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Placoderm

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Placoderms were a significant group of extinct prehistoric fish. Their name comes from Ancient Greek words meaning "plate skin."

Placoderm anatomy
Placoderm anatomy

This name describes their unique physical structure. Most of their head and thorax were covered by articulated, bony armor plates. While their skeletons were mostly made of cartilage, these plates provided heavy protection. The rest of their bodies varied by species. Some were covered in scales, while others were naked. These animals were crucial to evolution. They were among the first jawed fish, or gnathostomes. They were also the first vertebrates to possess true teeth.

Evolution of placoderms
Evolution of placoderms

Placoderms were incredibly diverse in how they lived and moved. Many groups were bottom-dwellers that lived near the substrate. The antiarchs were a successful group of these bottom-dwellers. They inhabited freshwater and shallow marine environments during the Middle to Late Devonian. One genus, Bothriolepis, included over 100 valid species.

Bothriolepis canadensis (2024)
Bothriolepis canadensis (2024)

Other placoderms, called arthrodires, were active, nektonic predators. These fish lived in the middle or upper parts of the water column. Some had streamlined, bullet-shaped head armor to help them swim fast.

Amazichthys
Amazichthys

While most were predators, some species were herbivorous. Others, like the giant Titanichthys, were planktivores that ate tiny floating organisms.

Reproduction in placoderms provides some of the most extraordinary fossil evidence. In the Gogo Formation of Western Australia, scientists found fossils that prove live birth.

Xiushanosteus
Xiushanosteus

One fossil, named Materpiscis attenboroughi, shows a female that died while giving birth. The fossil includes a 6 cm offspring with an intact umbilical cord. This proves that some placoderms were viviparous, meaning they gave birth to live young. This discovery pushes the known history of live birth back by 200 million years. Other specimens, such as Incisoscutum ritchei, also show embryos inside them. Males reproduced by using long structures called claspers. Interestingly, these claspers were not attached to pelvic fins like those in modern sharks. This is an example of convergent evolution, where different structures evolve to perform similar roles.

One of the most famous placoderms was the massive Dunkleosteus. This huge arthrodire is considered one of the world's first vertebrate superpredators.

Dunkleosteus terrelli 2024 reconstruction
Dunkleosteus terrelli 2024 reconstruction

It likely preyed upon other predators. Its remains have been found in Europe, North America, and possibly Morocco. The size and strength of such predators helped placoderms dominate the oceans. They eventually outcompeted other marine animals like eurypterids and cephalopod molluscs. This allowed them to become the apex predators of their time. Their presence shaped the entire food web of the Devonian period.

Our understanding of these fish has changed through careful scientific study. In the 1830s, Louis Agassiz published early studies on fossil fishes. At that time, people thought placoderms were jawless fish or even turtle-like. In the late 1920s, Dr. Erik Stensiö changed this view. He worked at the Swedish Museum of Natural History in Stockholm.

Brindabellaspis
Brindabellaspis

Stensiö used a very meticulous method to study fossil skulls. He ground the fossils away one tenth of a millimeter at a time. After each layer, he made a wax imprint of the surface. This allowed him to see tiny anatomical details. His work helped prove that placoderms were true jawed fishes related to sharks.

Modern research continues to refine where placoderms fit in the tree of life. Recent analysis of fossils from the Gogo reef has provided new clues. These fossils show that placoderms share features with many different gnathostome groups. For example, they have separate bones for nasal capsules. In modern sharks and bony fish, these bones are part of the braincase. Because of these unique traits, scientists now view placoderms as a group of basal gnathostomes. This means they are a fundamental group near the base of the jawed vertebrate lineage. They represent a critical stepping stone in vertebrate history.

Despite their long success, all placoderms eventually went extinct. They lived through the Silurian and Devonian periods. However, they disappeared about 358.9 million years ago. This occurred during the end-Devonian Hangenberg event.

Scientists once thought they lost to bony fish or sharks. Now, they believe environmental catastrophes caused their decline. These catastrophes affected both marine and freshwater ecosystems. When the placoderms died out, they left ecological niches open. This allowed survivors like osteichthyans and chondrichthyans to radiate and expand. The disappearance of the placoderms changed the course of life in the oceans forever.

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🖼️ Images & Media (18)
File:Placoderm anatomy.png
Placoderm anatomy.png
File:Evolution of placoderms.png
Evolution of placoderms.png
File:DunkleosteusSannoble.JPG
DunkleosteusSannoble.JPG
File:Amazichthys.jpg
Amazichthys.jpg
File:Eczematolepis.jpg
Eczematolepis.jpg
File:Xiushanosteus.jpg
Xiushanosteus.jpg
File:Dunkleosteus terrelli 2024 reconstruction.jpg
Dunkleosteus terrelli 2024 reconstruction.jpg
File:Bothriolepis_canadensis_(2024).png
Bothriolepis_canadensis_(2024).png
File:Brindabellaspis.png
Brindabellaspis.png
File:Phyllolepis12DB.jpg
Phyllolepis12DB.jpg
File:Kimbryanodus williamburyensis.jpg
Kimbryanodus williamburyensis.jpg
File:Asterosteus stenocephalus.jpg
Asterosteus stenocephalus.jpg

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