The question why non-avian dinosaurs went extinct 66 million years ago (Ma) remains unresolved because of the coarseness of the fossil record. A sudden extinction caused by an asteroid is the most accepted hypothesis but it is debated whether dinosaurs were in decline or not before the impact. We analyse the speciation-extinction dynamics for six key dinosaur families, and find a decline across dinosaurs, where diversification shifted to a declining-diversity pattern ~76 Ma. We investigate the influence of ecological and physical factors, and find that the decline of dinosaurs was likely driven by global climate cooling and herbivorous diversity drop. The latter is likely due to hadrosaurs outcompeting other herbivores. We also estimate that extinction risk is related to species age during the decline, suggesting a lack of evolutionary novelty or adaptation to changing environments. These results support an environmentally driven decline of non-avian dinosaurs well before the asteroid impact.
The most famous mass extinction was the disappearance of non-avian dinosaurs at the end of the Cretaceous, 66 million years ago (Mya), after ruling the Earth for 170 million years1,2,3. The best-supported extinction model is the impact of a large asteroid in the Yucatán Peninsula (Chicxulub, Mexico), which set off a global cataclysm and environmental upheaval4,5. Although evidence for an end-Cretaceous impact is indisputable6, most scientific debate has focused on whether the extinction was geologically abrupt or gradual7,8,9,10,11, whether it was caused by factors intrinsic to dinosaurs12,13,14,15 or by extrinsic physical drivers16,17,18 or both acting in concert19,20. If extrinsic events had a role, the question is whether this driver was terrestrial or extra-terrestrial21,22,23. It has proved harder to posit a convincing killing model that explains exactly how the dinosaurs, as well as many other groups24,25, vanished. And yet other groups of animals and plants survived through this singular, short-term crisis26,27. Could some groups have been teetering on the brink already? Furthermore, the extinctions coincide with a period of long-term environmental changes that resulted in remarkably high sea levels, cooling climates and the spread of new habitat types on land, as well as massive volcanic activity at the end of the Cretaceous16,19,20.
There is a debate about how these events affected non-avian dinosaurs, and yet little evidence exists for a global decline across dinosaur groups prior to their extinction at the end of the Cretaceous3,7,28,29,30,31. The latest thorough analyses of fossil data found no evidence for a decline of non-avian dinosaurs before their extinction3,30, and little evidence of any decline in dinosaur species richness or ecological diversity during the last million years of the Cretaceous. However, a phylogenetic study using dinosaur timetrees10 challenged the idea of a sudden extinction, but instead supported a diversity decline with extinction rates exceeding speciation rates well before the K/Pg event, which has been disputed recently32. Thus, there is no consensus on whether dinosaurs were in decline or not prior to their extinction.
Although the dinosaur fossil record provides invaluable data for our understanding of macroevolutionary patterns and processes through time, it is biased and incomplete3,11,33. Previous attempts to estimate dinosaur diversity dynamics were based on simple counts of the numbers of species in specific time intervals8,9. However, the extent to which these raw data have been biased by preservation and sampling artefacts has long been debated34,35,36. New analytical methods have attempted to alleviate these biases, but despite their widespread application to a wide range of taxa, these methods are constrained by their inability to deal with the absence of data, especially when the spatial distribution of the fossil record in a particular time interval is strongly heterogeneous37,38. Biases in primary data can produce a misleading estimate of palaeodiversity, and this has been argued to be the case with the dinosaur fossil record; using climatic and environmental modelling, Chiarenza et al.11 suggested that the apparent diversity decline of North American dinosaurs could be a product of sampling bias whereby Maastrichtian diversity was likely underestimated.
The lack of consensus can impede our understanding of the drivers of dinosaur diversification and diversity dynamics. Yet, many hypotheses have been proposed to explain the extinction of dinosaurs39, and little is known about the drivers of a putative decline3,10,11,28,31,40. Identifying causal mechanisms for the demise of dinosaurs can be challenging because there are so many possibilities in the Cretaceous, including the continued breakup of the supercontinents Laurasia and Gondwana41,42, intense and prolonged volcanism43, climate change, fluctuations in sea levels44,45, and novel ecological interactions with rapidly expanding clades like flowering plants46,47,48,49 and mammals50,51,52. Testing and teasing apart the effect of all these drivers on dinosaur diversification remain difficult, and, for instance, previous studies have found mixed support for the hypothesis that global dinosaur diversity is tied to sea-level fluctuations18,40,53,54.
Recent methodological developments, however, allow estimation of the temporal dynamics of speciation and extinction rates while taking into account severe biases in fossil data31,36,37,55. Among these methods, PyRate implements process-based speciation and extinction models while also incorporating the preservation process and the uncertainties associated with the age of each fossil occurrence55. PyRate has been thoroughly tested under a wide range of conditions, such as low levels of preservation (down to 1–3 fossil occurrences per species on average), severely incomplete taxon sampling (up to 80% missing), and high proportion of singletons (exceeding 30% of the taxa in some cases)37,55,56. As opposed to other methods (including boundary-crossers and three-timers), which are prone to edge effects and tend to flatten the extinction estimates, especially during mass extinctions, PyRate recovers the dynamics of speciation and extinction rates, including sudden rate changes and mass extinctions37. The Bayesian framework of PyRate also allows testing hypotheses related to the drivers of diversification56,57,58. Yet, this approach has never been used to address questions on dinosaur diversification.
Here we compile and analyse a dataset of dinosaur fossils comprising over 1600 occurrences at a global scale and stage- or formation-level for dinosaur ages, which spans the Cretaceous Period and represents 247 dinosaur species of the most speciose and well-documented dinosaur families that composed the Late and end-Cretaceous ecosystems, namely the ornithischians Ankylosauridae, Ceratopsidae, and Hadrosauridae, and the theropods Dromaeosauridae, Troodontidae, and Tyrannosauridae. First, we address whether dinosaur extinction resulted from a decline, with the bolide impact being the coup de grâce, or whether it was caused by geologically brief or instantaneous events. Given that the dinosaur fossil record is biased, we rely on the Bayesian framework of PyRate55,56 (see Methods) to estimate variations in net diversification rates (speciation minus extinction) through time for dinosaurs (the six dinosaur families as a whole). Second, we examine whether the carnivorous and herbivorous dinosaur families as two groups, and the six dinosaur families individually, had heterogeneous patterns of diversification. Finally, we investigate whether and to what extent speciation and extinction rates responded to major environmental changes in Earth history by examining the correlations between speciation and extinction with a set of abiotic and biotic drivers. We first find strong evidence that dinosaurs began to decline well before the K/Pg extinction due to both a marked increase of extinction from the late Campanian onwards and a decrease in their ability to replace extinct species. Our results also reveal that long-term environmental changes likely made dinosaurs particularly prone to extinction because of a combination of global climate cooling, a drop in diversity of herbivorous dinosaurs, and age-dependent extinction that impacted dinosaur extinction in the Maastrichtian.
Results and discussion
Dinosaurs in decline 10 million years before the K/Pg event
Our results indicate that the diversity dynamics of dinosaurs conform to a time-variable birth–death model including several shifts in speciation and extinction rates (Fig. 1a, Supplementary Fig. 1). Net diversification rates increased during the Early Cretaceous and culminated in the middle Late Cretaceous (Fig. 1b). In the late Campanian (~76 Ma), however, net diversification rates became negative due to a significant upshift of extinction rates that exceeded speciation rates (Fig. 1a, b, Supplementary Fig. 1). In the Maastrichtian, speciation rates decreased slightly while extinction rates remained constant and high, resulting in a negative net diversification (Fig. 1a, b). Negative net diversification rate translates into a decline in species diversity starting in the late Campanian (Fig. 1c). We estimate the palaeodiversity of dinosaurs and find there was rapid species accumulation at the beginning of the Late Cretaceous until diversity peaked in the middle Campanian (Fig. 1c). At that time, our results indicate a progressive decline towards the end of the Cretaceous, with a marked difference between carnivorous and herbivorous dinosaurs.
The carnivorous and herbivorous dinosaur families, analysed separately, show the same pattern of negative diversification rates at least 10 million years before the K/Pg boundary for herbivores (Fig. 1d, e, Supplementary Fig. 2) and at the Campanian/Maastrichtian boundary for carnivores (Fig. 1g, h, Supplementary Fig. 3). An upshift in extinction rates is also responsible for the negative diversification in both groups, although there is also a downshift in speciation rates in herbivores. The palaeodiversity of herbivores largely fits the general pattern (Fig. 1f) while carnivores had a delayed decline that began in the early Maastrichtian (Fig. 1i). Overall, our results indicate that the diversity dynamics of Late Cretaceous dinosaurs support the hypothesis of a diversity decline 10 million years before the K/Pg event, which is in agreement with a recent phylogeny-based analysis10. This result, however, contrasts with other fossil-based estimates showing no decline prior to the K/Pg3,30,32.
Estimating palaeodiversity remains a challenging goal because the known (sampled) diversity is biased by the availability of fossiliferous rock outcrops, as shown in dinosaurs11,30,31. Hence, the diversity decline of dinosaurs could be the outcome of sampling bias inherent to the primary data. We explored this issue by estimating preservation rates through the Cretaceous at the stage level using PyRate37 and compared them with the number of geological formations. When dinosaurs declined, we find that the Campanian and Maastrichtian both have the highest preservation rates (4.30 and 7.18 occurrences/Myr/species, respectively) and highest number of geological formations (Fig. 2). This suggests that dinosaur species diversity could be evenly sampled during the peak of dinosaur diversity and the decline phase. Besides, elevated preservation rates in the Campanian and Maastrichtian help to estimate both gradual and sudden shifts in diversification rates, limiting the Signor-Lipps effect59. Such a bias has previously made it difficult to find a confident estimate of the timing and speed of dinosaur extinction8,9,28,30 and to test hypotheses about the causes of their extinction3,5,17,53,60. In addition, spatial biases can hamper the estimation of diversity trajectories38. In dinosaurs, the North American fossil record is much better documented than the Eurasian counterpart3,11,61 such that the diversity decline could be regional and not global (bearing in mind that our dataset is mostly Laurasian). We addressed this issue by estimating the diversification and diversity dynamics of New and Old World dinosaurs independently. Despite spatial heterogeneity in macroevolutionary dynamics, both the New and Old World dinosaurs show a pattern of diversity decline before the K/Pg boundary (Supplementary Fig. 4). The palaeodiversity of New World dinosaurs complies with the global dinosaur diversity in that the decline started in the Campanian (~76 Ma), while the Old World dinosaurs show a delayed declining phase initiated at the Campanian–Maastrichtian boundary (~72 Ma). Overall, our results provide evidence that dinosaur biodiversity was declining prior to the asteroid impact.
Analysing the six dinosaur families as a whole assumes that diversification rates and their dynamics were homogeneous for all clades. However, rate heterogeneity is a common phenomenon in macroevolution62,63 and clade-specific evolutionary dynamics could be expected in dinosaurs10,13,14,16. We therefore repeated the analyses for each family independently. As for the whole dataset, we find evidence for significant temporal changes in both speciation and extinction rates for all families except Troodontidae (Fig. 3; Supplementary Figs. 5–10). As expected, these results further support the idea that rate heterogeneity is rampant in dinosaurs. Analyses recovered two patterns of diversification among the tested clades: (1) a decrease in speciation rate toward the K/Pg boundary coupled with constant extinction so that speciation became lower than extinction, which occurred in hadrosaurs and tyrannosaurs (Fig. 3; Supplementary Figs. 8, 10); (2) an increase of extinction rate towards the K/Pg that exceeds speciation, which occurred in ankylosaurs, ceratopsians and dromaeosaurs (Fig. 3; Supplementary Figs. 5, 6, 7). Accordingly, the demise of the dinosaurs was controlled by both a failure to originate and an increase in extinction rates. Interestingly, the slowdown of speciation and the increase of extinction started in the mid-Campanian or early Maastrichtian. More importantly, all clades other than Troodontidae had negative net diversification rates before the asteroid impact: ankylosaurs, ceratopsians and tyrannosaurs declined in the Campanian (~76 Mya), thus predating the K/Pg boundary by 10 million years, while dromaeosaurs and hadrosaurs declined in the Maastrichtian (Fig. 3). Among all studied groups, ceratopsians seem to have experienced the strongest diversity decline following a mid-Campanian peak of diversity (~15 species) and ending the Maastrichtian with only two species. On the contrary, hadrosaurs show the weakest diversity decline with a peak of diversity in the late Campanian (~20 species) and reaching the K/Pg boundary with ~13 species prior to the bolide impact. This is in agreement with previous studies that showed a dynamic biogeographical dispersal across the Northern Hemisphere64 (in particular in Eurasia65,66,67) and rapid rates of morphological evolution68, which could have allowed hadrosaurs to sustain their Campanian diversity level until the K/Pg event. Although slightly delayed, the diversity decline in carnivorous families is stronger than for herbivores: dromaeosaurs and troodontids had two species, or even a single species for tyrannosaurs (Tyrannosaurus rex), when the asteroid hit the Earth. However, we should remain cautious about these diversity estimates because new fossil discoveries or taxonomic revision could bring new results. For instance, the family Troodontidae has an unstable phylogeny and many taxa require revision (e.g. Troodon formosus)69,70. Even though the family has an Early Cretaceous or Late Jurassic origin70 and diversified in the Late Cretaceous, our analyses show that the Turonian, Coniacian, and Santonian are depauperate in troodontids, a pattern that requires further study.
Drivers of dinosaur diversity decline
Several factors could explain these dynamics, and we test competing hypotheses. We explore potential drivers of this diversity decline and assess the role of environmental changes on dinosaur diversity patterns prior to the asteroid impact. Abiotic and biotic factors could explain these dynamics, but no study could identify a causal mechanism for the downturn in dinosaur diversification, although it has been proposed that variations of sea level were an important driver10,18,53,71. For instance, it is thought that seaway transgressions during high-stands isolated non-marine sedimentary basins and promoted allopatric diversification, the results of which are recorded in early and middle Campanian deposits throughout Laramidia, as seen in tyrannosaurs18, but has received low support40. Yet, the inferred diversity decline seems to coincide with global climatic changes. The Late Cretaceous was a greenhouse world, characterized by high temperatures and reduced latitudinal temperature gradients72,73, which likely contributed to a flat latitudinal diversity gradient in dinosaurs74. Peak warmth was attained in the Cenomanian-Turonian (100–90 Ma) with sea-surface temperatures reaching ≥30 °C in the tropics and the southern latitudes72,73,75. After this interval, sea-surface and deep-water temperatures decreased to the cooler greenhouse of the Campanian–Maastrichtian (80–66 Ma)72,73,76. This important cooling (~7 °C in North Atlantic77, and ~10 °C in southern latitudes76), which intensified during the Maastrichtian until the K/Pg event, could have impacted dinosaur diversity. However, other factors, such as Cretaceous geological changes17,41 or floristic turnover78,79 should not be discarded.
We relied on a multivariate birth–death (MBD) model57 to analyse simultaneously the effects of abiotic and biotic palaeoenvironmental changes56,63,80. The MBD estimates the correlations between speciation (Gλ) and extinction (Gμ) rates, as well as their explanatory power (shrinkage weights, ω), with a series of environmental variables approximating the temporal variations of the environment through time (Methods)57,58. Given the numerous hypotheses proposed to explain diversity changes in Late Cretaceous dinosaurs, we incorporated four biotic variables extrinsic to dinosaurs (relative diversity of angiosperms, gymnosperms, non-Polypodiales, and Polypodiales ferns57,81) and three abiotic variables (global temperature variations82, sea-level fluctuations83, and continental fragmentation41; Supplementary Fig. 11). To estimate the role of diversity dependence, we also took into account the past diversity fluctuations of dinosaurs, carnivores and herbivores in the MBD model (Fig. 1c, f, i).
Among all ten variables tested, the MBD model (Fig. 4) indicates only a significant effect of herbivorous dinosaur diversity and global temperature (ω > 0.5), with extinction varying negatively with both herbivorous dinosaur diversity (Gμ = −0.0353, 95% credibility interval [CI] = −0.0862, 0) and temperature (Gμ = −0.0809, 95% CI = −0.132, −0.028; Supplementary Table 1). These results suggest that the change in herbivorous diversity, which peaked ~76 Ma and declined thereafter, and the cooling of global temperature in the Campanian–Maastrichtian led to an increase in dinosaur extinction (Fig. 4a). Interestingly, our results also show that some supposedly important drivers of dinosaur diversification had no influence. The MBD model estimates a strong negative correlation with dinosaur speciation (Gλ = −1.064; Fig. 4c) and a strong positive correlation between dinosaur extinction (Gμ = 0.663; Fig. 4d) and angiosperm diversity but both are not significant (ω < 0.5) and have 95% CI overlapping with zero (Supplementary Table 1). Diets of herbivorous dinosaurs are under discussion, but it seems they mostly fed on gymnosperms, ferns and horsetails rather than flowering plants84. Although the rise of angiosperms would have massively diminished the availability of key components of their diets, our analyses suggest dinosaurs did not suffer significantly from the increase in angiosperm diversity and subsequent changes in global floras. The MBD model also rules out the hypothesis of an effect of sea-level fluctuations (this variable received the least support from the Bayesian inference), which agrees with a previous global dinosaur study40. Importantly, the MBD model captures the previously demonstrated diversity decline due to negative net diversification rates starting in the mid to late Campanian (Fig. 4b), inferred with BDMCMC and RJMCMC models, and reveals that such a decline could be due to global temperature and herbivore diversity (Fig. 4d).
These results imply that warm periods favoured dinosaur diversification whereas cooler periods led to enhanced extinctions, as observed in the latest Late Cretaceous77. This result is particularly in agreement with a recent analysis of multiple tetrapod phylogenies showing the significant effect of Cenozoic cooling on diversification slowdowns, which is linked to the metabolic theory of biodiversity63. As dinosaurs were probably mesothermic organisms85 with varying thermoregulation abilities in different groups86, their activities were probably partially constrained by environmental temperatures. This is particularly true of larger dinosaurs, which almost certainly relied substantially on mass homeothermy to maintain constant body temperatures. It is likely that climatic deterioration would have made such a thermoregulatory strategy more difficult, and that global climate cooling was an important driver of the dinosaur diversity decline as indicated by the MBD diversification model. A physiological explanation for the cooling-driven extinction could be the hypothesis that if sex determination in dinosaurs was temperature dependent, as in crocodiles and turtles, sex switching of embryos could have contributed to diversity loss with a cooling global climate at the end of the Cretaceous87.
According to analyses of Late Cretaceous ecosystem networks20, ankylosaurs, ceratopsians and hadrosaurs represent the very-large-herbivores guild, which was highly influential because of a high number of connections in the food web (depending on their life stages, large herbivores would have been prey of different predators). In addition, the Campanian had higher β-diversity (proportionally more endemic taxa, e.g. Chasmosaurus)88, whereas the Maastrichtian had higher α-diversity (proportionally more widespread taxa, e.g. Triceratops). Therefore, removing a single species of a very large herbivore such as Triceratops could have affected carnivore species distributed among several guilds. The extinction of such highly connected species can have cascade effects on communities89,90,91 so the impact of a declining guild such as very large herbivores could have had consequences throughout the entire food web. The dinosaur decline could thus be explained by the combined effect of interaction with large herbivores and a shift in geographic richness partitioning, which restructured trophic networks and made dinosaurs more sensitive to end-Cretaceous environmental changes like global cooling.
Interactions within and between dinosaur clades
As shown by the MBD model, herbivorous dinosaur diversity could have been linked to the decline of dinosaurs prior to the asteroid impact. Biotic interactions, including competition for resources92, between and within dinosaur groups could have driven species extinction or a speciation failure by either active displacement or passive replacement, respectively58,79,91,93. We used the Multi-Clade Diversity-Dependent (MCDD) model56 to assess clade interactions as a possible mechanism for dinosaur diversification at a global scale and also for North America alone. We expected that negative biotic interactions occurred within families (niche filling), among different groups with similar ecology (competition), and between carnivores and herbivores (predation).
The MCDD analyses first indicate that intra-clade diversity dependence played a role in all dinosaur families except Ankylosauridae (Fig. 5; Supplementary Table 2), and only for Ceratopsidae and Dromaeosauridae at the North American scale (Supplementary Fig. 12, Supplementary Table 3). We find a negative correlation between the diversity and speciation (sometimes extinction) of a clade, meaning that dinosaur speciation rates decreased as they diversified through time. Ecological constraints to dinosaur diversification, such as within-clade competition for resources (niche), probably limited their species diversity. This diversity dependence is particularly strong among carnivores, as we find an effect of negative within-clade interactions for all three carnivorous families (Fig. 5; Supplementary Table 2). For instance, our results suggest that tyrannosaurs decreased their own speciation rates by 23.4% each time a new tyrannosaur species originated, while the speciation rate of ceratopsians reduced by 13.1% when a new ceratopsian species originated. The fact that intra-clade diversity dependence seems lower for herbivores could be explained by differences in patterns of niche partitioning, which might explain the high number of sympatric herbivores92,94,95,96. Browse mode (not height) is a possible niche-partitioning mechanism, as shown by differences in jaw mechanics, dental wear, and skull shapes95. This assumes that inferred functional differences such as those between the grinding dentition of a hadrosaur and the slicing dentition of a ceratopsian implies use of different food plants or plant tissues84. Systematic differences in snout width, which are indicative of different browsing modes, are found between coexisting ankylosaurs, ceratopsians, and hadrosaurs in the Late Cretaceous95. These varied anatomical features among and within dinosaur groups may be linked to the processes of within-clade diversity dependence and niche filling in our model.
The MCDD analyses also show only two negative inter-clade interactions between the studied families (Fig. 5; Supplementary Table 2), suggesting little effect of competition for resources or predation between the different dinosaur groups, in line with palaeoecological analyses of regional fossil assemblages97 (in North America, there is no competition inferred between the families; Supplementary Fig. 12, Supplementary Table 3). These two negative inter-clade interactions involve the Hadrosauridae, and it turns out that each time a new hadrosaur species originated the extinction rate increased by 0.6% in ankylosaurs and by 9.1% in ceratopsians. This result suggests active displacement of Ankylosauridae and Ceratopsidae by the Hadrosauridae, and could explain the more pronounced diversity decline of the two former families (Fig. 3c, f), while the latter declined less markedly in the Maastrichtian (Fig. 3i). Competition exerted by hadrosaurs is not unexpected. In clade-specific analyses revealing how different herbivorous clades rose and fell in disparity during the Cretaceous, Hadrosauridae conform to a pattern of morphospace packing96. This suggests that they did not expand proportionally in morphospace, but rather retained a specific tooth/jaw morphology. Hadrosaurs share certain features in common with ankylosaurs and others in common with ceratopsians95,96, and the fact that ankylosaurs, ceratopsians, and hadrosaurs occupy the same general regions of eco-morphospace92, suggests that Hadrosauridae had comparatively broad herbivorous diets and likely shared food resources with both ankylosaurs and ceratopsians. Nevertheless, hadrosaurs were distinct in that they could feed at heights of up to 5 m above ground, and their teeth were capable of crushing, grinding, and shearing, giving these animals access to plants not available to the other herbivores. In light of their particularly large sizes, generalist diets, and propensity to form herds, hadrosaurs may have had the greatest impact on structuring Late Cretaceous communities92 because of their impact on other herbivores inferred with the MCDD model.
The MCDD analyses at global and North American scales did not identify a significant role for predation on herbivores (Fig. 5; Supplementary Fig. 12, Supplementary Tables 2, 3), perhaps because the studied carnivorous families were not specialized specifically to feed on just these herbivorous families. Indeed, dromaeosaurs, troodontids, and tyrannosaurs are considered more as generalists than specialists as suggested by many functional studies, which show adaptations to a large ecological spectrum (e.g. ambush predators, amphibious predators, scavengers) and diet breadth (e.g. birds, insects, lizards)98,99,100,101,102,103,104,105,106. Our analyses did not detect interactions between carnivorous families, which agrees with evidence from stable isotopes that theropods had different niches within the predator guild, suggesting plausible means by which ecospace was divided among the predatory dinosaurs107,108. However, this result contrasts with recent results showing that tyrannosaur juveniles outcompeted smaller theropods109, although we estimated marginally non-significant competition in North American carnivores (tyrannosaurs over dromaeosaurs; Supplementary Table 3).
Surprisingly, the MCDD analyses also estimate several cases of positive inter-clade interactions mostly driven by Ankylosauridae (and Dromaeosauridae in North America). We estimate that increasing ankylosaur diversity improved the speciation rates of Ceratopsidae and Hadrosauridae by 11.9% and 4.9%, respectively, (Fig. 5; Supplementary Table 2), and, unexpectedly, it also reduced the extinction rate of Dromaeosauridae by 16.6%. It is well recognized that large bodied herbivorous dinosaurs such as ceratopsians, hadrosaurs and sauropods likely had gregarious behaviour. Evidence of gregarious behaviour exists for some Asian ankylosaurs (Pinacosaurus, Talarurus) at juvenile stages110,111,112. However, ankylosaur data point to a solitary adult life with efficient anti-predator defence system. Indeed, the extensive armour of adult ankylosaurs composed of plates, spikes and tail clubs indicates stronger agonistic behaviour than in other medium- to large-sized herbivorous dinosaurs113. Bearing in mind that the osteoderms could have performed multiple functions, such as thermoregulation or display, the ankylosaur armour complex is considered as an example of an efficient passive defence system, which is further elaborated to active defence with the tail club113. Tail clubs are extremely rare across the animal tree of life114. The evolution of this structure suggests they experienced an adaptive response to selective pressures imposed by predation (predator deterrence and active defence), which prompted the evolution of skeletal precursors necessary to support the evolution of tail clubs114,115. Thus we may hypothesize that ankylosaurs may have acted as predator deterrence for the whole herbivorous guild.
Old dinosaur species went extinct in the Maastrichtian
Van Valen’s law of constant extinction was that the probability of extinction is independent of taxon age116. However, study of various fossil groups points to age-dependent extinction (ADE), either that recently originated species turn over faster than old species58, evidence of taxon selectivity for survival, or that old species could go extinct first, suggesting a lack of evolutionary novelty or poor fitness to a changing environment. We fit the Bayesian ADE model117 in PyRate (see Methods). Throughout the Late Cretaceous, we find no evidence for ADE (ɸ = 1.077, 95% CI = 0.856–1.299; Supplementary Table 4) in agreement with Van Valen’s law of constant extinction. However, when analysing the fossil record of the pre-declining phase (before 76 Ma) versus the declining phase (76–66 Ma) there is a significant effect of ADE, with old species having higher rates of extinction during the declining phase (ɸ = 1.478, 95% CI = 1.046–1.930; Supplementary Table 4), while there was no effect during the pre-declining phase (ɸ = 0.718, 95% CI = 0.304–1.256; Supplementary Table 4). This result holds when we analyse the Campanian versus Maastrichtian fossil record with the Maastrichtian dinosaurs showing strong evidence for ADE, in which old species are much more likely to become extinct than new species (ɸMaastrichtian = 1.733, 95% CI = 1.136–2.477; ɸCampanian = 0.847, 95% CI = 0.616–1.104; Supplementary Table 4). For instance, the extinction rate for a Maastrichtian dinosaur species 0.1 Myr after its speciation is 0.032, whereas for a species that has lived 1 Myr, it is considerably increased (0.1705). Extinction rates increase with increasing taxon age, reaching as high as 0.923 after 10 Myr. These results are generally in contrast with previous studies on ADE, which mostly found that the recently originated species are more likely to become extinct than older species58,117,118,119. Geographic range is often considered as a key factor for ADE such that widely distributed taxa are buffered against extinction. However, dinosaurs show an opposite pattern with the Campanian (and pre-declining phase) having higher endemism, whereas the Maastrichtian (and declining phase) dinosaurs have a more widespread distribution88. Therefore, geographic ranges are unlikely to explain the ADE detected here. Instead, given the results from the MBD and MCDD models, we hypothesize a lack of evolutionary novelty (e.g. morphological disparity, niche packing96,120,121) or adaptation to a changing environment (e.g. few angiosperms in herbivorous diets92) for the non-avian dinosaurs in the last 10 Myr before the asteroid impact.
Here we propose an explanation for variations and decline of dinosaur diversity through time, which not only relies on both abiotic (temperature) and biotic (herbivorous dinosaur diversity) factors, but also on intrinsic species age effect on extinction. However, our study comes with issues either related to the dataset or the analytical approaches. First, it is important to recall that our results hold for six species-rich families of the Cretaceous that are well represented in the fossil record. This does not represent a complete picture of the global diversification dynamics for all dinosaurs, but this study is a step forward in our understanding of the causes of dinosaur extinction. As new fossil discoveries and descriptions are continuously being made66,122, assembling and analysing new large global fossil datasets will improve our understanding of the diversification of non-avian dinosaurs. Second, as with any process-based model PyRate makes assumptions about the processes generating the evolutionary history of a clade. These assumptions can violate real evolutionary processes. For instance, we did not explicitly take into account the geographic bias in sampling fossils while modelling diversification rates. Third, our results depend on the choice and availability of environmental and biological variables used as diversification drivers. Our data and analyses focus on ten candidates reflecting widespread environmental changes as likely factors that could have influenced the diversification of dinosaurs. Additional factors could be at play, such as changes in land area or biogeochemical cycles. Given the general difficulties around the estimation of birth–death models, we attempted to identify and test clear hypotheses under simplifying assumptions. These data show that the final extinction of dinosaurs cannot be attributed solely to the K/Pg mass-extinction event, and that long-term drivers affected the probability of speciation and extinction before the K/Pg. However, considering the constraints in data availability at high resolution through the periods examined, we could not address here the precise ecological mechanisms underlying the effect of global cooling or the interactions among herbivorous dinosaurs. Future palaeoecological studies at finer spatial or temporal scales might allow testing whether these candidate drivers did play a role during the last stages of dinosaur evolution in the Cretaceous.
Although non-avian dinosaurs dominated terrestrial ecosystems until the end-Cretaceous, our results show that both a marked increase of extinction and a decrease in their ability to replace extinct species led dinosaurs to decline well before the K/Pg extinction. Even though the latest Cretaceous dinosaur fossil record is geographically dominated by Laurasian taxa, the diversity patterns observed here are based on continent-scale samples that reflect a substantial part of latest Cretaceous dinosaur global diversity. Our results lend support to hypotheses that long-term environmental changes led to restructuring of terrestrial ecosystems that made dinosaurs particularly prone to extinction20. These results are also consistent with modelling studies of ecological food-webs13 and suggest that loss of key herbivorous dinosaurs would have made terminal Maastrichtian ecosystems—in contrast with ecosystems from earlier in the Late Cretaceous (Campanian)—more susceptible to cascading extinctions by an external forcing mechanism. We propose that a combination of global climate cooling, the diversity of herbivores, and age-dependent extinction had a negative impact on dinosaur extinction in the Late Cretaceous; these factors impeded their recovery from the final catastrophic event.
Selection of non-avian dinosaur families
The focus of this study was on species-rich, well known and widespread Cretaceous dinosaur families that were the major faunal elements until dinosaurs went extinct at the K/Pg boundary. Four main criteria were used to select the dinosaur families to be analysed: (i) the family must have been a dominant component of the Cretaceous with high taxonomic diversity in the Late Cretaceous (i.e. the family is a good representative of dinosaur macroevolutionary trends); (ii) the family fossil record must have been well represented in the Late Cretaceous, in particular over the last two stages (Campanian and Maastrichtian), with different species having several occurrences in order to avoid biases towards the inference of speciation slowdown; (iii) the family must be represented by a minimum number of 100 occurrences per family and at least 10 species; and (iv) the family systematics and taxonomy should be sufficiently well known that we could make a species list of currently known and accepted species and make decisions regarding the assignment of dubious specimens to a specific taxon based on critical appraisal of type material.
Based on these selective criteria, the following dinosaur families were retained in the analyses: Ankylosauridae (armoured dinosaurs), Ceratopsidae (horned dinosaurs), Dromaeosauridae (feathered theropod dinosaurs), Hadrosauridae (duck-billed dinosaurs), Troodontidae (bird-like theropod dinosaurs), and Tyrannosauridae (tyrant dinosaurs). Although other groups were surveyed for inclusion in the dataset, such as the theropod clades Abelisauroidae, Allosauroidea, Megalosauroidea, and also ornithischian clades Nodosauridae and Pachycephalosauridae, they could not be analysed for two main reasons. Fossil occurrences in the Campanian–Maastrichtian are not currently available in quantity to assemble a large dataset, almost entirely due to poor fossil sampling. Taxonomic confusion remains for the status of many taxa, including the family itself (e.g. Pachycephalosauridae123,124,125), which results in a small dataset (130 occurrences in the case of Pachycephalosauridae) likely due to the difficulty of assigning some taxa to a given higher-level group.
Birds were not included in the dataset, because we chose to focus specifically on non-avian dinosaurs, and more importantly, because of severe sampling biases that limit the number of Campanian–Maastrichtian lineages with too few occurrences that could be used (resulting in a reduced dataset). However, we included two non-avian dinosaur clades (Dromaeosauridae, Troodontidae) that are included with birds in the clade Paraves126.
Fossil occurrences for each family were initially retrieved using the Paleobiology Database through the FossilWorks website (fossilworks.org/; regularly accessed between November 11, 2015 and May 2, 2020). The literature was thoroughly screened to check and clean each occurrence one by one but also to include additional occurrences. We decided to include in the dataset the recently described and valid taxa (species or genus) but only known from a single specimen and thus lacking multiple occurrences (e.g. Zuul crurivastator Arbour & Evans127 for which ROM 75860 is the single known specimen of this ankylosaur species; Dynamoterror dynastes McDonald, Wolfe & Dooley128 for which UMNH VP 28348 is the single known specimen of this tyrant species), despite the possibility to increase singletons. The literature search was done especially to clarify and correct the taxonomy based on the latest advances in dinosaur systematics and discoveries. Because the databases also include records of fragmentary specimens that have been assigned to various species in the literature (sometimes, regardless of whether or not that assignment is well-supported or based on solid evidence), each entry was scrutinized using the museum specimen number to track its assignment in the literature. Only specimens that could confidently be assigned to a species were included and we were able to identify 1555 unique specimen numbers out of 1636 total occurrences (81 occurrences had no specimen numbers). All dubious or poorly justified material was removed to avoid biases in diversity or age of first/last appearance and singletons. In cases of conflict, two approaches were followed depending on whether the conflict was ‘hard’ or ‘soft’: either there is a soft conflict meaning that there is a taxonomic consensus about the assignment of material according to several studies and the occurrence can be retained (e.g. the genus Torosaurus is separated from the genus Triceratops129), or there is a hard conflict meaning that no taxonomic solution is found based on current data, and the fossil occurrences were discarded (e.g. Nanotyrannus is either considered a distinct genus or a junior synonym of Tyrannosaurus130,131,132,133).
For Troodontidae, arguably one of the least understood dinosaur groups, we decided to include the Anchiornithinae134 that are more often ranked as Anchiornithidae70,99,135,136,137. Indeed, anchiornithids have been recovered in alternative positions within the maniraptoran tree, with some phylogenetic studies classifying them as a distinct family, an early-diverging subfamily of Troodontidae, members of Archaeopterygidae, or a phyletic grade within Avialae or Paraves70,99,136,137,138,139,140. However, most of the latest phylogenetic studies found the following anchiornithine species: Anchiornis huxleyi, Aurornis xui, Caihong juji, Eosinopteryx brevipenna, Jianianhualong tengi, and Xiaotingia zhengi, to form a clade that is either sister to Troodontidae or included in Troodontidae99,135,136,141. These anchiornithine taxa are all from the Late Jurassic to Early Cretaceous, hence the diversification and diversity dynamics in the Late Cretaceous are not altered whether they are included or excluded from the troodontid dataset.
We included as many specimens as possible in each family dataset. Despite a low sample size of fossil occurrences, we still included the Ankylosauridae because the family was an important component of Late Cretaceous ecosystems and their taxonomy has been well studied53,142,143,144,145. Overall, we retained six family datasets containing at least 100 occurrences and 10 species, and groups spanning the entire Late Cretaceous while being important elements of the ecosystems.
To examine whether carnivorous and herbivorous dinosaurs had similar diversification dynamics over time, these six families were divided into two datasets based on their diets (carnivorous versus herbivorous). The carnivorous dinosaurs (Theropoda) included the three families Dromaeosauridae, Troodontidae and Tyrannosauridae, and the herbivorous dinosaurs (Ornithischia) comprised the three families Ankylosauridae, Ceratopsidae and Hadrosauridae. Finally, we assembled a ninth dataset including all six families in order to estimate a general macroevolutionary trend for the Cretaceous dinosaurs. It is important to mention that because of long-standing historical collection biases, there is an abundance of Laurasian (North American and Asian) taxa relative to Gondwanan taxa in all datasets (a common problem previously encountered and discussed11,13). Hence, it should be borne in mind that our results are dominated by Laurasian dinosaur diversity trends and might not exactly reveal global diversification dynamics. All taxa included (genus and species) and analysed in this study, along with their temporal information (period, epoch, stage, and absolute age), geographic provenance (country and province/state) and when possible the type material information (specimen number) are listed in the Source data files (see Data availability).
Assignment of specimen (taxon) age
Each taxon was first placed in a geological period, epoch, stage, and geological formation (temporal categories) as accurately as possible and using the latest geological timescale146. Each taxon in the six families was then assigned a minimum age and maximum age that correspond to the upper and lower boundaries of the respective geological strata, respectively. For instance, if a specimen of a given taxon is found in the Maastrichtian without additional information, we assigned a minimum age of 66.0 and a maximum age of 72.1 Myr ago146. Otherwise, in the Maastrichtian of North America, for example, we can distinguish the early Maastrichtian (Edmontonian, 72–69 Myr ago) versus the late Maastrichtian (Lancian, 69–66 Myr ago). Fossil specimens often come with radiometric dating providing accurately determined ages (minimum and maximum ages are close); for instance the specimen of Regaliceratops peterhewsi (TMP 2005.055.0001) found in the Late Cretaceous of the Oldman River in the area of Waldron Flats (164 km south of Calgary, Alberta, Canada) is dated at 67.5–68.5 Myr ago147. Most terminal Cretaceous dinosaur-bearing formations can confidently be assigned either a late Campanian or Maastrichtian age, but, if not, we used a conservative approach and regarded specimens (taxa) from these formations as ranging through the late Campanian and Maastrichtian (and thus they were placed in both stages). However, the narrow stratigraphic ranges for North American dinosaurs are not as accurate for dinosaurs from Mongolia and South America for example, where many classic dinosaur-bearing formations are of uncertain age. To balance these uncertainties, we chose 10 Myr bins or stage level as a compromise, but we acknowledge the ages can be revised further when future studies refine these ages into smaller time bins. For instance, after considerable debate, the Djadokhta Formation is considered to be late Campanian in age and the overlying Nemegt is Maastrichtian13. Fortunately, this issue concerned only seven species (Byronosaurus jaffei, Gobivenator mongoliensis, Mahakala omnogovae, Pinacosaurus grangeri, Saurornithoides mongoliensis, Velociraptor mongoliensis, and Zhuchengtyrannus magnus). There is also strong evidence supporting the Nemegt Formation as being early Maastrichtian in age or even the possibility that it is synchronous with the Djadokhta as late Campanian in age148. In all cases, our decision to regard these formations as late Campanian and Maastrichtian in age, respectively, should maximize the differences between the two time bins, making it more likely that they exhibit significant diversification dynamics.
Final fossil datasets
In total, we were able to assemble a dataset of dinosaur fossils comprising 1636 occurrences, which represent 247 Cretaceous dinosaur species (Dataset 1). The whole dataset splits up into a carnivorous dinosaur dataset including 763 occurrences and 105 species (Dataset 2), and into an herbivorous dinosaur dataset comprising 873 occurrences and 142 species (Dataset 3). The six-family fossil datasets contain: 184 (125 originally from Paleobiology Database) occurrences and 32 species for Ankylosauridae (Dataset 4), 329 (335) occurrences and 49 species for Ceratopsidae (Dataset 5), 288 (492) occurrences and 51 species for Dromaeosauridae (Dataset 6), 360 (388) occurrences and 61 species for Hadrosauridae (Dataset 7), 175 (172) occurrences and 37 species for Troodontidae (Dataset 8), and 300 (206) occurrences and 17 species for Tyrannosauridae (Dataset 9). All nine fossil-occurrence datasets are available as data files (Datasets 1–9, see Data availability).
Modelling the evolutionary dynamics of speciation and extinction
We carried out analyses of the fossil datasets based on the Bayesian framework implemented in the program PyRate55,149. We analysed the fossil datasets under time-varying birth–death models to estimate simultaneously for each clade (i) the parameters of the preservation process, (ii) the times of speciation (Ts) and extinction (Te) of each species, (iii) the speciation and extinction rates and their variation through time, and (iv) the number and magnitude of shifts in speciation and extinction rates. The preservation process infers the individual origination and extinction times of each taxon based on all fossil occurrences and on an estimated preservation rate, denoted q, and expressed as expected occurrences per taxon per Myr. To cross-validate rate inferences, we applied two birth–death models that estimate rate variations and infer shifts of diversification as well as the Ts and Te for each species. We first performed the classical BDMCMC (-A 2 option) and secondly its recently enhanced version through the reversible-jump MCMC (RJMCMC) algorithm (-A 4 option).
For each of the nine datasets, we ran PyRate for 5 million MCMC generations for the family datasets and 10 million MCMC generations for the whole, carnivorous and herbivorous dinosaurs datasets. All analyses were set with the best-fit preservation process after comparing (-PPmodeltest option) the homogeneous Poisson process (-mHPP option), the non-homogeneous Poisson process (default option), and the time-variable Poisson process (-q option). The time-variable Poisson process estimated a preservation rate for each geological stage. We also accounted for varying preservation rates across taxa using the Gamma model (-mG option), that is, with gamma-distributed rate heterogeneity55. We monitored chain mixing and effective sample sizes by examining the log files in Tracer 1.7.1150 after excluding the first 10% of the samples as the burn-in period. We then combined the posterior estimates of the origination and extinction rates across all replicates to generate rates-through-time plots (origination, extinction, and net diversification).
We replicated all the analyses on ten randomized datasets of each clade and calculated estimates of times of speciation and times of extinction as the mean of the posterior samples from each replicate. Thus, we obtained ten posterior estimates of the Ts and Te for all species and we estimated the past diversity dynamics by calculating the number of living taxa at every point in time based on the Ts and Te. For all the subsequent analyses, we used the estimated Ts and Te for all species, which avoids re-modelling preservation and re-estimating times of speciation and extinction, therefore focusing exclusively on the estimation of the birth–death parameters for specific models. This procedure reduced drastically the computational burden, while still allowing us to account for the preservation process and the uncertainties associated with the fossil ages.
We analysed the datasets at the global scale, and did not analyse them at the regional scale given that in most cases (e.g. Ankylosauridae and Tyrannosauridae) there are a low number of species and/or small regional sample sizes53,143,151. Ceratopsidae could only be analysed at the North American level because the group is almost completely absent outside this continent152,153.
We then used the estimated times of speciation and extinction of all species to carry out additional sets of analyses to test whether speciation and extinction rate dynamics correlate with abiotic or biotic factors. The former are exemplified by Cretaceous changes in environmental conditions using proxies for abiotic factors such as global temperature and sea-level fluctuations. The latter are exemplified by positive or negative interactions between dinosaur diversification and changes in plant (angiosperms and gymnosperms) diversity through time. Thus, the times of speciation and extinction used in all the subsequent analyses were obtained while accounting for the heterogeneity of preservation, speciation, and extinction rates.
Robustness of evolutionary dynamics inference
The robustness of PyRate has been thoroughly evaluated using simulations that reflect commonly observed diversity dynamics37,55,56. Datasets were simulated under a range of potential biases, including violations of the sampling assumptions, variable preservation rates, and incomplete taxon sampling. Simulation results showed that the dynamics of speciation and extinction rates, including sudden rate changes and mass extinction, are correctly estimated under a wide range of conditions, such as low levels of preservation (down to 1–3 fossil occurrences per species on average), severely incomplete taxon sampling (up to 80% missing), and high proportion of singletons (exceeding 30% of the taxa in some cases).
It is known that the strongest bias in birth–death rate estimates is caused by incomplete data because missing lineages alter the distribution of taxa; an effect notably pervasive in phylogeny-based models. However, in the case of PyRate, simulations confirm the absence of consistent biases due to the incompleteness of the data in the fossil record. Incomplete taxon sampling appears to have a less problematic effect on the estimation of speciation and extinction rates because, in contrast to molecular phylogenies, removing a random set of taxa does not affect the observed occurrences of other lineages55. In addition, it has recently been shown that the RJMCMC model is very accurate for estimating speciation and extinction rates, and is able to recover sudden extinction events regardless the biases in the fossil dataset37. Finally, the RJMCMC model in PyRate estimates diversification dynamics more accurately than traditional approaches such as the boundary-crossing and three-time methods37.
We have nonetheless assessed the robustness of the diversification and diversity dynamics as inferred in PyRate at the global scale by analysing the fossil dataset at the hemisphere scale. We divided the global dataset into a New World and an Old World dataset to estimate whether we recovered similar dynamics of speciation, extinction and species diversity. We repeated the PyRate analyses with the BDMCMC model (as explained previously) and compared the hemisphere-scale patterns to the global patterns (Supplementary Fig. 4).
Selection of potential drivers of diversification dynamics
Sakamoto et al.10 could not identify a causal mechanism for the speciation downturn in dinosaurs, although they proposed that variations of sea level were an important driver as often proposed18,40,71. To identify putative mechanisms of Mesozoic dinosaurian demise, we examined the correlation between a series of past environmental variables and speciation/extinction rates over the entire Cretaceous. There are several possible global or regional phenomena that occurred during the Cretaceous Period, especially towards the end of the Late Cretaceous19,29, which could have affected dinosaur diversification. We focused on the role of four palaeoenvironmental variables, also called proxies, which have been linked to extinctions and biodiversity change in marine invertebrates154,155. These proxies were classified as either abiotic or biotic controls as follows:
(i) Abiotic controls: Climate change (variations from warming to cooling periods) is one of the most probable drivers of diversification changes throughout the history of life63,156,157. Major trends in global climate change through time are typically estimated from relative proportions of different oxygen isotopes (δ18O) in samples of benthic foraminifer shells158. We merged δ18O global temperature data from different sources82,158,159,160 to provide δ18O data spanning the full time-range over which dinosaur families diversified. Second, fluctuations in sea level have also been proposed as a possible driver of dinosaur diversity dynamics, perhaps by limiting dispersal and gene flow. Such physical changes are expected to isolate populations and eventually foster speciation (allopatry) or could also lead to extinction if populations are too small. Major trends in global changes in sea level through time are also estimated with oxygen isotope (δ18O) data indirectly recorded in the chemistry of foraminifera44. Comparing modern and past values of δ18O allows us to estimate changes in sea level (in metres) relative to present sea level. Third, global continental fragmentation, as approximated by plate tectonic change over time, has often been proposed as a driver of dinosaur diversity dynamics17. We retrieved the index of continental fragmentation developed by Zaffos et al.41 using palaeogeographical reconstructions for 1-million-year time intervals. This index approaches 1 when all plates are not connected (complete plate fragmentation) and approaches zero when there is maximum aggregation.
(ii) Biotic controls: Ecological interactions with rapidly expanding clades are increasingly recognized as important macroevolutionary drivers56,155. Dinosaurs experienced a drastic floristic change in the mid-Cretaceous with the origin and rapid radiation of angiosperms16,161,162 at the expense of a decline in diversity of gymnosperms and non-Polypodiales ferns, while polypodialean ferns expanded after the Cretaceous. The rise and dominance of angiosperms may have contributed to altering the dietary regimes of herbivorous dinosaurs, which could in turn have affected carnivorous dinosaurs by a cascading effect. We thus compiled the relative diversity trajectories of angiosperms, gymnosperms, non-Polypodiales, and Polypodiales ferns based on previous estimates of plant diversity57,81.
(iii) Dinosaur diversity: Biotic interactions within and among dinosaurs could also have influenced dinosaur diversification92,94,95,96,97,107. For instance, we could draw hypotheses of inter-group diversity dependence such that carnivorous dinosaurs, potentially preying on herbivorous dinosaurs, could either impact or be impacted by herbivore diversity. In other words, the change in diversity of one ecological group can affect the diversification of the other. We thus included the palaeodiversity of all studied dinosaurs, of carnivorous dinosaurs, and of herbivorous dinosaurs to account for diversity dependence within and among dinosaurs. We estimate, for instance, whether carnivores imposed some predation pressure that would have affected the diversification of herbivores, and whether herbivorous diversity limited the diversification of carnivores.
Estimating palaeoenvironment-dependent diversification
Recently developed methods enable quantification of the potential effect of external (environmental) variables on diversification rates. Such an approach allows speciation and extinction rates to depend not only on time but also on an external variable that varies through time63,80. This approach assumes that clades evolve under a birth–death process, that speciation and extinction rates can vary through time, and both can be influenced by one or several environmental variables that also vary through time, for instance past variations in global temperature. Note that while observations of the environmental variables are discrete, we use a smoothing function to model diversification rates in continuous time that stands for speciation and extinction rates influenced by temperature and time for instance. The approach can be used to derive likelihoods for functional forms of λ and μ.
PyRate has developed and implemented this birth–death model to test for a correlation between speciation and extinction rates and changes in environmental variables56. We used the Multivariate Birth-Death model (MBD) to assess to what extent biotic and abiotic factors can explain temporal variation in speciation and extinction rates57. Under the MBD model, speciation and extinction rates can change through time (but equally across all lineages as in the RJMCMC model) through correlations with multiple time-continuous variables, and the strengths and signs (positive or negative) of the correlations are jointly estimated for each variable. We applied two models, one with linear and the other with exponential correlations. The model with linear correlations is similar to the recently described Multiple Clade Diversity Dependence model56, where speciation and extinction rates were modelled through linear correlations with the diversity trajectories of several clades. The MBD model replaces clade trajectories with environmental variables, so that the speciation and extinction rates depend on the temporal variations of each factor. The correlation parameters can take negative values indicating negative correlation, or positive values for positive correlations. When their value is estimated to be approximately zero, no correlation is estimated. A MCMC algorithm jointly estimates the baseline speciation (λ0) and extinction (µ0) rates and all correlation parameters (Gλ and Gµ) using a horseshoe prior to control for over-parameterization and for the potential effects of multiple testing57. The horseshoe prior provides an efficient approach to distinguishing correlation parameters that should be treated as noise (and therefore shrunk around 0) from those that are significantly different from 0 and represent true signal.
We ran the MBD model using 20 million MCMC iterations and sampling every 20,000 to approximate the posterior distribution of all parameters (λ0, µ0, ten Gλ, ten Gµ, and the shrinkage weights of each correlation parameter, ωG). We summarized the results of the MBD analyses by calculating the posterior mean and 95% CI of all correlation parameters and the mean of the respective shrinkage weights (across ten replicates), as well as the mean and 95% CI of the baseline speciation and extinction rates.
Regarding the biological meaning of the parameters estimated with MBD with temperature for instance, the estimation of a positive Gλ would indicate that higher temperatures increase speciation rates, whereas a negative Gλ would indicate that higher temperatures decrease speciation rates. The same rationale applies to the extinction rate but with the parameter Gμ quantifying the correlation between changes in extinction rates and this variable. Let’s imagine the positive effect of temperature on speciation given by Gλ = 0.05. This result means that speciation and temperature correlate positively such that speciation increased by 5% as global temperatures increased every time step (here, every 0.1-million years) and conversely.
Estimating between-family interactions on diversification
We attempted to gain insights into the effect of between-clade and within-clade interactions on dinosaur diversification using the Multiple Clade Diversity Dependence (MCDD) model in which speciation and extinction rates are correlated with the diversity trajectory of a clade56. Under competitive interactions, increasing species diversity has the effect of suppressing the speciation rates and/or increasing the extinction rates (e.g. when hadrosaurs diversify, ankylosaurs do not). Under positive interactions, increasing species diversity has the effect of boosting speciation rates and/or decreasing extinction rates (e.g. when herbivores diversify, so do carnivores). Such birth–death models are generally referred to as diversity-dependent models. The MCDD model allows for competition/positive interaction to take place not only among the species of a given clade but also among species that are not closely related but share similar ecology. Therefore, we assessed the effects of competition/positive interaction within and between clades by jointly analysing all clades and estimate the baseline speciation and extinction rates for each clade, the marginal probability of competition/positive interaction for each clade, and parameters that quantify the intensity of the diversity dependence between each pair of clades. Each parameter expresses a diversity-dependence relationship between the diversity of a clade and the speciation or extinction rates of the other clade. Hence, the model is able to infer directionality of the reciprocal interactions between two clades, i.e. either competition or positive interaction between the clades.
We estimated the past diversity dynamics for each dinosaur family by calculating the number of living species at every point in time based on the times of speciation and extinction estimated under the RJMCMC model (see above, Fig. 3). We calculated ten diversity trajectories from the ten replicated analyses under the RJMCMC model. The estimation of past species diversity might be biased by low preservation rates, taxonomic uncertainties, or cases of anagenetic speciation. However, such trajectory curves are likely to provide a reasonably accurate representation of the past diversity changes in the studied clades.
We ran 20 million MCMC iterations of the MCDD model with sampling frequency of 2000 to obtain posterior parameter estimates. We repeated the analyses on the ten replicates, using the times of speciation and extinction estimated under the RJMCMC model. For each of the six dinosaur families we computed median and 95% CI of the baseline speciation and extinction rates (λi and μi), the within-clade diversity-dependence parameters gλi and gμi, and the between-clade diversity-dependence parameters gλij and gμij. We used the mean of the sampled diversity-dependence parameters (e.g. gλij) as a measure of intensity of competition (if positive) or positive interaction (if negative) between each pair of families. The respective probabilities of competition or positive interaction between pairs of families were calculated as the sampling frequency of positive or negative values.
Because the MCDD analyses were performed at global scale, it is possible that some inferred clade interactions are artefactual and the result of a similar response to an external variable58. Adding a geographical component by restricting the analyses to North America could help narrowing the ecological interpretations of such analyses. The North American fossil record of dinosaurs stands among the best and there is a good background on the dinosaur communities in the Late Cretaceous, with the prior assumption that an ecological restructuring facilitated the end-Cretaceous mass extinction20.
Regarding the biological meaning of the parameters estimated with the MCDD model, let’s imagine the competing effects given by gλij = 0.1 and gμij = 0.2. These results mean that the addition of one species in clade j will decrease the speciation rate in clade i by 10% of the baseline rate (λi) and increase its extinction rate by 20% of the baseline rate (μi). Conversely, the extinction of a species in clade j will increase clade’s i speciation rate and decrease its extinction rate by 10% and 20%, respectively.
Further information on research design is available in the Nature Research Reporting Summary linked to this article.
All dinosaur datasets to repeat the analyses described here are available through the Figshare digital data repository (https://doi.org/10.6084/m9.figshare.14169575.v1).
The command lines set to run all the models presented in this study are available through the Figshare digital data repository (https://doi.org/10.6084/m9.figshare.14169575.v1).
Weishampel, D. B., Dodson, P. & Osmólska, H. The Dinosauria 2nd edn (University of California Press, 2004).
Fastovsky, D. E. & Weishampel, D. B. The Evolution and Extinction of the Dinosaurs (Cambridge University Press, 2005).
Brusatte, S. L. et al. The extinction of the dinosaurs. Biol. Rev. 90, 628–642 (2015).
Alvarez, L. W., Alvarez, W., Asaro, F. & Michel, H. V. Extraterrestrial cause for the Cretaceous-Tertiary extinction. Science 208, 1095–1108 (1980).
Chiarenza, A. A. et al. Asteroid impact, not volcanism, caused the end-Cretaceous dinosaur extinction. Proc. Natl Acad. Sci. USA 117, 17084–17093 (2020).
Schulte, P. et al. The Chicxulub asteroid impact and mass extinction at the Cretaceous-Paleogene boundary. Science 327, 1214–1218 (2010).
Russell, D. A. The gradual decline of the dinosaurs—fact or fallacy? Nature 307, 360–361 (1984).
Sloan, R. E., Rigby, J. K., Van Valen, L. M. & Gabriel, D. Gradual dinosaur extinction and simultaneous ungulate radiation in the Hell Creek Formation. Science 232, 629–633 (1986).
Sheehan, P. M., Fastovsky, D. E., Hoffmann, R. G., Berghaus, C. B. & Gabriel, D. L. Sudden extinction of the dinosaurs: Latest Cretaceous, upper Great Plains, USA. Science 254, 835–839 (1991).
Sakamoto, M., Benton, M. J. & Venditti, C. Dinosaurs in decline tens of millions of years before their final extinction. Proc. Natl Acad. Sci. USA 113, 5036–5040 (2016).
Chiarenza, A. A. et al. Ecological niche modelling does not support climatically-driven dinosaur diversity decline before the Cretaceous/Paleogene mass extinction. Nat. Commun. 10, 1091 (2019).
Russell, L. S. Body temperature of dinosaurs and its relationships to their extinction. J. Paleontol. 39, 497–501 (1965).
Brusatte, S. L., Butler, R. J., Prieto-Márquez, A. & Norell, M. A. Dinosaur morphological diversity and the end-Cretaceous extinction. Nat. Commun. 3, 804 (2012).
Benson, R. B. J. et al. Rates of dinosaur body mass evolution indicate 170 million years of sustained ecological innovation on the avian stem lineage. PLoS Biol. 12, e1001853 (2014).
Rezende, E. L., Bacigalupe, L. D., Nespolo, R. F. & Bozinovic, F. Shrinking dinosaurs and the evolution of endothermy in birds. Sci. Adv. 6, eaaw4486 (2020).
Lloyd, G. T. et al. Dinosaurs and the Cretaceous Terrestrial Revolution. Proc. R. Soc. B Biol. Sci. 275, 2483–2490 (2008).
Gates, T. A., Prieto-Márquez, A. & Zanno, L. E. Mountain building triggered Late Cretaceous North American megaherbivore dinosaur radiation. PLoS ONE 7, e42135 (2012).
Loewen, M. A., Irmis, R. B., Sertich, J. J. W., Currie, P. J. & Sampson, S. D. Tyrant dinosaur evolution tracks the rise and fall of late Cretaceous oceans. PLoS ONE 8, e79420 (2013).
Archibald, J. D. et al. Cretaceous extinctions: Multiple causes. Science 328, 973 (2010).
Mitchell, J. S., Roopnarine, P. D. & Angielczyk, K. D. Late Cretaceous restructuring of terrestrial communities facilitated the end-Cretaceous mass extinction in North America. Proc. Natl Acad. Sci. USA 109, 18857–18861 (2012).
Schoene, B. et al. U-Pb constraints on pulsed eruption of the Deccan Traps across the end-Cretaceous mass extinction. Science 363, 862–866 (2019).
Sprain, C. J. et al. The eruptive tempo of Deccan volcanism in relation to the Cretaceous-Paleogene boundary. Science 363, 866–870 (2019).
Hull, P. M. et al. On impact and volcanism across the Cretaceous-Paleogene boundary. Science 367, 266–272 (2020).
Landman, N. H. et al. Ammonite extinction and nautilid survival at the end of the Cretaceous. Geology 42, 707–710 (2014).
Longrich, N. R., Martill, D. M. & Andres, B. Late Maastrichtian pterosaurs from North Africa and mass extinction of Pterosauria at the Cretaceous-Paleogene boundary. PLoS Biol. 16, e2001663 (2018).
Longrich, N. R., Tokaryk, T. & Field, D. J. Mass extinction of birds at the Cretaceous-Paleogene (K-Pg) boundary. Proc. Natl Acad. Sci. USA 108, 15253–15257 (2011).
Longrich, N. R., Bhullar, B.-A. S. & Gauthier, J. A. Mass extinction of lizards and snakes at the Cretaceous-Paleogene boundary. Proc. Natl Acad. Sci. USA 109, 21396–21401 (2012).
Fastovsky, D. E. et al. Shape of Mesozoic dinosaur richness. Geology 32, 877–880 (2004).
Archibald, J. D. in Volcanism, Impacts, and Mass Extinctions: Causes and Effects (eds. Keller, G. & Kerr, A. C.) 213–224 (The Geological Society of America Special Paper 505, 2014).
Wang, S. C. & Dodson, P. Estimating the diversity of dinosaurs. Proc. Natl Acad. Sci. USA 103, 13601–13605 (2006).
Starrfelt, J. & Liow, L. H. How many dinosaur species were there? Fossil bias and true richness estimated using a Poisson sampling model. Philos. Trans. R. Soc. B Biol. Sci. 371, 20150219 (2016).
Bonsor, J. A., Barrett, P. M., Raven, T. J. & Cooper, N. Dinosaur diversification rates were not in decline prior to the K-Pg boundary. R. Soc. Open Sci. 7, 201195 (2020).
Benton, M. J., Wills, M. A. & Hitchin, R. Quality of the fossil record through time. Nature 403, 534–537 (2000).
Alroy, J. et al. Effects of sampling standardization on estimates of Phanerozoic marine diversification. Proc. Natl Acad. Sci. USA 98, 6261–6266 (2001).
Alroy, J. et al. Phanerozoic trends in the global diversity of marine invertebrates. Science 321, 97–100 (2008).
Close, R. A., Evers, S. W., Alroy, J. & Butler, R. J. How should we estimate diversity in the fossil record? Testing richness estimators using sampling-standardised discovery curves. Methods Ecol. Evol. 9, 1386–1400 (2018).
Silvestro, D., Salamin, N., Antonelli, A. & Meyer, X. Improved estimation of macroevolutionary rates from fossil data using a Bayesian framework. Paleobiology 45, 546–570 (2019).
Close, R. A., Benson, R. B. J., Saupe, E. E., Clapham, M. E. & Butler, R. J. The spatial structure of Phanerozoic marine animal diversity. Science 368, 420–424 (2020).
Benton, M. J. Scientific methodologies in collision: The history of the study of the extinction of the dinosaurs. Evol. Biol. 24, 371–400 (1990).
Butler, R. J., Benson, R. B. J., Carrano, M. T., Mannion, P. D. & Upchurch, P. Sea level, dinosaur diversity and sampling biases: Investigating the ‘common cause’ hypothesis in the terrestrial realm. Proc. R. Soc. B Biol. Sci. 278, 1165–1170 (2011).
Zaffos, A., Finnegan, S. & Peters, S. E. Plate tectonic regulation of global marine animal diversity. Proc. Natl Acad. Sci. USA 114, 5653–5658 (2017).
East, M., Müller, R. D., Williams, S., Zahirovic, S. & Heine, C. Subduction history reveals Cretaceous slab superflux as a possible cause for the mid-Cretaceous plume pulse and superswell events. Gondwana Res. 79, 125–139 (2020).
Grasby, S. E., Them, T. R., Chen, Z., Yin, R. & Ardakani, O. H. Mercury as a proxy for volcanic emissions in the geologic record. Earth Sci. Rev. 196, 102880 (2019).
Miller, K. G. et al. The Phanerozoic record of global sea level change. Science 310, 1293–1298 (2005).
Ray, D. C. et al. The magnitude and cause of short-term eustatic Cretaceous sea-level change: a synthesis. Earth Sci. Rev. 197, 102901 (2019).
Coiffard, C., Gomez, B., Daviero-Gomez, V. & Dilcher, D. L. Rise to dominance of angiosperm pioneers in European Cretaceous environments. Proc. Natl Acad. Sci. USA 109, 20955–20959 (2012).
Chaboureau, A.-C., Sepulchre, P., Donnadieu, Y. & Franc, A. Tectonic-driven climate change and the diversification of angiosperms. Proc. Natl Acad. Sci. USA 111, 14066–14070 (2014).
Magallón, S., Gómez-Acevedo, S., Sánchez-Reyes, L. L. & Hernández-Hernández, T. A metacalibrated time-tree documents the early rise of flowering plant phylogenetic diversity. N. Phytol. 207, 437–453 (2015).
Magallón, S., Sánchez-Reyes, L. L. & Gómez-Acevedo, S. L. Thirty clues to the exceptional diversification of flowering plants. Ann. Bot. 123, 491–503 (2019).
Meredith, R. W. et al. Impacts of the Cretaceous terrestrial revolution and KPg extinction on mammal diversification. Science 334, 521–524 (2011).
Grossnickle, D. M. & Newham, E. Therian mammals experience an ecomorphological radiation during the Late Cretaceous and selective extinction at the K–Pg boundary. Proc. R. Soc. B Biol. Sci. 283, 20160256 (2016).
Liu, L. et al. Genomic evidence reveals a radiation of placental mammals uninterrupted by the KPg boundary. Proc. Natl Acad. Sci. USA 114, E7282–E7290 (2017).
Arbour, V. M., Zanno, L. E. & Gates, T. A. Ankylosaurian dinosaur palaeoenvironmental associations were influenced by extirpation, sea-level fluctuation, and geodispersal. Palaeogeogr. Palaeoclimatol. Palaeoecol. 449, 289–299 (2016).
Tennant, J. P., Mannion, P. D. & Upchurch, P. Sea level regulated tetrapod diversity dynamics through the Jurassic/Cretaceous interval. Nat. Commun. 7, 12737 (2016).
Silvestro, D., Schnitzler, J., Liow, L. H., Antonelli, A. & Salamin, N. Bayesian estimation of speciation and extinction from incomplete fossil occurrence data. Syst. Biol. 63, 349–367 (2014).
Silvestro, D., Antonelli, A., Salamin, N. & Quental, T. B. The role of clade competition in the diversification of North American canids. Proc. Natl Acad. Sci. USA 112, 8684–8689 (2015).
Lehtonen, S. et al. Environmentally driven extinction and opportunistic origination explain fern diversification patterns. Sci. Rep. 7, 4831 (2017).
Condamine, F. L., Romieu, J. & Guinot, G. Climate cooling and clade competition likely drove the decline of lamniform sharks. Proc. Natl Acad. Sci. USA 116, 20584–20590 (2019).
Signor, P. W. & Lipps, J. H. in Geological Implications of Impacts of Large Asteroids and Comets on The Earth (eds. Silver, L. T. & Schultz, P. H.) vol. 190, 291–296 (Geological Society of America Special Publication, 1982).
Benson, R. B. J. Dinosaur macroevolution and macroecology. Annu. Rev. Ecol. Evol. Syst. 49, 379–408 (2018).
Dean, C. D., Chiarenza, A. A. & Maidment, S. C. R. Formation binning: a new method for increased temporal resolution in regional studies, applied to the Late Cretaceous dinosaur fossil record of North America. Palaeontology 63, 881–901 (2020).
Moen, D. & Morlon, H. Why does diversification slow down? Trends Ecol. Evol. 29, 190–197 (2014).
Condamine, F. L., Rolland, J. & Morlon, H. Assessing the causes of diversification slowdowns: Temperature-dependent and diversity-dependent models receive equivalent support. Ecol. Lett. 22, 1900–1912 (2019).
Prieto-Márquez, A., Dalla Vecchia, F. M., Gaete, R. & Galobart, À. Diversity, relationships, and biogeography of the lambeosaurine dinosaurs from the European archipelago, with description of the new aralosaurin Canardia garonnensis. PLoS ONE 8, e69835 (2013).
Prieto-Márquez, A., Fondevilla, V., Sellés, A. G., Wagner, J. R. & Galobart, À. Adynomosaurus arcanus, a new lambeosaurine dinosaur from the Late Cretaceous Ibero-Armorican Island of the European archipelago. Cretac. Res. 96, 19–37 (2019).
Longrich, N. R., Suberbiola, X. P., Pyron, R. A. & Jalil, N.-E. The first duckbill dinosaur (Hadrosauridae: Lambeosaurinae) from Africa and the role of oceanic dispersal in dinosaur biogeography. Cretac. Res. 120, 104678 (2021).
Kobayashi, Y., Takasaki, R., Kubota, K. & Fiorillo, A. R. A new basal hadrosaurid (Dinosauria: Ornithischia) from the latest Cretaceous Kita-ama Formation in Japan implies the origin of hadrosaurids. Sci. Rep. 11, 8547 (2021).
Stubbs, T. L., Benton, M. J., Elsler, A. & Prieto-Márquez, A. Morphological innovation and the evolution of hadrosaurid dinosaurs. Paleobiology 45, 347–362 (2019).
Reest, A. J. van der & Currie, P. J. Troodontids (Theropoda) from the Dinosaur Park Formation, Alberta, with a description of a unique new taxon: Implications for deinonychosaur diversity in North America. Can. J. Earth Sci. 54, 919–935 (2017).
Hartman, S. et al. A new paravian dinosaur from the Late Jurassic of North America supports a late acquisition of avian flight. PeerJ 7, e7247 (2019).
Horner, J. R., Varricchio, D. J. & Goodwin, M. B. Marine transgressions and the evolution of Cretaceous dinosaurs. Nature 358, 59–61 (1992).
O’Brien, C. L. et al. Cretaceous sea-surface temperature evolution: Constraints from TEX86 and planktonic foraminiferal oxygen isotopes. Earth Sci. Rev. 172, 224–247 (2017).
Huber, B. T., MacLeod, K. G., Watkins, D. K. & Coffin, M. F. The rise and fall of the Cretaceous Hot Greenhouse climate. Glob. Planet. Change 167, 1–23 (2018).
Mannion, P. D. et al. A temperate palaeodiversity peak in Mesozoic dinosaurs and evidence for Late Cretaceous geographical partitioning. Glob. Ecol. Biogeogr. 21, 898–908 (2012).
Forster, A., Schouten, S., Baas, M. & Damsté, J. S. S. Mid-Cretaceous (Albian–Santonian) sea surface temperature record of the tropical Atlantic Ocean. Geology 35, 919–922 (2007).
O’Connor, L. K. et al. Late Cretaceous temperature evolution of the southern high latitudes: a TEX86 perspective. Paleoceanogr. Paleoclimatol. 34, 436–454 (2019).
Linnert, C. et al. Evidence for global cooling in the Late Cretaceous. Nat. Commun. 5, 4194 (2014).
Crane, P. R. & Lidgard, S. Angiosperm diversification and paleolatitudinal gradients in Cretaceous floristic diversity. Science 246, 675–678 (1989).
Condamine, F. L., Silvestro, D., Koppelhus, E. B. & Antonelli, A. The rise of angiosperms pushed conifers to decline during global cooling. Proc. Natl Acad. Sci. USA 117, 28867–28875 (2020).
Condamine, F. L., Rolland, J. & Morlon, H. Macroevolutionary perspectives to environmental change. Ecol. Lett. 16, 72–85 (2013).
Silvestro, D., Cascales-Miñana, B., Bacon, C. D. & Antonelli, A. Revisiting the origin and diversification of vascular plants through a comprehensive Bayesian analysis of the fossil record. N. Phytol. 207, 425–436 (2015).
Prokoph, A., Shields, G. A. & Veizer, J. Compilation and time-series analysis of a marine carbonate δ18O, δ13C, 87Sr/86Sr and δ34S database through Earth history. Earth Sci. Rev. 87, 113–133 (2008).
Miller, K. G. et al. The phanerozoic record of global sea-level change. Science 310, 1293–1298 (2005).
Barrett, P. M. Paleobiology of herbivorous dinosaurs. Annu. Rev. Earth Planet. Sci. 42, 207–230 (2014).
Grady, J. M., Enquist, B. J., Dettweiler-Robinson, E., Wright, N. A. & Smith, F. A. Evidence for mesothermy in dinosaurs. Science 344, 1268–1272 (2014).
Eagle, R. A. et al. Isotopic ordering in eggshells reflects body temperatures and suggests differing thermophysiology in two Cretaceous dinosaurs. Nat. Commun. 6, 8296 (2015).
Paladino, F. V., Dodson, P., Hammond, J. K. & Spotila, J. R. Temperature-dependent sex determination in dinosaurs? Implications for population dynamics and extinction. in Paleobiology of the Dinosaurs (ed. Farlow, J. O.) vol. 238, 63–70 (Geological Society of America Special Papers, 1989).
Vavrek, M. J. & Larsson, H. C. E. Low beta diversity of Maastrichtian dinosaurs of North America. Proc. Natl Acad. Sci. USA 107, 8265–8268 (2010).
Dunne, J. A., Williams, R. J. & Martinez, N. D. Network structure and biodiversity loss in food webs: Robustness increases with connectance. Ecol. Lett. 5, 558–567 (2002).
Brodie, J. F. et al. Secondary extinctions of biodiversity. Trends Ecol. Evol. 29, 664–672 (2014).
Fraser, D. et al. Investigating biotic interactions in deep time. Trends Ecol. Evol. 36, 61–75 (2021).
Mallon, J. C. Competition structured a Late Cretaceous megaherbivorous dinosaur assemblage. Sci. Rep. 9, 15447 (2019).
Benton, M. J. Progress and competition in macroevolution. Biol. Rev. 62, 305–338 (1987).
Fricke, H. C. & Pearson, D. A. Stable isotope evidence for changes in dietary niche partitioning among hadrosaurian and ceratopsian dinosaurs of the Hell Creek Formation, North Dakota. Paleobiology 34, 534–552 (2008).
Mallon, J. C. & Anderson, J. S. Skull ecomorphology of megaherbivorous dinosaurs from the Dinosaur Park Formation (Upper Campanian) of Alberta, Canada. PLoS ONE 8, e67182 (2013).
Nordén, K. K., Stubbs, T. L., Prieto-Márquez, A. & Benton, M. J. Multifaceted disparity approach reveals dinosaur herbivory flourished before the end-Cretaceous mass extinction. Paleobiology 44, 620–637 (2018).
Lyson, T. R. & Longrich, N. R. Spatial niche partitioning in dinosaurs from the latest Cretaceous (Maastrichtian) of North America. Proc. R. Soc. B Biol. Sci. 278, 1158–1164 (2011).
Li, Z. et al. Ultramicrostructural reductions in teeth: Implications for dietary transition from non-avian dinosaurs to birds. BMC Evol. Biol. 20, 46 (2020).
Cau, A. et al. Synchrotron scanning reveals amphibious ecomorphology in a new clade of bird-like dinosaurs. Nature 552, 395–399 (2017).
Cau, A. The body plan of Halszkaraptor escuilliei (Dinosauria, Theropoda) is not a transitional form along the evolution of dromaeosaurid hypercarnivory. PeerJ 8, e8672 (2020).
Fowler, D. W., Freedman, E. A., Scannella, J. B. & Kambic, R. E. The predatory ecology of Deinonychus and the origin of flapping in birds. PLoS ONE 6, e28964 (2011).
Frederickson, J. A., Engel, M. H. & Cifelli, R. L. Ontogenetic dietary shifts in Deinonychus antirrhopus (Theropoda; Dromaeosauridae): Insights into the ecology and social behavior of raptorial dinosaurs through stable isotope analysis. Palaeogeogr. Palaeoclimatol. Palaeoecol. 552, 109780 (2020).
O’Connor, J. et al. Microraptor with ingested lizard suggests non-specialized digestive function. Curr. Biol. 29, 2423–2429 (2019).
King, J. L., Sipla, J. S., Georgi, J. A., Balanoff, A. M. & Neenan, J. M. The endocranium and trophic ecology of Velociraptor mongoliensis. J. Anat. 237, 861–869 (2020).
Owocki, K., Kremer, B., Cotte, M. & Bocherens, H. Diet preferences and climate inferred from oxygen and carbon isotopes of tooth enamel of Tarbosaurus bataar (Nemegt Formation, Upper Cretaceous, Mongolia). Palaeogeogr. Palaeoclimatol. Palaeoecol. 537, 109190 (2020).
Dalman, S. & Lucas, S. New evidence for cannibalism in tyrannosaurid dinosaurs from the Late Cretaceous of New Mexico. N. Mex. Mus. Nat. Hist. Sci. Bull. 82, 39–56 (2021).
Frederickson, J. A., Engel, M. H. & Cifelli, R. L. Niche partitioning in theropod dinosaurs: Diet and habitat preference in predators from the uppermost Cedar Mountain Formation (Utah, U.S.A.). Sci. Rep. 8, 17872 (2018).
Hassler, A. et al. Calcium isotopes offer clues on resource partitioning among Cretaceous predatory dinosaurs. Proc. R. Soc. B Biol. Sci. 285, 20180197 (2018).
Schroeder, K., Lyons, S. K. & Smith, F. A. The influence of juvenile dinosaurs on community structure and diversity. Science 371, 941–944 (2021).
Currie, P. J., Badamgarav, D., Koppelhus, E. B., Sissons, R. & Vickaryous, M. K. Hands, feet, and behaviour in Pinacosaurus (Dinosauria: Ankylosauridae). Acta Palaeontol. Polon. 56, 489–504 (2011).
Burns, M. E., Currie, P. J., Sissons, R. L. & Arbour, V. M. Juvenile specimens of Pinacosaurus grangeri Gilmore, 1933 (Ornithischia: Ankylosauria) from the Late Cretaceous of China, with comments on the specific taxonomy of Pinacosaurus. Cretac. Res. 32, 174–186 (2011).
Burns, M. E., Tumanova, T. A. & Currie, P. J. Postcrania of juvenile Pinacosaurus grangeri (Ornithischia: Ankylosauria) from the Upper Cretaceous Alagteeg Formation, Alag Teeg, Mongolia: Implications for ontogenetic allometry in ankylosaurs. J. Paleontol. 89, 168–182 (2015).
Botfalvai, G., Prondvai, E. & Ősi, A. Living alone or moving in herds? A holistic approach highlights complexity in the social lifestyle of Cretaceous ankylosaurs. Cretac. Res. 118, 104633 (2021).
Arbour, V. M. & Zanno, L. E. The evolution of tail weaponization in amniotes. Proc. R. Soc. B Biol. Sci. 285, 20172299 (2018).
Arbour, V. M. & Zanno, L. E. Tail weaponry in ankylosaurs and glyptodonts: An example of a rare but strongly convergent phenotype. Anat. Rec. 303, 988–998 (2020).
Van Valen, L. A new evolutionary law. Evol. Theory 1, 1–30 (1973).
Hagen, O., Andermann, T., Quental, T. B., Antonelli, A. & Silvestro, D. Estimating age-dependent extinction: Contrasting evidence from fossils and phylogenies. Syst. Biol. 67, 458–474 (2018).
Finnegan, S., Payne, J. L. & Wang, S. C. The Red Queen revisited: Reevaluating the age selectivity of Phanerozoic marine genus extinctions. Paleobiology 34, 318–341 (2008).
Doran, N. A., Arnold, A. J., Parker, W. C. & Huffer, F. W. Is extinction age dependent? PALAIOS 21, 571–579 (2006).
Larson, D. W., Brown, C. M. & Evans, D. C. Dental disparity and ecological stability in bird-like dinosaurs prior to the end-Cretaceous mass extinction. Curr. Biol. 26, 1325–1333 (2016).
Romano, M. Disparity versus diversity in ankylosaurid dinosaurs: Explored morphospace indicates two separate evolutive radiations. Rend. Online Soc. Geol. It. 53, 2–8 (2021).
Turner, A. H., Montanari, S. & Norell, M. A. A new dromaeosaurid from the Late Cretaceous Khulsan locality of Mongolia. Am. Mus. Novitat. 2020, 1–48 (2021).
Maryańska, T. & Osmólska, H. Pachycephalosauria, a new suborder of ornithischian dinosaurs. Palaeontol. Polon. 30, 45–102 (1974).
Sereno, P. C. National Geographic Research: Phylogeny of the bird-hipped dinosaurs (Order Ornithischia). Natl Geogr. Res. 2, 234–256 (1986). https://d3qi0qp55mx5f5.cloudfront.net/paulsereno/i/docs/86-NGRes-PhyloOrnithis_1.pdf?mtime=1591821557.
Sullivan, R. M. A taxonomic review of the Pachycephalosauridae (Dinosauria: Ornithischia). N. Mex. Mus. Nat. Hist. Sci. Bull. 35, 347–365 (2006).
Lee, M. S. Y., Cau, A., Naish, D. & Dyke, G. J. Morphological clocks in paleontology, and a mid-cretaceous origin of crown aves. Syst. Biol. 63, 442–449 (2014).
Arbour, V. M. & Evans, D. C. A new ankylosaurine dinosaur from the Judith River Formation of Montana, USA, based on an exceptional skeleton with soft tissue preservation. R. Soc. Open Sci. 4, 161086 (2017).
McDonald, A. T., Wolfe, D. G. & Dooley, A. C. Jr A new tyrannosaurid (Dinosauria: Theropoda) from the Upper Cretaceous Menefee Formation of New Mexico. PeerJ 6, e5749 (2018).
Longrich, N. R. & Field, D. J. Torosaurus is not Triceratops: Ontogeny in chasmosaurine ceratopsids as a case study in dinosaur taxonomy. PLoS ONE 7, e32623 (2012).
Larson, P. L. in Tyrannosaurid Paleobiology (eds. Parrish, J. M., Molnar, R. A., Currie, P. J. & Koppelhus, E. B.) 15–54 (Indiana University Press, 2013).
Yun, C. Evidence points out that ‘Nanotyrannus’ is a juvenile Tyrannosaurus rex. PeerJ 3, e1052 (2015).
Brusatte, S. L. et al. Dentary groove morphology does not distinguish ‘Nanotyrannus’ as a valid taxon of tyrannosauroid dinosaur. Comment on: “Distribution of the dentary groove of theropod dinosaurs: Implications for theropod phylogeny and the validity of the genus Nanotyrannus Bakker et al., 1988. Cretac. Res. 65, 232–237 (2016).
Schmerge, J. D. & Rothschild, B. M. When a groove is not a groove: Clarification of the appearance of the dentary groove in tyrannosauroid theropods and the distinction between Nanotyrannus and Tyrannosaurus. Reply to Comment on: “Distribution of the dentary groove of theropod dinosaurs: Implications for theropod phylogeny and the validity of the genus Nanotyrannus Bakker et al., 1988. Cretac. Res. 65, 238–243 (2016).
Xu, X., Zhou, Z., Sullivan, C., Wang, Y. & Ren, D. An updated review of the Middle-Late Jurassic Yanliao biota: Chronology, taphonomy, paleontology and paleoecology. Acta Geol. Sin. 90, 2229–2243 (2016).
Cau, A., Brougham, T. & Naish, D. The phylogenetic affinities of the bizarre Late Cretaceous Romanian theropod Balaur bondoc (Dinosauria, Maniraptora): Dromaeosaurid or flightless bird? PeerJ 3, e1032 (2015).
Agnolin, F. L. & Motta, M. J. Paravian phylogeny and the dinosaur-bird transition: An overview. Front. Earth Sci. 6, 252 (2019).
Pei, R. et al. Potential for powered flight neared by most close avialan relatives, but few crossed Its thresholds. Curr. Biol. 30, 4033–4046 (2020).
Foth, C. & Rauhut, O. W. M. Re-evaluation of the Haarlem Archaeopteryx and the radiation of maniraptoran theropod dinosaurs. BMC Evol. Biol. 17, 236 (2017).
Rauhut, O. W., Tischlinger, H. & Foth, C. A non-archaeopterygid avialan theropod from the Late Jurassic of southern Germany. eLife 8, e43789 (2019).
Lefèvre, U. et al. A new Jurassic theropod from China documents a transitional step in the macrostructure of feathers. Sci. Nat. 104, 74 (2017).
Shen, C. et al. A new troodontid dinosaur from the Lower Cretaceous Yixian formation of Liaoning province. China Acta Geol. Sin. 91, 763–780 (2017).
Arbour, V. M. & Currie, P. J. Euoplocephalus tutus and the diversity of ankylosaurid dinosaurs in the Late Cretaceous of Alberta, Canada, and Montana, USA. PLoS ONE 8, e62421 (2013).
Arbour, V. M. & Currie, P. J. Systematics, phylogeny and palaeobiogeography of the ankylosaurid dinosaurs. J. Syst. Palaeontol. 14, 385–444 (2016).
Arbour, V. M., Currie, P. J. & Badamgarav, D. The ankylosaurid dinosaurs of the Upper Cretaceous Baruungoyot and Nemegt formations of Mongolia. Zool. J. Linn. Soc. 172, 631–652 (2014).
Arbour, V. M. et al. A new ankylosaurid dinosaur from the Upper Cretaceous (Kirtlandian) of New Mexico with implications for ankylosaurid diversity in the Upper Cretaceous of Western North America. PLoS ONE 9, e108804 (2014).
Gradstein, F. M., Ogg, J. G., Schmitz, M. D. & Ogg, G. M. The Geologic Time Scale 2012 (Elsevier B.V., 2012).
Brown, C. M. & Henderson, D. M. A new horned dinosaur reveals convergent evolution in cranial ornamentation in Ceratopsidae. Curr. Biol. 25, 1641–1648 (2015).
Jerzykiewicz, T., Currie, P. J., Fanti, F. & Lefeld, J. Lithobiotopes of the Nemegt Gobi Basin. Can. J. Earth Sci. https://doi.org/10.1139/cjes-2020-0148 (2021).
Silvestro, D., Salamin, N. & Schnitzler, J. PyRate: A new program to estimate speciation and extinction rates from incomplete fossil data. Methods Ecol. Evol. 5, 1126–1131 (2014).
Rambaut, A. R., Drummond, A. J., Xie, D., Baele, G. & Suchard, M. A. Posterior summarization in Bayesian phylogenetics using Tracer 1.7. Syst. Biol. 67, 901–904 (2018).
Brusatte, S. L. et al. Tyrannosaur paleobiology: New research on ancient exemplar organisms. Science 329, 1481–1485 (2010).
Ryan, M. J., Chinnery-Allgeier, B. J. & Eberth, D. A. New Perspectives on Horned Dinosaurs (Indiana University Press, 2010).
Xu, X., Wang, K., Zhao, X. & Li, D. First ceratopsid dinosaur from China and its biogeographical implications. Chin. Sci. Bull. 55, 1631–1635 (2010).
Hannisdal, B. & Peters, S. E. Phanerozoic Earth system evolution and marine biodiversity. Science 334, 1121–1124 (2011).
Liow, L. H., Reitan, T. & Harnik, P. G. Ecological interactions on macroevolutionary time scales: Clams and brachiopods are more than ships that pass in the night. Ecol. Lett. 18, 1030–1039 (2015).
Erwin, D. H. Climate as a driver of evolutionary change. Curr. Biol. 19, R575–R583 (2009).
Mayhew, P. J., Bell, M. A., Benton, T. G. & McGowan, A. J. Biodiversity tracks temperature over time. Proc. Natl Acad. Sci. USA 109, 15141–15145 (2012).
Zachos, J., Pagani, M., Sloan, L., Thomas, E. & Billups, K. Trends, rythms, and aberration in global climate 65 Ma to present. Science 292, 686–693 (2001).
Zachos, J. C., Dickens, G. R. & Zeebe, R. E. An early Cenozoic perspective on greenhouse warming and carbon-cycle dynamics. Nature 451, 279–283 (2008).
Cramer, B. S., Toggweiler, J. R., Wright, J. D., Katz, M. E. & Miller, K. G. Ocean overturning since the late cretaceous: Inferences from a new benthic foraminiferal isotope compilation. Paleoceanography 24, 1–14 (2009).
Barba-Montoya, J., Reis, M., Schneider, H., Donoghue, P. C. J. & Yang, Z. Constraining uncertainty in the timescale of angiosperm evolution and the veracity of a Cretaceous Terrestrial Revolution. N. Phytol. 218, 819–834 (2018).
Zhang, M., Dai, S., Du, B., Ji, L. & Hu, S. Mid-Cretaceous hothouse climate and the expansion of early angiosperms. Acta Geol. Sin. 92, 2004–2025 (2018).
This project received funding from the Marie Curie International Outgoing Fellow under the European Union’s Seventh Framework Programme (project BIOMME, agreement No. 627684) and a PICS grant from the CNRS (project PASTA) to F.L.C.; from the NERC grant NE/ I027630/1 and European Research Council (ERC) under the European Union’s Horizon 2020 research and innovation programme (agreement No. 788203) to M.J.B.; from the NSERC grant 2017-04715 to P.J.C. The analyses benefited from the Montpellier Bioinformatics Biodiversity (MBB) platform services.
The authors declare no competing interests.
Peer review information Nature Communications thanks Peter Dodson, Jonathan Mitchell and the other, anonymous, reviewer(s) for their contribution to the peer review of this work. Peer reviewer reports are available.
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Condamine, F.L., Guinot, G., Benton, M.J. et al. Dinosaur biodiversity declined well before the asteroid impact, influenced by ecological and environmental pressures. Nat Commun 12, 3833 (2021). https://doi.org/10.1038/s41467-021-23754-0
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Short-term paleogeographic reorganizations and climate events shaped diversification of North American freshwater gastropods over deep time
Scientific Reports (2022)