Heritage Futures: Learning from Nature
2026-09-16
by Claudio Pescatore
Heritage is often imagined as something we preserve for the future: we identify what matters, protect it from change, and hope it survives long enough for others to encounter it. That is the popular picture, at least.
But Nature suggests another way of thinking about continuity — and it may deserve a place in that conversation.
A soil, a sediment layer or a peat deposit can act as an environmental archive. It records traces of what has happened, yet it never stays untouched.
Material is deposited, transformed, mixed, eroded and redistributed; radioactive substances decay; new ones are formed.
The archive changes continuously — and still it keeps information about the past.
This made me wonder: could it be a useful way of thinking about heritage?
Nature does not preserve by standing still
My recent work concerns a rather obscure radioactive isotope, lead-210 (210Pb), which environmental scientists use to study atmospheric fallout and to date relatively recent sediments, soils and peat.
The interesting point for me was not the isotope itself but the idea of the environment as an archive.
The 210Pb record is not a document filed away intact. It is produced by natural processes that never stop: material arrives, radionuclides transform, sediments shift, and the record that results has to be read and interpreted.
A sediment layer need not stay identical to its original state to tell us something about its history. In other words, the archive stays useful not despite change but through it.
The real question may be less whether something stays exactly as it was, and more whether, as it changes, it still holds on to a pointer to what came before.
This is not a new thought in heritage studies.
Cornelius Holtorf has argued for years that heritage strengthens cultural resilience precisely by helping us accept loss and transformation rather than resist them, and more recently that conservation itself can be understood as regeneration — ever changing, never less than whole. What the environmental sciences add is a very concrete example of the same idea.

Schematic: excess ²¹⁰Pb decays with depth while the ¹³⁷Cs peak fixes 1963 — a record that keeps time while never ceasing to change. (Illustration by the author)
What about human traces?
The uranium-mining landscapes that prompted my study make this more interesting still.
Mining leaves behind long-lived material: tailings, waste rock, stockpiles, open workings and other residues. These keep interacting with air, water, soil, plants and sediments long after the mining itself has stopped. Uranium mines also release radon gas, which travels in the air and, in turn, generates 210Pb.
This raised a specific worry. Most of the 210Pb in soils and sediments comes from radon gas emanating naturally out of the ground; the steady amount that settles each year is what lets scientists read the record, rather as one reads tree rings. Could that extra radon from uranium mines add enough 210Pb to distort the record?
For documented mine sizes, the answer is largely reassuring: the added radon is far too little to shift regional 210Pb levels in any measurable way. Close to a site the picture can differ, and there it is dust and eroded material that could disturb the record.
What I find more intriguing is what the question reveals.
Human activity does not only leave heritage objects behind. It also leaves materials that enter the ongoing processes of nature.
The landscape itself can become part of the recording mechanism.
What this really describes is archaeology — an archaeology that faces the other way. The archaeologist reads a record already deposited; here the record is still being laid down, as heritage or as mining residue, and the question is how some later present will read it.
Memory without stasis
This brings me close to an idea that seems important for heritage:
that keeping memory is about more than keeping things unchanged.
Something can change a great deal and still work as a memory, so long as it keeps some capacity to point beyond itself — to an event, a place, an action, a history.
The pointer may itself change. What matters is that the relationship holds.
Nature offers no end of examples. A landscape can be transformed and still carry traces of earlier uses. Sediments can be disturbed and still preserve a chronology. Material can move, decay and recombine while some trace stays legible.
The archive, in this sense, is not a container. It is a process.
Learning from Nature
The heritage sector will recognise all this; it has been working in this direction for some time. What Nature offers is a reminder of how ordinary the principle really is. It invites a small shift of emphasis — from asking only:
How do we preserve this for future generations?
to also asking:
How might this change through time and still point back — remaining a past that some future can still read?
That is a different kind of responsibility. It does not mean giving up on preservation, nor assuming that every trace will survive.
It means only that continuity and sameness are not the same thing.
Nature does not keep its records by stopping time. It keeps them while time is passing — and culture, in its own way, does much the same.
That is less a lesson Nature teaches heritage than a resemblance worth sitting with: good company, perhaps, for a field already moving this way.
Further reading
Pescatore, C. (2026) An upper bound on uranium-mining radon contributions to regional environmental 210Pb inventories. Journal of Environmental Radioactivity 299, 108143. https://doi.org/10.1016/j.jenvrad.2026.108143
Pescatore, C. (2026) When Nuclear Waste Becomes Archaeology. UNESCO Chair on Heritage Futures blog, Linnaeus University, 25 August 2026. https://blogg.lnu.se/unesco/?p=4834
Holtorf, C. (2018) Embracing change: how cultural resilience is increased through cultural heritage. World Archaeology 50(4), 639–650. https://doi.org/10.1080/00438243.2018.1510340
Holtorf, C. (2026) Beyond the 1964 Venice Charter: cultural heritage as regeneration (ever changing never less than whole). Conservar Património. https://conservarpatrimonio.pt/article/view/37063
Holtorf, C. & Högberg, A. (2018) Archaeology and the future. In C. Smith (ed.), Encyclopedia of Global Archaeology. Springer. https://doi.org/10.1007/978-3-319-51726-1_2792-1


















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