Paleontological work must balance the needs of the researcher with the long-term conservation of specimens1,2. Nondestructive methods are preferred when preparing vertebrate fossils for exhibit or research, and considerable effort has gone toward developing less invasive alternatives to conventional, destructive methods2,3,4. For example, high-resolution computed tomography (CT) can be paired with 3D printing to minimize specimen handling by providing an alternative to conventional molding/casting2,5,6. As another example, synchrotron-based micro-tomography is a nondestructive alternative to histological sampling2,5,6,7,8. Furthermore, advances in equipment and techniques have made CT a viable option for increasingly larger specimens2,4,6,9.
The geologically younger specimens of the Cenozoic, particularly those of the Quaternary Period, often are non- or minimally-permineralized ("sub-fossil"). For this reason, large Cenozoic fossils may be underrepresented in CT research. While it is challenging to quantify how often specimens are excluded from analysis, as these decisions are rarely reported, it is possible to assess biases in the types of specimens scanned by surveying the published proceedings of professional conferences, which serve as a snapshot of a field's current work.
Abstracts of presentations at the Society of Vertebrate Paleontology (SVP) annual meetings from 202210, 202311, and 202412 were surveyed, and presentations of new CT data were tabulated. Presentations using only pre-existing CT data were not included. When more than one presentation used the same data, only one presentation was included. When a presentation included data from more than one geologic age, it was categorized by the oldest specimen scanned. This did not result in any Cenozoic fossils (pre-modern specimens) being excluded from the final tallies.
When initially reviewing CT data presented at SVP annual meetings from 2022 to 2024, Cenozoic taxa appear to be well-represented (Figure 1). For example, in 2024, 29 presentations focused on Cenozoic taxa, compared to 34 presentations focused on Mesozoic taxa. In 2023, presentations of Cenozoic taxa outnumbered those of Mesozoic taxa. However, for each of the years surveyed, about a third of the CT data for Cenozoic taxa are of modern specimens. Additionally, pre-modern Cenozoic specimens are predominantly microvertebrates, teeth, or particularly durable bones, such as vertebrae and distal phalanges. Of the 219 presentations surveyed, only three involved new CT data from large Cenozoic fossils: a partial mammoth tusk presented in 2022, a mammoth humerus presented in 2024 (discussed in this study), and a Uintatherium cranium presented in 2024 (Supplement 1). The paucity of data from large, fragile fossils suggests a need to address obstacles to CT analysis of these specimens.

Figure 1: Presentations at the Society of Vertebrate Paleontology annual meetings, 2024, 2023, and 2022. Information was compiled from abstracts, and authors were contacted for clarification as needed. Presentations were categorized by the oldest specimen scanned; no Cenozoic fossils were removed using this method (see Supplement 1 for full details). Please click here to view a larger version of this figure.
One obstacle to CT scanning of fossils is durability; specimens must withstand transport, handling, and positioning1,2,9. Some researchers opt to use medical CT scanners, which are built to produce images of the human body. Medical CT scanners allow researchers to keep specimens in horizontal positions, which reduces the likelihood of damage3,4. However, medical CT scanners cannot accommodate specimens larger than a typical human. Those who research large taxa, such as cetaceans13 or proboscideans6, report excluding specimens or limiting images to partial scans due to the size constraints of medical CT scanners. Industrial CT scanners can accommodate larger specimens and also produce higher-resolution images than their medical-grade counterparts3,4. To do this, large specimens typically are oriented vertically on a turntable, rotating the specimen on its longest axis while being scanned by stationary instruments9. Given these parameters, specimens that are both too large for medical CT scanners and too fragile to withstand vertical orientation in an industrial CT scanner may be excluded from tomographic research.
Another obstacle to CT scans, and to radiography (X-ray imaging) in general, is that highly attenuating materials must be avoided. These materials can obstruct details from view or produce artifacts, which are distortions that can be problematic during analysis. High-density materials, such as bone and many minerals, increase the likelihood of beam hardening artifacts14. In most instances, beam hardening creates a "halo" along the periphery of an object, giving a false impression that the outer edge has a higher density than the interior4,14. In more extreme examples, beam artifacts can make an object appear smaller and/or thinner than actuality15. Other highly-attenuating materials, such as metals, can create streak or starburst artifacts, which block out detail2,3,4,9,16,17.
None of these artifacts can be completely avoided when scanning fossils, as fossil bone is especially dense and may be permineralized14. However, excluding certain materials from the fossil preparation process can prevent the creation of any additional artifacts. Traditionally, preparators have reinforced fragile specimens with materials such as wood, metal, gypsum compounds (plaster of Paris, "water putty," etc.), and/or two-part epoxy putties1,2,5,18,19. These materials allow specimens to be stored or displayed for long periods, but they can produce the artifacts detailed above, which can limit the ability to use radiographic research methods. Additionally, attempts to remove fillers such as gypsum compounds or epoxy putties can irreparably damage a specimen20. The movement to prepare fossils with archival grade, reversible materials1,18,21 may address obstacles to both transport and imaging.
Kozo washi is an artisanal Japanese paper used in the construction of such traditional objects as hanging scrolls and sliding doors22,23,24. This paper is useful in the conservation of artifacts and natural history objects due to its strength and flexibility23. Thermoplastic resins also are used widely in conservation work. For instance, acrylic "glass" (poly[methyl methacrylate]) is considered an inert material21. A variety of other thermoplastic resins (B-72, B-76, B-98, etc.) are ubiquitous in fossil preparation laboratories1,18,20,25,26.
Experiments combining kozo paper with thermoplastic resins have resulted in composite materials that can replace the use of gypsum compounds and epoxy putties in stabilizing specimens23,27,28,29. This composite of natural fibers in a resin matrix can be used to create "bandages" that have gap filling, backing, and facing applications. The composite also can be combined with acrylic supports to create an alternative to reinforcements made of wood or metal. These methods address concerns in both long-term conservation and paleontological research: the method is reversible, and the materials are lightweight, archival grade23,27,28, and radiolucent (do not interfere with X-ray or CT imaging)30.
For the purposes of the following protocols, an adhesive is a thermoplastic resin dissolved in acetone or ethanol, typically at a 1:1 ratio, to create a high viscosity solution for "gluing" two fragments together. A consolidant is a more dilute solution of a thermoplastic resin in acetone or alcohol (1:4 or 1:5 ratio), which is applied to a specimen to harden or solidify it25,26. Paper is graded by weight, which is expressed as grams per square meter (GSM). Please see the Table of Materials for a full materials list with suppliers.