Different Directions

Different Directions

Eurypterids

Eurypterids were the top predators of the Silurian seas.

Eurypterids were aggressive predators; large eyes to detect movement, enormous spined claws that could crush and bring prey towards the mouth.

Abundant Prey species in the form of armored trilobites and bony skin (ostracoderm) fishes during the Silurian meant that a lot of crushing was needed to get the soft stuff into its small mouth.

Just behind the eight small walking legs were large flattened paddles, which are believed to have had a swimming function. The paddles may have been used to "row" through the water somewhat like water boatmen and backswimmer bugs of today.

The broad tail of Pterygotus ended in a large rounded paddle with dorsal keels. The tail could flex up and down and may have been the best bet for Pterygotus to cover a distance or make a quick getaway.

But being one of the larger predators of the Silurian lagoons, Pterygotus probably caused more fleeing than anything else.

Here's a geological map of this time that shows some of the lagoons.


Use this link to compare the Silurian landmasses with our current Earth.

Side Trip

The Silurian

The Silurian period lasts from about 440 to 410 mya.

  • A relatively short period in geological history.
  • A time of stabilization of global temperatures.
  • A time of the first terrestrial animals and

The most predominant organisms during the Silurian were the hard-shelled Brachiopods.


It is estimated that these creatures made up about 80% of the total species at the time.

Tropical Reefs were common in the shallow seas with

  • Corals
  • Stromatoporid organisms, and
  • Bryoza being most common.
  • Trilobites
  • Graptolites
  • Cephalopds
  • Gastropods
  • Echinoderms

However the Trilobites were still in a period of decline. During this period the Graptolites also began declining in numbers.

The Silurian period is the first period in history where fish begin to appear in the fossil record.

At the beginning of the period, jawless fishes appeared to have invaded the freshwaters while at the end of the period, jawed fishes begin to appear. These animals were not considered to be the dominant creatures, however.

Also, during the Silurian is the appearance of the first terrestrial ecosystem.

The first evidence of vascular plants (plants with tissues that carry food) appear in the fossil record of areas above sea level. The earliest land plant and possible millipede-like animal fossils were found in modern day Europe.

Back To Eurypterids

Eurypterids resembled giant water scorpions, usually measuring 5 to 17 inches, but the biggest (Pterygotus) reached 6 to 8 feet in length.


The Eurypterids terrorized the shallow seas, estuaries, and lakes.

In addition to pincers on some of the preoral appendages, the eurypterid could flex its thorax up and forward, like the terrestrial scorpion, to attack with its spiny telson, which was probably poisonous.


Eurypterids first appear in the early Ordovician, peak in number and diversity by the late Silurian, and then decline through the Carboniferous.

They meet their ultimate demise along with the trilobites and 95% of all extant species during the great Permian extinction.

Their Prey

Early Eurypterid fossils occur with marine invertebrates during the Ordovician, but the Silurian, they appear in sediments from brackish lagoons and bays.

By the Pennsylvanian period, they have moved to freshwater swamps as seen by associated plant fauna as well as freshwater mussels and snails.

To understand the rise and decline of the eurypterids and their change in territories, one must understand their prey.

Text Box:  Copyright Karen Carr. To see more of her exciting work: www.karencarr.com/gallery_silurian.html

The most primitive of vertebrates, the jawless fish or Agnatha, appeared and flourished in the Silurian period.

These primitive fish

  • Lacked lateral fins
  • Slow moving, sitting ducks for a larger predator.

The Agnatha were adapted to bottom dwelling habits, scraping the bottom and sucking up food (referred to as benthonic).

The Agnatha developed strong external armor formed from bony plates, resulting in the alternate name of Ostracoderms (shell skins).

The armor was the only defense against the ravages of the Eurypterids. These fish congregated in shallow waters and were ultimately followed by their predator.


There were two types of armored fish ( Acanthodians and Placoderms -- See Below ) that developed mobile jaws and paired lateral fins. The fins allowed much faster swimming to elude predators and also allowed adaptation to larger bodies of water such as oceans and thus evade the more confined and less mobile Eurypterids.

As these new prototypes dominated in the Devonian period, the Eurypterids began a steady decline in number of species and of individuals, never to recover.

Just One More Thing

Ostracoderm - is an archaic and informal term for a member of the group of armoured, jawless, fishlike vertebrates that emerged during the early part of the Paleozoic Era (542-251 million years ago).

Ostracoderms include both extinct groups, such as the heterostracans and hagfishesand lampreys.

Acanthodians and Placoderms -

  • Acanthodians are a poorly understood group of extinct jawed fishes that are distinguished by the bony spines projecting in front of their fins and by minute, diamond-shaped scales.
  • Placoderms are arguably the most diverse groups of the early jawed fishes.

For more information about these, go here, an outstanding site: Devonian Times

http://www.devoniantimes.org/index.html

Here's an interesting video about Eurypterids:

http://animal.discovery.com/videos/animal-armageddon-eurypterids.html

The Permian-Triassic-Tr) extinction event, informally known as the Great Dying, was an extinction event that occurred 251.4 million years ago, forming the boundary between the Permian and Triassic geologic periods.

It was the Earth's most severe extinction event, with up to 96 percent of all marine species and 70 percent of terrestrial vertebrate species becoming extinct; it is the only known mass extinction of insects. 57% of all families and 83% of all

Because so much biodiversity was lost, the recovery of life on earth took significantly longer than after other extinction events.


Main

an archaic and informal term for a member of the group of armoured, jawless, fishlike vertebrates that emerged during the early part of the Paleozoic Era (542-251 million years ago). Ostracoderms include both extinct groups, such as the heterostracans and osteostracans, and living forms, such as hagfishes and lampreys.

Paleo Fun

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