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Megalodon Size vs Tooth Size
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Fossil Great White Shark Gallery

Megalodon Collecting Location: PCS Mine, Aurora, NC

Megalodon Collecting Location: Calvert CLiffs, MD

Parts of Sharks that Fossilize

Shark Evolution

Fossil Shark Gallery

Squalodon Gallery - Facts and Information
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Reconstructed Megalodon Jaw, complete with fossil teeth. Image taken by Edenpictures.
CARCHAROCLES (Jordan & Hannibal, 1923)
The Megatooth Sharks
Megalodon Shark Facts and Information
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Origins of the Megalodon shark - Megalodon History and Evolution
Megalodon Tooth Size vs Great White Tooth vs T-Rex Tooth.
This is a reconstructed megalodon skeleton from the Calvert Marine Museum, Solomons, Maryland.
The image was taken by Dr. Alton C. Dooley.
4 1/16" Fossil Megalodon Shark Tooth from South Carolina
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With teeth that could reach over 7 inches, and a body more massive than a T-Rex,
Megatooth sharks, particularly Carcharocles Megalodon, are undoubtedly the most infamous of all prehistoric sharks. This
shark could eat Jaws in one bite!
By now, most paleontologists believe the Megatooth shark lineage dates back to the giant mackerel shark of the
Paleocene, Otodus obliquus. Otodus was the top predator of the Paleocene oceans. Although Otodus became extinct
somewhere in the Eocene, Otodus was not a dead-end link. Throughout the Eocene Otodus teeth became more and more
serrated. The Eocene Tologaysor (say that 3 times in a row) formation in Kazakhstan shows this transition nicely.
Each zone of the formation has Otodus teeth that are slightly more serrated over geologic time until they start looking
like an early Carcharocles tooth.
Once the Otodus teeth became mostly serrated, paleontologists renamed the serrated Otodus genus to the Carcharocles
genus, and thus the Carcharocles genus arose. Where the genus transition occurs depends on which paleontologist you
ask. For instance, one transitional form, O. aksuaticus is called C. askuaticus by some; others regard C. auriculatus
to be O. auriculatus, and so forth. Regardless of which transitional form is officially called a Carcharocles is a
moot point. The point is that it is clear the Megatooth shark lineage (Carcharocles) was born from the Otodus lineage.
Notice, nothing was said about the Great White Shark, Carcharodon Carcharias. That's because the Megalodon is NOT related to the
Great White Shark. Their evolutionary lines are very different. To learn about Great White shark origins and evolution,
click here to go to the Great White Shark Gallery page.
Over time the Megatooth shark went through slight morphological changes. The teeth became more regularly serrated,
the Otodus cusps got smaller, the crown got broader, and the overall size increased. Paleontologists assigned each
slight tooth change of the Megatooth shark to a new Carcharocles species. The Megatooth shark reached its high mark
as C. megalodon, a shark of monstrous proportions. The megalodon shark became extinct during the Pliocene and left no next
of kin; the megalodon became too large and too specialized for its own good. It is a dead-end link on the tree of life.
A very rough chronology of Megatooth species, leading to the megalodon is shown on the following table:
| Rough Time Period | Shark Name |
| Paleocene | O. obliquus |
| Early Eocene | O. mugodzharicus |
| Early Eocene | C. aksuaticus |
| Middle Eocene | C. auriculatus |
| Late Eocene/Oligocene | C. angustidens |
| Late Oligocene/Miocene | C. subauriculatus |
| Miocene/Pliocene | C. megalodon |
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It's important to note that each species is the Megatooth shark, with a slight change in tooth form over different
periods of time. As a result, there are many teeth that are a cross between two species. For example,
in the early Miocene, C. subauriculatus have large cusps, where by late Miocene the cusps are very small.
Some paleontologists may further subdivide the many C. species, but it's important to remember all of the species are
the same shark evolving over time. So don't worry if you find a tooth with very small cusps, and can't tell if it's a juvenile megalodon or
a subauriculatus; it's a Megatooth shark, leave it at that!
For more information,
click here to read a great article by Lutz Andres about megalodon evolution.
Also, Elasmo.com has
a nice section explaining the carcharocles lineage in much greater detail than presented here.
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Size of the Megalodon, Behavior, & Extinction
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The megatooth shark was clearly a top predator of its time. So, how big did a megalodon get? Megalodon shark teeth reached sizes over 7 inches. With that said, no one is sure what
the body of the shark looked like. Therefore it is difficult to say how big the megalodon shark could get.
Years ago, lengths of 100 feet were speculated. Today, this length has been
vastly shortened. Using tooth and jaw reconstructions, paleontologists have calculated possible size estimates. Some estimates give a megalodon a maximum length
of around lengths around 54 feet (16.5 m), while other estimates are a bit lower, around 43 feet (13 m). The true size may lie somewhere in between.
Either way, it was an impressive animal!
(Click here to go to the megalodon tooth size vs body size chart).
Here are some size comparisons of a megalodon shark:
A megalodon was probaby around three times larger than a Great White Shark, which a length of 20+ feet is rare.
A megalodon was, on average, probably slightly larger than a Whale Shark, which can reach lengths of slightly over 41 ft.
A megalodon, however, was probably about half the size of a Blue Whale, which can reach lengths of around 94 ft.
If you have a
fossil megalodon tooth in your collection, click here to get a rough estimate
of the size of the megalodon shark your megalodon tooth came from.
Evidence suggests the obvious; this prehistoric shark ate whales for breakfast! Many fossil whale bones of the Miocene and
Pliocene show bite marks from megalodon teeth. An example of megalodon predation evidence is shown in the image below.
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C. Megalodon vs other animals - Megalodon size comparison to other animals.
Click on the image for the full sized version.
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The above image shows a "normal" intact fossil whale vertebra
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This image shows a whale vertebra that has been bitten in half by a C. megalodon shark. Notice the large gouge marks where it
has been bitten in half. The quality of this vertebra indicates it was probably swallowed.
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How did the megalodon shark become extinct?
Being the biggest predator of the time has its disadvantages. History shows the big top predators are usually the
first to go during times of extreme environmental change. By the end of the Pliocene, the Isthmus of Panama closed,
which changed global ocean currents. Whales began to migrate into arctic regions, cold places where megalodons could
not go. Also during this time period, Orcas, the Killer Whales, appeared on the scene. These large marine mammals that
hunted in packs competed with the megalodons. If there are two top predators vying for the same food supply, one is
going to lose, and we all know it wasn't the Orcas. It appears that a number of these factors contributed to the demise
of the Megatooth shark. Millions of years of evolution had made the megatooth shark too large and too specialized to
adapt to its changing environment.
Many people think a megalodon would also compete with Great White sharks in the Pliocene. This isn't the case. Due
to the distinct size differences, Great Whites would have hunted smaller prey; i.e. Seals. Seals would have only
whetted a megalodon's appetite. Megalodons would have had to prey on larger food; i.e Whales. Therefore, the megalodons
and Great Whites would not have competed with each other.
If you want to read more about Great Whites and their own origins, go to the
Great White Shark Gallery
on this page.
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Where to Find Megalodon Teeth
Megalodons are sharks, which mean they are made of cartilage. Cartilage is much softer than bone. Because of this, most of the megalodon will not fossilize.
On some occasions, vertebra will fossilize, and occasionally fragments of cartilage. However, since shark teeth are made of dentin, a very hard substance, megalodon
teeth readily fossilize, and are common as fossils in many fossil bearing Miocene and Pliocene formations worldwide. Below are some notable locations where megalodon teeth are found.
Two famous global places for megalodon teeth are:
Peru and Chile:The Pisco Formation contains very large and beautiful megalodon teeth. They are found on land in the desert regions, with many other shark and whale fossils.
New Caledonia:Megalodon teeth have been dredged from the deep slopes of a fringing reef around New Caledonia. These teeth have eroded out of their Miocene formation, and are
heavily worn. These South Pacific Megalodon teeth can no longer be dredged. However, this location is mentioned here, because
these New Caledonian teeth continue to stir up controversy from time to time. Manganese dioxide dating of the teeth in the late 50's indicated an age of 11,000 to 24,000 years. Which means
megalodon must have survived extinction. However, this type of manganese dioxide dating is now considered obsolete and invalid. The teeth from this area are clearly Miocene in age.
North America Megalodon Shark Tooth Fossil Hunting Locations
South Carolina has a few formations which contain Megalodon teeth. The main formation is the Hawthorne Formation. A while back, one could surface hunt
in areas being developed that exposed this formation. The big development boom is now over, and it is now difficult to find places to legally access. However, the
famous Black water rivers in South Carolina, such as the Cooper River, continually wash out megalodon teeth from this formation. The best way to find megalodon
teeth in South Carolina is to dive for them! This isn't normal diving, it's Blackwater diving! This means there are strong currents, almost zero visibility, and
alligators. It can be dangerous, and there are occasionally fatalities, so it is not for the novice diver.
If you think you are ready to Blackwater dive, there are lots of charters that go out.
Just be sure to have "Hobby License" From the SCIAA before booking a charter.
To read about one of our Blackwater Dives,
Click here.
Maryland has the famous Calvert Cliffs, which is a large Miocene exposure that runs along the Chesapeake Bay. It's in fact one of the largest continually
running Miocene Exposures in the world. It's an awesome place to fossil shark tooth hunt. One simply combs the beach, looking in the surf line.
Unfortunately, there are a few downfalls to this location for Megalodon teeth. First, the megalodon teeth are usually smaller than many other collecting locations. A 4" tooth
is considered HUGE here. Secondly, access to most of the cliffs is private, and therefore illegal, and the public spots get hit HARD by fossil collectors.
Despite this, it's a wonderful place to explore and fossil hunt at. For more information, go to the Calvert Cliff Site Page.
-Calvert Cliff Fossil Site-
North Carolina has the famous Pungo River and Yorktown Miocene and Pliocene Exposures. These exposures are however underground, and
only pop out along some of the rivers. The PCS Phosphate mine in Aurora, NC use to allow collectors in to hunt these exposures. Now, due to safety reasons,
fossil hunting has been restricted. However, the Aurora Fossil Museum near the mine has truckloads of the mine tailings to search through. One can still find a
small megalodon tooth here. For more information, go to the Aurora Site Page.
-Aurora, North Carolina Fossil Site-
Florida has the Peace River Formation, which contains the Bone Valley Member. This streatches across central Florida. Famous places to look for megalodon teeth
include the Peace River, and off the coast in the Gulf. The teeth here are usually smaller than normal. Again, a 4" tooth is HUGE for the Bone Valley area.
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Megalodon Shark Tooth Diving in the Blackwater Rivers of South Carolina
Megalodon Shark Tooth Hunting at a land site in South Carolina. It's was raining and getting dark, but it payed off!
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Megalodon Teeth Morphology
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The megalodon shark teeth are unmistakable. They are big, robust, and serrated. However, identifying
a specific species is a bit more difficult. Generally, knowing the formation, and thus the time period the tooth was
found in, helps tremendously.
For example, if the tooth was found in an Eocene formation, its probably C. auriculatus, or C. aksuaticus,
depending on the serrations. If it was found in Oligocene deposits, it's probably C. angustidens. Miocene
formations would most likely have C. subauriculatus or C. megalodon, depending on if there are cusps on
adult teeth, and a Pliocene formation would have C. megalodon.
Generally speaking, each successor species has the following changes: smaller cusps (no cusps for adult C. megalodon),
a broader tooth form, a larger size, and more regular serrations. Juvenile C. megalodon sometimes have cusps, and
therefore look identical to C. subauriculatus. Also remember, depending on the exact age and formation, a
tooth may look more like a transition between two species.
The only genus Carcharocles may look similar to is that of Carcharodon. Carcharodon carcharias, the Great White shark,
may look similar to the Megatooth shark. There are, however, some straightforward differences. First, Great Whites
only occur in Miocene and Pliocene deposits, so they can be found with C. subauriculatus teeth and C. megalodon
teeth. However, compared to Megatooth shark teeth, Great Whites are much thinner and smaller with less robust roots.
Also Great White teeth do not have a bourlette, whereas Megatooth sharks have a very wide and noticeable one. Finally,
Great White teeth have very coarse and irregular serrations, compared with the regular serrations of the Megatooth
sharks.
The following fossil shark tooth Identification diagrams show three of the megatooth species, Carhcarocles megalodon, C. subauriculatus, and C. angustidens.
On the fossil tooth identification images below, the lingual sides of the teeth are the side facing the tongue, and are usually shown as the "display" side. The labial side is the side facing the front of the mouth. Labial sides are usually the smoother sides.
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Carcharocles megalodon tooth from Aurora, NC
Carcharocles subauriculatus tooth from the Calvery Cliffs of MD
Carcharocles angustidens tooth from Berkeley County, S.C.
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C. megalodon(Agassiz, 1843)
Megatoothed Shark
Obviously, this is the most famous prehistoric shark, as it is the pinnacle of megatooth shark evolution. It has the largest teeth, was
twice the size of a Great White, and included whales in its diet!
They lived from the Miocene and became extinct in the Pliocene. I sure am glad they're dead!
Just how big was that shark your tooth came from?
Click here to find out.
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This is our biggest Aurora meg yet. It's a robust upper. Unfortunately, there is feeding damage to the tip.
It measures a hair over 4.5" across, and a hair over 5" tall, with a 6" slant height. It would probably have
a 6 1/4" slant height if the tip was there.
Formation: Yorktown fm.
Age: 2.5-5 m.y.
Location: PCS Mine, Aurora, NC
Size: 6" slant (152 mm)
Date: Feb. 2009 TRIP
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This is a robust lower. There are a few chipped serrations however.
Click on the image to see it when found.
Formation: Yorktown fm.
Age: 2.5-5 m.y.
Location: PCS Mine, Aurora, NC
Size: 4 7/8" slant (124 mm)
Date: March 2008 TRIP
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This is a decent sized Upper tooth. However the serrations are chipped off. It has the look of a reworked fossil.
Click on the image to see it when found.
Formation: Yorktown; reworked from the Eastover fm.??
Age: 2.5-5 m.y.
Location: PCS Mine, Aurora, NC
Size: 4 5/8" slant (117 mm)
Date: March 2007 TRIP
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This is an upper tooth. The root has some damage done to it.
Click on the image to see it when found.
Formation: Yorktown fm.
Age: 2.5-5 m.y.
Location: PCS Mine, Aurora, NC
Size: 4.5" slant (114 mm)
Date: Feb. 2009 TRIP
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This is a beat up Lower lateral meg found while Blackwater Diving in the Lowcountry of South Carolina.
Formation: Hawthorne Formation.
Age: Pliocene, 2.5-5 m.y.
Location: Beaufort County, S.C.
Size: 4 5/16" slant (109 mm)
Date: July 2008 TRIP
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This is my favorite meg, because its my largest complete land find from South Carolina. Just look at the colors! The coloration of
lowcountry land teeth are beautiful.
It's an Upper tooth.
Formation: Undetermined Formation.
Age: Pliocene, 2.5-5 m.y.
Location: "Superpit" in Berkeley County, S.C.
Size: 4 1/16" slant (103 mm)
Date: Aug. 2003 TRIP
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Here is a near perfect Upper Aurora tooth.
Click on the image to see it when found.
Formation: ? Yorktown
Age: 5 m.y.
Location: PCS Mine, Aurora, NC
Size: 3 7/8" slant (98 mm)
Date: March 2006 TRIP
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I nice little Upper tooth with some feeding damage.
Click on the image to see it when found.
Formation: ?Yorktown
Age: 2.5-5 m.y.
Location: PCS Mine, Aurora, NC
Size: 2 7/8" slant (73 mm)
Date: March 2007 TRIP
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Lingual and labial view of a nice looking Lower lateral meg.
Click on the pic to see the trip this was found on.
Formation: Calvert
Age: Middle Miocene ~ 18-15 m.y.
Location: From
a private spot along the cliffs, Calvert Co., MD
Size: 2 3/8" (60mm) slant height
Date: November 2007.
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Lingual and labial view of a nice looking Lower lateral meg.
Click on the pic to see the trip this was found on.
Formation: Calvert, Plum Point member
Age: Middle Miocene ~ 18-15 m.y.
Location: From
a private spot along the cliffs, Calvert Co., MD
Size: 2 3/8" (60mm) slant height
Date: January 2004.
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The left tooth was found by snorkeling
, The right one is a small but almost
perfect anterior, except for the feeding damage on the tip.
This was pulled out of a chunk of fallen zone 10 of the Calvert formation.
Based on these teeth, the size of the sharks these teeth came
from were probably around 15 feet in length.
Formation: Left is Choptank. Right is Calvert, Plum Point member, Zone 10
Age: Middle Miocene ~ 18-15 m.y.
Location: Left is from a snorkel spot. Right is from
Randle Cliff, Calvert Co., MD
Size: Both have a 1 7/8" (47mm) slant height
Date: Left is from spring 2002, right is from spring 2000.
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These are three small lateral megs. The left one is a labial view of a
marble looking tooth. The right one is a lingual view of the first nearly complete
C. megalodon tooth Amy found. The left two are labial views.
Formation: Calvert, Plum Point Member
Age: Middle Miocene ~ 18-15 m.y.
Location: left-most one
is from Plum Pt. Other two are from near Willows, Calvert Co., MD
Size: 1 3/8 & 1 5/8" (35 & 41mm) slant
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All 3 of these laterals were found on the same stretch of beach
in less than an hour. The person I was collecting with now hates me.
The left one is in perfect condition.
Formation: Calvert, Plum Point Member
Age: Middle Miocene ~ 18-15 m.y.
Location: Willows, Calvert Co., MD
Size: Complete one has a 1 5/8" slant (41mm)
Date: Spring 2002
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C. chubutensis (Ameghino, 1906) aka subauriculatus (Agassiz, 1839)
Megatooth Shark
This species is thought to have evolved into C. megalodon. The only difference
is the tiny cusplets, and smaller size.
This species is only found in the Miocene.
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This is a 3 5/8" C. subauriculatus in a chunk of Pungo River contact layer.
Click on the image to see it as found and being prepped.
Formation: Pungo River
Age: Roughly 18-22 m.y.
Location: PCS Mine, Aurora, NC
Size: 3 5/8" Slant Height (92mm)
Date: Sept 2008 TRIP
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This is a nice 3" subauriculatus in a chunk of Pungo River Coquina (Limestone).
Click on the image to see it as found and being prepped.
Formation: Pungo River
Age: Roughly 18-22 m.y.
Location: PCS Mine, Aurora, NC
Size: 3" Slant Height (75mm)
Date: Sept 2005 TRIP
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This is a lingual view of a 3" upper tooth.
Click on the image to see it when found.
Formation: Pungo River
Age: Roughly 18-22 m.y.
Location: PCS Mine, Aurora, NC
Size: ~3" slant (76mm)
Date: March 2005 TRIP
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Here is a chipped 3" subauriculatus.
Click on the image to see is as found.
Formation: Pungo River
Age: Roughly 18-22 m.y.
Location: PCS Mine, Aurora, NC
Size: 3" Slant Height (75mm)
Date: March 2006 TRIP
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This is the very first megatooth sharktooh I found!
It's an Upper tooth.
Based on this tooth, the
size of the shark it came from was probably
around 21 feet in length.
Formation: Calvert, Plum Point member
Age: Early - Middle Miocene ~ 18-15 m.y.
Location: Plum Pt., Calvert Co., MD
Size: 2.75" (70mm) slant height
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This is a lingual view of a small lateral that Amy found.
Click on the image to see it when found.
Formation: Pungo River
Age: Roughly 18-22 m.y.
Location: PCS Mine, Aurora, NC
Size: ~1 7/8" slant (47mm)
Date: March 2005 TRIP
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We found a tiny one... This guy was dug out of a chunk of fallen Zone 10 in the Calvert Formation. It
appears to have some feeding damage on the tip.
Formation: Calvert, Plum Point member, Zone 10
Age: Middle Miocene ~ 16-15 m.y.
Location: Randle Cliff, Calvert Co., MD
Size: 1 1/4" (30mm) slant height
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This is a small chipped Chubutensis posterior (from the rear of the mouth).
You can tell it's a Chubby, due to the tiny "cusp" at the edge of the tooth
Formation: Calvert, Plum Point Member
Age: Middle Miocene ~ 18-15 m.y.
Location: Willows, Calvert Co., MD
Size: 1 1/8" (28.5mm) slant height
Date: Summer, 2001
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C. angustidens (Agassiz 1843)
Megatooth Shark
This species is thought to have evolved into Carhcarocles subariculatus. The only difference
is the cusps are larger, the blades are not as broad, and the teeth are often smaller in size.
This species found in the Oligocene.
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This is a worn/beat up fossil tooth found while diving.
Formation: Chandler Bridge Formation.
Age: Oligocene, ~28 m.y.
Location: Edisto River, Colleton County, S.C.
Size: 2 5/8" slant (66 mm)
Date: Aug. 2004 TRIP
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Here is another water worn shark tooth found from diving.
Formation: Chandler Bridge Formation.
Age: Oligocene, ~28 m.y.
Location: Edisto River, Colleton County, S.C.
Size: 2 3/8" slant (60 mm)
Date: Aug. 2004 TRIP
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Here is a chipped angustidens fossil tooth from a land site in S.C.
Formation: Undetermined Formation.
Age: Reworked into Pliocene?, 2.5-5 m.y.
Location: "Superpit" in Berkeley County, S.C.
Size: 2" slant (51 mm)
Date: Aug. 2003 TRIP
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Here is a nice looking one with a "lightening" pattern on the blade. This fosisl tooth is from a drainage ditch in SC.
Formation: Chandler Bridge Formation.
Age: Oligocene, ~28 m.y.
Location: Berkeley County, S.C.
Size: 1 3/4" slant (44 mm)
Date: Aug. 2006 TRIP
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This is a small shark tooth in near perfect shape from a land site in S.C.
Formation: Undetermined Formation.
Age: Reworked into Pliocene?, 2.5-5 m.y.
Location: "Superpit" in Berkeley County, S.C.
Size: 1 5/16" slant (33 mm)
Date: Aug. 2003 TRIP
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