Jurassic Park Period Part 4

Fauna - Reptiles

During the Jurassic, dinosaurs came to dominate the animal world, but they were not the only type of animals. The first birds appeared, evolving from a branch of theropod (hollow-boned) dinosaurs, to share the skies with pterosaurs, the dominant flying vertebrates. Lizards made an appearance and have been with us ever since. Therian mammals evolved, meaning creatures that gave birth to live young, and that includes marsupials. Crocodylomorphs (which eventually gave rise to modern crocodylia, but not during the Jurassic) transitioned from a terrestrial to an aquatic life. The oceans were inhabited by marine reptiles such as ichthyosaurs and plesiosaurs.

This is a lot of ground to cover (so to speak), so I'm going to start in the oceans and work my way to land and sky.

The Triassic/Jurassic extinction event decimated crocodile-like reptilian diversity, with crocodylomorphs (which originated during the last half of the Triassic) being the only group to survive. Even the herbivorous aetosaurs died out. [Can you imagine if they had survived, and we had vegetarian crocodiles raiding our gardens?] The diversity of crocodylomorphs during the Early Jurassic was about the same as those of the Late Triassic, but they occupied different ecological niches.

A group of predominantly marine crocodylomorphs became a prominent part of marine ecosystems. Within that group, some became highly adapted for life in the open ocean, including the transformation of limbs into flippers, the development of a tail fluke, and smooth, scaleless skin.

Turtles - Turtles (Testudinata) diversified during the Jurassic. The Jurassic turtles are believed to have formed 2 more advanced groups, the Mesochelydia (which were aquatic), and the Perichelydia. There are 2 modern groups turtles (the Testudines), which are terrestrial and had diverged by the Middle Jurassic. The Thalassochelydia is a diverse lineage of sea turtles, and is known from the Late Jurassic of Europe and South America.

Lepidosaurs - The tuatara is a reptile native only to New Zealand, and is the sole living representative of the Rhynchocephalians, which had achieved a global distribution by the beginning of the Jurassic. The Rhynchocephalians occupied a wide range of lifestyles, including the aquatic pleurosaurs with long snake-like bodies and reduced limbs, the herbivorous eilenodontines, and the Oenosaurus, which had broad tooth plates indicative that they ate creatures that were hard-shelled or had an exo-skeleton, such as corals, shelled mollusks and crabs. Rhynochocephalians disappeared from Asia after the Early Jurassic. The last common ancestor of living squamates (which includes lizards and snakes) is estimated to have lived around 190 million years ago during the Early Jurassic. Squamates first appear in the fossil record during the Middle Jurassic and included early members of a snake lineage. However, many Jurassic squamates have unclear relationships to living groups. Eichstaettisaurus from the Late Jurassic of Germany has been suggested to be an early relative of geckos and displays adaptations for climbing.

Ichthyosaurs - The Ichthyosaurs suffered an evolutionary bottleneck during the Triassic/Jurassic extinction event, with all but one group of them becoming extinct. Ichthyosaurs reached its apex of species diversity during the Early Jurassic, including the huge apex predator Temnodontosaurus and the swordfish-like Eurhinosaurus. However, Early Jurassic ichthyosaurs were significantly less morphologically diverse than their Triassic counterparts

Plesiosaurs - The Plesiosaurs originated at the end of the Triassic Period. At least 6 lineages of plesiosaur crossed the Triassic-Jurassic boundary, so they were already diverse in the Earliest Jurassic. Early plesiosaurs were generally small-bodied, with body size increasing later. There appears to have been a strong turnover as the middle of the Jurassic Period began, with the extinction of 2 groups that had been widespread, and the first appearance of the Cryptoclididae group, which became the dominant group of the latter half of the Jurassic. During this time, the thalassophonean pliosaurs, which had ancestrally been small-headed and long-necked, evolved short necks and large heads. Some species, such as the Pliosaurus, had skulls up to 2 metres (6 ft) in length, with body lengths estimated around 10-12 meters (30-36 feet), making them the apex predators of Late Jurassic oceans. Small-bodied plesiosaurs also invaded freshwater environments during the Jurassic, as shown by remains found in freshwater sediments from China and Australia.

Pterosaurs - Pterosaurs first appeared in the Late Triassic, but a major group of Jurassic pterosaurs is the Rhamphorhynchidae, which first appeared in the Early Jurassic. They ate fish. Another group, the Anurognathids, first appeared in the Middle Jurassic. They had short heads and densely furred bodies, and were probably insectivores. Short-tailed pterodactyloids first appeared in the at the beginning of the Late Jurassic. These include the ctenochasmatids, which have closely spaced needle-like teeth that were presumably used for filter feeding. The Late Jurassic Cycnorhamphus had a jaw with teeth only at the tips, with bent jaws like those of living openbill storks, that may have been used to hold and crush hard invertebrates.

Some of these animals could be found on land, as indicated in the above paragraphs by what they ate. But I'm fairly confident that they had branches of relatives living in the oceans. I am sorry for the use of huge tongue-twisting names, but there were so many names, I would have gotten completely bogged down trying to describe the various species.

There you have some of the reptiles that lived in the oceans and other waterways. This has been a long post, so I am going to end it here and take up fish next time. Yes, there were fish in the waters, too.

There will not be a quiz on the names used in this blog. Class dismissed.

https://en.wikipedia.org/wiki/Jurassic

https://en.wikipedia.org/wiki/Crocodylomorpha

Triassic Period Part 2

 Now let's take a look at the inhabitants of the Triassic Period.

Three categories of organisms can be distinguished in the Triassic record: survivors from the Permian–Triassic extinction event, new groups which flourished briefly, and other new groups which went on to dominate the Mesozoic Era.

To go back to the beginning, after the extinction event just before the Triassic Period began, the Earth's biosphere was impoverished. It was well into the middle of the Triassic before life recovered its former diversity. Therapsids (including what would become mammals) and archosaurs (including crocodilian reptiles) were the chief terrestrial vertebrates of this period. A specialized subgroup of archosaurs, called dinosaurs, first appeared late in the Triassic, but did not become dominant until the succeeding Jurassic Period.

The first true mammals also evolved during this period, as well as the first flying vertebrates, the pterosaurs, who were a specialized subgroup of archosaurs.

In marine environments, new types of corals appeared in the Early Triassic, forming small patches of reefs of modest extent compared to the great reef systems of modern times. The shelled ammonites (whose shell resembled that of the modern nautilus, but is not an ancestor) recovered, diversifying from a single line that survived the Permian-Triassic extinction.

The fish fauna was remarkably uniform, with many families and genera exhibiting a global distribution in the wake of the mass extinction event. There were also many types of marine reptiles. The first of the lizard-like animals appeared in the Early Triassic seas and soon diversified, and some developed to huge size during the Late Triassic.

On land, the surviving plants included ginkos, ferns, and horsetails, among others. Seed plants came to dominate the terrestrial flora. In the northern hemisphere, conifers and ferns flourished. A seed fern genus would dominate Gondwana throughout the period.

Many groups of terrestrial fauna appeared in the Triassic period or achieved a new level of evolutionary success during it. They include lungfish, Temnospondyls (early amphibians that had mostly been replaced by reptiles, they made a come-back in this period), Rhynchosaurs (the primary large herbivores in many Triassic ecosystems), Phytosaurs (looked like crocodiles, but unrelated), Aetosaurs (heavily armored and mostly herbivorous), Rauisuchians (the keystone predators of most Triassic terrestrial ecosystems), Theropods (dinosaurs but not the large kind that would come later; most were 1-2 meters long), and Cynodonts (a large group that includes true mammals, complete with hair and a large brain).

Some amphibians were among those groups that survived the Permian-Triassic extinction event. The first ancestors of frogs are known from the Early Triassic, but did not become common until the Jurassic (which comes next).

Among reptiles, the earliest turtles appeared during the Late Triassic Period.

During the Triassic, archosaurs displaced therapsids as the dominant amniotes. This may have contributed to the evolution of mammals by forcing the surviving therapsids and their mammalia-form successors to live as small, mainly nocturnal insectivores. Nocturnal life may have forced the mammaliaforms to develop fur and a higher metabolic rate.

Though the end-Triassic extinction event was not equally devastating in all terrestrial ecosystems, several important clades of large reptiles disappeared, as did most of the amphibians, groups of small reptiles, and others (except for the proto-mammals). Some of the early, primitive dinosaurs also became extinct, but more adaptive ones survived into the Jurassic. Surviving plants that went on to dominate the Mesozoic Era included modern conifers.

The cause of the Late Triassic extinction in uncertain. It was accompanied by huge volcanic eruptions that occurred as the supercontinent Pangaea began to break apart about 202 to 191 million years ago, forming one of the largest known inland volcanic events since the planet had first cooled and stabilized. Another possible but less likely cause for the extinction event might be global cooling.

 

 

https://en.wikipedia.org/wiki/Triassic

Permian Period Part 2

 Mammals and reptiles could cope with the desert conditions better than amphibians, and so rose to dominate the Permian. Such dry conditions favored plants with seeds enclosed in a protective cover, rather than plants like ferns, that disperse spores. Modern trees like conifers, ginkgos and cycads appeared in the Permian.

On land, life included diverse plants and fungi. At first, a lot of the Carboniferous flora still flourished. But around the middle of the period, a massive desert covered the interior of Pangaea, and there are indications that the desert was devoid of vegetation. Even in areas where it wasn't such a stark desert, more advanced seed ferns and early conifers moved in. A number of types of plants and animals died out or became marginal elements. By the end of the Permian, swamps reminiscent of the Carboniferous survived only on a series of equatorial islands east of Pangaea that would later become South China.

The Permian saw the diversification of many important conifer groups, including ancestors of many present-day families. Rich forests were present in many area, with a diverse mix of plants. Southern Pangaea saw extensive seed fern forest, and oxygen levels were probably high there. The ginkgos and cycads also appeared.

Insects were very prevalent during the Permian, especially considering that 90% of the insects at the start of this period were cockroach-like insects. Primitive forms of dragonflies were the dominant aerial predators. Several insect groups appeared or flourished during this time, including beetles, true bugs and others.

Larger 'more advanced' types of animal life included reptiles and amphibians. A number of the reptiles seemed to be what I call the 'sail-backed' lizards, where they have bone ridges protruding from their spine and covered in skin. Some of these were herbivore and some were carnivore. I didn't find any indication of how large they might have gotten.

At some point, amphibians declined, and at least one family of the 'sail-backed' lizards was replaced with more advanced animals, including mammals and mammal-like animals. Towards the very end of the period, the first archosauriforms appeared. These were reptiles that possibly rose from the crocodile family and would go on in the next period to produce dinosaurs and pterosaurs. There were no flying vertebrates, although there was a family of gliding reptiles by the end of the period.

Also appearing late in the Permian were the first synodonts, which would evolve into mammals during the next period. Permian synapsids (the group that would later include mammals) thrived and included some large members, such as Dimetrodon. Their special adaptations enabled them to flourish in the drier climate, and they grew to dominate the vertebrates.

In the Permian sea, life was everywhere. You might have found mollusks, starfish, sea dollars, sea urchins and sea cucumbers if you went swimming, or animals very much like these modern versions. But as stated earlier, most of the marine life went extinct during the last days of this period. Nothing was said about the sharks or fish that were so prevalent in the previous period.

Could we live here? Plenty of plants are growing, at least, where it wasn't a desert, so maybe we could grow crops. Could we domesticate some of the herbivore sail-backed lizards? Would we want to? They're lizards, so they wouldn't give any milk. I have no idea how big their eggs might be, so that might be a reason to domesticate them. Okay, we'll leave some of us here to colonize the Permian, and the rest of us will go on to see what comes next.

 

https://en.wikipedia.org/wiki/Permian

https://en.wikipedia.org/wiki/Emeishan_Traps

https://en.wikipedia.org/wiki/Cimmeria_(continent)

Carboniferous Period

 The Carboniferous Period spanned 358.9 million years ago to 298.9 million years ago. On a time table, it sits behind the Devonian Period and before the Permian Period.

In the Early Carboniferous Period, average global temperatures were approximately 68 F (20 C). During the Middle Carboniferous, they dropped to about 54 F (12 C). Carbon dioxide levels fell during the period from roughly 8 times today's level at the beginning to about the same as today's level at the end. Lack of growth rings of fossilized trees suggest a lack of seasons, or a tropical climate. Glaciations in Gondwana were triggered by its southward movement, and continued beyond this time period.

Also, there was mountain building as continents collided to form Pangaea. There was a minor extinction event at the end of the period, caused by climate change.

Now, the last we heard, pieces of Gondwana had broken off and were sitting at the equator or slightly north, while the rest of Gondwana drifted south to the south pole.

During the Carboniferous Period, the land was covered by vast forests, which would eventually become the coal beds characteristic of this period's stratigraphy. Some of the Early Carboniferous land plants were very similar to those of the Late Devonian, but new groups also appeared. The main plants of the early period were horse-tails, scrambling plants, club mosses, scale trees, and ferns. The club mosses of this period are cousins to today's tiny club-moss, but not ancestors; and they had trunks 30 meters high and up to 1.5 meter in diameter. Another type of large tree was ancestor of today's ferns. These continued throughout the period, but late in the period, they were joined by cycads (a new form of 'seed fern') and plants related to conifers.

At least one tall plant (6 to over 30 meters tall) was related to cycads (often mistaken for palm trees) and conifers and are thought to have lived in swamps. True conifer trees appeared later in the period and preferred higher, drier ground.

During this period, animals and bacteria had great difficulty processing the lignin and cellulose that made up the gigantic trees. After the trees died, they piled up on the ground, occasionally becoming part of long-running wildfires after a lightning strike. Others very slowly degraded into coal. White rot fungus was the first living creature that could process these trees and break them down.

Animal life was well established by now. Amphibians were diverse and common by the middle of the period, the dominant type of land vertebrates. Some were as long as 6 meters, but most were probably about 6 in (15 cm) in length. Some were aquatic and lived in rivers, while others may have been semi-aquatic. One branch of amphibians would eventually evolve into the first solely terrestrial vertebrates. The cooling climate slowed the evolution of amphibians, who could not survive as well in the new conditions.

Insects, spiders, crustaceans, and others were also very common, and many were much larger than those of today. The atmospheric content of oxygen reached its highest level in Earth's history—35% compared to today's 21%—which allowed the land invertebrates to get so large. There was a millipede-like creature that grew to 8.5 ft (2.6 m) long. Startling to come across, but if you could kill it, there should be some meat on all those legs. This was the largest known land invertebrate of all time. Among the insects, there were the griffinflies, which included a dragonfly-like insect with a wingspan of 30 in (75 cm). This was the largest flying insect ever to roam the planet. Many other insects flew and crawled about, including cockroach ancestors.

Reptiles, however, prospered due to specific adaptations, such as the amniote egg, which allowed the laying of eggs in a dry environment. Some of the small lizard-like animals gave rise to many descendants, including reptiles, birds and mammals.

I wanted to include a statement about the marine animals of the time, but that section of the article was mostly full of names and little else. I did gather than sponges were fairly prolific and diverse. Also sharks evolved into a multitude of shapes and sizes. Although sharks were mostly sea creatures, there was one type that would sometimes visit swamps. At least one marine fish explored river outlets, and fresh-water fish were common in rivers.

During the latter half of this period, there were glaciations, which meant low sea levels. The cooling and drying of the climate led to a minor extinction event at the end of the period. The tropical rainforest fragmented and then was devastated by climate change.

 

https://en.wikipedia.org/wiki/Carboniferous

Velociraptors

Velociraptors lived about 75 to 71 million years ago. There are 2 known species, both from Mongolia. The second species was only discovered in 2008.

They were depicted in the Jurassic Park movie as swift bipedal reptiles with a long tail and an enlarged sickle-shaped claw on each hindfoot, 6 1/2 feet tall and weighing about 180 pounds. Not so, say the scientists. They were bipedal reptiles, they were fast, and they had the fearsome claw. But they also had feathers, and were actually the size of a turkey. The raptors depicted in the movie series were based on a related genus, because the script said they had to look suitably fierce.

Instead of being 6.5 feet tall, velociraptors were as much as 6.75 feet long, snout to tail tip. Scientific artistic renditions show a very long, feathered tail. They were about 1 ft 7 inches high at the hip and weighs about 33 lbs. Although bipedal, their body and tail were roughly parallel to the ground. Their forefeet were also feathered, but were too short to serve as wings.

Their skulls grew up to 10 in long. The jaws were lined with 26-28 widely-spaced, serrated teeth on each side, more strongly serrated on the back edge than the front.

Their hands were large, with 3 curved claws. However, the structure of the wrist bones forced the hands to be held with palms facing inwards and not downwards.

On their feet, the first toe was a small dewclaw, and the 2nd held the ferocious claw spoken about earlier, which could get 2.5 inches long along its outer edge. Only their 3rd and 4th toes were used in walking or running. Although some beliere their 2nd toe claw was used for disemboweling prey, tests have proven it was most likely used for stabbing and holding, to keep their prey from escaping.

If we’re going to compare fiction to fact, then we must consider the depiction in the Jurassic Park movies of velociraptors hunting in packs. Although there are some indications of other species in the family hunting in packs, there is little to no indication in the fossils of velociraptors doing it.

Most of the known velociraptor fossils have been found in current desserts, under conditions that indicate the locale at the time of their death was also arid and covered in sand dunes, or possibly a little less arid.

Now, my first thought about incorporating velociraptors in a story involves a comedy-ish story where a town in the desert is suddenly overrun by predatory turkeys, which turn out to be—according to the local Wise Guy—descendants from velociraptors, long thought extinct these millions of years. Of course, once the raptors ate up all the local cats, dogs, and chickens, they would necessarily start picking on larger prey... large dogs, wolves, goats... children? Alas, I don’t do horror, which is where this thought is quickly leading me. Anybody out there have any other ideas?

https://en.wikipedia.org/wiki/Velociraptor

https://www.livescience.com/23922-velociraptor-facts.html

https://www.nhm.ac.uk/discover/velociraptor-facts.html

Rhynchosaurs

Imagine a reptilian pig with a hammerhead, no visible ears, and a parrot-like beak, and you'll have a pretty good mental picture of a rhynchosaur.

Rhynchosaurs were herbivores that in some fossil localities account for 40 to 60% of the specimens found, making them the most abundant plant eaters on land. They were reptiles with stocky bodies and a powerful beak.

Early forms were small, less than a meter long, and typically lizard-like in build. They had narrow, wedge-shaped skulls with a few small, blunt teeth for eating plants.

Later versions grew up to two meters in length. The skull in these later forms were short, broad and triangular, becoming much wider than long, giving them a somewhat hammer-head appearance, although the eyes were set close together, near the top of the beak. The broad skull accommodated powerful jaw muscles that enabled the rhynchosaurs to cut up tough plant material. The teeth were modified into broad tooth plates, and the lower jaw fit into a groove on the upper jaw, enabling the ‘cutting’ of plant fibers.

The hind feet were equipped with massive claws, presumably for digging up roots and tubers, although digging claws are usually found on the front feet. Like many animals of their time, they spread all across Pangea, and thus across the world.

And that seems to about all there is to say about the rhynchosaurs. They lived during the Triassic era (251 to 199 million years ago), dying out just before herbivore dinosaurs appeared.

I think I would have found rhynchosaurs terrifying, particularly the larger ones, even though they were basically reptilian cows or deer. Let’s face it, the larger ones were as long as a man is tall, and who’s to say they wouldn’t try munching on this new plant called human that invaded their space, even if it didn’t sit still like other plants?

What do you think? If you had a time machine, would you venture back to visit them up close and personal?

 

https://ucmp.berkeley.edu/taxa/verts/archosaurs/rhynchosauria.php

https://en.wikipedia.org/wiki/Rhynchosaur

A Brief Study of Euramerica

Sometimes it’s called Euramerica, sometimes it’s known as Laurussia (not to be confused with Laurasia). It’s called a minor supercontinent because it consisted of several (3) cratons, which are pieces of crust that include land.

About 410 million years ago, the Laurentian (most of North America), the Baltica (Baltic states) and Avalonia cratons all slammed together to form Euramerica. Avalonia was the smallest of the 3; a microcontinent that was long and skinny and sat along the southern border. Euramerica appears to have sat pretty squarely on the equator and was mostly covered with tropical rainforests.

Around 300 million years ago, the climate changed rather abruptly. Many of the lycopsids - such as clubmosses - were replaced by ferns. There was a great loss of diversity in amphibians while the reptiles diversified.

Later, Euramerica became part of the major supercontinent Pangaea. When Pangaea broke into two continents - Gondwana and Laurasia - Euramerica was a part of Laurasia.

Eventually, Laurasia split into the continents of North America and Eurasia. The Laurentian craton became a big portion of North America. Baltica became part of Eurasia. Avalonia ceased to be a long skinny microcontinent as bits of it became some of the east coast of North America, and bits became parts of Ireland, England and other areas of southern Europe.

https://en.wikipedia.org/wiki/Euramerica

https://en.wikipedia.org/wiki/Avalonia

The Malagasy Dinosaur

When I first read the name Malagasy Dinosaur, my eyes rearranged the letters and I thought I had read “Madagascar Dinosaur”. Then I thought, Of course not. Madagascar isn’t big enough to have had a population of dinosaurs.

Well, it turns out Madagascar is big enough. I guess you can’t judge a place by how it looks on a map. Especially not when it’s snuggled up next to a continent as big as Africa.

Madagascar is an island, and it’s believed it separated from the super-continent Gondwana about 85 million years ago. It has plenty of wildlife of some pretty strange species, as evolution has worked to fill all the niches in the food chain. Fossils found on Madagascar seem to indicate it’s had some strange species for a long, lo-o-ong time. Here’s some samples:

Beelzebofus antinga, an extinct frog that weighed up to five kilo (11 pounds). It is the heaviest extinct frog ever known. (Okay, not a dinosaur, but still…) If they were still around, maybe they’d be raised as food, like a chicken?

Rapetosaurus krausei was a dinosaur that reached 15 meters (49 feet) in length. It walked on all 4 feet and had a small head on a very long neck. It was a vegetarian, so I suppose we’d only have to worry that it might step on us, if we’d been alive at the same time as it.

Rahonavis ostromi was about 50 cm (19-20 inches), wore feathers over its entire body, had claws, a long skull and a mouth full of sharp teeth. Could this be the ‘missing link’ between dinosaurs and birds?

Sinosuchus clarki looked somewhat like a modern crocodile. Kinda. Except it was less than 80 cm (32 inches) long, including a short, broad head and a short tail. It also had teeth perfect for grazing on plants, and bone plates under its skin to protect it from predators.

Speaking of crocodile-like dinosaurs, the Araripesuchus tsangatsangana looked a lot like modern crocodiles, except it had much longer legs.

But none of these interesting creatures were the one called the Malagasy dinosaur. Only the Majungasaurus crenatissimus bears that nick-name. The Malagasy looked similar to a Tyrannosaurus rex, except it only reached a length of 6 to 8 meters (19 to 26 feet) and probably only weighed a ton. Even though it was so much smaller than its cousins, scientists say it took 20 years to reach its full size, so it grew much more slowly than the others, also. They made that discovery by studying cross-sections of several bones from a nearly complete skeleton found in 2003. The bones had marks of annual growth, rather like trees have tree rings. Of course, some bones had marrow in the center, displacing the earliest years’ record of growth. Other bones were hollow, and many of the bones were carved in order to reduce the creature’s weight.

The Malagasy lived 66 to 70 million years ago. However, it seems to have links to dinosaurs in south Asia (India) and South America (Argentina). So, could it be that Madagascar clung to Gondwana longer than was thought?

http://www.madamagazine.com/en/die-dinosaurier-von-mahajanga/

https://www.msn.com/en-us/news/science/fearsome-malagasy-dinosaur-remained-a-pipsqueak-most-of-its-life/ar-AAksFEa

Ick! It’s an Ichthyosaur!

Ichthyosar means “fish reptile” in Greek. Fossils reveal that they appeared about 250 million years ago, and one branch lasted until 90 million years ago. Their ancestors were some unidentified land reptile that decided to return to the water and become fish-like, much like dolphins and whales.

Science became aware of ichthyosaurs in the early 1800s when the first complete skeleton fossil was discovered in England. Later that century, many more Ichy fossils were found in Germany, and some of them included soft tissue remains. (No longer soft, after being fossilized, of course.)

Ichys ranged from 1 meter to over 16. Some resembled modern fish, others looked more like dolphins. They had pointed heads and often pointed teeth. Some could and did attack large animals that wandered into reach. They had large eyes, probably so they could dive deep. Their legs had completely converted into flippers, although many species’ flippers had numerous digits and phalanges (bones of the digits). They were not really fish, because they breathed air, gave birth to live offspring (up to 11 at a time), and were warm-blooded.

Life as an ichy was not all hunting and reproducing. One fossil had bite marks on its snout, apparently from one of his own kind. The bites had started to heal, so it survived the attack, but was this common? Or had he/she really made someone angry? Another fossil was complete… except for its tail. The theory is that it was ambushed by another of the big ocean predators, which bit off its tail. That ichy – unable to swim – sank deeper, drowned, and eventually became a fossil.

At one of my jobs, they decided to install an aquarium. If you want a healthy aquarium, you need a bottom feeder, usually a catfish. The fish they got included a bottom feeder, probably some type of catfish, but I thought it was ugly; flat bottom, thick whiskers, brown with black spots on skin that looked slightly fuzzy. I wound up calling it ‘Ichy’. I was familiar with the name, but didn’t realize they had all died out long ago. And since this fish didn’t actually look anything like an Ichthyosar, the name really didn’t fit.

I feel sorry for that poor bottom-feeder, now. I grew to rather like him, but I still called him ‘Icky’ (my pronunciation). It really wasn’t fair. I’m sure others of his species – whichever one he belonged to – thought him quite acceptable.

https://en.wikipedia.org/wiki/Ichthyosaur