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Pinacosaurus grangeri (ZPAL MgD-II/32) The caudal tendons reveal extensive secondary remodelling, with at least three generations of secondary osteons (Fig. 3A–E). The cross-section of the flattened, elliptical tendon shows a densely secondary remodelled inner part (Fig. 3B, C) in the thickest place and more loosely arranged secondary osteons in the thinner parts of the cross-section and the periphery of the tendon (Fig. 3D). The latter is mainly composed of bundles of mineralized fibres and few vascular canals. Although, the secondary osteons mainly overlap each other in some places, between them patches of mineralized fibres are present (interfascicular spaces; Fig. 3E, F). The cross-section of the second sample from the same individual shows three circular tendons. The two bigger tendons (2.1 and 1.7 mm in diameter) are extensively secondarily remodelled (Fig. 3A) and almost nonvascular mineralized fibres are present on their periphery. In contrast, the smallest tendon (0.6 mm in diameter) is exclusively composed of mineralized fibres, weakly vascularized. The difference in the structure between the smallest and two larger tendons result from different places of sectioning: the smallest is from the terminal part of the tendon, and the bigger ones closer to the middle part. NANOSTRUCTURE OF THE TENDONS Detailed scanning electron microscopy (SEM) observation of vascular canals of fossilized tendons revealed the presence of mostly randomly oriented fibrous matrix in all three studied ornithischian samples (Fig. 4A–G). Comparative SEM images of modern-day turkey tibialis cranialis tendons (Fig. 4I–H) reveal similar fibrous structures. The observed structures exhibit a hierarchic pattern – individual fibres are gathered in bundles (or fascicles). The diameters of the bundles range from 0.7 to 2 µm (Supporting Information, Fig. S1) and the bundles are located in the walls of vascular canals of diameters varying between a dozen and 50 µm. The fibrous structures are visible only in the vascular walls exposed on the surfaces of freshly broken tendons. The EDS spectra collected from the fibrous structures and surrounding mineral matrix of all studied tendons reveal oxygen, calcium and phosphorus as the main components in all studied taxa (Fig. 4K, L), which is a typical elemental signature of modern and fossil bones. To visualize vascular canal shape and geometry, topographic microscope imaging (Fig. 5A, B) of a Homalocephale calathocercos tendon sample was applied. The results indicate that the observed fibrous structures are located deep inside the vascular canals exclusively and incorporated in their walls along their length. In addition to the surface morphology imaging, information of vascular canal topography in the tendon was collected using an atomic force microscope (AFM) in contact mode. The generated images (lock-in amplitude and lockin-phase, Fig. 5B–G) show the nanostructure of the fibres. Furthermore, AFM imaging on an individual fibre (Fig. 5G, H) reveals its striped pattern and the performed measurements allow estimation of a periodicity measuring about 24 nm (Fig. 5I, J; Supporting Information, Data S2). PRESERVATION OF SOFT PARTS All fossil tendon samples were demineralized (see Material and methods) to remove the apatite matrix and to assess whether any soft parts were preserved. No fossilized soft parts were obtained from the extract of Pinacosaurus grangeri. The demineralization of the tendons of Homalocephale calathocercos (Fig. 6A) revealed an extract consisting of individual brown- to orange-coloured tubular structures, as well as a dense network of vascular canals still attached to a translucent layer loosening from the tendon (Fig. 6C, D; Supporting Information, Fig. S2). Furthermore, the Edmontosaurus regalis sample revealed the presence of numerous rust- to brown, dark to translucent, elongated, bifurcated and H-shaped structures (Fig. 6B). Additionally, over a dozen tubular, branched structures (Fig. 6C, D) seems to be morphologically consistent with blood vessels or fibril bundle layers lining the vascular canals observed with SEM. Among them, ovate to tent-shaped cell-like structures attached to the surfaces of vessels or bundle layers were found (Fig. 6F–K). Other cell-like structures, more spindle-shaped, and projecting branching structures (Fig. 6L–N, black asterisks) were usually observed in isolation (Fig. 6L, N), sometimes attached to the fibrous matrix. The EDS spectra collected from the demineralized parts of the tendons show that their elemental composition is different from the mineral matrix of the tendons. In the case of the external sheath of a partially demineralized tendon of H. calathocercos, which detached from the tendon, a dense network of vessel-like tubes was observed (Fig. 6C, D; compare also: Supporting Information, Fig. S2A, B). In this sample, oxygen, silicon and aluminium dominate (Fig. 4E), while remains of phosphates are still present (Supporting Information, Fig. S2C). The fossilized vascular-like tubular structures with attached cell-like structures (Fig. 6F–K), as well as individual cells (Fig. 6L–N) extracted from the samples taken from E. regalis and H. calathocercos, are composed mainly of iron and sulphur with smaller addition of oxygen and silicon (Fig. 6P). ORGANIC MATTER RESIDUES Total carbon (TC), total organic carbon (TOC) and total inorganic carbon (TIC), as well as total sulphur (TS), contents were measured (see Material and methods) to document the preservation of organic matter in all studied fossil samples. Obtained results demonstrate TOC values equal to 1.28 wt% for Homalocephale calathocercos, 2.57 wt% for Pinacosaurus grangeri, and 2.81 wt% for Edmontosaurus regalis tendon samples. An elevated level of total sulphur (4.54 wt%) was also reported for the latter. Furthermore, the control sample of sediment associated with E. regalis tendons reveals the highest level of TOC, up to 6 wt% with sulphur content below 0.5 wt%. SPECTROSCOPIC STUDIES AND MASS SPECTROMETRY FTIR spectroscopic studies, intended mainly to identify organic residues in the fossil samples, were performed only on the selected tendon samples that were never glued or treated with any organicbased materials (e.g. consolidants). Therefore, the Pinacosaurus grangeri tendon sample was not included (Supporting Information, Data S3). A modern-day turkey (Meleagris gallopavo, GIUS-12-3741) was a control sample. FTIR studies of H. calathocercos, E. regalis and M. gallopavo show a band arrangement pointing to co-association of various minerals, including phosphate (PO 4) 3–, carbonate (CO 3) 2– and iron oxide (FeO 4) 5–, as well as silicon dioxide (SiO 2) moieties, suggesting the presence of carbonate apatite, goethite and silicates (Fig. 7). The results are thus consistent with the EDS spectra (Fig. 4H, L, P) for the same samples. The FTIR measurements of demineralized parts of tendon samples from H. calathocercos and E. regalis revealed also signals associated with organic residues (Fig. 5B, D), especially well visible due to several bands in the 1550–1800 cm –1 corresponding to the amide I (Fig. 7F, G). A percentage proportion of each component in the amide I band was computed as a ratio of a fractional area of the suitable peak after the band fitting and the sum of the areas of the peaks belonging to the amide I band (Byler & Susi, 1986; Jackson & Mantsch, 1995; Litvinov et al., 2012). As a result, two intensive bands were observed at 1633 and 1668 cm –1 with 64 and 36% proportion between β- sheet structures and turns (Litvinov et al., 2012) for H. calathocercos, as well as three bands at 1630, 1663 and 1690 cm –1 with 56, 25 and 19% for E. regalis. Two other marginal bands (at 1594 and 1714 cm –1) were also detected in both samples and correspond to the lipid signal, including fatty acids. The comparison of the fossilized tendons with the turkey tendon (Fig. 7E, H) strongly support the possibility of organic (proteinaceous) preservation in the fossil samples, especially based on the comparison of the amide I fingerprint region (Fig. 7F–H). Mass spectra (Supporting Information, Data S4) were collected both from the demineralized sample of H. calathocercos and E. regalis tendons across the regions of interest with a mass-to-charge ratio (m / z) range of 1–150 Da, the fingerprint region for lower mass amino acid anions (Surmik et al., 2017). There, various non-organic (Si-containing and Fe-containing), as well as organic (N-containing), species were identified. The detected ions CH 4 N + (at m / z 30.03 Da), C 2 H 3 N + (at m / z 41.03 Da), C 2 H 6 N + (at m / z 44.05 Da), C 3 H 3 N + (m / z 53.02 Da), C 3 H 6 N + (at m / z 56.04 Da), C 4 H 6 N + (at m / z 68.05 Da), C 4 H 8 N + (at m / z 70.07 Da), C 4 H 10 N + (at m / z 72.08 Da) and C 5 H 10 N + (at m / z 84.08 Da) are related to amino-acids (Surmik et al., 2017) (see also fibrous matrix (white arrow) and cell-like structures attached to the surface (yellow arrows); H, group of cells-like structures attached to the surface; I, lateral view of a cell-like structures (white arrow) attached to the fibrous surface of the vessel-like structures; J, K, examples of cells on the fibrous surface of vessels; L–N, osteocyte-like cells with branching cytoplasmic processes (white arrows) attached to the fibrous matrix (yellow arrow); O, example of isolated vessel-like tubular structure with attached cells (yellow asterisk indicate spot for EDS survey); P, AFM 3D height profile of an individual cell (rectangle in O) documenting the height difference between the cell and the surface of the vessel; the EDS spectrum revealing the elemental composition of the studied cell as iron and sulphur with addition of oxygen and silicon. Supporting Information, Data S4). The presence of the Si- and Fe-containing species correlates with the results of the EDS surveys (Fig. 6E, P) and confirms the mineralogical composition of the studied samples., Published as part of Surmik, Dawid, Słowiak-Morkovina, Justyna, Szczygielski, Tomasz, Wojtyniak, Marcin, Środek, Dorota, Dulski, Mateusz, Balin, Katarzyna, Krzykawski, Tomasz & Pawlicki, Roman, 2023, The first record of fossilized soft parts in ossified tendons and implications for the understanding of tendon mineralization, pp. 747-766 in Zoological Journal of the Linnean Society 198 (3) on pages 752-758, DOI: 10.1093/zoolinnean/zlad001, http://zenodo.org/record/8141891, {"references":["Byler DM, Susi H. 1986. Examination of the secondary structure of proteins by deconvolved FTIR spectra. Biopolymers 25: 469 - 487.","Jackson M, Mantsch HH. 1995. The use and misuse of FTIR spectroscopy in the determination of protein structure. Critical ReVieaes in Biochemistry and Molecular Biology 30: 95 - 120.","Litvinov RI, Faizullin DA, Zuev YF, Weisel JW. 2012. The α- helix to β- sheet transition in stretched and compressed hydrated fibrin clots. Biophysical Journal 103: 1020 - 1027.","Surmik D, Rothschild BM, Pawlicki R. 2017. Unusual intraosseous fossilized soft tissues from the middle triassic nothosaurus bone. The Science of Nature 104: 25."]}

Edmontosaurus regalis (UAMES 52615) Both cross-sectioned tendons show a highly porous structure built of fibrous primary matrix (Fig. 1A–C). The general structure of the sectioned tendons is homogenous. The matrix is composed of coarse collagenous fibre bundles containing numerous bone cell lacunae (Fig. 1A, C). The vascular canals forming the porous structure of the tendons are young Haversian canals (Fig. 1A–C). The cross-sectioned larger tendon shows few scattered secondary osteons in the centre of the tendon surrounded by collagen-fibre bundles (Fig. 1D). The tendon of a slightly smaller cross-section (3.5 mm diameter; Fig. 1A, B) is more porous than the larger one (6 mm; Fig. 1C, D). The different structure between the sampled tendons may result from a different location in the body., Published as part of Surmik, Dawid, Słowiak-Morkovina, Justyna, Szczygielski, Tomasz, Wojtyniak, Marcin, Środek, Dorota, Dulski, Mateusz, Balin, Katarzyna, Krzykawski, Tomasz & Pawlicki, Roman, 2023, The first record of fossilized soft parts in ossified tendons and implications for the understanding of tendon mineralization, pp. 747-766 in Zoological Journal of the Linnean Society 198 (3) on page 751, DOI: 10.1093/zoolinnean/zlad001, http://zenodo.org/record/8141891

Homalocephale calathocercos (MPC-D 100/1201) The cross-section of the tendon shows dispersed primary osteons embedded in mineralized fibrous primary matrix (Fig. 2A–F). In some cases, the structural remnant of a primary osteon encapsulates a smaller concentric ring of lamellar bone apparently separated with a cement line, appearing to be a small secondary osteon deposited in the centre of a primary osteon (Fig. 2D). These structures probably represent a first generation of secondary osteons (a short cycle of resorption of primary tissue and subsequent deposition of secondary tissue along blood vessels). The osteons are bigger and denser in the innermost part of the tendon, and become less abundant and smaller closer to the periphery (Fig. 2A, B, E). Under normal light, in both the longitudinal and cross-section, visible bone cell lacunae are numerous in the centre of the tendon, but rare to absent close to the external margin of the tendon (Fig. 2A, E). Under polarized light, the longitudinal section shows bundles of fibres running in a herringbone-like pattern along the tendon (Fig. 2F), in the cross-section the fibres form a lattice-like pattern (Fig. 2B, C). Thus, the osteons are surrounded by coarse collagenous fibre bundles. The width of the longitudinally sectioned tendon varies from 1.1 to 1.4 mm, its total length is 7 mm., Published as part of Surmik, Dawid, Słowiak-Morkovina, Justyna, Szczygielski, Tomasz, Wojtyniak, Marcin, Środek, Dorota, Dulski, Mateusz, Balin, Katarzyna, Krzykawski, Tomasz & Pawlicki, Roman, 2023, The first record of fossilized soft parts in ossified tendons and implications for the understanding of tendon mineralization, pp. 747-766 in Zoological Journal of the Linnean Society 198 (3) on page 751, DOI: 10.1093/zoolinnean/zlad001, http://zenodo.org/record/8141891

Supplemental material, sj-docx-1-anr-10.1177_20530196221136425 for The Śnieżka peatland as a candidate for the Global Boundary Stratotype Section and Point for the Anthropocene series by Barbara Fiałkiewicz-Kozieł, Edyta Łokas, Beata Smieja-Król, Simon Turner, Francois De Vleeschouwer, Michał Woszczyk, Katarzyna Marcisz, Mariusz Gałka, Mariusz Lamentowicz, Piotr Kołaczek, Irka Hajdas, Monika Karpińska-Kołaczek, Katarzyna Kołtonik, Tomasz Mróz, Sarah Roberts, Neil Rose, Tomasz Krzykawski, Arnoud Boom and Handong Yang in The Anthropocene Review

Supplemental material, sj-docx-4-anr-10.1177_20530196221136425 for The Śnieżka peatland as a candidate for the Global Boundary Stratotype Section and Point for the Anthropocene series by Barbara Fiałkiewicz-Kozieł, Edyta Łokas, Beata Smieja-Król, Simon Turner, Francois De Vleeschouwer, Michał Woszczyk, Katarzyna Marcisz, Mariusz Gałka, Mariusz Lamentowicz, Piotr Kołaczek, Irka Hajdas, Monika Karpińska-Kołaczek, Katarzyna Kołtonik, Tomasz Mróz, Sarah Roberts, Neil Rose, Tomasz Krzykawski, Arnoud Boom and Handong Yang in The Anthropocene Review

Supplemental material, sj-docx-3-anr-10.1177_20530196221136425 for The Śnieżka peatland as a candidate for the Global Boundary Stratotype Section and Point for the Anthropocene series by Barbara Fiałkiewicz-Kozieł, Edyta Łokas, Beata Smieja-Król, Simon Turner, Francois De Vleeschouwer, Michał Woszczyk, Katarzyna Marcisz, Mariusz Gałka, Mariusz Lamentowicz, Piotr Kołaczek, Irka Hajdas, Monika Karpińska-Kołaczek, Katarzyna Kołtonik, Tomasz Mróz, Sarah Roberts, Neil Rose, Tomasz Krzykawski, Arnoud Boom and Handong Yang in The Anthropocene Review

Supplemental material, sj-docx-2-anr-10.1177_20530196221136425 for The Śnieżka peatland as a candidate for the Global Boundary Stratotype Section and Point for the Anthropocene series by Barbara Fiałkiewicz-Kozieł, Edyta Łokas, Beata Smieja-Król, Simon Turner, Francois De Vleeschouwer, Michał Woszczyk, Katarzyna Marcisz, Mariusz Gałka, Mariusz Lamentowicz, Piotr Kołaczek, Irka Hajdas, Monika Karpińska-Kołaczek, Katarzyna Kołtonik, Tomasz Mróz, Sarah Roberts, Neil Rose, Tomasz Krzykawski, Arnoud Boom and Handong Yang in The Anthropocene Review

The cause of the split of 4A4E(4G) Mn2+ excited level measured on minerals spectra is discussed. It is our view that ∆E = |4E(4G) − 4A(4G)| should be considered an important spectroscopic parameter. Among the possible reasons for the energy levels splitting taken under consideration, such as the covalent bond theory, the geometric deformation of the coordination polyhedron and the lattice site’s symmetry, the first one was found to be inappropriate. Two studied willemite samples showed that the impurities occur in one of the two available lattice sites differently in both crystals. Moreover, it was revealed that the calculated crystal field Dq parameter can indicate which of the two non-equivalent lattice sites positions in the willemite crystal structure was occupied by Mn2+. The above conclusions were confirmed by X-ray structure measurements. Significant differences were also noted in the Raman spectra of these willemites.

Value of meteorites can be explained at least in two aspects. From the scientific point of view they are priceless objects, which can bring important information about the very beginning of the Universe. Because of their rarity anduniqueness, the meteorites often are extremely expensive in the term of a commercial value. This situation is used by dishonest sellers who offer fake meteorites. It has happened with the paleometeorite remnants, which were originallyfound in Cretaceous-Paleogene clay boundary in Lechówka, Poland. The so-called fake Lechówka remnants were offered by one seller on domestic online shops. All grains had certificate of authenticity that was included with the sold grains. In this paper we described the most common and diagnostic features, which can be easily applied to distinguish the original meteorite remnants from the fake ones.