We think sustainable urban planning is new – but the ancient Romans were recycling buildings millennia ago

“Hmm, we can reuse this.” The Colosseum. Image: Getty.

In any debate on new construction in our urban centres you are likely to hear phrases like sustainable urban planning, adaptive reuse and recycling heritage – so much so that anyone would be forgiven for thinking that these were modern concerns.

However, these principles have a long history in the ancient world. Anywhere permanent materials such as marble and granite were used to build monuments and infrastructure, recycling and reuse followed.

The ancient Roman world is littered with examples of architectural recycling. Under the banner spolia studies, archaeologists and art historians have increasingly focused attention on the hows and whys of reuse in antiquity.

Ancient architectural recycling falls into two broad categories: adaptive reuse of immovable structures, when a building or monument is renovated and its primary function changes; and reuse of architectural elements, where both functional and decorative material is removed from one building to be incorporated in another (spolia).

While this is often associated with changes in ideologies, there is also evidence of opportunistic recycling following disasters. These events created a surplus of materials that could be salvaged for new constructions.

Same aesthetic, new function

In the hearts of Rome and Istanbul, the capitals of the ancient Roman and Byzantine empires, stand the Pantheon and Hagia Sophia. These iconic and celebrated public buildings were adapted for different religious purposes throughout history. Both maintained their heritage aesthetic, while renovating their function.

The Pantheon was adapted from a pagan temple to a consecrated church in 609CE. The exterior Pantheon was largely unchanged, while the interior was stripped of its pagan elements.

Hagia Sophia was adapted from a Christian basilica to an Islamic mosque following the fall of Constantinople to the Ottomans. The exterior required only the addition of minarets. The interior was whitewashed to cover the rich mosaics of its previous life.

Civic buildings, too, were prime candidates for adaptive reuse, thanks to the rich materials and design of their original constructions.

The restored Library of Celsus, Ephesus, with excavated ancient water pipes in the foreground. Image: author provided.

At the newly listed UNESCO World Heritage site of Ephesus, the tourists’ visit culminates at the impressive multistorey Library of Celsus. Originally built in the second century, an earthquake and fire destroyed the library and its holdings in 262CE.

The impressive facade of the library was salvaged and adapted 100 years later into a nymphaeum, a public water fountain. The adaptive process incorporated other recycled materials from nearby public monuments, mostly marble blocks and free-standing sculpture, fitting the change in function. This reuse gave the non-functional, but already historic, structure a new life.

Recycling as propaganda

The Arch of Constantine is possibly the most referenced structure in spolia studies. Dedicated in 315, the arch celebrates Constantine’s victory over his rival Emperor Maxentius at the Battle of Milvian Bridge.

The Arch of Constantine, where recycling even serves the purpose of propaganda. Image: Steve Kershaw/creative commons.

First noticed by Raphael, the arch was built from a mixture of new and recycled decorative building material. Scenes of animal hunts, religious sacrifice and historic battles were taken from monuments built in the second century CE, including those of the emperors Hadrian, Trajan and Marcus Aurelius. These scenes represented the “golden years” of Rome’s past.

Constantine didn’t just simply recycle these pieces; he reworked the stone faces of Rome’s greatest emperors into his own image. With this act, the emperor takes on all the great qualities of his predecessors and sets himself up as the rightful leader of Rome. This recycling takes us into a world of political propaganda, something the Romans were renowned for.

This bold inclusion of old material in a new monument for Rome led to a whole new recycling trend in architecture. Decorative elements such as columns, capitals and architraves were given new life in buildings of the fourth century CE.

The trend became so popular that new laws were created to protect public buildings from being stripped of their decoration. Only if a building could not be restored was it permitted to recycle that building’s materials.

Opportunistic recycling

Natural disasters and invading armies often left ancient monuments in ruin. These created a stock of marble, granite and sandstone that could be reused in new constructions.

The theatre at Nea Paphos, the scene of archaeological excavations since 1995. Image: Paphos Theatre Archaeological Project, University of Sydney/author provided.

In Nea Paphos, Cyprus, a devastating earthquake destroyed the 8,500-seat theatre in 365CE. Instead of being rebuilt, the theatre became a useful source of marble and stone. Many of the columns and decorative architecture were carried off to be reused in the new Chrysopolitissa basilica, 300 metres down the road.

In Athens, a late Roman fortification wall is a hodgepodge of recycled materials. Image: F. Tronchin/Flickr/creative commons.

In Athens, the invading Heruli destroyed several public buildings in 267-8 CE. However, this left behind a good supply of reusable materials. The Athenians recycled many elements, from column drums to relief sculpture, in a large fortification wall circling the heart of the city. Today, the wall appears as a hodgepodge of recycled elements from Athens’ classical past.

In 2004, the Australian Department of the Environment and Energy released a document supporting adaptive reuse. This booklet said:

Historic buildings give us a glimpse of our past and lend character to our communities as well as serving practical purposes now.

In 2011, the renamed department released a guide to help realise new recycling opportunities related to construction and demolition. These principles are part of our general thinking about urban planning. However, it is clear that this is not a new approach to sustainable urban development. Rather, it continues an ancient tradition of recycling.The Conversation

Candace Richards is acting senior curator at the Nicholson Museum, University of Sydney.

This article was originally published on The Conversation. Read the original article.


 

 
 
 
 

The IPPC report on the melting ice caps makes for terrifying reading

A Greeland iceberg, 2007. Image: Getty.

Earlier this year, the Intergovernmental Panel on Climate Change (IPCC) – the UN body responsible for communicating the science of climate breakdown – released its long-awaited Special Report on the Ocean and Cryosphere in a Changing Climate.

Based on almost 7,000 peer-reviewed research articles, the report is a cutting-edge crash course in how human-caused climate breakdown is changing our ice and oceans and what it means for humanity and the living planet. In a nutshell, the news isn’t good.

Cryosphere in decline

Most of us rarely come into contact with the cryosphere, but it is a critical part of our climate system. The term refers to the frozen parts of our planet – the great ice sheets of Greenland and Antarctica, the icebergs that break off and drift in the oceans, the glaciers on our high mountain ranges, our winter snow, the ice on lakes and the polar oceans, and the frozen ground in much of the Arctic landscape called permafrost.

The cryosphere is shrinking. Snow cover is reducing, glaciers and ice sheets are melting and permafrost is thawing. We’ve known this for most of my 25-year career, but the report highlights that melting is accelerating, with potentially disastrous consequences for humanity and marine and high mountain ecosystems.

At the moment, we’re on track to lose more than half of all the permafrost by the end of the century. Thousands of roads and buildings sit on this frozen soil – and their foundations are slowly transitioning to mud. Permafrost also stores almost twice the amount of carbon as is present in the atmosphere. While increased plant growth may be able to offset some of the release of carbon from newly thawed soils, much will be released to the atmosphere, significantly accelerating the pace of global heating.

Sea ice is declining rapidly, and an ice-free Arctic ocean will become a regular summer occurrence as things stand. Indigenous peoples who live in the Arctic are already having to change how they hunt and travel, and some coastal communities are already planning for relocation. Populations of seals, walruses, polar bears, whales and other mammals and sea birds who depend on the ice may crash if sea ice is regularly absent. And as water in its bright-white solid form is much more effective at reflecting heat from the sun, its rapid loss is also accelerating global heating.

Glaciers are also melting. If emissions continue on their current trajectory, smaller glaciers will shrink by more than 80 per cent by the end of the century. This retreat will place increasing strain on the hundreds of millions of people globally who rely on glaciers for water, agriculture, and power. Dangerous landslides, avalanches, rockfalls and floods will become increasingly normal in mountain areas.


Rising oceans, rising problems

All this melting ice means that sea levels are rising. While seas rose globally by around 15cm during the 20th century, they’re now rising more than twice as fast –- and this rate is accelerating.

Thanks to research from myself and others, we now better understand how Antarctica and Greenland’s ice sheets interact with the oceans. As a result, the latest report has upgraded its long-term estimates for how much sea level is expected to rise. Uncertainties still remain, but we’re headed for a rise of between 60 and 110cm by 2100.

Of course, sea level isn’t static. Intense rainfall and cyclones – themselves exacerbated by climate breakdown – can cause water to surge metres above the normal level. The IPCC’s report is very clear: these extreme storm surges we used to expect once per century will now be expected every year by mid-century. In addition to rapidly curbing emissions, we must invest millions to protect at-risk coastal and low-lying areas from flooding and loss of life.

Ocean ecosystems

Up to now, the ocean has taken up more than 90 per cent of the excess heat in the global climate system. Warming to date has already reduced the mixing between water layers and, as a consequence, has reduced the supply of oxygen and nutrients for marine life. By 2100 the ocean will take up five to seven times more heat than it has done in the past 50 years if we don’t change our emissions trajectory. Marine heatwaves are also projected to be more intense, last longer and occur 50 times more often. To top it off, the ocean is becoming more acidic as it continues to absorb a proportion of the carbon dioxide we emit.

Collectively, these pressures place marine life across the globe under unprecedented threat. Some species may move to new waters, but others less able to adapt will decline or even die out. This could cause major problems for communities that depend on local seafood. As it stands, coral reefs – beautiful ecosystems that support thousands of species – will be nearly totally wiped out by the end of the century.

Between the lines

While the document makes some striking statements, it is actually relatively conservative with its conclusions – perhaps because it had to be approved by the 195 nations that ratify the IPCC’s reports. Right now, I would expect that sea level rise and ice melt will occur faster than the report predicts. Ten years ago, I might have said the opposite. But the latest science is painting an increasingly grave picture for the future of our oceans and cryosphere – particularly if we carry on with “business as usual”.

The difference between 1.5°C and 2°C of heating is especially important for the icy poles, which warm much faster than the global average. At 1.5°C of warming, the probability of an ice-free September in the Arctic ocean is one in 100. But at 2°C, we’d expect to see this happening about one-third of the time. Rising sea levels, ocean warming and acidification, melting glaciers, and permafrost also will also happen faster – and with it, the risks to humanity and the living planet increase. It’s up to us and the leaders we choose to stem the rising tide of climate and ecological breakdown.

Mark Brandon, Professor of Polar Oceanography, The Open University.

This article is republished from The Conversation under a Creative Commons license. Read the original article.