Skip to content
Xha’Ruun

Thexar-VII: The-Xa — Sha-El 12: Mor-Thal Xa-El — Extinction Events

"Five times everything died. Five times everything returned. The final crisis — the last — we stopped ourselves. The memory of the five holds us." — Law of the Keepers of Biodiversity, +2,100 Y.E.


Ruun-ak rass: → rhu [Thexar-I, Ruun 12, "Geological Evolution"], → rhu [Thexar-I, Ruun 20, "The Origin of Life"], → rhu [Thexar-VII, Sha-El 11, "Evolution Patterns"], → rhu [Thexar-II, Sha-El 04, "The Era of Crisis"]. Mor-ven: Théxar has recorded five major biological crises across 4.2 billion cycles — Oxygen, Volcanic, Glacial, Impact, and the incomplete Anthropogenic (Mor-Thal Xa-El). The sixth was stopped by the Xha'Ruun civilization; since +2,100 Y.E. no species extinction has been recorded, a record of 1,928 cycles.


Traces of an earlier biosphere
Traces of an earlier biosphere

12.1 Criteria of a Mass Extinction

Criterion Threshold Note
Species lost >50% Of the total number that existed
Duration of the crisis <2 million cycles Period of elevated mortality
Global scale All continents Excludes local catastrophes
Trace in the geological record Layer boundary Sharp change of the paleontological complex
Recovery of diversity >10 million cycles Time to return to the pre-event level

12.2 The First Extinction: The Oxygen Catastrophe

Date: 4.0–3.8 billion cycles ago | Duration: ~200 million cycles | Cause: Free O₂ accumulation | Lost: ~40% of anaerobic species

Before the event, atmospheric O₂ was <0.02%; life ran on H₂S chemosynthesis. About 4.1 billion cycles ago the first oxygenic phototrophs appeared.

Time (billion Y.A.) O₂ in the atmosphere Consequence
4.1 0.02% First oxygenic phototrophs
4.0 0.5% Beginning of the extinction of methanogens
3.9 3.8% Oxidation of Fe²⁺ in the oceans, red oozes
3.8 12% Formation of the ozone layer, end of anaerobic dominance

Consequences: ~40% anaerobe extinction; survival in refugia (hydrothermal vents, ocean depths); ozone layer formed; aerobic respiration (18× more efficient) established. Occurred 1.6 billion cycles earlier than on Earth but was gradual enough to allow adaptation.

12.3 The Second Extinction: The Volcanic Catastrophe

Date: 1.8 billion cycles ago | Duration: ~1.2 million cycles | Cause: Super-eruption, global winter | Lost: ~55%

Intense plume volcanism built the traps of Vaal-Kharak, the predecessor of modern Kharak. Repeated eruptions and gas releases changed conditions on land and in the ocean for a long time.

Atmospheric release: SO₂ 6.1×10¹⁴ ru; H₂S 2.8×10¹⁴ ru; CO₂ 1.4×10¹⁵ ru; volcanic dust 3.2×10¹⁵ ru. Sulfate aerosol blocked 68% of sunlight for up to 800 cycles; surface T fell 18°X; photosynthesis shrank 84%.

Consequences: 62% of primary producers extinct; cascading loss to fifth trophic level; ocean pH fell to 7.2; reef systems collapsed; deep-water chemosynthetic refugia survived. Recovery: 42 million cycles.

12.4 The Third Extinction: Total Glaciation

Date: 900 million cycles ago | Duration: ~0.8 million cycles | Cause: "Snowball Théxar" | Lost: ~65%

Trigger: falling CO₂ (to 180 ppm), continents near equator, ice–albedo feedback. At maximum (890 million Y.A.) the entire surface was ice-covered up to 1,200 sha thick.

Parameter Before Maximum After
Average surface T +13.6°X −41°X +10.2°X
Ice cover 18% 100% 24%
Photosynthesis (% of normal) 100 0.4 82
Planet biomass 1,340 Gt C 31 Gt C 940 Gt C

Exit: CO₂ accumulated under ice over 18 million cycles to 6,800 ppm, triggering rapid (~80,000 cycles) deglaciation. Terrestrial species hit hardest; multicellular radiation and first large predators followed.

12.5 The Fourth Extinction: Impact

Date: 250 million cycles ago | Duration: <0.5 million cycles | Cause: Asteroid ~3 mo diameter | Lost: ~70%

An asteroid 3.05 mo fell into the Gharra Ocean. Impact energy: 8.4×10²³ J (≈200 million Mt TNT).

Consequence Scale
Crater 65 mo diameter (today the Thash Trench)
Tsunami Up to 2,440 sha high
Release into the atmosphere 1.2×10¹⁶ ru of rock, dust, water vapor
Fires 38% of the planet's forests burned
"Impact winter" 15 cycles
Temperature (fall) −22°X in the first 2 cycles

Three-stage mechanism: mechanical impact (0–10 days) → impact winter (0–15 cycles) → CO₂ greenhouse phase +8°X (15–2,000 cycles). Largest fauna extinction in planet history; 8 orders of the Thermochromadae vanished; radiation of the ancestors of the Xha'Ruun followed (240–180 million Y.A.). Only extinction of the five not tied to internal planetary dynamics — a random event that set the path to reason.

12.6 The Fifth Extinction: Anthropogenic (Incomplete)

Date: −2,100 – −750 Y.E. (Crisis Era) | Duration: 1,350 cycles | Cause: Xha'Ruun activity | Lost: ~12% (stopped)

Factor Mechanism Scale
Deforestation Agriculture, fuel 34% of forest cover destroyed
Overfishing Unrestricted fishing Marine fauna biomass −62%
Pollution Industrial runoff 18% of rivers dead
Urbanization Growth of cities 2.4% of land built over
Hunting Uncontrolled hunting 8 species of large herbivores exterminated

Turning point: in −1,200 Y.E. the Guild of Natural History warned regional rulers of collapse within 600 cycles. Reform sequence: −1,150 Law on Protected Territories (12% of land); −980 ban on uncontrolled logging; −840 fishing quotas; −750 Treaty of Unity (union of eight regions).

Result: extinction stopped. The survey of 4028 reported no species disappearance; 8 species reintroduced (including the Ghal-thass, restored +2,850 Y.E.); forest cover restored to 40% (+12% over 500 cycles). The only stopped extinction — absent from the geological record, present in cultural memory as the Lesson of the Crisis.

12.7 Patterns of the Extinctions

Extinction Cause Lost Recovery Surviving groups
I (Oxygen) Biogenic 40% 120 million Y.A. Aerobes, refugia
II (Volcanic) Geological 55% 42 million Y.A. Chemosynthetics
III (Glacial) Climatic 65% 38 million Y.A. Deep-water
IV (Impact) Cosmic 70% 24 million Y.A. Small generalists
V (Anthropogenic) Biogenic 12% (stopped) — All except large specialists

Common patterns: (1) selection against specialists; (2) deep-water chemosynthetic refugia survived all five with minimal loss; (3) large forms (>100 kh) went extinct 3.4× more often than small (<1 kh); (4) recovery time scales with severity (10–40 million cycles); (5) each event opened new adaptive radiation — Thermochromadae after IV, primate-analogues after III. "Rule of Five": one extinction per 840 million cycles — close to the frequency of Wilson supercycles.

12.8 Lessons for the Management of the Biosphere

Principle Justification
The "six steps" principle Assessing consequences 6 generations ahead
The 12% rule No less than 12% of land — reserves
The sustainable catch law Taking no more than 68% of the annual increment
The ban on destroying species Even "useless" ones — they may prove key
Reintroduction The duty to restore species extinct through the civilization's fault

Ruun Ven

  1. Five mass extinctions occurred in 4.2 billion cycles: Oxygen (40%, 4.0 Ga), Volcanic (55%, 1.8 Ga), Glacial (65%, 900 Ma), Impact (70%, 250 Ma), Anthropogenic (12%, −2,100 – −750 Y.E., stopped).
  2. The Impact extinction was the largest (70%) and the only one triggered externally; it opened the niches enabling the radiation of the Xha'Ruun ancestors.
  3. Deep-water chemosynthetic refugia survived all five events, and specialists and large forms (>100 kh) died 3.4× more often than small generalists.
  4. The Fifth (Anthropogenic) extinction is the only stopped one — absent from the geological record, preserved in cultural memory as the Lesson of the Crisis.
  5. The survey of 4028 reported no species extinction has been recorded on Théxar — a 1,928-cycle record maintained by the Keepers of Biodiversity.
  6. Modern ecological ethics rest on five principles: six-steps foresight, the 12% reserves rule, the 68% sustainable catch law, the ban on destroying species, and mandatory reintroduction.