DSpace Repository

Ancient Nursery Area for the Extinct Giant Shark Megalodon from the Miocene of Panama

Show simple item record

dc.contributor.author Pimiento, Catalina en
dc.contributor.author Ehret, Dana J. en
dc.contributor.author MacFadden, Bruce J. en
dc.contributor.author Hubbell, Gordon en
dc.date.accessioned 2010-07-21T13:40:37Z
dc.date.available 2010-07-21T13:40:37Z
dc.date.issued 2010
dc.identifier.citation Pimiento, Catalina, Ehret, Dana J., MacFadden, Bruce J., and Hubbell, Gordon. 2010. "<a href="https://repository.si.edu/handle/10088/9851">Ancient Nursery Area for the Extinct Giant Shark Megalodon from the Miocene of Panama</a>." <em>PLoS One</em>, 5, (5) e10552. <a href="https://doi.org/10.1371/journal.pone.0010552">https://doi.org/10.1371/journal.pone.0010552</a>. en
dc.identifier.issn 1932-6203
dc.identifier.uri http://hdl.handle.net/10088/9851
dc.description.abstract Background <br/>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 <I>Carcharocles megalodon</I> 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 <I>C. megalodon</I> from the late Miocene of Panama, about 10 million years ago. Methodology/Principal Findings <br/>We collected and measured fossil shark teeth of <I>C. megalodon</I>, 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&#39;s <I>C. megalodon</I> 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. Conclusions/Significance <br/>We propose that the Miocene Gatun Formation represents the first documented paleo-nursery area for <I>C. megalodon</I> 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. en
dc.relation.ispartof PLoS One en
dc.title Ancient Nursery Area for the Extinct Giant Shark Megalodon from the Miocene of Panama en
dc.type Journal Article en
dc.identifier.srbnumber 90656
dc.identifier.doi 10.1371/journal.pone.0010552
rft.jtitle PLoS One
rft.volume 5
rft.issue 5
rft.spage e10552
dc.description.SIUnit STRI en
dc.description.SIUnit Center for Tropical Palaeoecology and Archaeology en
dc.citation.spage e10552


Files in this item

This item appears in the following Collection(s)

Show simple item record

Search DSpace


Browse

My Account