Figures
Abstract
We examined the dietary habits of contemporary and Middle to Late Holocene (ancient) populations of African softshell turtles (Trionyx triunguis) from the northern Levant using stable isotope analysis (δ13C, δ15N, and δ34S) and ZooMS biomarker identification. Our study presents the first application of ZooMS to this taxon, facilitating species-level identification. Stable isotope values point to potential variation in T. triunguis diets, possibly reflecting changing ecosystem conditions. Modern turtles from the south-western Turkish coast exhibit relatively high δ15N values, but low δ13C values, likely influenced by human-provided carrion and agriculture-driven inputs. Ancient turtles (n = 4) from the Levant exhibit more diverse diets, with two individuals indicating a more pronounced marine foraging signature. These preliminary findings are consistent with increased anthropogenic influence on T. triunguis foraging in some regions. This study provides new biomolecular insights into the ecological history of T. triunguis, increasing our understanding of its (long-term) dietary plasticity and potential response to anthropogenic pressures.
Citation: de Kock W, van der Meer MTJ, van Bommel R, Taurozzi AJ, Von Tersch M, Allentoft ME, et al. (2026) Stable isotope evidence of anthropocene disruption in African softshell turtle foraging. PLoS One 21(2): e0339589. https://doi.org/10.1371/journal.pone.0339589
Editor: Vitor Hugo Rodrigues Paiva, MARE – Marine and Environmental Sciences Centre, PORTUGAL
Received: August 4, 2025; Accepted: December 9, 2025; Published: February 11, 2026
Copyright: © 2026 de Kock et al. This is an open access article distributed under the terms of the Creative Commons Attribution License, which permits unrestricted use, distribution, and reproduction in any medium, provided the original author and source are credited.
Data Availability: The mass spectrometry proteomics data have been deposited to the ProteomeXchange Consortium via the PRIDE partner repository (Perez-Riverol et al. 2019) with the dataset identifier PXD062259.
Funding: The first author received support from the Marie Skłodowska-Curie Innovative Training Network SeaChanges, funded by the European Union’s Horizon 2020 research and innovation programme (Marie Skłodowska-Curie grant agreement No. 813383), and from the Netherlands Sectorplan Social Sciences and Humanities (SSH, 2022). This study was funded by the Royal Netherlands Academy of Arts and Sciences (KNAW) Ecology Fund under grant number KNAWWF/747/ECO2021-17. There was no additional external funding received for this study.
Competing interests: The authors have declared that no competing interests exist.
Introduction
Turtles are among the most threatened vertebrates groups due to habitat destruction, overexploitation for pets and food, and climate change ([1]; [2]). Turtles play vital ecological roles, including bioturbation of soils, infaunal mining of seabeds, seed dispersal and germination facilitation, nutrient recycling, and consumption [3]. Furthermore, they contribute to regulating water quality in freshwater ecosystems [4]. The African softshell turtle (Trionyx triunguis), is a freshwater species found in the Middle East and Africa, particularly in the Levant and the Nile River basin (Fig 1.). It is a member of one of the most threatened turtle clades, and yet one of the least studied turtle species. Although the global population of T. triunguis is classified as “Vulnerable” by the IUCN [5] and is protected under the Bern Convention (Convention on the Conservation of European Wildlife and Natural Habitats) and CITES (Convention on International Trade in Endangered Species of Wild Fauna and Flora), the African population is considered “rare”, with some suggesting it warrants a higher IUCN Red List category [6]. In Turkey, major contemporary threats include accidental and intentional fishing, predation, and pollution [7].
Softshell turtles occasionally venture into marine environments [8], raising questions about their reliance on marine resources. Understanding how these turtles’ diets have shifted over time, particularly in response to anthropogenic pressures, is crucial for evaluating the current health of vulnerable populations. By studying dietary shifts, we can place their present ecological status within a broader temporal context, illustrating the long-term effects of human activity. The dietary habits of modern African T. triunguis populations have been examined in both oil-polluted and pristine habitats, revealing considerable differences in their dietary preferences [9]. However, there is limited evidence regarding the broader food ecology of contemporary T. triunguis, which exhibited a more carnivorous diet compared to sympatric pelomedusidae [6,9]. To contextualise these ecological patterns, it is essential to consider the species’ life history and its ability to exploit both freshwater and marine environments. Despite their primary freshwater habitat, African Softshell Turtles have demonstrated the ability to exploit marine environments, first documented in Iskenderun Bay in the early 20th century [10]. Their presence as bycatch in the eastern Mediterranean Sea [11,12] suggests that some individuals opportunistically forage in marine settings. Whether such marine foraging behaviour can be detected across time or populations, however, remains uncertain.
There have been no studies addressing whether modern and ancient populations of T. triunguis show similar patterns of environmental use or dietary signatures. Any comparison of past and present remains therefore provides an opportunity to investigate potential continuity or divergence in foraging strategies. Moreover, it is not yet clear whether the observed ecological plasticity of T. triunguis is a universal trait of the species or one that emerges only in certain local populations. Addressing these uncertainties can provide insight into the functional roles of T. triunguis within their ecosystems [3], which may inform conservation and management strategies of this understudied species.
The oldest published Holocene specimen of T. triunguis comes from the southern Aegean island of Symi, dating to the 1950s [13]. Archaeological records also indicate their presence in the Levant during the Middle Holocene [14,15], where they were likely hunted for consumption. However, no archaeological evidence of this species has been found in Cyprus or along the Aegean coast of modern-day Turkey. This absence could suggest that populations in regions such as Dalaman or Samandağ may have become established relatively recently. If T. triunguis had been present in antiquity, we would expect to find remains, especially the highly distinguishable shells, or artistic depictions, as seen with sea turtles, which are commonly represented in archaeological contexts [14]. Evidence of human-softshell interactions in the wider region during the Holocene is diverse. In ancient Egypt, T. triunguis appears in both literature and art, and was part of the diet of communities along the Nile as far back as the Predynastic (~8–5 kya) period [16]. A striking example of human-softshell turtle interactions comes from the Assyrian site of Kavuşan Höyük (~2.7 kya) located in modern-day eastern Turkey, where Rafetus euphraticus (Euphrates softshell turtles) were found interred alongside human burials [17]. These records highlight the potential biogeographic plasticity and the presence of soft shelled turtles in the anthropogenic niche since the middle Holocene, and provide context for studying their past ecological roles and dietary shifts.
Stable isotope analysis provides a powerful means of investigating diet and habitat use in both modern and archaeological specimens. The ratios of stable isotopes (used in this study) expressed as δ13C, δ15N, and δ34S can reflect different aspects of diet and environmental interaction. δ13C values distinguish between sources of primary production, such as C3 and C4 plants or marine and freshwater resources, offering insights into habitat and carbon source variability [18; 19]. δ15N values increase with trophic level, providing information on an organism’s position within the food web [20,21]. δ34S values, are especially useful in aquatic systems because marine environments typically exhibit higher and more homogeneous sulphur isotope values than freshwater or terrestrial ecosystems, thus serving as a sensitive indicator of habitat use [22,15]. When used together, stable isotope measurements can enable broad reconstructions of dietary and ecological variation across space and time.
In this study, we explore these questions through a small but informative dataset (ancient n = 4, modern n = 11), aiming to identify whether stable isotope values from both modern and archaeological T. triunguis specimens show evidence of marine foraging and to what extent such signatures are consistent between time periods and regions. To address questions about the dietary habits, ecological interactions, and potential anthropogenic impacts on T. triunguis, we combined biomolecular and isotopic approaches. First, we employed ZooMS (Zooarchaeology by Mass Spectrometry, [23]) to identify T. triunguis remains from collagen type 1 peptide sequences, as osteological species identification was unfeasible due to high fragmentation. Next, we compared stable isotope values (δ13C, δ15N, and δ34S) from newly identified prehistoric bones and freshly sampled modern individuals to assess broad-scale patterns rather than definitive temporal trends. This study represents the first stable isotope and historical ecology analysis of T. triunguis, offering preliminary insights into its past and present ecological roles and testing the potential of isotopic data to inform future studies on ecological plasticity in the African softshell turtle.
Methods
Sample description
Eleven modern and four ancient T. triunguis were sampled in this study. Sampling of eight modern turtles was conducted from August 16th to 20th, 2021, near Dalaman, Muğla, Turkey (Fig 1). Turtles moving between Lake Küçükdalyan and the Aegean Sea pass through this area. Turtles were lured with bait (chicken liver) into a trap formed by three eel fykes arranged in a triangle. Once captured, each turtle was weighed, its curved carapace length and width measured, and its sex recorded, as both size and sex can influence competitive dynamics in feeding, resource access, and overall ecological interactions. A skin tissue sample was taken from the rear end of the carapace using a sterile 0.3 cm punch, immediately stored in ethanol, and exported for stable isotope analysis. Seven turtles (Da2–Da8) were sampled and released back into the water, although turtle Da6 was not weighed. One skin biopsy (Da1) was collected from a recently deceased turtle found near the sampling site, likely bycatch. Additionally, three skin biopsies (Samandağ_1–3) from stranded (deceased) modern T. triunguis individuals in Samandağ, Hatay, Turkey, were provided. This study was conducted in accordance with the regulations of the Directorate of Nature Conservation and National Parks of the Ministry of Agriculture and Forestry, Turkey, which granted research permission for the fieldwork. Ethical approval for sampling procedures was obtained from the Animal Experiments Ethics Committee of Aydın Adnan Menderes University (Permit Number: 64583101/2021/039). The biopsy location on each turtle was selected to minimize disturbance, and all handling was performed using clean gloves. Turtles were processed as quickly and gently as possible to reduce stress and were released immediately into their natural environment after sampling, within 5 minutes. No turtles were sacrificed in this study. All eleven skin biopsies were exported to the University of Groningen under CITES permit 22NL305802/11.
We examined one ancient T. triunguis bone fragment from the Early Bronze Age settlement Tell Fadous-Kfarabida, situated in the central Levant (Lebanon). Radiocarbon dating and stratigraphy [24] place this specimen to ca. 5–4.5 kya. The other three ancient samples came from Tell el-Burak, ca. 100 km south of Fadous. These remains exclusively belong to the Iron Age II phases A, B, and C, dating to ca. 2.6–2.4 kya [25]. Prior to destructive sampling, all bones were scanned using a three-dimensional scanner and reconstructed to have a record of the unsampled specimen.
Site geomorphology
The modern sampling site near Dalaman (Muğla, Turkey) is a brackish, riverine environment where turtles move between Lake Küçükdalyan and the Aegean Sea. Samandağ (Hatay, Turkey), the source of additional modern samples, lies at the mouth of the Orontes River, an active freshwater outflow, forming a coastal delta. The archaeological site Tell Fadous-Kfarabida (Lebanon), the Early Bronze Age site, is coastal but lacks evidence for a perennial freshwater source. In contrast, the Iron Age site of Tell el-Burak, located further south, shows greater access to freshwater environments, as supported by the presence of other freshwater species in the faunal assemblage [26]. Expanded descriptions of the archaeological sites are present in the supplementary information.
Sample analyses
- i). ZooMS
Species identification with ZooMS analysis of ancient bones was conducted following the protocol of [23] at the Globe Institute, University of Copenhagen. The matrix assisted laser desorption ionisation-time of flight mass spectrometry (MALDI-TOF) measurements were undertaken at the University of Cambridge (Supporting Information S1 File for further details). Comprehensive shotgun proteomic data were also acquired from a museum reference specimen for peptide marker identification, using nanoflow liquid chromatography tandem mass spectrometry (LC-MS/MS) on an EASY-nLC 1200 system coupled to an Exploris 480 mass spectrometer (Thermo Scientific). Detailed mass spectrometry parameters are described in [26]. The mass spectrometry proteomics data have been deposited to the ProteomeXchange Consortium via the PRIDE partner repository [27] with the dataset identifier PXD062259.
- ii). Stable isotope analyses
Collagen extraction from ancient bone samples followed a modified [28,28] and were conducted at BioArCh, University of York, while modern turtle tissue samples were prepared using a standard methodology for sea turtle biopsies [29]. Details are provided in Appendix S1.
Stable carbon (δ13C), nitrogen (δ15N), and sulphur (δ34S) isotope analyses were performed on extracted collagen and freeze-dried tissue samples at the Scottish Universities Environmental Research Centre (SUERC) and the Royal Netherlands Institute for Sea Research (NIOZ), respectively, using continuous-flow isotope ratio mass spectrometers. Isotopic compositions were normalised using IAEA and in-house standards. Full methodological details and standards used are provided in Appendix S1.
Data analysis
ZooMS biomarker identification using MALDI-TOF and LC–MS/MS followed the data analysis steps outlined in [15], additional details can be found in Appendix S1. Stable isotope results were quality-controlled using previously published criteria for archaeological collagen [30,31]. To compare modern and ancient specimens, modern δ13C values were adjusted for the Suess effect, the depletion of atmospheric δ13C due to fossil fuel emissions, using Dombrosky’s [32] model, applying a correction factor of +2 units. The stable isotope data were visualised with scatterplots, and linear relationships between trophic position (δ15N), length and weight were analysed. ANOVA and post hoc testing were carried out in R [33] to test for differences in δ13C, δ15N and δ34S between Dalaman, Samandağ and Tell el-Burak, we didn’t include Tell Fadous in statistical testing as there is just one data point. All visualisations were conducted in R using ggplot2 [34].
Results
Physical characteristics of Dalaman turtles
The sizes and weights of sampled T. triunguis specimens are summarised in S1 Table. Most sexed individuals were male (n = 5), with only two females. Females were notably lighter than males, who also had larger curved carapace lengths (CCL) and widths (CCW), suggesting possible sexual dimorphism in the population.
ZooMS
The four reliable ZooMS biomarkers identifying T. triunguis are shown in Fig 2. These biomarkers were detected in the MALDI-TOF spectra of all specimens, including those also morphologically identified as T. triunguis. One of these biomarkers, COL1α1 774–797, is shared with the softshell turtle Pelodiscus sinensis. However, given that these two species do not have overlapping ranges, this shared biomarker does not pose an issue in this context. Additional ZooMS biomarkers that were either not unique to T. triunguis or less reliable are displayed in S2 Fig. Peptide sequences were verified by LC-MS/MS on a museum reference specimen (S2 Fig).
(A) ZooMS biomarkers identified in this study that differentiate Trionyx triunguis from all sea turtle species, as well as seven additional turtle species with COL1 sequences available on NCBI: Chelonoidis abingdonii, Chrysemys picta bellii, Gopherus evgoodei, Mauremys reevesii, Pelodiscus sinensis, Terrapene carolina triunguis, and Trachemys scripta elegans. (B-E) Spectra of the four identified biomarkers for T. triunguis (upper), compared to spectra of the sea turtle Chelonia mydas (lower) for reference.
Stable isotope analyses
Stable isotope values for all specimens are presented in S2 Table. All specimens fell within the C/N quality control range of 2.9–3.6 [30,31]. However, seven of the fifteen specimens failed at least one sulphur quality control criterion (%S, C:S, or N:S) established for archaeological mammals (%S of 0.28 ± 0.07%, C of 600 ± 300, N of 200 ± 100; [31]), used because the equivalent for reptiles is not available. Specifically, three ancient and four modern specimens did not meet these criteria. Pearson’s correlations (S3 Table) showed no relationship between sulphur isotopic composition (δ34S) and QC indicators (molar C:S, molar N:S, and %S), which suggested no post-mortem alteration of the collagen [35].
The δ13C values obtained from the epidermis in modern T. triunguis specimens had a narrow range from −22.3‰ to −20.3‰, except for one individual from Samandağ, which had a δ13C value of −12.7‰. In contrast, the range of δ13C values among the ancient specimens was much wider (−24.3‰ to −12.4‰, Fig 3A, S2 Table). The three individuals from the ancient site at Tell el-Burak displayed highly variable δ13C values. However, the sample size is too small to draw strong conclusions. ANOVA testing did not show any statistically significant differences in δ13C between sites (S4 Table).
(A) Scatterplot of stable isotope values (δ13C, δ15N, δ34S) of ancient and modern T. triunguis samples. (B) Linear regression of weight (kg) of modern Dalaman T. triunguis turtles vs δ15N of skin epidermis. (C) Linear regression of weight (kg) vs curved carapace length (cm) in the same individuals. (D) Linear regression of δ34S vs δ15N of skin epidermis.
The δ15N values in modern specimens varied by geographic location (Fig 3A). Specimens from Samandağ had higher δ15N values, ranging from 12.2‰ to 15.3‰, compared to those from Dalaman, which ranged from 5.9‰ to 8.8‰. In the ancient specimens from Tell el-Burak, one individual had a much lower δ15N value of 3.5‰, while the other two had values of 9.3‰ and 10.6‰. In modern specimens from Dalaman (n = 6), δ15N values were strongly positively correlated with weight (R² = 0.71, p < 0.05; Fig 3B), and weight showed a very strong positive relationship with curved carapace length (R² = 0.94, p < 0.001; Fig 3C). ANOVA and subsequent posthoc testing showed significant differences between δ15N at Samandağ and Dalaman (p < 0.001) and Samandağ and Tell el-Burak (p = 0.01).
δ34S values were generally higher in ancient specimens compared to modern turtles (Fig 3A), though one modern turtle from Samandağ had δ34S values similar to those of ancient specimens. Modern specimens had δ34S values ranging from 2.5‰ to 11.2‰ (S2 Table), while ancient samples ranged from 11.8‰ to 14.2‰. ANOVA and subsequent posthoc testing showed significant differences between δ34S at Tell el-Burak and Samandağ (p < 0.05) and Tell el-Burak and Dalaman (p < 0.01).
Discussion
Our examination of the modern T. triunguis population near Dalaman revealed a predominance of males over females. Although the sample size may be insufficient for definitive conclusions, our findings align with [36], who also reported a male bias in this region. A male-biased sex ratio has also been observed in this species on the west coast of Africa [37]. Softshell turtles have genetic sex determination, therefore we would not expect the sex distribution to be skewed from hatching. Instead it is possible that the observed sex distribution could have been influenced by factors such as thermal sampling bias, niche partitioning or the capture technique [38]. Notably, the two females sampled were significantly smaller and lighter than the males (S1 Table). We observed a positive relationship between turtle weight and δ15N values (Fig 3C), suggesting that males are feeding at a trophic level half to one level higher than females. Semi-aquatic turtle species often display male-biased sexual size [39], and it is possible that smaller females are less competitive at accessing higher trophic-level prey, such as carcasses.
Our study also identified ZooMS biomarkers with potential for future research in archaeology, museums or ecology. These biomarkers may be particularly valuable for archaeologists working with faunal assemblages from the Levant, where sea turtles and African softshell turtles are frequently found together and can be difficult to distinguish morphologically when remains are fragmented. Visualising stable isotope data (Fig 3A, S2 Table), we noted that seven specimens failed one or more quality control criteria in the sulphur stable isotope analysis [31]. These criteria are typically used to identify post-mortem alterations in collagen, yet four of the failed specimens were modern and therefore had not undergone such degradation. This discrepancy suggests a need to revisit the application of these criteria for reptiles [15]. Using the methodology from [35], correlations between isotopic compositions and quality control criteria (S3 Table) revealed no significant correlations, further suggesting that the observed deviations are not due to post-mortem alteration. These results suggest that quality control criteria established for mammalian bone collagen may not be wholly applicable to reptilian collagen, and highlight the need for developing reptile-specific criteria to assess reliability of sulphur isotopes from archaeological remains. Potential lipid contamination in the modern skin samples warrant consideration, as lipids are depleted in 13C relative to collagen and can thus lower δ13C values while raising C:N ratios. Guiry and Szpak [40] propose a modern-specific C:N atomic ratio threshold of 3.0–3.38, beyond which δ13C values may be compromised by residual lipids. Only one of our modern samples falls within this stricter range (S2 Table), however, exploration of any correlation between δ13C and C:N atomic ratios (S1 Fig) shows no statistically significant relationship, suggesting that lipid contamination is not the principal driver of δ13C variation in our dataset. Ethanol storage prior to analysis may have facilitated some lipid removal, as ethanol is a mild solvent capable of extracting certain polar lipids over extended periods. Any lipid residues present, would likely have a minial effect; Guiry and Szpak [40] estimate that a 0.5 increase in C:N would result in a δ13C shift of approximately −1‰, a margin insufficient to alter the broader interpretations of dietary ecology presented here. Additionally, when comparing bone and skin collagen isotope values, Doherty et al. [41] report consistent isotopic offsets in modern terrestrial mammals, with skin being depleted in 13C by ~0.7‰ and enriched in 15N by ~1.0‰. These offsets, while notable, do not affect our interpretations regarding trophic level or habitat use. Overall, while acknowledging the limitations of sample preservation and tissue type, the isotope data are suitable for cautiously comparing foraging patterns in ancient and modern T. triunguis.
The stable isotope results suggest shifts in T. triunguis foraging ecology, with modern individuals relying more on anthropogenically influenced diets. While ancient turtles showed a mix of marine and terrestrial signals, modern turtles reflect C3-based (associated with most pasture and traditional agricultural crops, such as wheat and rice) and human-provided resources, whereas Samandağ individuals show higher trophic-level feeding (Fig 3). Ancient T. triunguis remains are extremely rare, making this dataset uniquely valuable despite its small size. Similarly, living T. triunguis are both rare and challenging to study [6], as their large size and aggressive nature make them difficult to capture and handle. However, the severe limitations in sample size and site representation necessitate caution in interpreting these differences. While statistical comparisons are limited, the observed data provide insights into past and present foraging, and susceptibility to human impact.
The narrow δ13C range among the modern T. triunguis specimens suggest a diet primarily influenced by C3 plants, which include most temperate-climate crops such as wheat, barley and most pasture in temperate areas. C3 plants follow a photosynthetic pathway that results in lower δ13C values compared to C4 plants, such as maize or sugarcane, which have a more enriched δ13C signature [42]. The δ13C values from Dalaman T. triunguis are the same as modern sheep from the Aegean coast of Turkey [43], sheep carcasses are the predominant carrion expected in the waterways of this region. The findings indicate human-modified environments likely contributed to the dietary signatures observed in these turtles, warranting further investigation into the extent of anthropogenic influence on their feeding ecology. A single exception was the specimen from Samandağ (specimen Samandağ_3), which had higher δ13C values in line with marine foraging. Two of the ancient specimens, one from Tell-Fadous-Kfarabida (W68) and one from Tell el-Burak (W44) have depleted δ13C values which could have been due to agricultural influence in T. triunguis diets. Tell-Fadous-Kfarabida’s barley (Hordeum vulgare) was particularly depleted in δ13C, likely due to higher rates of precipitation at the time (Hermann [44]). At Tell el-Burak, grape (Vitis vinifera) remains, comprising 35.5% of the assemblage [45], showed δ13C depletion compared to grains [46], indicating a potentially substantial agricultural influence on T. triunguis’ diet at the time. In contrast, the other two Tell el-Burak individuals (W45 and W49) resembled the modern turtle Samandağ_3, with δ13C values suggesting marine foraging.
The low δ15N in ancient Tell el-Burak samples W44 and W68 complement the theory that these ancient turtles were influenced by agriculture. At the same site, a contemporary freshwater detritus-feeding vertebrate (Clarias gariepinus) has higher δ15N (9.54) values [26]. Archaeobotanical remains from nearby Tel Kabri, like olive (Olea europaea) and grapes have negative δ15N values (Nicoli’ et al. 2023), supporting the idea of an agriculture influenced diet in these turtles. Conversely, W45 and W49 showed higher δ15N values, indicative of a wild diet possibly influenced by marine environments. Modern δ15N values varied; Dalaman specimens showed similar δ15N values, whereas Samandağ turtles fed at higher trophic levels or in a food web with a higher δ15N baseline (Fig 3A). Generally, food chains are longer in aquatic environments, leading to higher δ15N values in omnivores and carnivores who have wild aquatic diets [47]. It is possible that the Dalaman population is primarily anthro-dependent, feeding on human-discarded carrion, or fed by tourists, while Samandağ turtles consume higher-level aquatic prey. Taken together, these results suggest that foraging patterns may differ between populations and between time periods, although the small number of samples limits robust comparison.
Sulphur stable isotope (δ34S) results showed significant variation between Tell el-Burak and the modern sites. Ancient Levant specimens had higher δ34S values than modern Turkish specimens, except for Samandağ_3, which matched the ancient specimens (Fig 3A). Elevated δ34S levels indicate marine influence [48]. For the modern specimen Samandağ_3, this is consistent with the δ13C and δ15N results, which also suggest marine foraging. The δ34S interpretation for ancient samples is complex due to the effect of sea spray, potentially affecting δ34S up to 30 km inland [48]. Modern specimens, except Samandağ_3, did not exceed δ34S values seen in ancient and modern freshwater fish from outside the sea spray range [49]. Therefore, despite Dalaman turtles being caught within two kilometres of the sea, minimal sea spray effect is suggested. Although all ancient specimens exhibited relatively high and similar δ34S values, only W45 and W49 also displayed elevated δ13C and δ15N values indicative of marine feeding behaviour. The other two ancient specimens exhibited freshwater isotope values; however, the absence of freshwater fish, bivalves, or gastropod remains at Tell Fadous-Kfarabida suggests that freshwater resources were not available locally. This raises the possibility that the two distinct specimens, W44 and W68, were imported from a strongly freshwater environment, such as an inland lake or the Nile River. Modern Dalaman specimens showed varied δ34S values, however the lack of significant relationship to δ15N indicates factors beyond size or sex influence δ34S values. Samandağ turtles with low δ34S values likely spent most of their lives in freshwater.
Our study suggests that T. triunguis diets may vary among populations and between past and present contexts, with some evidence for marine foraging and anthropogenic influence. Modern turtles from Samandağ exhibit significantly higher δ15N values than those from Dalaman, suggesting a shift toward higher trophic-level feeding. In contrast, ancient Tell el-Burak turtles show no significant δ15N difference from Dalaman but exhibit significantly elevated δ34S values, indicating stronger marine influences. These patterns suggest that while prehistoric turtles had varied diets, including marine foraging, modern populations are more dependent on human-altered resources. The varied T. triunguis foraging highlights their adaptability but also their vulnerability to human-driven ecological changes. Anthropogenic influences on T. triunguis diets may pose risks through exposure to agricultural pollutants and toxins [7]. Given the small sample sizes, these patterns are preliminary, but they provide useful insights for future research and management of this little-studied species.
Supporting information
S1 File. Additional descriptions, methods and results.
https://doi.org/10.1371/journal.pone.0339589.s001
(DOCX)
S1 Table. Curved carapace length (CCL), curved carapace width (CCW), weight (kg), and sex of the eight Trionyx triunguis sampled in Dalaman.
https://doi.org/10.1371/journal.pone.0339589.s002
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S2 Table. Sample information and stable isotope measurements of modern and ancient Trionyx triunguis specimens.
Quality control criteria which fell outside the range proposed for archaeological collagen [30,31] are displayed in red.
https://doi.org/10.1371/journal.pone.0339589.s003
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S3 Table. Results of Pearson’s product-moment correlation tests performed to evaluate the relationships between δ34S and three quality control (QC) criteria: the molar carbon to sulphur ratio (CS Molar), the molar nitrogen to sulphur ratio (NS Molar), and the percentage sulphur (%S).
Provided are the t-statistic, degrees of freedom, p-value indicating significance, 95% confidence interval for the correlation coefficient, and the Pearson correlation coefficient.
https://doi.org/10.1371/journal.pone.0339589.s004
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S4 Table. Post hoc testing of pairwise comparisons of δ¹³C, δ¹⁵N, and δ³⁴S isotope values between sites (Samandağ, Dalaman, and Tell Burak).
Differences between site pairs are reported alongside the 95% confidence intervals (CI) and associated p-values. Significant differences (p < 0.05) are in bold.
https://doi.org/10.1371/journal.pone.0339589.s005
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S1 Fig. Pearson’s product-moment correlation tests of δ¹³C vs C:N ratio in A: all modern T. triunguis skin samples, and B: all modern samples excluding Samandağ_3 which appears to have a separate ecological niche.
https://doi.org/10.1371/journal.pone.0339589.s006
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S2 Fig. A) Summary of ZooMS biomarkers identified in this study.
Biomarkers are categorised as either shared with sea turtles (Harvey et al. 2019), shared with Pelodiscus sinensis (a softshell turtle native to China and Taiwan), or unique to T. triunguis. *In this context, “unique” refers to biomarkers that were not found in any of the tested turtle COL1 sequences. (B-E) LC-MS/MS spectra of the four reliable biomarkers presented in Figure 2 of the manuscript, visualised using pBuild. The spectra show coverage of Y and B ions, along with the amino acid substitutions and any post-translational modifications.
https://doi.org/10.1371/journal.pone.0339589.s007
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Acknowledgments
We gratefully acknowledge Dr. Simona Ceriani for her valuable advice on skin biopsy processing, and M. Munoz-Alegre for her mass-spectrometry support. Our sincere thanks go to Dr. Bektaş Sönmez for providing the Samandağ specimens. Skin biopsies were exported to the University of Groningen under CITES permit 22NL305802/11. Archaeological samples are stored in the zooarchaeological collection of the Groningen Institute of Archaeology (University of Groningen). Our research would not have been possible without the work of the Tell Fadous-Kfarabida and Tell el-Burak excavation teams. Many thanks to S. Ikram. We also appreciate D. Klingberg Johansson and the National History Museum of Denmark for permitting us to sample T. triunguis for proteomic analysis.
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