As we know from modern species, nursery areas are essential shark habitats for vulnerable young. Nurseries are typically highly productive, shallow-water habitats that are characterized by the presence of juveniles and neonates. It has been suggested that in these areas, sharks can find ample food resources and protection from predators. Based on the fossil record, we know that the extinct Carcharocles megalodon was the biggest shark that ever lived. Previous proposed paleo-nursery areas for this species were based on the anecdotal presence of juvenile fossil teeth accompanied by fossil marine mammals. We now present the first definitive evidence of ancient nurseries for C. megalodon from the late Miocene of Panama, about 10 million years ago.
We collected and measured fossil shark teeth of C. megalodon, within the highly productive, shallow marine Gatun Formation from the Miocene of Panama. Surprisingly, and in contrast to other fossil accumulations, the majority of the teeth from Gatun are very small. Here we compare the tooth sizes from the Gatun with specimens from different, but analogous localities. In addition we calculate the total length of the individuals found in Gatun. These comparisons and estimates suggest that the small size of Gatun's C. megalodon is neither related to a small population of this species nor the tooth position within the jaw. Thus, the individuals from Gatun were mostly juveniles and neonates, with estimated body lengths between 2 and 10.5 meters.
We propose that the Miocene Gatun Formation represents the first documented paleo-nursery area for C. megalodon from the Neotropics, and one of the few recorded in the fossil record for an extinct selachian. We therefore show that sharks have used nursery areas at least for 10 millions of years as an adaptive strategy during their life histories.
Citation: 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(5): e10552. doi:10.1371/journal.pone.0010552
Editor: Anna Stepanova, Paleontological Institute, Russian Federation
Received: February 24, 2010; Accepted: April 18, 2010; Published: May 10, 2010
Copyright: © 2010 Pimiento et al. This is an open-access article distributed under the terms of the Creative Commons Attribution License, which permits unrestricted use, distribution, and reproduction in any medium, provided the original author and source are credited.
Funding: This project was funded by NSF EAR 0418042 (http://www.nsf.gov/funding), Sigma Xi G2009100426 (http://www.sigmaxi.org/programs/giar/index.shtml), The Florida Museum of Natural History (www.flmnh.ufl.edu), The Smithsonian Tropical Research Institute (www.stri.org), The Mitchell Hope Scholarship (http://www.southwestfloridafossilclub.com/) and the Ken Ericson Scholarship (http://www.flmnh.ufl.edu/vertpaleo/kenericsonscholarship.htm). 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.
Sharks, especially large species, are highly mobile organisms with a complex life history and wide distribution. During their lifetime they generally utilize three types of areas: adult feeding, reproduction and nurseries . In modern species, nursery areas are historically defined by the presence of gravid females and free-swimming neonates. It is also an area that can be shared by several shark species, where young sharks spend their first weeks, months or years . More recent studies have defined nursery areas as geographically discrete essential zones for shark survival  that provides them with two types of benefits: protection from predation (mainly larger sharks ) and abundant food resources. Productive, shallow-water ecosystems thus provide sharks significant protection from larger predators and/or abundant food resources, both of which are essential to survival .
The Gatun is a highly fossiliferous Neogene formation located in the Isthmus of Panama (Figure 1) with a diverse fauna of sharks –. It was located within a marine strait that connected the Pacific Ocean and the Caribbean Sea during the late Miocene (∼10 Ma) . Studies of different taxa, including the exceedingly diverse molluscan fauna, indicate that it was a shallow-water ecosystem (∼25 m depth) with higher salinity, mean annual temperature variations, seasonality and productivity relative to modern systems in this region , –. Over the past 20 years, the Gatun Formation localities have been extensively used to extract sediment for construction. During the more recent years, these extraction activities have increased substantially. Based on our observations made during the two past years of fieldwork, we predict that these outcrops will soon likely be excavated completely. Therefore it is timely and urgent to study the fossils occurring in these outcrops before they are no longer available to science.
A. Location of Panama and the Gatun Formation. The shaded box represents the general study area in northern Panama. B. Expanded geological map (from “See Below” shaded box in Fig. A). This map shows the exposures of the Gatun Formation and surrounding rock units (modified from Coates et al., 1992). The two fossil localities collected from the Gatun Formation during this study include: (1) Las Lomas and (2) Isla Payardi.
Fossil sharks were first reported from Panama in 1862 . In 1984, the first description of the elasmobranchs from the Gatun Formation was published . More recently, in 2010 the biodiversity of the fossil sharks from the Gatun has been documented from large new collections, and comprise 16 recognizable taxa. This work also included paleoecological and paleodepth analyses that supported the interpretation of the paleoecology of the Gatun Formation as shallow-water habitat in a productive environment .
Although it is not very common, the extinct Carcharocles megalodon (Agassiz 1843) is one of the species that occurs in the Gatun Formation. The taxonomic assignment of this species has been debated for nearly a century, and there are three possible interpretations: (1) Some authors place C. megalodon and other megatoothed sharks with the extant white shark (Carcharodon carcharias) in the same genus (Carcharodon) and therefore the same family (Lamnidae) –. (2) Other authors place C. megalodon and megatoothed sharks in a different genus (Carcharocles) and family (Otodontidae) –. Although a minority point of view, some workers recognize (3) megatoothed sharks as a series of chronospecies of the genus Otodus, and place all megatoothed sharks except C. megalodon in this genus. Furthermore, C. megalodon is assigned to the genus Megaselachus, based on the loss of lateral cusplets . We follow the second hypothesis; that Carcharocles megalodon and Carcharodon carcharias belong to separate genera in different families. However, both species belong to the order Lamniformes, and in the absence of living members of the Otodontidae, C. carcharias should be regarded as ecologically analogous species to C. megalodon. We base this analogy on the fact that both species share similar ecological niches with presumed similarities in body shape, feeding habits, and overall tooth and vertebral centrum morphology. Even though these species are not direct relatives, no other extant lamniform species share as many characteristics with C. megalodon as does C. carcharias.
C. megalodon is widely regarded as the largest shark to have ever lived. Based on tooth crown height (CH), this giant reached a total length (TL) of more than 16 m. One single tooth can exceed more than 168 mm of total height . The diagnostic characters of C. megalodon teeth include: large size, triangular shape, fine serrations on the cutting edges, a convex lingual face, a slightly convex to flat labial face, and a large v-shaped neck . Juvenile specimens of C. megalodon can have lateral cusplets , or not . The size and shape of the teeth vary within the jaw: anterior teeth are large and symmetrical whereas the latero-posterior teeth are asymmetrical with slanted crowns. Moving antero-posteriorly through the jaw, there is a slight initial increase in size on either side of the mid-line, followed by a progressive decrease that continues to the last tooth, e.g.  (Figure S1). Fossil teeth of C. megalodon range in age from 17 to 2 Ma (middle Miocene to Pleistocene) and have a cosmopolitan distribution , , .
Of relevance of this study, two shark paleo-nursery areas have previously been proposed: the Paleocene Williamsburg Formation of South Carolina, based on the presence of juvenile teeth of four lamnoid taxa ; and the late Oligocene Chandler Bridge Formation of South Carolina, based on the abundance of juvenile Carcharocles teeth, accompanied by small odontocete and mysticete skulls, which are assumed to be their prey species . However, neither of the collections from these two localities have been rigorously analyzed and thus the presence of paleo-nurseries remained anecdotal until the present report.
The presence of mammals as potential prey does not represent evidence of a shark nursery area. As known from modern studies of sharks, the main purpose of the nursery areas is not feeding –. Studies have shown that some shark species do not consume large quantities of food during their juvenile stages –. Even when high-productivity nursery areas provide ample food resources for juvenile sharks, some species select these habitats more for predator avoidance and not food consumption –. Furthermore, some shark species present an ontogenetic shift in feeding patterns –. For example, the lamnoid white shark (C. carcharias) feeds mostly on fishes (including other sharks) during their juvenile stage and on mammals during their adult stage –. Marine mammals are not commonly found in the Gatun Formation. On the other hand, bony fish otoliths  and other shark species  are abundant, representing a food source for the marine fauna that lived in this diverse environment.
In this study C. megalodon teeth were collected and measured from two localities within the Gatun Formation of Panama (Figure 1). Surprisingly, large teeth are uncommon with specimens recovered having CH ranging between 16 to 72 mm (Figure 2). The objective of this work is to determine if the late Miocene Gatun Formation was used as a nursery area by young C. megalodon. Accordingly, we compared the tooth sizes from the Gatun Formation with those found in older and younger formations to determine if the smaller size distribution observed is unique to the species during the late Miocene. In addition, we compared these sizes with tooth sets from individuals of different life stages to determine if the small size observed is related to age, or position within the jaw. Finally, we calculated the TL of all C. megalodon individuals from the Gatun Formation to estimate their life stage. The results obtained in this study from tooth measurement comparisons and individual total length estimates allowed us to determine the age class/size of individuals that inhabited the shallow-water habitats of the late Miocene Gatun Formation, ∼10 million years ago.
Results and Discussion
Temporal comparisons of similar faunas
In many clades represented in the fossil record, animals oftentimes show a general tendency to become larger through time, i.e., also called “Cope's Rule” –. For example, within lamnoid sharks there is a chronoclinal trend towards increasing size of species within the genus Carcharocles from Carcharocles auriculatus to Carcharocles angustidens to its larger species, Carcharocles megalodon . However, there is no evidence of such a microevolutionary trend within the single species C. megalodon through time, as we will show below.
In order to know if the small size observed in the fossil C. megalodon from the Gatun Formation is a special feature during the late Miocene in a potentially chronoclinally evolving species, we performed tooth size comparisons through time within other marine faunas that have sufficiently large numbers of specimens of C. megalodon. Given the fact that the C. megalodon from the Calvert Formation of Maryland are older (∼14 Ma) and the C. megalodon from the Bone Valley Formation of Florida are younger (∼5 Ma), comparing these populations with C. megalodon from the Gatun Formation can determine if there is a long-term, chronoclinal trend for size increase, or if C. megalodon from the Gatun Formation are unusually small. Figure 3 shows that both large and small tooth sizes are found in the faunas older and younger than the Gatun Formation, and thus there is no observed microevolutionary trend for increased size in C. megalodon over time. We therefore assert that the small size observed in the Gatun Formation is not related to microevolutionary shifts in body size. Consequently, we demonstrate stasis in body size within the species C. megalodon, which provides us important context in which to compare ancient populations from the localities described above.
Comparisons of Carcharocles megalodon tooth measurements (CH: crown height, CW: crown width), in millimeters from the Gatun Formation (late Miocene), with isolated teeth from a younger (Bone Valley, early Pliocene) and an older formation (Calvert, middle Miocene), which represent three localities from which this species is relatively abundant.
Life stage comparisons
It is known that within an individual, C. megalodon teeth vary in size within the jaw, e.g. –,  (Figure S1). It could therefore be argued that the small size observed in the Gatun Formation is related to tooth position, rather than juvenile life stage of the individuals. In order to test this, we compared tooth sizes of the Gatun Formation specimens with associated tooth sets from individuals of different life stages (juvenile and adult) from other localities. Our results indicate that most teeth from the Gatun Formation are close to the observed range of a juvenile dentition (Figure 4), regardless of tooth position within the jaw.
Comparisons of Carcharocles megalodon tooth measurements (CH: crown height, CW: crown width) from the Gatun Formation with tooth sets of: a juvenile from the Bone Valley Formation and an adult from the Yorktown Formation. Note the size difference in relation with the tooth positions: larger teeth are the most anterior (e.g. A1, A2, L1, L2) whereas smaller teeth are the most lateral (e.g. L8, L9, l7, l8, l9). For more details on tooth positions, see figure S1.
Comparing the Gatun's isolated teeth with tooth sets of individuals from different life stages helps to determine if the tooth size observed is related with tooth position. Nevertheless, in order to determine the life stage of those animals were neonates, juveniles or adults; it is necessary to establish total length estimates as well, as presented below.
Life stage and total length estimates
The tooth size comparisons made in this research suggest that the small size of C. megalodon teeth from the Gatun Formation is not related to temporal differences within a chronoclinally evolving species or to the tooth position within the jaw (as described above); but rather they belong to juvenile sharks. When only the teeth of a shark species are preserved, life (ontogenetic) stages of individuals can be predicted in two different ways: (1) studying morphological features of the teeth during juvenile stages; and (2) extrapolating total length using the relationship between body size and tooth crown height.
(1) In C. megalodon, teeth of juveniles sometimes demonstrate lateral cusplets  or not . For example, UF 237914 (a lateral tooth) exhibits lateral cusplets and is assumed to be from a juvenile. On the other hand, UF 237959 (a lower anterior tooth) and UF 237949 (an upper anterior) are both very small teeth that exhibit no lateral cusplets (Figure 2). The latter teeth are small thick, heart-shaped, and are considered to represent embryonic C. megalodon teeth (Hubbell teeth). These latter teeth retain the morphology of the species even at small sizes and do no demonstrate lateral cusplets .
(2) Gottfried et al. (1996)  made inferences about the skeletal anatomy of C. megalodon based on comparisons with ontogenetic trends in the white shark, Carcharodon carcharias. They deduced that a C. megalodon fetus could reach ∼4 m, juveniles ∼10.5 m, and adults more than 10.5 m (∼17 m). Based on crown heights (CH) and following the work of Shimada (2003) , we estimate the total lengths (TL) of C. megalodon specimens from the Gatun Formation (Table 1). Based on Gottfried et al.'s inferences, the total length estimates made in this research suggest that the C. megalodon specimens from the Gatun Formation represent mostly juveniles (21 individuals), with total lengths less than 10.5 m, while a few specimens (7 individuals) are interpreted as adults, with an estimated total lengths beyond 10.5 m (Figure 5).
Frequency of Carcharocles megalodon individuals at different life stages based on Gottfried et al. . Neonates of C. megalodon reach until 4 m; juveniles until 10.5 m, and adults more than 10.5 m.
There is some expectation to find adult individuals inside a paleo-nursery area, along with the juvenile sharks for two reasons: (1) sharks constantly produce and shed teeth , if gravid females lay their eggs or give birth in nursery areas, one would expect to find some larger teeth; and (2) while nursery areas do offer some protection from larger predators, they do not necessarily keep all large individuals out , in fact, nursery areas are productive environments where competition for food can be very high .
Concluding Remarks: Nursery area hypothesis
As described earlier, in addition to nurseries, extant sharks utilize adult feeding and reproduction areas . Based on what is known about aggregations of the analogous species, the white shark (C. carcharias), we have also considered the hypothesis that the late Miocene Gatun Formation was used as an aggregation site by C. megalodon for feeding and/or reproduction rather than as a nursery area. Following their oceanic migrations, C. carcharias individuals aggregate in the eastern Pacific (also called SOFA or Shark CafÈ) –. They seasonally return to this pelagic area that is suggested to be used for feeding/foraging and mating –. Furthermore, C. carcharias also aggregates in various coastal “hot spots” where they feed around pinniped colonies –. Nevertheless, based on the presence of neonates of C. megalodon, the generally high proportion of juvenile individuals, the estimated shallow depth of the Gatun Formation and the scarcity of large mammals, we reject the hypothesis of the Gatun as a primarily area for reproduction or feeding.
In this study we show that the abundance of small tooth size observed in C. megalodon specimens from the Gatun Formation is not related to its temporal position within a chronoclinally evolving species or tooth position within the jaw. Thus, the C. megalodon from the Gatun Formation indicates the dominant juvenile life stage of individuals present from this fossil locality (with estimated body lengths between 2 and 10.5 meters). The C. megalodon and associated marine invertebrate and vertebrate faunas from the late Miocene Gatun Formation of Panama presents the typical characteristics of a shark nursery area, i.e., a shallow, productive environment that contains juveniles and neonates (the later indicating these individuals probably were born in the Gatun area). We therefore propose the Miocene Gatun Formation, as a nursery area that offered juvenile C. megalodon protection from larger predators and ample food resources (i.e. fishes).
Given that C. megalodon was the largest shark that has ever lived, it could be argued that this species may not have represented a potential prey for other sharks and therefore nursery areas would not be needed. In this study however, we report that neonate individuals of C. megalodon from the late Miocene Gatun Formation of Panama could be as small as 2 m long. Furthermore, many other shark species in the Gatun Formation apparently were sympatric with juvenile C. megalodon, including potential predators that can reach more than 6 m of total length (e.g. the great hammerhead shark (Sphyrna mokarran) and the extinct snaggletooth shark (Hemipristis serra)) . Moreover, in spite of a juvenile dominance, adult individuals of C. megalodon (reaching until ∼17 m of TL) are also found in the Gatun Formation, representing additional potential predators. With regard to modern species, large-bodied sharks such as the tiger shark (Galeocerdo cuvier) and the great hammerhead (S. mokarran) also use nursery areas . Additionally, it has been demonstrated that the modern apex shark predator of the oceans (and the analogous species of C. megalodon in this study), the white shark, uses the Southern California Bight as a nursery ground .
In summary, this study represents the first definitive evidence of an ancient shark nursery area from the Neotropics. Sharks are a very successful group that has been common in our oceans for at least 400 million years . This research presents evidence that sharks have used nursery areas since ancient times, i.e., for at least 10 million years, and therefore extends the record of this behavior and adaptive strategy based on fossil evidence.
Materials and Methods
Carcharocles megalodon teeth are relatively rare in the Gatun Formation. Of more than 400 teeth of fossil sharks collected from the Gatun Formation between 2007 and 2009 representing 16 taxa, a total of 28 specimens (Figure 2) of C. megalodon have been collected. Fossils do not provide a record of life as complete as when studying living organisms. For that reason and also because of the rarity of this species in the area of study, we consider our sample size adequate. In addition, it is urgent to study the fossils of a formation that will soon disappear due to the increasing excavations.
The two localities studied in the Neogene marine sediments of the Gatun Formation of Panama (Figure 1), crop out in a broad area in north-central Panama and have been proposed to be late Miocene, spanning from about 12 to 8.4 Ma . The materials were collected mainly by surface prospecting by the Panama Canal Project Field Team of the Center of Tropical Paleobiology and Archaeology (CTPA) of the Smithsonian Tropical Research Institute (STRI), as well as the University of Florida (UF) scientists. Some of the specimens collected are deposited in the Florida Museum of Natural History (FLMNH) and are designated with a UF catalogue number which are available in its database: http://www.flmnh.ufl.edu/databases/VP/intro.htm. The remaining specimens are designated with a CTPA or AT number and are part of the STRI collection.
Crown height (CH) and width (CW) (Figure S2) of all specimens were measured (Table 1, S1, S2, S3 and S4) using digital calipers. In order to calculate dimensions of incomplete specimens, CW vs. CH data were plotted and a line regression was calculated (Figure S3). Measurements were then compared with isolated teeth from geologically younger and older collections and with different tooth sets from individuals of different life stages. The specimens' total lengths (TL) were calculated based on their CH.
Temporal comparisons of similar faunas
Isolated teeth from the younger Bone Valley Formation, Florida (early Pliocene, ∼5 Ma) –, from the Vertebrate Paleontology Collection at the FLMNH in Gainesville, Florida, were measured (Table S1) and compared with the Gatun teeth. Additionally, isolated teeth from the older Calvert Formation, Maryland (middle Miocene, ∼14 Ma) , from the Vertebrate Paleontology Collection at the U. S. National Museum of Natural History (NMNH), in Washington, D.C, were also measured (Table S2) and then compared with the Gatun Formation teeth.
Life stage comparisons
Tooth sizes of the Gatun isolated teeth were measured and compared with two C. megalodon associated tooth sets of different life stages from the Hubbell collection at Gainesville, FL. The adult tooth set is from the Yorktown Formation, North Carolina (early Pliocene)  (Table S3). And the juvenile tooth set is from the Bone Valley Formation, Florida (early Pliocene) – (Table S4).
Total length estimates
As described above, the extant white shark (Carcharodon carcharias), has been used as a general ecological analog to the extinct Carcharocles megalodon. Likewise, previous studies have asserted that teeth of C. carcharias can be used to estimate the total length of C. megalodon , . Based on C. carcharias tooth height and total length ratios, we have measured C. megalodon tooth CH to extrapolate its TL estimates based on the work of Shimada (2003)  on the white shark, where every tooth position in the jaw corresponds to one regression equation that calculates its body size (Table S5). We assigned a range of possible positions to the Gatun teeth and estimated the TL of every specimen by calculating it from the average among the different positions where every tooth could have belonged (TL, Table 1). We then inferred the life stage of every C. megalodon, by extrapolating it from the relationship between body size and life stage in C. carcharias following Gottfried et al. (1996) . We based our C. megalodon estimates on extrapolations from the extant C. carcharias given their similarities in body shape, feeding habits, and tooth and vertebral morphology. In addition, both species belong to the same order (Lamniformes), and in the absence of living members of the Otodontidae, C. carcharias is the most analogous species available.
Representation of a Carcharocles megalodon dentition. Tooth size and shape varies greatly within the jaw: most anterior teeth are larger and symmetrical; most lateral teeth are smaller and asymmetrical. Capital letters represent upper teeth, lowercase letters represent lower teeth. Letter A(a) is for anterior and L(l) for lateral. Adapted from Gottfried et al. (1996) .
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Tooth measurement codes and dimensions. CW represents crown width and CH represents crown height. All measurements were taken in millimeters.
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Tooth measurements line regressions. A. Known crown width (CW). Line regression calculated when is possible to measure the CW (i.e. CW in the x or independent axes) but the CH is unknown due to fossil preservation. B. Known crown height (CH). Line regression calculated when is possible to measure the CH (i.e. CH in the x or independent axes) but the CW is unknown due to fossil preservation.
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Carcharocles megalodon isolated teeth, from the Bone Valley Formation, Florida, USA.
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Carcharocles megalodon isolated teeth, from the Calvert Formation, Maryland, USA.
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Adult Carcharocles megalodon associated tooth set, from the Yorktown Formation, North Carolina, USA.
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Juvenile Carcharocles megalodon associated tooth set, from the Bone Valley Formation, Florida, USA.
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We thank C. Jaramillo for facilitating the material collected in Panama; to A. Rincon, James Wilson, Cesar Silva, Sandra Suarez, C. Montes and the Panama Canal Project Field Team in the CTPA at STRI for helping with the collection of the material; to F. Rodriguez and A. O'Dea for facilitating previous collected material (numbered AT); and to the Direccion de Recursos Minerales of Panama for collecting permits. Thanks to D. Bohaska and R. Purdy from the National Museum of Natural History for access to collections. We thank G. Morgan for beneficial suggestions about this research. We also thank to A. Hendry for reviewing earlier versions of this manuscript. We are grateful for the constructive comments made by A. Stepanova, Michael Gottfried and an anonymous reviewer, which substantially improved the original version of the manuscript. Finally thanks to J. McLaughlin for his constant support. This is University of Florida Contribution to Paleobiology number 629. Any opinions, findings, conclusions, or recommendations expressed in this paper are those of the authors and do not necessarily reflect the views of the National Science Foundation.
Conceived and designed the experiments: CP DJE BJM. Performed the experiments: CP. Analyzed the data: CP. Contributed reagents/materials/analysis tools: CP GH. Wrote the paper: CP. Intellectual support and editorial input: DJE BJM GH.
- 1. Alejo-Plata C, Gomez-Marquez JL, Ramos S, Herrera E (2007) Presence of neonates and juvenile scalloped hammerhead sharks Sphyrna lewini (Griffith & Smith, 1834) and silky sharks Carcharhinus falciformis (Muller & Henle, 1839) in the Oaxaca coast, Mexico. Rev Biol Mar Oceanog 42: 403–413.
- 2. Castro JI (1993) The shark nursery of Bulls Bay, South Carolina, with a review of the shark nurseries of the southeastern coast of the United States. Environ Biol Fish 38: 37–48.
- 3. Heupel MR, Carlson JK, Simpfendorfer CA (2007) Shark nursery areas: concepts, definition, characterization and assumptions. Mar Ecol Prog Ser 337: 287–297.
- 4. Heithaus MR (2007) Nursery areas as essential shark habitats: a theoretical perspective. American Fisheries Society Symposium 50: 3–13.
- 5. Blake SF (1862) Fossil shark teeth at Panama. The Geologist 5: 316.
- 6. Gillette DD (1984) A marine ichthyofauna from the Miocene of Panama, and the Tertiary Caribbean faunal province. J Vertebr Paleontol 4: 172–186.
- 7. Pimiento C (2010) Systematics, paleobiology, and paleoecology of late Miocene sharks (Elasmobranchii, Selachii) from Panama: integration of research and education. Gainesville: University of Florida. 131 p.
- 8. Coates AG (1996) Lithostratigraphy of the Neogene strata of the Caribbean coast from Limon, Costa Rica, to Colon, Panama. In: Collins LS, Coates AG, editors. A Paleobiotic Survey of Caribbean Faunas from the Neogene of the Isthmus of Panama. Bulletin 357. Ithaca: Paleontological Research Institute, Ithaca. pp. 17–38.
- 9. Collins LSA, Coates G, Berggren WA, Aubry MP, Zhang JJ (1996) The late Miocene Panama isthmian strait. Geology 24: 687–690.
- 10. Coates AG, Obando JA (1996) The geologic evolution of the Central American Isthmus. In: Jackson JBC, Budd AF, Coates AG, editors. Evolution and environment in tropical America. pp. 21–56. University of Chicago Press; University of Chicago Press.
- 11. Gussone N, Eisenhauer A, Tiedemann R, Haug GH, Heuser A, et al. (2004) Reconstruction of Caribbean sea surface temperature and salinity fluctuations in response to the Pliocene closure of the Central American Gateway and radiative forcing, using Δ44/40Ca, Δ18O and Mg/Ca ratios. Earth Planet Sc Lett 227: 201–214.
- 12. Haug GH, Tiedemann R, Zahn R, Ravelo AC (2001) Role of Panama uplift on oceanic freshwater balance. Geology 29: 207–210.
- 13. Teranes JL, Geary DH, Bemis BE (1996) The oxygen isotopic record of seasonality in Neogene Bivalves from the Central American Isthmus. In: Jackson JBC, Budd AF, Coates AG, editors. Evolution and environment in tropical America. pp. 105–129. University of Chicago Press; University of Chicago Press.
- 14. 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.
- 15. 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.
- 16. 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.
- 17. Jordan DS, Hannibal H (1923) Fossil sharks and rays of the Pacific Slope of North America. Bull South Calif Acad Sci 22: 27–63.
- 18. Casier E (1960) Note sur la collection des poissons paleochnes et iochnes de l'Enclave de (Congo). pp. 1–28. Annales Museum Royal Congo Belge (A.30) 1, 2.
- 19. Gluckman LS (1964) Sharks of Paleogene of stratigraphic significance. Moscow: Nauka Press. 229 p.
- 20. Cappetta H (1987) Chondrichthyes II.Mesozoic and Cenozoic Elasmobranchi. Handbook of paleoichthyology Vol. 3B. New York: Gustav Fischer Verlag. 193 p.
- 21. Nyberg KG, Ciampaglio CN, Wray GA (2006) Tracing the ancestry of the Great White Shark, Carcharodon carcharias, using morphometric analyses of fossil teeth. J Vertebr Paleontol 26: 806–814.
- 22. Ward D, Bonavia C (2001) Additions to, and a review of, the Miocene shark and ray fauna of Malta. The Central Mediterranean Naturalist 3: 131–146.
- 23. Ehret DJ, Hubbell G, MacFadden BJ (2009) Exceptional preservation of the white shark Carcharodon (Lamniformes, Lamnidae) from the early Pliocene of Peru. J Vertebr Paleontol 29: 1–13.
- 24. Zhelezko V, Kozlov V (1999) Elasmobranchii and Paleogene biostratigraphy of Transurals and Central Asia. Materials on stratigraphy palaeontology of the Urals Vol 3. Ekkaterinburg: Russian Academy of Sciences Urals Branch Uralian Regional Interdepartment Stratigraphical Comission. 324 p.
- 25. 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.
- 26. Purdy RW (1998) Chondrichthyan fishes from the Paleocene of South Carolina. T Am Philos Soc 88: 122–146.
- 27. Bush A, Holland K (2002) Food limitation in a nursery area: estimates of daily ration in juvenile scalloped hammerheads, Sphyrna lewini (Griffith and Smith, 1834) in Kane'ohe Bay, O'ahu, Hawaii. Journal Exp Mar Biol Ecol 278: 157–178.
- 28. Lowe CG (2002) Bioenergetics of free-ranging juvenile scalloped hammerhead sharks (Sphyrna lewini) in Kane'ohe Bay, O'ahu, HI. Journal Exp Mar Biol Ecol 278: 141–156.
- 29. Lowe CG, Wetherbee BM, Crow GL, Tester AL (1996) Ontogenetic dietary shifts and feeding behavior of the tiger shark, Galeocerdo cuvier, in Hawaiian waters. Environ Biol Fish 47: 203–211.
- 30. McElroy WD, Wetherbee BM, Mostello CS, Lowe CG, Crow GL, et al. (2006) Food habits and ontogenetic changes in the diet of the sandbar shark, Carcharhinus plumbeus, in Hawaii. Environ Biol Fish 76: 81–92.
- 31. Yamaguchi A, Taniuchi T (2000) Food variations and ontogenetic dietary shift of the starspotted-dogfish Mustelus manazo at five locations in Japan and Taiwan. Fisheries Sci 66: 1039–1048.
- 32. Ebert DA (2002) Ontogenetic changes in the diet of the sevengill shark (Notorynchus cepedianus). Mar Freshwater Res 53: 517–523.
- 33. Estrada JA, Rice AN, Natanson LJ, Skomal GB (2006) Use of isotopic analysis of vertebrae in reconstructing ontogenetic feeding ecology in white sharks. Ecology 87: 829–834.
- 34. Tricas TC, McCosker JE (1984) Predatory behavior of the white shark (Carcharodon carcharias), with notes on its biology. Proc Calif Acad Sci 43: 221–238.
- 35. Cliff G, Dudley SFJ, Davis B (1989) Sharks caught in the protective gill nets off natal South Africa 2. The great white shark Carcharodon carcharias Linnaeus S Afr J Mar Sci 131–144.
- 36. Aguilera O, De Aguilera DR (1996) Bathymetric distribution of Miocene and Pliocene Caribbean teleostean fishes from the coast of Panama and Costa Rica. In: Collins LS, Coates AG, editors. Paleobiotic survey of Caribbean faunas from the Neogene of the Isthmus of Panama. Ithaca: Paleontological Research Institute Ithaca. pp. 251–270.
- 37. Hone DWE, Benton MJ (2005) The evolution of large size: How does Cope's Rule work? Trends Ecol Evol 20: 4–6.
- 38. MacFadden BJ (1992) Fossil Horses: Systematics, palaeobiology and evolution of the family Equidae. New York:: Cambridge University Press. 369 p.
- 39. Shimada K (2003) The relationship between the tooth size and total body length in the white shark, Carcharodon carcharias (Lamniformes: Lamnidae). J Fossil Res 35: 28–33.
- 40. Hubbell G (1996) Using tooth structure to determine the evolutionary history of the white shark. In: Klimley A, Ainley D, editors. Great white sharks: the biology of Carcharodon carcharias. San Diego: Academic Press. pp. 9–18.
- 41. Domeier ML, Nasby-Lucas N (2008) Migration patterns of white sharks Carcharodon carcharias tagged at Guadalupe Island, Mexico, and identification of an eastern Pacific shared offshore foraging area. Mar Ecol Prog Ser 370: 221–237.
- 42. Jorgensen SJ, Reeb CA, Chapple TK, Anderson S, Perle C, et al. (2010) Philopatry and migration of Pacific white sharks. Proc R Soc Lond [Biol] 277: 679–688.
- 43. Nasby-Lucas N, Dewar H, Lam CH, Goldman KJ, Domeier ML (2009) White shark offshore habitat: a behavioral and environmental characterization of the eastern Pacific shared offshore foraging area. PLoS ONE 4(12): e8163. doi:10.1371/journal.pone.0008163.
- 44. Ainley DG, Henderson RP, Huber HR, Boekelheide RJ, Allen SG, et al. (1985) Dynamics of white shark/pinniped interactions in the Gulf of the Farallones. South Calif Adac Sci Mem 8: 109–122.
- 45. Bruce BD (1992) Preliminary observations on the biology of the white shark Carcharodon carcharias in south Australian waters. Aust J Mar Freshw Res 43: 1–11.
- 46. Ferreira CA, Ferreira TP (1996) Population dynamics of white sharks in South Africa. In: Klimley AP, Ainley DG, editors. Great white sharks: the biology of Carcharodon carcharias. San Diego: Academic Press. pp. 381–391.
- 47. Goldman KJ, Anderson SD (1999) Space utilization and swimming depth of white sharks, Carcharodon carcharias, at the South Farallon Islands, central California. Env Biol Fish 56: 351–364.
- 48. McCandless CT, Kohler NE, Pratt H Jr (2007) Shark nursery grounds of the Gulf of Mexico and the east coast waters of the United States. American Fisheries Society Symposium 50: i–xii, 1–390.
- 49. Dewar H, Domeier M, Nasby-Lucas N (2004) Insights into young of the year white shark, Carcharodon carcharias, behavior in the Southern California Bight. Environ Biol Fish 70: 133–143.
- 50. Morgan GS (1994) Miocene and Pliocene marine mammal faunas from the Bone Valley Formation of central Florida. In: Berta A, Deméré TA, editors. Contributions in marine mammal paleontology honoring Frank C. Whitmore, Jr. San Diego: Proceedings of the San Diego Society of Natural History. pp. 239–268.
- 51. Tedford RH, Albright LBA III, Barnosky D, Ferrusquía-Villafranca I, Hunt RM Jr, et al. (2004) Mammalian biochronology of the Arikareean through Hemphillian interval (late Oligocene through early Pliocene epochs). In: Woodburne MO, editor. Late Cretaceous and Cenozoic mammals of North America: biostratigraphy and geochronology. New York: Columbia University Press. 391 p.
- 52. Ward LW, Bohaska DJ (2008) Synthesis of paleontological and stratigraphic investigations at the Lee Creek Mine, Aurora, N.C. (1958–2007). In: Ray CE, Bohaska DJ, Koretsky IA, Ward LW, Barnes LG, editors. pp. 325–436. Geology and Paleontology of the Lee Creek Mine, North Carolina, IV. Virginia Museum of Natural History Special Publication 14.