Seven of Earth’s Earliest Gigantic and Bizarre Creatures

Anomalocaris Canadensis Lived 500 Million Years Ago

1. Strange Anomalocaris

Anomalocaris canadensis dominated the Cambrian period seas for tens of millions of years beginning approximately 540 mya. It grew to only two feet (60 cm) long, which doesn’t seem very big by today’s standards, but in relation to every other organism during the Cambrian, it was a giant.

Interesting history of its stalled scientific discovery: A segment fossil of Anomalocaris canadensis was first discovered in the Canadian Rockies in 1892, but it wasn’t until 1981 that a major breakthrough about its identity occurred; and that was further refined in 1996. This one hundred year history of inaccurate theories is but one example of the difficulty identifying fossil remains of Cambrian organisms having no apparent living descendants. Anomalocaris and other genera have since been discovered at various Cambrian fossil locations around the world, including the famous Burgess Shale site in the Canadian Rocky Mountains, the USA, China, and Australia.

Photo: Anomalocaris Canadensis Complete Fossil Specimen

Anomalocaris with its large eyes, impaling front spines and strong swimming lobes probably could overtake any prey during its lifespan, including trilobites. Except, some scientists argue that its pineapple-ring mouth did not have hard parts necessary to crush the tough outer shells of trilobites. Much still remains to be clarified about their anatomy and habits. Scientists believe it swam with an “S” method of locomotion, undulating up and down the length of its body.

Fossils of Anomalocaris Front Spines and Mouth

Watch the video below to observe Anomalocaris unique movement in the water!

Giant Cameroceras – Straight Shelled Nautiloid “Orthocone” Source

2. Straight Shelled Nautiloid “Giant Orthocone”

The T-Rex of the following time period, the Late Ordovician, beginning around 470 mya, emerged the cephalopod nautiloid creature related to squids and octopuses known as the Giant Orthocone “Cameroceras”. The massive creature’s living tissue was contained primarily at one end of a very long conical shell which could reach 20-30 feet (6-9 meters) in length. Straight-shelled nautiloids (orthocones) varied wildly in size from just a few inches to massive, but most were in the range of several feet long. The animal’s inner shell contained chambers that it could fill with water and then push the water out in order to jet propel itself in a backwards motion. This also alowed it to maneuver up and down throughout the ocean strata. The inner chambers also contained special gases for buoyancy.

The Giant Orthocones seized its prey using meter long (three feet) muscular tentacles and a beak-like mouth in order to rip apart its victims. It fed upon fish and its arch enemy, sea scorpions.

Did you know fossils of straight-shelled cephalopod nautiloids have been quarried by Europeans for many years and adorn floors, stairs, jewelry, gravestones and art pieces with their durable and desirable beauty?

Straight Shelled Nautiloid Polished Fossils

3. Eurypterid Sea Scorpion

Eurypterid Sea Scorpions (Pentecopterus, the earliest known eurypterid) Artist Rendition Patrick J. Lynch, Yale University

Eurypterids, simply put, were scorpions of the sea, otherwise known as sea scorpions. They were the largest known arthropods that ever lived. The fossils of sea scorpions have been found all over the world. The U.S. state of New York has unearthed an especially large number of this predatory animal. Eurypterids survived a long history beginning with the Ordovician Period extending into the Permian Period from about 460 million-years-ago to 248 mya. That’s over a 200 million year history!

Sea Scorpion Fossils Source: Fossil Guy

Sea scorpions both swam and walked using six legs, two of which were flattened like paddles. They were normally marine sea-floor dwellers, and interestingly, they could also live in freshwater. Sea scorpions preyed upon fish, trilobites and other animals living near the seabed. They possessed strong defenses such as sharp spines, crushing claws and armored plating. Their has been disagreement among scientists whether some of the prehistoric species possessed stingers. The eurypterid’s arch enemies were the straight-shelled nautiloids.

Megalograptus was one of the earlier large species of eurypterid sea scorpions measuring 4 feet (1.2 meters) long, not including its front pincher claws. However, the most common species of eurypterids typically measured only 8 inches (20 cm) long.

Photo: Megalograptus – Giant Eurypterid Sea Scorpion

Jaekelopterus was a later species of sea scorpions emerging during the Devonian Period around 390 mya, reaching over 8 feet (2 meters) or more in length. Try to imagine a scorpion about the size of a kayak! Terrifying!

Note: The tables were turned when the sea scorpion’s arch enemies, the straight shelled nautiloids, declined in size during the Devonian time slot from their giant Ordovician Period predecessors. As a result, eurypterids like Jaekelopterus gained the upper hand using their powerful claws to clamp down and crush the linear shells of smaller nautiloids.

Photo: Jaekelopterus – Scale of Giant Eurypterid Sea Scorpion

4. Dunkleosteus Placoderm Fish

Dunkleosteus

During the Devonian Period around 416 mya until about 360 mya, vertebrates had greatly arisen on the ocean scene. A highly evolved class of fish called “placoderms” possessing advanced characteristics stemming from their predecessor “ostracoderms” dominated the ancient seas. For protection, both classes of fish possessed armored plates covering their head and upper torso regions. The main advancement with placoderms was the development of a jawbone and paired fins. Those two significant adaptations provided them the necessary speed and power to become fearsome predators, aggressively chasing prey rather than waiting for the perfect opportunity. Ostracoderms were eventually overrun into extinction unable to compete with their cousin placoderms.

Dunkleosteus terrelli Fossil

Dunkleosteus placoderm was the T-Rex of the Devonian time-period, terrorizing the ancient seas. He reached lengths up to 10 meters (33 feet) and weighed almost 4 tons. Instead of teeth, Dunkleosteus possessed two pairs of impaling sharp boney blades. Dunkleosteus could open its mouth in 1/50th of a second, which would have caused a powerful suction that pulled prey into its mouth, a food-capturing ability reinvented by many of the most advanced fish today. The placoderm fish could then bite down with a pressure of up to 8,000 pounds per square inch (55 mph), placing it in the league of T-Rex and modern crocodiles! There wasn’t much of anything the great placoderm didn’t or couldn’t eat during its lifespan, including its own kind.

In recent decades, Dunkleosteus has finally achieved the recognition it deserves as a super predator. There are a large number of its fossil specimens on display which have been found in North America, Poland, Belgium and Morocco.

Terataspis Grandis Trilobite

5. Grand Trilobites

Trilobites have an incredible history first appearing approximately 520 million years ago during the Cambrian Period. They thrived for nearly 300 million years, acting as dominant marine arthropods, before going extinct during the Permian-Triassic mass extinction event around 250 million years ago. They were among the earliest and most successful complex animals on Earth!

Terataspis grandis (shown above) means “great monster shield”. Through millions of years of evolution, by the middle of the Devonian Period around 400 mya, trilobites, although low on the food chain, had evolved some serious defenses to survive predators such as the large and spiny Terataspis grandis. Like most trilobites, Terataspis grandis was a bottom feeder, scavenging anything it could find, but it also was an opportunistic predator preying on burrowing animals such as small mollusks, worms and smaller arthropods. Terataspis grandis reached about 2 feet (60cm) in length, which in relation to most other trilobites, was enormous. The vast majority of trilobite species were small, typically measuring between 1 and 4 inches (3 and 10 cm) in length.

Large Species of Trilobite Comparison Chart shows Isotelus the largest, Terataspis grandis the third largest and Acadoparadoxides briareus (Paleo Joe’s Sample) the fourth largest!

Isotelus, rex is the largest trilobite ever found going back in the time scale from the Ordovician Period which began 485 mya. It could reach 28 inches (71 cm) in length. Many of Isotelusrex fossils have been discovered in the great state of Ohio where it is the proud state fossil.

Paleo Joe holding Acadoparadoxides briareus large trilobite!

All trilobites were sea creatures having the distinction of possessing a segmented body, multiple jointed limbs and an armored outer shell, placing them in the category of arthropods related to insects and crustaceans. Trilobite means three lobes in Greek, from tri and lobos, named for its three major lengthwise sections.

Stethacanthus Extinct Shark Rendition by Michael Schlesinger

5. Bizarre Prehistoric Sharks

Beginning in the late Devonian Period and into the early Carboniferous Period around (345 to 300 mya) sharks were diversifying so much that scientists have labeled it the “Golden Age of Sharks”. The placoderms were dying out, only lasting a 50 million year history compared to sharks 400 million year history. With the decline of placoderms, environmental niches allowed sharks to fill in, and as a result they assumed a wide variety of bizarre shapes. From this stage of evolution, they had become the top predators of the oceans.

Stethacanthus Extinct Shark Fossil

Stethacanthus shark may have grown to 11 feet (3.3 meters) long, but sources differ referring somewhat smaller. One thing undisputed is the strange anvil-like growth protruding from its back that was completely overlaid with sharp brush-like spikes. The same type of spikes also covered the top of its head. There has been much speculation about the use of these spikes. One theory proposes it may have played a role in courtship, while another proposes it simply may have made the creature look more frightening.

Prehistoric Shark Helicoprion Source

Another strange shark emerging during the period was Helicoprion. Not much is truly known about this shark, but the pattern of its teeth is instantly recognizable. They formed a whorl semi-circle arrangement protruding out of its mouth. One theory suggests the whorl may have aided in shelling or extracting the bodies of nautiloids and ammonites.Unlike modern sharks, the teeth did not fall away at the front possibly resulting in the rotated bizarre spiral which mystifies modern science.

Tooth Worl Fossil of Prehistoric Shark Helicoprion – Photo by James St. John

The largest genus of sharks in the bizarre top-predator group was Edestus giganteous described in the video below. Edestus giganteous lived during the latter part of the Carboniferous Period around 325 mya. He reached up to 20 feet (6 meters) long weighing up to 2 tons. That’s comparable to the largest great white sharks of today. Comparable to its relative, Helicoprion, Edestus giganteus’s teeth formed a strange curved shape, and it also did not shed its teeth. It must have been very intimidating to other creatures looking as if it possessed saw blades for a mouth.

Gigantic Ammonite “Parapuzosia seppenradesis” – Artist Rendering

7. Giant Cephalopod Ammonites

Ammonites were closely related to the straight-shelled cephalopod nautiloids only they had adapted a coiled shell which allowed them more freedom of mobility. They even used the same jet propulsion mode of movement. Their numbers greatly grew beginning as early as the Devonian and peaked some 300 million years later during the Cretaceous Period (144 – 65 mya). Consecutively, the straight-shell forms greatly declined, unable to compete with the more mobile ammonite nautiloids.

Parapuzosia seppenradesis lived during the Cretaceous Period (145 to 66 mya). The sample in the photo was unearthed in Germany and measured 6.5 feet (2 meters) in diameter. The biggest forms of ammonites have been especially found in later rocks of the upper Jurassic Period from around (180 -145 mya) such as Titanites occidentalis, shown below.

The ammonite fossil shown in the photo below with the lady was first discovered in 1947 on the side of a mountain in British Columbia, Canada. It has been scientifically recognized as Titanites occidentalis. The original fossil was too fragile to move, so scientists used latex to make molds of it. The fossil measures 6.7 feet (2 meter) in diameter earning the nickname “Fossil Truck Tire”. Later, in 2004, another, even larger specimen was found in the same region confirming that the current mountainous region was formerly a shallow, tropical sea.

Titanites Occidentalis Giant Ammonite Fossil

The ammonites were so successful and numerous with approximately 30 to 40 thousand species that their remains are used as index fossils for scientists to date rock layers and other organisms within the same rock strata. The super successful ammonites experienced the same final fate 65 million years ago along with the dinosaurs. Their close relative, the nautilus, often referred to as a living fossil, is the lone survivor among nautiloids.

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Check out my two fiction books featuring prehistory insights blended with imaginative storytelling that educate as they entertain! Perfect for young explorers, ages 11-15+! A coloring/activiy book available includes story scenes, fossil photos with descriptions of plants and animals from the Devonian time period and more, suitable for adults, as well! Available on Amazon.com.

Identifying Fossils (Crinoids, Bryozoans, Corals and More) Discovered on Lake Michigan Beaches

Lake Michigan Beach Fossil Hunting

I Found a Fossil on the Beach and Wondered

You’re enjoying a walk on the beach and something catches your eye lying in the sand. It’s not driftwood or beach glass or even a pretty rock. You suspect you have found something that was once a living creature and you can’t let it go. Has that ever happened to you? A deep sense of wonder and childlike imagination may drive you to find out what you picked up from our freshwater or saltwater sandy-shores. My own sense of wonder led to learn about the fossilized creatures I have found on the beaches of Lake Michigan, including what they looked like when they were alive and how and when they lived. I was also curious to know how they showed up so prevalent along our freshwater beaches. Taking things a step further, I drew illustrations of their living beings included in my article.

  • Fossil Facts in the following order:
  • Crinoids
  • Bryozans
  • Brachiopods
  • Clams
  • Petoskey Stones
  • Favosites Honeycomb Corals
  • Horn Corals
  • Chain Coral Halysites
  • Stromatolites

NOTE: The following fossil descriptions are individually included articles in my fossillady site under “Categories” with additional info, illustrations or photos. I decided it would be expedient for Lake Michigan beach fossil-hunters to present them here together in a single article.

Crinoid Fossil Stems and Tiny Crioid Fossil Pieces

Crinoid Fossils

Crinoid fossils are some of the most common fossils found along Lake Michigan beaches. They’re often referred to as “Indian Beads” because Native Americans are known to have strung together their broken off cheerio-shaped pieces in order to make necklaces. They’ve also been referred to as Lucky Stones because spotting one of the tiny pieces requires a bit of luck! Crinoid animals were sessile creatures—in other words, they remained attached to the sea floor by means of a long single stem. Attached atop of their stem was an intricate cup-like structure from where numerous branching arms grew outwards, much like a plant or tree. The frame works of crinoids were constructed from each individual circular section (shown above) which were stacked one on top of another. The hole in the center of each section contained soft tissue supplying nutrients throughout the animal. Some varieties were known to have towered several meters high off the seafloor. Their entire structure resulted in the living organisms’ beautifully colored and flower-like appearance, which granted them another common name “sea lilies”.

Crinoid “Sea Lily” Illustration Drawing

Sea lily crinoids captured tiny food particles passing by in ocean currents with their feathery network of fingers that functioned like traps. Crinoids invertebrate animals fit into the phylum of Echinoderm, meaning spiny skin. They are cousins to starfish, sea urchins, and feather stars.

“Sea lily” crinoids lengthy history dates far back to the Ordovician Period around 500 million years ago, although the fossil record reveals their heyday occurred during the Mississippian Period around 345 mya. Today, there are far few species, but they lack the long meandering stems common in Paleozoic varieties and live in colder, deep ocean depths. For more photos and drawing of crinoids go to another fossillady article specifically about theme HERE.

How Are Saltwater Ocean Fossils Found as Far North as Michigan? During their Paleozoic lifetimes, much more of the world’s continents were covered under warm, shallow, saltwater seas, including the Great Lakes regions. When after thousands of Paleozoic ocean species died, including crinoids, they became buried in sediment and under certain conditions, fossilized.

Millions of years later, around ten thousand years ago, the giant glaciers sculpted deep basins, forming the Great Lakes. In the process, they also dug into the deep layers of sediment where crinoid remains and their counterparts lay buried and were thusly released. Since then, the perpetual wave action of the big lakes has continued to deposit them on our beaches where we have the privilege of finding them!

Extinct Bryozoan Fossil “Fenestella” Found on Lake Michigan Beach

Bryozoan Fossils

Bryozoans earn the common name, lace corals, due to their delicately threaded appearance, but they were not true corals. Instead, they were moss-like invertebrate animals. My sample belongs to the family of extinct “Fenestellida” known for their fan-shaped, mesh-like constructs and the genus “Fenestella”. They lived in tight colonies sculpted by hard, limy, branching structures. The colony consisted of thousands of individual animals called “zooids”. Each individual zooid lived inside its own limy tube called a zooecium. The zooecium were the size of sewing needles. A single zooid began the colony. A modern day bryozoan colony has been observed growing from a single zooid to 38,000 in just five months. Each additional zooid is a clone of the very first.

Bryozoan “Fenestella” Extinct Fossil Drawing

Interesting how bryozoans feed. Each zooid has an opening through which the animal can extend its “lophophore” a ring of tentacles that captured microscopic plankton passing by in the oceanic currents. If one zooid receives food, it nourishes the neighboring zooids joined by strands of protoplasm. If only we humans could be more like them, ensuring everyone on the planet is fed!

Their incredible fossil record dates back 500 million years ago (mya), with 15,000 known species. Today there are approximately 3,500 living species. For more information and photos about bryozoans you can go to the fossillady article specifically about them HERE.

Polished Petoskey Stone (Hexagonaria, percarinata) Coral Fossil, Michigan

Petoskey Stone Coral Fossils

Petoskey Stones “Hexagonaria, percarinata” flourished in mass colonies during the Paleozoic time slot when Michigan and all of the Americas were covered under shallow, saltwater seas. The ancient seascape must have been lit up with a quiltwork of colors created by their vast colonies. Sadly, they became extinct at the end of the Permian Period mass extinction approximately 250 million years ago.

The name “Petoskey” originated from an Ottawa fur-trader chief named, Petosegay. A northern Michigan city was named after him, later, the name was modified to Petoskey. Because the coral fossils are so abundant near the city of Petoskey and surrounding region, Governor George Romney signed a bill in 1965 making the Petoskey Stone the official state stone and fossil.

Petoskey Stone found on Southwestern Lake Michigan Beach
Petoskey Stone (Side View) Lake Michigan

I found the above Petoskey Stone on Oval Beach in Southwestern Michigan. This sample is rough and raw and unpolished. It’s smoothness and wear is a good example demonstrating Lake Michigan’s natural polishing process produced by perpetual winds, waves, and sand movement. It’s a fairly large sample at least the size of a man’s fist. The sideview of it, shown right, reveals the stem where the coral attached to the ancient seafloor. It’s kind of rare to see this because so many of these coral fossils are sanded down and polished for their intricate beauty and sold as gifts and keepsakes.

Each individual coral hexagon structure called, corrallite, is visible in most Petoskey Stone fossils. Corallites held a single animal (polyp) which opened a mouth to expose tentacles. The tentacles took in food and were also used to sting other organism or even neighboring coral tentacles that came too close. Calcite, silica, and other minerals replaced the original corallite exoskeleton. For addition fossillady photos and information specifically about Petosky Stones click HERE.

Drawing of Extinct Hexagonaria, percarinata “Petoskey Stone” Living on Cliffside
Favosites “Honeycomb” Coral Fossils “Charlevoix Stones” found on SW Michigan Beach

Favosites “Honeycomb” Coral Fossils

Favosites fossils are fairly common to find if you live in Northern Michigan, particularly near Charlevoix, but they are more rare to find in Southwestern Michigan where I found the above samples on the beach. Favosites is a genus of corals that belonged to the extinct order of “tabulate” colony corals. Gathered together they created colorful reefs thriving in warm, shallow seas during the same time period as the “Petoskey Stone” extinct corals, which I described above. The favosites can easily be identified by the honeycomb patterns enfolding their exterior fossil remains. These where the casings supporting their individual living coral polyps that could retract inside or stretch out, as with all coral species. Consequently, they are often referred to as, “Honeycomb Corals”, but they are also called “Charlevoix Stones” due to their dominant appearance in that region of Michigan.

Drawing of Favosites Coral “Honeycomb Coral” with polyps out!
Favosite Fossil

The tabulae (horizontal internal layers) of favosites were built outward as the organism grew. These layers can clearly be seen in the fossil photos provided. The walls between each corallite (cup housing for the individual animal polyps) were pierced by pores known as mural pores which allowed a transfer of nutrients between polyps. For more photos and information specifically about favosites in another fossillady article go HERE.

Brachiopod Fossil found on Lake Michigan Beach

Brachiopod Fossils

No other organisms typify the Age of Invertebrates more than brachiopods. They were the most abundant animals during the Paleozoic Era, except for maybe trilobites. Due to their abundance, paleontologists use them to date rocks and other fossils found in the same rock strata. Countless billions accumulated on the ocean floor with over 30,000 forms. Today there are far fewer species, only around 300, which live mostly in cold, deep ocean environments.

Brachiopods look similar to clams but are very different inside. Also, clams (pelecypods) have uneven-shaped shells, but both top and bottom halves are identical. Brachiopod possess symmetrical shells, left to right, but the bottom shell is smaller. Brachiopods are commonly called “lampshells” due to some species displaying a similar shape as a Roman oil lamp.

Varied Shapes of Brachiopods Drawing (sample page from fossillady coloring book)

Brachiopods live in communities attached to objects by a muscular foot called a “pedicle”. They strain water in and out of their shells, filtering microorganisms with a crown of feathery tentacles called “lophophores”. They come in a variety of interesting shapes as demonstrated in this image included in my fossil coloring book available for sale! More interesting information about brachiopods by fossillady described HERE!

Clam Fossils found on Lake Michigan beach

Clam Shell Fossils

I found these clam fossils on the shore of Oval Beach in Southwestern Michigan. The sample above left clearly reveals hardened muddy sediment that has completely encrusted the clam shell inside and out. The samples above right and below (dark grey) are examples of mold casts of the animal’s shells, where sediment and minerals permeated inside the shell after the animal died. Their smooth surfaces are the telltale demonstration of Lake Michigan’s sand, wind and water movement acting as a polisher.

Clam” can be a term that covers all bivalves. Some clams bury themselves in sand and breathe by extending a tube to the water’s surface. Bivalve oysters and mussels attach themselves to hard objects, and scallops can free swim by flapping their valves together. All types lack a head and usually have no eyes, although scallops are a notable exception. With the use of two adductor muscles, clams can open and close their shells tightly. Very fittingly, the word “clam” gives rise to the metaphor “to clam up,” meaning to stop speaking or listening.

Bivalves have occupied Earth as early as the Cambrian Period 510 million years ago, but they were particularly abundant during the Devonian Period around 400 million years ago. Their fossils are discovered in all marine ecosystems and most commonly in near shore environments. In 2007, off the coast of Iceland, a clam was discovered that was estimated to be about 507 years old. It was declared the world’s oldest living creature by researchers at Bangor University in North Wales. For more in-depth information about extinct clam species click HERE.

Horn Corals found on Lake Michigan Beach

Horn Coral Fossils

It’s always exciting to find these curious horn coral fossils when combing the beach for something interesting to discover. Horn corals are a genus of corals that belonged to the extinct order of “rugose” corals which appeared as early as 450 million years ago until about 250 mya. That’s an astounding 200 million years living on Earth. Their name derives from their unique horn-shaped chamber with its wrinkled (or rugose) wall. When viewed from its widest opening, it looks like a pinwheel from where the coral polyps once poked out in order to sift microorganisms passing by in the ocean currents. Some species grew two meters high off the seafloor. They were mostly solitary animals, with a few exceptions that grew in mass colonies. For more information and photos about horn corals you can visit another fossillady article specifically about them HERE.

Fossillady Coloring Book Drawing of Paleozoic Coral Reef

This is a page from my coloring book I illustrated featuring a Paleozoic coral reef vista. It includes horn corals and the other extinct invertebrate animals which I have outlined in this article. See if you can identify them. For purchase of the coloring book or my two fiction books centered on Paleozoic insights that educate as they entertain, you can go to Amazon or IngramSpark.

Hayisites “Chain Coral” Fossils found on Lake Michigan Beach

Chain Coral Fossils

The trail of chains in these beach-smoothed fossil stones is another occasional fun and interesting find from our Michigan beaches. “Chain Coral” is a common name given to the genus “Halysites” coral from the order “Tabulate” colony corals. Halysites survived from the Ordovician Period (starting around 480 mya) through the Silurian Period (ending around 416 mya). As with most coral polyps, they possessed stinging cells, but the polyps were mainly used to grasp plankton floating by in the ocean currents. As their coral polyps continued to multiply, they added more links to the chain, sometimes building large limestone reefs.

Halysites “Chain Coral” with polyps out
Stromatolite Fossil Stone found on Lake Michigan Beach

Stromatolite Fossils

You’re combing the beach and pick up a common looking smooth stone and admire its sleek texture. You wet the stone and suddenly layers of striations are revealed. That’s what happend with this fossil stone that I found on the beach. It turned out to be a stromatolite fossil and I learned that they are the oldest of all fossils, dating as far back as 3.5 billion years. Their heyday was long before the Cambrian creatures evolved (stromatolites actually paved the way for their existence). Stromatolites were simple cyanobacteria capable of photosynthesis. Their structures grew solid, layered, and varied, some of which looked like giant mushrooms reaching eight feet tall. Through photosynthesis, they changed Earth’s atmosphere from carbon-dioxide-rich to oxygen-rich. Before 1956, scientists believed they were extinct until living stromatolites were discovered in Shark Bay of Australia. Since then, there have been many more stromatolite discoveries around the globe. For more photos and information about stromatolites you can go to this fossillady article specifically about them HERE.

The stromatolites forming today in the shallow waters of Shark Bay, Australia are built by colonies of microbes. Credit: University of Wisconsin-Madison

Check out my two fiction books blended with prehistory insights and imaginative storytelling that entertain as they educate. Geared toward young exlporers interested in early life and fossils, or young readers who simply like a good story; ages 11-15+. Also available, a coloring/activity book featuring scenes from the books along with many of the plants and animals that lived during the amazing Devonian Time Period; fossil photos and descriptions included. Available onAmazon or IngramSpark.

All rights reserved © Fossillady 2026

Straight Shelled Nautiloids Have a Long History

Straight-shelled nautiloids date back from the Cambrian Period roughly 500 million years ago and survived into the Late Triassic Period around 230 mya. That’s approximately 270 million years of living on earth . . . overwhelming and astounding!  Their fossilized shells have been discovered all around the world in large assemblages commonly occurring in marine limestone rock.

During the 18th and 19th centuries, all the straight-shelled nautiloids were named orthoceras, creating a wastebasket taxon and confusion. To clarify, orthoceras is a specific genus of extinct nautiloids restricted to Middle Ordovician aged marine limestones of the Baltic States and Sweden. And more recently to add to the confusion, orthocone refers to just the straight shell.

Orthocone (Orthoceras) Straight-Shelled Nautiloid Fossil

The straight-shelled nautiloids were an abundant group of marine mollusk cephalopods that flourished during the Paleozoic timeslot and diminished by the end of the Triassic period into extinction. They are related to modern day cephalopods including octopus, squids, cuttlefish and the nautilus. They were also related to the extinct ammonites possessing coiled shells, which evolved after them. The straight-shelled nautiloids likely were not as agile as their cousin coiled-shelled ammonites. Both species possessed a siphuncle tube that ran through the entire lenght the animal’s inner chambers inside their shells. Each inner chamber was separated by a wall called, a septa wall. As the animal grew, it added another septa wall and a new septa chamber of a larger size.

To move throught the ocean water, the straight-shelled nautiloids and ammonites filled their inner chambers with water by using the siphuncle tube. They then forced the water out which propelled them backward with a kind of jet propulsion. The tube also served as a buoyancy device by releasing the water and leaving air space. This allowed the animal to raise and lower itself through various ocean depths.

The straight-shelled nautiloids possessed 8 to 10 powerful tentacles which protruded from the wide opened end of its shell and out its head. The tentacles detected and captured prey. The animal possessed well developed eyes, a beak and a well developed brain and head with a hood.

(Orthoceras) Straight-Sheled Nautiloid Fossil

Their fossils have been quarried by Europeans for many years and adorn floors, stairs, jewelry, gravestones and more with their durable and desirable beauty.

The straight-shelled nautiloids displayed extreme diversity in size from a few inches to 14 feet in length. One of the largest straight-shell giants from the earliest years, Cameroceras, reached approximately 30 feet ( 9 meters) in length.

cameroceras

 CLASSIFICATION

Kingdom:  Animalia

Phylum:    Mollusk  (large diverse group of invertebrates with soft bodies encased in a shell i.e. clams, snails, oysters )

Class:      Cephalopoda  (means prominent head and tentacles i.e. squid, octopus, nautilus, cuttlefish)

Subclass: Nautiloidea   (series of chambers of increasing size connected by a central tube)

Order:     Orthocerida  (extinct group of  cephalopods possessing long straight shells)

Family:     Orthoceridae (early Ordovician to the Triassic period (approx. 490–200 million years ago) straight horn nautiloids)

Genus:    Orthoceras (means straight horn)

Scan_Pic0006
Cephalopod Straight Shelled Nautiloid Orthoceras Drawing Rendition

Check out my fiction book, one of two in a series, featuring factual prehistory insights blended with imaginative storytelling that educates as it entertains. Also availabale, a coloing/activity book featuring scenes from both books along with many of the plants and animals that lived during the amazing Devonian Time Period; fossil photos and descriptions included. Perfect for young explorers interested in fossils or young readers who simply like a good story. Ages 11-15+ available on a Amazon.com

All rights reserved © Fossillady 2026