Epona may not really exist, but it�s certainly a good example of how scientific principles can be used to imagine worlds and beings that might exist!
Figure One: A computer generated Eponan landscape offering a view from one of Epona�s warm temperate regions. The umbrella leafed �plants� are pagoda trees, and are grouped in the phylum Myophyta.
Epona is a strikingly detailed fictional alien world. How detailed?
The genesis of Epona came from a project created by members of
After taking part in a COTI session, people sometimes mentioned that three days was not enough time to significantly develop an alien world and culture. In response, at Contact X, it was decided to build a world over three years. A regular newsletter for the Epona project was created, inviting
Epona is the third world of nine which circle the star Taranis, originally 82 Eridani. Taranis is a yellow dwarf (G5 V main-sequence) star that is roughly 5 billion years old. As its original name implies, the star resides in the constellation Eridanis, and currently drifts in its galactic orbit some 21 light-years from Sol. Names of worlds follow a Gaelic tradition.
The four inner planets of Taranis, including Epona, are terrestrial in nature, being small, ranging from 0.1 to 2.0 Earth masses in size, and having average densities within the range of rock, from 3.8-6.4 g/cm3. The inner two worlds, Belenos and Grannos respectively, are similar to Mercury, with small bodies, high densities and little in the way of atmospheres. The large chunks of rock are tidally locked to Taranis, and Grannos�s long-ago atmosphere has been frozen into carbon dioxide ice on its night side. Epona follows, with a mass of 0.55 Earth�s, an oxygenated atmosphere that averages 0.577 bar at the surface, continents of silicate rock, temperate climate and seas of water. The fourth world, Sucellus, with a high density of 6.4 and mass of 2.0 is a sizable terrestrial world covered in a deep ocean and insulated by a carbon dioxide atmosphere of roughly four bars.
Figure Two: Epona�s family of worlds. Unlike the Earth, which holds the number one spot in size for terrestrial worlds in the Solar System, Epona is only the second largest rocky planet in the Taranis system, and, only massing about half that of the Earth, Epona has experienced significant internal cooling. As explained in the text, failure of the carbonate silicate cycle due to Epona�s solidifying mantle has significantly affected the climate, and subsequently biological evolution.
The next four planets are a family of gaseous giants, with huge masses, from 5.9 to 206 Earth�s, and light densities, all sitting around 0.7-2.4 g/cm3. The fifth world, Rosmerta, is the smallest of the family, a mini gas giant with a viciously hot world-encircling ocean being sustained under an equally challenging atmosphere that exceeds 1,000 bars in pressure. The small gas giant is followed by the largest, Borvo. Borvo is 65% the mass of Jupiter and is similar in nature, producing a powerful magnetic field, tightly holding a vast array of moons and presenting a surface of seething storms. Bormo, world number seven, is similar to Uranus, even possessing a strong axial inclination of 73 degrees. Bormanus, the eighth planet from Taranis, is similar to Saturn in density and mass. This icy-ringed world follows the most elliptical path of Epona�s sister planets, maintaining a mean eccentricity of 0.16.
The final world, Sirona, is Tritonian, being comprised of ices, though it is more massive than Mars. Occasional cryovulcanism maintains a thin atmosphere of nitrogen, methane and hydrogen.
Epona accreted a similar distance from Taranis as the Earth did the Sun, so the composition of the two worlds is quite alike. Epona has a lower abundance of heavy elements, accounting for a lower density. During the first 3 3 billion years of existence, Epona possessed a liquid iron-nickel core, a convective mantle and shifting lithospheric plates.
Epona�s tectonic activity did not last as long as it has on the Earth. Being a smaller world, Epona has a higher surface-to-volume ratio than the Earth, and thus has had its store of internal heat dissipated at a significantly faster rate. Nearly two billion years ago, Epona�s tectonism began to slow, and later froze up completely as the lithosphere continued thickening. Many types of mountain building stopped, and continental masses simply weathered and eroded away.
Highly weathered continents are OK as far as Epona�s biome is concerned, but breakdown of tectonism has one major side effect for life. Epona�s dead geology severs the important carbonate-silicate cycle.
In a �normal� state of affairs, as on Earth, carbon dioxide in the atmosphere combines with water to produce carbonic acid. This carbonic acid falls as rainwater and breaks down continental rock�a major feature of weathering. Bicarbonate ions, HCO3 (-), created by the chemical weathering, wash down the streams and into the oceans. In the sea, these ions reach saturation and precipitate from the ocean as carbonate ions, CO3 (2-), and accumulate in vast seafloor deposits, or are used by some animals to create hard shells.
Once converted to rock, the carbon atoms cannot escape, except by subduction. As the seafloor is pushed underneath the world�s numerous lithospheric plates, heating eventually releases the carbon as a gas again, which finds its way back into the world�s atmosphere via volcanoes and sea-floor spreading margins, where the cycle starts anew�
Except when subduction and volcanism fail, as with modern Epona, dropping carbon dioxide production to bare minimum as outgassing ceases. Lose one tie in a loop, and the entire system crashes, so to speak. No more CO2 for Epona.
All the world�s carbon dioxide will be lost when tectonism fails. How does this affect life? Very simply, and very profoundly. The carbon dioxide in the atmosphere provides Epona a buffer against a changing amount of sunlight from Taranis. See it this way: As a main sequence star ages, it becomes
The amount of carbon dioxide taken from the atmosphere depends on the amount of water that is being evaporated from the seas, because one needs water to make carbonic acid. An early Epona receiving less sunlight will have less evaporation, which means less rainfall. Less rainfall means more CO2 molecules left in the atmosphere and we all know what more CO2 means: greenhouse effect. A good quantity of CO2 equals a warm and equitable habitat for life. As Taranis grew brighter with time, the amount of evaporation on Epona increased, making more rainfall and taking greater quantities of CO2 from Epona�s atmosphere. With less greenhouse effect over time, the climate maintained fairly even in temperature�until a few eons ago.
Kill tectonism, and the production of carbon dioxide stops entirely. In a few tens of millions of years, much of the available CO2 becomes chemically bound to Epona�s crust. Freeze time.
At the beginning of the new low carbon dioxide era for Epona, some 1.7 billion years ago, her previously equitable climate eroded into the cold clasp of a prolonged ice
Epona�s internal heat has not completely dissipated. Enough warmth has remained to produce residual bouts of terminal volcanism every one hundred million years or so, give or take an epoch or two. These huge plagues of eruptive activity release vast quantities of CO2 back into the atmosphere, providing a new greenhouse effect and an initially abundant carbon source for photosynthesizing life.
Under this warming trend, the ice retreats, and land areas previously covered in glacial ice become exposed for repatriation by life. The volcanism spike is short-lived, say a few million years, and the warm periods only last ten to twenty million years. Long enough for terrestrial life to radiate and become established, only to be choked from the continents as the C02 steadily drops, allowing Epona to ice over yet again.
Epona has experienced at least twenty of these glacial events in the last 1.7 billion years, and is at a warm period�s end right now, in our mod-ern era. Much new aerial, terrestrial and aquatic life has evolved during this most recent ten million years of equitable clime.
Much is known about the Tir fo Thuinn region of Epona, an ancient, flat, tectonically dead continental craton that has been weathered by rainfall and glacial action for at least one billion years. Due to space constraints, we�ll only look at the primary microfauna, megafauna and megaflora of Tir fo Thuinn. A very detailed aquatic realm, one terrestrial animal class, and at least two kingdoms of photosynthetic metazoans are being left out. The organisms described below are a world-wide presence, however, so Tir fo Thuinn provides a good opportunity to show some of what lives in the Eponan countryside.
Figure Three: Modern Epona. Many of the names for the large landforms follow a Gaelic tradition. Tir fo Thuinn, meaning �land under the waves� is also called the Sunken Continent. Tiene Eilean (Fire Island) is the most recent addition to Epona�s landmasses, having been produced by Epona�s latest convective bulging (not unlike the Tharsis region on Mars) and sudden bout of atmosphere warming volcanics beginning some ten million years ago. Large plumes of ejecta still billow from Tiene Eilean�s massive 10 km high volcanoes about every century or so.
Kingdom Archaeanimalia contains those Eponan animals possessing a somewhat Earth-like morphology and physiology, namely the silacopods, springcrocs and the flectocellids. Nevertheless, do not let these words fool you into thinking that mammals and reptiles are running around on the surface of Epona. Quite the contrary. Though the archaeanimalia have some similarities to Earth critters, such as internal mineralized skeletons in the case of springcrocs and external skeletons in the silacopods, there are no vertebrates, and members of the existing archaeanimalia classes are quite different from anything existing on the Earth.
Silacopods are a class of segmented organisms ranging from ant to gazelle in height�Epona�s lighter gravity seems to be aiding the larger forms. Silacopod bodies are supported and protected by an exoskeleton of silicon dioxide, basically glass. Respiring through solid silica is difficult, so the stem species had a pair of breathing stalks, which resemble antennae, on each of its ten segments. Being structured somewhat like a centipede, the basal species also had a pair of legs attached to each segment.
Figure Four: A nailbug, dread of the bare-footed walker. The tail, which is actually the reproductive organ, is shaped like the creature�s head, a mimicry which further aids the nailbug from predators by causing confusion. Not all carnivores are deterred by the spines and tricked by the tail, however, and one line of silacopod predators smashes the nailbug�s hard shells with limbs modified into heavy clubs.
All known silacopod species have evolved from the basal centipede form and are modifications of it: usually having fused many of the segments into three significant body parts and reducing the legs to four, two on some occasions. Thus, many of the critters appear to have an inordinate amount of antennae on each major segment, when in reality, these organs aid in respiration. Modification to the numerous limbs is common, with typical products being the creation of liquid-filled spines for sensing sound and grasping organs like those used by some arachnids and crustaceans on the Earth.
Silacopods have filled a variety of ecological positions throughout the terrestrial reaches of Epona, though the greatest variety of critters are found in the tropics of Tir fo Thuinn, and on an isolated chain of islands found far east of the continent�s mainland, called the Chirping Chain. Indeed, the Chirping Chain holds some of the most exotic species, including nailbugs, a herbivorous lineage that forms vast, ground-covering herds. Tall, sharp siliceous spines protrude from the back, making for a painful bed of nails for any soft-footed creature to walk upon.
Figure Five: The snapping flower commonly hangs from Epona�s vegetation, waiting for small flying critters to fly past, often avian pentapods. Like a chameleon firing its tongue, the snapping flower catapults its powerful clamlike jaws on a long, single leg, quickly plucking items from the air. Digestion is slow, with fluids filling the cavity made by the hard shells, not too unlike a Venus�s fly-trap.
The springcrocs are, well, weird. Looking somewhat like a singlelegged clam in their basic form, one would hardly guess that they rate amongst the most vicious predators on Epona. All springcrocs acquire food by hiding and then pouncing upon a hapless prey item that has wandered near. The leap is achieved by using the single, flexible and wellmuscled leg. Prey are usually killed with the springcroc�s clam-like jaws, though some use poison.
Many of the springcroc species live only in swamps and marshes, where they tend to hide under shallow water in wait for a prey item to come for a drink or wander near. Once captured, the meal is taken underwater for slow consumption, with some of the chemical reactions during digestion providing oxygen for the springcroc as it feasts. Digestion is carried out inside the two shell halves, a region which serves as the creature�s stomach.
Figure Six: The entire mantel of the giant snail is capable of digestion, though some cells are better at it than others. Even if one were to grasp the snail�s eye-stalks, the cells would convert and one would begin feeling a tickling as their hand slowly became consumed. Aside from their usual transfer of reproductive cells, giant snails can reproduce parthenogenically: That is, a small piece torn off of the parent body, if given nurturing moist conditions, will quickly grow a shell, small eyestalks and begin its life as a new snail.
Class Gastrognatha has derived significantly, and contains species occupying a wide range of niches. One of the most abundant clades is the snapping flower, which oftentimes hang from pagodas on their long, thin legs, with their clamshell mouths wide open. Fleshy growths in the mouth mimic brightly colored ar-chaeplants, tricking would-be herbivores into becoming a meal for the little springcroc.
This class is best represented by the giant snail,
For reproduction,
Figure Seven: Extensile muscles work by extending, as opposed to the contracting muscles of Earth fauna. Aside from offering mobility to the organism, extensile muscles also act as the entire skeleton, giving the animals a strong degree of flexibility. All organisms in Kingdom Myoskeleta have this soft dual muscle-skeleton. Even Epona�s primary �plants,� called pagoda trees, have extensile muscles, albeit in primitive form.
The myoskeletal kingdom consists of organisms that do not possess mineralized skeletons. Instead, their bodies are supported by continuous lengths of osmotic muscle called extensile muscle rods, a combination skeleton-muscle which makes the organisms very flexible. These muscle rods can extend forward and backward, as well as twist through differential activation of muscle cells. Joints are not needed, for they can be created �on the fly� by animating the proper cell groups. The basic body plan built around the osmotic muscle skeleton consists of a barrel-like midsection with five muscle-rod limbs protruding from either end. The tips of the five limbs are then further divided into three smaller digits. What can such a simple body plan accomplish? A surprising amount.
The kingdom is broken down into two phyla, the myophyta, which consists of photosynthetic organisms that reside in plantlike niches on Epona, and the pentapoda, which has produced a host of animals highly derived from the basic body plan described above.
Figure Eight: Variants of the simple pagoda form depicted here can be found all over Epona, though the greatest diversity exists on the Sunken Continent. A number of tropical pagoda species are able to achieve heights similar to Earth trees, while some ground covering species have leaf diameters less than a centimeter. A subgroup called neopagodas has developed a branching method of growth with some trees making beautiful palmate fractal growth patterns.
These photosynthetic organisms, which have evolved from a tiered seaweed, have a very simple form: The previously mentioned barrel is often carried upright, like the trunk of a tree, and the five limbs on one end are sunk into the ground, like roots. At the top of the barrel, the other five limbs have evolved into a large umbrella leaf, so that a single tiered member of this phylum looks somewhat like an oversized mushroom. Five to fifteen spines, derived from the tridactyl nature of the muscle rod limbs, support the leaf, like the arms of said umbrella.
This �plant� form, known as the pagoda tree, is not restricted to one tier. A new barrel and associated leaf can be cloned from a growth bud that exists in the center of the leaf, quickly adding another level. Growth can continue, carrying pagodas to great height. Some myophytes are capable of branching via a polyembryonic method, effectively multiple cloning, though this tends to be simple and is usually carried out in twos, threes, or fives. Though the branching forms share many features with the pagodas, they are not the same, and are called neopagodas.
There is no wood on Epona. The carbon dioxide required for the wood-making process was not available for the pagoda�s tiered seaweed ancestors, and the terrestrial myophytes have maintained this ancient carbon-conserving trait. Pagoda stems are held rigid by the osmotic pressure in the extensile muscle cells. This osmotic muscle characteristic gives the pagoda animal-like freedoms. Trunks are very mobile, and they easily track the sun. Tendrils and stems can wrap around a support while one is watching. As a storm nears, pagodas can detect the dropping atmospheric pressure, and lift their leaves up or drop them down (like skirts?!) in an effort to protect the large photosynthetic structures from high winds. A natural and striking barometer! Occasionally pagodas will shrug off an unwanted visitor, like an avian myoskeletal critter who�s landed on the myophyte for a hearty meal.
Figure Nine: The pentapod respiratory system is one way, with air coming through the mouth, and waste gases being expelled through pores in the skin. With this unidirectional airflow, pentapods have a much simpler organ system than Earth vertebrates, as they do not require lungs. The muscles operating the windsack also drive the circulatory system, further simplifying pentapod internal anatomy.
Strongly cold climes and pagodas are usually not a successful combination. Having no bark for protection, the winters kill myophytes off by the billions, whole forests decimated by a single hard freeze. However, Epona has a very thin atmosphere, and even in the tropics at sea level the temperatures tend to drop toward freezing during the night. To combat this problem, pagodas produce various alcohols as antifreeze. Be careful with your campfires.
Silacopods like to eat pagodas, as do myoskeletal animals. Pagodas, in most instances, can�t run away. Disliking growing holes in their leaves, pagodas have established a defense routine similar to Earth flora: chemical warfare. Silacopods aren�t the only reason for a poison defense, for pagodas also have each other. Carbon dioxide necessary for photosynthesis is rarefied even on modem Epona, and pagodas have very large leaves to absorb enough of the life-sustaining gas. Those dome leaves require much space. To create room, the myophytes diligently spend energy making pagodacides to keep near relatives away. Toxin differentiation is so detailed, in fact, that it is the most effective characteristic to use when identifying species, since many pagodas look quite alike morphologically.
Figure Ten: Ceretridons are a diverse group, with many assuming a pagodivorous roll. Being nearly four meters tall, the twintails depicted here feed from large pagoda trees, and perform saltatory north-south migrations in vast herds, responding to the sharp seasons of the Sunken Continent�s southern extremes. The herds are thought to offer protection for the single springtime young born to each individual.
Figure Eleven: A swiftgrasper pursuing two rodent-sized pagoda runners. In parallel to Earth mammals, many ceretridon lineages have developed teeth specialized to their task of survival, probably due to their very conserved morphology. The swiftgrasper has two long, sharp teeth that it uses to impale prey snatched up by its swift mouthpart limbs. The lesser teeth are used to masticate an opening in the skin of its victim, where the internal fluids and organs are sucked through. Lacking true jaws, many predatory ceretridontids have a difficult time eating the tough musculature of their prey.
Figure Twelve: The small pet rock is a member of the rare quadrupedal ceretridons. The �tail� is actually the rear, or third, leg on more typical ceretridons. In the case of the pet rock, the limb is used for holding its silacopod prey for consumption. Often, the pseudo-tail is held underneath the animal and cannot be seen from above.
In pentapods, the basic myoskeletal barrel contains all the vital organs, including the brain (housed in a region of collagenized muscle rod [basically tendon]), and the sensory apparatus, which consists of four eyes, two ears, and a third ear located on top of the head that serves as a sonar sender/receiver.
The barrel also houses the respiratory organ, a chamber created by a sheath of muscle rod, forming a hoop-like structure. Two lesser rings of muscle rod sit at either end. Air enters through the mouth, and the muscles sequentially pump it into a network of self-similarly branching bronchi. Upon reaching the lowest level of branching, the alveoli, oxygen is absorbed directly into the muscle (and any aerobic organs) from the airstream. At the same level, carbon dioxide and water are expelled, being carried through a number of tributary paths before being �exhaled� from pores in the skin.
Reproduction is achieved by an exchange of spoor through the mouths of two individuals. The spoor travel to the back of the respiratory pump, where they fertilize a tiny bud. Since individual pentapods have both spoor-producing and bud-producing capability, both participants will get pregnant (no gender roles here), a sort of hermaphroditism. The embryos develop in the budding zone at the back of the respiratory pump, remaining attached to the cavity wall. Birthing is achieved by coughing up the newborn before it becomes too large and obstructs breathing. Since pentapods do carry an entire complement of reproductive organs, they can reproduce parthenogenically, though this only happens rarely, when the organism is under great stress.
The pentapod phylum has produced at least two well-known major groups on Epona, the ceretridons and avians. In a several-million-year radiation similar to the Earth�s Paleocene Era, both groups have diversified significantly in the past ten million years, and contain many species.
The pentapod�s simple form has been modified significantly in the ceretridons. The barrel has elongated and grown larger, housing a massive digestive system, and has become fenestrated to reduce weight. A headlike structure exists at the front end of the barrel, though it houses only the sensory organs�the brain is still deep within the original barrel. The sonar ear is practically nonexistent, for it has atrophied in favor of eyesight. All ceretridons utilize their four eyes, with many having a pair aimed forward for binocular vision and a pair aimed upward to spot aerial predators. At the front of the head is a simple mouth that has four to twelve conical, chitinous teeth and a single tongue. The teeth represent the finger terminations on what would otherwise be four of the standard five pentapod arms originating from the front of the barrel. The tongue is the fifth limb. Five other limbs originate from the back end of the barrel. Two arms are carried forward, often inside the body, so that they protrude from the sides of the head, and are used for grasping. The other three limbs trail behind and are the animal�s legs, hence the �tridon� in ceretridon. However, there are thousands of species of ceretridontid, and many locomotory patterns have evolved among them: monopedal, bipedal, tripedal, and even quadrupedal and pentapedal (using the �arms� by the head). The class has also produced herbivores (actually pagodivores), carnivores, scavengers, and parasites along with the different leg numbers.
Figure Thirteen: A large predatory avian banks from an incoming thunderstorm. Avians, often feeding on terrestrial pentapods, are the driving force behind the ceretridon�s extra two upward-facing eyes. Swift and very strong, avians prove remarkably lethal to any animal caught unawares, often using sharp tipped �talons� of chitin on the tips of their mouthpart limbs as spears. Despite Epona�s thin atmosphere, soaring avians such as the one depicted are efficient flyers, often able to glide for hours on end, silently seeking food from altitudes reaching into the hundreds, and even thousands, of meters.
Figure Fourteen:
Pagodivorous ceretridons have to tolerate many toxins in their lives. Most ceretridons, in fact, are only capable of consuming one, or a few, toxins, so the pagodivores tend to be quite specialized, seeking a specific type of pagoda, usually identifying it through taste. Many pagoda eaters store the toxins they consume as a defense against predators, wearing garish colors and patterns as a warning to any lurking carnivores. With their toxin defense, most pagodivores are solitary, or form very small groups. However, a number of migratory herding species do exist in the temperate climes, where their food pagodas die back into the warm temperate reaches every winter. A common herbivore is the twintail, which hops around Eponan forests on a single rear leg, while the two forelegs typical of a tripedal ceretridon are carried over the back and held horizontally as counterbalances against the weight of the body up front.
Because of their prey�s inherent toxicity, many carnivores also tend to specialize, feeding solely on one, or a few, species of pagodivores. Carnivores also tend to be brightly colored and patterned, features for mate selection not too unusual for an animal group with exceptional eyesight. Some carnivores have all four eyes facing forward, establishing a very acute depth perception in combination with their color vision. Carnivore mouth part limbs tend to be very specialized, many having chitinous talons on their fingertips, an aid in prey acquisition. The coyote-sized swift-grasper is an example, having deeply taloned arms held at the sides of the head, ready to snatch prey with a mantis shrimplike speed.
Silacivorous ceretridontids face similar toxin problems, for the silacopods use pagoda toxins for defense. These small ceretridons have the largest teeth relative to body size among their kind, a requirement for crushing the hard siliceous shells of their food. The teeth wear down quickly, and are perennially growing to compensate for the loss of material. A unique example of silacivore is the �pet rock.� This little ceretridontid has developed a rough-looking armor from the hair typical of its kind in a way similar to armadillo of Earth. The armor is perforated, a necessity considering the one-way air exchange of the pentapod respiratory system, yet is quite strong, giving the pet rock much protection against predators. The shelled silacivores are sometimes mistaken for stones when they are clamped up, hence their name.
Avians are similar to the ceretridons in construction, save for a few important aspects. Two of the three standard ceretridon legs have elongated into wings that sit near the head of the critter, while the remaining leg has grown very large, lengthening its three fingers to support another (two-part) broad wing, one that is larger than the other two lifting members. The middle �finger� stretches through the fluke of this large hind wing and becomes a tail. The tail effectively pulls the beast�s center of mass rearward, putting it at the center of lift located in the region of the massive rear wing. A triangular sonar �ear� sits ahead of the eyes on top of the �cranium.� Sonar is the avian�s primary sense, though their eyesight is good. Eyes in avians are often located on the side of the head, giving the creature a 360 degree field of view. Usually the other pair of optical sensors are highly atrophied.
Propulsion is achieved through flapping the two forewings, and lift is generated by the broad hind fluke. This is an effective combination, capable of carrying the animal forward at speeds similar to light aircraft.
Many avians have assumed the role of predator, pouncing upon ceretridons and snatching each other from the sky. There are large predators called the dracowolf, with wingspans over ten meters, that hunt solely by sonar, having atrophied eyesight. Such predators tend to feed on midsized avians, as well as many of the ceretridontids�avians have developed organs that the ceretridons don�t have, and can tolerate a broader range of toxins than their terrestrial brethren. Other predators are small, like sparrows, and flock, attacking prey
One lineage of avians has produced Epona�s sophont, the uther. Singularly the most fascinating physiological trait of die species in the uther line is the interdependence of the parent and neonate. Uther young are born extremely undeveloped, being mainly a football-sized head and body with vestigial wings hanging from one end. The neonate�s nervous system is also relatively undeveloped, save for eyesight, which is nearly as capable as any adult�s. Being placed on the parent�s back in a depression between the two forewings, where a single nipple is located, the neonate drinks a milklike substance for nourishment. Two vestigial fingers, one from each forewing, hold the young securely in place (unfortunately not shown in the illustration). Even with their sideways facing eyes, adult uthers are not able to see backwards very well, and, in this piggyback position, the neonate becomes a rear guard for the adult. A simple reflex response, the neonate will clamp down hard on the teat if a nonuther avian is detected, giving the parent warning of an attack. This symbiosis lasts for about five years, ending when the neonate is able to fly on its own. Having a neonate is of paramount importance to an adult uther, and rarely is an adult seen without one. There are potentially many cultural ramifications of this physiology, though, as with many things involving the uther, the social effects haven�t been explored in great depth at this time.
Utheran cultural evolution is known in general. Early uthers were originally scavengers, flying in widely separated groups to aid each other in finding the rare corpse on the ground. There are a number of predatory species of avian that feed on the uther, and the groups served a dual purpose as some members watched for predators. Such organizing behavior resulted in a complex communicative ability which eventually evolved into language.
Due to the limited nature of the pentapod respiratory system, uther speech is somewhat restricted in scope. Uthers do not have any type of vocal cords, like humans, so are unable to make a similar range of sounds. Instead, uthers sing, or chirp, their words using a simple system of rising and falling high-frequency pitches. Sentences end with a simple marker note of a specific frequency, so that the uther �singing� is interrupted periodically with this somewhat random �beat.� Uther writing looks like stock-market graphs, with the lines showing the rising and falling of various note arrangements for each word.
Having the typical weak chitinous teeth of pentapods, the scavenging and speaking uthers were not well, suited for the task of eating raw meat. With their strong need, uthers eventually created cutting tools in order to process food easily. Sharp tools led to hunting, and a new lifestyle. One ramification of predatory uthers was direct competition with a number of large aerial carnivores, and many megaavian species slowly disappeared as the uther improved on its weapons technology. Indeed, avian species that fed primarily on the uther were the first to be eliminated from Epona.
Created by a need for watching their prey herds very closely, uthers learned animal husbandry. Maintaining the nomadic lifestyle of their scavenger ancestors, uthers initially followed ceretridon herds around guarding them from carnivores, both terrestrial and aerial. As uther populations grew, violent encounters with other bands increased, and a need for territory arose. Uthers created permanent settlements, at first in pagoda trees, to maintain control over specific lands. Under this close protection the herds grew, and quickly denuded the lands. As agricultural methods were developed to feed the voracious herd animals, full-fledged civilization resulted, with an accelerating technological growth.
The paragraphs above summarize only a few aspects of Epona, a tiny glimpse at a world that is very complex and detailed. Fortunately, for those who are interested in seeing more of Epona, there�s an effort to depict the planet in its own publication(s). Epona is no longer restricted to