely submerged, then presumably next to none of the current fauna and flora can have remained in situ since the continent broke away from Gondwana. The evidence for and against includes geology, macro- and micro-fossils, and genetic comparisons, but nothing as yet provides enough certainty for a water-tight case in either direction. In Search of Ancient New Zealand examines evidence that all Zealandia was under water around twenty-three million years ago, during the event known as the Oligocene Drowning. However, Hamish Campbell's subsequent 2014 book (co-written with Nick Mortimer) Zealandia: Our continent revealed discusses the finding of land-eroded sediments during this epoch, implying not all the continent was submerged.

It's easy to see why experts might be reticent to alter their initial stance, since in addition to the conservative nature of geology there are other non-science factors such as patriotism at stake. New Zealand's unusual biota is a key element of its national identity, so for New Zealand scientists it's pretty much a case of damage it at your own peril! In 2003 I visited the predator-free Karori Wildlife Reserve in Wellington. Six years later it was rebranded as Zealandia, deliberately referencing the eighth continent and with more than a hint of support for Moa's Ark, i.e. an unbroken chain of home-grown oddities such as the reptile tuatara and insect weta. With the nation's reliance on tourism and the use of the '100% Pure New Zealand' slogan, a lot rests on the idea of unique and long-isolated wildlife. If the flightless kakapo parrot for example turns out not to be very Kiwi after all, then who knows how the country's reputation might suffer.

What isn't well known, even within New Zealand, is that some of the best known animals and plants are very recent arrivals. In addition to the numerous species deliberately or accidentally introduced by settlers in the past two hundred years, birds such as the silvereye / waxeye (Zosterops lateralis) and Welcome swallow (Hirundo neoxena) are self-introduced, as is the monarch butterfly.

The volcanic island of Rangitoto in Auckland's Hauraki Gulf is only about six centuries old and yet - without any human intervention - has gained the largest pohutukawa forest in the world, presumably all thanks to seeds spread on the wind and by birds. Therefore it cannot be confirmed with any certainty just how long the ancestors of the current flora and fauna have survived in the locality. A number of New Zealand scientists are probably worried that some of the nation's best-loved species may have arrived relatively recently from across the Tasman; a fossil discovered in 2013 suggests that the flightless kiwi is a fairly close cousin of the Australian emu and so is descended from a bird that flew to New Zealand before settling into an ecological niche that didn't require flight.

Other paleontological evidence supports the Moa's Ark hypothesis: since 2001 work on a lake bed at St Bathans, Central Otago has produced a wide range of 16 million year-old fossils, including three bones from a mouse-sized land mammal. The diversity of the assemblage indicates that unless there was some uniquely rapid colonisation and subsequent speciation, there must have been above-water regions throughout the Oligocene. In addition, whereas the pro-underwater faction have concentrated on vertebrates, research into smaller critters such as giant land snails (which are unable to survive in salt water conditions) supports the opposite proposition.

So all in all, there is as yet no definitive proof one way or the other. What's interesting about this particular set of hypotheses is the way in which an array of disciplines are coming together to provide a more accurate picture of New Zealand's past. By working together, they also seem to be reducing the inertia that has led geology to overlook new ideas for far too long; Zealandia, your time has come!

Sunday 15 January 2017

Devoted to dinosaurs: Joan Wiffen and the role of the amateur scientist

I was recently at a second hand book stall, browsing a first edition of Graeme Steven's Prehistoric New Zealand. The market stall owner told me that she had thumbed through the book and was amazed to learn that New Zealand had any wildlife prior to the moa. This seemingly widespread lack of knowledge about the nation's past is no doubt partially due to the small number of both practitioners and finds, although the state education system cannot be considered blameless. Still, in an age of easily-accessible information via the World Wide Web and the likes of the National Geographic Channel, such gaps do seem rather surprising.

Of course a lack of public knowledge concerning ancient life isn't restricted to New Zealand. I recall several amusing (yes, I know it sounds smug) encounters at London's Natural History Museum, where I discovered that parents of dinosaur-crazed children cannot differentiate giant ground sloths from dinosaurs, let alone bipedal carnosaurs from quadrupedal sauropods.

The poor understanding of New Zealand's past is exacerbated by the low population and correspondingly small amount of funding available. Therefore perhaps it's not surprising that amateurs have made significant discoveries, from the Hamilton Junior Naturalist Club's discovery of a giant penguin fossil at Kawhia to Joan Wiffen, the 'Hawke's Bay housewife' (an epithet that always causes me to grit my teeth) who discovered New Zealand's first dinosaur fossils and much more besides.

I've previously discussed the joys of amateur fossicking from a primarily fun aspect but also mentioned how New Zealand relies on non-professionals. The Kawhia penguin is a case in point, as it would have eroded within a year had it not been discovered. Indeed, I was recently collecting some Pleistocene marine molluscs above a Taranaki river valley, on a steep slope prone to severe flooding. These fossils had been uncovered following a landslide caused by a severe rainstorm in 2015 and would no doubt be washed away with the next one.

Fossil hunting in New Zealand

In addition to the lack of professionals, the discipline's funding within New Zealand has decreased over the past half century. The Marsden Fund is a key sponsor of science projects but less than 10% of proposals are successful. The obvious wider issue here is that for the foreseeable future there is unlikely to be any private funding for scientific research that isn't financially viable in the short-term; let's face it, most paleontology isn't going to earn big bucks. That isn't to say there aren't some income streams available, especially around museums, merchandise and occasionally site tourism. However, New Zealand's dinosaur, marine reptile and pterosaur remains are mostly isolated fragments, hardly likely to prove star attractions for even the most ardent dino enthusiast.

Which brings us back to Joan Wiffen. She went from a minimal secondary education (due to her father's prejudice) to an honorary science degree from Massey University - whilst still supporting the view that it is the duty of married women to do all the housework. Although she may not have actively negated the Hawke's Bay housewife appellation, the term is hardly suitable for an extremely conscientious scientist; after all, if her husband had been the team leader, he probably wouldn't have been referred to as a Hawke's Bay electronics technician!

Having recently finished reading Wiffen's 1991 book Valley of the Dragons: The Story of New Zealand's Dinosaur Woman I was struck by the obvious lack of professional expertise available in New Zealand as recently as the 1970s and 1980s. Even today, the thirty or so professional paleontologists in the country don't have their own organisation and fall under the auspices of the Geoscience Society of New Zealand. Yet I've long considered geology to be an extremely conservative discipline (think that meteorologist Alfred Wegener's continental drift hypothesis gained little traction for decades until evidence of plate tectonics was found, rather than there being any active interest in resolving the mystery) and so can do few favours to outsiders.

Therefore, Joan Wiffen faced almost complete indifference from scientists who proclaimed there were no relevant strata in which to locate dinosaur remains. Apparently someone had previously noticed reptilian bones in a Te Hoe Valley stream bed - which is what sparked off Wiffen's first expedition - but no-one had the interest or funding to follow it up. Her narrative hints at the disdain professionals felt for amateurs in general but happily this situation has changed markedly in the interim, with citizen science helping to bridge gaps in many fields. In the case of New Zealand paleontology, the notable finds by amateurs have included previously unknown species, adding to the evidence that areas of the 'lost' continent of Zealandia have been continually above water since the Mesozoic.

My recent Taranaki excursion was child's play compared to the deprivations Wiffen and co endured in their rat-infested self-built hut, not to mention funding the entire work themselves. From learning how to remove rock matrix via acetic acid (in an old baby bath, no less) to building a stereo microscope stand from a pillar drill base, the Hawke's Bay team certainly utilised classic kiwi number eight wire ingenuity.

In a pre-internet age - it took six months just to pin down the location and land owner of the area marked 'reptile bones' - gaining technical advice from foreign experts was slow and cumbersome. Ironically, in later years New Zealand professionals visited Wiffen's fossil preparation workshop to gain insight into their operation, including as to how she and her friends achieved such high standards. Clearly, her work wasn't the product of a casual dilettante but the output of a highly motivated and hard-working scientist, albeit an unpaid one.

The American paleontologist and evolutionary biologist Stephen Jay Gould frequently observed that his disciplines were forms of historical science, built upon a series of unrepeatable events created by the complex interaction of disparate factors. Therefore deposition and preservation - even the discovery - of fossils are unique circumstances; remains that are visible today may be little more than dust tomorrow. We owe Joan Wiffen and her colleagues an enormous debt for increasing the sum of human knowledge at their own time and expense, purely for the love of science. And if any Hawke's Bay residents want to pick up where she left off, then I'm sure both professionals and posterity would be most grateful!