Chapter 21: Ecosystems of Théxar
"The Great Harmony is not a metaphor. It is an accurate description of how life is arranged. Every leaf, every beast, every microbe is part of a pattern that existed before us and will exist after." — From the treatise "Principles of Unity," Archive of the First Library
Related sections: → see [Ch.11, "Ecology"], → see [Ch.17, "Flora"], → see [Ch.18, "Fauna"] Key principle: Théxar demonstrates 10 major biomes, from equatorial jungles to polar deserts. The key difference is the sulfur cycle, linking geological, biological, and atmospheric processes into a single system.

Introduction
Théxar's ecosystems are the product of 4 billion cycles of evolution under an orange star, active tectonics, and a sulfur-rich biosphere. The fundamental difference of Théxar's ecosystems is the presence of a sulfur cycle (H₂S), parallel to the carbon cycle and playing a dominant role in a number of biomes.
Théxar has formed 10 major terrestrial biomes, 5 marine, and 3 unique ecosystems (hydrothermal vents, cave systems, subglacial lakes) without direct analogs.
21.1 Ecosystem Classification
21.1.1 Major Biomes
TABLE 21.1: Biomes of Théxar
Biome Productivity (t C/ha/yr) Biomass (Gt C) Endemism Moist jungles 18–22 820 35% Savannas 8–12 380 18% Temperate forests 10–14 580 24% Taiga 4–6 210 28% Deserts 0.5–1.5 12 42% Steppes/grasslands 6–10 95 15% Tundra 1–2 22 30% Glaciers <0.1 0.1 — Anthropogenic — — — Mangroves 8–12 48 45% Inland waters 4–8 35 52%
21.1.2 Sulfur Cycle
The sulfur cycle is the key difference of Théxar's ecosystems; on Théxar, sulfur is a full-fledged analog of nitrogen in biogeochemical cycles.

Théxar sulfur cycle
- Atmosphere
H₂S: 0.0008%
- Biosphere
H₂S becomes organic S
Chemosynthesis: H₂S + CO₂ produces organic matter
Photosynthesis: S-amino acids
- Soils/Ocean
Sulfates: SO₄²⁻
FeS₂ (pyrite); dissolved H₂S
- Lithosphere
FeS₂, CaSO₄, S°
Mantle sulfur
- LithosphereVolcanic emissionsAtmosphere
- BiosphereBiogenic emissionAtmosphere
- BiosphereMineralizationSoils/Ocean
- Soils/OceanAssimilationBiosphere
- LithosphereLeachingSoils/Ocean
- LithosphereVolcanic degassingSoils/Ocean
Fig. 21.1. Sulfur cycle of Théxar.
21.2 Trophic Levels
21.2.1 Producers
Primary production of Théxar's ecosystems is estimated at ~120 Gt C/year. The reason for high productivity is more efficient photosynthesis (4.2%).
| Producer group | Contribution | Mechanism |
|---|---|---|
| Terrestrial plants (forests) | 58% | Chromophyll photosynthesis |
| Phytoplankton (oceans) | 28% | Chromophyll + phycobilin |
| Chemoautotrophs (H₂S) | 8% | Chemosynthesis (hydrothermal, soils) |
| Algae (freshwater) | 4% | Chromophyll |
| Other (cryptoendoliths) | 2% | Chemosynthesis + photosynthesis |
21.2.2 Food Chains
Grazing chain (Kharak savannas):

Grassland food relationships
- Chromophyta (grasses)food transfer toGhal-Shar (herbivore, 2nd level)
- Ghal-Shar (herbivore, 2nd level)food transfer toShar-Ghar (predator, 3rd level)
- Ghal-Shar (herbivore, 2nd level)scavenging branchRhu-Hopper (scavenger)
- Shar-Ghar (predator, 3rd level)rarely feedsTor-Mor (superpredator, 4th level)
Detrital chain (Vexar forests):

Litter food relationships
- Leaf litter (from Ven-Shar)food transfer toKhal-Burrower (detritivore) + Mycophyta fungi
- Khal-Burrower (detritivore) + Mycophyta fungifood transfer toRhu-Hopper (scavenger)
- Rhu-Hopper (scavenger)food transfer toVex-Thorn (predator)
21.3 Unique Ecosystems
21.3.1 Equatorial Jungles
Théxar's jungles are the most productive terrestrial biome. Located in the equatorial belt (0°–8° latitude) in southern Kharak and northern Rhuval.
Structure:
| Layer | Height | Closure | Species | Photosynthesis |
|---|---|---|---|---|
| A (emergent) | 60–85 m | <10% | 120 | Full light |
| B (main canopy) | 30–60 m | 85% | 2,800 | Partial shade |
| C (understory) | 5–30 m | 60% | 4,200 | Heavy shade |
| D (shrubs) | 1–5 m | 30% | 3,800 | Low light |
| E (forest floor) | 0–1 m | <5% | 1,200 | Minimal |
Characteristic adaptation — H₂S air-filtration: leaves of lower layers have stomata capable of absorbing H₂S directly from the air and using it in metabolism (compensation for low light).
21.3.2 Cave Ecosystems
Théxar's karst systems (especially on the Raal plateau, Rhuval) form the largest underground ecosystems on the planet. Total explored cave length — ~69,100 мо.
| Parameter | Value |
|---|---|
| Total area of underground ecosystems | ~33,000 мо² |
| Endemism | ~95% of species are endemics |
| Main energy source | H₂S + Fe²⁺ chemosynthesis |
| Average T | +51.9°X (stable ±0.3°X) |
| Largest cave | Thal-Ven (depth 3,460 ша, volume 871 million ша³) |
| Deepest | Khar-Deep (3,810 ша from surface) |
Cave ecosystems have been isolated from the surface for millions of cycles. Some species show complete loss of vision and pigmentation, replaced by developed electroreception and chemosensitivity.
21.3.3 Hydrothermal Oases
At least 12 hydrothermal vent fields have been discovered on the floor of Théxar's oceans. The largest:
| Field | Ocean | Depth | Vent T | Unique Feature |
|---|---|---|---|---|
| Tor-1 | Thalas | 3,900 ша | 232.7°X | Largest (0.33 мо²) |
| Thash-Deep | Gharra | 10,000 ша | 254.4°X | Deepest field on the planet |
| Gharra-Vent | Gharra | 5,850 ша | 213.6°X | Rich in sulfur and REE |
These ecosystems are living fossils, preserving the metabolic pathways of ancient Théxar.
21.3.4 Mangrove Forests
Théxar's mangrove ecosystems are distributed along the coasts of all three continents. Their key difference is silicon biomineralization of roots, allowing trees to grow in water with a high concentration of dissolved H₂S (up to 2.5× lethal for ordinary plants).
| Region | Area (мо²) | Dominant | Productivity |
|---|---|---|---|
| Southern coast of Kharak | 19,800 | Mangro-Ven | 12 t C/ha/yr |
| Thar Delta | 5,000 | Mangro-Khal | 9 t C/ha/yr |
| Rhuval coast | 13,200 | Mangro-Thal | 10 t C/ha/yr |
| Vexar bays | 11,600 | Mangro-Vex | 8 t C/ha/yr |
21.4 Seasonal Dynamics
21.4.1 Seasons on Théxar
Due to the small axial tilt (14.2°), seasonal changes are less pronounced:
| Zone | Winter T | Summer T | Amplitude | Precipitation (seasonality) |
|---|---|---|---|---|
| Equatorial | +60.3°X | +61.4°X | ~1.1°X | Uniform |
| Tropical | +54.9°X | +60.3°X | ~5.4°X | Dry/wet |
| Temperate | +47.3°X | +53.8°X | ~6.5°X | Moderate seasonality |
| Subpolar | +40.7°X | +47.3°X | ~6.5°X | Snow summer/winter |
| Polar | +31.5°X | +42.4°X | ~10.9°X | Minimum precipitation |
21.4.2 Migrations
The Great Migration of Ghal-Shar — the largest seasonal animal movement on the planet. Twice a year, herds totaling 2–4 million individuals cross the Central Plain of Kharak, following the seasonal rains.
| Parameter | Value |
|---|---|
| Population | 2–4 million individuals |
| Distance | up to 305 мо |
| Duration | 4–6 weeks |
| Speed | 5.1–7.1 мо/day |
| Mortality | 8–12% (predators, disease, old age) |
21.5 Invasive Species
With the development of intercontinental trade and transport, some species spread beyond their natural ranges:
| Species | Original Range | Invasive Range | Damage | Control Measures |
|---|---|---|---|---|
| Shan-Scale (desert) | Shan Desert | Rhuval plains | Displaces local species | Biocontrol |
| Khal-Burrower | Kharak | All continents | Soil aeration (beneficial) | Monitoring |
| Rhu-Crab (crab) | Rhuval | Vexar coasts | Damage to mariculture | Physical barriers |
Chapter Summary
Key conclusions:
- Théxar has 10 terrestrial and 5 marine biomes with a total primary production of ~120 Gt C/year.
- The sulfur cycle is the key difference of Théxar's ecosystems; H₂S participates in metabolism on par with carbon.
- Endemism is highest in deserts (42%), mangroves (45%), and inland waters (52%).
- Cave ecosystems — the largest underground biomes on the planet (33 thous. мо², 95% endemism).
- Equatorial jungles are five-layered, with H₂S air-filtration in lower layers.
- Great Migration of Ghal-Shar — up to 4 million individuals, 305 мо, twice a year.
Connections to other chapters:
- → see [Ch.11, "Ecology"] — overview ecology
- → see [Ch.17, "Flora"] — vegetation by biome
- → see [Ch.18, "Fauna"] — animals by ecosystem
- → see [Ch.13, "Continents"] — biome distribution
- → see [Ch.14, "Oceans"] — marine ecosystems