Abstract
In this article, I examine how contemporary artists are responding to the unprecedented surge of anthropogenic mineral diversity and the rapid accumulation of technofossils by envisioning their potential future manifestations. These artworks move beyond the prevailing nostalgic and apocalyptic narratives by fostering a sense of concern and curiosity about the future interplay of biological, geological and technological compounds and their coevolutionary dynamics. Firstly, I analyse the works by Agnieszka Kurant and Sylvia Noronha, which challenge the conventional, ahistorical notions that often guide
Introduction
The dynamic multispecies environments of the Anthropocene are characterised not only by death and extinction but also by ‘emergent and unexpected constellations of life, nonlife and afterlife’, as Baubandt (2017: 137) has noted. An unprecedented increase in mineral diversity is significantly contributing to these new landscapes and, as Hazen (2014) explains, is caused by ‘widely accelerated feedbacks between life and rocks, with a special emphasis on a single organism: Homo sapiens’. These interactions also propel technological advancements and foster the proliferation and global dissemination of diverse artefacts. We are consequently witnessing the emergence and concentration of materials that were previously rare or entirely alien to natural ecosystems. To encapsulate this phenomenon, Zalasiewicz et al. (2014c: 34) coined the term ‘technostratigraphy’, which denotes ‘the geologically accelerated evolution and diversification of technofossils – the preservable material remains of the technosphere’. These profound material transformations and dynamics, which require us to ‘relearn multiple forms of curiosity’ (Tsing et al., 2017: 11), underpin ongoing conceptual debates among mineralogists concerning the criteria and the methods used to distinguish and characterise mineral species (Cleland et al., 2021; Heaney, 2017).
A focus on chemical composition and the crystal structure alone ‘without regard to its environment of formation’ (Cleland et al., 2021: 2) informed traditional ways of defining minerals. In this context, a mineral is a ‘naturally occurring solid that has been formed by geological processes either on Earth or in extraterrestrial bodies’ (Nickel and Grice, 1998: 913); hence, the International Mineralogical Association’s 1998 statement maintains that compounds produced by human activity are typically not classified as minerals. However, there are instances where human involvement in substance formation is less straightforward, blurring the distinction between what qualifies as a mineral and what does not (Hazen et al., 2017: 596). Therefore, the ongoing proliferation of novel compounds can no longer be ignored, and more inclusive definitions and conceptualisations are called for. In their paper ‘On the mineralogy of the “Anthropocene Epoch”’, Hazen et al. (2017) catalogue 208 mineral compounds that are directly or indirectly anthropogenic and approved by the International Mineralogical Association. However, a recent ‘more inclusive survey of the paragenetic modes of all minerals points to more than 600 mineral species that may form as byproducts of human industry, though most of those phases occur by natural processes, as well’ (Hazen and Morrison, 2022: 60). Hence, the rapid dynamics of the biosphere, geosphere and techno-sphere must be considered together as contributors to the emergence of Anthropocenic geodiversity.
In both general audiences and scholarly circles within the environmental humanities, the recent surge in mineral diversity has received far less nuanced attention than the decline in biological diversity. Aside from omnipresent alarmist and apocalyptic rhetoric concerning undesirable novel materials that jeopardise life (Dibley, 2018; Gille and Lepawsky, 2021; Paranada and Tothill, 2023; Rosol and Rispoli, 2022), inquiries into novel mineral compounds and their unique ways of emerging within the environment require the cultivation of the ‘arts of noticing’ (Tsing, 2015). Nonetheless, recent research on Anthropocenic materialities builds upon a longstanding tradition within the humanities and arts of conceptualising natural environments beyond biotic communities, an area which has experienced significant revitalisation through the contemporary geologic turn in cultural awareness. Ellsworth and Kruse (2012: 6), in their edited collection
Artists are now rediscovering minerals, mineraloids, (techno)fossils, geosites and geomorphosites, seeking to understand better this unprecedented ‘explosive expansion of species’ (Heaney, 2017: 926). They are considering minerals in light of the complex relations that actively shape geological diversity, which Stanley (2002: 1) has defined as ‘the link between people, landscapes, and their culture through the interaction of biodiversity, soils, minerals, rocks, fossils, active processes, and the built environment’. Art is creatively embracing the present challenging moment, recognising the necessity to depart from abstract and isolating terms traditionally used to classify minerals in modern science. 1 Instead, it is following those mineralogists who are exploring ‘a newly emerging “evolutionary system of mineralogy” which attempts to categorise minerals according to their historical contexts and consequent idiosyncratic combinations of attributes’ (Cleland et al., 2021: 2). Hence, with rapidly developing technologies becoming a geological phenomenon, the concept of geological diversity must also expand to accommodate various novel processes in which ‘minerals (considered sensu lato, including organogenic materials such as paper and textiles) and rocks, both natural and artificial, are combined in diversity patterns to produce the diverse and changing range of technofossils’ (Zalasiewicz et al., 2014c: 37).
In this paper, I aim to demonstrate how selected artworks that embrace anthropogenic mineral diversity and speculate on its future manifestations contribute to a better understanding of the ontological, ethical and political challenges posed by the Anthropocene. Being ‘ontologically inventive and sensible’ (Haraway, 2016: 98), these artworks manifest ‘a willingness to explore’ (Tsing, 2021) the unexpected, unpredictable, unsettling but also marvellous interspecies dynamics of this emerging materiality. As material curiosities themselves, these artworks stand as peculiar objects of contemporary
This article is divided into two main sections. In the first, I explore artworks by Agnieszka Kurant and Sylvia Noronha which simulate future mineral compounds capable of challenging conventional concepts in mineralogy and disrupting the traditional narratives guiding the
Integrating Anthropocene minerals, mineraloids and technofossils into the narratives of natural history museums and other geological collections is a political project and demands fresh conceptual frameworks and practical solutions. As material expressions of storytelling and knowledge production (McNiff, 2013), the analysed artworks inspire and facilitate alternative forms of experiencing, conceptualising and responding to the burgeoning mineral diversity
Art objects-cum-future rocks and technofossils
Art galleries and museums – sometimes made almost entirely of rocks – effectively convey that art has always been closely associated with lithic materials. This connection is evident in various forms such as petroglyphs, stone sculptures, land art and cave paintings, all utilising a wide range of mineral pigments (Boivin and Owic, 2013). This indicates that in the West, for centuries,
Geoscientist Heaney (2017: 925) was apparently inspired by Zalasiewicz’s (2009) book
Kurant, operating in the imaginary realm of possible future impactful events, both anthropogenic and contingent, created bio-techno-mineral compounds by meticulously selecting her materials from contemporary biological laboratories, electronic waste dumps and the post-industrial environment of automobile production. The focus of Noronha’s explorations was elsewhere, in the vast chaotic impact zone of a current anthropogenic natural disaster. Her art objects were created from material samples taken from a post-catastrophic environment and subsequently subjected to laboratory-simulated sedimentary dynamics and metamorphic processes similar to those naturally induced by volcanic eruptions. In the context of Kurant’s

Agnieszka Kurant,
The composition of Kurant’s synthetic rock,
While nuclear blasts are regarded as the most precise indicators of the Anthropocene epoch due to the resulting fallout, which is readily identifiable in the chemostratigraphic record (Zalasiewicz et al., 2015), the impacts of meteors throughout Earth’s history are viewed as natural catalysers in the coevolution of minerals and life. This combination of anthropogenic and non-anthropogenic factors invoked by Kurant alludes to the most recent unfolding of the co-evolution of life and minerals, inscribing human agency into the more-than-human deep-time context of planetary or even cosmic evolutionary dynamics. Being a part of these complex processes, however, humans have emerged as ‘the immersed subject of trans-corporality’, which, as Alaimo (2016: 158) claims, ‘recon with the Anthropocene as an intermingling of biological, chemical, and climatic processes, which are certainly neither simply “natural” nor managed by human intention’. This suggests that while humans should indeed be able to respond with care to the devastation they have caused, the widespread fantasy of the exclusive agency of humans – a notion often associated with the Anthropocene – frequently leads to the reinstatement of old hierarchies. This problematic mindset fuels nostalgic beliefs, as highlighted by Malm (2020: 167), who contends that ‘
In her other artwork,

Agnieszka Kurant,
Fordite was first collected in the 1940s in old auto factories in Detroit and was only recently discovered by gemologists and jewellers. The most attractive material of this kind comes from the 1960s and 1970s, as it has the brightest and boldest colours, reflecting the fashion in car paint during that period. It emerged initially from layers of over-sprayed car paint accumulated in paint bays. The over-sprayed paint was repeatedly baked, which hardened the material and resulted in a rock-like appearance. This painting technique for car parts has long since ceased, rendering fordite a marker of a specific technological history of Michigan’s industrial environment and a brief period in the material history of the planet. However, fordite is also a reminder that the current prolific stage of mineral evolution might be ‘short-lived, unlike the case with natural minerals. . . Many man-made minerals will become extinct (i.e. cease to form), either because they come to be obsolete for humans or, ultimately, with the extinction of humans’ (Zalasiewicz et al., 2014a: 112).
Kurant’s
Highlighting technologies that are not merely outdated but inherently disastrous, Silvia Noronha’s series, As the large-scale flow of viscous material moved along at high speed after the dam collapse, it scraped up large-scale trees, animals, septic tanks, pigsties and drains. It swept away towns and villages. It swept away old gold mines and pans that used mercury. The gates of hydroelectric plants were opened completely to allow the wave of material to pass. (Robson, 2017: 16)
Waste deposition along the Rio Doce River has affected the lives of 1.4 million people, who are still awaiting ecosystem remediation. Noronha herself sampled heavily contaminated mud from four locations around Mariana and then, in collaboration with laboratories at the Technische Universitat in Berlin, subjugated them to simulated processes, which usually lead to volcanic and sedimentary rocks forming. This allowed her to speculate on the future geological landscapes left by the broken dam’s rupture and demonstrate to viewers the future accumulative effect of the ‘wave of mud [which] became an amalgam of contested meanings and materials, appearing as something both separate from and invasive of the river and its delta’ (Creado et al., 2018: 37). However, her work does not explicitly focus on the current toxicity of industrial waste as part of contemporary anthropogenic materiality. Instead, it shows how an event of such magnitude and complexity will not be materially forgotten as it becomes embedded in geological strata through anticipated transformational processes.
The form and mode of display of the artworks as isolated rocks and fossils, in the cases of both Kurant and Noronha, allude to the
Incorporating Anthropocene minerals, mineraloids and technofossils into the narratives of natural history museums and other geological collections requires interconnecting the diversification of mineral species with the evolution of biological species and the technosphere. This linkage is provided by the theory of mineral evolution, first introduced in 2008 by a group of earth scientists led by Hazen et al. (2008), who recognised Anthropocene mineralogy as part of the deep history of exchanges between minerals and life. Unlike more traditional approaches that favour solid-state chemistry and physics, this theory focuses on changes in mineral diversity resulting from a range of physical, chemical and biological dynamics that have formed the mineral composition of the Earth. Accordingly, on the surface of the pre-organic Earth, mineral evolution was shaped by crystallisation when molten lava cooled down, evaporation that left behind mineral residues and the deposition of these minerals in water. In this way, the atoms of various periodic table elements formed minerals (crystalline lattices), and physical processes, combined with chemical processes, generated different varieties. However, unlike biological species, mineral species do not mutate, reproduce and compete, but throughout their long geological history, they have been constantly diversifying. Mineral evolution research suggests (Hazen and Morrison, 2022) that almost half of the Earth’s 5659 minerals presently classified have formed from biological processes, while more than 1900 existed exclusively through life. Thus, anthropogenic minerals and technofossils emerge as the latest unfolding of evolutionary processes.
In recent years, some mineralogical gallery exhibits have undergone reconceptualisation in order to integrate, albeit in a limited manner, contextual and process-oriented perspectives on mineral formation. These insights hint at the co-evolution of minerals and life. However, despite these advancements, a rigid distinction between life and minerals persists, with biological species predominantly showcased in separate galleries from mineral specimens. This suggests a reluctance to embrace Anthropocene minerals, which could further blur traditional divisions and transcend the nature/culture dichotomy. Museums that have embraced the need to rethink and rearrange their mineral collections, such as the Smithsonian Institution, the Natural History Museum in Vienna, the American Museum in NYC, the National Museum of Natural History in Paris and the Natural History Museum of Milan, have acknowledged and explored coevolutionary life and mineral connections from a deep-time perspective. Each of them, to a different extent, not only displays ‘organic gems’ but also explains the complex geophysical and metabolic dynamics that lead to the formation of minerals. However, the direct or mediated anthropogenic impact on the diversification of mineral species and, hence, on mineral evolution is still rarely presented.
Extraction and evolution
‘Human subterranean explorations’, Zalasiewicz (2016: 177) suggests, ‘will form one of the more enduring parts of our rock-bound legacy’ not only as rock transformative punctures resulting in the translocation of materials but also as unique environments, such as dumps and the walls of mines, where new minerals have been observed forming, catalysed by high temperatures, fire gasses and changes in humidity (Hazen et al., 2017). Extraction sites operating at the intersection of the bio-, geo- and technospheres are usually characterised as threats to biodiversity, but they have likewise emerged as prolific locations for mineral diversification. These extreme environments also the sites of ongoing developments in the technosphere induced by complex forces, of which only some are human-related. As Zalasiewicz et al. (2014c: 41) has observed, ‘the technosphere, although clearly currently mediated through human agency, has a dynamic of its own and cannot be said to be under any central human control’.
Anika Schwarzlose, a German artist based in Amsterdam interested in environments heavily influenced by the mining industry, chose the Yekaterinburg and Chelyabinsk regions of the Ural Mountains on the border of Europe and Asia for her investigations. Her recent projects, such as

Anika Schwarzlose,
While the work
Transitioning from the surface reality of burning slag heaps, the camera leads viewers into underground locations currently being explored and exploited by drilling machinery. The mining technology is further investigated while viewers are taken to a contemporary mining fair in Russia. In these documentary fair scenes, a voiceover narrates the historical evolution of the infrastructure, highlighting pivotal moments such as the transition from animal-powered machinery to human-controlled machines and, subsequently, replacing human workers with robots. It is projected that human presence underground will become obsolete in the foreseeable future. In this film segment, the predominant visual realism of a contemporary mine documentary unexpectedly transitions into an animated fabulation. This animation serves as a speculative visual narrative depicting the evolution of the technosphere, taking an unforeseen major twist. The animation portrays monumental drilling devices undergoing a spectacular transformation into elaborate and colourful crystalline objects. Through slow motion, viewers can observe the intricate process wherein a piece of mining infrastructure transmutes, completely shedding its functional shape (Figure 4).

Anika Schwarzlose and Brian McKenna,
This video showcases the transformative evolutionary force of self-organising mineral matter in two instances. Firstly, anthropogenic mineral diversification spontaneously emerges from the environmental ruins of waste heaps. Secondly, the evolutionary development of the mining technosphere results in the loss of human connections and, ultimately, the loss of biotic connections. This latter phenomenon echoes the
Schwarzlose’s and McKenna’s video is a critical fabulation boldly answering the ‘what if’ question. It attempts to imaginatively visualise phenomena that resist conventional representation through scientific methods, thus aligning with
Recognising mineral agency (Bennett, 2010) and the diversity of underground environments, which to some degree have co-evolved with nonhuman and human life and machines, underscores the importance of curiosity about the emergent unexpected species constellations. This requires what Haraway calls respons-abilty, which in this case is an obligation to respond to the plural agencies involved in current practices of rapacious extraction and other modifications affecting rock structure, hence the Earth’s geology (Zalasiewicz et al., 2014b: 7). These artworks cultivate response-ability by speculating about being witnesses to mineral species evolving diversely within the underground wilderness at their own pace and through their unique processual modes and relationships with biological and abiotic species. This approach reflects an ethical stance rarely extended to abiotic species (Stoner, 2017), especially in the form of underground rocks, and enables a caring appreciation of both known and imagined mineral futures.
Coda: Becoming mineral sensitive again
Following Niels Bubandt’s (2017:137) assertion that ‘a metaphysics that has lost the ability to distinguish the
The artworks examined here, taking the form of rocks and technofossils, act as
Highlighting a resurgence in the format of cabinets of curiosities as a mode of curation and display in the Anthropocene, Robin (2020: 205) observes that museums and artists are drawn to ‘objects of strange change’ because they ‘seek to make sense of the chaotic changes of our present “strange times”’. Complex mineral compounds-cum-artworks align with Robin’s observation while revealing multiple fabulations about rapidly transforming environments, turbulent processes and radical time scales and underscoring the curious entanglements of organic and inorganic species. In many ways, these art objects relate to the rare and wonderful specimens once displayed in the cabinets of curiosities that achieved an exceptional level of popularity in 16th- and 17th-century Europe. These predecessors of museums of natural history offered displays of objects that often articulated perplexing narratives within a universe of entangled cultures and natures (
Drawing on the fascination with the marvellous, paradoxical and bizarre reignited by surrealists, Wilson (2023: 5) proposes ‘a surrealist art of noticing’ as a critical approach
And yet, anthropogenic minerals and technofossils are slowly infiltrating museums, demonstrating a capacity to evade human control. Paradoxically, many traditional mineral galleries and their storage rooms have become sites where mineral evolution’s ‘unexpected others’ emerge. Ordinary oak storage cabinets can transform into cabinets of Anthropocene curiosities, serving as unique anthropogenic environments where one can look for novel mineral formation processes. For instance, the mineral calclacite was serendipitously discovered in 1945 inside an old cabinet at the Royal Museum of Natural History in Brussels. This peculiar mineral formed on calcareous rocks that had come into contact with acetic acid leaching from the oak wood used in crafting the display furniture. Since then, this mineral species, forming white crystals in a silky hair-like efflorescence, has also been found on fossils and ceramics stored in similar wooden cabinets in various locations (Boccia Paterakis and Steiger, 2015: 172).
Another conspicuous sign of this encroachment upon museums is the well-documented presence of plastiglomerate, a unique amalgam initially discovered on Kamilo Beach on the Big Island of Hawaii in 2006 by oceanographer Charles Moore. After being subsequently examined by geologist Patricia Corcoran and artist Kelly Jazvack, it had its institutional debut in an art exhibition (Corcoran et al., 2014). Plastiglomerate, formed from the fusion of plastic, volcanic rock, coral skeletons and shells through the process of campfire burning, has since become recognised as a global phenomenon, finding its way into the collections of esteemed institutions such as the Yale Peabody Museum, Het Nieuwe Instituut in Rotterdam and Natura Artis Magistra in Amsterdam (Robertson, 2016). The plastiglomerate case highlights how art spaces embrace experimentation and boundary-pushing, suggesting their potential as catalysers in integrating Anthropocene materials into museum settings.
Contemplating the reality that human endeavours have created ‘a host of crystalline compounds that never existed in the solar system, and perhaps in the universe’ (Hazen et al., 2017: 606) evokes a profound ontological and epistemological sense of wonder. At the same time, it brings to light significant ethical concerns regarding the inadequately comprehended consequences of destructive mining practices. Many of these novel compounds remain undiscovered; some evolve rapidly, embedded in the constellations of connections that are hard to grasp, while others await their eventual emergence. Amid this uncertainty, artists continuously scrutinise the present and probe the deep future of mineral environments, envisioning scenarios devoid of gloomy nostalgia or paralysing apocalyptic overtones, even in the absence of human presence. Through their explorations, they align with Tsing et al. (2017: 7), who urge that ‘in the midst of ruins, we must maintain enough curiosity to notice the strange and wonderful as well as the terrible and terrifying’.
Footnotes
Acknowledgements
My sincere thanks to the organisers of the 2019
Funding
The author(s) disclosed receipt of the following financial support for the research, authorship, and/or publication of this article: This publication was supported by the Excellence Initiative–Research University Programme of Adam Mickiewicz University [grant number 166/08/POB5/0052].
Declaration of conflicting interests
The author(s) declared no potential conflicts of interest with respect to the research, authorship, and/or publication of this article.
