Showing posts with label paleontology. Show all posts
Showing posts with label paleontology. Show all posts

7.22.2008

Giant Lanky Rhinoceros


Baluchitherium "osborni"
National Museum of Natural History, Smithsonian Institution, Washington, DC
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This monstrous mammal reached the height of a giraffe and the girth of a mammoth, though it was a relative of the rhino. Convergence in tooth structures with grazers of trees shows the formidable front teeth (partially obscured in the photo) were for stripping leaves from twigs. It should be noted that there are some taxonomic problems with this genus. It is currently properly known as Paraceratherium, though Indricotherium is also commonly used. As per usual, a life restoration follows; it appears as a large, lanky rhino.



Crow Shark


Squalicorax
Cretaceous formation of Alabama

6.29.2008

Hell Pig


Archaeotherium
National Museum of Natural History, Smithsonian Institution, Washington DC

This is a type of entelodont, a distant relative of modern pigs. It's odd teeth, though similar to pigs, indicate scavenging on meat playing a larger part of the diet. Though one might not think a pig is the scariest thing in the world, this animal could have looked you in the eye, with a shoulder height of about two meters. They were the apex predators of around the Oligocene-Miocene boundary across the northern hemisphere.

6.24.2008

Roofed Lizard


Stegosaurus
National Museum of Natural History, Smithsonian Institution, Washington DC

I'm sure everyone who might read this knows what this thermoregulating, Jurassic ornithischian knows what this looks like, but here goes:


6.08.2008

Whorl-tooth



Helicoprion
National Museum of Natural History, Smithsonian Institution, Washington DC

Though it is not clear by looking at it, this is perhaps one of the most interesting vertebrate dentitions. It is actually the teeth of the lower jaw of an ancient shark that lived from 280 to 225 million years ago. The entire set of lower teeth is visible. How it captured prey with this unique structure is not understood. Here is what it would have looked like in life:












6.05.2008

And Now, For Something a Bit Older


Triceratops horridus
National Museum of Natural History, Smithsonian Institution

5.25.2008

Miocene Anapsid Scute


From Brownie's Beach, Chesapeake Beach, MD; Miocene Epoch

4.22.2008

Monster Mouth

Dunkleosteus terrelli

Members of Order Arthrodira, meaning joint-necked, composed the majority of the Class Placodermi and, for that reason, are the most familiar to science. Truly the top carnivores of their time, aquatic monsters such as Dunkleosteus terrelli filled the role of the largest sharks or even crocodiles in our time. They are named arthrodires due to a peculiar craniovertebral joint behind the skull, allowing the chondrocranium to rise as the splanchnocranium drops, resulting in a monstrous maw (Linzey 2001, Murphy 2004). Also unique amongst the arthrodires is the presence of gnathals, a structure performing the same function as teeth in more advanced gnathostomes. This means that teeth arose at least twice, convergently, given that placoderms have no living relatives and some arthrodires have very unique gnathal structure (Smith and Johanson 2003, Stokstad 2003).

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Major differences, however, are structure and replacement methods. In the latter, the general opinion is that arthrodires had no replacement, unlike most fish which are polyphyodonts, though that has been recently questioned (Smith and Johanson 2003). Instead of many small teeth for capturing or rending prey, which other fishes of the time had, the arthrodires had what can be likened to broad axes in their mouths rather than daggers. These semidentine blades, supragnathals on top and infragnathals below, had a biting power surpassed only by archosauromorphs while being able to open with lightning speed (Stokstad 2003). This creates a truly frightening picture of arthrodires like Dunkleosteus. Not only did the up to thirty foot long creature have a bite surpassing anything in the oceans today, but its quickly opening gape created a pressure gradient causing suction, meaning the smallest and swiftest of prey had as much to fear as other heavily armored arthrodires.

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Because of its size, it is supposed Dunkleosteus was an ambush predator, not unlike crocodilians. However, unlikely evidence seems to point to otherwise. A specimen was recovered with intact skin cells, bringing attention to color as well as behavior. Black and red pigments were recovered from the dorsum, while the venter was covered in a silvery, reflection layer (Waggoner 2000, Linzey 2001). This could be a shared trait, similar to the iridocytes found in modern fish, gleaming from guanine crystals. Determining the first instances of color would be crucial in determining whether this is a homology or homoplasy. This discovery had two major implications. The first was that color vision could have been around at the time, given that Dunkleosteus would have blended in with the reddish sediment if viewed from above and looked similar to the surface if viewed from the sea floor. It would have needed some visual camouflage from members of its own species, given little else could have done it harm and gouges matching gnathals from the same species have been found on their four-foot-wide armored heads (Waggoner 2000). The second point is that if Dunkleosteus was a benthic, ambush predator, it would not have evolved ventral camouflage. Needing camouflage on the venter means if was viewed enough from the bottom, and was vulnerable, to be selected for. This indicates that arthrodires are much more active predators that what was once thought, swimming as much in the middle of the water column as on the bottom of the sea.

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Arthrodires had a range covering most seas of the Devonian, from species of the genera Confractamnis, Atlatuidosteus, and Doseyosletts of Queensland, Australia, to species in Morocco (Young 2005). Individuals have also been found in Scotland, such as Cosmacanthus, which was initially confused with an acanthodian (Newman 2004). This means that placoderms have an interesting zoogeography, their total range is sub-Equatorial, from Euramerica to Australia. However, there appears to be no evidence of placoderms unearthed from Arabia or India, lands that are between Euramerica and Australia, though areas further south in what would become North Africa have fossils. Therefore, an argument for a Gondwanan distribution could be made, though this would be tenuous. Arthrodire placoderms were apex predators, filling the niche of sharks today (Young 2005).

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Linzey, D. 2001. Gnathostome Fishes. Pages 91-128. Vertebrate Biology. McGraw Hill, New York.
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Murphy, DC. 2006. “Devonian Times.” Retrieved 05 Apr 2008 from http://www.devoniantimes.org/index.html.
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Smith, MM & Z Johanson. 2003. “Separate Evolutionary Origins of Teeth from Evidence in Fossil Jawed Vertebrates.” Science, Vol. 299 (5610), 1235.
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Stokstad, E. 2003. “Primitive Jawed Fishes had Teeth of Their Own Design.” Science, Vol. 299 (5610), 1164.
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Waggoner, B. 2000. “Introduction to the Placodermi.” Retrieved 29 Mar 2008 from http://www.ucmp.berkeley.edu/vertebrates/basalfish/placodermi.html.
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Young, GC. 2005. “A New Middle Devonian Arthrodire (Placoderm Fish) from
the Broken River Area, Queensland.” Records of the Australian Museum, Vol. 57
(2), 211-220.

3.29.2008

The Little Placoderm Who Could

Bothriolepis

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When one considers the placoderms, the image of Dunkleosteus terrelli probably comes to mind. However, the class is much more diverse than the arthrodires, with a myriad of body forms arising over the group’s fifty million year run. Bothriolepis is a good example of this. Though they share armor plating, the similarities between these general seem to end there. Size, for instance, provides a stark contrast. Dunkleosteus grew to between twenty and thirty feet long, with a head up to four feet wide, whereas the diminutive Bothriolepis had a head only four inches wide (Waggoner, 2000).

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Bothriolepis lacks the craniovertebral joint of the arthrodires that allowed its chondrocranium to rise as its splanchnocranium drops. However, this may have allowed for a larger braincase in this benthic creature (Young, 1984). This genus, along with the rest of the placoderms, went extinct in the Mississippian Period with no modern relatives. The reason for placoderm extinction, especially when members of Class Chondrichthyes survive today, is mysterious.
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Young, G.C. (1984). “Reconstruction of the Jaws and Braincase in the Devonian Placoderm Fish, Bothriolepis .” Palaeontology, Vol. 27 (3), 635-661.
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Waggoner, B. (2000). “Introduction to the Placodermi.” Retrieved 29 Mar 2008 from http://www.ucmp.berkeley.edu/vertebrates/basalfish/placodermi.html.

3.28.2008

To Be or Not to Be ... an Acanthodian


Groenlandaspis disjectus
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Found in the Upper Devonian (~365 million years ago) of Scotland, Cosmacanthus malcolmsoni caused a bit of confusion when it was unearthed in the mid-1800's. It had a peculiar spine that seemed to place it with the members of Class Acanthodia, which all sported a spine structure on their dorsum and venter that had membranous connections to the body mass. However, upon further comparison, the difference between C. malcolmsoni and acanthodians widened, and it was placed in Class Placodermi. Newman (2004) reviewed this taxonomic revision and found it to be better, seeing as it is similar spinal plates to, and was nearby, the known placoderm Groenlandaspis disjectus.
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Newman, M.J. (2004). “A Systematic Review of the Placoderm Genus Cosmacanthus and a Description of Acanthodian Remains from the Upper Devonian of Scotland.” Paleontology, Vol. 48 (5), 1111-1116.

3.27.2008

Was It Ever Safe to Go in the Water?


Guarinisuchus munizi
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In what I'm sure will be a long line of blogging on ScienceBlogs posts as well as on peer reviewed research - and sometimes both - here is a summary of a post from Laelaps on a new crocodilian, G. munizi. After the K-T extinction that finished off the non-avian dinosaurs, especially the monstrous aquatic mosasaurs, the three-meter long archosauromorph fluorished. These sauropsids have a Gondwanan distribution, most likely moving from North Africa to the (then nearby) South America. G. munizi would certainly have made a snack out of the other major group filling the space left by the absent dinosaurs - mammals.

3.26.2008

What Big Teeth You Have


Smilodon populator

An interesting piece of research published recently describes what it perceives to be the point of such long canine teeth in Smilodon and members of Nimravidae. Initially conceived to rend wounds into their prey, it has been shown that such force would snap those teeth right off. New tests propose a stabbing motion. Whether mainly for slicing or stabbing, the awe at this spectacularly singular dentition remains.