~Hi All! i realized i've shown only small snippets of the world map of Demeter and figured i'd give a full tour from the perspective of prospective researchers interested in seeking a posting there. For now this is just an early draft, but i would enjoy expanding on this for each location if it turns out there’s some interest regarding it. Let me know and enjoy the view!
((also, please ignore the name-drops of specific researchers, i'm a big fan of the Expanse by James S A Corey and i wrote these briefs from the perspective of it being framed as a world in the gate-network under early exploration. Regardless this is all origonal work and not fanfiction, it was just something to help me picture my world through the lense of human researchers.))
We will move Northeast to Southwest by locational posting. Read closely for the available opportunities at each posting to find which best matches your respective discipline, specialization, and psychological profile. Not all postings are well suited to those fitting certain predispositions, and whatever posting you are assigned is likely to last for several months to years, so be certain to read your employment contract carefully and link your psych evaluation along with your resume.
With all that out of the way, welcome prospective and applying researchers! read on to see the career opportunities that are available to explore during your time on:
Planet Demeter
Cichol’s Throne (A shallow sea of reefs and “false-kelp” forests in the polar northwest of demeter) (rich in silicates and phosphates, lead and nickel is abundant)
This nutrient rich shallow sea hosts a number of reefs dominated by manganese, zinc, and arsenic phosphates. They are brought here by upwellings from balor’s castle carried further by oceanic currents. This (excluding the arsenic) houses one of the safest locales for marine biologists looking to study the marine ecology of demeter without the near year-round storms of the Dionesyan Goblet. The high latitude of this location makes it exceptionally protected from UV for half the year compared to the more equatorial postings. It also offers close access to the head-offices of HR in the north pole depots, and regular visitation and collaboration with both the teams of the Balorian Hydrothermal Fields and Connand’s Inverted Tower. This gives researchers a look at a range of different aquatic habitats for those stationed here.
Balor’s Castle (Hydrothermal Fields; White, Rainbow, and Black) (Rich in copper, barium, iron, strontium, and arsenic) (Stretches from the northern temperate to south of the equator, west of the westernmost landmass)
These undersea hellscapes are composed of three hydrothermal fields:
Cethlenn’s Ill Portents
This field is the oldest of the three, initially formed 250 million years ago and rapidly dying out. It is a black smoker field formed from tectonic rifting as the landmass that eventually collide with another to create “emerald Olympus” and the Atlas Isles, move eastward, exposing fresh mantle beneath it. However, like any black smoker field, it is short-lived, and gradually dies out as the plate migrates further and further. Hence the name, a warning that hints and the fragility and short lifespan of the energetic activity that makes this habitat so favorable to extremophilic life on demeter.
Rich in: iron, lead, arsenic, manganese oxides, zinc sulfides, silver,
pyrite, chalcopyrite, galena, todorokite, Birnessite, Manganite, sphalerite, and others.
Lasts: 1,000-10,000 years per field
Balor’s castle
This is what is called a “Rainbow Hydrothermal field,” the rarest type on earth, but rather common on demeter due to its strange chemical make-up and resulting geology. On earth, rainbow fields are produced by a process called “serpentinization,” where newly exposed magmatic rock on the ocean floor undergoes immediate chemical change to magnesium-rich minerals, generating significant heat and the release of hydrogen from the chemical reaction. Naturally the lack of magnesium on demeter makes the inclusion of this type of field on demeter questionable, but the abundance of reactive copper and manganese will replace it. In addition, these types of fields, when found on earth, are the most abundant in the rare elements that we have highlighted as relatively common on demeter, so they are significantly more commonplace here.
Rich in: copper, manganese, sulfates, uranium, phosphates, silicates, thorium, titanium, nickel, vandium
bornite, Manganosite,
Lasts: 10,000-100,000 years per field
Ethnui’s Inheritance
This is a long-lasting white smoker hydrothermal field, due to the slower tectonic activity that formed it, supplying ample opportunity for native habitats to form. These types of fields can last millions of years, sustaining stable environments for slower forms of life, and a greater understanding of the most stable of demeter’s native habitats.
Rich in: Copper, silicates, barium, strontium, carbonates, gallium, chlorine
Lasts: 100,000-1,000,000 years
This posting is divided between time spent at the terrestrial facilities at the Silver Spine, and the aquatic bases situated near Cichol’s Throne. These workers have trouble adjusting to their posting, as it requires constant back-and-forth between the two, and foster hostility as outsiders who never truly incorporate into either stationing. It is also one of the most fascinating locations to investigate, so there is an underlying resentment that fosters that animosity that Balorian researchers experience. They are also only third to the Womb of Mefetis and Ogma’s Canal in terms of funding and resource allocation, deepening that resentment that those whose facilities they take up the space of often demonstrate.
Silver Spine (Equatorial-North Temperate Desert Basins and Mountain Ranges) (narrow continent rich in silver and lead)
This narrow Landbridge is rich primarily in five elements: silver, arsenic, barium, lead, and copper; bound together in a resinous matrix rich in the hallucinogen psilocybin. These are among the most abundant elements on all of demeter, but this sub-continent in particular sports a surplus beyond normal convention elsewhere on this world; makes this location uniquely stable in comparison to more turbulent locales. This abundance of silver is due to the resin produced by a local species that creates a liquid epoxy (Bisphenol A Diglycidyl Ether or as it’s more commonly called BADGE) that naturally chelates silver ions along with production of psylocybin. While such a potent hallucinogen is tempting, it requires heavy filtration to make potable to researchers (both because of the local proteins AND the arsenic). A laborious task that took all of seven months for a team of bored industrial chemists from Auberon, Bara Gaon, and a couple dozen belters; to find a workaround to make it ingestible.
While the land touching the ocean to the north and west of this region is primarily silver-antimonies most rich in arsenic, the south and eastern undercarriage are formed from the more brittle metal carbonates supported by the Carbonated “Soda Sea” directly beneath it. The abundant carbonation is due to decarboxylation of ketones produced by the many species reliant on ketogenesis in this sea. The southern portion of this landmass is almost tolerable to human lungs after heavy filtration. The high wind and crashing of waves makes this a rich location for aeroplankton looking to take flight, so breathing open air is a quick way to be infected by alien bacteria. Demeter’s significantly higher atmospheric density compared to earth makes this planet rich in potential for organisms that can survive in open air, possibly living most, if not all of their life cycle in clouds and the wind of storms. This, along with the Janus Pass, are among the best places to study the very species that take advantage of this ecological strategy of taking flight.
Fomorii Wastes (North-Polar Ocean) (Rich shallow seas and high nutrients, with the deepest reaching hydrothermal fields of this young strange world)
Named by the first exploration team’s lead geologist Fayez Sarkis and bio-chemist Ahmed O’Connell, after the Monstrous creatures of old Celtic pre-Christian myths, the microbiomes of this Ocean occupies the northern temperate and polar regions, along the top of the world continent. This ocean stretches into the temperate and equatorial regions at the Balorian Hydrothermal fields to the west of the supercontinent. Otherwise, this ocean remains primarily in the region of this world covered by its northern glacier caps. Shallow seas offer ample opportunities for phototrophic life, making for colorful “False-kelp Forests” of microbial life in shades of pink, orange, and purple.
This also houses the polar home-base that can act as the communications hub that human resources uses to coordinate the various deployments and financing. It is the most stable meteorologically, but the most turbulent politically, as most leadership is concentrated here, where most meetings and higherups of collected.
The Titan’s Teats (Equatorial-North Temperate Mountains) (phosphate volcano north, and sturdy solid landmass south rich in lead and zinc phosphates)
This dual set of mountains houses the highest altitude mountains of Demeter, specifically “Emerald Olympus” (Which is actually primarily composed of pyromorphite and not true emerald) and the lake at its tip called “Apollo’s Pride” in the hollow of the mostly dormant phosphate volcano. The seeping phosphate in the rivers that run from this lake react with the high lead minerology of Emerald Olympus to form the pyromorphite that contributed to its confusing name.
The southern lesser mountain of “Atlas Isle” to Olympus’ south is a hunk of lead and titanium that has gradually been chemically altered by the phosphate leakage from its northern neighbor to instead compose its exterior from mostly zinc and tin minerals. Sitting between the carbonated “Soda Seas” to the west and the Naiad Sea of the Dionysian Goblet to it’s south and west, the lead and titanium ions are pulled from much of the exposed rock and replaced by elements more vulnerable to acidic decay.
Helm of Athena (Western Equatorial Narrow Continent) (high Tin and Zinc rich with silicates and carbonates)
This small outlet sub-continent at the southwestern tip of the narrow silver spine composes the western-most tip of the supercontinent, putting itself at the midway point between the acidic and alkaline oceans of demeter’s equatorial waters. This is considered more moderate and safe in terms of both climate and conditions. Even the arsenic rich hydrothermal fields of “Cethlenn’s Ill Portents” are miniscule in comparison to the fields located north and are quickly sequestered in the acrylic resin many intertidal hive-building species produce obsessively. Other resin producing species to the south are blue with psilocybin, creating another economic niche for bored scientists looking for chemical distractions during their off-hours.
Dionysian Goblet (Prime Meridian Tipsy Ocean) (series of ethanol-rich seas due to high count of fermentation bacteria, with regular storms and ozone clouds)
The series of seas that makes up this ocean is enclosed in on all sides but the southwest corner at the prime meridian of demeter. Its name is owed to the unusually high concentration of ethanol in these seas, hypothesized by lead exobiologist Elvie Okoye to be the product of the many microbes in these seas favoring alcohol fermentation as their primary metabolic strategy. This chemical makeup is believed to be the source of the constant storms and hurricanes that plague these strange seas.
After this discovery, it took all of seventeen days for some Illusian biochemist to concoct a filter to make it safe for consumption. Since then, it has become common practice for the majority of the research teams to partake after a long work-day. Many different “flavors” are available based on location and season, and a bustling economy that many higher-ups in management have been very careful to pretend not to notice. On rainy days, what else is there to do but stay in, watch the storm, and drink with colleagues.
In contrast, to such unfortunate weather, these seas still however provide the most protection from UV light on this world that still lacks a fully formed ozone layer, thanks entirely to the ozone clouds produced by these “Tipsy Seas” as some have taken to calling them.
Predictably, this makes it one of the safest and most desired postings on Demeter for researchers to request as assignment. Should you be long-lived enough to survive the astronomical waiting list, or well-connected enough to skip the line, this habitat makes for one of the few locals where researchers are welcome to traverse the outside terrane when typhoon season subsides (though still a vac-suit for proper air and isolation from native life is heavily advised).
The Phantom’s Limb (Equatorial-North Temperate plateau and mountain range) (Copper/Iron Desert Flats)
This massive plateau and mountain range are composed of soft metal silicates and phosphate minerals, with especially rich lithium and copper veins intersecting the many rivers that flow through this stretch of the supercontinent. The plateau stretching into the goblet itself is especially recent, as evidence indicates that it only recently breached the ocean surface after a rise in oxygen levels led to global cooling and dropping sea levels as glaciers form at the poles. This has made it the primary base of operations, and the region from which all incoming researchers and workers land when they make landfall, as there was minimal life occupying this region as a newly surfaced landmass.
Womb of Mefetis (North Temperate-Polar Eastern-Most Continent) (desert plateaus, salt basin desert, acid lakes)
This portion of the supercontinent and its subsequent microbiomes are simultaneously the most dangerous and most fascinating place on all of demeter, and the primary reason for the urgency of researching this strange world. To both biologists and geologists, this region holds the record for the most ongoing research projects, and to a casual viewer the most visually dazzling place on this planet that leaves no doubt how alien it is in comparison to earth. The only place on earth that remotely resembles this local is the Danakil depression of Ethiopia or old faithful of Yellowstone. It is primarily composed of a low altitude desert composed almost entirely of salts rather than sand, dotted with cavernous cenote of technicolor sulfuric acid lakes. These lakes (as best can be told from our most recent efforts to map the cave system beneath) stretch for miles down in mineral formations invoking visions of chetaluga cave or the paintings of Heironimus Bossche. On earth such locations are almost always the product of purely abiotic factors, but here on demeter, this seems to be the product of a number of related species of bacterial analogues that act photorophic-decomposers. This Phyla of Demetarian life have been dubbed “Ydra,” after the Greek root word for the mythical Hydra, a multiheaded beast slayed by Hercules, said to spit acid. This name is due to not just the concentrated sulfuric acid they produce, but their ability to reproduce by way of “Ternary Fission,” a method of producing three identical offspring at once in contrast to the two identical daughter cells produced by the method of binary fission found across all kingdoms of life descended from earth. This, along with the astronomical radiation levels thanks to Mount Forge to this region’s southwest, makes Ydra a metaphorical holy grail for the future of cancer research, prolonging lifespan, and preventative treatment for telomere degradation.
Ogma’s Canal – (East-Equatorial Brine River, stretching from the Boiling Passage to the De Danann Ocean, and ending at the Dungeons of Brigid)
This brine river carves into the sea floor and stretches thousands of miles to drain into the Dungeons of Brigid and fill connand’s inverted tower. This leak is the early warning sign of the gradual leak of sulfate salts and acids from the womb of mefetis, facilitating the urgency for the research teams to catalogue this strange world’s life before the cataclysm that will be unleashed when the world oceans flood lake lernea. The lakebed itself forms deep-stretching cave systems connecting the various acid-cenote pools, thickly saturated with salts, solidifying into massive salt deposits. This brine river formed when one of those salt veins broke to the surface in boiling passage to its south.
1. The Caesium Halocline Interface
- Chemistry: Caesium Chloride and Sulfate.
- Conditions & Aesthetics: A completely colorless, highly refracting zone. Because caesium has an immense atomic mass but its salts form exceptionally low-viscosity solutions in water, this layer acts as a shimmering, watery optical illusion. To an uncalibrated probe, it looks like normal seawater but possesses a much higher density 1.25g/cm. It shields the open ocean from the toxic hellion below.
2. The Zinc-Iron Sulfate Band
- Chemistry: Concentrated Zinc Sulfate and Iron(II) Sulfate.
- Conditions & Aesthetics: A glassy, pale green fluid layer. Here, density creeps up toward 1.4 g/cm. The temperature rises sharply from ambient ocean temperatures to roughly 70 degrees Celsius due to the geothermal heat trapped by the density gradient above.
3. The Manganese-Copper Halide Layer
- Chemistry: Saturated Copper(II) Chloride and Manganese(II) Chloride.
- Conditions & Aesthetics: A thick, oily, green to teal fluid. The complete lack of calcium allows these transition metals to reach concentrations unheard of in Earth geology. Hydrolysis of the copper halides begins to strip hydroxyl ions from the water, causing the pH to plunge directly to 2.0 (hyper-acidic).
This assignment is a dream come true for both disturbance and restoration ecologists, as it puts the early signs of the coming cataclysm under a microscope and lets them monitor the early signs of what is to come for this strange world. This is for those dedicated and serious about this mission, and it positions them as those monitoring the life-signs for this terminal ecosystem. When, not if but when, this world enters its death throes, it will be those positioned here that determine when this world must be evacuated for the safety of the crew.
Connand’s Inverted Tower – (Northeastern Polar Brine Pool) (Acidic, and highly stratified with a variety of salt layers making a multilayered brine pool where each layer is separated by the conditions of the water directly above)
This is a massive pit that, true to its name, plunges downward like an inverted sky scraper. Like a solution spun through a centrifuge, each layer of this stratified brine pool increases in density dramatically with depth, and houses unique chemical properties for each layer. The absence of alkaline earth metals like magnesium and calcium allows heavy transition metals and rare alkali elements to form an incredibly crisp, hyper-dense fluid column.
The top layers are the ones we discussed in Ogma’s Canal, but the depth of this pit creates new layers beneath:
4. The Barite-Anglesite Pandemonium
- Chemistry: Saturated Barium Chloride and Lead(II) Chloride solution, suspended over a dense porridge of precipitating barite and anglesite.
- Conditions & Aesthetics: A turbid, milky, opaque layer. As trace sulfate ions circulate downward from the upper ocean, they instantly react with the ascending barium and lead currents from the mantle. This triggers a nonstop chemical precipitation, making this layer look like a blinding, heavy snowstorm locked inside a liquid medium.
5. The Radiolytic Uranyl Sump
- Chemistry: Super-saturated Uranyl Chloride Radium Halides, and heavy radioactive decay complexes.
- Conditions & Aesthetics: A sluggish, ultra-dense fluid slurry boiling at temperatures exceeding 180 degrees Celsius. It glows with a self-sustaining, brilliant neon-lime luminescence. The sheer volume of Uranium-238 in the basement rock bathes this sump in intense ionizing fields, continuously splitting the surrounding brine via radiolysis into hydrogen and oxygen gasses that bubble up through the "snow" layer like an effervescent cauldron.
For prospective exobiologists studying the fringes of Connand's Tower, understanding cellular transport on Demeter requires discarding Earth textbooks entirely. On Earth, arsenic compounds are highly cytotoxic because they act as chemical mimics. Arsenate uncouples ATP synthesis by impersonating phosphate, while inorganic arsenite disrupts voltage-gated potassium channels, leading to instant systemic failure
However, on Demeter, where arsenic is vastly more abundant than potassium, native life has flipped this evolutionary paradigm:
- Arsenic as the Primary Electrolyte: Demeter’s extremophiles utilize trivalent and pentavalent arsenic complexes as their principal intracellular cations and osmotic regulators. Their cellular machinery is natively tailored to the ionic radius and kinetic properties of arsenic.
- Potassium as the Lethal Neurotoxin: Because their voltage-gated ion channels are structurally mapped around arsenic pathways, potassium acts as the blocking agent. If an alien microbe or complex organism from Demeter is exposed to trace potassium, the foreign ion jams their membrane channels, instantly arresting their bio-electric nervous or metabolic cycles.
- Field Protocol: When gathering biological samples from the caesium halocline, exobiologists must ensure all sampling equipment is entirely stripped of terrestrial potassium residues. Introducing even a fingerprint's worth of Earth-standard sweat can cause immediate cellular lysis and death in native specimens.
The Janus Pass (Equatorial Mid-East Land-Bridge) (Epitomized by dividing basic and acidic, low and high salinity, and cold and hot oceans of this world)
This narrow land-bridge sits between the alkaline and stable ocean of the Goblet and the Turbulent and violently acidic seas to the eastern ocean, with its sulfate brine rivers, such as Ogma’s Canal and Orna’s Edge. The sudden drastic temperature fluctuations creates tornados and typhoons, making this habitat even more opportune for aeroplankton taking flight than the silver spine. The vulcanism of mount forge, responsible for the formation of this land bridge and dividing the world oceans, pumps out a surplus of ionizing radiation since 2% of demeter is uranium-238. This fragile divide however wears thinner every year, and a collapse of it is sure to occur within our lifetime, triggering a mass extinction. This is one reason for the rush to catalogue and classify the life of demeter before it’s tree of life has who knows how many branches sheared off permanently.
De Danann Ocean (Southeastern Temperate Ocean) (Acidic and salty, rich with brine rivers and hydrothermal fields)
This ocean exists directly east and south of the Womb and is directly influenced by the acidic inland. It plays host to Ogma’s Canal and a series of rainbow hydrothermal fields that give an average pH several orders of magnitude lower than the alkaline seas of the Dionysian Goblet. The life found in these waters is largely underpopulated compared to other oceans, but house unique extremophiles that become so well-adjusted to these hostile conditions that they are often unable to survive elsewhere. Many haloarchaea of earth’s tree of life are unable to survive freshwater or even oceanic conditions because of the low salinity compared to what they have become accustomed to. This is much the same on demeter, where the runoff of Ogma’s Canal makes seas and habitats within this ocean drastically different from those found in the fomorii wastes, Dionysian goblet, or the last we will explore, the howling abyss.
Clubfoot of Hephaestus (South-Temperate Mid-Eastern Sub-Continent) (Carbonate Volcano and Carbonated Lakes)
This unfortunately shaped sub-continent has also been nicknamed “Demi’s Dong” by many researchers and visitors alike. Its most fascinating feature is it’s carbonated lakes formed by underground vents and runoff from the semi-dormant carbonate volcano, positioned at the ankle (or upper scrotum for the vulgar). The lakes and close proximity to the Dionysian Goblet makes this a popular runner-up for the many unfortunate enough to miss out on that assignment.
Where it exceeds the Goblet, however, is in the rich opportunity for both geological and biological research. The carbonated and alkaline chemistry inland contrasted with the ethanol silicates to the northwest and acid-rich seas to its northeast make it the meeting point for opposite environmental forces, and the life found to maintain the balance here have already played host to hundreds of post-doctoral theses and dozens of patents in environmental engineering.
Elatha’s Golden Locks
Abyssal Plains like these are the oceanic equivalent of deserts: vast swaths of surface bereft of nutrient or energy sources. The key difference between these sea deserts and land ones is the concept of “marine snow.” This creates the sole source of energy that is fed to these habitats and make up the fields of ooze that serve as the transitional zones between the opulent reefs and shallow seas, and the deep brine or hydrothermal habitats found at the deepest depths of this strange world.
Naturally this is one of the least sought-after assignments on demeter, as well as a place that those who have pissed off the wrong person get sent. It creates a dichotomy of troublemakers and undesirables who are some of the biggest customers for the grey economy of demeter. Since the Janus Pass is much more heavily monitored by the security services, smugglers who operate in sending Dionysian distillations to other sites on the planet operate through here, operating under the logic of “the last place anyone would look.” Many of the deep-ocean probes meant to be taking sediment samples are re-tasked to carry orders intended for the helm, spine, or womb to hand-off points. Since local security is also likely here as a disciplinary punishment, they are often happy to ignore such inconsistencies in the equipment logs, so long as they receive their cut.
Howling Abyss (South-Polar and Mid-Western Equatorial Ocean) (abundant abyssal plains and lifeless depths)
This is in many ways the final frontier of Demeter and overlooked by many for its seemingly barren micro-biomes. While it is true that much of this region is unoccupied abyssal plains, there are likely many lifeforms yet to be discovered beneath the glacial ice. This region is also often seen as a first stage for many new recruits and researchers before they can get their bearings and achieve placement elsewhere.
However, there are some who never leave, and insist that there is much yet to be uncovered in this underestimated posting.