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Xha’Ruun

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.


The underwater forest of Thalas
The underwater forest of Thalas

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

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

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

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:

  1. Théxar has 10 terrestrial and 5 marine biomes with a total primary production of ~120 Gt C/year.
  2. The sulfur cycle is the key difference of Théxar's ecosystems; H₂S participates in metabolism on par with carbon.
  3. Endemism is highest in deserts (42%), mangroves (45%), and inland waters (52%).
  4. Cave ecosystems — the largest underground biomes on the planet (33 thous. мо², 95% endemism).
  5. Equatorial jungles are five-layered, with H₂S air-filtration in lower layers.
  6. Great Migration of Ghal-Shar — up to 4 million individuals, 305 мо, twice a year.

Connections to other chapters: