Carcharocles megalodon (“Megalodon”) is the largest shark that ever lived. Based on its distribution, dental morphology, and associated fauna, it has been suggested that this species was a cosmopolitan apex predator that fed on marine mammals from the middle Miocene to the Pliocene (15.9–2.6 Ma). Prevailing theory suggests that the extinction of apex predators affects ecosystem dynamics. Accordingly, knowing the time of extinction of C. megalodon is a fundamental step towards understanding the effects of such an event in ancient communities. However, the time of extinction of this important species has never been quantitatively assessed. Here, we synthesize the most recent records of C. megalodon from the literature and scientific collections and infer the date of its extinction by making a novel use of the Optimal Linear Estimation (OLE) model. Our results suggest that C. megalodon went extinct around 2.6 Ma. Furthermore, when contrasting our results with known ecological and macroevolutionary trends in marine mammals, it became evident that the modern composition and function of modern gigantic filter-feeding whales was established after the extinction of C. megalodon. Consequently, the study of the time of extinction of C. megalodon provides the basis to improve our understanding of the responses of marine species to the removal of apex predators, presenting a deep-time perspective for the conservation of modern ecosystems.
Citation: Pimiento C, Clements CF (2014) When Did Carcharocles megalodon Become Extinct? A New Analysis of the Fossil Record. PLoS ONE 9(10): e111086. https://doi.org/10.1371/journal.pone.0111086
Editor: Brian Lee Beatty, New York Institute of Technology College of Osteopathic Medicine, United States of America
Received: July 29, 2014; Accepted: September 29, 2014; Published: October 22, 2014
Copyright: © 2014 Pimiento, Clements. This is an open-access article distributed under the terms of the Creative Commons Attribution License, which permits unrestricted use, distribution, and reproduction in any medium, provided the original author and source are credited.
Data Availability: The authors confirm that all data underlying the findings are fully available without restriction. All relevant data are within the paper and its Supporting Information files and are also available in the Paleobiology Database (http://paleobiodb.org). There, the data can be found when doing a “Full Search” of “Fossil collection records” using the species name Carcharocles megalodon under “Taxon Name”, and restricting the search to Pliocene to Holocene under “Time interval”.
Funding: This project was funded by the National Science Foundation NSF EAR 0418042, PIRE 0966884 (http://www.nsf.gov/funding). The funders had no role in study design, data collection and analysis, decision to publish, or preparation of the manuscript.
Competing interests: The authors have declared that no competing interests exist.
Carcharocles megalodon (“Megalodon”) was the largest shark that ever lived . Based on its dentition, distribution and associated fauna, it has been suggested that this species could reach up to 18 m of total length, was a cosmopolitan apex predator and fed on cetaceans –. Its gigantic size and abundant fossil record has made this shark a charismatic example of extinct marine megafauna. However, despite its popularity and widespread fossil record, remarkably little is known about its extinction.
It has been widely stated in the literature that the extinction of apex predators can trigger cascading effects through entire food webs and impact ecosystem composition and function –. Concurrently, it has been demonstrated that the elimination of large sharks produces broad marine ecosystem degradation . In modern marine systems, apex predators, especially large sharks, are significantly declining throughout the global oceans –. The study of the extinction of apex predatory sharks is therefore of significant interest.
A fundamental step towards understanding the effects of an extinction event is to know when it occurred. However, identifying the exact time of extinction of a species is notoriously difficult because the fossil record is inherently incomplete. Hence, the absence of records of a species does not necessarily mean that it is extinct, but could instead reflect preservation bias, spatially heterogeneous populations, sampling effort, or as yet uncovered fossil remains –. Such issues imply that the last recorded occurrence of a species, or “Last Appearance Date” (LAD) as a proxy for time of extinction provides an inherently biased estimate .
In order to identify the time of extinction of a species, multiple methods based on the temporal distribution of the most recent sighting events (or analogously the fossil record), have been proposed (see  for a review). Many of these remain poorly tested; however, the Optimal Linear Estimation (OLE) model  has been shown to provide accurate estimates of when a species can be considered to have become extinct .
Given that C. megalodon has an abundant fossil record, cosmopolitan distribution and high trophic level, its extinction is an ideal case study to better understand the ecological and macroevolutionary responses of marine species to top-down control release. It is generally reported that fossils of this species range from the middle Miocene (15.9–11.6 Ma) to the Pliocene (5.3–2.6 Ma), with some unconfirmed reports (i.e. considered to be unreliable, see Supplementary Information) from the Pleistocene (2.6–0.01 Ma) –. However, the time of extinction of C. megalodon has never been quantitatively assessed before.
Here, we synthesize the most recent records of C. megalodon from the literature and scientific collections, and probabilistically infer the time by which it became extinct by using the OLE model. Because OLE has only been previously used to tackle the problem of inferring the time of extinction of modern species , in this study we extend its use to the analogous issue of inferring extinction events in deep time (for a more detailed explanation of the reasons why we used this method, see the Materials and Methods section). Based on our estimated time of extinction and known ecological and macroevolutionary trends in cetaceans, we further outline the possible effects of this event, providing the basis for better understanding of the responses of marine species to the removal of apex predators.
Based on the known age range of Carcharocles megalodon, we considered any post-Miocene occurrence as part of the most recent records of the species, and treated them as historic sightings to be used in the OLE calculation. Accordingly, we identified a total of 53 most recent records, which are made available in the Paleobiology Database (PaleoBioDB, http://paleobiodb.org). However, we only included in our analysis a subset of data consisting of the 42 records deemed to be reliable (Table S1).
The age of the fossils is not absolute, but instead falls within a range, with an upper and lower time estimate. To account for this unbiased uncertainty, we re-sampled the fossil data 10,000 times, bootstrapping the timing of each record from a uniform distribution between its upper and lower age. Hence, the results presented will to some extent be sensitive to the uniform distribution used in this analysis. Nevertheless, given that the actual age of the fossils is equally likely to have occurred anywhere within their age span, the use of this distribution is justified.
Because OLE infers the time by which a species can be considered extinct from the temporal distribution of the most recent sighting events , we regarded the time of the extinction event to most likely have occurred between the oldest inferred date of extinction (the first point in time at which the species can be considered as extinct), and the modal value (the most frequently inferred time of extinction). We use the modal value, as opposed to the mean, as it gives a more accurate reflection of the skewed distribution of inferred dates of extinction.
Results from applying OLE to our set of most recent records show that the modal inferred time of extinction is 2.6 Ma. This suggests that C. megalodon was unlikely to have survived beyond this time, with extinction time thus likely to have occurred between 3.5 Ma (oldest inferred extinction date), and this modal value (Figure 1). Approximately 50% of the simulations inferred the extinction event to have occurred before 2.6 Ma (modal value), with the remaining 50% of simulations being roughly uniformly distributed between 2.6 Ma and 0.1 Ma (Figure 1). In a very small proportion of simulations (1.5%), the inferred date of extinction fell after 0.1 Ma. In six simulations (0.06%) the inferred date of extinction fell after the present day (and thus the species could not be considered as extinct). However, because in the vast majority of the 10,000 simulations (>99.9%) the extinction time was inferred to have occurred before the present day, we reject the null hypothesis (that the species is extant) and the popular claims of present day survival of C. megalodon.
The orange area shows the distribution of inferred dates of extinction through time, whereas the green line shows the cumulative frequency of inferred dates of extinction. The modal peak represents the point in time by which the species was most likely to have gone extinct (2.6 Ma). Approximately 50% of simulations fell before the modal peak of inferred dates of extinction (2.6 Ma), whereas the remaining 50% are roughly evenly distributed between the mode and the present day. The two vertical dashed lines indicate the most recent and oldest inferred dates of extinction (160,000 years in the future and 3.5 Ma respectively). The horizontal bars represent the time range of each fossil occurrence. The blue bars are the occurrences used in OLE. The grey bar represents the occurrences that failed the age evaluation process and were not used in the analysis.
Our analysis suggests that the extinction of Carcharocles megalodon most likely occurred around Pliocene–Pleistocene boundary (∼2.6 Ma, modal value). Interestingly, subsequent to this time and throughout the Pleistocene, baleen whales (Cetacea, Mysticeti) reached modern gigantic sizes –. This mysticete composition contrasts with assemblages that were contemporaneous with C. megalodon, and that included mostly small-bodied species . Because body size correlates with ecological functions, it has been further proposed that the faunal turnover observed in cetaceans during the Pliocene-Pleistocene boundary resulted in additional niches occupied by baleen whales , –.
Fossils of mysticetes are frequently found along with C. megalodon teeth. This has led to the hypothesis that they interacted in ancient marine communities [e.g. 5]. Whether or not C. megalodon preyed upon mysticetes needs further investigation. However, based on the inferred time of extinction of C. megalodon and the known ecological and macroevolutionary trends of cetaceans, we propose that the modern composition and function of gigantic filter-feeding whales established after the extinction of C. megalodon.
The controlling factors within ecosystems are not limited to top-down processes. Bottom-up effects are also important drivers in marine ecosystem dynamics [e.g. 22] and should be taken into consideration when studying the ecological and macroevolutionary trends of marine organisms. Of relevance to this work, diatom diversity and temperature changes (indicated by oxygen stable isotopes) have been associated with the changes in diversity of marine mammals throughout the Cenozoic . However, it is not clear if these bottom-up processes drove the evolution of modern gigantic sizes in filter-feeding whales. Future work contrasting top-down and bottom-up processes with mysticetes body size trends are needed to discern the drivers of the evolution of gigantism in cetaceans.
Even though ecosystems are not driven entirely by only one type of control, the study of the extinction of apex predators has great potential to advance the understanding of the responses of marine species to top-down control release. Despite the limitations and uncertainties of the fossil record, the study of the time of extinction of C. megalodon provides a baseline to understand the establishment of the modern structure and function of gigantic filter-feeding whales. Furthermore, the methods used here could be applied to quantitatively assess the time of extinction of other fossil organisms, ultimately helping elucidate the causes and effects of extinction events.
Materials and Methods
Based on the known fossil record of Carcharocles megalodon, we considered any post-Miocene occurrence as part of the most recent records of the species. Accordingly, we gathered all known post-Miocene records from the literature and scientific collections. First, we searched for C. megalodon occurrences in the PaleoBioDB using the following parameter: Species name = Carcharocles megalodon. The PaleoBioDB includes all known synonyms (e.g. Carcharodon megalodon) in the search. There, each data record represents a fossil collection. A collection is any set of fossils whose exact geographic and stratigraphic position and date of collection cannot be distinguished, regardless of when they were described, and by whom. With relevance to this study, a data record or collection in the PaleoBioDB is treated as an occurrence (i.e. data record = collection = occurrence) and each of them are linked to one or more supporting references. Second, we searched for additional C. megalodon reports in ISI Web of Science (http://webofknowledge.com) GeoRef (http://geoscienceworld.org), Shark-References (http://shark-references.com) and Google Scholar (http://scholar.google.com) using the search terms: Megalodon OR Carcharodon AND megalodon OR Carcharocles AND megalodon.
With the data collected, we created a comprehensive and updated dataset of the most recent records of C. megalodon. These include 15 pre-existing PaleoBioDB records and 38 new records, for a total of 53 post-Miocene records. They accessible in the PaleoBioDB, and can be found when doing a “Full Search” of “Fossil collection records” using the species name Carcharocles megalodon under “Taxon Name”, and restricting the search to Pliocene to Holocene under “Time interval”. These records are part of the ongoing PaleoBioDB Data Archive # 20 (http://goo.gl/PpIh0G) and are also presented in the Supporting Information.
To determine which of these records to include in our analyses, we performed a standardized evaluation as follows: for each reference reporting a post-Miocene occurrence of C. megalodon, we assessed if the age of the record was clearly stated in the text. In addition, we studied a number of supplementary references that further documented or refined the age of the localities from which some of the specimens were recovered. Finally, we visited the most relevant museum collections housing the specimens referenced in the literature. There we analyzed their morphology to assess for signs of re-deposition, examined their labels, and explored the collection databases to verify the age assignments. Whenever a reference did not meet the requirements of our evaluation process, we did not include that record in our analysis (Table S2). Additional information, including all records and their evaluations can be found in the Supporting Information section (Text S1). Furthermore, more detailed information and supporting references can be accessed when clicking on the PaleoBioDB# of each record.
As a result of our age evaluation process (Text S1), we selected the records deemed to be reliable (Table S1) and treated them as historic sightings to apply the OLE model. We employed this method, rather than other methods that have previously been used to infer extinction from the fossil record – because of two main reasons: (1) OLE has been thoroughly tested and shown to produce accurate estimates of the date of extinction of a species, and to outperform many similar methods –, . (2) The problem of inferring the time of extinction of a species from the fossil record is mathematically analogous to inferring the extinction of modern species from sighting record [e.g. 14], –.
OLE infers the time by which a species can be considered as extinct from the temporal distribution of the most recent sighting events . This method assumes that, regardless of the distribution of the complete sighting record, the most recent k sighting events have the form of a Weibull extreme value distribution, and infers the shape parameter, and thus the timing of extinction, from the joint distribution of these k sightings . In effect, the method uses the spacing between recorded sighting events to infer the time at which, probabilistically, no more sightings will occur (the species can be considered extinct).
From Roberts and Solow , the Optimal Linear Estimation takes k sighting events and estimates , the time at which the extinction can be inferred, using the form:Where the weight vector w, length k, is given by:
Note that in Solow  there is an error in the final equation, but presented above is the correct version.
There has been some debate as to what should be considered the k most recent sighting events –, however recent work has shown that increasing the number of sighting events used in the calculation provides increasing accuracy of inferred dates of extinction . Because of this, we use the most recent sighting events as presented in the Supporting information.
As in Clements et al. , we disregarded the confidence intervals produced by the technique as they have been shown to be very wide (Figure S1) and hence, concentrated on the distribution of the inferred extinction dates. Therefore, we regarded the modal value of the 10,000 estimates as the time by which C. megalodon is most likely to have gone extinct, with the exact date to have occurred between the mode and the oldest estimate. All simulations were made using the R statistical software  and the code is made available in the Supporting Information section (Files S1–S2).
Distribution of inferred extinction date (red line), as well as upper (blue) and lower (green) 95% confidence intervals through time. The modal peaks of the upper and lower 95% confidence intervals fall close to the modal peak of the inferred date of extinction; however, the tail of the upper 95% confidence interval extends far beyond the present day, with the latest estimate falling 2.6 million years in future.
Code to calculate the distribution of inferred dates of extinction of Carcharocles megalodon using the Optimal Linear Estimation (OLE) model.
Data set of the Post-Miocene occurrences of Carcharocles megalodon used in the analysis.
Post-Miocene records of Carcharocles megalodon included in the Optimal Linear Estimation (OLE) model (click on the PaleoBioDB# for more details).
Post-Miocene records of Carcharocles megalodon excluded from Optimal Linear Estimation (OLE) model (click on the PaleoBioDB# for more details).
Age evaluation of Carcharocles megalodon post-Miocene records (click on the PaleoBioDB# for more details).
CP thanks B. MacFadden for his constant encouragement and feedback. We would like to thank C. Jaramillo, J. Velez-Juarbe and J. Griffin for commenting on earlier versions of this manuscript; M. Uhen for support with the PaleoBioDB; A. Hendy for support with the NPC Database; R. Boessenecker and G. Morgan for insight regarding the data from California and Florida respectively; and M. Balk for assisting in visiting collections. We thank the Florida Museum of Natural History, the British Museum of Natural History, the National Museum of Natural Histroy, the Natural History Museum of Los Angeles County, the Museo Nacional de Historia Natural de Chile, the Muséum national d'Histoire naturelle (special thanks to Gäel Clément), the University of California Museum of Paleontology, and the San Diego Natural History Museum for allowing us accessing their collections and databases. Finally, we are grateful for the reviews made by N. D. Pyenson and D. Roberts, which substantially improved the original version of the manuscript. This is University of Florida Contribution to Paleobiology number 672 and Paleobiology Database publication number 210.
Analyzed the data: CC. Wrote the paper: CP. Collected and processed the data: CP. Preparation of the final manuscript: CP CC.
- 1. Gottfried MD, Compagno LJV, Bowman SC (1996) Size and skeletal anatomy of the giant megatooth shark Carcharodon megalodon. In: Klimley AP, Ainley DG, editors. Great white sharks: the biology of Carcharodon carcharias. San Diego: Academic Press. pp. 55–89.
- 2. Pimiento C, Ehret DJ, MacFadden BJ, Hubbell G (2010) Ancient nursery area for the extinct giant shark Megalodon from the Miocene of Panama. Plos One 5: e10552
- 3. Pimiento C, González-Barba G, Ehret DJ, Hendy AJW, MacFadden BJ, et al. (2013) Sharks and Rays (Chondrichthyes, Elasmobranchii) from the Late Miocene Gatun Formation of Panama. Journal of Paleontology 87: 755–774 doi:http://dx.doi.org/10.1666/12-117.
- 4. Applegate SP, Espinosa-Arrubarrena L (1996) The fossil history of Carcharodon and its possible ancestor, Cretolamna: a study in tooth identification. In: Klimley AP, Ainley DG, editors. Great white sharks: the biology of Carcharodon carcharias. San Diego: Academic Press. pp. 19–36.
- 5. Purdy R (1996) Paleoecology of fossil white sharks. In: Klimley AP, Ainley DG, editors. Great white sharks: the biology of Carcharodon carcharias. San Diego: Academic Press. pp. 67–78.
- 6. Purdy RW, Schneider VP, Applegate SP, McLellan JH, Meyer RL, et al. (2001) The Neogene sharks, rays, and bony fishes from Lee Creek Mine, Aurora, North Carolina. Smithsonian Contributions to Paleobiology 90: 71–202.
- 7. Cappetta H (2012) Handbook of paleoichthyology. Volume 3E. Chondrichthyes. Mesozoic and Cenozoic Elasmobranchii: teeth. Stuttgart; New York: Gustav Fisher Verlag. 512 p.
- 8. Terborgh J, Holt RD, Estes JA (2010) Trophic cascades: predators, prey, and the changing dynamics of nature. Washington, D.C.: Island Press. 465 p.
- 9. Estes JA, Terborgh J, Brashares JS, Power ME, Berger J, et al. (2011) Trophic downgrading of planet Earth. Science 333: 301–306
- 10. Myers RA, Baum JK, Shepherd TD, Powers SP, Peterson CH (2007) Cascading Effects of the Loss of Apex Predatory Sharks from a Coastal Ocean. Science 315: 1846–1850
- 11. Myers RA, Worm B (2003) Rapid worldwide depletion of predatory fish communities. Nature 423: 280–283
- 12. Dulvy NK, Fowler SL, Musick JA, Cavanagh RD, Kyne PM, et al. (2014) Extinction risk and conservation of the world's sharks and rays. Elife 3: e00590
- 13. Roberts DL, Solow AR (2003) Flightless birds – When did the dodo become extinct? Nature 426: 245–245
- 14. Rivadeneira MM, Hunt G, Roy K (2009) The use of sighting records to infer species extinctions: an evaluation of different methods. Ecology 90: 1291–1300
- 15. Clements CF, Worsfold NT, Warren PH, Collen B, Clark N, et al. (2013) Experimentally testing the accuracy of an extinction estimator: Solow's optimal linear estimation model. J. Anim. Ecol. 82: 345–354
- 16. Steadman DW, Martin PS, MacPhee RDE, Jull AJT, McDonald HG, et al. (2005) Asynchronous extinction of late Quaternary sloths on continents and islands. PNAS 102: 11763–11768
- 17. Boessenecker RW (2013) Pleistocene survival of an archaic dwarf baleen whale (Mysticeti: Cetotheriidae). Naturwissenschaften 100: 365–371
- 18. Pyenson ND, Sponberg SN (2011) Reconstructing body size in extinct crown cetacea (Neoceti) using allometry, phylogenetic methods and tests from the fossil record. J. Mamm. Evol. 18: 269–288
- 19. Lambert O, Bianucci G, Post K, de Muizon C, Salas-Gismondi R, et al. (2010) The giant bite of a new raptorial sperm whale from the Miocene epoch of Peru. Nature 466. doi:10.1038/nature09067
- 20. El Adli JJ, Demere TA, Boessenecker RW (2014) Herpetocetus morrowi (Cetacea: Mysticeti), a new species of diminutive baleen whale from the Upper Pliocene (Piacenzian) of California, USA, with observations on the evolution and relationships of the Cetotheriidae. Zool. J. Linn. Soc. 170: 400–466
- 21. Bouetel V (2005) Phylogenetic implications of skull structure and feeding behavior in balaenopterids (Cetacea, Mysticeti). J. Mamm 86: 139–146
- 22. Micheli F (1999) Eutrophication, fisheries, and consumer-resource dynamics in marine pelagic ecosystems. Science 285: 1396–1398
- 23. Marx FG, Uhen MD (2010) Climate, critters, and cetaceans: Cenozoic drivers of the evolution of modern whales. Science 327: 993–996
- 24. Marshall CR (1997) Confidence intervals on stratigraphic ranges with nonrandom distributions of fossil horizons. Paleobiology 23: 165–173.
- 25. Turney CSM, Flannery TF, Roberts RG, Reid C, Fifield LK, et al. (2008) Late-surviving megafauna in Tasmania, Australia, implicate human involvement in their extinction. PNAS 105: 12150–12153
- 26. Collen B, Purvis A, Mace GM (2010) When is a species really extinct? Testing extinction inference from a sighting record to inform conservation assessment. Divers. Distrib. 16: 755–764
- 27. Solow AR, Roberts DL, Robbirt KM (2006) On the Pleistocene extinctions of Alaskan mammoths and horses. PNAS 103: 7351–7353
- 28. Solow AR, Roberts DL, Robbirt KM (2006) On the Pleistocene extinctions of Alaskan mammoths and horses. PNAS 103: 7351–7353
- 29. Robson DS, Whitlock JH (1964) Estimation of a truncation point. Biometrika 31(1/2): 33–39
- 30. Strauss D, Sadler PM (1989) Classical confidence intervals and Bayesian probability estimates for ends of local taxon ranges. Mathematical Geology 21: 411–427
- 31. Clements CF, Collen B, Blackburn TM, Petchey OL (2014) Effects of recent environmental change on accuracy of inferences of extinction status. Conservation Biology 28: 971–981
- 32. Solow AR (2005) Inferring extinction from a sighting record. Mathematical Biosciences 195(1): 47–55
- 33. R Development Core Team (2012) R: A language and environment for statistical computing. Vienna, Austria: R foundation for statistical computing.