Carcharocles chubutensis
Encyclopedia
Carcharocles chubutensis is a prehistoric megatoothed shark that lived during Oligocene
, Miocene
, and Pliocene
epochs, approximately about 28 - 5 million years ago. This shark is considered to be a close relative of another prehistoric megatoothed shark, C. megalodon
. However, as is the case with C. megalodon, the classification of this species is disputed.
teeth and some fossilized vertebral centra. Shark skeleton
is composed of cartilage
and not bone
, and cartilage rarely gets fossilized. Hence, fossils of C. chubutensis are generally poorly preserved. Although the teeth of C. chubutensis are morphologically similar to teeth of C. megalodon, they are comparatively slender with curved crown, and with presence of lateral heels feebly serrated. Fossils of this species have been found in North America
, South America
, Cuba
, Puerto Rico
, Africa
, and Europe
.
and commonly preyed upon fish
, sea turtles, cetaceans (e.g. whales), and sirenids.
of C. chubutensis remains in dispute. The Swiss naturalist Louis Agassiz
first identified this shark as a species of Carcharodon in 1843. In 1906, Ameghino
renamed this shark as C. chubutensis. In 1964, shark researcher, L. S. Glikman recognized the transition of Otodus obliquus
to C. auriculatus. In 1987, shark researcher, H. Cappetta reorganized the C. auriculatus - C. megalodon lineage and placed all related megatoothed sharks along with this species in the genus Carcharocles. Finally, the complete Otodus obliquus to C. megalodon progression became clear and has since gained the acceptance of many shark researchers.
Within the Carcharocles lineage; C. chubutensis is the succeeding species of C. angustidens and is succeeded by C. megalodon. In short, C. chubutensis is considered to be the ancestor of C. megalodon. However, due to its co-existence with C. megalodon during the Miocene and Pliocene epochs, it is regarded as a morpho-species.
Oligocene
The Oligocene is a geologic epoch of the Paleogene Period and extends from about 34 million to 23 million years before the present . As with other older geologic periods, the rock beds that define the period are well identified but the exact dates of the start and end of the period are slightly...
, Miocene
Miocene
The Miocene is a geological epoch of the Neogene Period and extends from about . The Miocene was named by Sir Charles Lyell. Its name comes from the Greek words and and means "less recent" because it has 18% fewer modern sea invertebrates than the Pliocene. The Miocene follows the Oligocene...
, and Pliocene
Pliocene
The Pliocene Epoch is the period in the geologic timescale that extends from 5.332 million to 2.588 million years before present. It is the second and youngest epoch of the Neogene Period in the Cenozoic Era. The Pliocene follows the Miocene Epoch and is followed by the Pleistocene Epoch...
epochs, approximately about 28 - 5 million years ago. This shark is considered to be a close relative of another prehistoric megatoothed shark, C. megalodon
Megalodon
The megalodon and ὀδούς ) is an extinct species of shark that lived roughly from 28 to 1.5 million years ago, during the Cenozoic Era .The taxonomic assignment of C...
. However, as is the case with C. megalodon, the classification of this species is disputed.
Fossil record
This species is also known from fossilFossil
Fossils are the preserved remains or traces of animals , plants, and other organisms from the remote past...
teeth and some fossilized vertebral centra. Shark skeleton
Skeleton
The skeleton is the body part that forms the supporting structure of an organism. There are two different skeletal types: the exoskeleton, which is the stable outer shell of an organism, and the endoskeleton, which forms the support structure inside the body.In a figurative sense, skeleton can...
is composed of cartilage
Cartilage
Cartilage is a flexible connective tissue found in many areas in the bodies of humans and other animals, including the joints between bones, the rib cage, the ear, the nose, the elbow, the knee, the ankle, the bronchial tubes and the intervertebral discs...
and not bone
Bone
Bones are rigid organs that constitute part of the endoskeleton of vertebrates. They support, and protect the various organs of the body, produce red and white blood cells and store minerals. Bone tissue is a type of dense connective tissue...
, and cartilage rarely gets fossilized. Hence, fossils of C. chubutensis are generally poorly preserved. Although the teeth of C. chubutensis are morphologically similar to teeth of C. megalodon, they are comparatively slender with curved crown, and with presence of lateral heels feebly serrated. Fossils of this species have been found in North America
North America
North America is a continent wholly within the Northern Hemisphere and almost wholly within the Western Hemisphere. It is also considered a northern subcontinent of the Americas...
, South America
South America
South America is a continent situated in the Western Hemisphere, mostly in the Southern Hemisphere, with a relatively small portion in the Northern Hemisphere. The continent is also considered a subcontinent of the Americas. It is bordered on the west by the Pacific Ocean and on the north and east...
, Cuba
Cuba
The Republic of Cuba is an island nation in the Caribbean. The nation of Cuba consists of the main island of Cuba, the Isla de la Juventud, and several archipelagos. Havana is the largest city in Cuba and the country's capital. Santiago de Cuba is the second largest city...
, Puerto Rico
Puerto Rico
Puerto Rico , officially the Commonwealth of Puerto Rico , is an unincorporated territory of the United States, located in the northeastern Caribbean, east of the Dominican Republic and west of both the United States Virgin Islands and the British Virgin Islands.Puerto Rico comprises an...
, Africa
Africa
Africa is the world's second largest and second most populous continent, after Asia. At about 30.2 million km² including adjacent islands, it covers 6% of the Earth's total surface area and 20.4% of the total land area...
, and Europe
Europe
Europe is, by convention, one of the world's seven continents. Comprising the westernmost peninsula of Eurasia, Europe is generally 'divided' from Asia to its east by the watershed divides of the Ural and Caucasus Mountains, the Ural River, the Caspian and Black Seas, and the waterways connecting...
.
Size
C. chubutensis was larger than C. angustidens. Teeth of C. chubutensis can approach 130 mm in slant height (diagonal length), which according to size estimation method proposed by Gottfried at al, in 1996, indicate 12.2 m (40 ft) long specimen.Paleoecology
Paleontological research suggests that this species may have changed habitat preferences through time, or it may have had enough behavioral flexibility to occupy different environments at different times.Diet
C. chubutensis was likely an apex predatorApex predator
Apex predators are predators that have no predators of their own, residing at the top of their food chain. Zoologists define predation as the killing and consumption of another organism...
and commonly preyed upon fish
Fish
Fish are a paraphyletic group of organisms that consist of all gill-bearing aquatic vertebrate animals that lack limbs with digits. Included in this definition are the living hagfish, lampreys, and cartilaginous and bony fish, as well as various extinct related groups...
, sea turtles, cetaceans (e.g. whales), and sirenids.
Phylogeny
As is the case with other known megatoothed sharks, the genusGenus
In biology, a genus is a low-level taxonomic rank used in the biological classification of living and fossil organisms, which is an example of definition by genus and differentia...
of C. chubutensis remains in dispute. The Swiss naturalist Louis Agassiz
Louis Agassiz
Jean Louis Rodolphe Agassiz was a Swiss paleontologist, glaciologist, geologist and a prominent innovator in the study of the Earth's natural history. He grew up in Switzerland and became a professor of natural history at University of Neuchâtel...
first identified this shark as a species of Carcharodon in 1843. In 1906, Ameghino
Florentino Ameghino
Florentino Ameghino was an Argentine naturalist, paleontologist, anthropologist and zoologist.Born in Luján, son of Italian immigrants, Ameghino was a self-taught naturalist, and focused his study on the lands of the southern Pampas...
renamed this shark as C. chubutensis. In 1964, shark researcher, L. S. Glikman recognized the transition of Otodus obliquus
Otodus obliquus
Otodus obliquus is an extinct mackerel shark which lived during the Paleocene and Eocene epochs, approximately about 60 to 37.5 million years ago.-Known physiology:This shark is known from the fossil teeth and fossilized vertebral centra...
to C. auriculatus. In 1987, shark researcher, H. Cappetta reorganized the C. auriculatus - C. megalodon lineage and placed all related megatoothed sharks along with this species in the genus Carcharocles. Finally, the complete Otodus obliquus to C. megalodon progression became clear and has since gained the acceptance of many shark researchers.
Within the Carcharocles lineage; C. chubutensis is the succeeding species of C. angustidens and is succeeded by C. megalodon. In short, C. chubutensis is considered to be the ancestor of C. megalodon. However, due to its co-existence with C. megalodon during the Miocene and Pliocene epochs, it is regarded as a morpho-species.
See also
- List of prehistoric fish
- List of apex predators
- Largest prehistoric organismsLargest prehistoric organismsThe largest prehistoric organisms include both vertebrate and invertebrate species. Many are described below, along with their typical range of size...
External links
- Carcharocles: Extinct Megatoothed shark from ELASMO